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
76934|Aberfeldy Basalt|66244|4|Described|p5.|Oligocene|Cenozoic|Originally named the Aberfeldy Province (Wellman 1974); a basalt flow from near Mount Gregory, preserved in remnants along the ridge from Aberfeldy to Beardsmore, then along three palaeovalleys from Rawson into the La Trobe Valley. Has a strong magnetic signature. Two K-Ar ages give and age of mid Oligocene, although degree of alteration suggests the flows could be older (Wellman, 1974).||||Is locally overlain by Haunted Hills Formation.|Alkali olivine basalt with lesser olivine tholeiite and hawaiite, and minor interbedded sedimentary rocks.|
76934|Aberfeldy Basalt|68116|5|Briefly described|Appendix, Maps 43, 52.|Aquitanian|Oligocene||||||Alkali olivine basalt, olivine tholeiite and hawaiite, with alkali olivine basalt being the most abundant; interbedded sedimentary rocks.|
27690|Acheron Volcanics|35186|6|Mentioned|Table.1|||||||||
27690|Acheron Volcanics|35277|3|Fully described|p90|||||||||
27690|Acheron Volcanics|39291|6|Mentioned|Table 1|||||||||
27690|Acheron Volcanics|41641|4|Described|p160|||||||||
27690|Acheron Volcanics|42726|5|Briefly described|map legend|||||||||
27690|Acheron Volcanics|42827|4|Described|p160|||see also Table 5.1||||||
98|Adaminaby Group|12100|5|Briefly described|p819|Middle Ordovician|Early Ordovician|Eastern Lachlan Fold Belt area; upward fining succession with an upward decrease in lithic content.||||||08-MAY-12
98|Adaminaby Group|13139|5|Briefly described|p9 Fig. 4|Middle Ordovician|Middle Ordovician|Geological Province: Rockley-Gulgong Volcanic Belt.||||||12-APR-05
98|Adaminaby Group|22472|5|Briefly described|p36|Ordovician|Ordovician|||||||
98|Adaminaby Group|22503|5|Briefly described|p645, Fig.3b|Ordovician|Early Ordovician|||||||
98|Adaminaby Group|22529|5|Briefly described|1|Early Ordovician|Early Ordovician|||||||
98|Adaminaby Group|22530|6|Mentioned|p693||Llanvirn|||||||
98|Adaminaby Group|22545|4|Described|p498-507, Fig.5||Ordovician|||||||
98|Adaminaby Group|22577|6|Mentioned|p120||Ordovician|||||||
98|Adaminaby Group|22624|5|Briefly described|p678, Fig.3 p679|Ordovician|Ordovician|See also Fig.4 p679||||||
98|Adaminaby Group|22628|6|Mentioned|fig1p108|Ordovician|Ordovician|||||||
98|Adaminaby Group|22679|3|Fully described|p 6|Ordovician|Ordovician|Lachlan Fold Belt. Overlain by Coombing Formation.||||||01-SEP-08
98|Adaminaby Group|22704|6|Mentioned|p63|||Also Fig6(b),p61. Previously Abercrombie beds||||||
98|Adaminaby Group|22708|5|Briefly described|p210|Ordovician|Ordovician|||||||
98|Adaminaby Group|22798|5|Briefly described|p856|Late Ordovician|Early Ordovician|||||||
98|Adaminaby Group|22815|3|Fully described|p18,19,122|Ordovician|Ordovician|Equivalent to Pinnak Sandstone.||||||30-OCT-14
98|Adaminaby Group|22832|5|Briefly described|Fig.1b p634|Ordovician|Ordovician|Quartz turbidite, See also p636.||||||
98|Adaminaby Group|22842|6|Mentioned|p25||Ordovician|||||||
98|Adaminaby Group|22857|4|Described|p112, p422 App. 1, Tb. A1.5|Early Ordovician|Early Ordovician|A turbiditic sequence of interbedded arenite-siltstone-shale/slate together with chert beds. Geological Province: Lachlan Fold Belt.||||||
98|Adaminaby Group|22876|5|Briefly described|p16|Early Ordovician|Early Ordovician|||||||
98|Adaminaby Group|22878|5|Briefly described|p29|Ordovician|Ordovician|||||||
98|Adaminaby Group|22879|5|Briefly described|map|Early Ordovician|Early Ordovician|||||||
98|Adaminaby Group|22880|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Includes: Pinnak Sandstone.||||||01-OCT-04
98|Adaminaby Group|22881|5|Briefly described|map|Ordovician|Ordovician|||||||
98|Adaminaby Group|22968|4|Described|P19, P99|Ordovician|Early Ordovician|Overlying unit is Bendoc Group.||||||04-MAR-09
98|Adaminaby Group|22971|5|Briefly described|p 17||Ordovician|of Lachlan Fold Belt.||||||
98|Adaminaby Group|23020|5|Briefly described|Map legend||Ordovician|||||||
98|Adaminaby Group|23021|5|Briefly described|Map legend|Ordovician|Early Ordovician|||||||
98|Adaminaby Group|23028|5|Briefly described|Map legend|Ordovician|Early Ordovician|Overlying unit is Bendoc Group.||||||01-SEP-08
98|Adaminaby Group|23029|5|Briefly described|Map legend|Ordovician|Early Ordovician|Overlying units are the Bendoc Group and the Kiandra Group.||||||01-SEP-08
98|Adaminaby Group|23030|5|Briefly described|Map legend|Ordovician|Ordovician|||||||
98|Adaminaby Group|23043|5|Briefly described|Map Legend|Gisbornian|Yapeenian|||||||11-JAN-10
98|Adaminaby Group|23100|5|Briefly described|p575 (Fig 1)||Ordovician|||||||
98|Adaminaby Group|23170|2|Defined|p29 Fig.3|Ordovician|Darriwilian|Age: Late Darriwillian (Ordovician) - Ordovician.||||||
98|Adaminaby Group|23181|5|Briefly described|p1,7||Darriwilian|formerly 'Lue Beds'. Age from conodonts in chert.||||||
98|Adaminaby Group|23202|6|Mentioned|Fig.1|||||||||
98|Adaminaby Group|23213|5|Briefly described|Fig.10 p24|Darriwilian|Darriwilian|Includes some Darriwilian fossils. of Rockley-Gulgong Volcanic Belt.||||||
98|Adaminaby Group|23214|2|Defined|p19|Ordovician|Ordovician|Includes rocks previously mapped as Adaminaby Beds/beds, Triangle Group and Abercrombie Beds. Type Section refer to Glen et al 1990. Age determined by fossil assemblages (Fell, 1984). Geological Province: Lachlan Fold Belt. Max. thickness: >1500m.||||||05-MAR-12
98|Adaminaby Group|23245|5|Briefly described|p112,134||Early Ordovician|||||||
98|Adaminaby Group|23307|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
98|Adaminaby Group|23309|5|Briefly described|p53-58 Fig 1.3||Ordovician|||||||
98|Adaminaby Group|23327|4|Described|1009|Ordovician|Ordovician|||||||
98|Adaminaby Group|23329|6|Mentioned|1042|Ordovician|Ordovician|||||||
98|Adaminaby Group|23334|5|Briefly described|9 Fig.4|Ordovician|Ordovician|||||||
98|Adaminaby Group|23335|5|Briefly described|p15 Tb. 1, p19|Ordovician|Ordovician|||||||
98|Adaminaby Group|23464|5|Briefly described|p245|Ordovician|Ordovician|||||||
98|Adaminaby Group|23541|5|Briefly described|p398|||also see p396 Fig 1. In the Lachlan Fold Belt||||||
98|Adaminaby Group|23615|6|Mentioned|p64|Ordovician|Ordovician|||||||
98|Adaminaby Group|23850|5|Briefly described|p793|||||||||
98|Adaminaby Group|23860|5|Briefly described|p944|Ordovician|Ordovician|Overlying unit Bendoc Group.||||||
98|Adaminaby Group|23938|5|Briefly described|p11|Middle ordovician|Early Ordovician|Geological Province: Lachlan Fold Belt. See also p71 Fig. 25, p75 Fig. 27. .||||||
98|Adaminaby Group|24003|5|Briefly described|p258|Late Ordovician|Late Ordovician|||||||
98|Adaminaby Group|24004|5|Briefly described|p277|||||||||
98|Adaminaby Group|24006|5|Briefly described|p312|Ordovician|Ordovician|||||||
98|Adaminaby Group|24007|5|Briefly described|p336|Ordovician|Ordovician|||||||
98|Adaminaby Group|24037|6|Mentioned|p423|||Geological Province: Lachlan Fold Belt||||||
98|Adaminaby Group|24133|4|Described|p35|Ordovician|Ordovician|Formerly Adaminaby Beds.  Geological Province: Lachlan Fold Belt.||||||
98|Adaminaby Group|24142|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
98|Adaminaby Group|24143|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
98|Adaminaby Group|24144|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
98|Adaminaby Group|24145|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt||||||
98|Adaminaby Group|24146|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
98|Adaminaby Group|24177|6|Mentioned|p48|||||||||
98|Adaminaby Group|24215|5|Briefly described|p804 Fig. 3|||Geological Province:  Lachlan Fold Belt||||||
98|Adaminaby Group|24233|5|Briefly described|p253 Fig.1, p256|||Geological Province: Lachlan Orogen.||||||
98|Adaminaby Group|24317|5|Briefly described|p14, p15 Fig.1|Ordovician|Ordovician|||||||
98|Adaminaby Group|24329|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Includes the Hotham beds||||||
98|Adaminaby Group|24339|5|Briefly described|p47 Fig. 4|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt. Age: 445 +/- 2 Ma (Ar/Ar)||||||
98|Adaminaby Group|24383|6|Mentioned|p88 Fig.57|||Geological Province: Lachlan Fold Belt||||||
98|Adaminaby Group|24463|5|Briefly described|p319|||Overlain by Sofala Volcanics.  Geological Province: Lachlan Fold Belt.||||||
98|Adaminaby Group|24551|5|Briefly described|p96, p100|Middle Ordovician|Early Ordovician|Only includes Pinnak Sandstone in Victoria.||||||
98|Adaminaby Group|24575|5|Briefly described|p711|Middle Ordovician|Early Ordovician|Geological Province: Lachlan Fold Belt||||||
98|Adaminaby Group|24576|5|Briefly described|p727|Middle Ordovician|Early Ordovician|Geological Province: Lachlan Fold Belt||||||
98|Adaminaby Group|42294|4|Described|p24|||Intended as a redefinition to replace Adaminaby beds.||||||
98|Adaminaby Group|42712|4|Described|5, 12, 19|Late Ordovician|Early Ordovician|Previously called the Triangle Group. Overlain by and interfingers with Rockley Volcanics.||||||04-MAR-09
98|Adaminaby Group|43233|5|Briefly described|Map Legend||Early Ordovician|||||||11-JAN-10
98|Adaminaby Group|43312|5|Briefly described|Map Legend|||||||||
98|Adaminaby Group|43313|5|Briefly described|Map Legend|||||||||
98|Adaminaby Group|43314|5|Briefly described|Map Legend||Early Devonian|||||||
98|Adaminaby Group|43315|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Includes Pinnak Sandstone.||||||03-MAY-05
98|Adaminaby Group|43494|5|Briefly described|p8, p15|Ordovician|Ordovician|Consists of slaty white and purplish siltstone and fine-grained massive quartz sandstone, with some siltstone. Overlain by the Tucklan Formation.||||||09-MAR-06
98|Adaminaby Group|43633|5|Briefly described|p17||Early Ordovician|||||||
98|Adaminaby Group|43639|5|Briefly described|Map Legend||Ordovician|||||||
98|Adaminaby Group|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Consists of quartz sandstone, siltstone, slate, phyllite, black carbonaceous slate, chert.||||||15-JUL-08
98|Adaminaby Group|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Quartz sandstone, siltstone, slate phyllite, black carbonaceous slate, shale.||||||
98|Adaminaby Group|43782|5|Briefly described|Map Legend|Darriwilian|Yapeenian|||||||
98|Adaminaby Group|44093|5|Briefly described|p50|Ordovician|Ordovician|See also p189 and 190 Appendix 1.||||||
98|Adaminaby Group|44184|5|Briefly described|Map Legend||Early Ordovician|||||||
98|Adaminaby Group|44185|5|Briefly described|Map legend.|Middle Ordovician|Early Ordovician||||Includes Pinnak Sandstone.|||30-OCT-14
98|Adaminaby Group|44187|5|Briefly described|Map Legend||Early Ordovician|||||||
98|Adaminaby Group|50230|5|Briefly described|Map legend|Ordovician|Ordovician|Sandstone and siltstone.  Includes the Beacons Hill Chert.  Overlain by the Bendoc Group.||||||
98|Adaminaby Group|50231|5|Briefly described|Map Legend|Late Ordovician|Middle Ordovician|Includes: Beacons Hill Chert.  Underlies: Bendoc Group.||||||
98|Adaminaby Group|50232|5|Briefly described|Map legend|Late Ordovician|Middle Ordovician|Contains the Nattery Chert.  Overlain by the Bendoc Group.||||||
98|Adaminaby Group|50233|5|Briefly described|Map Lagend|Gisbornian|Ordovician|Overlain by the Bendoc Group.||||||
98|Adaminaby Group|50234|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes: Nattery Chert.||||||
98|Adaminaby Group|60503|5|Briefly described|p27, p28 Fig. 9|Early Ordovician|Early Ordovician|Includes Pinnak Sandstone and metamorphics. Turbidites; largely metamorphosed to schists and gneisses of biotite grade. Geological Province: Lachlan Fold Belt. See also p45 Tb. 2. ||||||
98|Adaminaby Group|60504|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Includes Pinnak Sandstone||||||
98|Adaminaby Group|60505|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Includes the Pinnak Sandstone||||||
98|Adaminaby Group|60506|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Includes the Pinnak Sandstone||||||
98|Adaminaby Group|60507|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Includes the Pinnak Sandstone||||||
98|Adaminaby Group|60508|5|Briefly described|Map legend|Ordovician|Ordovician|Includes Pinnak Sandstone.||||||20-OCT-04
98|Adaminaby Group|60536|6|Mentioned|p552|||||||||
98|Adaminaby Group|60542|5|Briefly described|p45|Early Silurian|Early Ordovician|In ORBOST is represented by only the Pinnak Sandstone, also referred to as Hotham slates and Mallacoota beds. Geological Province: Lachlan Fold Belt. ||||||
98|Adaminaby Group|60902|5|Briefly described|p859, p868|Early Ordovician|Early Ordovician|Includes Numeralla Chert. Craton-derived turbidites adjacent to Wagonga Group rocks. Overlain by Bendoc Group. Geological Province: Bega Terrane.||||||11-APR-06
98|Adaminaby Group|60904|5|Briefly described|p782|Middle Ordovician|Early Ordovician|Includes the Numeralla Chert. Sandstone.||||||
98|Adaminaby Group|60988|5|Briefly described|p144 Fig.1, p146|Late Ordovician|Late Ordovician|Includes rocks formerly known as the "Bombala Beds".|||||Undifferentiated sediments, turbidites, sandstone, mudstone, shale.|
98|Adaminaby Group|61160|5|Briefly described|p44, p35 Tb. 5.2|||Geological Province: Lachlan Fold Belt.||||||
98|Adaminaby Group|61161|5|Briefly described|p78, p76-77 Fig 6.1|Middle Ordovician|Early Ordovicioan|Includes mainly Pinnak Sandstone. Also been called Hotham Group, Hotham slates and Mallacoota beds. Geol. Prov: Lachlan Fold Belt.||||||
98|Adaminaby Group|61163|5|Briefly described|p7, p38 Tb. 6.2|Ordovician|Ordovician|Overlain by Bendoc Group. Geological Province: Lachlan Fold Belt. Variously named Hotham slates, Pinnak Sandstone and Mallacoota beds in different parts of the eastern LFB.||||||
98|Adaminaby Group|61164|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Includes Pinnak Sandstone.||||||05-MAR-12
98|Adaminaby Group|61165|5|Briefly described|map legend|Middle Ordivician|Early Ordivician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61166|5|Briefly described|map legend|Middle Ordivician|Early Ordivician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61167|5|Briefly described|map legend|Middle Ordivician|Early Ordivician|Includes Pinnak Sandstone.||||||07-FEB-11
98|Adaminaby Group|61168|5|Briefly described|map legend|Late Ordivician|Early Ordivician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61169|5|Briefly described|map legend|Middle Ordovician|Early Ordivician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61170|5|Briefly described|map legend|Middle Ordovician|Early Ordivician|Includes Pinnak Sandstone.||||||07-FEB-11
98|Adaminaby Group|61171|5|Briefly described|map legend|Middle Ordovician|Early Ordivician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61172|5|Briefly described|map legend|Middle Ordovician|Early Ordivician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61173|5|Briefly described|map legend|Middle Ordovician|Early Ordivician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61174|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Includes Pinnak Sandstone.||||||07-FEB-11
98|Adaminaby Group|61175|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61176|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61177|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61178|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61187|5|Briefly described|p4, p5 Fig.3, p26 Fig.2, p29 Fig.4. |Early Ordovician|Early Ordovician|Benambra Terrane. Correlative of Castlemaine Supergroup (Bendigo Zone, Melbourne Terrane).|||Includes Hotham beds and Pinnak Sandstone.||Mainly turbidite sandstones.|
98|Adaminaby Group|61413|5|Briefly described|p7, p46, p82 Fig.103.|Early Ordovician|Early Ordovician|Suggested term for Early Ordovician turbidites in southeastern Lachlan Fold Belt.|||Includes Numeralla Chert.||Turbidites.|
98|Adaminaby Group|61731|5|Briefly described|p1037, p1038 Fig.1c|Ordovician|Ordovician|Conformably overlain by Wagonga Group.||||||
98|Adaminaby Group|61762|6|Mentioned|p19 Fig. 2(a)||Ordovician|||||||
98|Adaminaby Group|61964|5|Briefly described|p20|||Similar in age and lithology (quartz sandstone turbidite sequences) to Wagga Group but separated by the Gilmore Fault Zone. However, for this study these sequences have been mapped as Wagga Group pending further work. In the eastern Lachlan Orogen.||||||
98|Adaminaby Group|62070|5|Briefly described|p34 Fig.1, p38, p39,|Darriwilian|Bendigonian|||||Overlain by the Bendoc Group.|Predominantly quartz-rich turbidite succession with minor chert horizons.|
98|Adaminaby Group|63283|5|Briefly described|p205, p206|Ordovician|Early Ordovician|Includes; Budhang Chert. Geological Province: Rockley-Gulgong Volcanic Belt and Kiandra Volcanic Belt.||||||07-FEB-11
98|Adaminaby Group|63285|6|Mentioned|p275 Fig. 2|||Geological Province: Molong Volcanic Belt. Consists of quartz-rich sandstone, siltstone, minor siliceous siltstone and rare black mudstone.||||||
98|Adaminaby Group|63286|6|Mentioned|p294 Fig. 1|||Consists of quartz-rich sandstone, siltstone and chert.||||||07-FEB-11
98|Adaminaby Group|63289|4|Described|p364, p369, p372, p374|Gisbornian|Darriwilian|Conformably overlain by Triangle Formation and Coombing Formation. Geol Province: Kiandra Volcanic Belt. Consists of metamorphosed quartz-rich turbidites. Age constrained by conodonts and graptolites. Multiply deformed. See p374 for petrological info.||||||02-OCT-15
98|Adaminaby Group|63290|5|Briefly described|p388, p395, p396 Fig. 3|Middle Ordovician|Ordovician|Includes; Numeralla Chert, Chakola Formation. Overlain by Bendoc Group in eastern subprovince. Sandstones in group are matrix-rich, quartz-feldspar-mica sandstones.||||||05-MAR-12
98|Adaminaby Group|63635|6|Mentioned|p39|||In NSW. Correlation between mainland Australia and Tasmania discussed.||||||
98|Adaminaby Group|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Includes the Abercrombie Formation with its one sandstone member and 3 chert members.||||||
98|Adaminaby Group|64295|5|Briefly described|p198 Fig. 1, p199|Middle Ordovician|Early Ordovician|||||||
98|Adaminaby Group|64616|6|Mentioned|p343 Fig.23|||||||||
98|Adaminaby Group|64826|5|Briefly described|p1037|Ordovician|Ordovician|Includes quartz-rich turbidites.||||||04-MAR-09
98|Adaminaby Group|65469|6|Mentioned|p20|||East of the Macquarie Arc, Lachlan Orogen. ||||||
98|Adaminaby Group|65900|5|Briefly described|p162||Ordovician|Tabberabbera Zone.  Turbidite, intruded by I-type granites.||||||10-MAY-12
98|Adaminaby Group|65969|5|Briefly described|p3, p13|||Overlies Heathcote Volcanic Group. Metaturbidites.||||||
98|Adaminaby Group|66087|6|Mentioned|p3 Fig. 2, p4 Fig.3|Ordovician|Ordovician|||||||
98|Adaminaby Group|66182|6|Mentioned|p323 Fig.5|Middle Ordovician|Early Ordovician|Turbidites.||||||11-MAY-12
98|Adaminaby Group|66185|4|Described|p397, p396 Fig. 1|Late Ordovician|Early Ordovician|Backarc extensional setting. Thin quartz rich psammites (turbidites), minor black carbonaceous shale units. A thick package between the Wyangala Granite and the Reids Flat and Wywurri Granites.||||||
98|Adaminaby Group|66196|5|Briefly described|p616,617|Middle Ordovician|Early Ordovician|Turbidites. Overlies the Howqua Chert.||||||
98|Adaminaby Group|66300|5|Briefly described|p17, p23, p52, 64.|Ordovician|Ordovician|Eastern Lachlan Orogen.||||Intruded by Lockhart Igneous Complex, Touga Granite, Tullyangela Granite.|Turbiditic sedimentary rocks.|24-OCT-13
98|Adaminaby Group|66713|5|Briefly described|p3 Fig.2, p3, p5, p10|||Quartz-rich, turbiditic sedimentary rocks. Underlies the Bendoc Group. Includes Abercrombie Formation.||||||
98|Adaminaby Group|67106|6|Mentioned|p681|||||||||
98|Adaminaby Group|67107|6|Mentioned|p686||||||||Quartz-rich turbiditic sedimentary rocks.|
98|Adaminaby Group|67322|4|Described|p2,p4 Fig.2,p5,p13,p15-16,p25,p28;Fig.5|Early Ordovician|Late Cambrian|Albury-Bega Terrane and Macquarie Arc. First named by Fairbridge (1953), according to Glen (1994); current definition dates from Glen et al. (1990). Green to grey-green laminated slates and siltstones interbedded with sandstones of variable thickness. Includes chert bearing fossils of late Darriwilian age. Has at least five distinct conodont-based zones. Maximum age from p20 Fig.5 (Strat. column). Occurs in the Cooma-Mallacoota region, and Sofala-Dunedoo-Mudgee and Canberra-Queanbeyan regions.|||Budhang, Mozart and Numeralla Cherts; Abercrombie, Pittman and Chakola Formations; Pinnak Sandstone.|Conformably overlain by the Coomber Formation and Bendoc Group. Equivalent to Pinnak Sandstone.|Turbiditic sandstone sequence punctuated by 2-3 prominent and regionally extensive chert-rich horizons, of which the lowermost is more sporadic, consisting of thinly bedded cherts, sometimes interlayered with turbiditic sandstones.|
98|Adaminaby Group|67802|6|Mentioned|p28, p30|Middle Ordovician|Lower Ordovician|Tabberabbera Zone. Sediment derived from the south and west.||||Is overlain conformably by Bendoc Group.|A thick pile of turbidites.|
98|Adaminaby Group|67803|4|Described|p34|Ordovician|Ordovician|This unit is split in two. The western half in the Wagga Basin is in situ. The eastern half (east of the Macquarie Arc) is allochthonous, constituting (with overlying shales) the Bega Terrane. Deposited as a submarine fan, draining the northern part of the Ross Orogen.||||||
98|Adaminaby Group|67820|6|Mentioned|p135|||Has a gross domal distribution in the Kiawarra and Murrumbateman areas; this and a gravity low suggest a concealed (?mineralising) granite body at depth.||||||
98|Adaminaby Group|67847|5|Briefly described|p19, p21, p22, p26 fig 4.2|Middle Ordovician|Early Ordovician|Lachlan Orogen. See also p27-p30, p54, p59.|||||Quartz-rich turbidites.|
98|Adaminaby Group|67849|4|Described|p21, p22, p23, p27, p30. |Middle Ordovician|Early Ordovician|Lachlan Orogen. Turbidite sequences. Dominant part of an westward-dipping accretionary complex in the Batemans Bay area. Kubler Index measurements show this unit experienced much the same metamorphic conditions as Wagonga Group. Underplating and associated metamorphism occurred c.460-440 Ma.||Unit in Narooma Accretionary Complex.||Conformably overlies, and interfingers with, Wagonga Group.|Includes sandstones and minor chert lenses.|
98|Adaminaby Group|68255|4|Described|p1049-p1059, p106-p1064|Givetian|Ordovician|Lower to Middle Ordovician. Sequences within this unit have reached lower greenschist metamorphic grade. Intruded by the Buckenbowra Granodiorite around 395.8 +/- 8.1 Ma.|> 395.8 +/- 8.1 Ma|||Lenses of this group interfinger the Wagonga Group. Intruded by the Buckenbowra Granodiorite. Unconformably underlain by the Comerong Volcanics and Merrimbula Group.|Comprises a monotonous sequence of turbidites and minor black shale comprising well-bedded quartzose meta sandstone, meta siltstone and slate.|20-JUL-15
98|Adaminaby Group|68309|5|Briefly described|p225-226, 232-233|Middle Ordovician|Early Ordovician|Tectonic slices occur in the Wagonga Group; emplaced by thrust faulting during subduction. Extends ~30km inland, W of Batemans Bay (Bega Terrane).||||Is overlain conformably by Wagonga Group (locally thrust-faulted against).||
98|Adaminaby Group|68466|5|Briefly described|p64-66, 70|Middle Ordovician|Early Ordovician|Albury-Bega Terrane.|||Numeralla Chert.|Is overlain by Bendoc Group.|Turbiditic sandstones and cherts.|
98|Adaminaby Group|68592|2|Defined|p269-319, p320, p323-5, p338, p344,|Middle Ordovician|Early Ordovician|See also xxiv, p71, p73 Tb.5, p136-7, p182, p230, p235, p241-2, p255, p348, p350, p355, p357, p361-3, p376, p384-5, p408-9, p411-3, p416, p421, p425-6, p443, p731, p743, p750, p771, p819, p835. Originally Adaminaby Beds of Fairbridge (1953) after Adamson (1955) and defined by Richardson (1979); divided into Adaminaby Group and Warbisco Shale by Glen et al. (1990). Adaminaby Group was defined by Lewis et al. (1994) incorporating Mallacoota Beds of Fenton et al. (1982). Reference areas described. Thickness estimated up to 5 km. Geophysical properties described. Frogmore, Wyangala, Peelwood, Goulburn and Bungonia structural zones: deformation and metamorphism described. Is intruded by Banshea Granite and Wyangala Supersuite. Quarried locally. Major source of sediment for Covan Creek Formation. Palaeontology detailed. Hosts gold mineralisation in the Dalton area; Pb-Ag-Zn at Rye Park (Wallah Wallah mine: detailed).|||Includes Abercrombie and Chakola Formations, Numeralla Chert and Pinnak Sandstone.|Is overlain conformably by Bendoc Group, unconformably (or faulted) by Bungonia Group, and unconformably by Shivering Conglomerate. Equivalent to Wagga Group and Girilambone Group.|Uniform sequence of interbedded, turbiditic, quartzose to lithic-feldspar-quartz sandstone, siltstone and mudstone; minor chert intervals.|
98|Adaminaby Group|68822|5|Briefly described|p334, p349, p351|||Overlain by an Upper Ordovician sequence. The youngest conodonts are Darriwilian 4-Gisbornian-1, based on the presence of Pygodus serra, P.anserinus and Periodon aculeatus.|||Includes the Pinnak Sandstone.|Overlain by the Bendoc Group.||
98|Adaminaby Group|69002|6|Mentioned|p13|||||||Overlain by the Bendock Group.||
98|Adaminaby Group|69159|5|Briefly described|Map legend|Ordovician|Ordovician||||Includes Abercrombie Formation.|||
98|Adaminaby Group|69270|6|Mentioned|p1, p4||||||Abercrombie Formation|||
98|Adaminaby Group|69539|6|Mentioned|p607-608|||||||||
98|Adaminaby Group|69541|5|Briefly described|p652-653|Late Ordovician|Early Ordovician|Top of the Group is early Gisbornian.|||Includes Chakola Formation.|Is overlain by Bendoc Group.||
98|Adaminaby Group|69564|5|Briefly described|p3|Ordovician|Ordovician||||||Stacked turbidites.|
98|Adaminaby Group|69668|5|Briefly described|p927, p929 Fig.2, p930 Fig.3, p931, p948|Middle Ordovician|Early Ordovician|Albury-Bega terrane. Geochemical similarity of cherts with those of the Girilambone Group suggests both regions shared identical sources and depositional regimes, occupying near-identical tectonic settings in a back-arc basin.|||Includes Abercrombie Formation, Numeralla Chert..||Turbiditic sandstones and cherts.|18-JUN-20
98|Adaminaby Group|69801|5|Briefly described|p98|Ordovician|Ordovician|Central Lachlan Orogen.||||Intruded by the Thologolong Granite.|Sedimentary rocks.|
98|Adaminaby Group|70026|4|Described|p37,39-41,49,51-p52|Ordovician|Latest Cambrian|Geological province: Lachlan Orogen. 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). Detrital zircon ages from the sandstone turbidites at Melville Point, NSW mainly in the ranges 600-500 Ma and 1200-1000 Ma, similar to those reported from Ordovician turbidites elsewhere in the Lachlan Orogen (Fergusson et al. 2013). Cambrian basaltic breccia unit and associated limestones occur adjacent to and within disrupted quartz turbidites at Burrewarra Point (Fergusson & Frikken 2003).||||Underlain by (or interfingers with) Wagonga Group and gradationally by the Narooma Chert.|Quartzose turbidites; thick-bedded sandstone with thin-bedded mudstone and chert.|17-JUL-19
98|Adaminaby Group|70178|6|Mentioned|p3, p13|Ordovician|Ordovician||||||Siliciclastic turbidites.|
98|Adaminaby Group|70192|5|Briefly described|Map Legend|Gisbornian|Lancefieldian|On Boorowa, Crookwell, Taralga, Yass, Gunning and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.|||Includes Abercrombie Formation.|Is overlain by Bendoc Group.||
98|Adaminaby Group|70297|5|Briefly described|map legend, on side 2 of map sheet|Gisbornian|Bendigonian|Age: Middle Ordovician to earliest Late Ordovician. Includes thick sequence of thin, rhythmically bedded, quartz-rich fine- to coarse-grained turbidites, and chert with minor black carbonaceous shale of a distal turbidite fan, deposited in a deep water environment. Small structurally controlled low sufide (orogenic) gold, and copper-dominated structurally  controlled high sulfide (orogenic) base metal +/- gold veins.|||Mozart Chert Member, Budhang Chert Member|Is overlain by Bendoc Group.|Turbiditic sequence of quartz-rich sandstone, mudstone, shale; carbonaceous shale, greywacke; chert, quartzite, phyllite, slate.|17-MAY-16
98|Adaminaby Group|70493|5|Briefly described|p53-64|Ordovician|Ordovician|Lachlan Orogen. Numerous geochemical diagrams. Most sediments underwent one cycle of erosion; some have been recycled. Sediments were derived from a mainly felsic granodioritic, probably shoshonitic, source in a collisional, not subduction-related, setting.||||Overlies Howqua and Narooma Cherts. Is overlain by Bendoc Group.|Turbidites; lower part dominated by sandy turbidite facies with thin intervals of bedded chert, and an upper part with a thick (300-400m) unit of black shale largely lacking sandstone.|
98|Adaminaby Group|70540|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Abercrombie Formation.|||
98|Adaminaby Group|70541|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Abercrombie Formation.|||
98|Adaminaby Group|70542|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Abercrombie Formation.|||
98|Adaminaby Group|70543|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Abercrombie Formation|||
98|Adaminaby Group|70544|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Abercrombie Formation|||
98|Adaminaby Group|70545|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Abercrombie Formation.|||
98|Adaminaby Group|70546|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Abercrombie Formation|||
98|Adaminaby Group|70601|4|Described|p23, p25-27, p39-57|Gisbornian|Early Ordovician|Onshore geology. Conformable junction with overlying Narooma Chert. Above zone of melting where Moruya Suite granites extend onshore. Conodont age ca 485Ma. Outcrops extensively from the NSW coast to the eastern boundary of the Melbourne Zone.||Narooma Accretionary Complex.|Pinnak Sandstone, Chakola Formation, Numeralla Chert.|Underlies Warbisco Shale (Bendoc Group), Bogolo Formation, Numeralla Chert. Overlies Howqua Chert, "Melville Chert".|Quartz turbidites with crenulation cleavage that overprints a bedding-parallel slaty cleavage; siliceous shale, gradational, generally upward-fining sequence of siltstone, black shale and sandstone with thin cross-laminated quartzic silt layers.|18-JAN-19
98|Adaminaby Group|70629|6|Mentioned|p986|Late Ordovician|Early Ordovician|Melbourne Zone.||||||
98|Adaminaby Group|70661|3|Fully described|vii, viii, p3, p4, p7, p8 fig 2, p9|Gisbornian|Bendigonian|Named after the town of Old Adaminaby. Outcrops primarily in the southwest of the map, sporadically outcrops in the northwest. Estimated to be at least 1000m thick, may be 3-5km thick. Lithology in different map areas discussed in greater detail. Deposited in submarine fan or fan apron system below storm wave base.  Equivalent to the Wagga Group, Girilambone Group. See also p10, p11, p12, p13, p14, p15, p16, p17, p19,p21- p26, p41, p101, p130, p145, p243.||||Conformably overlain by Bindook Group, Bendoc Group, faulted against Merrimbula Group, intruded by Bundundah Granite, conformably overlies Howqua Chert, Unconformably overlain by Shoalhaven Group.|Thin to thickly bedded micaceous quartz-rich metasandstone, metasiltstone, medium to fine grained, poorly sorted and subangular to subrounded turbiditic sandstone, hornfels, shale, slate, phyllite and minor interbedded chert.|26-JUL-17
98|Adaminaby Group|70684|5|Briefly described|p7 Fig.1, p14-15|Ordovician|Ordovician|||||Is overlain by Bendoc Group.|Deformed turbidites.|
98|Adaminaby Group|70718|5|Briefly described|p43-p44|Late Ordovician|Early Ordovician|Tabberabbera  and Wagga-Omeo Zones, Murray Basin. Turbidite succession.|||Includes the Pinnak Sandstone.||Sandstone, mudstone, shale, carbonaceous shale, greywacke, chert, quartzite and phyllite.|
98|Adaminaby Group|70727|6|Mentioned|p172|Ordovician|Ordovician|Geological province: Hill End Zone, Eastern Lachlan Orogen.||||Passive intruded by Wyangala Granite.||
98|Adaminaby Group|70744|5|Briefly described|p944-945|Late Ordovician|Late Ordovician|SE Lachlan Orogen. Detrital zircon age distribution graph.||||||
98|Adaminaby Group|70754|5|Briefly described|p447|Darriwilian|Darriwilian|Contains rare linguloid and acrotretoid brachiopods.|||||Includes deep-water cherts.|
98|Adaminaby Group|71040|6|Mentioned|p10 Fig.6, p19|Ordovician|Ordovician|||||||
98|Adaminaby Group|71069|3|Fully described|p9, p19, p21 fig 7, p22, p31|Ordovician|Ordovician|Name derived from Old Adaminaby. Previously termed the Adaminaby Beds. Reference sections mentioned [However there is some ambiguity as to whether or not these are suitable]. Distributed widely across the Lachlan Orogen where it usually forms low, weathered outcrop. Possible source of gold in placer deposits near the map sheet (Captains Flat) area.Estimated thicknesses ranging from 2000-5000m. Structure, metamorphism and fossil assemblages discussed.  Age poorly constrained, [author states that is believed to be older than Ordovician, but no evidence is provided]. Equivalent to the Wagga and Girilambone Groups. Deposited in a submarine fan or fan apron system below storm-wave base, probably in an outer slope or basin plain setting. Lithology shows elements of being a bouma sequence and is thus interpreted to indicate depositon from turbidity currents. Intruded by the Harrisons Peak Granite. See also  p39 fig 16, p40 fig 17, p42, p51, p52, p55-p58, p60, p61, p65-67, p72, p75, p76 fig 27, p77, p80, p82, p88, p92, p93, p95, p100, p105-p107, p120, p125, p134, p144, p172, p178, p183, p184, p201, p202.|||Includes the Abercrombie Formation, Peach Tree Chert Member, Mummel Chert Member, Willigam Sandstone Member, Numeralla Chert, Chakola Formation and the Pinnak Sandstone|Conformably overlain by the Bendoc Group and the Warbisco Shale. Unconformably overlain by the Hoskinstown Group. Overlain by the Covan Creek Formation.|Interbedded quartzose to lithic-feldspar-quartz sandstone, siltstone and mudstone with minor but conspicuous chert rich intervals. |
98|Adaminaby Group|71303|5|Briefly described|map legend|Late Ordovician|Early Ordovician||||Includes Nattery Chert Member.||Thin- to thick-bedded micaceous quartz-rich sandstone and shale (turbidites), shales and slates, phyllite and minor interbedded chert. Rocks variably regionally metamorphosed to lower greenschist facies with hornfelsing near intrusions.|
98|Adaminaby Group|71656|4|Described|p10 Fig.1, p11-14, p12, 13 Fig 2|Gisbornian|Early Ordovician||||Includes Abercrombie Formation.|Underlies Bendoc Group.|Strata include chert bodies.|
98|Adaminaby Group|71691|5|Briefly described|Map legend.|Ordovician|Ordovician||||Abercrombie Formation.|Is overlain by Bendoc Group.||
98|Adaminaby Group|71699|5|Briefly described|Map legend.|Ordovician|Ordovician||||Abercrombie Formation.|Is overlain by Bendoc Group.||
98|Adaminaby Group|71700|3|Fully described|vi, ix, x, p5, p7-p10, p36-p41, p43,  CD|Ordovician|Ordovician|Albury-Bega Terrane. Named for the town of old Adaminaby. A type section has not been defined but a number of reference sections have been proposed over time [see CD]. Originally the "Adaminaby Beds" of Fairbridge (1953) , the unit and the Bendoc Group were subsequently seperated into the Birkenburn Beds and Merigan Black Shale by Felton and Huleatt (1975) before being divided into the Adaminaby Group and the overlying Warbisco Shale by Glen et al (1990). The unit was thereafter formally defined by Lewis et al (1994) incorporating the Mallacoota Beds. Distribution, geomorphic expression, outcrop characteristics, depositional environment, structural geology, geochemistry, fossils, mineralisation and estimated thicknesses are discussed. Structural geology and metamorphism are discussed. See also p45, p48-p50, p57, p63-p64, p66, p71, p74, p79, p81-p83, p85-p86, p90, p114, p116-p119.|||Includes the Abercrombie Formation, Numeralla Chert, Chakola Formation and Pinnak Sandstone.|Conformably overlain by the Bendoc Group. Unconformably overlain by the Bindook Group, Mount Fairy Group and the Woodlawn Volcanics. Intruded by the Tallaganda Granodiorite.|Interbedded quartzose to lithic-feldspar-quartz sandstone, siltstone and mudstone with conspicuous chert rich intervals.|
98|Adaminaby Group|71889|6|Mentioned|p12|Darriwilian|Darriwilian|||||Equivalent to the Wagga Group.|Black shales.|
98|Adaminaby Group|72263|5|Briefly described|p514-515,524|Early Ordovician|Early Ordovician|Geological province: Lachlan Orogen. Deposited on a passive margin. Juxtaposed against, and surrounds the Macquarie Arc. Zircon analysis by Glen et al. (2011) on the Mitchell Formation, yielded zircon ages of ~494 Ma, and combined with Hf isotope analysis from this study (Zhang et al., 2019), suggests that the samples studied by Glen et al., 2011 were likely to be of Adaminaby Group instead (similar to Adaminaby zircon data presented by Meffre et al., 2007), with a peri-Gondwanan afinity.|||||Quartz-rich turbidites, cherts and black shales.|
98|Adaminaby Group|72296|6|Mentioned|p6||||||Pinnak Sandstone.|||
98|Adaminaby Group|72528|5|Briefly described|p11, p18, p25.|Ordovician|Ordovician|||Campbells Group||Underlies Lambie Group and is intruded by Whipstick Monzogranite and Bandshea Granite||
98|Adaminaby Group|73059|5|Briefly described|p1053 Fig.2, 1055, 1059-1061, 1063|Ordovician|Ordovician|Detrital zircons aged ~510-485 Ma attributed to a Delamerian Fold Belt source.||||Overlies Wagonga Group, Howqua Chert. Is overlain by Bendoc Group and Narooma Chert.|Quartz-lithic sandstones unit overlain by quartz-rich sandstones unit.|
98|Adaminaby Group|73140|5|Briefly described|p495|Gisbornian|Late Cambrian|Proposed to incorporate and supersede the Wagga Group. Also proposed to be incorporated into a new Lachlan Supergroup.||Lachlan Supergroup|Abercrombie Formation|Underlies Bendoc Group|Terrigenous turbiditic sequence.|
98|Adaminaby Group|73186|6|Mentioned|p227, p229-230, p236-237, p239-240, p242|Ordovician|Early Ordovician|Tabberabera Zone and Omeo Zone.|||||Turbidites with deep water chert, includes sandstones, mudstones and hemipelagic black slates.|
98|Adaminaby Group|73211|6|Mentioned|p909|Upper Ordovician|Middle Ordovician|Referred to as the foundation of the Lachlan Orogen/Fold Belt.||||||
98|Adaminaby Group|73264|6|Mentioned|p1390 Fig.12, p1392, p1393 Fig.15|Middle Ordovician|Early Ordovician|Lachlan Orogen. Age described as Early and late-Middle Ordovician.|||||Turbidites.|
98|Adaminaby Group|73299|5|Briefly described|p1094 Fig.2, p1095-1096, p1098|Ordovician|Ordovician|Lachlan Orogen. Generally strongly deformed with abundant tight to isoclinal mesoscopic folds. Poorly constrained early folds east of Mudgee prior to the dominant deformation, Capertree High. Locations in text include p1100 Fig.5.|||||Turbidites.|
98|Adaminaby Group|73431|5|Briefly described|p362-366, p370, p372, p374-375|Ordovician|Early Ordovician|Lachlan Orogen. Passive margin sequence along the east Gondwana continental margin. Coeval with, and in faulted contact with the Macquarie Arc. Location in text includes p371 Fig.7.||||Intruded by Sunset Hills Granite|Quartz and clay-rich turbidites, shales.|
98|Adaminaby Group|73440|6|Mentioned|p146||||||||Includes quartz-rich turbidites.|
98|Adaminaby Group|73457|5|Briefly described|p4, p6 Fig.4, p8-12, p13 Fig.8, p14|Ordovician|Ordovician|||||Unconformably underlies Galore Hill Formation, Kengal Formation, Yambla Formation, faulted against Granya Granite|Metasedimentary rock.|
98|Adaminaby Group|73497|5|Briefly described|Map legend|Ordovician|Ordovician||||||Marine turbiditic sandstone, siltstone and shale: magnetic response below limit of detection.|
98|Adaminaby Group|73505|6|Mentioned|p35|||||||||
98|Adaminaby Group|75070|6|Mentioned|p183|||||||||
36801|Addiscot Formation|23778|1|Redefined|p679 App 1|Early Oligocene|Late Eocene|Of Demons Bluff Group. Overlying unit Angahook Formation. Underlying unit Anglesea Formation. Torquay Basin.||||||
36801|Addiscot Formation|69297|6|Mentioned|p98|Rupelian|Rupelian|||||Overlies the Anglesea Formation. Unconformably overlain by the Angahook Formation. ||
37625|Adjie Granodiorite|23309|6|Mentioned|Table 4.1, App 1|||G105, I-type.||||||
37625|Adjie Granodiorite|24133|3|Fully described|p67|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37625|Adjie Granodiorite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37625|Adjie Granodiorite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37625|Adjie Granodiorite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37625|Adjie Granodiorite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt||||||
37625|Adjie Granodiorite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37625|Adjie Granodiorite|68116|5|Briefly described|Appendix, Map 20.|Pridoli|Wenlock||||||Hornblende granodiorite: pale grey, medium to coarse grained; equigranular; minor pale pink K-feldspar; I-type; highly magnetic.|
30073|Admiral Formation|13323|5|Briefly described|p393 Fig. 2|Turonian|Cenomanian|Of Emperor Subgroup (Latrobe Group). Fluvial sandstones and shallow lacustrine mudstones - blocky sandstones separated by shales. Overlain by Kipper Shale. Geol. Prov: Gippsland Basin. Partly laterally equivalent and overlying Kersop Arkose.||||||26-JUN-06
30073|Admiral Formation|24090|5|Briefly described|p8 Fig.3|Cretaceous|Cretaceous|Geological Province: Gippsland Basin.||||||
30073|Admiral Formation|24407|5|Briefly described|p13 Fig.2|||Geological Province: Gippsland Basin||||||
30073|Admiral Formation|24551|5|Briefly described|p267, 476|||Of the Emperor Subgroup.  Overlies: Kersop Arkose.  Underlies: Kipper Shale.||||||
30073|Admiral Formation|61552|6|Mentioned|p583 Fig.2. |Late Cretaceous|Late Cretaceous|||Unit in Emperor Subgroup.||||
30073|Admiral Formation|64876|5|Briefly described|p145 Fig.2|Turonian|Turonian|Gippsland Basin.||Emperor Subgroup.||||
30073|Admiral Formation|65717|5|Briefly described|p9 figure 2.2, p10|Turonian|Cenomanian|Bernecker and Partridge (2001). Gippsland Basin.||Emperor Subgroup||Conformably overlain by Curlip Formation, overlies Kersop Arkose|Quartz dominated lithic arenites.|05-SEP-17
30073|Admiral Formation|65973|4|Described|p14, p28, p45-47, p57-58|||Gippsland Basin. Interpreted to be derived from the erosion of Palaeozoic sedimentary and metamorphic terrains. Deposited in an alluvial fan, lacustrine or fluvial environment. Reservoir qualities are poor. Intersected in the Longtom-1, Longtom-2/ST1, Leatherjacket-1 and Judith-1 petroleum drillholes. At least 160m in the Longtom-1 and Longtom-2/ST1 drillholes. See also p82-83, p93, p96-101, p123, p127, p132-134, p171.||Emperor Subgroup.||Faulted against the Strzelecki Group. Overlain by the Kipper Shale.|Coarse-grained quartz-dominated lithic arenites, fine- to medium-grained, poorly to moderately-sorted sands, shales and siltstones.|
30073|Admiral Formation|70076|5|Briefly described|Regional: Fig.3|Turonian|Turonian|||Emperor Subgroup.||Overlies Wombat Volcanics. Is overlain by Chimaera Formation.||
30073|Admiral Formation|75065|5|Briefly described|p151, 154, 161|Cenomanian|Cenomanian|Gippsland Basin; offshore. Alluvial/fluvial deposits.||Emperor Subgroup.||Unconformably overlies Korumburra Subgroup. Is overlain by Curlip Formation and Kipper Shale.||
154|Agnes Formation|24551|6|Mentioned|p443|||Tertiary sediments in Toora area. Contains alluvial cassiterite (tin).||||||03-NOV-14
154|Agnes Formation|41868|6|Mentioned|p589|||||||||
154|Agnes Formation|42827|6|Mentioned|p589|||||||||
25757|Akuna Mudstone|22815|4|Described|p26|Late Ordovician||Equivalent to the Gungoandra Siltstone||||||
25757|Akuna Mudstone|22857|4|Described|p420 App. 1 Tb. A1.5||Late Ordovician|Of the Bendoc Group. Three lithofacies: top mudrock (mainly siltstone) - middle 30m of siliceous siltstone - basal 150m laminated mudrocks alternating with khaki mudstone. Max. thickness: 300m.||||||
25757|Akuna Mudstone|22876|6|Mentioned|p16|||||||||
25757|Akuna Mudstone|22878|5|Briefly described|p33|Early Silurian|Late Ordovician|||||||
25757|Akuna Mudstone|22968|6|Mentioned|P103|||Parent is Bendoc Group||||||
25757|Akuna Mudstone|23309|5|Briefly described|p60||Ordovician|Of Bendoc Group.||||||
25757|Akuna Mudstone|23615|3|Fully described|p20 Fig.6, p68|Late Ordovician|Late Ordovician|Of Bendoc Group.  Overlain by Yalmy Group, underlain by Warbisco Shale.  Thinly bedded dark grey and green siltstone.  Age within the 'deep marine Ordovician sedimentation' period: 500-438Ma - probably Middle to late Bolindian.  Geological Province: Lachlan Fold Belt.||||||16-AUG-18
25757|Akuna Mudstone|24004|5|Briefly described|p275 Fig.2|Ordovician|Ordovician|||||||
25757|Akuna Mudstone|24037|6|Mentioned|p425 Fig.2|Bolindian|Bolindian|Geological Province: Lachlan Fold Belt.||||||
25757|Akuna Mudstone|24133|3|Fully described|p38|||Parent: Bendoc Group.  Geological Province: Lachlan Fold Belt.||||||
25757|Akuna Mudstone|24551|4|Described|p106|Bolindian|Bolindian|Of Bendoc Group. Overlies by New Country Sandstone.||||||
25757|Akuna Mudstone|41570|4|Described|p93|||||||||
25757|Akuna Mudstone|41585|6|Mentioned|p129|||||||||
25757|Akuna Mudstone|42142|6|Mentioned|p587|||See also Fig.3||||||
25757|Akuna Mudstone|42627|5|Briefly described|Map legend|late Bolindian||||||||
25757|Akuna Mudstone|42647|2|Defined|p21|Early Silurian|Bolindian|||||||
25757|Akuna Mudstone|42827|5|Briefly described|p93|||see also Table 4.1||||||
25757|Akuna Mudstone|43206|5|Briefly described|map legend|Llandovery|Bolindian|of Bendoc Group||||||
25757|Akuna Mudstone|43233|5|Briefly described|Map Legend|Llandovery|Bolindian|of Bendoc Group.||||||
25757|Akuna Mudstone|43314|5|Briefly described|Map Legend||Bolindian|of Bendoc Group.||||||
25757|Akuna Mudstone|43315|5|Briefly described|Map Legend||Bolindian|Of the Bendoc Group. Mudstone - laminated, well-bedded; siliceous siltstone, thin sandstone beds: purple, khaki and green-grey.||||||03-MAY-05
25757|Akuna Mudstone|60541|5|Briefly described|p53-54, p35|Bolindian|Bolindian|Of the Bendoc Group. Green, grey and purple mudstones with thin interbedded sandstones. Conformably overlies Warbisco Shale; in faulted contact above with Yalmy Group, Sunlight Creek Formation and Pinnak Sandstone. Max. thickness: >300m. Geol.Prov: LFB.||||||
25757|Akuna Mudstone|60542|5|Briefly described|p12|Ordovician|Ordovician|Green shale.||||||
25757|Akuna Mudstone|60988|6|Mentioned|p144 Fig.1|Early Silurian|Early Silurian|||||||
25757|Akuna Mudstone|61160|5|Briefly described|p48|Late Ordovician|Late Ordovician|Of the Bendoc Group. Geological Province: Lachlan Fold Belt.||||||
25757|Akuna Mudstone|61161|5|Briefly described|p31-32, p82|||Rock of the Bendoc Group similar to Akuna Mudstone in BUFFALO. Mostly pelagic and hemipelagic mudstone deposited in conditions that ranged from deep anoxic, to aerated, with burrowing organisms present. Overlies New Country Sandstone.||||||
25757|Akuna Mudstone|61163|4|Described|p84, p14 Fig. 3.2|Late Ordovician|Late Ordovician|Of the Bendoc Group. Overlies New Country Sandstone. Geological Province: Lachlan Fold Belt (Tabberabbera Zone). Includes black shale and interbedded bioturbated mudstone. See also p38 Tb. 6.2.||||||
25757|Akuna Mudstone|61174|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Shale, siltstone: black shale, grey laminated and minor bioturbated siltstone and thin-bedded sandstone; with abundant Bolindian graptolites. Deep-marine hemipelagic and turbidite deposits. GSV map code: Oba.||||||07-FEB-11
25757|Akuna Mudstone|61175|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Shale, siltstone: black shale, grey laminated and minor bioturbated siltstone and thin-bedded sandstone; with abundant Bolindian graptolites. Deep-marine hemipelagic and turbidite deposits. GSV map code: Oba.||||||12-SEP-05
25757|Akuna Mudstone|61176|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Shale, siltstone: black shale, grey laminated and minor bioturbated siltstone and thin-bedded sandstone; with abundant Bolindian graptolites. Deep-marine hemipelagic and turbidite deposits. GSV map code: Oba.||||||12-SEP-05
25757|Akuna Mudstone|61177|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Shale, siltstone: black shale, grey laminated and minor bioturbated siltstone and thin-bedded sandstone; with abundant Bolindian graptolites. Deep-marine hemipelagic and turbidite deposits. GSV map code: Oba.||||||12-SEP-05
25757|Akuna Mudstone|61178|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of Bendoc Group. Black shale, laminated siltstone (turbidite): nonmagnetic (5 nt; k = 0-100 [avg = 10] x10^-6 cgs); moderate gravity; moderate radioelements except in SE where lower total radioelement and K. GSV map code: Oba.||||||
25757|Akuna Mudstone|67322|5|Briefly described|p16, p20 Fig.5|Silurian|Late Ordovician|In Victoria, the New Country Sandstone is laterally equivalent to, or overlain by, the Akuna Mudstone of late Bolindian age. Occurs in the Cooma-Mallacoota region.||Of the Bendoc Group.||Laterally equivalent to the New Country Sandstone. Overlies New Country Sandstone and Warbisco Shale.||21-FEB-18
25757|Akuna Mudstone|68116|5|Briefly described|Appendix, Maps 36, 45.|Hirnantian|Katian|Bolindian age in text.|||||Black shale, laminated siliceous siltstone: thinly bedded; thin sandstone beds; rare bioturbated mudstone; dark grey weathered to various pale colours.|
25757|Akuna Mudstone|68466|6|Mentioned|p65|Late Ordovician|Late Ordovician|Albury-Bega Terrane.||||||
25757|Akuna Mudstone|68592|6|Mentioned|p320-2, p367|||||Unit in Bendoc Group.||||
25757|Akuna Mudstone|69668|5|Briefly described|p929 Fig.2|Late Ordovician|Late Ordovician|Cooma-Bega area, Albury-Bega terrane.||||Overlies Warbisco Shale.||
25757|Akuna Mudstone|70601|5|Briefly described|p43, p54|Llandovery|Bolindian|Albury-Bega Basin: Inland Zone. Stratigraphically equivalent to Bogolo Formation.||Topmost Bendoc Group.||Overlies Warbisco Shale. Unconformably underlies Yalmy Group.|Deformed and cleaved khaki-coloured mudstones.|
25757|Akuna Mudstone|70661|6|Mentioned|p19|||||Bendoc Group||||26-JUL-17
25757|Akuna Mudstone|71069|5|Briefly described|p72, p74, p77, p84|Early Silurian|Late Ordovician|Maximum estimated thickness of 300m.||Bendoc Group||Is equivalent to the Gungoandra Siltstone and members of the Margules Group. Conformably overlies the Warbisco Shale.|Dark-grey to khaki, often laminated mudstone and siltstone, occurring as thin to thick beds. Some rippled sandstone beds are also present.|
25757|Akuna Mudstone|71700|6|Mentioned|CD|||||Bendoc Group||||
25757|Akuna Mudstone|73140|5|Briefly described|p495|Bolindian|Bolindian|Proposed to be reassigned from the Bendoc Group to Margules Group. Age based on graptolites.||Margules Group||Overlies Warbisco Shale, New Country Sandstone||
37365|Albacore Subgroup|13323|5|Briefly described|p394 Fig. 3|Middle Miocene|Early Miocene|Of the Seaspray Group. Marine carbonates and marine clastics. Geological Province: Gippsland Basin.||||||
37365|Albacore Subgroup|23625|4|Described|p58|Miocene|Miocene|Parent: Seaspray Group.  Geological Province: Gippsland Basin||||||
37365|Albacore Subgroup|24038|5|Briefly described|p439 Fig.2|Miocene|Miocene|Geological Province: Gippsland Basin||||||
37365|Albacore Subgroup|24468|5|Briefly described|p405 Fig.2|Late Miocene|Middle Miocene|Geological Province: Gippsland Basin. Of the Seaspray Group. Overlying Unit: Hapuku Subgroup||||||
37365|Albacore Subgroup|24551|6|Mentioned|p333 Fig. 10.41|||Of the Gippsland Basin||||||
37365|Albacore Subgroup|60538|5|Briefly described|p483 Fig. 22|||Geological Province: Gippsland Basin.||||||
37365|Albacore Subgroup|66181|5|Briefly described|p310 Fig.5|Miocene|Oligocene|Overlies the Angler Subgroup, in the Seaspray Group.||||||
37365|Albacore Subgroup|67061|6|Mentioned|p554 Fig.10.|Miocene|Miocene|Gippsland Basin, offshore.||||Overlies Angler Subgroup. Is overlain by Hapuke Subgroup.||
37365|Albacore Subgroup|70076|5|Briefly described|South-Eastern: Fig.2; Regional: Fig.3|Miocene|Miocene|||Seaspray Group.|Cod Formation.|Overlies Angler Subgroup.Is overlain by Hapuku Subgroup.||
225|Albert Park Aeolianite|24551|6|Mentioned|p343|Early Pleistocene|Early Pleistocene|Of the Bridgewater Group.||||||
225|Albert Park Aeolianite|41769|4|Described|p51|||||||||
225|Albert Park Aeolianite|73386|6|Mentioned|p14|||||Bridgewater Formation||||
83092|Alberton A seam|73289|6|Mentioned|p776|Miocene|Oligocene|Said to be mostly equivalent to Morwell [Formation] seams; precisely which seams are not specified.||Alberton Coal Measures.||||
83093|Alberton B seam|73289|6|Mentioned|p776|Miocene|Oligocene|Said to be mostly equivalent to Morwell [Formation] seams; precisely which seams are not specified.||Alberton Coal Measures.||||
83094|Alberton C Seam|73289|5|Briefly described|p776|||Up to 30m thick. May be age-equivalent to some Traralgon [Formation] seams, particularly the Traralgon 0 Seam.||Alberton Coal Measures.||||
23325|Alberton Coal Measures|24551|6|Mentioned|p328, 498|Miocene|Miocene|||||||
23325|Alberton Coal Measures|38929|4|Described|p50|||See also Fig.6||||||
23325|Alberton Coal Measures|38930|5|Briefly described|p58|||||||||
23325|Alberton Coal Measures|42649|5|Briefly described|Fig.3 P197-198|||||||||
23325|Alberton Coal Measures|61336|4|Described|p(iv), p(vi), p(xii)|||Includes two main coal seams - an upper A seam (55m thick) and lower B seam (15m thick); separated by a 12m clay split. Angular unconformity over Traralgon Formation. In the Seaspray depression. See also Albertan Fm.||||||07-FEB-11
23325|Alberton Coal Measures|65718|6|Mentioned|p10 Fig 3.2|Miocene|Miocene|Early to middle Miocene age.||||||
23325|Alberton Coal Measures|67727|5|Briefly described|p59.|||Folded, uplifted and eroded in Late Miocene-Pliocene.||||Overlies Traralgon Formation.||
23325|Alberton Coal Measures|73289|5|Briefly described|p776|Miocene|Eocene|Greer and Smith (1982). Alberton Depression, South Gippsland.|||Alberton A, B, C, D seams.|Overlies Carrajung Volcanics.||16-MAY-23
23325|Alberton Coal Measures|73488|5|Briefly described|p636, p641 Fig.9, p643, p646-647|||Gippsland Basin. See also Alberton coal measures p630, Alberton coal seams p641 Fig.9, Alberton Formation p630 and p644.||||Overlies Traralgon Formation||
83095|Alberton D Seam|73289|5|Briefly described|p776|||Up to 10m thick. May  be age-equivalent to some Traralgon [Formation] seams, particularly the Traralgon 0 Seam.||Alberton Coal Measures.||Overlies Carrajung Volcanics.||
72620|Albion Formation|62741|5|Briefly described|p680 Fig. 2|||Also known as "Mine schist". See also p682 Fig. 4b.||||||
72620|Albion Formation|62742|5|Briefly described|p697-698, p699 Fig. 2|Early Cambrian|Early Cambrian|Deformed, strongly altered unit; diverse range of acritarchs and minor other fossil fragments from siliceous mudst.(chert) within unit.Contains a middle Botoman chert + 35 well-preserved spinose acritarchs. Conformable over Magdala Basalt. In Stawell Zone||||||
72620|Albion Formation|62744|5|Briefly described|p708, p709 Fig. 2|Early Cambrian|Early Cambrian|Quartz-rich turbidites. Underlies and is intercalated with Magdala Basalt; overlain by Leviathan Formation. Geologcial Province: Stawell Zone.||||||
72620|Albion Formation|62747|5|Briefly described|p734 Fig. 1, p737|||Sedimentary rocks - pervasively muscovite-altered. Overlies both Eastern Schist and Magdala Basalt.||||||28-NOV-06
72620|Albion Formation|62749|5|Briefly described|p722, p724|||Mudstone-dominated strata. Conformably overlain by Leviathan Formation. Overlies the Dukes Nose structure (basalts) with a sharp contact.||||||
72620|Albion Formation|62751|5|Briefly described|p759|||Mudstone-rich unit, lowest stratigraphic unit in Stawell. Locally intercalated with Magdala Basalt. Conformably overlain by Leviathan Formation. See also p761 Fig. 2||||||
72620|Albion Formation|62752|5|Briefly described|p759, p760 Fig.1b|||This mudstone-rich unit is the lowermost stratigraphic unit at Stawell. Conformably overlain by Leviathan Formation and intercalated with Magdala Basalt. See also p761 Fig. 2.||||||23-JAN-07
72620|Albion Formation|62753|5|Briefly described|p800|||Interlayered black mudstone with minor siliceous sltst and calcareous sst; base is strongly chlorite+/-stilpnomelane altered and previously referred to as "volcanogenics" by Watchorn and Wilson (1989); now referred to as Stawell Facies.||||||22-JAN-07
72620|Albion Formation|64597|5|Briefly described|p760 Fig.1, p761. |||||||Overlies and locally envelopes the Magdala Basalt. Is overlain by the Leviathan Formation.|Basal interbedded fine-grained quartz-rich sandstone, sulfidic mudstone with framboidal pyrite, fossiliferous siliceous siltstone, and calcareous sandstone layers; thinly-interbedded mudstone and fine-grained quartz-rich sandstone.|
72620|Albion Formation|65969|6|Mentioned|p13|||Correlated with Knowsley East Formation by Squire and Wilson (2005).||||||
72620|Albion Formation|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Saint Arnaud Group. Defined by Squire and Wilson 2005 p751||||||
72620|Albion Formation|66769|6|Mentioned|117|Cambrian|Cambrian|Stawell Zone. Mudstone and shale.||||||02-JUN-19
72620|Albion Formation|67847|6|Mentioned|p10 fig 2.3|Upper Cambrian|Upper Cambrian|||||||
72620|Albion Formation|68116|5|Briefly described|Appendix, Maps 22, 30.|Early Cambrian|Early Cambrian|Contains a diverse range of Early Cambrian acritarch fossils, and other fossils from within interbedded siliceous chert bands.|||||Interlayered black mudstone with minor siliceous siltstone and calcareous sandstone; base is characterised by strong chlorite +/- stilpnomelane alteration. |
72620|Albion Formation|68314|5|Briefly described|p750-755|Early Cambrian|Early Cambrian|Stawell area. Three facies described. Up to c.210m thick.||||Overlies Magdala Basalt. Is overlain conformably by Leviathan Formation.|Pale grey, fine- to medium-grained quartz-rich sandstone; black to dark grey, massive with lesser thinly laminated, mudstone; black to dark grey and bronze, well-stratified, medium- to thinly-laminated sulphidic mudstone with pyrite and pyrrhotite.|
72620|Albion Formation|70493|6|Mentioned|p56|Early Cambrian|Early Cambrian|Western Stawell Zone, Lachlan Orogen.||||Overlies Magdala Basalt. Is overlain by Leviathan Formation.||
72620|Albion Formation|70718|5|Briefly described|p37|||Contain Botoman acritarchs (Squire et al. 2006).||||Intercalated with the Magdala Basalt.|Siliceous mudstones.|02-JUN-19
72620|Albion Formation|73059|5|Briefly described|p1059-1061, 1064|Early Cambrian|Early Cambrian|Western Stawell Zone.||Saint Arnaud Group.||Overlies Magdala Basalt. Is overlain by Leviathan Formation.||
72620|Albion Formation|73177|6|Mentioned|1114 Fig.16|||||||||
72620|Albion Formation|73264|6|Mentioned|p1389 Fig.11|Early Cambrian|Early Cambrian|Lachlan Orogen.||||||
72620|Albion Formation|73505|6|Mentioned|p6||||||||Sulphide-rich black mudstone.|
72620|Albion Formation|75072|6|Mentioned|p232, 240|Late Cambrian|Late Cambrian|Stawell Zone, Central Victoria. Zircon age distribution.||Saint Arnaud Group.||||
234|Albury Gneiss|30909|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
234|Albury Gneiss|31278|6|Mentioned|Fig. 2|||||||||
234|Albury Gneiss|31800|6|Mentioned|p205|||||||||
234|Albury Gneiss|34544|6|Mentioned|p183|||||||||
234|Albury Gneiss|35278|6|Mentioned|p362|||||||||
234|Albury Gneiss|40328|4|Described|p202|||||||||
234|Albury Gneiss|40497|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
234|Albury Gneiss|40498|6|Mentioned|p392|||||||||
234|Albury Gneiss|45003|14|Not recorded|p16,26|||||||||
234|Albury Gneiss|70910|14|Not recorded|p46|||Refers to Joplin (1947).||||||
275|Alkemade Siltstone|42591|6|Mentioned|p228|||||||||
34781|Allanvale Granodiorite|22942|6|Mentioned|p274|||||||||
35957|Allwood Granodiorite|23309|5|Briefly described|p298|Silurian|Ordovician|G566. S-Type. Age: 434+/-3 Ma.||||||
35957|Allwood Granodiorite|24133|3|Fully described|p58|Silurian|Silurian|Intruded by Guys Forest Granodiorite.  Geological Province: Lachlan Fold Belt.||||||
35957|Allwood Granodiorite|24142|5|Briefly described|Map Legend|||Geological Province: Lachlan Fold Belt.||||||
35957|Allwood Granodiorite|24143|5|Briefly described|Map Legend|||Geological Province: Lachlan Fold Belt.||||||
35957|Allwood Granodiorite|24144|5|Briefly described|Map Legend|||Geological Province: Lachlan Fold Belt.||||||
35957|Allwood Granodiorite|24145|5|Briefly described|Map Legend|||Geological Province: Lachlan Fold Belt. Two mica cordierite granodiorite: pale to medium grey; fine to medium grained; locally foliated; sparse enclaves; S-type; non-magnetic||||||09-SEP-04
35957|Allwood Granodiorite|24146|5|Briefly described|Map Legend||Silurian|Geological Province: Lachlan Fold Belt. Age: 434 +/-3 Ma (K/Ar). Biotite-muscovite-cordierite granodiorite: S-type; non-magnetic, low K, moderate to low Th, variable U||||||09-SEP-04
35957|Allwood Granodiorite|24551|6|Mentioned|p233|||||||||
35957|Allwood Granodiorite|61160|6|Mentioned|p137|||Replaces Pheasant Creek Granite on CORRYONG.||||||01-FEB-07
35957|Allwood Granodiorite|61161|5|Briefly described|p153|||Age: K/Ar 434+-3 Ma, Simpson et al., 2001.||||||
35957|Allwood Granodiorite|68116|5|Briefly described|Appendix, Map 20.|Llandovery|Llandovery||||||Biotite-muscovite-cordierite granodiorite: pale to medium bluish grey, weathering to pale brownish grey; fine to medium-grained; locally foliated; sparse enclaves of schist, dark grey psammite; very rare enclaves of vein quartz; S-type; nonmagnetic.|
328|Almonds Granite|22971|5|Briefly described|p 20|||||||||
328|Almonds Granite|23309|5|Briefly described|App1 Table 4.1|||G207. S-Type||||||27-AUG-04
328|Almonds Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
328|Almonds Granite|68116|5|Briefly described|Appendix, Maps 18, 19.|Late Devonian|Late Devonian||||||Biotite granite; coarse grained and porphyritic with K-feldspar phenocrysts to 15 mm; contains cordierite and accessory fluorite; S-type.|
69700|Alpine Road pluton|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Subsurface Pluton: low to moderate gravity response (-400 ums^-2); moderately to highly magnetic (70 to 210 nT). GSV map code: G565.||||||20-SEP-05
69700|Alpine Road pluton|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Subsurface Pluton: low to moderate gravity response (-400 ums^-2); moderately to highly magnetic (70 to 210 nT). GSV map code: G565.||||||07-FEB-11
69700|Alpine Road pluton|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Subsurface Pluton: low to moderate gravity response (-400 ums^-2); moderately to highly magnetic (70 to 210 nT). GSV map code: G565.||||||20-SEP-05
69700|Alpine Road pluton|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Subsurface Pluton: low to moderate gravity response (-400 ums^-2); moderately to highly magnetic (70 to 210 nT). GSV map code: G565.||||||20-SEP-05
69700|Alpine Road pluton|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Subsurface Pluton: low to moderate gravity response (-430 to -360 ums^-2); moderately to highly magnetic (70 to 210 nT). GSV map code: G565.||||||
337|Altona Coal Seam|33604|6|Mentioned|p20|||||||||
337|Altona Coal Seam|35276|6|Mentioned|p236|||||||||
337|Altona Coal Seam|35712|6|Mentioned|Table 6|||||||||
337|Altona Coal Seam|37035|6|Mentioned|Map|||Appears on map in back pocket of publication.||||||
337|Altona Coal Seam|39865|6|Mentioned|p28|||||||||
337|Altona Coal Seam|42827|5|Briefly described|p311|||see also Fig. 8.14||||||
337|Altona Coal Seam|60083|5|Briefly described|Map legend|Oligocene|Oligocene|Stated to be synonymous with Maddingley Coal Seam.  Brown coal, minor lignitic sand and clay.||||||19-JUL-04
337|Altona Coal Seam|65715|5|Briefly described|p11 Tb.7, p13|Paleogene|Paleogene|Of Werribee Formation. Referred to as 'Altona brown coal beds' by Herman (1922). Senior synonym of Parwan Seam and Maddingley Coal Seam of Edwards (1950).||||||06-FEB-15
35958|Amberley Park Volcaniclastic Member|23309|4|Described|p119,121 Fig 2.86, p118 Tb 2.41.|||Of the Buchan Caves Limestone/Buchan Group.  Maximum Thickness: 15m.||||||22-FEB-10
35958|Amberley Park Volcaniclastic Member|24551|5|Briefly described|p147|||Of Buchan Caves Limestone.||||||24-JUL-08
35958|Amberley Park Volcaniclastic Member|60542|3|Fully described|p80-81, p43|Early Devonian|Early Devonian|Of the Buchan Caves Limestone. Thin band of andesitic volcaniclastics. Max. thickness: ~15m. ||||||
357|Amboyne Granodiorite|22815|4|Described|p44|Silurian|Silurian|Intruded Yalmy Group.||||||
357|Amboyne Granodiorite|22876|5|Briefly described|p28|||Bullenbalong Suite||||||
357|Amboyne Granodiorite|22877|5|Briefly described|map|Silurian|Silurian|Bullenbalong Suite. G71. Cordierite-garnet-biotite granodiorite. S-Type.||||||26-OCT-04
357|Amboyne Granodiorite|23309|5|Briefly described|p63, 113, 121, 303, 338, 465||Early Silurian|(G71). Age: U/Pb Zircon 430+/-3Ma, K/Ar Biotite 427+/-3 / 415+/-8 / 407+/-13Ma.  Includes McKillops Bridge Granodiorite (G72). Of Bullenbalong Suite.||||||
357|Amboyne Granodiorite|23615|3|Fully described|p154, p153 Tb. 2|Silurian|Silurian|Of Bullenbalong Suite.  See also p231 App 2.  Intrudes the Bendoc and Yalmy Groups.  Age 407+/-13Ma (Evernden & Richards, 1962) and 427+/-3Ma Henley and Webb, 1990).; 427+/-3Ma (Henley & Webb, 1990).||||||
357|Amboyne Granodiorite|23938|5|Briefly described|p54 Tb. 4|||See also p127.||||||25-SEP-08
357|Amboyne Granodiorite|24551|5|Briefly described|p132 Fig.5.23, p234, 728 Table 8.11, 440|||||||||
357|Amboyne Granodiorite|40761|6|Mentioned|p239|||||||||
357|Amboyne Granodiorite|41850|6|Mentioned|p431|||||||||
357|Amboyne Granodiorite|41905|2|Defined|p77|Silurian||||||||
357|Amboyne Granodiorite|41933|5|Briefly described|Map legend|Late Silurian||||||||
357|Amboyne Granodiorite|42627|5|Briefly described|Map legend|Wenlock||||||||
357|Amboyne Granodiorite|42647|3|Fully described|p47|||||||||
357|Amboyne Granodiorite|42827|6|Mentioned|p431|||||||||
357|Amboyne Granodiorite|43206|5|Briefly described|map legend||Wenlock|Of Bullenbalong Suite.||||||
357|Amboyne Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Bullenbalong Suite.||||||11-JAN-10
357|Amboyne Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb13.||||||
357|Amboyne Granodiorite|44185|5|Briefly described|Map legend.|Silurian|Silurian|S-type.||||||
357|Amboyne Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
357|Amboyne Granodiorite|60503|6|Mentioned|p78|Llandovery|Llandovery|Age: 427+/-3Ma. ||||||
357|Amboyne Granodiorite|61160|5|Briefly described|p120|Silurian|Silurian|Age: 430Ma. ||||||
357|Amboyne Granodiorite|61181|5|Briefly described|p16|||Contains a barite-calcite lode close to its faulted contact with Warbisco Shale on the Deddick River; the lode is reported to be 1m wide and near vertical. ||||||
357|Amboyne Granodiorite|68115|5|Briefly described|p4, p6.|Paleozoic|Paleozoic|Orth et al. (1995). Now includes the former Deddick Granodiorite (of Chappell et al. 1991) on its western side. Deddick Zone.||||||11-FEB-13
357|Amboyne Granodiorite|68116|5|Briefly described|Appendix, Maps 28, 36.|Wenlock|Llandovery||||||Biotite-cordierite granodiorite: medium grained; dark grey; abundant inclusions; S-type.|
357|Amboyne Granodiorite|75072|6|Mentioned|p236|||Deddick Valley, East Victoria. Contains mid-crustal metasedimentary xenoliths with U-Pb zircon age peaks at c.430 Ma.||||||
73146|Anakie Eastern Hill Complex|61896|5|Briefly described|p75|||Probably a structural term in this context. Consists of a scoria cone with late-stage radial dykes resting on a hydroclastic ring structure.||||||19-DEC-07
419|Anderson Creek Formation|13996|6|Mentioned|p143|||Melbourne Trough. Contains a few Wenlock trilobite species.||||||
419|Anderson Creek Formation|22511|5|Briefly described|p660, p661||Silurian|||||||
419|Anderson Creek Formation|22542|6|Mentioned|p662||Wenlock|||||||
419|Anderson Creek Formation|22628|6|Mentioned|fig1p108|Silurian|Silurian|||||||
419|Anderson Creek Formation|22684|4|Described|p744, p751, Fig.2|Wenlock|Wenlock|See also p755||||||
419|Anderson Creek Formation|22885|5|Briefly described|map|Early Silurian|Early Silurian|||||||
419|Anderson Creek Formation|23229|5|Briefly described|Table3-3p26, 28|Wenlock|Llandovery|Also known as 'Springfield Sandstone'.||||||14-APR-08
419|Anderson Creek Formation|23268|5|Briefly described|Fig14-2.1p388, 391, 395|Silurian|Early Silurian|||||||
419|Anderson Creek Formation|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
419|Anderson Creek Formation|23309|5|Briefly described|p139,150, 152, 155||Llandovery|||||||
419|Anderson Creek Formation|24177|5|Briefly described|p50 Fig.22|Early Silurian|Early Silurian|Geological Province: Darraweit Guim Province.||||||14-APR-08
419|Anderson Creek Formation|24551|5|Briefly described|p123|||||||||
419|Anderson Creek Formation|24588|5|Briefly described|p18-19, p12 Fig.3, 21|Wenlock|Llandovery|Geological Province: Darraweit Guim Province.||||||29-NOV-13
419|Anderson Creek Formation|30867|6|Mentioned|Fig.2|||Refers Garratt,Gill,Vandenberg & Williams.||||||14-APR-08
419|Anderson Creek Formation|30930|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
419|Anderson Creek Formation|30931|6|Mentioned|Map legend|Silurian|Silurian|||||||
419|Anderson Creek Formation|31676|5|Briefly described|p10|||Quartz stibrite lodes.||||||14-APR-08
419|Anderson Creek Formation|33462|6|Mentioned|p10|||Strat.table.||||||
419|Anderson Creek Formation|33464|6|Mentioned|Table 1|||||||||
419|Anderson Creek Formation|33598|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
419|Anderson Creek Formation|33599|4|Described|p2|||See also p3. Lower Silurian.||||||14-JAN-09
419|Anderson Creek Formation|33601|6|Mentioned|Fig.6|||||||||
419|Anderson Creek Formation|33604|5|Briefly described|p16|||||||||
419|Anderson Creek Formation|33607|6|Mentioned|Map legend|Silurian|Silurian|||||||
419|Anderson Creek Formation|33804|6|Mentioned|p9|||Silurian||||||
419|Anderson Creek Formation|34843|4|Described|p6|||||||||
419|Anderson Creek Formation|35073|6|Mentioned|p6|||||||||
419|Anderson Creek Formation|35283|3|Fully described|p47|||||||||
419|Anderson Creek Formation|35712|6|Mentioned|Table 6|||||||||
419|Anderson Creek Formation|37013|6|Mentioned|p11|||||||||
419|Anderson Creek Formation|37727|4|Described|p35|||See also P6 and Fig.I.||||||
419|Anderson Creek Formation|38146|6|Mentioned|Map legend|Silurian|Silurian|||||||
419|Anderson Creek Formation|38378|6|Mentioned|p142|||||||||
419|Anderson Creek Formation|38787|6|Mentioned|p125|||||||||
419|Anderson Creek Formation|39331|6|Mentioned|Table 2-1|||||||||
419|Anderson Creek Formation|41585|4|Described|p107|||||||||
419|Anderson Creek Formation|42826|6|Mentioned|p45|||||||||
419|Anderson Creek Formation|42827|4|Described|p107|||||||||
419|Anderson Creek Formation|44187|5|Briefly described|Map Legend||Early Silurian|||||||
419|Anderson Creek Formation|44197|5|Briefly described|Map Legend||Early Silurian|||||||
419|Anderson Creek Formation|60083|5|Briefly described|Map legend|Ludlovian|Llandoverian|Massive mudstone, interbedded with thin sandstone, rhythmically interbedded thin shale and sandstone; numerous greywacke-conglomerate intervals (turbidites).||||||19-JUL-04
419|Anderson Creek Formation|60599|5|Briefly described|p13, p47 Fig. 19, p54|Ludlow|Llandovery|Discussed only in terms of upper and lower Anderson Creek Formation. Geological Province: Melbourne Zone, Lachlan Fold Belt. Upper section equivalent to part of the redefined Dargile Formation.||||||14-JAN-09
419|Anderson Creek Formation|61185|5|Briefly described|p13, p21 Fig. 6|Ludlow|Llandovery|Turbidites. Underlies Melbourne Formation. Geological Province: Lachlan Fold Belt, Melbourne Zone. See also Anderson Creek Formation, upper.||||||07-FEB-11
419|Anderson Creek Formation|61187|5|Briefly described|p5 Fig.3. |Early Silurian|Early Silurian|Melbourne Zone, Melbourne Terrane. Correlative of Seldom Seen Conglomerate, Towanga Formation and Yalmy Group in the Benambra Terrane.||||||
419|Anderson Creek Formation|62469|6|Mentioned|p5 Fig. 2, p54|Wenlock|Wenlock|Includes the Warrandyte Conglomerate Member. Geological Province: Darraweit Guim Province.||||||07-FEB-11
419|Anderson Creek Formation|63083|5|Briefly described|p215, p216 Tb. 1|Wenlock|Wenlock|Contains trilobite fossils. See also p235.||||||07-FEB-11
419|Anderson Creek Formation|68116|5|Briefly described|Appendix, Maps 42, 51.|Wenlock|Llandovery||||||Sandstone: thick to thin bedded; siltstone, minor conglomerate.|
32293|Anemone Formation|13323|5|Briefly described|p393 Fig. 2|Campanian|Campanian|Of Golden Beach Subgroup (Latrobe Group). Predominantly sequences of interbedded shales and sands in varying percentages. Lateral facies of and overlies the Chimaera Formation. Geological Province: Gippsland Basin.||||||26-JUN-06
32293|Anemone Formation|24090|5|Briefly described|p8 Fig.3|Campanian|Santonian|Geological Province: Gippsland Basin.||||||
32293|Anemone Formation|24407|5|Briefly described|p13 Fig.2|||Geological Province: Gippsland Basin||||||
32293|Anemone Formation|24551|5|Briefly described|p262 Fig. 9.29, 268, 476|Late Cretaceous|Late Cretaceous|Of the Golden Beach Subgroup.||||||
32293|Anemone Formation|61552|5|Briefly described|p583 Fig.2, p586, p590. |Campanian|Santonian|The youngest Cretaceous unit dredged from the walls of the Bass Canyon, implying that structure has been in existence since c.75 Ma (the Seahorse Unconformity).||Unit in Golden Beach Subgroup.||||
32293|Anemone Formation|64876|5|Briefly described|p145 Fig.2|Campanian|Santonian|Gippsland Basin.||Golden Beach Subgroup.||||
32293|Anemone Formation|65717|5|Briefly described|p9 figure 2.2, p10|Campanian|Santonian|Represents shallow- to open-marine deposition.||Golden Beach Subgroup|||Predominantly mudstones (shales) and fine-grained siliciclastics.|05-SEP-17
32293|Anemone Formation|65973|5|Briefly described|p15, p171|||Gippsland Basin. Deposited in shallow to open marine environments.||Golden Beach Subgroup|||Mudstones, shales and fine-grained siliciclastics.|
32293|Anemone Formation|70028|6|Mentioned|p79|Campanian|Santonian|Offshore Gippsland Basin.||||||
32293|Anemone Formation|70076|5|Briefly described|South-Eastern: Fig.2; p2-p3|Campanian|Santonian|See also Regional: p2, p4-5. Hydrocarbon source and reservoir rocks; also intraformational seal. Generation is a critical risk due to thermal immaturity. Represents the first marine incursion into the Basin.||Golden Beach Subgroup||Overlies Chimaera Formation. Is overlain by Volador Formation.|Includes marine shales.|
32293|Anemone Formation|73471|5|Briefly described|p86-87, p90|Campanian|Santonian|Gippsland Basin. Upper Santonian shales demonstrate a first marine ingression from the east. Underlies Seahorse Unconformity.||Golden Beach Subgroup|||Marine clastics. Shales.|
32293|Anemone Formation|75065|5|Briefly described|p151, 163|Campanian|Santonian|Gippsland Basin; offshore.||Golden Beach Subgroup.||Overlies and abuts Chimaera Formation. Is overlain unconformably by Halibut Subgroup.|Restricted shallow-marine muds.|
434|Angahook Formation|22504|3|Fully described|p261, Table1|Late Oligocene|Early Oligocene|||||||10-AUG-15
434|Angahook Formation|22626|6|Mentioned|446 fig 10|Late Oligocene|Late Oligocene|Geol province East Otway Basin. Overlying unit Point Addis Limestone/Jan Juc Marl, underlying unit Anglesea Sand||||||
434|Angahook Formation|23372|4|Described|p250|Pliocene|Miocene|Preferred name Angahook Member of Demons Bluff Formation. of Torquay Group?/Bass Basin.||||||
434|Angahook Formation|23778|5|Briefly described|p668|||Of Demons Bluff Group. Underlying unit Addiscot Formation. Torquay Basin. Max. thickness: 37 m.||||||
434|Angahook Formation|23909|5|Briefly described|p294|||||||||
434|Angahook Formation|24038|5|Briefly described|p439 Fig.2|Oligocene|Oligocene|Geological Province: Torquay Basin||||||
434|Angahook Formation|24551|5|Briefly described|p311, 313, 630|Late Oligocene|Early Oligocene|Of the Demons Bluff Group.||||||
434|Angahook Formation|33155|4|Described|p117|||See also p118.||||||10-AUG-15
434|Angahook Formation|35854|5|Briefly described|p159|||Stratigraphy discussed.||||||
434|Angahook Formation|41043|6|Mentioned|p96|||See also P101||||||
434|Angahook Formation|43667|6|Mentioned|Fig.3,p12||Oligocene|||||||
434|Angahook Formation|60563|5|Briefly described|p47|||Basalt. Time equivalent to the upper part of the Narrawaturk Marl.||||||
434|Angahook Formation|65316|4|Described|p595, p597-598|Chattian|Bartonian|Upper boundary is subaerial exposure surface. Previous correlations discussed.|28.7 +/-0.2 Ma Ar/Ar.|Of Demons Bluff Group.||Unconformably underlies Point Addis Limestone.|Basalt, sandstone, conglomerate, claystone, tuff, breccia and pyroclastics.|05-SEP-18
434|Angahook Formation|67061|5|Briefly described|p546.|Eocene|Eocene||Basalts = 28.7 Ma.|Topmost unit in Demons Bluff Group.||Overlies Anglesea Siltstone.|Lithologically varied unit with sand, clay, gravel, tuffs and basalt.|
434|Angahook Formation|69297|6|Mentioned|p98|Chattian|Chattian|||||Unconformably overlies the Addiscot Formation. Overlain by the Point Addis Limestone. ||
434|Angahook Formation|69879|5|Briefly described|p436|Miocene|Oligocene|The rhyolite was intersected in Tilana-1, and the pyroclastics in Yolla-1.||Torquay Group|||Contains a 154m interval of rhyolitic volcanics of probable Oligocene age, and a 68m interval of altered Miocene pyroclastics.|
434|Angahook Formation|70942|5|Briefly described|p120-121, 119|||||||||17-FEB-17
434|Angahook Formation|73217|5|Briefly described|p1008 Fig.1, 1009, 1017-1018, 1022-1023|Cenozoic|Cenozoic|Eastern Otway Basin. Folds and fracture sets at the Soapy Rocks locality are described in detail.|c.28.7 Ma.|Demons Bluff Group.||Unconformably overlies Anglesea Formation. Is overlain by Torquay Group.|Shallow marine sediments including sandstone and loamy siltstone, pyroclastics, tuffs and basalts.|
37366|Angler Subgroup|13323|5|Briefly described|p394 Fig. 3|Early Miocene|Early Oligocene|Of the Seaspray Group. Marine carbonates. Geological Province: Gippsland Basin.||||||
37366|Angler Subgroup|23625|4|Described|p56|Miocene|Miocene|Parent: Seaspray Group.  Geological Province: Gippsland Basin||||||
37366|Angler Subgroup|24038|5|Briefly described|p439 Fig.2|Miocene|Oligocene|Geological Province: Gippsland Basin||||||
37366|Angler Subgroup|24468|5|Briefly described|p405 Fig.2|||Geological Province: Gippsland Basin. Of the Seaspray Group||||||
37366|Angler Subgroup|24551|6|Mentioned|p333 Fig. 10.41|||Of the Gippsland Basin||||||
37366|Angler Subgroup|60538|5|Briefly described|p475 Fig. 14, 483 Fig. 22|Oligocene|Oligocene|Geological Province: Gippsland Basin.||||||
37366|Angler Subgroup|66181|5|Briefly described|p310 Fig.5|Miocene|Oligocene|In the Seaspray Group; underlies the Albacore Subgroup.||||||
37366|Angler Subgroup|67061|6|Mentioned|p554 Fig.10.|Miocene||Gippsland Basin, offshore.||||Is overlain by Albacore Subgroup.||
37366|Angler Subgroup|70076|5|Briefly described|South-Eastern: Fig.2|Miocene|Oligocene|||Seaspray Group.|Conger, Swordfish Formations.|Overlies Cobia Subgroup (Latrobe Group). Is overlain by Albacore Subgroup.||
442|Anglers Rest Granite|22968|5|Briefly described|P32, Table7, P208||Early Devonian|Age of unit is 400+/-16 Ma and 390+/-16 Ma, parent is Boggy Plain Supersuite||||||
442|Anglers Rest Granite|23029|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is the Boggy Plain Supersuite. Biotite-muscovite granite; leucocratic I-type; medium to coarse grained, pink; no xenoliths||||||13-MAY-05
442|Anglers Rest Granite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Age: 395+/-16 Ma (K/Ar biotite). G114a: weakly magnetic; high K, moderate to high Th, moderate U. G114b: weakly magnetic; moderate K, moderate to high Th, moderate U.||||||10-JAN-07
442|Anglers Rest Granite|23309|5|Briefly described|p344,350.|Early Devonian|Late Silurian|G114.  Age: K/Ar Biotite 400 / 390Ma. Of Boggy Plain Supersuite.||||||
442|Anglers Rest Granite|24551|6|Mentioned|p233|||Of the Boggy Plain Supersuite.||||||
442|Anglers Rest Granite|39860|4|Described|p19|||||||||
442|Anglers Rest Granite|42089|5|Briefly described|p92|||||||||
442|Anglers Rest Granite|42726|5|Briefly described|map legend|Early Devonian||563. Outcrop coincides with Knocker Granite of Wyborn et al. 1987 (87/25796).||||||
442|Anglers Rest Granite|43220|5|Briefly described|p11||Devonian|||||||
442|Anglers Rest Granite|44184|5|Briefly described|Map Legend||Early Devonian|||||||
442|Anglers Rest Granite|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|I-type.||||||
442|Anglers Rest Granite|60503|4|Described|p158, p199|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. I-type. Within Omeo Metamorphic Complex. Pink, medium-grained, almost devoid of xenoliths. Intruded through Bingo Munjie Quart Diorite; intrusive contact with Hinno Munjie Granite and contact with Ludrik Munjie Granite.||||||
442|Anglers Rest Granite|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite muscovite granite: I-type; medium to coarse grained, pink.||||||
442|Anglers Rest Granite|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite muscovite granite: I-type; medium to coarse grained, pink.||||||
442|Anglers Rest Granite|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite muscovite granite: I-type; medium to coarse grained, pink.||||||
442|Anglers Rest Granite|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite muscovite granite: I-type; medium to coarse grained, pink.||||||07-OCT-04
442|Anglers Rest Granite|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Boggy Plains Supersuite. Biotite-muscovite granite: I-type; 395+/-16 Ma (K/Ar biotite); moderately to highly magnetic (0-200 nT); high K in west, high Th in north and south; low U and moderate total count, K in south||||||
442|Anglers Rest Granite|61160|3|Fully described|p81, p30 Tb. 5.2, p10|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Previously referred to as "The Knocker" (Wyborn et al 1987); and Red Granite (Crohn 1950). Homogeneous, massive, equigranular granite; leucocratic; minor biotite, abundant pink K-feldspar. Age: 390+/-16Ma, 400+/-16Ma. ||||||
442|Anglers Rest Granite|61161|5|Briefly described|p105-106, p76-77 Fig 6.1|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Leucocratic, medium to coarse grained, massive, equigranular granite. Intrudes Cobungra Granite and Omeo Metamorphic Complex gneiss. Age: K/Ar biotite 390+-16 and 400+-16Ma. GSV map code: G114. See Red Granite.||||||
442|Anglers Rest Granite|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite-muscovite granite: pink; medium to coarse grained; equigranular; leucocratic; I-type intrusion. GSV map code: G114.||||||12-SEP-05
442|Anglers Rest Granite|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite-muscovite granite: pink; medium to coarse grained; equigranular; leucocratic; I-type intrusion. GSV map code: G114.||||||12-SEP-05
442|Anglers Rest Granite|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite-muscovite granite: pink; medium to coarse grained; equigranular; leucocratic; I-type intrusion. GSV map code: G114.||||||12-SEP-05
442|Anglers Rest Granite|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite-muscovite granite: pink; medium to coarse grained; equigranular; leucocratic; I-type intrusion. GSV map code: G114.||||||07-FEB-11
442|Anglers Rest Granite|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Biotite-muscovite granite (I-type, 395 +/- 16 Ma: K/Ar biotite): highly magnetic, except where joints are demagnetised; gravity low; high total radioelement and K, low to moderate Th, low U. GSV map code: G114.||||||05-OCT-05
442|Anglers Rest Granite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite-muscovite granite: pink; medium-grained; leucocratic; I-type intrusion. Age: 395+/-16 Ma (K/Ar biotite). GSV map code: G114.||||||
442|Anglers Rest Granite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite-muscovite granite: pink; medium-grained; leucocratic; I-type intrusion. Age: 395+/-16 Ma (K/Ar biotite). GSV map code: G114.||||||07-FEB-11
442|Anglers Rest Granite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite-muscovite granite: pink; medium-grained; leucocratic; I-type intrusion. Age: 395+/-16 Ma (K/Ar biotite). GSV map code: G114.||||||
442|Anglers Rest Granite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite-muscovite granite: pink; medium-grained; leucocratic; I-type intrusion. Age: 395+/-16 Ma (K/Ar biotite). GSV map code: G114.||||||
442|Anglers Rest Granite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Biotite-muscovite granite: low gravity (-510 to -430 ums^-2); moderately to highly magnetic (60 to 130 nT, k up to 400 x10^-6 cgs); high K, moderate to high Th and total radioelements, low to moderate U. GSV map code: G114.||||||
442|Anglers Rest Granite|61187|5|Briefly described|pp15-16.|||Mentioned as possibly prospective for copper-gold mineralisation, although may be less prospective than NSW mineralisation, having formed on continental crust.||Unit in Boggy Plains Supersuite.||||
442|Anglers Rest Granite|68116|5|Briefly described|Appendix, Maps 27, 35.|Middle Devonian|Early Devonian||||||Biotite leucogranite: pink; equigranular, medium to coarse grained; minor muscovite and blue-green hornblende locally present; accessories include common allanite and rare sphene, as well as apatite, zircon, magnetite and ilmenite.|
444|Anglesea Formation|23778|1|Redefined|p678|Late Eocene|Late Eocene|Previously 'Anglesea Siltstone'. Of Demons Bluff Group. O'lying unit Addiscott Formation, U'lying unit Salt Creek Formation. Torquay Basin. Max. thickness 50 m.||||||
444|Anglesea Formation|24551|6|Mentioned|p311, 515|||Of the Demons Bluff Group.||||||
444|Anglesea Formation|34991|6|Mentioned|p386|||||||||
444|Anglesea Formation|41868|6|Mentioned|p507|||||||||
444|Anglesea Formation|42827|5|Briefly described|p507|||||||||
444|Anglesea Formation|60538|5|Briefly described|p476 Fig. 15|||Geological Province: Torquay Basin.||||||
444|Anglesea Formation|61553|5|Briefly described|p613.|||Up to 350 m of shallow bay deposits, under deepening marine influence.||Unit in Flinders Sequence.||Overlies Boonah Formation.|Siltstone and shale.|12-NOV-12
444|Anglesea Formation|69297|6|Mentioned|p97, p98, p101|Rupelian|Priabonian|Torquay Sub-basin of the Otway Basin. Deposited in a shelfal marine environment. Potential seal to the Boonah Formation and the Eastern View Formation. ||Demons Bluff Group||Overlies the Boonah Formation or the Salt Creek Formation. Overlain by the Addiscot Formation.  ||
444|Anglesea Formation|69879|5|Briefly described|p431, p435|Oligocene|Eocene|||Demons Bluff Sequence||Overlies Boonah Sand unconformably.||
444|Anglesea Formation|70077|5|Briefly described|Regional: p5, p11|Oligocene|Oligocene|Bass Basin and Torquay Sub-basin. Potential seal facies.||Demons Bluff Group.||Overlies Boonah Formation. Is overlain by Torquay Group.||
444|Anglesea Formation|73217|5|Briefly described|p1008 Fig.1, 1009, 1022|||Eastern Otway Basin. Nearshore to marginal marine sediments.|c.37-34.5 Ma.|Demons Bluff Group.||Overlies Boonah Formation. Is overlain unconformably by Angahook Formation and Torquay Group.||
24159|Angry Hill Sandstone|23309|5|Briefly described|p42 Fig. 2.14|||||||||
24159|Angry Hill Sandstone|40136|5|Briefly described|p15|||||||||
24159|Angry Hill Sandstone|41050|6|Mentioned|p51|||||||||
24159|Angry Hill Sandstone|41570|4|Described|p86|||||||||
24159|Angry Hill Sandstone|42560|6|Mentioned|p51|||||||||
24159|Angry Hill Sandstone|42628|5|Briefly described|Map legend|Bendigonian|Lancefieldian|||||||
24159|Angry Hill Sandstone|42790|5|Briefly described|Fig.14 P189|||||||||
24159|Angry Hill Sandstone|42826|2|Defined|p29|Early Ordovician||of Romsey Group||||||
24159|Angry Hill Sandstone|42827|4|Described|p86|||see also Fig 3.8||||||
24159|Angry Hill Sandstone|43493|6|Mentioned|16|||||||||
24159|Angry Hill Sandstone|65715|5|Briefly described|p4 Tb.2|Ordovician|Ordovician|Of Romsey Subgroup. Contains an unnamed microconglomerate member. Formation rank.||||||
24159|Angry Hill Sandstone|68116|5|Briefly described|Appendix, Map 32.|Floian|Tremadocian|Age written as Lancefieldian to Bendigonian in text.|||||Sandstone, siltstone, black shale: sandstone mostly thick-bedded; minor black chert: thinly bedded; conglomerate: pale coloured; fine-grained; mostly of rounded vein quartz pebbles; with horizontal lamination and tabular cross-bedding.|
459|Angusvale Diorite|23710|14|Not recorded|p84|||Excursion details.||||||
459|Angusvale Diorite|33393|6|Mentioned|p173|||||||||
459|Angusvale Diorite|34989|5|Briefly described|p80|||||||||
459|Angusvale Diorite|42577|5|Briefly described|Fig.3 P28|||||||||
459|Angusvale Diorite|42827|5|Briefly described|p150|||||||||
533|Ararat Granodiorite|23309|5|Briefly described|p64, 65, 229, 335, 341||Early Devonian|G380.  Age: U-Pb Zircon 401+/-4Ma, Ar/Ar 397+/-2Ma. Supersedes Ararat Granite and Ararat Adamellite.||||||29-MAR-05
533|Ararat Granodiorite|23402|5|Briefly described|p30|Devonian|Devonian|||||||
533|Ararat Granodiorite|24221|6|Mentioned|p894|Devonian|Devonian|||||||
533|Ararat Granodiorite|24551|6|Mentioned|p717 Table 2.4, p718 Table 8.5|Early Devonian|Early Devonian|Age: 401 +/- 4Ma, 397 +/- 2Ma.||||||
533|Ararat Granodiorite|30579|6|Mentioned|Map legend|Devonian|Devonian|||||||
533|Ararat Granodiorite|38436|6|Mentioned|p420|||||||||
533|Ararat Granodiorite|40761|6|Mentioned|p221|||||||||
533|Ararat Granodiorite|41850|6|Mentioned|p437|||||||||
533|Ararat Granodiorite|41868|6|Mentioned|p584|||||||||
533|Ararat Granodiorite|42154|5|Briefly described|p336|||||||||
533|Ararat Granodiorite|42827|5|Briefly described|p584|||||||||
533|Ararat Granodiorite|60451|4|Described|p88, 164, 219|Early Devonian|Early Devonian|I-Type. Of the Ararat Suite. Type section in text. Equigranular, medium to coarse grained, pale grey. Age: 401 +/- 4Ma (Arne et al, 1996), 397 +/- 4(Bierlein et al, 1998a).||||||
533|Ararat Granodiorite|60454|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Ararat Suite. Hornblende-biotite granodiorite; pale grey; porphyritic; equigranular; fine to medium grained, oxidised, I-Type.||||||
533|Ararat Granodiorite|60459|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Ararat Suite. Hornblende-biotite granodiorite: oxidised, I-Type.||||||
533|Ararat Granodiorite|60491|5|Briefly described|p34|Devonian|Devonian|Age: 401+/-4 Ma (U/Pb SHRIMP)||||||
533|Ararat Granodiorite|61726|5|Briefly described|p925|Early Devonian|Early Devonian|Age: 401+/-4Ma (SHRIMP U-Pb zircon, Arne et al. 1998). Geological Province: Lachlan Fold Belt.||||||
533|Ararat Granodiorite|61751|5|Briefly described|p45|Early Devonian|Early Devonian|Age: 383+/-5Ma (K-Ar biotite age) and 401+/-4Ma (Pb-U)||||||
533|Ararat Granodiorite|63599|6|Mentioned|p976 Fig. 1|||Geological Province: Stawell Zone.||||||10-DEC-07
533|Ararat Granodiorite|66002|5|Briefly described|p7 Tb.5|||Of Ararat Suite. In Ararat Pluton area. G380.  Defined by Cayley and Taylor 2001.||||||
533|Ararat Granodiorite|67978|6|Mentioned|p496 Fig.1, p499 Tb.1|Eifelian|Pragian|Mount is spelt Mt in text. Zircon dating by Black (unpublished data) from granodiorite adjacent to Rocky Point Road, south of Mt Ararat.|402 +/- 8 Ma. SIMS U-Pb|||||19-SEP-14
533|Ararat Granodiorite|68116|5|Briefly described|Appendix, Map 30.|Middle Devonian|Early Devonian||||||Hornblende-biotite granodiorite: pale grey; porphyritic; equigranular; fine to medium grained; miarolitic cavities, symplectic intergrowth textures suggest shallow intrusion level; oxidised, I-type, moderately magnetic.|
28331|Ararat Suite|22756|6|Mentioned|P40, P49|||||||||
28331|Ararat Suite|24551|5|Briefly described|p226|||Of the Stawell Province.||||||
28331|Ararat Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
28331|Ararat Suite|42827|6|Mentioned|p437|||||||||
28331|Ararat Suite|43260|6|Mentioned|Map Legend||Early Devonian|||||||
28331|Ararat Suite|60451|5|Briefly described|p87|Early Devonian|Early Devonian|Includes: Ararat Granodiorite, Burrumbeep Granodiorite, Curtis Diorite.||||||
28331|Ararat Suite|60454|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Burrumbeep Granodiorite, Ararat Granodiorite, Curtis Diorite, Merrymbuela Gabbro.||||||
28331|Ararat Suite|60456|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Units do not appear on this map.||||||
28331|Ararat Suite|60457|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Bulgana Diorite, Two Eyed Creek Granodiorite, Stawell Granite.||||||
28331|Ararat Suite|60458|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Cut-throat Diorite, White Rabbit Diorite, Stawell Granite.||||||
28331|Ararat Suite|60459|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Merrymbuela Gabbro, Cut-throat Diorite, White Rabbit Diorite, Bulgana Diorite, Two Eyed Creek Granodiorite, Stawell Granite, Curtis Diorite, Ararat Granodiorite, Burrumbeep Granodiorite.||||||14-MAY-13
28331|Ararat Suite|66002|5|Briefly described|p7 Tb.5|||Includes Ararat Granodiorite, Burrumbeep Granodiorite, Curtis Diorite all in Ararat Pluton; Ballyrogan Granite; and in Stawell Pluton: Stawell Granite, Two Eyed Granodiorite, Bulgana Diorite, White Rabbit Diorite. Defined in White and Chappell 1988.||||||14-MAY-13
30509|Archie Granodiorite|22878|4|Described|p73|||||||||
30509|Archie Granodiorite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Biotite-minor hornblende granodiorite: grey, medium to coarse grained, massive; scattered hornblende crystals to 12mm long.||||||01-OCT-04
30509|Archie Granodiorite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Biotite-minor hornblende granodiorite: grey, medium to coarse grained, massive; scattered hornblende crystals to 12mm long.||||||01-OCT-04
30509|Archie Granodiorite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Biotite-minor hornblende granodiorite: Highly magnetic (165-175 nT). High K, low Th and U.||||||06-OCT-04
30509|Archie Granodiorite|23309|6|Mentioned|p422 App1|||G531. I-Type.||||||
30509|Archie Granodiorite|68116|5|Briefly described|Appendix, Map 37.|Early Devonian|Early Devonian||||||Biotite - minor hornblende granodiorite: grey, medium to coarse grained, massive; scattered hornblende crystals to 12 mm long; I-type.|
30509|Archie Granodiorite|68592|6|Mentioned|p1674|Early Devonian|Early Devonian|||Unit in Glenbog Supersuite.||||
594|Aringa Volcanics|41701|6|Mentioned|Map legend|Oligocene||||||||
620|Armstrong Sand|24551|5|Briefly described|p343, 345|Holocene|Holocene|Of the Bridgewater Group.||||||
620|Armstrong Sand|34993|4|Described|p302|||||||||
620|Armstrong Sand|35722|6|Mentioned|Table 2|||Quaternary stratigraphic units and nature of components.||||||
620|Armstrong Sand|41769|4|Described|p55|||||||||
620|Armstrong Sand|41848|5|Briefly described|p377|||Age 2500 - 5120 yrs C-14 palaeosols||||||
620|Armstrong Sand|42827|5|Briefly described|p374|||||||||
620|Armstrong Sand|73386|6|Mentioned|p14|||||Bridgewater Formation||||
642|Arte Gabbro|22876|6|Mentioned|p29|||||||||
642|Arte Gabbro|23232|5|Briefly described|p66||Middle Devonian|Intruded before last deformation in the region and is probably 370Ma.||||||
642|Arte Gabbro|23309|5|Briefly described|p68,312, 314, 338||Early Silurian|G38. Of Arte Gabbro Complex.||||||
642|Arte Gabbro|24551|6|Mentioned|p49|||||||||
642|Arte Gabbro|41850|6|Mentioned|p429|||||||||
642|Arte Gabbro|42726|5|Briefly described|map legend|||||||||
642|Arte Gabbro|42827|5|Briefly described|p429|||||||||
642|Arte Gabbro|60541|2|Defined|p79, p22-23, p44|||Of Beams and Hough (1979). Intrusive within the Kuark Met. Complex. Separate parts are: central largely undeformed, medium-grained hornblende orthopyroxene gabbro - surrounded by fine- to medium-grained hornblende gabbro; with small body of tonalite in SE||||||21-FEB-13
642|Arte Gabbro|68115|5|Briefly described|p6.|||Contains four phases: gabbro, hornblende gabbro, tonalite and mylonite. Disagreement between their text descriptions (Hendrickx et al. 1996b) and their distribution shown on the 1:50 000 maps (Willman et al. 1996; Hendrickx et al. 1996a), have been corrected.||Unit in Arte Suite.|||Gabbro, hornblende gabbro, tonalite and mylonite.|
642|Arte Gabbro|68116|5|Briefly described|Appendix, Map 45.|Wenlock|Wenlock|Informally subdivided into gabbro, hornblende gabbro, tonalitic, and mylonitic phases. See text for a detailed lithological description of these phases.|||||Hornblende gabbronorite, hornblende gabbro, hornblende tonalite, and hornblende mylonite and amphibolite; plagioclase-hornblende-magnetite rock; I-type.|28-MAY-14
75779|Arte Suite|68115|6|Mentioned|p6.||||||Includes Arte Gabbro.|||
77887|Arthurs Seat Rhyodacite|68116|5|Briefly described|Appendix, Map 50.|Late Devonian|Middle Devonian||||||Hornblende rhyodacite and dacite, biotite rhyodacite: rhyodacite porphyritic with phenocrysts of perthitic orthoclase and oligoclase; dacite porphyritic with phenocrysts of quartz, hornblende, oligoclase and minor biotite.|
677|Arundel Formation|24551|6|Mentioned|p348|||||||||
677|Arundel Formation|30995|5|Briefly described|p31|||||||||
677|Arundel Formation|31512|5|Briefly described|p308|||||||||
677|Arundel Formation|32008|5|Briefly described|p64|||Strat. relations. Refers Bowler (1970)||||||
677|Arundel Formation|41848|5|Briefly described|p386|||||||||
677|Arundel Formation|42827|5|Briefly described|p386|||||||||
677|Arundel Formation|71203|14|Not recorded|p207-208|||River Terraces.||||||
74891|Ashwin Siltstone Member|64010|5|Briefly described|p258 Fig.1. |Tournaisian|Tournaisian|||Of the Snowy Plains Formation.||||
74891|Ashwin Siltstone Member|64536|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation (Mansfield Group). Mudstone, minor sandstone: mudstone is red, laminated; sandstone is quartz-lithic. Recessive; fluvial deposits.||||||07-FEB-11
74891|Ashwin Siltstone Member|64537|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation (Mansfield Group). Mudstone, minor sandstone: mudstone is red, laminated; sandstone is quartz-lithic. Recessive; fluvial deposits.||||||07-FEB-11
74891|Ashwin Siltstone Member|64538|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation (Mansfield Group). Mudstone, minor sandstone: mudstone is red, laminated; sandstone is quartz-lithic. Recessive; fluvial deposits.||||||07-FEB-11
74891|Ashwin Siltstone Member|64606|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation. Mudstone, minor sandstone: alluvial deposits. Bright green to light blue in RGB with moderate to high U and Th. Nonmagnetic.||||||
74891|Ashwin Siltstone Member|64616|4|Described|p139, p300|Early Carboniferous|Early Carboniferous|New member of Snowy Plains Formation. Conformable over Dungeon Gully Sandstone Member, Mount Kent Conglomerate. Overlain conformably by Home Station Sandstone Member. Top truncated by Barjarg Fault in NW. 200-300m thick. Laminated red siltstone with minor  quartz-lithic sandstone interbeds. Recessive. Geophysical characteristics given.||||||
34838|Attunga Paringa Formation|22968|4|Described|P51, Fig49, P136||Early Devonian|Oldest unit of the Avonmore Subgroup (new name). Type section location given on p137, unconformably underlain by Blueys Creek Formation, maximum thickness is 320m||||||05-AUG-08
34838|Attunga Paringa Formation|23021|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is the Snowy River Volcanics.||||||05-AUG-08
34838|Attunga Paringa Formation|23028|5|Briefly described|Map legend|Pragian|Lochkovian|Parent is Avonmore Subgroup.||||||05-AUG-08
34838|Attunga Paringa Formation|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Avonmore Subgroup.||||||05-AUG-08
34838|Attunga Paringa Formation|23309|4|Described|p113 Tb2.40|||Of the Avonmore Subgroup.  Maximum Thickness: 320m.||||||22-FEB-10
34838|Attunga Paringa Formation|24551|5|Briefly described|p145, p139 Fig. 5.30|Early Devonian|Early Devonian|Of Avonmore Subgroup.||||||
34838|Attunga Paringa Formation|68116|5|Briefly described|Appendix, Map 35.|Pragian|Lochkovian||||||Fluvial sediments: Breccia, conglomerate, sandstone, pebbly sandstone: poorly bedded, with poor to fair sorting; variable rounding; lithic clasts predominant and include volcanics, slate, granite; sandstone generally feldspathic to arkosic.|
37626|Aughaderry Tonalite|23309|6|Mentioned|p422,  App. 1|||G360, I-type. Supersedes Nine Mile Tonalite.||||||
37626|Aughaderry Tonalite|60452|4|Described|p53|||Of the Nine Mile Suite. Originally called Nine Mile Tonalite by White and Chappell (1988). Previously known as Gracedale Tonalite (Evans, 1993). Fine-grained, yellowish grey and weakly porphyritic, with plagioclase phenocrysts up to 7mm in length.||||||
37626|Aughaderry Tonalite|60461|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Nine Mile Suite.  Hornblende tonalite: fine grained, yellowish-grey; weakly porphyritic in plagioclase.||||||
37626|Aughaderry Tonalite|60462|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Nine Mile Suite. Tonalite: I-type, oxidised; highly magnetic (to 250 nT); variable radiometric response, K, Th and U each dominating in some areas||||||
37626|Aughaderry Tonalite|66002|5|Briefly described|p6 Tb.5|||Of Nine Mile Suite. G360. Replaces Nine Mile Tonalite. See VandenBerg et al 2000.||||||
37626|Aughaderry Tonalite|68116|5|Briefly described|Appendix, Map 16.|Early Devonian|Early Devonian||||||Hornblende tonalite: fine grained, yellowish grey; weakly porphyritic in plagioclase; abundant cordierite hornfels xenoliths; I-type; strongly magnetic.|
35960|Avon Supergroup|23309|5|Briefly described|Fig 1.3 p160,171|Carboniferous|Late Devonian|Of the Snowy River Volcanics.||||||
35960|Avon Supergroup|24004|5|Briefly described|p275 Fig.2|Carboniferous|Devonian|||||||
35960|Avon Supergroup|24133|5|Briefly described|p20 Fig. 8|Carboniferous|Late Devonian|Geological Province: Lachlan Fold Belt.||||||
35960|Avon Supergroup|24164|5|Briefly described|p15 Fig.8, p16|Carboniferous|Devonian|Named onshore. Fluvial. Continental sedimentation after the Middle Devonian Tabberabberan Orogeny. Offshore, Curnow (1970) recorded similar rocks in Groper-2 on Gippsland Basin southern platform.|||||Sandstone, conglomerate, acid volcanics|
35960|Avon Supergroup|24551|5|Briefly described|p118 Fig. 5.1, 168, 462|Early Carboniferous|Devonian|Includes the Delatite Group, Wellington Volcanic Group, and Mansfield Group.||||||
35960|Avon Supergroup|24580|6|Mentioned|p828 Fig.1|||Supergroup is supergp in text. Geological Province: Eastern Lachlan Fold Belt.||||||
35960|Avon Supergroup|61161|5|Briefly described|p124-125, p5, p8, p76-77 Fig 6.1|||Includes Delatite Group, Wellington Volcanic Group and Mansfield Group. Non-marine sedimentary and volcanic rocks. Unconformably overlies Cobannah Group.||||||
35960|Avon Supergroup|61163|4|Described|p97, p33|Late Devonian|Late Devonian|Includes all Late Devonian rocks of Howitt Province excluding Tolmie Igneous Complex which it overlies. Supersedes Avon Group. Subdivided into: Delatite Group, Wellington Volcanics and Mansfield Group. Only the latter occurs within BUFFALO. Geol Prov: LFB||||||
35960|Avon Supergroup|61169|5|Briefly described|map legend|Late Devonian|Late Devonian|Includes Mansfield Group (including Mount Kent Conglomerate), Wellington Volcanic Group, and Delatite Group (including Moroka Glen Formation).||||||
35960|Avon Supergroup|61170|5|Briefly described|map legend|Late Devonian|Late Devonian|Includes Mansfield Group (including Mount Kent Conglomerate), Wellington Volcanic Group, and Delatite Group (including Moroka Glen Formation).||||||07-FEB-11
35960|Avon Supergroup|61171|5|Briefly described|map legend|Late Devonian|Late Devonian|Includes Mansfield Group (including Mount Kent Conglomerate), Wellington Volcanic Group, and Delatite Group (including Moroka Glen Formation).||||||
35960|Avon Supergroup|61172|5|Briefly described|map legend|Late Devonian|Late Devonian|Includes Mansfield Group (including Mount Kent Conglomerate), Wellington Volcanic Group, and Delatite Group (including Moroka Glen Formation).||||||
35960|Avon Supergroup|61173|5|Briefly described|map legend|Late Devonian|Late Devonian|Includes Mansfield Group (including Mount Kent Conglomerate), Wellington Volcanic Group, and Delatite Group (including Moroka Glen Formation).||||||
35960|Avon Supergroup|61174|5|Briefly described|map legend|Late Devonian|Late Devonian|Includes Mansfield Group.||||||07-FEB-11
35960|Avon Supergroup|61175|5|Briefly described|map legend|Late Devonian|Late Devonian|Includes Mansfield Group.||||||
35960|Avon Supergroup|61176|5|Briefly described|map legend|Late Devonian|Late Devonian|Includes Mansfield Group.||||||
35960|Avon Supergroup|61177|5|Briefly described|map legend|Late Devonian|Late Devonian|Includes Mansfield Group.||||||
35960|Avon Supergroup|61178|5|Briefly described|map legend|Late Devonian|Late Devonian|Includes Mansfield Group.||||||
35960|Avon Supergroup|61187|5|Briefly described|p16.|Carboniferous|Late Devonian|A post-cratonic transtensional rift sequence. Hosts minor sedimentary copper +/- uranium +/- vanadium +/- silver minerals.||||||
35960|Avon Supergroup|63738|5|Briefly described|p3|Early Carboniferous||Includes the Mansfield Group. Geological Province: Mansfield Basin.||||||28-FEB-08
35960|Avon Supergroup|64010|5|Briefly described|p257, p258 Fig.1, p259  |||Of the Mansfield Basin.|||Includes the Mansfield, Wellington Volcanic and Delatite Groups.|||
35960|Avon Supergroup|64535|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Contains the Mansfield Group.||||||17-DEC-08
35960|Avon Supergroup|64536|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Contains the Mansfield, Wellington and Delatite Groups.||||||07-FEB-11
35960|Avon Supergroup|64537|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Contains the Mansfield, Wellington and Delatite Groups.||||||07-FEB-11
35960|Avon Supergroup|64538|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Contains the Mansfield, Wellington and Delatite Groups.||||||07-FEB-11
35960|Avon Supergroup|64539|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Contains the Mansfield Group.||||||17-DEC-08
35960|Avon Supergroup|64540|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Contains the Mansfield Group.||||||17-DEC-08
35960|Avon Supergroup|64605|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Includes the Mansfield Group.||||||
35960|Avon Supergroup|64606|5|Briefly described|Map Legend|Quaternary|Middle Devonian|Includes Mansfield Group, Wellington Volcanic Group, Delatite Group.||||||12-NOV-08
35960|Avon Supergroup|64616|3|Fully described|p131, p182, p183 Fig.6.29, p186, p189|Mississippian|Givetian|See also p197 Fig.6.34, p278-280, p299-301, p343 Fig.23. Howitt Province. Includes Delatite, Wellington Volcanic, Mansfield Groups. Plant remains common. Less common fish fossils more useful for dating & correlation. Subaerial, mostly fluvial. Geophysical characteristics given.||||||18-SEP-17
35960|Avon Supergroup|68116|5|Briefly described|Appendix, Maps 34, 43.|Late Devonian|Late Devonian||||||Basalt: black to greenish, commonly amygdaloidal; alteration common with abundant chlorite.|
35960|Avon Supergroup|71040|5|Briefly described|p13|Early Carboniferous|Late Devonian|Mt Howitt Province.||||Unconformably overlies Wentworth Group.|Flat-lying sandstones.|
34825|Avonmore Subgroup|22968|4|Described|P91, P136||Early Devonian|New subgroup of Snowy River Volcanics, conformably overlain by Buchan Group, maximum thickness of 700m||||||
34825|Avonmore Subgroup|23028|5|Briefly described|Map legend|Pragian|Lochkovian|Parent is Snowy River Volcanics, overlying unit is Buchan Group||||||
34825|Avonmore Subgroup|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Snowy River Volcanics||||||
34825|Avonmore Subgroup|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Snowy River Volcanics||||||
34825|Avonmore Subgroup|23309|4|Described|p113,132 Table: 2.40.|||Of Snowy River Volcanics. Maximum Thickness: 700m.||||||22-FEB-10
34825|Avonmore Subgroup|24551|5|Briefly described|p145, p147, p139 Fig. 5.30|Early Devonian|Early Devonian|Of Snowy River Volcanics.||||||
34825|Avonmore Subgroup|66197|5|Briefly described|p629, p634, p635 Fig.5c|||Buchan Basin. Includes basement-derived conglomerate/breccia, silicic volcanics and volcaniclastics. Underlies the Buchan Caves Limestone.||||||13-MAR-12
41187|Awaiti Granite|50154|2|Defined|p94, p247 App.5|Cambrian|Cambrian|Mapped as 'felsic Tuloona Granodiorite' by Kemp & Gray (1999). Of the Glenelg River Metamorphic Complex.||||||25-SEP-09
41187|Awaiti Granite|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Muscovite-biotite granite||||||
41187|Awaiti Granite|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite.||||||20-AUG-04
41187|Awaiti Granite|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite.||||||20-AUG-04
41187|Awaiti Granite|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite.||||||20-AUG-04
41187|Awaiti Granite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite.||||||20-AUG-04
41187|Awaiti Granite|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite.||||||20-AUG-04
41187|Awaiti Granite|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite.||||||20-AUG-04
41187|Awaiti Granite|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite.||||||20-AUG-04
41187|Awaiti Granite|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite.||||||20-AUG-04
41187|Awaiti Granite|66002|5|Briefly described|p9 Tb.5|||G444. Referred to as the 'felsic phase' of Tuloona Granodiorite of Kemp and Gray (1999). Defined by Morand et al. 2003.||||||
41187|Awaiti Granite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Muscovite-biotite granite: foliated to massive, buff, medium grained, porphyritic with phenocrysts of microcline and quartz; local schlieric foliation; metasedimentary enclaves common near northern margin; non-magnetic.|
839|Bacchus Marsh Formation|23258|5|Briefly described|Fig12-3.1p214, 215, 218||Permian|||||||
839|Bacchus Marsh Formation|23259|5|Briefly described|Fig12-4.3p228, 230, 237||Permian|||||||
839|Bacchus Marsh Formation|23979|5|Briefly described|p207|Permian|Carboniferous|||||||
839|Bacchus Marsh Formation|24383|4|Described|p40 Fig.17|Permian|Permian|Overlain by Newer Volcanic Group. Underlain by Castlemaine Group. Max. Thickness: 100m. Geological Province: Lachlan Fold Belt.||||||14-JAN-09
839|Bacchus Marsh Formation|24384|5|Briefly described|Map legend|Permian|Permian|Tillite, silty diamictite, diffusely stratified, poorly sorted, well rounded;  pebbles commonly striated; exotic clasts include pink and grey granite, intermediate volcanic rocks, ignimbrite, chert, pink gneiss, metasedimentary rocks.||||||
839|Bacchus Marsh Formation|24385|5|Briefly described|Map legend|Permian|Permian|Tillite: silty diamictite, diffusely stratified; poorly sorted, well rounded; pebbles commonly striated; exotic clasts include pink and grey granite, intermediate volcanic rocks, ignimbrite, chert, pink gneiss, metasedimentary rocks.||||||
839|Bacchus Marsh Formation|24386|5|Briefly described|Map legend|Permian|Permian|Tillite: silty diamictite; diffusely stratified; poorly sorted, well rounded; pebbles commonly striated; exotic clasts include pink and grey granite, intermediate volcanic rocks, ignimbrite, chert, pink gneiss, metasedimentary rocks.||||||
839|Bacchus Marsh Formation|24387|5|Briefly described|Map legend|Permian|Permian|Tillite: silty diamictite; diffusley stratified; poorly sorted, well rounded; pebbles commonly straited; exotic clasts include pink and grey granite, intermediate volcanic rocks, ignimbrite, chert, pink gneiss, metasedimentary rocks.||||||22-JUN-04
839|Bacchus Marsh Formation|24388|5|Briefly described|Map legend|Permian|Permian|Tillite: nonmagnetic; no distinctive radiometric response.||||||27-OCT-08
839|Bacchus Marsh Formation|24551|5|Briefly described|p196, 607|Early Permian|Early Permain|Maximum Thickness: 1100m.  ||||||22-OCT-22
839|Bacchus Marsh Formation|39865|4|Described|p15|||||||||
839|Bacchus Marsh Formation|41567|4|Described|p2|||||||||
839|Bacchus Marsh Formation|44186|5|Briefly described|Map Legend||Permian|||||||
839|Bacchus Marsh Formation|44197|5|Briefly described|Map Legend||Permian|||||||
839|Bacchus Marsh Formation|50154|2|Defined|p25, p121-123|Permian|Permian|Has been erroneously referred to as the Wild Duck Formation. Nonconformably overlies metamorphics of the Glenelg River Metamorphic Complex. Disconformably overlain by the Coleraine Volcanic and Otway Groups. Intruded by the Coleraine Volcanic Group.||||||25-SEP-09
839|Bacchus Marsh Formation|50155|5|Briefly described|Map Legend|Permian|Permian|Glacial to fluviglacial; tillite, diamictite, varved clay.||||||25-JUN-13
839|Bacchus Marsh Formation|50156|5|Briefly described|Map Legend|Permian|Permian|Glacial deposits: tillite, silty diamictite, diffusely stratified, moderately consolidated to unconsolidated; varved clay.||||||25-JUN-13
839|Bacchus Marsh Formation|50157|5|Briefly described|Map Legend|Permian|Permian|Glacial deposits: tillite, silty diamictite, diffusely stratified, moderately consolidated to unconsolidated; varved clay.||||||25-JUN-13
839|Bacchus Marsh Formation|50158|5|Briefly described|Map Legend|Permian|Permian|Overlies Glenelg River Metamorphic Complex, Mount Stavely Complex and Nangkita Granite. Glacial deposits: tillite, silty diamictite, diffusely stratified, moderately consolidated to unconsolidated; varved clay.||||||25-JUN-13
839|Bacchus Marsh Formation|50159|5|Briefly described|Map Legend|Permian|Permian|Glacial deposits: tillite, silty diamictite, diffusely stratified, moderately consolidated to unconsolidated; varved clay.||||||25-JUN-13
839|Bacchus Marsh Formation|50160|5|Briefly described|Map Legend|Permian|Permian|Glacial deposits: tillite, silty diamicrite, diffusely stratified, moderately consolidated to unconsolidated; varved clay.||||||24-JUN-04
839|Bacchus Marsh Formation|50161|5|Briefly described|Map Legend|Permian|Permian|Overlies the Glenelg River Metamorphic Complex and Hassalls Creek. Glacial deposits: tillite, silty diamictite, diffusely stratified, moderately consolidated to unconsolidated; varved clay.||||||25-JUN-13
839|Bacchus Marsh Formation|50162|5|Briefly described|Map Legend|Permian|Permian|Glacial deposits: tillite, silty diamicrite, diffusely stratified, moderately consolidated to unconsolidated; varved clay.||||||
839|Bacchus Marsh Formation|50163|5|Briefly described|Map Legend|Permian|Permian|Glacial deposits: tillite, silty diamicrite, diffusely stratified, moderately consolidated to unconsolidated; varved clay.||||||
839|Bacchus Marsh Formation|50164|5|Briefly described|Map Legend|Permian|Permian|Glacial to fluviglacial; tillite, diamicrite, varved clay.||||||27-OCT-08
839|Bacchus Marsh Formation|60421|5|Briefly described|p408 Fig. 1, 414 Fig. 4|Permian|Permian|Underlies: Duddo Limestone, Dorodong Sands. Fluvio-glacial deposits.||||||
839|Bacchus Marsh Formation|60599|5|Briefly described|p79-80, p82|Late Permian|Early Permian|Of Roberts (1984, 1985). Considered to be a junior synonym of Wild Duck Formation. Contains Glossopteris and Gangamopteris flora. ||||||
839|Bacchus Marsh Formation|62370|5|Briefly described|p447|Permian|Permian|Fluviomarine-glacial diamictites.||||||
839|Bacchus Marsh Formation|64532|4|Described|p373-384|Sakmarian|Sakmarian|Of Roberts (1984). Nine glacial advances are recorded in a section at Korkuperrimul Creek. Contains Gangamopteris.|||Includes Morton Conglomerate Member.||Diamictites interbedded with massive to laminated sandstone, conglomerate, interbedded sandstone and siltstone (often dolomitised).|
839|Bacchus Marsh Formation|64611|5|Briefly described|Map legend|Permian|Permian|Tillite, diamictite, conglomerate, sandstone + mudstone: variably sorted/rounded; massive to diffusely stratified; mod'ly to poorly consolidated; lithics commonly striated; exotic clasts incl. granite, intermed. volcs, chert + metsed. rocks||||||
839|Bacchus Marsh Formation|64612|2|Defined|p28, p46-47, p55|Early Permian|Early Permian|Murray (1887). Unconformably underlain by Castlemaine Group. In places disconformably overlain by Newer Volcanics. Thickness: 25.4m. Diamictite interbedded with medium to coarse-grained lithic sandstone.||||||25-JUN-13
839|Bacchus Marsh Formation|65715|5|Briefly described|p9 Tb.5|Permian|Permian|Includes Morton Conglomerate Member. Junior synonym of Wild Duck Formation of Edwards et al. (1998).||||||25-JUN-13
839|Bacchus Marsh Formation|65969|6|Mentioned|p17 Fig.7|||||||||
839|Bacchus Marsh Formation|68116|5|Briefly described|Appendix, Maps 23-24, 29, 31-32, 38, 41.|Permian|Carboniferous|Contains plant fossils and rare shallow-marine shelly fossils.|||||Tillite, diamictite, sandstone, mudstone, conglomerate: tillite and diamictite grey; massive to slump-folded; conglomerates (well-rounded)are pebble to boulder size; mudstone dark grey to black; thinly bedded to laminated; sedimentary dykes common.|
839|Bacchus Marsh Formation|71419|6|Mentioned|p16 Fig 17|Permian|Carboniferous|Periglacial sediments.||||||02-FEB-18
839|Bacchus Marsh Formation|71593|4|Described|p8, p12, p44-p45,49-50|Permian|Permian|Glacial deposits. Maximum thickness up to 370m. Preserved in the Netherby Trough. See also  p102, p133, p138.|||||Fluvioglacial sedimentary outwash and till deposits.|23-AUG-22
839|Bacchus Marsh Formation|73497|5|Briefly described|Map legend|Permian|Permian||||||Fluvioglacial deposits: nonmagnetic, low K, Th and U.|
899|Bairnsdale Limestone|23768|5|Briefly described|p28 Fig.5|Middle Miocene|Middle Miocene|Geological Province: Gippsland Basin. See also p43, p45, p91.||||||11-SEP-09
899|Bairnsdale Limestone|23909|5|Briefly described|p290 Fig.3|Miocene|Miocene|Of the Seaspray Group.  Geological Province: Gippsland Basin.||||||
899|Bairnsdale Limestone|24551|5|Briefly described|p327 Fig. 10.33|Miocene|Miocene|||||||
899|Bairnsdale Limestone|30093|6|Mentioned|p19|||||||||
899|Bairnsdale Limestone|31509|6|Mentioned|p156|||||||||
899|Bairnsdale Limestone|33459|6|Mentioned|Table 1|||||||||
899|Bairnsdale Limestone|33689|5|Briefly described|p13|||||||||
899|Bairnsdale Limestone|34421|6|Mentioned|p253|||See also P268||||||
899|Bairnsdale Limestone|34954|6|Mentioned|Fig.35|||||||||
899|Bairnsdale Limestone|34962|6|Mentioned|p325|||||||||
899|Bairnsdale Limestone|35271|6|Mentioned|Fig.2|||||||||
899|Bairnsdale Limestone|35720|6|Mentioned|p131|||See also Fig.2, stratigraphic column.||||||
899|Bairnsdale Limestone|37330|6|Mentioned|p34|||||||||
899|Bairnsdale Limestone|38070|6|Mentioned|Fig.12|||Gippsland Basin||||||
899|Bairnsdale Limestone|41043|6|Mentioned|p105|||||||||
899|Bairnsdale Limestone|41231|6|Mentioned|p110|||||||||
899|Bairnsdale Limestone|41511|4|Described|p14|||||||||
899|Bairnsdale Limestone|41519|6|Mentioned|p172|||||||||
899|Bairnsdale Limestone|42827|6|Mentioned|p401|||||||||
899|Bairnsdale Limestone|43667|6|Mentioned|Fig.3,p12||Miocene|||||||
899|Bairnsdale Limestone|60538|5|Briefly described|p482 Fig. 21, 488 Fig. 27|||Geological Province: Gippsland Basin.||||||
899|Bairnsdale Limestone|63217|5|Briefly described|p9, p102. |||Equivalent to the paralic clays and sands of the Boisdale Formation.||||Overlies Wuk Wuk Marl Formation. Is overlain by Haunted Hills Formation.||
899|Bairnsdale Limestone|65717|6|Mentioned|p12|Pliocene|Miocene|Part of unnamed marine sequence.||||||05-SEP-17
899|Bairnsdale Limestone|65718|6|Mentioned|p10 Fig 3.2, p12|Pliocene|Miocene|Middle Miocene minimum age.||Of the Seaspray Group.||||
899|Bairnsdale Limestone|66181|6|Mentioned|p311|Miocene||||||||
899|Bairnsdale Limestone|67061|5|Briefly described|p554 Fig.10.|Miocene|Miocene|Gippsland Basin, onshore.||Unit in Seaspray Group.||Overlies Wuk Wuk Marl. Is overlain by Tambo River Formation.||
899|Bairnsdale Limestone|69016|5|Briefly described|p88-89|||Of the Gippsland Basin. Marls act as aquitards, while fracture limestone acts as aquifers.||Unit of Seaspray Group.|||Marine marl and carbonate units.|
899|Bairnsdale Limestone|70076|5|Briefly described|Regional: Fig.3|Tortonian|Langhian|||Seaspray Group.||Overlies Wuk Wuk Marl. Is overlain by Tambo River Formation.||
899|Bairnsdale Limestone|70862|6|Mentioned|p48 Fig.1|||Latrobe Valley, Gippsland Basin.||Seaspray Group.||Overlies Wuk Wuk Marl. Is overlain by Tambo River Formation.||
899|Bairnsdale Limestone|70995|14|Not recorded|p159||Miocene|||||||
31143|Bald Hill Volcanic Complex|24440|6|Mentioned|Map legend|||{Located in "Regolith Excursion Sites" legend on main map].||||||
31143|Bald Hill Volcanic Complex|43493|4|Described|34-66||Pleistocene|Radiometric K-Ar Age: 1.64 Ma||||||
31143|Bald Hill Volcanic Complex|65969|5|Briefly described|p30|Calabrian|Calabrian|Basaltic extrusives. Age of 1.64 Ma (Webb, 1989).||||||
34843|Bald Hills Creek Tonalite|22968|5|Briefly described|P60, P201|Early Devonian|Late Silurian|New name, parent of unit is Ensay Suite||||||
34843|Bald Hills Creek Tonalite|23029|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Ensay Suite||||||
34843|Bald Hills Creek Tonalite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Part of the Ensay Suite.||||||19-AUG-08
34843|Bald Hills Creek Tonalite|23309|5|Briefly described|p296|||G149. I-Type.||||||
34843|Bald Hills Creek Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Biotite-hornblende tonalite: grey; medium to coarse-grained; equigranular; porphyritic in euhedral hornblende; rare microgranitoid enclaves; patchy chlorite, epidote and hematite alteration.|
34911|Baldhead Igneous Complex|22968|6|Mentioned|P190|||Intruded Pinnak Sandstone||||||
34911|Baldhead Igneous Complex|23309|6|Mentioned|p284,285,343|||See also Mount Baldhead Igneous Complex.||||||
73147|Ballan Volcanics|61896|6|Mentioned|p1|||Within the Ballan Graben.||||||19-DEC-07
35961|Ballantyne Megabreccia|23309|4|Described|p110, 114. Tb2.40|||Of the Bermarr Subgroup. Maximum Thickness: 300m.||||||22-FEB-10
35961|Ballantyne Megabreccia|23615|4|Described|p102|Early Devonian|Early Devonian|Of Berrmarr Subgroup.  Overlain by Black Mountain Ignimbrite. 300m thick at type section.  Overlies Currie Creek Ignimbrite south of the Wulgulmerang-Bonang Road.  See also Ballantyne Gap Megabreccia.||||||
35961|Ballantyne Megabreccia|24551|4|Described|p143|||Of the Berrmarr Subgroup||||||
35961|Ballantyne Megabreccia|68115|5|Briefly described|p4.|Devonian|Devonian|Originally Ballantyne Gap Megabreccia (Orth et al. 1995); name shortened by VandenBerg et al. (2000).||Unit in Snowy River Volcanic Group.||||
35961|Ballantyne Megabreccia|68116|5|Briefly described|Appendix, Maps 28, 36.|Pragian|Lochkovian||||||Megabreccia: volcanic and minor granite blocks (up to 30m across), in a pebbly mudstone matrix, intrusive rhyolite.|
23355|Ballark Conglomerate|37385|2|Defined|p35|Pliocene|late Miocene|Probably Late Miocene-Pliocene.||||||
23355|Ballark Conglomerate|37547|3|Fully described|p149|||||||||
23355|Ballark Conglomerate|38159|6|Mentioned|Map legend|Miocene|Miocene|Pliocene to Pleistocene||||||
23355|Ballark Conglomerate|39865|6|Mentioned|p36|||||||||
23355|Ballark Conglomerate|65715|4|Described|p9 Tb.6 p10, p12, p27, p31|Cretaceous|Cretaceous|Overlain by Werribee Formation. Consists almost entirely of lithic material locally derived from Castlemaine Group rocks. Age given as Early Cretaceous based on similarities with Crayfish Subgroup conglomerate.||||||
23355|Ballark Conglomerate|68116|5|Briefly described|Appendix, Map 41.|Early Cretaceous|Early Cretaceous||||||Conglomerate, minor sandstone: pebble to boulder conglomerate; massive; clasts predominantly of Ordovician sandstone with minor vein quartz pebbles; sandstone medium to coarse-grained; cross-bedded; with occasional pebbles.|
21183|Bally Hooley Ignimbrite|23309|4|Described|p109, 131 Tb 2.40|||Of Little River Subgroup.  Maximum Thickness: 500m.||||||12-JUN-08
21183|Bally Hooley Ignimbrite|23615|3|Fully described|p117|Early Devonian|Early Devonian|Of Little River Subgroup.  Granular to ash-like ignimbrite with abundant feldspar phenocrysts and few quartz crystals. Age: Early Devonian ~410-395Ma. Interfingers with the Moonkan Ignimbrite.||||||16-AUG-18
21183|Bally Hooley Ignimbrite|24551|5|Briefly described|p144|||Of Little River Subgroup.||||||
21183|Bally Hooley Ignimbrite|43206|5|Briefly described|map legend||Lochkovian|Of Little River Subgroup.||||||12-JUN-08
21183|Bally Hooley Ignimbrite|43312|5|Briefly described|Map Legend||Early Devonian|Of Little River Group.||||||12-JUN-08
21183|Bally Hooley Ignimbrite|43313|5|Briefly described|Map Legend||Early Devonian|Of Little River Group||||||12-JUN-08
21183|Bally Hooley Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Feldspar ignimbrite: up to 5% quartz, variable crystal content; pyroclastic deposits.|
21184|Ballyrogan Granite|22756|5|Briefly described|P40, P49|||||||||
21184|Ballyrogan Granite|23309|6|Mentioned|p422 App1|||G385. I-Type.||||||
21184|Ballyrogan Granite|43260|5|Briefly described|Map Legend||Early Devonian|Of the Ararat Suite. Biotite-muscovite granite: pale cream, felsic, fine grained; granophyric intergrowths between quartz and feldspar. Aggregates of muscovite and tourmaline scattered throughout; trace amounts of garnet.||||||27-OCT-04
21184|Ballyrogan Granite|44186|5|Briefly described|Map Legend||Early Devonian|G385 Unassigned.||||||
21184|Ballyrogan Granite|66002|5|Briefly described|p7 Tb.5|||Of Ararat Suite. G385.  Defined by Cayley and McDonald 1995.||||||
21184|Ballyrogan Granite|68116|5|Briefly described|Appendix, Map 31.|Early Devonian|Early Devonian||||||Biotite-muscovite granite: pale cream, felsic, fine grained; granophyric intergrowths between quartz and feldspar; aggregates of muscovite and of tourmaline scattered throughout; trace amounts of garnet.|
76928|Balmattum Basalt|66244|3|Fully described|pp7-8.|Cenozoic|Cenozoic|New unit. Occupies a small area near Balmattum, Euroa area. Description and analysis in Paul et al. (2005). Type location is the Balmattum quarry, around MGA 383000-5839400; the rock appears as a black fine-grained mafic rock with dark spots on weathered faces.||Unit in Euroa Volcanic Group.||Is overlain by Shepparton Formation at downstream end of flow..|Dark grey, basanite to alkali basalt; euhedral olivine phenocrysts 1 - 5 mm across in a groundmass of clinopyroxene prisms, magnetite cubes and minor interstitial glass; minor analcite after nepheline and red-brown biotite; amygdales common.|12-FEB-15
76928|Balmattum Basalt|68116|5|Briefly described|Appendix, Map 25.|Miocene|Miocene||||||Dark grey mafic volcanic rock with olivine phenocrysts 1-5 mm across in a groundmass of clinopyroxene, olivine, plagioclase, magnetite and glass, with minor analcite after nepheline. Ranges from basanite to alkali basalt.|
1002|Balmoral Pegmatite|42889|6|Mentioned|p288|||||||||
24171|Balook Formation|13323|5|Briefly described|p393 Fig. 2|Late Oligocene|Early Oligocene|Of the Latrobe Valley Subgroup (Seaspray Group). Fluvial-deltaic and paralic deposits. Geological Province: Gippsland Basin.||||||
24171|Balook Formation|23885|6|Mentioned|p163 Fig. 14.3|||Geological Province: Gippsland Basin.||||||18-FEB-05
24171|Balook Formation|24090|5|Briefly described|p8 Fig.3|Oligocene|Oligocene|Geological Province: Gippsland Basin.||||||
24171|Balook Formation|24551|5|Briefly described|p328, 504, p327 Fig. 10.33|Miocene|Oligocene|Maximum Thickness: 500m.||||||
24171|Balook Formation|37530|5|Briefly described|p9|||||||||
24171|Balook Formation|38929|4|Described|p49|||See also Fig.6||||||
24171|Balook Formation|38930|5|Briefly described|p64|||||||||
24171|Balook Formation|38973|6|Mentioned|p565|||||||||
24171|Balook Formation|40117|6|Mentioned|p66|||||||||
24171|Balook Formation|41868|6|Mentioned|Fig.12.14|||See also P550||||||
24171|Balook Formation|42184|6|Mentioned|p350|||||||||
24171|Balook Formation|42649|5|Briefly described|p201|||||||||
24171|Balook Formation|42827|5|Briefly described|Fig 8.21|||||||||
24171|Balook Formation|60538|5|Briefly described|p475 Fig. 14, 472 Fig. 11, 481|Oligocene|Oligocene|Geological Province: Gippsland Basin. Shoreline sand facies.||||||
24171|Balook Formation|61302|5|Briefly described|p11 Fig.4|Miocene|Oligocene|Of the Latrobe Group. Geological Province: Gippsland Basin.||||||
24171|Balook Formation|61336|5|Briefly described|p(iv), p(v) Fig. 5|Middle Miocene|Oligocene|Of the Seaspray Group. Two main units each comprising a series of stacked barrier sands; quartzose sands.  Max. thickness: 400m.||||||07-FEB-11
24171|Balook Formation|61552|6|Mentioned|p583 Fig.2. |Late Oligocene|Early Oligocene|||Unit in Latrobe Valley Subgroup.||||
24171|Balook Formation|63217|6|Mentioned|p102. |||East of Rosedale. A facies change between the terrestrial brackish Yallourn Seam and the marine Wuk Wuk Marl.|||||Barrier sand and clay.|
24171|Balook Formation|64876|5|Briefly described|p145 Fig.2|Oligocene|Oligocene|Gippsland Basin.||Seaspray Group.||||
24171|Balook Formation|65717|5|Briefly described|p9 figure 2.2|Oligocene|Oligocene|||Latrobe Valley Subgroup||Unconformably overlies Burong Formation|Sandstone.|
24171|Balook Formation|65718|5|Briefly described|p12, p10 Fig 3.2|Miocene|Oligocene|Comprises a barrier sand system that laterally separates the Seaspray Group from the Latrobe Valley Coal Measures. Limited in lateral extent but contains tongues that extend up to 30 km into the Latrobe Valley Coal Measures.||||Interfingers with the Lakes Entrance Formation.||
24171|Balook Formation|67727|5|Briefly described|p58 Fig.2, p60 Fig.3.|Oligocene|Oligocene|Onshore Gippsland Basin. Paralic equivalent to the coal and fluvial deposits of the Morwell Formation, and the marine deposits of the lower Lakes Entrance Formation in the offshore part of the Basin.||||Is overlain by Haunted Hill Formation.||11-JUL-12
24171|Balook Formation|69016|5|Briefly described|p88-91,93-97|Late Miocene|Early Oligocene|Of the Gippsland Basin. [Misspelt Baloock on p91, Ballok on p93].||||Laterally grades into Morwell and Yallourn fomations (west) and Lakes Entrance Formation and Gippsland Limestone (east).|Fine marine sand with considerable clay content, becoming coarser grained with less clay.|
24171|Balook Formation|69750|6|Mentioned|p68|||Gippsland Basin. Formed a barrier complex which was occasionally breached.||||||
24171|Balook Formation|70028|6|Mentioned|p79|Miocene|Oligocene|Onshore Gippsland Basin.||||||
24171|Balook Formation|73289|5|Briefly described|p764, 765 Fig.2, 767-768|Miocene|Oligocene|||||Interfingers with (lateral facies variation of) Morwell and Yallourn Formations and Seaspray Group.|Brackish marine sediments.|
24171|Balook Formation|73471|5|Briefly described|p86|||Gippsland Basin.||Seaspray Group||Overlies Burong Formation|Fluvial-deltaic and paralic sandstones and siltstones.|
24171|Balook Formation|73488|5|Briefly described|p631, p632 Fig.2, p633 Fig.3, p636, p646|Miocene|Oligocene|Gippsland Basin.||||Grades laterally into the Yallourn and Morwell Formations, and Seaspray Group.|Stacked barrier sand sequence.|
24171|Balook Formation|73562|5|Briefly described|p300, 303-304, 306, 310-312, 314, 316|Pliocene|Oligocene|Gippsland Basin; onshore. Barrier/shoreface setting.||||The lower part is equivalent to Lakes Entrance Formation. Interfingers with Morwell Formation.|Interbedded, marginal marine sandstones, clayey sandstones, and coals.|
24171|Balook Formation|75065|5|Briefly described|p151|Pliocene|Oligocene|Gippsland Basin.||Latrobe Valley Group.||Unconformably overlies Childers Formation. Is adjacent to Morwell and Yallourn Formations and Gippsland Limestone. Is overlain unconformably by Sale Group.|Shallow-marine and deltaic sands.|
72930|Bambra Sandstone|61186|5|Briefly described|p86|Tertiary|Tertiary|Hard, cream micaceous dimension stone found at Airey's Inlet; not ferruginised as are some of the Tertiary sandstones therefore pale in colour; bedded, micaceous quartzose sandstone.||||||
30358|Bandts Granite|23165|5|Briefly described|Map legend||Devonian|||||||
35970|Banimboola Quartz Monzodiorite|23309|4|Described|p294,342,344,345||Devonian|G110. I-Type. Age: K/Ar  405+/-16Ma, 399+/-16Ma, 406+/-6Ma, 388+/-4Ma, 400 +/-16Ma, 394+/-7Ma. Supersedes Banimboola Diorite, Banimboola Granodiorite, Banimboola Quartz Diorite. Of the Boggy Plain Supersuite.||||||11-JUL-13
35970|Banimboola Quartz Monzodiorite|24142|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||
35970|Banimboola Quartz Monzodiorite|24143|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||
35970|Banimboola Quartz Monzodiorite|24144|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||
35970|Banimboola Quartz Monzodiorite|24145|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt||||||
35970|Banimboola Quartz Monzodiorite|24146|5|Briefly described|Map Legend|Devonian|Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt. Age: 403 +/- 6 Ma (K/Ar)||||||13-SEP-04
35970|Banimboola Quartz Monzodiorite|24551|6|Mentioned|p408|Early Devonian|Early Devonian|Age: 398 +/- 5Ma, 406 +/- 11Ma.||||||
35970|Banimboola Quartz Monzodiorite|60503|4|Described|p157, p174|Early Devonian|Early Devonian|Of the Boggy Plains Supersuite. Probably superseded the Banimboola Granite? Intrusive rocks within the Omeo Metamorphic Complex. Intrudes both Pinnak Sandstone and Dartmouth Granite.||||||
35970|Banimboola Quartz Monzodiorite|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Boggy Plains Supersuite. Hornblende-biotite quartz diorite: I-type; 405+/-16 (K/Ar biotite), 401+/-14 Ma (K/Ar hornblende); intensely magnetic (750 nT) with north-northeast trends; moderate K, low total count, Th, U.||||||
35970|Banimboola Quartz Monzodiorite|61160|3|Fully described|p78, p30 Tb. 5.2, p10, p58-59 Fig.6.8|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. In outcrop, forms large tors of fresh greenish-grey quartz monzodiorite; variable in texture and evenly grained; no foliation. Intruded Dartmouth Granite, Pinnak Sandstone and Wallaby Granite. Age: 400+/-16Ma. ||||||
35970|Banimboola Quartz Monzodiorite|61161|5|Briefly described|p31|||Highly magnetic I-type granite; high gravity.||||||
35970|Banimboola Quartz Monzodiorite|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Hornblende-biotite-clinopyroxene quartz monzodiorite: quartz diorite in part; greenish grey; medium grained; equigranular; I-type intrusion. GSV map code: G110.||||||
35970|Banimboola Quartz Monzodiorite|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Hornblende-biotite-clinopyroxene quartz monzodiorite: quartz diorite in part; greenish grey; medium grained; equigranular; I-type intrusion. GSV map code: G110.||||||
35970|Banimboola Quartz Monzodiorite|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Hornblende-biotite-clinopyroxene quartz monzodiorite: quartz diorite in part; greenish grey; medium grained; equigranular; I-type intrusion. GSV map code: G110.||||||
35970|Banimboola Quartz Monzodiorite|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Hornblende-biotite-clinopyroxene quartz monzodiorite: quartz diorite in part; greenish grey; medium grained; equigranular; I-type intrusion. GSV map code: G110.||||||07-FEB-11
35970|Banimboola Quartz Monzodiorite|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Hornblende-biotite-clinopyroxene quartz monzodiorite, quartz diorite in part (I-type, 405 +/- 8 Ma: K/Ar biotite, 400 +/- 13 Ma: K/Ar hornblende); highly magnetic and nonmagnetic subdivisions. GSV map code: G110.||||||
35970|Banimboola Quartz Monzodiorite|61187|5|Briefly described|pp15-16.|||Mentioned as possibly prospective for copper-gold mineralisation, although may be less prospective than NSW mineralisation, having formed on continental crust.||Unit in Boggy Plains Supersuite.||||
35970|Banimboola Quartz Monzodiorite|68116|5|Briefly described|Appendix, Maps 20, 27.|Early Devonian|Early Devonian||||||Hornblende-biotite-clinopyroxene quartz monzodiorite, quartz diorite in part: greenish grey, equigranular, medium-grained; intensely magnetic; I-type.|
1066|Banksia Chert Member|22968|5|Briefly described|P50, P104||Late Ordovician|Parent is Blueys Creek Formation||||||
1066|Banksia Chert Member|23021|5|Briefly described|Map legend|Late Ordovician|Late Ordovician|Parent is the Blueys Creek Formation||||||
1066|Banksia Chert Member|23309|5|Briefly described|p60 Tb2.20||Gisbornian|Of Kiandra Group.||||||
1066|Banksia Chert Member|23615|5|Briefly described|p67|Late Ordovician|Late Ordovician|Of Blueys Creek Formation. Thin-bedded chert; contains conodont fossils indicating a possible Gisbornian age.||||||
1066|Banksia Chert Member|24551|5|Briefly described|p106|Late Ordovician|Late Ordovician|Of Blueys Creek Formation.||||||
1066|Banksia Chert Member|41570|3|Fully described|p92|||||||||
1066|Banksia Chert Member|42827|6|Mentioned|p92|||of Bluey's Creek Formation||||||
1066|Banksia Chert Member|63278|4|Described|p157|Gisbornian|Darriwilian |Of Blueys Creek Formation, Kiandra Group. Overlain by Brumby Mafic Arenite Member. Geological Province: Kiandra Volcanic Belt, LFB. Consists of thin-bedded chert. Conodonts present in unit give a probable Gisbornian age.||||||07-FEB-11
1066|Banksia Chert Member|67322|5|Briefly described|p26|Sandbian|Sandbian|Contains conodonts indicating a Gisbornian age.||Of the Blueys Creek Formation.|||Black chert layers.|
32305|Banoon Member|12796|5|Briefly described|p456 Fig. 2|Turonian|Turonian|Of the Flaxman Formation (Sherbrook Group). Sedimentary ironstone characterised by abundant authigenic and partly oolitic chamosite and goethite. Geological Province: Otway Basin/Port Campbell Embayment.||||||
32305|Banoon Member|67366|5|Briefly described|p103 Fig.2. |Coniacian|Coniacian|||Unit in Flaxman Formation.||Is overlain by Belfast Formation.|Shallow to nearshore marine sandstone and shale.|
32305|Banoon Member|69297|6|Mentioned|p98|Coniacian|Coniacian|Otway Basin. ||Flaxman Formation|||Mudstone. |
32305|Banoon Member|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Late Cretaceous|Late Cretaceous|Otway Basin: Port Campbell Embayment.||Flaxman Formation.||Is overlain by Belfast Mudstone.||
32305|Banoon Member|70193|6|Mentioned|p284 Fig 2|Turonian|Turonian|Geological province: Otway Basin. Part of the Sherbrook Supersequence.||Of Flaxman Formation?||||
32305|Banoon Member|73594|5|Briefly described|p25|||Of Partridge (2001). May be present at the top of the Flaxman Formation and is a reliable marker of the boundary with the overlying Belfast Mudstone.||Flaxman Formation|||Thin sedimentary ironstone unit.|
28253|Baranduda Granite|22971|5|Briefly described|p 30|||||||||
28253|Baranduda Granite|23309|5|Briefly described|p423 App1|Middle Devonian|Early Devonian|G176. I-Type. Age: 388 +/- 4.||||||
28253|Baranduda Granite|38879|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Middle to Lower Devonian||||||
28253|Baranduda Granite|39446|5|Briefly described|p26|||||||||
28253|Baranduda Granite|68116|5|Briefly described|Appendix, Map 19.|Early Devonian|Early Devonian||||||Biotite-muscovite granite: grey, medium grained, equigranular.|
35971|Barangaroo Ignimbrite|23309|5|Briefly described|p82, Tb2.28|||Of the Rockland Volcanics.||||||
35971|Barangaroo Ignimbrite|50154|2|Defined|p119-120|Early Devonian|Early Devonian|Of the Rocklands Volcanic Group. Overlies the Toolondo Volcaniclastics and Grampians Group.||||||15-SEP-04
35971|Barangaroo Ignimbrite|50155|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Quartz-feldspar ignimbrite||||||
35971|Barangaroo Ignimbrite|50156|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz-feldspar ignimbrite: crystal- and lithic-poor; fiamme foliation, rare fragmented crystals and a densely welded matrix of relict glass shards at base; rheomorphic flow banding and minor autobrecciation.||||||
35971|Barangaroo Ignimbrite|50157|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz-feldspar ignimbrite: crystal- and lithic-poor; fiamme foliation, rare fragmented crystals and a densely welded matrix of relict glass shards at base; rheomorphic flow banding and minor autobrecciation.||||||
35971|Barangaroo Ignimbrite|50158|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz-feldspar ignimbrite: crystal- and lithic-poor; fiamme foliation, rare fragmented crystals and a densely welded matrix of relict glass shards at base; rheomorphic flow banding and minor autobrecciation.||||||
35971|Barangaroo Ignimbrite|50159|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Overlies Grampians Group. Overlain by Shepparton Formation and Parilla Sand Quartz-feldspar ignimbrite: crystal- and lithic-poor; fiamme foliation, rare fragmented crystals, densely welded matrix of relict glass shards at base||||||25-JUN-04
35971|Barangaroo Ignimbrite|50160|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz-feldspar ignimbrite||||||
35971|Barangaroo Ignimbrite|50161|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz-feldspar ignimbrite: crystal- and lithic-poor; fiamme foliation, rare fragmented crystals and a densely welded matrix of relict glass shards at base; rheomorphic flow banding and minor autobrecciation.||||||24-JUN-04
35971|Barangaroo Ignimbrite|50162|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz-feldspar ignimbrite: crystal- and lithic-poor; fiamme foliation, rare fragmented crystals and a densely welded matrix of relict glass shards at base; rheomorphic flow banding and minor autobrecciation.||||||
35971|Barangaroo Ignimbrite|50163|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz-feldspar ignimbrite: crystal- and lithic-poor; fiamme foliation, rare fragmented crystals and a densely welded matrix of relict glass shards at base; rheomorphic flow banding and minor autobrecciation.||||||21-JUN-04
35971|Barangaroo Ignimbrite|66002|5|Briefly described|p6 Tb.4|Devonian|Devonian|Of Rocklands Volcanic Group. Defined by Simpson in Morand et al. 2003.||||||
1102|Baringhup Granodiorite|23300|5|Briefly described|Map Legend|Devonian|Devonian|Of Harcourt Suite||||||
1102|Baringhup Granodiorite|23301|5|Briefly described|Map Legend|Devonian|Devonian|Of Harcourt Suite||||||
1102|Baringhup Granodiorite|23302|5|Briefly described|Map Legend|Devonian|Devonian|Of Harcourt Suite||||||
1102|Baringhup Granodiorite|23303|5|Briefly described|Map Legend|Devonian|Devonian|Of Harcourt Suite||||||
1102|Baringhup Granodiorite|23304|5|Briefly described|Map Legend|Devonian|Devonian|Of Harcourt Suite||||||
1102|Baringhup Granodiorite|23305|4|Described|p44 Table 6, 7||Late Devonian|Of King (1977). Intruded Harcourt Granodiorite. Age: 368+/-2 Ma K-Ar. Of Harcourt Suite. Central Victorian Magmatic Province.||||||08-MAR-07
1102|Baringhup Granodiorite|23309|5|Briefly described|p423 Appendix 1|||G293. Age: 368 +/- 2Ma.||||||
1102|Baringhup Granodiorite|23603|5|Briefly described|p19|Late Devonian|Late Devonian|Geological Province: Harcourt Batholith.||||||
1102|Baringhup Granodiorite|23604|5|Briefly described|Map Legend|Late Devonian|Late Devonian|||||||
1102|Baringhup Granodiorite|23605|5|Briefly described|Map Legend|Late Devonian|Late Devonian|||||||
1102|Baringhup Granodiorite|23606|5|Briefly described|Map Legend|Late Devonian|Late Devonian|||||||
1102|Baringhup Granodiorite|23607|5|Briefly described|Map Legend|Late Devonian|Late Devonian|||||||
1102|Baringhup Granodiorite|24134|4|Described|p9|||||||||
1102|Baringhup Granodiorite|24177|4|Described|p62|Late Devonian|Late Devonian|Intrudes the Harcourt Granodiorite and Castlemaine Group. Age: 367 +/- 2 Ma (K/Ar; Webb 1989)||||||
1102|Baringhup Granodiorite|24328|5|Briefly described|Map legend|Devonian|Devonian|||||||
1102|Baringhup Granodiorite|24329|5|Briefly described|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
1102|Baringhup Granodiorite|24383|6|Mentioned|p23|||Geological Province: Lachlan Fold Belt.||||||08-MAR-07
1102|Baringhup Granodiorite|24384|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Harcourt Suite.  Age: <410Ma.  Biotite granodiorite, leucocratic fine to medium-grained.||||||25-JUN-13
1102|Baringhup Granodiorite|24385|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Harcourt Suite.||||||08-MAR-07
1102|Baringhup Granodiorite|24386|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Harcourt Suite.  Biotite granodiorite: leucocratic, fine- to medium-grained; slightly porphyritic.||||||08-MAR-07
1102|Baringhup Granodiorite|24387|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Harcourt Suite. Biotite granodiorite; leucocratic, fine- to medium-grained;  slightly porphyritic.||||||08-MAR-07
1102|Baringhup Granodiorite|24388|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Harcourt Suite.  Age: 368+/-2Ma (K/Ar).  Biotite granodiorite; oxidised I-type; moderately magnetic;  high K, moderate Th, moderate U, high total radioelements; low gravity response.||||||08-MAR-07
1102|Baringhup Granodiorite|24439|6|Mentioned|p56 App. 2|||Geological Province: Lachlan Fold Belt.||||||
1102|Baringhup Granodiorite|24440|5|Briefly described|Map legend|||||||||
1102|Baringhup Granodiorite|30936|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
1102|Baringhup Granodiorite|31654|6|Mentioned|Map legend|Recent|Recent|||||||
1102|Baringhup Granodiorite|34735|6|Mentioned|p22|||||||||
1102|Baringhup Granodiorite|43261|5|Briefly described|Map Legend||Late Devonian|||||||
1102|Baringhup Granodiorite|43493|4|Described|22,23||Late Devonian|Age: 367+/-2Ma. Fine - medium grained, grey slightly porphyritic granodiorite.||||||03-SEP-04
1102|Baringhup Granodiorite|65715|5|Briefly described|p8 Tb.4|||G293. Of Harcourt Batholith.||||||
1102|Baringhup Granodiorite|65969|6|Mentioned|p6 Fig.2, p30|||Magnetic. In BENDIGO 1:250 000 sheet. Called Baringhup granite in Fig.2. Associated with a cluster of earthquakes.||||||
1102|Baringhup Granodiorite|68116|5|Briefly described|Appendix, Maps 23, 24.|Late Devonian|Late Devonian||||||Biotite granodiorite; fine to medium grained, grey; slightly porphyritic; leucocratic, minor mafic enclaves: magnetic oxidised I-type.|
1102|Baringhup Granodiorite|69089|5|Briefly described|Map legend|Late Devonian|Late Devonian|I-type.||||||
1102|Baringhup Granodiorite|73497|5|Briefly described|Map legend|Late Devonian|Late Devonian|G293.||Harcourt Suite|||Granodiorite: I-type; moderately magnetic (up to 55 nT); low Th, variable U, high K in the south, low K in the north; gravity low of 175 micrometres/second/second.|
1107|Barjarg Granite|23309|5|Briefly described|p32, 347, 423|||(G216)  Supersedes Barjang Adamallite.||||||
1107|Barjarg Granite|24551|6|Mentioned|p167, p717 Table 2.4|Late Devonian|Late Devonian|Age 363 +/- 3Ma, Age: 367 +/- 3Ma..||||||
1107|Barjarg Granite|30906|6|Mentioned|Map legend|Devonian|Devonian|||||||
1107|Barjarg Granite|31713|4|Described|p11|||Mention P8||||||
1107|Barjarg Granite|32074|6|Mentioned|p181|||||||||
1107|Barjarg Granite|33305|5|Briefly described|p214|||Late Dev. Rb/Sr age. Refers McDougall et al. (1966)||||||
1107|Barjarg Granite|33602|6|Mentioned|p24|||||||||
1107|Barjarg Granite|35277|5|Briefly described|p96|||||||||
1107|Barjarg Granite|35278|6|Mentioned|p353|||||||||
1107|Barjarg Granite|35283|6|Mentioned|p48|||||||||
1107|Barjarg Granite|37501|6|Mentioned|p402|||||||||
1107|Barjarg Granite|39291|6|Mentioned|p217|||||||||
1107|Barjarg Granite|41641|4|Described|p166|||||||||
1107|Barjarg Granite|41850|6|Mentioned|p434|||||||||
1107|Barjarg Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
1107|Barjarg Granite|42827|5|Briefly described|p166|||||||||
1107|Barjarg Granite|48894|6|Mentioned|p96|||369+-11my||||||
1107|Barjarg Granite|68116|5|Briefly described|Appendix, Map 26.|Late Devonian|Late Devonian||||||Dark orange biotite-cordierite granite with minor muscovite; fine to coarse grained; even grained to porphyritic - the latter contains large garnet and plagioclase phenocrysts; accessory tourmaline and garnet; very weakly- to non-magnetic.|
1107|Barjarg Granite|70933|14|Not recorded|p90,91|||Geological map.||||||
32559|Barmouth Group|22968|4|Described|P19, Fig32, P116||Silurian|Faulted against the Pinnak Sandstone, New name, type section location given on P116||||||
32559|Barmouth Group|23020|5|Briefly described|Map legend|Pridoli|Pridoli|||||||
32559|Barmouth Group|23021|5|Briefly described|Map legend|Pridoli|Pridoli|Underlying unit is the Cowombat Siltstone||||||
32559|Barmouth Group|23028|5|Briefly described|Map legend|Pridoli|Pridoli|||||||
32559|Barmouth Group|23029|5|Briefly described|Map legend|Pridoli|Pridoli|||||||
32559|Barmouth Group|23030|5|Briefly described|Map legend|Late Silurian|Late Silurian|||||||
32559|Barmouth Group|23309|5|Briefly described|p90,96,97, 5 Fig. 1.3|Late Silurian|Late Silurian|||||||
32559|Barmouth Group|24004|5|Briefly described|p275 Fig.2|Silurian|Silurian|||||||
32559|Barmouth Group|24551|4|Described|p137, p113 Fig. 4.22|Silurian|Silurian|Includes two formations.||||||
32559|Barmouth Group|61161|6|Mentioned|p30, p35|||Marine sedimentary rocks.||||||
32559|Barmouth Group|61163|6|Mentioned|p9, p28|Silurian|Silurian|Geological Province: Lachlan Fold Belt (Tabberabbera Zone).||||||
32559|Barmouth Group|71040|6|Mentioned|p4 Fig.2, p9|||Deformation during Bindian (=Bowning) Orogeny described.||||||
26370|Barnawartha Gneissic Granodiorite|23309|5|Briefly described|p423 App1|||G182. S-Type. Supersedes Barnawatha Gneissic Granodiorite, Barnawartha Granite and Lady Franklin Granite.||||||
26370|Barnawartha Gneissic Granodiorite|30906|6|Mentioned|Map legend|Silurian|Silurian|||||||
26370|Barnawartha Gneissic Granodiorite|31800|5|Briefly described|p206|||||||||
26370|Barnawartha Gneissic Granodiorite|35278|6|Mentioned|p356|||||||||
26370|Barnawartha Gneissic Granodiorite|68116|5|Briefly described|Appendix, Map 19.|Pridoli|Llandovery||||||Granodiorite: foliated, medium grained, biotite-rich; interleaving boundary with gneiss country rock; pegmatite dykes common.|
26370|Barnawartha Gneissic Granodiorite|70910|4|Described|p46|||||||||
37628|Baroona Diorite|23309|6|Mentioned|p423 Appendix 1|||G323, V-type?||||||
37628|Baroona Diorite|60452|4|Described|p57|||||||||
37628|Baroona Diorite|60461|5|Briefly described|Map legend|Early Devonian|Early Devonian|Diorite, medium-grained; strongly magnetic.||||||
37628|Baroona Diorite|60462|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Diorite: high potassium, altered; magnetite giving some responses from secondary alteration; subsurface only.||||||
37628|Baroona Diorite|68189|6|Mentioned|p21, p39 App.1|||Possible association with molybdenum mineralisation.||||||
37629|Barrabilly Granite|23309|6|Mentioned|p423 Appendix 1|||Supersedes Barrabilly Adamellite. Shown as I-type.||||||04-NOV-14
37629|Barrabilly Granite|23615|5|Briefly described|p206 App.1|Early Silurian|Early Silurian|Also referred to as Barrabilly Adamellite throughout text.||||||
37629|Barrabilly Granite|68116|5|Briefly described|Appendix, Maps 28, 36.|Wenlock|Llandovery||||||Biotite-cordierite granite, fine to medium grained; dark grey; S-type.|
1156|Barracouta Formation|13323|5|Briefly described|p393 Fig. 2|Early Eocene|Maastrichtian|Of the Halibut Subgroup (Latrobe Group). Geological Province: Gippsland Basin.||||||
1156|Barracouta Formation|24090|5|Briefly described|p8 Fig.3|Eocene|Maastrichtian|Geological Province: Gippsland Basin.||||||
1156|Barracouta Formation|24407|5|Briefly described|p13 Fig.2|Early Eocene|Maastrichtian|Geological Province: Gippsland Basin||||||
1156|Barracouta Formation|24551|5|Briefly described|p262 Fig. 9.29, 477|Eocene|Late Cretaceous|Of the Halibut Subgroup.||||||
1156|Barracouta Formation|34842|6|Mentioned|p19|||||||||
1156|Barracouta Formation|35273|4|Described|p256|||||||||
1156|Barracouta Formation|41318|6|Mentioned|p189|||||||||
1156|Barracouta Formation|41868|6|Mentioned|p520|||||||||
1156|Barracouta Formation|42827|4|Described|p330|||Of Latrobe Valley Group.||||||20-JUL-06
1156|Barracouta Formation|61328|5|Briefly described|p112 Fig. 2|Late Cretaceous|Early Cretaceous|Of Latrobe Group. Age: ~80Ma to 52Ma. Geological Province: Gippsland Basin.||||||
1156|Barracouta Formation|61552|4|Described|p583 Fig.2, p584, p588, p592.  |Early Eocene|Maastrichtian|Deposited in alluvial-fluvial environments on the upper coastal plain. This unit is the lateral, landward equivalent of the Volador and Kingfish Formations.||Unit in Halibut Subgroup.|Includes Bonita Sandstone and Stonefish Sandstone Members.|Interfingers with the Volador and Kingfish Formations offshore.|Coarse-grained, partly conglomeratic, lithic arenites intercalated with occasional mudstone intervals; minor coal.|
1156|Barracouta Formation|64876|5|Briefly described|p145 Fig.2|Eocene|Maastrichtian|Gippsland Basin.||Halibut Subgroup.||||
1156|Barracouta Formation|65717|5|Briefly described|p9 figure 2.2, p11|Eocene|Maastrichtian|Revised and formalised by Hocking (1976). Deposited on an upper coastal plain.||Halibut Subgroup|Includes Stonefish Sandstone Member, Bonita Sandstone Member||Fluvial claystones, siltstones, sandstones and minor coals.|05-SEP-17
1156|Barracouta Formation|65718|5|Briefly described|p12, p16 Fig 3.5, p42 Fig 5.3 |Eocene|Campanian|Revised and formalised by Hocking (1976). Deposited on an upper coastal plain. Middle Eocene minimum age.|||||Characterised by fluvial siltstones, sandstones and minor coals.|
1156|Barracouta Formation|65973|5|Briefly described|p16, p22|||Gippsland Basin. Deposited in upper coastal plain settings and consists primarily of fluvial sediments.||Halibut Subgroup|||Sediments with minor coal.|
1156|Barracouta Formation|70028|6|Mentioned|p79|Eocene|Maastrichtian|||||||
1156|Barracouta Formation|70076|5|Briefly described|Regional: Fig.3; p3|Lutetian|Campanian|Coastal plain fluvial sediments.||Halibut Subgroup.|Yarram Member.|Overlies Chimaera Formation. Is overlain by Kingfish or Burong Formation. Encloses Campanian Volcanics.||
1156|Barracouta Formation|73471|5|Briefly described|p86|||Gippsland Basin.||Halibut Subgroup|||Alluvial and fluvial sandstones and siltstones.|
1156|Barracouta Formation|75065|5|Briefly described|p151|Eocene|Maastrichtian|Gippsland Basin; offshore. Alluvial/fluvial sediments.||Halibut Subgroup.||Unconformably overlies Chimaera Formation. Is overlain by Bream Volcanics.|Sandstone; minor siltstone, shale.|
35972|Barrakee Granite|23309|5|Briefly described|p342|||G340. I-Type.||||||
35972|Barrakee Granite|60452|4|Described|p51-52|||Mostly in the Charlton area. Cut by the Buckrabanyule Granite. Cuts the Narrewillock pluton.||||||14-MAY-13
35972|Barrakee Granite|60461|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Coonooer Suite.  Subsurface intrusion: hornblende granite, medium-grained.||||||
35972|Barrakee Granite|60462|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Coonooer Suite. Granite: I-type, oxidised, nonmagnetic; gravity response not distinguishable from edge effects of deeper gravity gradient; subsurface only.||||||
35972|Barrakee Granite|60491|4|Described|p47|||Of the Coonooer Suite. I-type. Probably intruded by the Buckrabanyule Granite and Nardoo Granite, and probably intrudes the Narrewillock pluton.||||||22-NOV-04
35972|Barrakee Granite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Coonooer Suite. Cordierite granite: S-type, reduced; pale grey, medium grained; also contains biotite||||||
35972|Barrakee Granite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of the Coonooer Suite. Granite; oxidised I-type; local gravity low; in areas of outcrop, both K and Th high, U moderate.||||||30-SEP-04
35972|Barrakee Granite|66002|5|Briefly described|p6 Tb.5|||Of Coonooer Suite. G340. Defined in Bibby and Moore 1998.||||||
35972|Barrakee Granite|68116|5|Briefly described|Appendix, Map 16.|Middle Devonian|Early Devonian||||||Cordierite-biotite granite: S-type, reduced; pale grey, medium grained.|
41191|Barrama Microgranite|50154|2|Defined|p88, p105, p246 App.5|||Intrudes the Glendara Granite. Max. thickness: 25m||||||25-SEP-09
41191|Barrama Microgranite|50155|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Biotite microgranite; I-type||||||
41191|Barrama Microgranite|50156|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite microgranite: massive, grey-buff, fine grained, equigranular; porphyritic with phenocrysts of microcline, quartz, biotite and plagioclase; accessory magnetite and muscovite.||||||
41191|Barrama Microgranite|50157|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite microgranite: massive, grey-buff, fine grained, equigranular; porphyritic with phenocrysts of microcline, quartz, biotite and plagioclase; accessory magnetite and muscovite.||||||
41191|Barrama Microgranite|50158|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite microgranite: massive, grey-buff, fine grained, equigranular; porphyritic with phenocrysts of microcline, quartz, biotite and plagioclase; accessory magnetite and muscovite.||||||
41191|Barrama Microgranite|50159|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite microgranite: massive, grey-buff, fine grained, equigranular; porphyritic with phenocrysts of microcline, quartz, biotite and plagioclase; accessory magnetite and muscovite.||||||24-JUN-04
41191|Barrama Microgranite|50160|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite microgranite||||||
41191|Barrama Microgranite|50161|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite microgranite: massive, grey-buff, fine grained, equigranular; porphyritic with phenocrysts of microcline, quartz, biotite and plagioclase; accessory magnetite and muscovite.||||||24-JUN-04
41191|Barrama Microgranite|50162|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite microgranite: massive, grey-buff, fine grained, equigranular; porphyritic with phenocrysts of microcline, quartz, biotite and plagioclase; accessory magnetite and muscovite.||||||24-JUN-04
41191|Barrama Microgranite|50163|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite microgranite: massive, grey-buff, fine grained, equigranular; porphyritic with phenocrysts of microcline, quartz, biotite and plagioclase; accessory magnetite and muscovite.||||||24-JUN-04
41191|Barrama Microgranite|66002|5|Briefly described|p9 Tb.5|||G436. Called Barrama Microadamellite by Kemp et al. (2002)||||||
41191|Barrama Microgranite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Late Cambrian||||||Biotite microgranite: massive, grey-buff, fine grained, porphyritic with phenocrysts of microcline, quartz, biotite and plagioclase; accessory muscovite and magnetite; magnetic.|
1187|Barringo Granodiorite|22885|5|Briefly described|map|||||||||
1187|Barringo Granodiorite|22886|4|Described|Table.1|||Of Mount Macedon Igneous Complex.||||||01-OCT-08
1187|Barringo Granodiorite|23309|5|Briefly described|p81,170,347||Late Devonian|G282. I-Type.  Supersedes Barringo Granite.||||||
1187|Barringo Granodiorite|24002|5|Briefly described|p240|Late Devonian|Late Devonian|||||||13-MAY-05
1187|Barringo Granodiorite|24551|5|Briefly described|p123, 719 Table 8.2|Late Devonian|Late Devonian|||||||
1187|Barringo Granodiorite|33153|6|Mentioned|p92|||||||||
1187|Barringo Granodiorite|33602|6|Mentioned|p14|||||||||
1187|Barringo Granodiorite|44197|5|Briefly described|Map Legend||Late Devonian|G282 I-type.||||||
1187|Barringo Granodiorite|64619|5|Briefly described|Map legend|Late Devonian|Late Devonian|Biotite granodiorite; mid- to dark grey, medium to fine-grained; I-type intrusion.||||||03-NOV-08
1187|Barringo Granodiorite|65715|5|Briefly described|p5-6, p7 Tb.4|Early Devonian|Early Devonian|Of Macedon Igneous Complex. Intrudes Kerrie Group and Willimigongong Ignimbrite. G282 of GSV database.||||||
1187|Barringo Granodiorite|65974|6|Mentioned|p28|||Probably related to a gravity low directly W of Mount William Fault, interpreted as an intrusion c.1.5km below the surface.||||||07-FEB-18
1187|Barringo Granodiorite|68116|5|Briefly described|Appendix, Map 32.|Late Devonian|Late Devonian||||||Biotite granodiorite and granite: mid- to dark grey; medium to fine-grained.|
1187|Barringo Granodiorite|70999|4|Described|p167|||||||||
1188|Barringo Suite|24551|6|Mentioned|p221|||||||||
1188|Barringo Suite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
1188|Barringo Suite|42827|6|Mentioned|p435|||||||||
1220|Barry Mountains Granite|23309|6|Mentioned|p423 App1|||G159. I-Type.||||||
1220|Barry Mountains Granite|42726|5|Briefly described|map legend|||Wagga Batholith. NOT variation on Barry Granite, Wyangala Batholith, NSW.||||||
1220|Barry Mountains Granite|44187|5|Briefly described|Map Legend||Early Devonian|G159 Unassigned. Shown as Barry Mountains.||||||
1220|Barry Mountains Granite|68116|5|Briefly described|Appendix, Map 34.|Early Devonian|Early Devonian||||||Granitic rock; highly magnetic.|
1227|Barwo Member|35091|6|Mentioned|Table 1|||||||||
1227|Barwo Member|42966|5|Briefly described|p406, p210|||Of Shepparton Formation. See also Barwo Sand Member.||||||10-NOV-08
77303|Barwon River Conglomerate|65715|4|Described|p9 Tb.6, p10,32-37|Albian|Albian|Of Otway Group. Formation rank. Referred to as Barwon River Member of Eumeralla Formation by Constantine and Liberman (2001). Included in Barrabool (or Barrarbool) Sandstone by Spencer-Jones (1963). Conglomerate and minor sandstone with clasts of hornfels, rotten gabbro and rotten granite, with a matrix of mostly granitic sand. Underlies and interfingers with Eumeralla Formation. Contains lower C. paradoxa spore-pollen, Mid-Albian age.||||||
77303|Barwon River Conglomerate|68116|5|Briefly described|Appendix, Map 50.|Albian|Albian||||||Conglomerate, minor sandstone, pebbly sandstone, mudstone: conglomerate is poorly sorted with clasts of hornfels, gabbro and granite in a matrix of granitic sand.|
21202|Bass Camp Ignimbrite|23309|5|Briefly described|p123, 124.|||of White Monkey Volcanics.||||||
21202|Bass Camp Ignimbrite|23615|4|Described|p97|Early Devonian|Early Devonian|Of White Monkey Subgroup.  Previously included in the Black Mountain Rhyodacite (of Ringwood, 1955a). Overlain by Douglas Ignimbrite. Overlies Minchin Ignimbrite and Bowen Track Ignimbrite.||||||
21202|Bass Camp Ignimbrite|24551|5|Briefly described|p149, p132 Fig.5.23|||Of White Monkey Volcanics||||||
21202|Bass Camp Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Early Devonian|Early Devonian||||||Quartz-pink feldspar ignimbrite: red with large pumice fragments; occasional cavities.|
41024|Bass Megasequence|14235|4|Described|p48|||||||||
41024|Bass Megasequence|61553|5|Briefly described|p608.|Late Early Eocene|Middle Campanian|This name appears to be used interchangeably with Bass Sequence in this article. Roughly correlative to the Middle Eastern View Coal Measures|||Includes Furneaux, Tilana and Narimba Sequences.|||
41024|Bass Megasequence|69297|5|Briefly described|p143, p148|Early Eocene|Middle Campanian|Durroon Sub-basin, Bass Basin. Deposited in fluvio-deltaic or overbank and delta plain environments. ||||Unconformably overlain by the Flinders Sequence. |Sandstones interbedded with shales and thin coal beds. |
41024|Bass Megasequence|69879|4|Described|p413, p431-433|Eocene|Campanian|Bass Basin, Cape Wickham Sub-basin - 3rd rift phase (Bass Rift Phase). Related closely to the evolution of the Australo-Antarctic Gulf. Fossil controls. Divided into 3 unconformity-bounded sequences with progradational geometry over most of Bass Basin.|||Includes Furneaux, Tilana, Narimba Sequences.|Overlies Durroon Megasequence unconformably. Underlies Aroo Sequence unconformably.|Non-marine sediments. Fluvio-deltaic to lacustrine equivalents of Lower Eastern View Coal Measures, consisting of basal volcanics (basalt) overlain by sandstone fining upwards into siltstone and shale.|
27329|Batesford Limestone|22626|6|Mentioned|446 fig 10|Middle Miocene|Early Miocene|Geol .province: East Otway Basin. Overlain by Fyansford Formation, underlain by Zeally Limestone.||||||13-FEB-07
27329|Batesford Limestone|23230|4|Described|Table4-1p40, 42||Oligocene|Present in the Port Phillip Basin.||||||
27329|Batesford Limestone|23239|4|Described|Table1p109, 116-8|Miocene|Miocene|||||||
27329|Batesford Limestone|23768|5|Briefly described|p28 Fig. 5|Middle Miocene|Early Miocene|In the Torquay/Geelong area.  See also p71.||||||
27329|Batesford Limestone|23909|5|Briefly described|p290 Fig.3|Middle Miocene|Oligocene|||||||
27329|Batesford Limestone|24038|6|Mentioned|p443|||||||||
27329|Batesford Limestone|24551|6|Mentioned|p316, 463|||||||||
27329|Batesford Limestone|30122|6|Mentioned|p37|||||||||
27329|Batesford Limestone|30818|5|Briefly described|p191|||Lower Miocene age.||||||
27329|Batesford Limestone|30929|6|Mentioned|Map legend|Miocene|Miocene|Unit of Torquay Group.||||||13-FEB-07
27329|Batesford Limestone|31242|6|Mentioned|p12|||Refers hydrogeology||||||
27329|Batesford Limestone|32815|6|Mentioned|p200|||||||||
27329|Batesford Limestone|33155|6|Mentioned|p119|||||||||
27329|Batesford Limestone|33228|4|Described|p3|||||||||
27329|Batesford Limestone|33231|6|Mentioned|p53|||||||||
27329|Batesford Limestone|33240|4|Described|p3|||||||||
27329|Batesford Limestone|33604|6|Mentioned|p21|||Strat. diagram.||||||
27329|Batesford Limestone|34421|6|Mentioned|p262|||||||||
27329|Batesford Limestone|34902|6|Mentioned|p78|||||||||
27329|Batesford Limestone|34954|6|Mentioned|Fig.33|||Analysis. See also Fig.35.||||||
27329|Batesford Limestone|35274|6|Mentioned|p421|||||||||
27329|Batesford Limestone|35276|4|Described|p239|||||||||
27329|Batesford Limestone|35290|4|Described|p39|||Mention p33.||||||13-FEB-07
27329|Batesford Limestone|35712|4|Described|p18|||See also p33 re aquifers.||||||13-FEB-07
27329|Batesford Limestone|36747|6|Mentioned|p104|||||||||
27329|Batesford Limestone|37385|6|Mentioned|p11|||||||||
27329|Batesford Limestone|38070|6|Mentioned|Fig.12|||In the Bass Basin.||||||13-FEB-07
27329|Batesford Limestone|41274|6|Mentioned|p9|||||||||
27329|Batesford Limestone|41537|6|Mentioned|p352|||||||||
27329|Batesford Limestone|41868|5|Briefly described|p576|||||||||
27329|Batesford Limestone|42016|6|Mentioned|p63|||||||||
27329|Batesford Limestone|42635|5|Briefly described|Table 17, P88|||||||||
27329|Batesford Limestone|42824|4|Described|p261|||||||||
27329|Batesford Limestone|42827|3|Fully described|p313|||Of the Torquay Group.||||||13-FEB-07
27329|Batesford Limestone|43604|6|Mentioned|p153||Middle Miocene|In Port Philip Basin.||||||
27329|Batesford Limestone|43667|6|Mentioned|Fig.3,p12||Middle Eocene|||||||
27329|Batesford Limestone|46983|6|Mentioned|Fig.4|||||||||
27329|Batesford Limestone|48911|6|Mentioned|Chart 1|||||||||
27329|Batesford Limestone|60785|5|Briefly described|p184 Fig.1, p191.  |Langhian|Burdigalian|Of the Torquay/Port Phillip Basins. Lower 21m is Longfordian (lower Miocene), the upper 12m is the Lepidocyclina-bearing type section of the uppermost Lower to lower Middle Miocene Batesfordian local marine stage. Has yielded fossil cetacean elements.||||Grades conformably into the overlying Fyansford Formation.|Basal beds are calcareous sands and gravel. Upper part consists of biocalcarenite|
27329|Batesford Limestone|61181|5|Briefly described|p119, p133|Miocene|Miocene|Used in cement manufacture. Consists of accumulated skeletal fragments of polyzoa, echinoids, foraminifera, etc. White and friable when fresh, but yellowish and hard when weathered. Underlies Fyansford Clay.||||||
27329|Batesford Limestone|61186|5|Briefly described|p7, p95|Miocene|Oligocene|Dimension stone - orig.called Moorabool Stone. Two lithologies: soft calcarenite of sand-sized fragments of marine fossils; and harder limestone (Moorabool Stone) of closely packed foraminifer tests; hardness due to carbonate cementation.||||||17-DEC-07
27329|Batesford Limestone|64769|6|Mentioned|p27|||VIC.||||||06-MAY-09
27329|Batesford Limestone|65715|4|Described|p14 Tb.8, p16, p60-62|Miocene|Oligocene|Name traces back to Hall & Prichard (1896). Senior synonym of Waurn Ponds Limestone used by Spencer-Jones (1970), and Upper and Lower Maude Limestone of Bowler (1963). Appears to under- and overlie Maude Basalt. Type locality is Batesford limestone quarry.||||||
27329|Batesford Limestone|67061|6|Mentioned|p554 Fig.10.|Miocene||Port Phillip Basin.||||Is overlain by Fyansford Formation.||
27329|Batesford Limestone|68116|5|Briefly described|Appendix, Map 50.|Miocene|Aquitanian||||||Limestone (calcarenite), minor sandstone and conglomerate: limestone pale brown to white; bryozoal; well sorted; well bedded; calcareous sandstone and gravel at base.|
27329|Batesford Limestone|70942|6|Mentioned|p122|||A little younger than the Yellow Bluff Beds.||||||
27329|Batesford Limestone|70998|14|Not recorded|p159||Middle Miocene|||||||
27329|Batesford Limestone|71419|6|Mentioned|p8 Fig 2|Miocene|Miocene|Marine deposits.||||||
27329|Batesford Limestone|71437|6|Mentioned|p161|||Deposited close to shoreline in fairly shallow seas protected by local geography from deposition of silt and clay.||||||
78701|Bats Ridge Member|73386|6|Mentioned|p14|||||Bridgewater Formation||||
37630|Batty Spur Granite|23309|6|Mentioned|p423 Appendix 1|||Supersedes Big River Granite.||||||
37630|Batty Spur Granite|24551|6|Mentioned|p234|||See also Big River Granite||||||
26374|Baw Baw Granodiorite|23265|4|Described|Fig13-4.1p338, 339, 342||Late Devonian|Max Age: 369 (+/-) 13 Ma.||||||
26374|Baw Baw Granodiorite|23269|6|Mentioned|Fig14-3.1p403|||||||||
26374|Baw Baw Granodiorite|23309|5|Briefly described|p142,143,347,350.||Late Devonian|G236. I-Type. Supersedes Baw Baw Granite.||||||29-MAR-05
26374|Baw Baw Granodiorite|32001|6|Mentioned|p78|||||||||
26374|Baw Baw Granodiorite|33607|6|Mentioned|Map legend|Devonian|Devonian|Granodiorite, medium, even-grained, hornblende-bearing.||||||29-NOV-04
26374|Baw Baw Granodiorite|35073|5|Briefly described|Table 4.|||||||||
26374|Baw Baw Granodiorite|41641|6|Mentioned|Fig.5.1|||||||||
26374|Baw Baw Granodiorite|42383|5|Briefly described|Fig. 1 P3|||||||||
26374|Baw Baw Granodiorite|44187|5|Briefly described|Map Legend||Late Devonian|G236 I-type.||||||
26374|Baw Baw Granodiorite|64535|5|Briefly described|Map legend|Late Devonian|Late Devonian|Biotite-hornblende granodiorite; bluish-grey, medium-grained, equigranular, small microgranitoid enclaves common; I-type intrusion.||||||
26374|Baw Baw Granodiorite|64539|5|Briefly described|Map legend|Late Devonian|Late Devonian|Biotite-hornblende granodiorite; bluish-grey, medium-grained, equigranular, small microgranitoid enclaves common; I-type intrusion.||||||
26374|Baw Baw Granodiorite|64540|5|Briefly described|Map legend|Late Devonian|Late Devonian|Biotite-hornblende granodiorite; bluish-grey, medium-grained, equigranular, small microgranitoid enclaves common; I-type intrusion.||||||
26374|Baw Baw Granodiorite|64605|5|Briefly described|Map legend|Late Devonian|Late Devonian|Biotite-hornblende granodiorite; I-type intrusive rock. bright to dark red and red-green in RGB. Nonmagnetic, intruded by magnetic dykes.||||||
26374|Baw Baw Granodiorite|64616|4|Described|p129, p146, p159, p162 Fig.6.8, p199|Late Devonian|Late Devonian|See also p200 Fig.7.1, p202-203, p208 Fig.8.1, p210 Fig.8.2, p292-294, p301, p434-435. Of Tynong Suite, Tynong Supersuite of White and Chappell (1988). Easternmost pluton in Tynong batholith. Intrudes Jordan River Group and Walhalla Group rocks. FT dating at 194 +/- 14 Ma. Grey, medium-grained, equigranular, biotite granodiorite with minor hornblende. Hornfels contact aureole up to 2km wide. Age: post-Middle Devonian. Geophysical characteristics given. Appears as Mt Baw Baw Granite [!] on p316.||||||
26374|Baw Baw Granodiorite|65900|5|Briefly described|p161||Late Devonian|Intrudes Melbourne Zone folded rocks.||||||
26374|Baw Baw Granodiorite|66181|6|Mentioned|p293|Late Devonian|Late Devonian|||||||
26374|Baw Baw Granodiorite|66576|6|Mentioned|p970.|||||||||
26374|Baw Baw Granodiorite|68116|5|Briefly described|Appendix, Map 43.|Late Devonian|Late Devonian||||||Biotite-hornblende granodiorite: bluish grey; medium-grained; equigranular; small microgranitoid enclaves common.|
32561|Bayliss Spur Tonalite|22968|5|Briefly described|P186, P190||Early Devonian|New name, parent is Swifts Creek Igneous Complex||||||
32561|Bayliss Spur Tonalite|23020|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Swifts Creek Igneous Complex||||||
32561|Bayliss Spur Tonalite|23030|5|Briefly described|Map legend|Early Devonian|Late Silurian|Parent is the Swifts Creek Igneous Complex||||||
32561|Bayliss Spur Tonalite|23309|6|Mentioned|p423 App1|||G546. I-Type||||||
32561|Bayliss Spur Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Tonalite: green to grey; medium to coarse-grained; minor pegmatitic leucogranite and hornblendite.|
1286|Baynton Granodiorite|22885|5|Briefly described|map|||||||||
1286|Baynton Granodiorite|23309|6|Mentioned|p423 App1|||Superseded by Baynton Granite.||||||
1286|Baynton Granodiorite|24383|5|Briefly described|p9 Fig.1|||Parent: Cobaw Suite. Geological Province: Lachlan Fold Belt||||||
1286|Baynton Granodiorite|24384|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Cobaw Suite.  Biotite granodiorite; medium-grained, equigranular, nonmagnetic, reduced I-type.||||||
1286|Baynton Granodiorite|24385|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Cobaw Suite.   Biotite granodiorite: medium-grained, equigranular, nonmagnetic; reduced I-type.||||||
1286|Baynton Granodiorite|24386|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Cobaw Suite. Biotite granodiorite: medium-grained; equigranular; nonmagnetic; reduced I-type.||||||
1286|Baynton Granodiorite|24387|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Cobaw Suite.  Biotite granodiorite; medium-grained; equigranular; nonmagnetic; reduced I-type||||||
1286|Baynton Granodiorite|24388|5|Briefly described|Map legend|Late Devonian|Late Devonian|Age: 359+/-7Ma (K/Ar).   Biotite granodiorite; reduced I-type; nonmagnetic; high K, low Th, moderate U and total radioelements; low gravity response.||||||03-FEB-09
1286|Baynton Granodiorite|41850|6|Mentioned|p435|||||||||
1286|Baynton Granodiorite|42827|6|Mentioned|p435|||||||||
1286|Baynton Granodiorite|44197|5|Briefly described|Map Legend||Late Devonian|G284 I-Type.||||||
1286|Baynton Granodiorite|64611|5|Briefly described|Map legend|Late Devonian|Late Devonian|Part of the Cobaw Batholith. Quartz-feldspar-biotite granodiorite: med-gr., equigran. with numerous sed+igneous xenoliths; a smaller porphyritic phase is present in southern half of batholith - lithological details included. I-type intrusion.||||||25-JUN-13
1286|Baynton Granodiorite|64612|2|Defined|p18 Fig. 3.7, p20 Fig. 4.3, p42, p44-45|Carboniferous|Devonian|Chappell et al. (1991). Of Harcourt Suite. Age: 347+/-7 and 358+/-7Ma (K-Ar). Intrudes Pyalong Granite. Has a gradational relationship to the Beauvallet Granodiorite. I-type. Medium-grained, equigranular granodiorite with qtz, K-feld, biot + hornblende.||||||07-FEB-11
1286|Baynton Granodiorite|65715|5|Briefly described|p7 Tb.4, p25 Fig.1a|||G284. Called Granodiorite G3 of Cobaw Granite by Stewart (1966) and Baynton Adamellite by White and Chappell (1988). Fig. 1a includes a porphyritic phase.||||||02-FEB-15
1286|Baynton Granodiorite|68116|5|Briefly described|Appendix, Map 32.|Late Devonian|Late Devonian|Contains a porphyritic phase comprising quartz-feldspar-biotite granodiorite with minor hornblende and euhedral phenocrysts of plagioclase and K-feldspar up to 20 mm long; locally with large crystals of biotite; numerous sedimentary and igneous enclaves.|||||Quartz-feldspar-biotite granodiorite: medium-grained, equigranular granodiorite with xenoliths of both sedimentary and igneous origin; nonmagnetic I-type. |
36977|Bealiba Granodiorite|23309|6|Mentioned|Appendix 1|||Superseded by Cochranes Creek Granodiorite?||||||26-AUG-05
36977|Bealiba Granodiorite|23603|5|Briefly described|p21|Early Devonian|Early Devonian|||||||
36977|Bealiba Granodiorite|23604|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
36977|Bealiba Granodiorite|23605|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
36977|Bealiba Granodiorite|23606|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
36977|Bealiba Granodiorite|23607|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
36977|Bealiba Granodiorite|66002|6|Mentioned|p7 Tb.5|||G353. Defined in Marlow and Bushell 1995, p21||||||
36977|Bealiba Granodiorite|68116|5|Briefly described|Appendix, Map 23.|Early Devonian|Early Devonian||||||Biotite granodiorite: coarse grained, marginal strongly porphyritic phase contains K-feldspar up to 2 cm; local porphyritic microgranodiorite; includes pegmatite and aplite; local hydrothermal alteration: I-type.|
35516|Bear Gully Chert Bed|23309|5|Briefly described|p43 Tb2.17||Lancefieldian|||||||
35516|Bear Gully Chert Bed|24002|6|Mentioned|p231, 232|Cambrian||||||||18-SEP-13
35516|Bear Gully Chert Bed|24098|6|Mentioned|p30|||See also Bear Gully Chert.||||||19-APR-05
35516|Bear Gully Chert Bed|24551|5|Briefly described|p100|Cambrian|Cambrian|See also Bear Gully Chert.||||||
35516|Bear Gully Chert Bed|75070|5|Briefly described|p175, 178, 184|Ordovician|Ordovician|Waratah Bay, southern Victoria. Detrital zircon, REE graphs. The Macquarie Arc is a possible distal source of detrital zircons in this unit. See also references to Bear Gully Chert (p178-180, 182, 184-185).||Basal Digger Island Marlstone.||Is overlain by Diggers Island Marl / Digger Island Marlstone.|Chert, sandstone.|
21209|Beaufort Formation|22531|6|Mentioned|p6|Cambrian|Cambrian|of Saint Arnaud Group||||||
21209|Beaufort Formation|22628|6|Mentioned|p113||Early Paleozoic|||||||07-NOV-08
21209|Beaufort Formation|22756|3|Fully described|P20, P25|Cambrian|Ordovician|||||||
21209|Beaufort Formation|23164|4|Described|p13|Cambrian|Cambrian|||||||
21209|Beaufort Formation|23165|5|Briefly described|Map legend|Ordovician|Cambrian|||||||
21209|Beaufort Formation|23166|5|Briefly described|Map legend|Ordovician|Cambrian|of Saint Arnaud Group.||||||
21209|Beaufort Formation|23167|5|Briefly described|Map legend|Ordovician|Cambrian|of Saint Arnaud Group.||||||
21209|Beaufort Formation|23168|5|Briefly described|Map legend|Ordovician|Cambrian|of Saint Arnaud Group.||||||
21209|Beaufort Formation|23169|5|Briefly described|Map legend||Devonian|of Mount Cole Suite.||||||
21209|Beaufort Formation|23300|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Saint Arnaud Group||||||
21209|Beaufort Formation|23302|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Saint Arnaud Group||||||
21209|Beaufort Formation|23303|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Saint Arnaud Group||||||
21209|Beaufort Formation|23304|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Saint Arnaud Group||||||
21209|Beaufort Formation|23305|3|Fully described|p37|Late Cambrian|Middle Cambrian|of Cayley and McDonald (1995). Of St Arnaud Group. Overlying unit Pyrenees Formation (conformably). Underlying unit Pitfield Volcanics? Lachlan Fold Belt.||||||
21209|Beaufort Formation|23307|5|Briefly described|Map Legend|Cambrian|Cambrian|Of Saint Arnaud Group||||||
21209|Beaufort Formation|23309|5|Briefly described|p41, 42 Tb2.12|||of St Arnaud Group.||||||
21209|Beaufort Formation|24551|5|Briefly described|p83|Cambrian|Cambrian|Of Saint Arnaud Group. Overlain by Pyrenees Formation.||||||
21209|Beaufort Formation|43260|5|Briefly described|Map Legend|Ordovician|Cambrian|of Saint Arnaud Group.||||||
21209|Beaufort Formation|43846|5|Briefly described|10|Ordovician|Cambrian|||||||
21209|Beaufort Formation|60452|5|Briefly described|p22|Late Cambrian|Late Cambrian|In BEAUFORT these rocks are interpreted to be the basal and most distal unit of the Saint Arnaud Group. Conformably overlain by the Pyrenees Formation.||||||27-OCT-04
21209|Beaufort Formation|60461|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Saint Arnaud Group.  Deep marine turbidites: interbedded siltstone and mudstone, minor sandstone; mostly contact metamorphosed to cordierite hornfels.  Age: ~520Ma.||||||06-OCT-04
21209|Beaufort Formation|60491|4|Described|p14, p17|Early Ordovician|Cambrian|Of the Saint Arnaud Group. Intruded by the Early Devonian granitoids. Unconformably overlain by Murray Basin sediments. Thickness at least 1-1.5km.||||||
21209|Beaufort Formation|60492|5|Briefly described|Map Legend|Ordovician|Cambrian|Of the Saint Arnaud Group. Overlain by Parilla Sand. Marine: turbiditic mudstone and fine grained sandstone; pyritic.||||||29-SEP-04
21209|Beaufort Formation|60493|5|Briefly described|Map Legend|Ordovician|Cambrian|Of the Saint Arnaud Group. Marine turbiditic interbedded siltstone & mudstone with minor sandstone; slightly higher regional magnetic response than other sediments; gravity response mostly moderate to high; high K, moderate to high Th, U.||||||
21209|Beaufort Formation|60581|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Saint Arnaud Group. Sandstone, mudstone, black shale; sand-poor turbidite facies tectonically modified to phyllite, quartz-mica or graphitic schist; weathered to partly kaolinised.||||||23-NOV-04
21209|Beaufort Formation|60582|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Saint Arnaud Group. Sandstone, mudstone, black shale; sand-poor turbidite facies tectonically modified to phyllite, quartz-mica or graphitic schist; weathered to partly kaolinised.||||||
21209|Beaufort Formation|60583|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Saint Arnaud Group. Sandstone, mudstone, black shale; sand-poor turbidite facies tectonically modified to phyllite, quartz-mica or graphitic schist; weathered to partly kaolinised.||||||
21209|Beaufort Formation|60584|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Saint Arnaud Group. Sandstone, mudstone, black shale; sand-poor turbidite facies tectonically modified to phyllite, quartz-mica or graphitic schist; weathered to partly kaolinised.||||||
21209|Beaufort Formation|60585|4|Described|p20|Late Cambrian|Middle Cambrian|Of the Saint Arnaud Group. Overlies the Pitfield Volcanics. Conformably overlain by the Pyrenees Formation.||||||
21209|Beaufort Formation|61750|5|Briefly described|p19, p21|||Of Saint Arnaud Group west of Avoca Fault (Cayley and McDonald 1995). Contains varied rock types - including turbiditic sst, sltst and carbonaceous mudstone; also has highest gold deposits of formations within the Group - the source host for alluvial gold||||||24-JAN-07
21209|Beaufort Formation|62099|5|Briefly described|p331|||Of the Saint Arnaud Group. Siltstone-dominated. Thickness: >1.5km. In the Stawell Zone of the Lachlan Orogen.||||||
21209|Beaufort Formation|62754|5|Briefly described|p863|||Of the Saint Arnaud Group. Geological Province: Stawell Zone.||||||23-JAN-07
21209|Beaufort Formation|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Saint Arnaud Group.  Defined by Cayley and McDonald 1995.||||||
21209|Beaufort Formation|68116|5|Briefly described|Appendix, Maps 16, 23, 31, 40.|Late Cambrian|Middle Cambrian||||||Sandstone, mudstone and black shale: sand-poor turbidite facies tectonically modified to phyllite, quartz-mica or graphitic schist; weathered to partly kaolinised; deep marine deposits.|
21209|Beaufort Formation|68189|6|Mentioned|p17 Tb.3.1|||||||||
21209|Beaufort Formation|68194|6|Mentioned|p20|Cambrian|Cambrian|||Unit in Saint Arnaud Group.||||
21209|Beaufort Formation|70268|6|Mentioned|p259|||Linton area, eastern Pyrenees province.||||||
21209|Beaufort Formation|73118|6|Mentioned|p13-14|||Stawell Zone, Lachlan Fold Belt, Western Victoria.|||||Pyrrhotitic black slate-dominated.|
21209|Beaufort Formation|73496|5|Briefly described|Map legend|Cambrian|Cambrian|||Saint Arnaud Group|||Parts either have magnetic responses typically of 10 to 30 nT, or are weakly magnetised with magnetic responses typically 1 to 5 nT. Includes strongly deformed sediments in hangingwall of the Avoca Fault.|
21209|Beaufort Formation|73497|6|Mentioned|Map legend|Cambrian|Cambrian|||Saint Arnaud Group||||
1342|Beaumaris beds|32687|5|Briefly described|p6|||||||||
32493|Beauvallet Granodiorite|22885|5|Briefly described|map|||||||||
32493|Beauvallet Granodiorite|22886|4|Described|Table.1|||Age: K/Ar*2 359+/-7 Ma, 363+/-7Ma. of Cobaw Batholith.||||||
32493|Beauvallet Granodiorite|23309|5|Briefly described|p424 App1|Early Carboniferous|Late Devonian|(G285). I-Type. Age: 359 +/- 7Ma, 363 +/- 7Ma. Supersedes Cobaw Granodiorite.||||||
32493|Beauvallet Granodiorite|24551|6|Mentioned|p221, 718 Table 8.1|||||||||
32493|Beauvallet Granodiorite|44197|5|Briefly described|Map Legend||Late Devonian|G285 I-Type.||||||
32493|Beauvallet Granodiorite|64611|5|Briefly described|Map legend|Late Devonian|Late Devonian|Part of the Cobaw Batholith. Biotite-hornblende granodiorite: medium- to coarse-grained, equigranular to porphyritic with quartz and feldspar phenocrysts; rare xenoliths of granite and diorite. I-type intrusion.||||||25-JUN-13
32493|Beauvallet Granodiorite|64612|2|Defined|p19, p42, p45-46, p69|Carboniferous|Devonian|Chappell et al. (1991). Of Harcourt Suite. Intrudes Pyalong Granite, Baynton Granodiorite and Castlemaine Group. Biotite-hornblende granodiorite, medium to coarse-grained, varying from equigranular to porphyritic, with qtz and feld phenocrysts.||||||25-JUN-13
32493|Beauvallet Granodiorite|64619|5|Briefly described|Map legend|Late Devonian|Late Devonian|Biotite-hornblende granodiorite; mid-grey, medium-grained equigranular to porphyritic with K-feldspar phenocrysts; I-type intrusion.||||||03-NOV-08
32493|Beauvallet Granodiorite|65715|5|Briefly described|p7 Tb.4|||G285. Called Granodiorite G4 of Cobaw Granite by Stewart (1966).||||||
32493|Beauvallet Granodiorite|68116|5|Briefly described|Appendix, Map 32.|Late Devonian|Late Devonian||||||Biotite-hornblende granodiorite: mid-grey; medium-grained equigranular to porphyritic with K-feldspar phenocrysts.|
1351|Beckworth Suite|22756|5|Briefly described|P40, P50|||||||||
1351|Beckworth Suite|23300|5|Briefly described|Map Legend|Devonian|Devonian|||||||
1351|Beckworth Suite|23301|5|Briefly described|Map Legend|Devonian|Devonian|||||||
1351|Beckworth Suite|23302|5|Briefly described|Map Legend|Devonian|Devonian|||||||
1351|Beckworth Suite|23303|5|Briefly described|Map Legend|Devonian|Devonian|||||||
1351|Beckworth Suite|23304|5|Briefly described|Map Legend|Devonian|Devonian|||||||
1351|Beckworth Suite|23305|4|Described|p45||Late Devonian|Geological Province: Central Victorian Magmatic Province.||||||
1351|Beckworth Suite|23309|6|Mentioned|p347|||||||||
1351|Beckworth Suite|24383|6|Mentioned|p49|||||||||
1351|Beckworth Suite|24551|6|Mentioned|p218|||||||||
1351|Beckworth Suite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
1351|Beckworth Suite|42827|5|Briefly described|p435|||||||||
1351|Beckworth Suite|43260|6|Mentioned|Map Legend||Middle Devonian|||||||
1351|Beckworth Suite|60581|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Includes: Chepstowe Granodiorite, Mount Bute Adamellite, Wallinduc Granodiorite.||||||
1351|Beckworth Suite|60582|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Includes: Chepstowe Granodiorite, Mount Bute Adamellite, Wallinduc Granodiorite.||||||
1351|Beckworth Suite|60583|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Includes: Chepstowe Granodiorite, Mount Bute Adamellite, Wallinduc Granodiorite.||||||
1351|Beckworth Suite|60584|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Includes: Chepstowe Granodiorite, Mount Bute Adamellite, Wallinduc Granodiorite.||||||
1351|Beckworth Suite|60585|6|Mentioned|p23|Late Devonian|Late Devonian|||||||
1351|Beckworth Suite|61750|5|Briefly described|p22|Devonian|Devonian|I-type granites. Age: 370 Ma.||||||
1351|Beckworth Suite|66002|5|Briefly described|p6 Tb.5|||Includes Illoura Granodiorite, Chepstowe Granodiorite, Tiac Granite, Mount Bute Granite and Ercildoun Granite. Defined in White and Chappell 1988.||||||
1351|Beckworth Suite|66012|3|Fully described|p12-16|Devonian|Devonian|Includes Mount Emu Granodiorite, Mount Bute Granite, and Lismore Granodiorite. Metaluminous, fractionated I-type granites. Forms subcircular, discordant, zoned plutons with associated  contact metamorphic aureoles in the host Saint Arnaud Group| | | | | |16-FEB-15
26377|Bee Tree Granodiorite|22876|5|Briefly described|p27|||||||||
26377|Bee Tree Granodiorite|22877|5|Briefly described|map|Silurian|Silurian|G33. Biotite-muscovite granodiorite. S-Type.||||||26-OCT-04
26377|Bee Tree Granodiorite|23309|6|Mentioned|p424 App1|||S-Type (G33).||||||
26377|Bee Tree Granodiorite|42627|5|Briefly described|Map legend|Wenlock|Wenlock|||||||
26377|Bee Tree Granodiorite|42647|4|Described|p43|||||||||
26377|Bee Tree Granodiorite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|Of Ocean View Suite. S-type. Foliated, medium grained biotite, muscovite granodiorite.||||||22-OCT-04
26377|Bee Tree Granodiorite|43315|5|Briefly described|Map Legend||Wenlock|Of the Ocean View Suite. S-type. Foliated, medium-grained biotite, muscovite granodiorite.||||||03-MAY-05
26377|Bee Tree Granodiorite|60541|4|Described|p79|Silurian|Silurian|Intrusive within the Kuark Metamorphic Complex, but most is on the BENDOC map sheet. Rock is dark grey (mafic), medium- to fine-grained, moderately foliated muscovite-biotite granodiorite. Age is Middle Silurian.  See also p18 Tb. 1.||||||16-JUN-05
26377|Bee Tree Granodiorite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Biotite-muscovite granodiorite: medium-grained; foliated; S-type intrusive.|
1381|Beechworth Granite|22971|5|Briefly described|p 33|||||||||
1381|Beechworth Granite|23308|6|Mentioned|Map Legend|||Mine name?||||||
1381|Beechworth Granite|23309|5|Briefly described|p331,349|||G195. Supersedes Beechworth Adamellite. Age: K/Ar Biotite 377+/-12 / 369+/-15Ma.||||||29-MAR-05
1381|Beechworth Granite|24551|6|Mentioned|p218, 467|||Of the Beechworth Group.||||||
1381|Beechworth Granite|37029|6|Mentioned|p62|||||||||
1381|Beechworth Granite|41868|6|Mentioned|p567|||||||||
1381|Beechworth Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
1381|Beechworth Granite|42827|6|Mentioned|p567|||||||||
1381|Beechworth Granite|61186|5|Briefly described|p41, p50|||Dimension stone used in the buildings of Beechworth Gaol. May not be a formal name? ||||||
1381|Beechworth Granite|68116|5|Briefly described|Appendix, Map 19.|Late Devonian|Late Devonian||||||Leucocratic biotite granite: medium grained, equigranular; accessory muscovite.|
31572|Beechworth Suite|24551|6|Mentioned|p229|||Of the Tabberabbera Province.||||||
31572|Beechworth Suite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
34710|Beehive Granite|22878|4|Described|p77|||||||||
34710|Beehive Granite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Of the Bemboka Supersuite. Biotite granite: pink, coarse grained, massive except on faulted margin; leucocratic; texturally variable with finer grained and megacrystic areas.||||||01-OCT-04
34710|Beehive Granite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Bemboka Supersuite. Biotite granite: pink, coarse grained, massive except on faulted margin; leucocratic; texturally variable with finer grained and megacrystic areas.||||||01-OCT-04
34710|Beehive Granite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Bemboka Supersuite. Biotite granite: Highly magnetic (up to 195 nT) section, moderately magnetic (100 -125 nT) section and a non-magnetic section. High K, Th and U||||||06-OCT-04
34710|Beehive Granite|23309|5|Briefly described|p324|||G21. I-Type. Supersedes Beehive Creek Granite and Beehive Adamellite.||||||13-NOV-12
34710|Beehive Granite|68116|5|Briefly described|Appendix, Maps 37, 46.|Early Devonian|Llandovery||||||Biotite granite: pink, coarse grained, massive except on faulted margin; leucocratic; texturally variable with finer grained and megacrystic areas; I-type.|
37870|Beetoomba Granodiorite|24133|3|Fully described|p67|Silurian|Silurian|I-type granodiorite.  Geological Province: Lachlan Fold Belt.||||||
37870|Beetoomba Granodiorite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37870|Beetoomba Granodiorite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37870|Beetoomba Granodiorite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37870|Beetoomba Granodiorite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt||||||
37870|Beetoomba Granodiorite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37870|Beetoomba Granodiorite|68116|5|Briefly described|Appendix, Map 20.|Pridoli|Wenlock||||||Hornblende granodiorite: pinkish grey, medium grained; equigranular; I-type; very altered; highly magnetic.|
75954|Begg Creek Basalt|68115|5|Briefly described|p9.|Paleogene|Paleogene|New name, after Begg Creek. Formerly Older Volcanic Group near Club Terrace, as well as outliers SW and NE of Combienbar.|||||Tholeiite with phenocrysts of plagioclase, olivine and augite in a groundmass of plagioclase, pyroxene and brown glass.|
75954|Begg Creek Basalt|68116|5|Briefly described|Appendix, Map 45.|Neogene|Paleogene||||||Basalt flow: tholeiite with phenocrysts of plagioclase, olivine and augite in a groundmass of plagioclase, pyroxene and brown glass.|
1415|Belfast Mudstone|12781|6|Mentioned|p386|Late Cretaceous|Late Cretaceous|Otway Basin. Maximum thickness 1362m.||Sherbrook Group.||Overlies Flaxman Formation. Is overlain by Paaratte Formation.||
1415|Belfast Mudstone|12796|4|Described|p458, p456 Fig. 2|Santonian|Coniacian|Of the Sherbrook Group. Glauconitic dark mudstones. Interfingers with and underlies Nullawarre Greensand; overlies Flaxman Formation. Geological Province: Otway Basin/Port Campbell Embayment. ||||||
1415|Belfast Mudstone|22674|5|Briefly described|Fig.2 p719|Santonian|Cenomanian|||||||
1415|Belfast Mudstone|22875|3|Fully described|p42|Campanian|Cenomanian|Of the Sherbrook Group.||||||27-MAR-07
1415|Belfast Mudstone|22930|6|Mentioned|50|||||||||
1415|Belfast Mudstone|22944|5|Briefly described|Fig3|||||||||
1415|Belfast Mudstone|23818|4|Described|p164, 165|Late Cretaceous|Late Cretaceous|Overlain by Paaratte Formation; underlain by Flaxman Formation. Geological Province: Otway Basin. Max. thickness: ~1000 ft.||||||27-MAR-07
1415|Belfast Mudstone|23830|6|Mentioned|Fig. 6|||Geological Province: Gambier Embayment, Otway Basin.||||||
1415|Belfast Mudstone|24314|5|Briefly described|p61 Fig.2|Santonian|Turonian|Geological Province: Otway Basin. Max. Thickness 362m. Of the Sherbrook Group.||||||30-NOV-04
1415|Belfast Mudstone|24405|5|Briefly described|p6|Late Cretaceous|Late Cretaceous|Geological Province: Otway Basin.||||||
1415|Belfast Mudstone|24453|5|Briefly described|p809 Fig.2|Campanian|Coniacin|Of Sherbrook Group. Overlain by Paaratte Formation and Nullawarre Greensand, overlies Flaxman Formation. Geological Province: Otway Basin.||||||07-FEB-11
1415|Belfast Mudstone|24551|6|Mentioned|p245|||Of the Sherbrook Group||||||
1415|Belfast Mudstone|24562|5|Briefly described|p1, 8 Fig. 2|Late Cretaceous|Late Cretaceous|Of the Sherbrook Group.  Geological Province: Otway Basin.  Maximum Thickness: >1810m.||||||
1415|Belfast Mudstone|29697|6|Mentioned|Fig.11|||||||||
1415|Belfast Mudstone|29856|5|Briefly described|p38|||||||||
1415|Belfast Mudstone|30454|6|Mentioned|p26|||See also Fig.1||||||
1415|Belfast Mudstone|30499|6|Mentioned|p12|||Stratigraphy||||||
1415|Belfast Mudstone|30578|6|Mentioned|p7|||||||||
1415|Belfast Mudstone|30754|6|Mentioned|Table 12|||Stratigraphic table||||||
1415|Belfast Mudstone|31372|6|Mentioned|p17|||||||||
1415|Belfast Mudstone|31424|6|Mentioned|Plate 1|||On composite bore log||||||
1415|Belfast Mudstone|31624|6|Mentioned|p101|||See also Table 15-1||||||
1415|Belfast Mudstone|31714|6|Mentioned|p33|||||||||
1415|Belfast Mudstone|31920|4|Described|p51|||U.Cret. Of the Sherwood Group. See Table 3-2,3.||||||27-MAR-07
1415|Belfast Mudstone|31922|6|Mentioned|p187|||||||||
1415|Belfast Mudstone|32162|6|Mentioned|p58|||||||||
1415|Belfast Mudstone|32344|6|Mentioned|Fig.2|||||||||
1415|Belfast Mudstone|32894|5|Briefly described|p286|||U. Cret.||||||
1415|Belfast Mudstone|32896|6|Mentioned|Encl. 7.1|||U.Cret.||||||
1415|Belfast Mudstone|32897|6|Mentioned|p183|||||||||
1415|Belfast Mudstone|32898|6|Mentioned|Table 2-1|||||||||
1415|Belfast Mudstone|33155|6|Mentioned|p115|||||||||
1415|Belfast Mudstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
1415|Belfast Mudstone|33936|6|Mentioned|Fig.6|||||||||
1415|Belfast Mudstone|33940|6|Mentioned|Fig.21-1|||Turonian - Santonian.||||||
1415|Belfast Mudstone|33943|6|Mentioned|p380|||||||||
1415|Belfast Mudstone|34063|6|Mentioned|p3|||Table. U.Cret.||||||
1415|Belfast Mudstone|34308|6|Mentioned|Fig.85|||U.Cret.||||||
1415|Belfast Mudstone|34611|5|Briefly described|p164|||Fig.80.||||||
1415|Belfast Mudstone|34759|6|Mentioned|p59|||||||||
1415|Belfast Mudstone|34987|6|Mentioned|p174|||||||||
1415|Belfast Mudstone|36913|6|Mentioned|p78|||||||||
1415|Belfast Mudstone|38625|6|Mentioned|Table 2|||||||||
1415|Belfast Mudstone|39923|6|Mentioned|p357|||||||||
1415|Belfast Mudstone|40003|5|Briefly described|p43|||See also Fig.10||||||
1415|Belfast Mudstone|40560|5|Briefly described|Fig.3|||||||||
1415|Belfast Mudstone|40947|6|Mentioned|p3|||||||||
1415|Belfast Mudstone|41016|5|Briefly described|p214|||||||||
1415|Belfast Mudstone|41185|6|Mentioned|p177|||See also Fig. 5||||||
1415|Belfast Mudstone|41269|5|Briefly described|p245|||||||||
1415|Belfast Mudstone|41642|6|Mentioned|p244|||||||||
1415|Belfast Mudstone|41704|6|Mentioned|p100|||||||||
1415|Belfast Mudstone|41714|5|Briefly described|p301|||See also Fig.2||||||
1415|Belfast Mudstone|41726|5|Briefly described|p421|||||||||
1415|Belfast Mudstone|41868|4|Described|p533|||||||||
1415|Belfast Mudstone|41936|6|Mentioned|p75|||||||||
1415|Belfast Mudstone|42152|5|Briefly described|p15|||See also Fig.11||||||
1415|Belfast Mudstone|42361|3|Fully described|p15|Santonian|Cenomanian|Formation status preferred herein to Member status used by many in Victoria.||||||
1415|Belfast Mudstone|42524|5|Briefly described|Fig.3 P27|||||||||
1415|Belfast Mudstone|42545|6|Mentioned|p9|||Otway Basin||||||
1415|Belfast Mudstone|42555|5|Briefly described|p285|||||||||
1415|Belfast Mudstone|42599|5|Briefly described|Fig.3 P614|||||||||
1415|Belfast Mudstone|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
1415|Belfast Mudstone|43171|5|Briefly described|5-8|||Of Sherbrook Formation. Age: 85-90 Ma||||||
1415|Belfast Mudstone|43195|5|Briefly described|Map Legend||Late Cretaceous|See also commentary on back of map. Of Sherbrook Group.||||||
1415|Belfast Mudstone|43208|5|Briefly described|map legend|Santonian|Turonian|Of Sherbrook Group.||||||
1415|Belfast Mudstone|43219|5|Briefly described|Fig.3,p6.|Santonian|Turonian|of Sherbrook Group||||||
1415|Belfast Mudstone|43590|4|Described|p13|Campanian|Turonian|||||||
1415|Belfast Mudstone|43660|5|Briefly described|p14,Fig.6,p15||Late Cretaceous|||||||
1415|Belfast Mudstone|43733|6|Mentioned|Fig.2.11,p65||Late Cretaceous|||||||
1415|Belfast Mudstone|43744|6|Mentioned|Fig.3,p3|||||||||
1415|Belfast Mudstone|43783|6|Mentioned|Fig14, p11||Late Cretaceous|||||||
1415|Belfast Mudstone|43784|6|Mentioned|Fig10, p12||Late Cretaceous|||||||
1415|Belfast Mudstone|43814|6|Mentioned|Fig.3,p115|||||||||
1415|Belfast Mudstone|43937|5|Briefly described|Map Legend|Santonian|Aptian|||||||
1415|Belfast Mudstone|44133|5|Briefly described|p146|Campanian|Turonian|Basal unit of Paarette Formation. Of the Sherbrook Group. Thickness: 1355m+.||||||
1415|Belfast Mudstone|48581|2|Defined|p33|||See also p1,27-29,31,25,39,40,Fig.4,6,Pl.1,2. (J54-12/Port Campbell).||||||
1415|Belfast Mudstone|48624|14|Not recorded|p5,7,Fig.2|||(J65-6/Benara).||||||
1415|Belfast Mudstone|48625|14|Not recorded|p7|||(J54-6/Benara).||||||
1415|Belfast Mudstone|48911|3|Fully described|p18|||Upper Cretaceous||||||
1415|Belfast Mudstone|48977|6|Mentioned|Fig.5|||||||||
1415|Belfast Mudstone|49060|5|Briefly described|Fig.33|||||||||
1415|Belfast Mudstone|60538|5|Briefly described|p474 Fig. 13|||Geological Province: Otway Basin.||||||
1415|Belfast Mudstone|61017|5|Briefly described|p5 Fig. 2, p6|Santonian|Coniacian|Of the Sherbrook Group. Provides the regional seal for oil. Geological Province: Otway Basin. See also p6 Fig. 3.||||||07-FEB-11
1415|Belfast Mudstone|61182|3|Fully described|p16, p83-84|Campanian|Turonian|Of Sherbrook Gp. Conformable over Flaxman Fm, and Waarre Fm in some areas; overlain by Nullawarre Greensand. Geol.Prov: Otway Basin. Formerly regarded as part of Paarratte Fm. Marine to marginal marine, largely light grey to black mudstone; fossils occur.||||||
1415|Belfast Mudstone|61470|5|Briefly described|p28 Fig. 5|Campanian|Coniacian|Of the Sherbrook Group. Overlies Flaxman Formation; underlies the Skull Creek Mudstone and Nullawarre Greensand, with which it also interfingers. Geological Province: Otway Basin.||||||12-OCT-05
1415|Belfast Mudstone|61547|6|Mentioned|p461 Fig.2, p462. |Campanian|Turonian|||Unit in Sherbrook Group.||Overlies Flaxman Formation and Waarre Sandstone. Is overlain by Paaratte Formation.||
1415|Belfast Mudstone|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
1415|Belfast Mudstone|61623|6|Mentioned|p449 Fig. 4|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
1415|Belfast Mudstone|61625|5|Briefly described|p475, p476 Fig. 1, p476, p477, p480|Late Creatceous|Late Cretaceous|Was first nominated as a member of the Paaratte Formation by Bock and Glenie (1965); however Reynolds (1971) reinststed formation status. Of Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
1415|Belfast Mudstone|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||31-MAR-09
1415|Belfast Mudstone|61627|5|Briefly described|p500 Fig. 2|Late Cretaceous|Late Cretaceous|Of Shipwreck Subgroup. Geological Province: Otway Basin.||||||07-FEB-11
1415|Belfast Mudstone|61628|5|Briefly described|p509 Fig. 3, p510|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||31-MAR-09
1415|Belfast Mudstone|63122|5|Briefly described|p17 Fig. 4.3|Campanian|Turonian|Of the Sherbrook Group. Max. thickness: 1362m. Geological Province: Otway Basin. ||||||
1415|Belfast Mudstone|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p81|Santonian|Turonian|Previously Belfast Mudstone Member of Paaratte Fm.(Sprigg 1986); upgraded by Williamson et al (1987). Overlies Waarre Fm; conformably underlies Paaratte Fm; intertongues with Nullawarre Greensand. Age: 91-83Ma. Max.thickness: 1362m. Geol.Prov: Otway Basin||||||
1415|Belfast Mudstone|63125|5|Briefly described|p113|||Geological Province: Otway Basin. Composed of terrigenous DOM (dispersed organic matter) rich in inertinite and lean in vitrinite. ||||||
1415|Belfast Mudstone|63129|6|Mentioned|p134|||Geological Province: Otway Basin.||||||30-JAN-08
1415|Belfast Mudstone|63130|5|Briefly described|p143|||Geological Province: Otway Basin. Acts as a seal in relation to Waarre Sandstone.||||||06-FEB-08
1415|Belfast Mudstone|63269|5|Briefly described|p605-607, p616|Late Cretaceous|Late Cretaceous|Otway Basin. Details of oils and oil stains in named wells tabulated. Oil-source correlation. Biomarker diagram.||Sherbrook Group.||||
1415|Belfast Mudstone|63431|5|Briefly described|p677 Fig. 2|Coniacian|Turonian|Of the Sherbrook Group. Overlies Flaxman Formation and Waarre Sandstone. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
1415|Belfast Mudstone|66245|5|Briefly described|p5, p6 Fig.5, pp68-69 Fig.D5.|Maastrichtian|Coniacian|The authors decribe this unit as a 'grab-bag' for anything that cannot be distinguished, and call for more work to be done on this unit and the Sherbrook Group.||Unit in Sherbrook Group.||Is intercalated with Nullawarre Greensand. Is overlain by Paaratte Formation.||
1415|Belfast Mudstone|67061|6|Mentioned|p546 Fig.3.|Late Cretaceous|Late Cretaceous|||Unit in Sherbrook Group.||||
1415|Belfast Mudstone|67367|5|Briefly described|p131 Fig.2, p133, pp152-153.|Late Cretaceous|Late Cretaceous|Poor potential as hydrocarbon source rock. Rapid and significant deposition caused hydrocarbon generation and expulsion from Waarre Formation source rocks, and increased the maturity of the Eumeralla Formation.|c.85 Ma.|Unit in Sherbrook Group.||||
1415|Belfast Mudstone|69297|5|Briefly described|p78, p79, p84, p98, p115|Campanian|Coniacian|Otway and Sorell Basins. Deposited in marine, marginal marine or coastal plain environments. Potential seal for the Waarre and Flaxman Formation reservoirs. ||Sherbrook Group |Includes the Thylacine Sandstone Member and the Mourum Member. |Overlies the Flaxman Formation. Overlain by the Paaratte Formation and the Nullawarre Greensand. |Mudstone and siltstone. |
1415|Belfast Mudstone|69651|5|Briefly described|p10, p15, p32-34, p38|Late Cretaceous|Late Cretaceous|Most widely distributed seal in the Otway Basin; seals Waarre and Flaxman Formation reservoirs. Modelling diagrams.||Sherbrook Group.|Thylacine Member.|Overlies Flaxman Formation unconformably and Nullawarre Greensand. Is overlain by Paaratte Formation.||
1415|Belfast Mudstone|70077|5|Briefly described|Nelson: Fig.2; p1-2. Regional: Fig.4; p5|Late Cretaceous|Late Cretaceous|See also Regional: p7-8, p10. Otway Basin: Port Campbell Embayment and Robe-Penola Trough. Interpreted geochemically to be a moderately good source in Breaksea Reef 1. Contains an important petroleum reservoir in its [informal] "Thylacine Sandstone Member". Provides a regional seal for reservoirs within Flaxman and Waarre Formations. Appears also as Belfast Formation on p10.||Sherbrook Group.||Overlies Banoon Member (Flaxman Formation). Is overlain by Nullawarre Greensand. Is equivalent to Mount Salt Formation.||
1415|Belfast Mudstone|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4; p4-5|Santonian|Coniacian|Otway Basin. Equivalent rocks in the Sorell Basin are potential intraformational seals.||Sherbrook Group.||Overlies Flaxman Formation. Is overlain by Mount Salt Formation.||
1415|Belfast Mudstone|70193|6|Mentioned|p284 Fig 2, p285 fig 3|Santonian|Coniacian|Geological province: Otway Basin. Part of the Sherbrook Supersequence.||||||
1415|Belfast Mudstone|70880|6|Mentioned|p77|Campanian|Coniacian|Otway Basin.||||||
1415|Belfast Mudstone|70942|14|Not recorded|p118|||Stratigraphy.||||||
1415|Belfast Mudstone|71266|6|Mentioned|p614 Fig.3|Late Cretaceous|Late Cretaceous|Otway Basin.||||||
1415|Belfast Mudstone|71437|6|Mentioned|p157|||[Abbreviation of Belfast Mudstone Member]||Of Paaratte Formation.||||
1415|Belfast Mudstone|73357|5|Briefly described|p20-21, p31, p45|Santonian|Coniacian|Otway Basin. Correlated with multiple biozones including Phyllocladidites mawsonii Spore-Pollen Zone and Conosphaeridium striatoconum Dinocyst Zone in lower part, and Isabelidinium cretaceum Dinocyst Zone in upper part. Belfast Mudstone equivalent p47.||Of Sherbrook Group.||Overlies Flaxman Formation, underlies Nullawarre Greensand, Skull Creek Mudstone.|Includes shales.|
1415|Belfast Mudstone|73383|5|Briefly described|p3, p11 Tb.3.9, p21-22, p27, p200, p248|Santonian|Turonian|Otway Basin. Interpreted as equivalent to chemostratigraphic package S5-P4 which was only identified in the Penryn-1 well, or to the S5-P5 package. Lithologies based on geochemistry using the ChemLith classification includes sandstone, argillaceous and calcareous sandstone, mudstone, limestone and calcareous limestone; and using the Herron classification (1988) includes Fe-sand, shale, Fe-shale, wacke. See also vi, p68, p119, p134, p261-262.||Sherbrook Group||Overlies Flaxman Formation, underlies Nullawarre Greensand|Shelfal siltstones and marine shales.|
1415|Belfast Mudstone|73385|5|Briefly described|p5|Santonian|Turonian|Otway Basin.||Sherbrook Group||Overlies Flaxman Formation, underlies Nullawarre Greensand.|Shelfal siltstones and marine shales.|
1415|Belfast Mudstone|73386|4|Described|p4, p6, p10-11, Attachment A1|Santonian|Coniacian|Otway Basin. Thickens offshore. Middle to outer shelf, open marine prodelta depositional environment. Partly a facies variant of the underlying Flaxman Formation and overlying Paaratte Formation. Designated type section is from 1501 m to 1685 m in Port Campbell-1. Diachronous unit, extends from Phyllocladidites mawsonii to Tricolporites apoxyexinus spore-pollen zones.||Sherbrook Group||Conformably overlies Flaxman Formation, underlies Nullawarre Greensand|Dark grey to black, pyritic, silty mudstone that becomes sandier to the northwest of the Otway Basin. Occasional thin, upward coarsening sandstone interbeds.|
1415|Belfast Mudstone|73594|5|Briefly described|p4-5, p13, p24-25, p27, p30-32, p67|Santonian|Turonian|Otway Basin. Forms a regionally extensive top seal to the the Upper Waarre play, the Thylacine Member and Flaxman Formation. [Misspelt Belfast Formation p27?]||Sherbrook Group|Thylacine Member|Overlies Flaxman Formation, underlies Nullawarre Greensand. Unconformably underlies Skull Creek Mudstone locally.|Prodelta silty mudstones.|
27334|Bell Point Limestone|23229|5|Briefly described|Table3-3p27, 35|Zlichovian|Pragian|||||||
27334|Bell Point Limestone|23266|5|Briefly described|Fig13-5.1p354|||||||||
27334|Bell Point Limestone|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
27334|Bell Point Limestone|23309|5|Briefly described|p149,152,154.|Early Carboniferous|Late Devonian|||||||
27334|Bell Point Limestone|23522|5|Briefly described|p247 Fig 3|Early Devonian|Early Devonian|||||||
27334|Bell Point Limestone|23710|14|Not recorded|p84|||Fauna.||||||
27334|Bell Point Limestone|24098|5|Briefly described|p27 Fig. 2|Emsian|Emsian|Of the Murrindindi Supergroup. Geological Province: Melbourne Zone, Lachlan Fold Belt.||||||19-APR-05
27334|Bell Point Limestone|24551|4|Described|p130, 616|||||||||
27334|Bell Point Limestone|30570|5|Briefly described|p5|||||||||
27334|Bell Point Limestone|30930|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27334|Bell Point Limestone|31508|6|Mentioned|Table 1|||Devonian||||||
27334|Bell Point Limestone|32583|6|Mentioned|p374|||||||||
27334|Bell Point Limestone|33156|5|Briefly described|p132|||||||||
27334|Bell Point Limestone|33159|6|Mentioned|p15|||Stratigraphy||||||
27334|Bell Point Limestone|33238|5|Briefly described|p642|||||||||
27334|Bell Point Limestone|33393|6|Mentioned|p173|||||||||
27334|Bell Point Limestone|33601|6|Mentioned|Fig.6|||||||||
27334|Bell Point Limestone|33602|6|Mentioned|Fig.2|||||||||
27334|Bell Point Limestone|33604|6|Mentioned|p17|||Correlation chart. L.Dev.||||||
27334|Bell Point Limestone|33732|6|Mentioned|p106|||||||||
27334|Bell Point Limestone|34287|6|Mentioned|p97|||||||||
27334|Bell Point Limestone|34843|6|Mentioned|p8|||||||||
27334|Bell Point Limestone|34954|6|Mentioned|Fig.34|||||||||
27334|Bell Point Limestone|35112|6|Mentioned|Fig.9|||||||||
27334|Bell Point Limestone|35193|6|Mentioned|p19|||||||||
27334|Bell Point Limestone|35274|5|Briefly described|p421|||||||||
27334|Bell Point Limestone|35281|5|Briefly described|p17|||||||||
27334|Bell Point Limestone|35283|3|Fully described|p57|||||||||
27334|Bell Point Limestone|37501|6|Mentioned|p405|||||||||
27334|Bell Point Limestone|38787|6|Mentioned|p128|||||||||
27334|Bell Point Limestone|39331|6|Mentioned|Table 2-1|||||||||
27334|Bell Point Limestone|39858|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27334|Bell Point Limestone|41555|6|Mentioned|p412|||||||||
27334|Bell Point Limestone|41571|6|Mentioned|p55|||||||||
27334|Bell Point Limestone|41585|4|Described|p116|||||||||
27334|Bell Point Limestone|41868|5|Briefly described|p575|||||||||
27334|Bell Point Limestone|42015|6|Mentioned|p316|||||||||
27334|Bell Point Limestone|42032|6|Mentioned|p496|||||||||
27334|Bell Point Limestone|42033|6|Mentioned|p653|||||||||
27334|Bell Point Limestone|42577|5|Briefly described|p29|||||||||
27334|Bell Point Limestone|42635|5|Briefly described|p26|||||||||
27334|Bell Point Limestone|42827|4|Described|p116|||see also Table 4.1||||||
27334|Bell Point Limestone|43461|14|Not recorded|p627|||U/C on Waratah Limestone||||||
27334|Bell Point Limestone|43525|14|Not recorded|p130,Tb p121,132||Emsian|||||||
27334|Bell Point Limestone|43527|14|Not recorded|p543,544|||||||||
27334|Bell Point Limestone|43530|14|Not recorded|p1025,1028-30|Emsian|Siegenian|U.Siegenian-L.Emsian||||||
27334|Bell Point Limestone|43532|14|Not recorded|p201,204,206,220||Devonian|Revision of Mictophyllum. See also Lexicon||||||
27334|Bell Point Limestone|43547|14|Not recorded|p151,Tb 153-4,161||Emsian|Unconformable on Waratah Limestone. Brachs= Buchan Caves Limestone (U.Emsian)||||||
27334|Bell Point Limestone|48971|6|Mentioned|p9|||See also P17, P18, P20, P26, P28.||||||
27334|Bell Point Limestone|61181|5|Briefly described|p127|Devonian|Devonian|Well bedded, dark grey, fossiliferous and shaly limestone. Unconformably overlies Waratah Limestone. See also p129 Tb. 32.||||||
27334|Bell Point Limestone|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Waratah Bay. Appears in text as Bell Pt Limestone. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
27334|Bell Point Limestone|68298|5|Briefly described|p222|Pragian|Pragian|A lungfish jaw and placoderm plates discovered (K.S.W. Campbell and J.A. Long, pers. comm). This unit also contains conodonts and microvertebrates of late Pragian age.||||||
27334|Bell Point Limestone|73143|6|Mentioned|p11|Pragian|Pragian|Contains Heliolites daintreei tabulate coral (Hill, 1954b).||||||
72699|Bellarine Volcanic Group|65715|2|Defined|p13, p14 Tb.8, p15|Neogene|Neogene|Newly defined here. Includes Murraduc Basalt and Clifton Springs Tuff. New name introduced for 'Older Volcanics' outcropping on the Bellarine Peninsula. Named after Mount Bellarine. Consists mostly of basalt lavas of the Marraduc Basalt.||||||
1423|Bellbird Creek Formation|22815|4|Described|p100, fig31,32|||Age: Frasnian||||||
1423|Bellbird Creek Formation|22857|4|Described|p216, p494 App. 1 Tb.A1.7|Frasnian|Frasnian|Of the Merrimbula Group. Max. thickness: 375m. Geological Province: Lambie Shelf / Lambie Basin.||||||
1423|Bellbird Creek Formation|22859|5|Briefly described|p216|||||||||
1423|Bellbird Creek Formation|22878|6|Mentioned|p50|||||||||
1423|Bellbird Creek Formation|23309|6|Mentioned|p186|||||||||
1423|Bellbird Creek Formation|23522|5|Briefly described|p260|Early Devonian|Early Devonian|Of Merrimbula Group.||||||
1423|Bellbird Creek Formation|30938|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
1423|Bellbird Creek Formation|32127|3|Fully described|p264|||Refers Steiner (1966)||||||
1423|Bellbird Creek Formation|32129|6|Mentioned|p5|||||||||
1423|Bellbird Creek Formation|32865|6|Mentioned|p483|||Fauna. See also P484||||||
1423|Bellbird Creek Formation|33268|6|Mentioned|Table 1|||||||||
1423|Bellbird Creek Formation|33269|4|Described|p47|||Lithology||||||
1423|Bellbird Creek Formation|33732|5|Briefly described|p113|||||||||
1423|Bellbird Creek Formation|35277|5|Briefly described|p121|||||||||
1423|Bellbird Creek Formation|35526|6|Mentioned|Table 2|||Fossil types and localities||||||
1423|Bellbird Creek Formation|38899|6|Mentioned|p71|||||||||
1423|Bellbird Creek Formation|39313|6|Mentioned|p280|||||||||
1423|Bellbird Creek Formation|40276|6|Mentioned|p27|||||||||
1423|Bellbird Creek Formation|40646|6|Mentioned|p29|||||||||
1423|Bellbird Creek Formation|41385|6|Mentioned|p373|||||||||
1423|Bellbird Creek Formation|41641|5|Briefly described|p191|||||||||
1423|Bellbird Creek Formation|42050|5|Briefly described|p228|||||||||
1423|Bellbird Creek Formation|42158|6|Mentioned|p2|||||||||
1423|Bellbird Creek Formation|42827|5|Briefly described|p191|||of Merimbula Group||||||
1423|Bellbird Creek Formation|42848|4|Described|p532|Late Devonian|Late Devonian|Of Merrimbula Group. Contains the Ettrema Limestone Member. Consists of marine interbedded sandstone and mudstone with rare plant and marine fossils. Overlain by the Conjola Subgroup (Shoalhaven Group). Max. thickness: 1740m. See also p531 Fig. 3.||||||05-SEP-14
1423|Bellbird Creek Formation|43233|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
1423|Bellbird Creek Formation|43461|14|Not recorded|p625|||||||||
1423|Bellbird Creek Formation|46574|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Of the Merrimbula Group (Lambie Shelf). Geological Province: Lambian Transitional Province.||||||
1423|Bellbird Creek Formation|63605|5|Briefly described|p993 Fig.2, p999-1000|Frasnian|Frasnian|Middle unit of Merrimbula Gp.Overlies Twofold Bay Fm.Thickness: 350m. Lower marine transgression deposits (barrier island, littoral + shallow marine) to subaqueous deltaic phase; and upper deltaic tidal flat deposits;+ invertebrate marine fossil assemblage||||||05-SEP-14
1423|Bellbird Creek Formation|66499|5|Briefly described|p61, p62 Fig.6|Frasnian|Frasnian|Deposited during late Frasnian sea level maximum transgression. Includes invertebrate fossils.||Of Merrimbula Group||Stratigraphically above [?overlies] Twofold Bay Formation||
1423|Bellbird Creek Formation|68298|5|Briefly described|p214-215, p232; p234|Frasnian|Frasnian|A marine interval that contains invertebrate fauna, and has fish faunas in both overlying and underlying units.||Merrimbula Group||Is overlain by Worange Point Formation. Overlies Twofold Bay Formation.||
1423|Bellbird Creek Formation|68592|5|Briefly described|p34|Frasnian|Frasnian|||Unit in Merrimbula Group.|Is correlated with Strathaird Formation and Gibbons Creek Sandstone.||Marine clastic sequence.|
1423|Bellbird Creek Formation|70661|3|Fully described|p101, p107 fig 8, p112-p116|Frasnian|Frasnian|Named for the Bellbird Creek on the South coast of NSW. Distribution, geomorphology, geochemistry and fossil assemblage all discussed. Type section mentioned.Maximum thickness of 1740m in Ettrema Creek. Lithology discussed in greater detail (p113-114) . Deposited in a transgressive marine regime with barrier island, littoral, shallow marine and subaqeous deltaic depositional environments represented.||Merrimbula Group|Ettrema Limestone Member.|Faulted against Adaminaby Group, disconformably overlies Yalwal Volcanics, overlies Twofold Bay Formation, unconformably overlain by Shoalhaven Group, intruded by Bundundah Granite|Cross bedded quartzose sandstone, tuffaceous sandstone with minor shale, claystone, siltstone, conglomerate, limestone and rare basalt.|
1423|Bellbird Creek Formation|71303|5|Briefly described|map legend|Frasnian|Frasnian|||Of Merrimbula Group.|Includes Ettrema Limestone Member.||White, red-brown and green-grey, current-bedded, quartzose, fine- to very coarse-grained sandstone, red shale, siltstone and conglomerate. Rare marine microfossils and macroflora. Rare tuffaceous sandstone and intermediate dykes.|
1423|Bellbird Creek Formation|71700|5|Briefly described|CD|||||Merrimbula Group||||
1423|Bellbird Creek Formation|73181|6|Mentioned|p64-65, p67|Frasnian|Frasnian|Includes marine fossils. Contains invertebrate fossils; the brachiopods Cyphoterorhynchus, Productella and Cyrtospirifer.||Merrimbula Group||Underlain by Twofold Bay Formation. Overlain by Worange Point Formation.|Marine.|
77284|Bellbridge Granite|68115|5|Briefly described|p7.|||Omeo Zone. Shown as Bellbridge Gneiss on the Hume 1:50 000 geological map (O'Shea, 1979). Later mapping showed it to be granite, hence its renaming as Bellbridge Granite, G174.||||||07-DEC-21
77284|Bellbridge Granite|68116|5|Briefly described|Appendix, Map 20.|Pridoli|Ludlow||||||Biotite granite: weakly foliated, medium to coarse grained, with orthoclase phenocrysts up to 3 cm and biotite schlieren; S-type.|
30286|Beloka Gap Granite|23938|5|Briefly described|p38-39 Tb. 2|Triassic|Triassic|||||||
30286|Beloka Gap Granite|60503|4|Described|p31, p40 Tb. 2|Triassic|Triassic|Formerly informally called Marengo Gap Porphyry and Marengo Granite. Of the Mount Leinster Igneous Complex. A strongly porphyritic rock with clear quartz crystals, large white feldspars and specks of biotite in a fine light grey groundmass.||||||
30286|Beloka Gap Granite|60504|5|Briefly described|Map Legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Biotite granite: A-type; grey, strongly porphyritic in quartz and feldspar, miarolitic cavitites often lined with smoky quartz.||||||20-OCT-04
30286|Beloka Gap Granite|60505|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Biotite granite: A-type; grey, strongly porphyritic in quartz and feldspar, miarolitic cavitites often lined with smoky quartz.||||||21-OCT-04
30286|Beloka Gap Granite|60506|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Biotite granite: A-type; grey, strongly porphyritic in quartz and feldspar, miarolitic cavitites often lined with smoky quartz.||||||21-OCT-04
30286|Beloka Gap Granite|60507|5|Briefly described|Map Legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Biotite granite: A-type; grey, strongly porphyritic in quartz and feldspar, miarolitic cavitites often lined with smoky quartz.||||||21-OCT-04
30286|Beloka Gap Granite|60508|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Biotite granite: A-type; nonmagnetic (0-5 nT) with weakly magnetic (10-20 nT) north trending dykes, overlies 200 nT increased background; high total count , K, Th, U||||||21-OCT-04
30286|Beloka Gap Granite|68116|5|Briefly described|Appendix, Map 27.|Triassic|Triassic||||||Biotite granite: grey, strongly porphyritic in quartz and feldspar, miarolitic cavities often lined with smoky quartz.|
1449|Bemboka Supersuite|22878|6|Mentioned|p77|||||||||
1449|Bemboka Supersuite|22879|5|Briefly described|map|Early Devonian|Early Devonian|||||||
1449|Bemboka Supersuite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Loomat Granite, Beehive Granite, Drummer Granodiorite||||||01-OCT-04
1449|Bemboka Supersuite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||06-OCT-04
1449|Bemboka Supersuite|23309|5|Briefly described|p339|||Includes parts of Bega Batholith.||||||
1449|Bemboka Supersuite|24551|5|Briefly described|p235 |||Consists Of: Collangubra Suite, Drummer Suite, Tamboon Suite, Everard Suite.||||||
1449|Bemboka Supersuite|42726|5|Briefly described|Map legend|Early Devonian|Early Devonian|Contains the Memboka, Cololangubra, Drummer, Everard, Hyde Creek, New Building, Tamboon and Wologorong Suites.||||||07-FEB-05
1449|Bemboka Supersuite|42827|5|Briefly described|p430|||||||||
1449|Bemboka Supersuite|68592|6|Mentioned|p24, p1542||||||||I-type.|
1451|Ben Boyd Formation|22815|3|Fully described|p101, fig31,32|||This sequence previously included in the Worange Point Formation.||||||
1451|Ben Boyd Formation|22857|5|Briefly described|p217, p494 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Merrimbula Group. A point bar sequence of massive mudstone and arenite. Max. thickness: 850m. Geological Province: Lambie Basin.||||||
1451|Ben Boyd Formation|22859|5|Briefly described|p217|||||||||
1451|Ben Boyd Formation|23309|6|Mentioned|p186,187|||of Merrimbula Group.||||||
1451|Ben Boyd Formation|42158|6|Mentioned|p2|||Reserved as Ben Boyd||||||
1451|Ben Boyd Formation|42848|6|Mentioned|p532|||||||||
1451|Ben Boyd Formation|43233|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
1451|Ben Boyd Formation|71700|5|Briefly described|CD|||||Merrimbula Group||||
1451|Ben Boyd Formation|73181|6|Mentioned|p64|||[Written as 'Ben Boyd' Formation].||Merrimbula Group||Underlain by Worange Point Formation.||
37632|Ben Major Granite|23309|6|Mentioned|p424, Appendix 1|||G368, I-type. Supersedes Ben Major Adamellite.||||||
37632|Ben Major Granite|66002|5|Briefly described|p7 Tb.5|||Of Glenlogie Suite. G368. Called Ben Major Adamellite by Cayley and McDonald (1995)||||||
37632|Ben Major Granite|68116|5|Briefly described|Appendix, Map 31.|Early Devonian|Early Devonian||||||Hornblende-biotite granite: pale grey, medium grained.|
23373|Ben Nevis Granite|22756|5|Briefly described|P44, Table2 P42||Early Devonian|Age of unit is 391+/-5 Ma||||||
23373|Ben Nevis Granite|23309|5|Briefly described|p424 App1|||(G374). I-Type. Age: K/Ar 391 +/- 5 Ma.||||||
23373|Ben Nevis Granite|42726|5|Briefly described|map legend|Early Devonian||Reserved in 1993.||||||
23373|Ben Nevis Granite|43260|5|Briefly described|Map Legend||Early Devonian|Of the Mount Cole Suite. Biotite granite: pale grey to cream, porphyritic; dykes, pegmatite and quartz veins prevalent; small miarolitic cavities||||||27-OCT-04
23373|Ben Nevis Granite|44186|5|Briefly described|Map Legend||Early Devonian|G374 I-type.||||||
23373|Ben Nevis Granite|66002|5|Briefly described|p7 Tb.5|||Of Mount Cole Suite. G374.  Defined by Cayley and McDonald 1995.||||||
23373|Ben Nevis Granite|68116|5|Briefly described|Appendix, Map 31.|Early Devonian|Early Devonian||||||Biotite granite: pale grey to cream, porphyritic; dykes, pegmatite and quartz veins prevalent; small miarolitic cavities.|
1474|Bendoc Group|5258|6|Mentioned|164|||Includes Sunlight Creek Formation at base.||||||22-JAN-10
1474|Bendoc Group|22530|6|Mentioned|p695||Late Ordovician|||||||
1474|Bendoc Group|22545|6|Mentioned|p504|||||||||
1474|Bendoc Group|22577|6|Mentioned|p120,122||Ordovician|||||||
1474|Bendoc Group|22624|5|Briefly described|p678, Fig.3 p679|Late Ordovician|Late Ordovician|||||||
1474|Bendoc Group|22628|6|Mentioned|p115,p118|||||||||
1474|Bendoc Group|22704|6|Mentioned|p49||Late Ordovician|||||||
1474|Bendoc Group|22708|5|Briefly described|p210|Late Ordovician|Late Ordovician|||||||
1474|Bendoc Group|22815|4|Described|p24,122, fig10|Ordovician|Ordovician|||||||
1474|Bendoc Group|22832|4|Described|Fig.1b p634|Late Ordovician|Late Ordovician|See also p637.||||||
1474|Bendoc Group|22857|5|Briefly described|p134, p420 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Pelagic/hemipelagic black slates and mudstones and pelagic cherts.||||||
1474|Bendoc Group|22876|5|Briefly described|p15|Ordovician|Ordovician|500-440Ma||||||
1474|Bendoc Group|22877|5|Briefly described|map|Silurian|Silurian|||||||
1474|Bendoc Group|22878|5|Briefly described|p29|Ordovician|Ordovician|||||||
1474|Bendoc Group|22879|5|Briefly described|map|Late Ordovician|Late Ordovician|||||||
1474|Bendoc Group|22880|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Includes: Warbisco Shale||||||01-OCT-04
1474|Bendoc Group|22881|5|Briefly described|Map legend|Ordovician|Ordovician|||||||06-OCT-04
1474|Bendoc Group|22968|4|Described|P19, P30, P103|Late Ordovician|Ordovician|Graptolite fauna ranges from late Darriwilian to Bolindian, underlying unit is Adaminaby Group||||||
1474|Bendoc Group|22971|4|Described|p 17|Late Ordovician|Ordovician|Included in the "Hotham beds" in WANGARATTA region. Geological Province:  Lachlan Fold Belt.||||||19-JAN-06
1474|Bendoc Group|23020|5|Briefly described|Map legend|Late Ordovician|Late Ordovician|||||||
1474|Bendoc Group|23021|5|Briefly described|Map legend|Late Ordovician|Late Ordovician|||||||
1474|Bendoc Group|23028|5|Briefly described|Map legend|Late Ordovician|Late Ordovician|Underlying unit is Adaminaby Group.||||||01-SEP-08
1474|Bendoc Group|23029|5|Briefly described|Map legend|Ordovician|Ordovician|Underlying unit is the Adaminaby Group||||||
1474|Bendoc Group|23030|5|Briefly described|Map legend|Ordovician|Ordovician|Overlying unit is the Yalmy Group||||||
1474|Bendoc Group|23214|5|Briefly described|p3|Ordovician|Ordovician|||||||
1474|Bendoc Group|23245|5|Briefly described|p134||Late Ordovician|||||||
1474|Bendoc Group|23307|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
1474|Bendoc Group|23454|5|Briefly described|p28|Late Ordovician|Late Ordovician|||||||
1474|Bendoc Group|23615|3|Fully described|p67, 19|Late Ordovician|Late Ordovician|Includes Blueys Creek Formation, Sunlight Creek Formation, Warbisco Shale and Akuna Mudstone. Age within the 'deep marine Ordovician sedimentation' period: 500-438Ma.  Geological Province: Lachlan Fold Belt.||||||16-AUG-18
1474|Bendoc Group|23850|5|Briefly described|p793|||Overlies the Pinnak Sandstone.||||||26-APR-06
1474|Bendoc Group|23860|5|Briefly described|p944|||Underlying unit Adaminaby Group.||||||
1474|Bendoc Group|23938|5|Briefly described|p11, p31-32 Fig. 12.|Late Ordovician|Late Ordovician|Consists of mainly deep marine siltstone and black shale. See also p139 Tb. 1 Appendix.||||||25-SEP-08
1474|Bendoc Group|24002|5|Briefly described|p228 Fig.2|Ordovician|Ordovician|||||||
1474|Bendoc Group|24004|5|Briefly described|p278|Ordovician|Ordovician|||||||
1474|Bendoc Group|24037|6|Mentioned|p423|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt||||||
1474|Bendoc Group|24098|5|Briefly described|p27 Fig. 2|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
1474|Bendoc Group|24133|4|Described|p37|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
1474|Bendoc Group|24142|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
1474|Bendoc Group|24143|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
1474|Bendoc Group|24144|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
1474|Bendoc Group|24145|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt||||||
1474|Bendoc Group|24146|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
1474|Bendoc Group|24177|5|Briefly described|p48|Ordovician|Ordovician|||||||
1474|Bendoc Group|24215|5|Briefly described|p806|||Geological Province:  Lachlan Fold Belt||||||
1474|Bendoc Group|24317|5|Briefly described|p14, p15 Fig.1|Late Ordovician|Late Ordovician|Overlain by Mundoonen Sandstone.||||||
1474|Bendoc Group|24339|6|Mentioned|p46 Fig. 3|||Geological Province: Lachlan Fold Belt||||||
1474|Bendoc Group|24551|3|Fully described|p105, 7, 606, 230, 118 Fig. 5.1|Silurian|Darriwilian |Includes the Sunlight Creek Formation, Warbisco Shale, New Country Sandstone and Akuna Mudstone.||||||
1474|Bendoc Group|24575|5|Briefly described|p711, p716 Tb. 1|Late Ordovician|Middle Ordovician|Geological Province: Lachlan Fold Belt||||||
1474|Bendoc Group|24576|6|Mentioned|p727|||Geological Province: Lachlan Fold Belt||||||
1474|Bendoc Group|24600|5|Briefly described|p481|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
1474|Bendoc Group|42294|5|Briefly described|p24|||Reserved in 1985.||||||
1474|Bendoc Group|42647|4|Described|p19|||Reserved for use in NSW.||||||
1474|Bendoc Group|43206|5|Briefly described|map legend|Llandovery|Gisbornian|||||||
1474|Bendoc Group|43228|5|Briefly described|p9||Late Ordovician|||||||
1474|Bendoc Group|43233|5|Briefly described|Map Legend|Llandovery|Gisbornian|||||||
1474|Bendoc Group|43312|5|Briefly described|Map Legend|Bolindian|Darriwilian|||||||
1474|Bendoc Group|43313|5|Briefly described|Map Legend|Bolindian|Darriwilian|||||||
1474|Bendoc Group|43314|5|Briefly described|Map Legend|Bolindian|Gisbornian|||||||
1474|Bendoc Group|43315|5|Briefly described|Map Legend|Bolindian|Gisbornian|Includes Sunlight Creek Formation, Warbisco Shale and Akuna Mudstone.||||||03-MAY-05
1474|Bendoc Group|44093|5|Briefly described|p190 App. 1|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
1474|Bendoc Group|44184|5|Briefly described|Map Legend||Late Ordovician|||||||
1474|Bendoc Group|44185|5|Briefly described|Map legend.|Late Ordovician|Late Ordovician||||||Marine: black shale, cherty shale, stripy thin-bedded sandstone and siltstone, laminated siltstone.|
1474|Bendoc Group|50230|5|Briefly described|Map legend|Bolindian|Gisbornian|Includes the Warbisco Shale.  Overlies the Adaminaby Group; overlain by Mundoonen Sandstone.||||||10-MAY-04
1474|Bendoc Group|50231|5|Briefly described|Map Legend|Late Ordovician|Late Ordovician|Includes: Warbisco Shale.  Overlies: Adaminaby Group.||||||
1474|Bendoc Group|50232|5|Briefly described|Map legend|Eastonian|Gisbornian|Overlies the Adaminaby Group.  Includes the Warbisco Shale and Malay Creek Formation.||||||
1474|Bendoc Group|50233|5|Briefly described|Map Lagend|Bolindian|Gisbornian|Overlies the Adaminably Group||||||
1474|Bendoc Group|50234|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes: Dignams Siltstone, Warbisco Shale, Bumballa Formation.  Overlies Adaminaby Group; underlies the Poidevins Sandstone.||||||13-MAY-04
1474|Bendoc Group|60503|5|Briefly described|p84, p45 Tb. 2|Late Ordovician|Late Ordovician|Comprises Blueys Creek, Sunlight Creek, Warbisco, New Country and Akuna Formations, of which the second,third and fourth units are present in BENAMBRA. Characterised by deep marine shales, mudstones and chert. Overlies the Adaminaby Group. See also p48.||||||05-SEP-05
1474|Bendoc Group|60504|5|Briefly described|Map Legend|Bolindian|Darriwilian|Includes: Sunlight Creek Formation, Warbisco Shale, New Country Sandstone||||||
1474|Bendoc Group|60505|5|Briefly described|Map legend|Bolindian|Darriwilian|Includes: Sunlight Creek Formation, Warbisco Shale, New Country Sandstone.||||||
1474|Bendoc Group|60506|5|Briefly described|Map legend|Bolindian|Darriwilian|Includes: Sunlight Creek Formation, Warbisco Shale, New Country Sandstone||||||
1474|Bendoc Group|60507|5|Briefly described|Map Legend|Late Ordovician|Early Ordovician|Includes: Sunlight Creek Formation, Warbisco Shale, New Country Sandstone.||||||06-OCT-04
1474|Bendoc Group|60508|5|Briefly described|Map legend|Ordovician|Ordovician|Black shale, sandstone: nonmagnetic except where altered (0-20 nT); very low total count, K, Th, elsewhere similar to Pinnak Sandstone.||||||
1474|Bendoc Group|60536|6|Mentioned|p552|Silurian||||||||
1474|Bendoc Group|60541|4|Described|p12, p51, p19 Tb.1|Llandovery|Late Ordovician|Comprises Sunlight Cr. and Blueys Creek Fms, Warbisco Shale and Akuna Mudstone. Accumulated deep anoxic seafloor shales, mudstones and cherts interbedded with occasional thin bedded quartz-rich sandstones. Age: 500-438Ma. Geol.Prov: Lachlan Fold Belt.||||||12-JAN-06
1474|Bendoc Group|60542|4|Described|p45-46, p12|Llandovery (Early Sil)|Late Ordovician|Characterised by black shales, black and dark grey mudstones and cherts with rare pale coloured sandstones. Comprises: Blueys Creek and Sunlight Creek Formations, Warbisco Shale and Akuna Mudstone.||||||
1474|Bendoc Group|60902|5|Briefly described|p870|Late Ordovician|Late Ordovician|Black shales. Overlies Adaminaby Group and Wagga Group.||||||11-APR-06
1474|Bendoc Group|61160|3|Fully described|p12, p48, p17 Fig. 3.5|Late Ordovician|Late Ordovician|In eastern Victoria, comprises: Sunlight Creek Fm., Warbisco Shale, New Country Sst. and Akuna Mudstone (divisions that could not be achieved in BOGONG due to structural complexity). Conformable on Pinnak Sst., and in places, faulted against it.||||||
1474|Bendoc Group|61161|5|Briefly described|p82, p6, p78 p76-77 Fig 6.1|Late Ordovician|Middle Ordovician|Includes Warbisco Shale, Sunlight Creek Formation, Akuna Mudstone and New Country Sandstone. Nonmagnetic. Deep marine: graphitic mudstone; thin bedded quartz wacke. Faulted against Adaminaby and Cobbannah Groups; overlies Pinnak Sandstone. GSV mapcode: Ob||||||
1474|Bendoc Group|61163|3|Fully described|p79, p10 Fig. 31|Late Ordovician|Late Ordovician|Includes Sunlight Creek Fm, Warbisco Shale, New Country Sandstone, Akuna Mudstone. Marine sedimentary rocks. Overlies Adaminaby Group. Geological Province: Lachlan Fold Belt (Tabberabbera Zone). See also p14 Fig. 3.2, p38 Tb. 6.2.||||||
1474|Bendoc Group|61164|5|Briefly described|map legend|Late Ordivician|Late Ordivician|Mudstone, siltstone and sandstone: laminated and siliceous black mudstone and siltstone; thin bedded buff quartzose sandstone and dark grey siltstone; deep marine. GSV map code: Ob.||||||
1474|Bendoc Group|61165|5|Briefly described|map legend|Late Ordivician|Late Ordivician|Mudstone, siltstone and sandstone: laminated and siliceous black mudstone and siltstone; thin bedded buff quartzose sandstone and dark grey siltstone; deep marine. GSV map code: Ob.||||||
1474|Bendoc Group|61166|5|Briefly described|map legend|Late Ordivician|Late Ordivician|Mudstone, siltstone and sandstone: laminated and siliceous black mudstone and siltstone; thin bedded buff quartzose sandstone and dark grey siltstone; deep marine. GSV map code: Ob.||||||
1474|Bendoc Group|61167|5|Briefly described|map legend|Late Ordivician|Late Ordivician|Mudstone, siltstone and sandstone: laminated and siliceous black mudstone and siltstone; thin bedded buff quartzose sandstone and dark grey siltstone; deep marine. GSV map code: Ob.||||||07-FEB-11
1474|Bendoc Group|61168|5|Briefly described|map legend|Late Ordivician|Late Ordivician|Mudstone and sandstone: nonmagnetic (<5 nT, kv = 0-15 x10^-6 cgs); no mapped gravity response; low total radioelement, K and Th, moderate U. GSV map code: Ob.||||||
1474|Bendoc Group|61169|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Warbisco Shale. Sandstone, siltstone, mudstone, black shale, chert; deep-marine hemipelagic and turbidite deposits. GSV map code: Ob.||||||
1474|Bendoc Group|61170|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Warbisco Shale. Sandstone, siltstone, mudstone, black shale, chert; deep-marine hemipelagic and turbidite deposits. GSV map code: Ob.||||||07-FEB-11
1474|Bendoc Group|61171|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Warbisco Shale. Sandstone, siltstone, mudstone, black shale, chert; deep-marine hemipelagic and turbidite deposits. GSV map code: Ob.||||||
1474|Bendoc Group|61172|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Warbisco Shale. Sandstone, siltstone, mudstone, black shale, chert; deep-marine hemipelagic and turbidite deposits. GSV map code: Ob.||||||
1474|Bendoc Group|61173|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Warbisco Shale. Sandstone, siltstone, mudstone, black shale, chert; insufficient gravity data to determine response; nonmagnetic (k up to 5 x10^-6 cgs); varying moderate K, Th, U and total radioelements. GSV map code: Ob.||||||
1474|Bendoc Group|61174|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Akuna Mudstone, New Country Sandstone, Warbisco Shale and Sunlight Creek Formation. Black shale, cherty shale, stripy thin-bedded sandstone and siltstone, laminated siltstone. Deep-marine hemipelagic and turbidite deposits. GSV map code: Ob.||||||07-FEB-11
1474|Bendoc Group|61175|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Akuna Mudstone, New Country Sandstone, Warbisco Shale and Sunlight Creek Formation. Black shale, cherty shale, stripy thin-bedded sandstone and siltstone, laminated siltstone. Deep-marine hemipelagic and turbidite deposits. GSV map code: Ob.||||||
1474|Bendoc Group|61176|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Akuna Mudstone, New Country Sandstone, Warbisco Shale and Sunlight Creek Formation. Black shale, cherty shale, stripy thin-bedded sandstone and siltstone, laminated siltstone. Deep-marine hemipelagic and turbidite deposits. GSV map code: Ob.||||||
1474|Bendoc Group|61177|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Akuna Mudstone, New Country Sandstone, Warbisco Shale and Sunlight Creek Formation. Black shale, cherty shale, stripy thin-bedded sandstone and siltstone, laminated siltstone. Deep-marine hemipelagic and turbidite deposits. GSV map code: Ob.||||||
1474|Bendoc Group|61178|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Akuna Mudstone, New Country Sandstone, Warbisco Shale and Sunlight Creek Formation. Siltstone, minor black shale: nonmagnetic; moderate to high gravity; low to moderate total radioelement. GSV map code: Ob.||||||
1474|Bendoc Group|61187|5|Briefly described|p4, p5 Fig.3, p26 Fig.2, p29 Fig.4. |Late Ordovician|Late Ordovician|Benambra Terrane, Eastern Victoria. Correlative of Warbisco Shale, and Mount Easton Shale in the Melbourne Zone, Melbourne Terrane.|||||Mainly siltstone and black shale.|
1474|Bendoc Group|61196|5|Briefly described|p17|Ordovician|Ordovician|Graphitic mudstone and thin-bedded quartz wackes included. Conformably overlies the Pinnak Sandstone. Age is Late Ordovician.||||||25-JAN-06
1474|Bendoc Group|61762|6|Mentioned|p18, p19 Fig. 2(a)|Ordovician|Ordovician|||||||
1474|Bendoc Group|61964|3|Fully described|p14 Fig. 4, p30|Bolindian|Gisbornian|Includes Willandra Sst+Currawalla Shale. Incorporates black-shale dominated component of former Tallebung Gp. Black shale-dominated successions.Overlies Wagga Gp; overlain by Cobar Supergp + Boothumble Fm. Intruded byYalgogrin, Kikoira+Ungarie Granites||||||
1474|Bendoc Group|62070|5|Briefly described|p34 Fig.1, p38|Late Ordovician|Darriwilian|Age: late Darriwilian to latest Ordovician.||||Overlies the Adaminaby Group.|Black shale overlain by siltstone.|
1474|Bendoc Group|62405|5|Briefly described|Map legend|Ordovician|Ordovician|Includes the Currawalla Shale and Willandra Sandstone. Interbedded quartz sandstone, siltstone, black carbonaceous mudstone and minor quartz pebble conglomerate.||||||10-APR-08
1474|Bendoc Group|63285|6|Mentioned|p275 Fig. 2|||Geological Province: Molong Volcanic Belt. Consists of quartz-rich sandstone, siltstone, minor siliceous siltstone and rare black mudstone.||||||
1474|Bendoc Group|63286|6|Mentioned|p294 Fig. 1|||Consists of quartz-rich sandstone, siltstone and chert.||||||07-FEB-11
1474|Bendoc Group|63289|5|Briefly described|p363, p369, p380|Bolindian|Gisbornian|Conformably overlain by Triangle Formation. Consists of black shale and siltstone.||||||07-FEB-11
1474|Bendoc Group|63290|4|Described|p385, p388, p396 Fig. 3|Early Silurian|Late Ordovician|Includes Acton Shale, Sunlight Creek Formation, Waribisco Shale, Akuna Formation, Gungoandra Siltstone. Underlain by Girlambone Group, Wagga Group and Adaminaby Group.||||||18-SEP-08
1474|Bendoc Group|63635|5|Briefly described|p39|Darriwilian||Overlies Pinnak Sandstone. Correlation between mainland Australia and Tasmania discussed.||||||
1474|Bendoc Group|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Includes Warbisco Shale, Bumballa Formation and Dignams Siltstone.||||||28-MAY-08
1474|Bendoc Group|64295|5|Briefly described|p198 Fig. 1, p199|Late Ordovician|Late Ordovician|||||||
1474|Bendoc Group|64568|5|Briefly described|Map legend|Ordovician|Ordovician|Includes Currawalla Shale and Willandra Sandstone. Unnamed section is of interbedded quartz sandstone, siltstone, black carbonaceous mudstone and minor quartz-pebble conglomerate.||||||24-SEP-08
1474|Bendoc Group|65469|5|Briefly described|p18, p20|Late Ordovician|Late Ordovician|Lachlan Orogen. Replaces rocks previously mapped as Tallebung Group east of Nymagee. ||||Overlies the Wagga Group.|Black shales and local sandstones. |
1474|Bendoc Group|66713|5|Briefly described|p3|Late Ordovician|Late Ordovician|Black shale units with thin bedded mudstones and rare turbidites. Overlies the Adaminaby Group.||||||
1474|Bendoc Group|67322|4|Described|p4 Fig.2, p5, p13, p16, p28, p20 Fig.5|Late Ordovician|Middle Ordovician|Albury-Bega Terrane. Age determined from  p20 Fig.5 (Strat. column). This is supported due to the presence of graptolites of Upper Ordovician age. Occurs in the Cooma-Mallacoota, Canberra-Queanbeyan, and Goulburn regions.|||Warbisco Shale, Currawalla Shale, Acton Shale, Sunlight Creek Formation, Akuna Mudstone, Willandra Sandstone.|Conformably overlies the Adaminaby and Wagga Groups. Overlies the Chakola and Bumballa Formations. Overlain by the Margules Group.|Graptolitic black shales with relatively minor sandstone.|
1474|Bendoc Group|67802|5|Briefly described|p28|Late Ordovician|Late Ordovician|In fault zones throughout Benambra Terrane in Victoria. Useful dating stratum due to abundant graptolites.||||Is conformable with underlying Adaminaby Group, but usually occurs in faulted contact.|Black shale, sandstone, mudstone, sometimes bioturbated. The change from quartz-turbidite to black shale correlated to relative rise of sea level.|03-OCT-14
1474|Bendoc Group|67847|6|Mentioned|p83|||May be associated with the Cobram mineralisation. ||||||
1474|Bendoc Group|68116|5|Briefly described|Appx, Maps 18-20, 26-27, 34-36, 44-45.|Hirnantian|Darriwilian|Minimum age written as Bolindian in text.|||||Black shale, cherty shale, stripy thin-bedded sandstone and siltstone, laminated siltstone.|06-SEP-16
1474|Bendoc Group|68466|6|Mentioned|p70|Late Ordovician|Late Ordovician|||||Overlies Adaminaby Group.|Includes black shales containing prolific graptolites.|
1474|Bendoc Group|68592|3|Fully described|p316, p320-43, p348, p350, p354, p358|Late Ordovician|Late Ordovician|See also xxiv, p71, p73 Tb.5, p116-8, p230, p269, p272, p275 Fig.57, p277-8, p280, p282, p287, p291-3, p298, p302, p310, p362, p364, p366-7, p376, p384, p419, p421, p426, p731, p742-3, p753, p750, p753, p756, p758, p771, p793, p813, p819. Glen et al. (1990), VandenBerg et al. (1992). Named after Bendoc region of East Gippsland, Vic. Includes black shales formerly attributed to Abercrombie Beds (Packham, 1968), Adaminaby Group (Raymond et al. 1998) and Bubalahla Formation (Scheibner, 1973). c.450m thick. Near-complete reference section in Mountain Creek, NE Victoria; reference sections in NSW described. Quarried (eg Carrick Hill) for road materials. Covan Creek Formation sandstone composition suggests derivation predominantly from deformed and uplifted Adaminaby Group quartzose turbidites and chert, and Bendoc Group black shale. Frogmore, Wyangala, Peelwood, Goulburn and Bungonia structural zones: deformation described. Is intruded by Lockyersleigh Granite.|||Includes Warbisco Shale and (in NSW) Bumballa Formation and (in Vic) Sunlight Creek Formation, New Country Sandstone and Akuna Mudstone.|Conformably overlies Abercrombie Formation. Is overlain conformably by Margules Group and unconformably by Shivering Conglomerate, Cobra, Argyle and Strathaird Formations.|Siliceous black shale, generally with turbiditic sandstone, blackshale and siltstone at the base.|
1474|Bendoc Group|68822|5|Briefly described|p351|Upper Ordovician|Upper Ordovician|Graptolite ages range from Gisbornian 1 to Bolindian 3 (VanderBerg and Cooper 1992; Percival et al. 2011).||||Underlain by the Adaminaby Group and Girilambone Group.|Black shale sequence.|
1474|Bendoc Group|69002|6|Mentioned|p13|||Contains Late Ordovician black shales.||||Underlain by the Wagga Group and the Adaminaby Group.||
1474|Bendoc Group|69159|5|Briefly described|Map legend|Ordovician|Ordovician||||Includes Warbisco Shale and Bumballa Formation.|||
1474|Bendoc Group|69160|5|Briefly described|Map legend|Ordovician|Ordovician||||Includes Currawalla Shale and Willandra Sandstone.||Interbedded quartz sandstone, siltstone, black carbonaceous mudstone and minor quartz pebble conglomerate.|
1474|Bendoc Group|69540|5|Briefly described|p640||||||Includes Currawalla Shale.||Black shale. Contains intercalated sequences of quartz-rich turbidites up to 200m thick.|
1474|Bendoc Group|69541|5|Briefly described|p652-653|Late Ordovician|Late Ordovician|||||Overlies Adaminaby and Wagga Groups.|Black to buff coloured shale, siltstone +/- sandstone.|
1474|Bendoc Group|69564|6|Mentioned|p3||||||||Black shale.|
1474|Bendoc Group|69635|6|Mentioned|p148|Ordovician|Ordovician|||||||
1474|Bendoc Group|69668|5|Briefly described|p927|Late Ordovician|Late Ordovician||||||Includes black shales.|
1474|Bendoc Group|70026|5|Briefly described|p40|Late Ordovician|Late Ordovician|Geological province: Lachlan Orogen. |||||Black shale.|
1474|Bendoc Group|70178|6|Mentioned|p3|Ordovician|Ordovician||||||Siliciclastic turbidites.|
1474|Bendoc Group|70192|5|Briefly described|Map Legend|Bolindian|Gisbornian|[Theta]b. Undifferentiated member composed of siliceous shale with interbedded, thinly bedded, ripple cross-laminated and thick bedded quartzose sandstone and siltstone. On Boorowa, Crookwell, Taralga, Yass, Gunning and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.|||Includes Bumballa Formation, Warbisco Shale and one undifferentiated unit.|Overlies Adaminaby Group. Is overlain by Margules Group.||
1474|Bendoc Group|70297|4|Described|map legend, on side 2 of map sheet|Early Ordovician|Early Ordovician|Max age: Gisbornian? Min age: Bolindian? Small slivers of siliceous black shale and variably developed quartzose sandstone and siltstone. Small structurally controlled low sufide (orogenic) gold, and copper-dominated structurally  controlled high sulfide (orogenic) base metal +/- gold veins.|||Bumballa Formation, Warbisco Shale|Overlies Adaminaby Group.|Black shale and slate, siliceous mudstone, chert, siltstone, fine-grained quartz sandstone to quartzite; massive to laminated, commonly graptolitic, deep marine.|18-MAY-16
1474|Bendoc Group|70493|6|Mentioned|p56||Late Ordovician|Lachlan Orogen.||||Overlies Adaminaby Group.||
1474|Bendoc Group|70540|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Warbisco Shale.|||
1474|Bendoc Group|70541|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Bumballa Formation, Warbisco Shale.|||
1474|Bendoc Group|70542|5|Briefly described|Map Legend|Late Ordovician|Late Ordovician||||Includes Bumballa Formation, Warbisco Shale|||
1474|Bendoc Group|70543|5|Briefly described|Map Legend|Ordovician|Ordovician|Undifferentiated member composed of siliceous shale with interbedded, thinly bedded, ripple cross-laminated and thick bedded quartzose sandstone and siltstone.|||Includes Bumballa Formation, Warbisco Shale and one undifferentiated member.|||
1474|Bendoc Group|70544|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Warbisco Shale|||
1474|Bendoc Group|70545|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Warbisco Shale.|||
1474|Bendoc Group|70601|5|Briefly described|p23, p25-27, p43, p45, p48-55, p57|Bolindian|Gisbornian|Albury-Bega Basin: Inland Zone. Uppermost unit is stratigraphically equivalent to Bogolo Formation.|||Warbisco Shale, Sunlight Creek Formation, Akuna Mudstone, Chakola Formation.|Overlies Numeralla Chert, Adaminaby Group. Underlies Akuna Mudstone, Bogolo Formation.|Black shales, minor turbidites, minor sandstones, chert.|
1474|Bendoc Group|70661|3|Fully described|vii, viii, p12, p13, p14|Eastonian|Gisbornian|Name derived from town of Bendoc, occurs over a vast area of NSW and VIC. Deposited in a deep marine environment with a mixture of hemipelagic and turbiditic sediments.Reference section in Mountain Creek, Victoria. Total thickness of 420m estimated in Moss Vale map sheet. Fossil assemblage described. See also p19, p20 fig 3, p21, p145.|||Bumballa Formation, Warbisco Shale, Sunlight Creek Formation, New Country Sandstone, Akuna Mudstone|Overlain by Bungonia group, Bindook group, Tallong Conglomerate, overlies Nattery Chert Member, overlies Adaminaby Group conformably,  also faulted against Adaminaby Group|Turbiditic sandstone, minor thin chert horizons that passes up into black  siliceous shales.|
1474|Bendoc Group|70684|5|Briefly described|p7 Fig.1, p15|||||||Overlies Adaminaby Group.|Black shales.|
1474|Bendoc Group|70718|4|Described|p43-p44|Late Devonian|Llandovery|Tabberabbera Zone, Murray Basin. Deposited in a deep marine setting. Hosts numerous small orogenic gold deposits.|||||Black shale, slate, siliceous mudstone, chert, siltstone, fine-grained quartz sandstone and quartzite.|02-JUN-19
1474|Bendoc Group|70751|6|Mentioned|p4-p6, p12, p15|Ordovician|Ordovician||||Includes the Currawalla Shale.|||
1474|Bendoc Group|70950|6|Mentioned|p1028-1029|Late Ordovician|Late Ordovician|Geological province: Central Lachlan Orogen. Turbiditic sedimentary rocks that form basement to the Lachlan Orogen|||Includes Currawalla Formation.|||
1474|Bendoc Group|71039|6|Mentioned|p6|Ordovician|Ordovician|||||||
1474|Bendoc Group|71040|6|Mentioned|p3, p10 Fig.6|Late Ordovician|Middle Ordovician|Marked by closely spaced thrust faults.||||||
1474|Bendoc Group|71069|3|Fully described|p9, p21 fig 7, p22, p23, p40 fig 17|Llandovery|Gisbornian|Lachlan Orogen. Name derived from the Bendoc region of Victoria. Previously mapped as part of the Adaminaby and Wagga Groups. Also mapped previously as the Bubalahla Formation, Merigan Black Shale, Birkenburn Beds, Copper Creek Shale and Tallebung Group or Beds. No single type section exists for the Bendoc Group, although a representative section has been proposed. Thickened during the Benambran Orogeny. Hosts VAMS mineralisation. Thickness estimated to range from 450 to over 900m.In deeply weathered areas forms low rounded hills associated with low outcrop, although good exposure is found in quarries and road cuttings. Also overlain by the Covan Creek Formation and unconformably overlain by the Hoskinstown Group.  Contains abundant graptolite fossils, also contains flattened spherical sponges, phosphatic brachiopods, burrows and conodonts.  Distribution, Metamorphism, Tectonic Structure and Geochemistry discussed. See also p41, p45, p51, p52, p53 fig 19, p56, p58, p61, p62, p68, p71-p77, p76 fig 27, p80, p81, p84, p85, p87, p92, p93, p95, p100, p105-p107, p116, p125, p126, p134, p144, p172.|||Includes the Warbisco Shale, Bumballa Formation, Sunlight Creek Formation, Akuna Mudstone, Gungoandra Siltstone, Currawalla Shale, New Country Sandstone and the Willandra Sandstone.|Conformably overlies the Adaminaby Group and the Wagga Group. Conformably overlain by the Margules Group and Yalmy Group.|Siliciclastic turbidite sequences of thick-bedded quartzose sandstone, black shale, siltstone and black carbonaceous to siliceous graptolitic shale.|
1474|Bendoc Group|71303|5|Briefly described|map legend|Late Ordovician|Late Ordovician||||Includes Bumballa Formation, Warbisco Shale.|||
1474|Bendoc Group|71656|4|Described|p10 Fig.1, p11, p14|Sandbian|Darriwilian|Contains poorly preserved graptolites in the early strata (Bumballa Formation).  Conodonts also present in  cherts.|||Bumballa Formation, Warbisco Shale.|Overlies Adaminaby Group. Underlies Margules Group.|Fossiliferous including graptolite bearing shales, conodont bearing cherts.|
1474|Bendoc Group|71691|5|Briefly described|Map legend.|Ordovician|Ordovician||||Warbisco Shale, Bumballa Formation.|Overlies Adaminaby Group. Is overlain by Margules Group.||
1474|Bendoc Group|71693|5|Briefly described|Map legend; p2.|Ordovician|Ordovician|This unit is mapped separately (with the symbol Obe), as well as in combination with the Clements Formation (with the symbol Owac_Obe) where these two units are fault-imbricated. Turbiditic sedimentary sequence.||||Overlies Clements Formation (Wagga Group).|Black shale and slate, siliceous mudstone, chert, siltstone, fine-grained quartz sandstone to quartzite; massive to laminated, commonly graptolitic, deposited as deep marine sediments.|
1474|Bendoc Group|71699|5|Briefly described|Map legend.|Ordovician|Ordovician||||Bumballa Formation, Warbisco Shale.|Overlies Adaminaby Group. Is overlain by Margules Group.||
1474|Bendoc Group|71700|3|Fully described|vi, viii, ix, p5, p7, p9-p11,  p36-p40,|Late Ordovician|Ordovician|Lachlan Orogen. VandenBerg et al (1992) described an almost complete reference section in Mountain Creek Additionally Thomas and Pogson (2012) proposed several represnetative sections in the Goulburn 1:250k sheet. The name is derived from the Bendoc region of East Gippsland, Victoria. Seperated by Felton and Huleatt (1975) from the Adaminaby Group as the "Merigan Black Shale". Rocks of this unit were previously included in the "Abercrombie Beds" (Packham 1968) and Adaminaby Group (Raymond et al. 1998). Scheibner (1973a) made the first attempt to map the shale-rich rocks as the "Bubalahla Formation". The Bendoc Group was subsequently mapped by Lewis et al (1994). Distribution, Geomorphic expression, outcrop, thickness, structure, geophysical characteristics, fossils and geochemistry are described. Thickness estimates for this group are difficult due to internal deformation and a lack of complete stratigraphic contacts; however, in the least-deformed sections thickness reaches up to 900m.Faulted against the Abercrombie Formation. See also p45-p46, p48, p50, p57, p60, p64, p71, p79, p82-p83, p90, p107, p110 and CD.|||Includes the Bumballa Formation, Warbisco Shale, Sunlight Creek Formation, New Country Sandstone and Akuna Mudstone.|Conformably overlies the Adaminaby Group. Conformably overlain by the Margules Group. Unconformably overlain by the Mount Fairy Group and the Woodlawn Volcanics. |Siliceous black shale which overlies a sequence of turbiditic, thin-bedded, ripple cross-laminated, and thick -bedded quartzose sandstone, black shale and siltstone (Bumballa Formation).|
1474|Bendoc Group|71889|6|Mentioned|p9, p12||||||Includes the Currawalla Shale.|||
1474|Bendoc Group|72082|5|Briefly described|p4|Ordovician|Ordovician||||||Metasedimentary sequences.|
1474|Bendoc Group|72083|6|Mentioned|p10||||||Currawalla Shale.|||
1474|Bendoc Group|72084|5|Briefly described|p2, p6 Fig.5a, p7, p9|Late Ordovician|Late Ordovician||||Currawalla Shale.||Metasedimentary sequence.|
1474|Bendoc Group|72296|5|Briefly described|p59|||Largely pelagic sequence.|||||Black muds.|
1474|Bendoc Group|72908|6|Mentioned|p4, p28|Ordovician|Ordovician||||||Contains black shale/carboniferous units.|
1474|Bendoc Group|73059|5|Briefly described|p1059|Late Ordovician|Late Ordovician|Tabberabbera Zone.||||Overlies Adaminaby Group.||
1474|Bendoc Group|73140|5|Briefly described|p495|Bolindian|Gisbornian|Following the division of the late Ordovician sequence in the Goulburn area by Thomas and Pogson (2012), it is proposed that the New Country Sandstone, Akuna Mudstone, Gungoandra Siltstone and Willandra Sandstone are reassigned from the Bendoc Group to Margules Group.|||Warbisco Shale, Bumballa Formation, Currawalla Shale, Sunlight Creek Formation|Overlies Adaminaby Group, underlies Margules Group|Defined by marked reduction in terrigenous sedimentation.|
1474|Bendoc Group|73186|6|Mentioned|p227, p229 Fig.2, p237, p242|Late Ordovician|Late Ordovician|Lachlan Orogen, Tabberabera Zone, Omeo Zone, Bega and eastern Victoria. 700 m thick.|||||Black shale.|
1474|Bendoc Group|73211|6|Mentioned|p909|Upper Ordovician|Middle Ordovician|Referred to as the foundation of the Lachlan Orogen/Fold Belt.||||||
1474|Bendoc Group|73431|6|Mentioned|p363 Fig.1|Late Ordovician|Late Ordovician||||||Sediments.|
83414|Benjeroop Granite|73505|5|Briefly described|p18, p21|||Newly named unit in Swan Hill and parts of Balranald and Deniliquin 1:250 000 map areas, (G656). Named after Benjeroop Parish and Benjeroop 1 which intersected the granite. Of the Lalbert Batholith. Aligned in the Governor Fault system 30 km north of Kerang. Magnetic high of 100 nT, shows magnetic zoning. Gravity response of a 10 micrometres/second/second low on a regional gradient.|||||Granite.|
69710|Bennies Formation|61163|3|Fully described|p90-92, p36 Tb. 6.2|Late Devonian|Late Devonian|Part of volcanic sequence of Tolmie Ig. Cmplx of ignimbrites (variable phenocrysts content, variable welding) and fluvial seds. - interbedded tab. to lent.conglom, sst, minor mudst. Under Mount Kent Conglom. Thick: >500m. Geol Prov: LFB. See also p89.||||||21-AUG-07
69710|Bennies Formation|61174|5|Briefly described|map legend|Late Devonian|Late Devonian|Of the Tolmie Igneous Complex. Ignimbrite, conglomerate, sandstone: ignimbrite, variable phenocryst content, commonly coarse-grained, +/- biotite and/or garnet, lesser intercalated conglomerate; minor sandstone and red mudstone. GSV map code: Dtb.||||||07-FEB-11
69710|Bennies Formation|61175|5|Briefly described|map legend|Late Devonian|Late Devonian|Of the Tolmie Igneous Complex. Ignimbrite, conglomerate, sandstone: ignimbrite, variable phenocryst content, commonly coarse-grained, +/- biotite and/or garnet, lesser intercalated conglomerate; minor sandstone and red mudstone. GSV map code: Dtb.||||||
69710|Bennies Formation|61176|5|Briefly described|map legend|Late Devonian|Late Devonian|Of the Tolmie Igneous Complex. Ignimbrite, conglomerate, sandstone: ignimbrite, variable phenocryst content, commonly coarse-grained, +/- biotite and/or garnet, lesser intercalated conglomerate; minor sandstone and red mudstone. GSV map code: Dtb.||||||
69710|Bennies Formation|61177|5|Briefly described|map legend|Late Devonian|Late Devonian|Of the Tolmie Igneous Complex. Ignimbrite, conglomerate, sandstone: ignimbrite, variable phenocryst content, commonly coarse-grained, +/- biotite and/or garnet, lesser intercalated conglomerate; minor sandstone and red mudstone. GSV map code: Dtb.||||||
69710|Bennies Formation|61178|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Tolmie Igneous Complex. Ignimbrite, lesser intercalated conglomerate; minor sandstone and red mudstone. GSV map code: Dtb.||||||
69710|Bennies Formation|68116|5|Briefly described|Appendix, Maps 26, 34.|Late Devonian|Late Devonian||||||Ignimbrite with variable, usually high, phenocryst content, commonly coarse-grained, with biotite and/or garnet, lesser intercalated conglomerate with well rounded vein quartz pebbles and lesser basement pebbles; minor sandstone and red mudstone.|
34905|Bentleys Plain Granodiorite|22968|5|Briefly described|P172, P218||Late Silurian|New name, type locality location given on P219, similar to the Cocks Break Granodiorite, weakly magnetic||||||
34905|Bentleys Plain Granodiorite|23021|6|Mentioned|Map legend|||||||||
34905|Bentleys Plain Granodiorite|23030|5|Briefly described|Map legend|Late Silurian|Late Silurian|parent is unassigned||||||
34905|Bentleys Plain Granodiorite|23309|6|Mentioned|p424 App1|||G325 I-Type.||||||
34905|Bentleys Plain Granodiorite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Granodiorite: grey; coarse-grained equigranular; moderate biotite foliation; occasional igneous enclaves have diffuse margins.|
34880|Berrawan Conglomerate|22968|4|Described|P122|Late Silurian|Late Silurian|New name, lowest unit of the Mount Tambo Group, includes the Deep Creek Conglomerates"" and the Mount Tambo Conglomerates"", type section location given on P122||||||
34880|Berrawan Conglomerate|23021|5|Briefly described|Map legend|Ludlow|Ludlow|Parent is Mount Tambo Group, overlying unit is Blackfellows Flat Conglomerate||||||
34880|Berrawan Conglomerate|23030|5|Briefly described|Map legend|Late Silurian|Late Silurian|Parent is the Mount Tambo Group||||||
34880|Berrawan Conglomerate|23309|5|Briefly described|p103,129 Tb2.37|||Informally subdivided. Of the Mount Tambo Group.||||||
34880|Berrawan Conglomerate|24551|4|Described|p138, p140|||Of the Mount Tambo Group.||||||
34880|Berrawan Conglomerate|60503|4|Described|p129|Early Devonian|Early Devonian|Basal unit of the Mount Tambo Group. Contains the Moonip Sandstone Member. Alluvial fan deposits comprising cobble conglomerates with minor coarse greywackes and pebbly greywackes and minor mudstones. Overlain by Blackfellows Flat Formation. ||||||
34880|Berrawan Conglomerate|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Mount Tambo Group. Fluvial sediments: conglomerate; thick-bedded, well-sorted.||||||20-OCT-04
34880|Berrawan Conglomerate|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Mount Tambo Group. Fluvial sediments: conglomerate; thick bedded, well sorted.||||||
34880|Berrawan Conglomerate|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Mount Tambo Group. Fluvial sediments: conglomerate; thick bedded, well sorted||||||20-OCT-04
34880|Berrawan Conglomerate|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Mount Tambo Group. Fluvial sediments: conglomerate; thick bedded, well sorted.||||||
34880|Berrawan Conglomerate|68116|5|Briefly described|Appendix, Maps 27, 35.|Pragian|Ludlow||||||Conglomerate with minor sandstone; includes an interval of sandstone and siltstone, and an interval of vitric-rich ignimbrite and conglomerate.|
37633|Berrigama Granodiorite|23309|6|Mentioned|p424 Appendix 1|||G571, I-type.||||||
1524|Berrigan Granite|22857|5|Briefly described|p213|Devonian|Devonian|Massive, pink, biotite, felsic, fractionated I-type granite. Geological Province: Barka Basin.||||||
1524|Berrigan Granite|22859|5|Briefly described|p213|||||||||
1524|Berrigan Granite|30909|6|Mentioned|Map legend|Silurian|Silurian|Prob. Silurian||||||
1524|Berrigan Granite|33553|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
1524|Berrigan Granite|34418|6|Mentioned|p502|||?Late Silurian||||||
1524|Berrigan Granite|40328|4|Described|p202|||||||||
1524|Berrigan Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
1524|Berrigan Granite|44340|14|Not recorded|p.5|||I/55-14. Upper Silurian?||||||
1524|Berrigan Granite|44341|14|Not recorded|map legend|||Coarse pink porphyritic granite. Upper Silurian?||||||
1524|Berrigan Granite|69798|6|Mentioned|p6, p13-14, p17|||Part of the basement to Oaklands Basin. Appears to have been significantly displaced by fault(s).||||||
1525|Berrimal Granite|23165|5|Briefly described|Map legend||Devonian|||||||
1525|Berrimal Granite|23166|5|Briefly described|Map legend||Devonian|of Mount Cole Suite.||||||
1525|Berrimal Granite|23167|5|Briefly described|Map legend|Early Devonian|Early Devonian|of Mount Cole Suite. Granite, medium grained, biotite-hornblende intergrowths; intensely weathered.||||||27-OCT-04
1525|Berrimal Granite|23168|5|Briefly described|Map legend||Devonian|of Mount Cole Suite.||||||
1525|Berrimal Granite|23169|5|Briefly described|Map legend||Devonian|of Mount Cole Suite.||||||
1525|Berrimal Granite|23309|6|Mentioned|p424 App1|||G358. I-Type.||||||
1525|Berrimal Granite|23603|5|Briefly described|p21|||||||||14-MAY-13
1525|Berrimal Granite|23604|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
1525|Berrimal Granite|23605|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
1525|Berrimal Granite|23606|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
1525|Berrimal Granite|23607|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
1525|Berrimal Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
1525|Berrimal Granite|60452|4|Described|p51|||Of the Coonooer Suite.||||||
1525|Berrimal Granite|60461|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Coonooer Suite.  Granite: weathered outcrops of quartz and kaolinite retaining original igneous texture.||||||
1525|Berrimal Granite|60462|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Coonooer Suite. Granite: I-type, oxidised, moderately magnetic (to 60 nT); radiometric response dominated by Th response although the K response is also higher than the nearby bedrock, U response is low.||||||
1525|Berrimal Granite|60491|4|Described|p48|||Of the Coonooer Suite. I-type.||||||
1525|Berrimal Granite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Coonooer Suite. Granite: very weathered.||||||
1525|Berrimal Granite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of the Coonooer Suite. Granite; oxidised I-type: moderately magnetic; gravity low; radiometric response shows low K, high Th, moderate U||||||30-SEP-04
1525|Berrimal Granite|66002|5|Briefly described|p6 Tb.5|||Of Coonooer Suite. G358. Defined in Marlow and Bushell 1995, p21.||||||
1525|Berrimal Granite|68116|5|Briefly described|Appendix, Maps 16, 23.|Middle Devonian|Early Devonian||||||Biotite-hornblende granite: medium grained, biotite-hornblende intergrowths: I-type; weakly magnetic; intensely weathered to relict quartz grains in a kaolinite matrix.|
37871|Berringama Granodiorite|24133|3|Fully described|p65|Silurian|Silurian|I-type granodiorite.  Geological Province: Lachlan Fold Belt.||||||
37871|Berringama Granodiorite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37871|Berringama Granodiorite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37871|Berringama Granodiorite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37871|Berringama Granodiorite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt||||||
37871|Berringama Granodiorite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37871|Berringama Granodiorite|68116|5|Briefly described|Appendix, Map 20.|Pridoli|Wenlock||||||Biotite granodiorite: dark grey, medium grained; equigranular, mainly weakly to moderately foliated; I-type; nonmagnetic.|
21238|Berrmarr Subgroup|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Snowy River Volcanics||||||
21238|Berrmarr Subgroup|23309|4|Described|p106,115,110. Tb2.40|||of Snowy River Volcanics.||||||
21238|Berrmarr Subgroup|23615|4|Described|p23, p101|Early Devonian|Early Devonian|Of Snowy River Volcanics.  Overlain by Little River Subgroup. Parts previously included in Ringwood's (1955a,b) Black Mountain Rhyodacite.  Composed of two major formations; Ballantyne Megabreccia and Black Mountain Ignimbrite. Age: Early Devonian ~410-395Ma.||||||16-AUG-18
21238|Berrmarr Subgroup|24551|4|Described|p143, p141 Fig.  5.32|||Of Snowy River Volcanics.||||||
21238|Berrmarr Subgroup|43206|5|Briefly described|map legend||Ludlow|Of Snowy River Volcanics||||||
21238|Berrmarr Subgroup|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Unit in Snowy River Volcanics.|||Extrusive, fluvial: felsic ignimbrite, megabreccia, minor rhyolite lava.|
30290|Besford Ignimbrite|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
30290|Besford Ignimbrite|23309|5|Briefly described|p123, 125, 126. Tb1.2/2.48||| Age: U/Pb 400+/-9Ma.||||||
30290|Besford Ignimbrite|24551|5|Briefly described|p118 Fig. 5.1|Devonian|Devonian|||||||
30290|Besford Ignimbrite|60503|3|Fully described|p128, p21 Fig. 4|Early Devonian|Early Devonian|Coarse-grained red quartz-biotite ignimbrite; abundant biotite. Uncon. overlies Pinnak S'stone, Bendoc Group and Toaks Creek Conglom; also overlies Warbisco Shale. Age: 400+/-7Ma;  Max. thickness: >500m. Geol. Prov: Cravensville Igneous Province.||||||16-NOV-09
30290|Besford Ignimbrite|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Ignimbrite: rhyolitic quartz ignimbrite, red, crystal-rich, with large quartz and feldspar phenocrysts and minor biotite in a welded groundmass.||||||
30290|Besford Ignimbrite|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Ignimbrite: rhyolitic quartz ignimbrite, red, crystal-rich, with large quartz and feldspar phenocrysts and minor biotite in a welded groundmass.||||||
30290|Besford Ignimbrite|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Ignimbrite: rhyolitic quartz ignimbrite, red, crystal-rich, with large quartz and feldspar phenocrysts and minor biotite in a welded groundmass.||||||
30290|Besford Ignimbrite|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Ignimbrite: rhyolitic quartz ignimbrite, red, crystal-rich, with large quartz and feldspar phenocrysts and minor biotite in a welded groundmass.||||||
30290|Besford Ignimbrite|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Dartella Volcanic Group. Ignimbrite: moderately magnetic (100 nT) complicated by Morass Creek Basalt in the west; moderate to high total count, high K except along ridge, moderate Th, U.||||||
30290|Besford Ignimbrite|68115|5|Briefly described|p5.|Devonian|Devonian|A unit within the (now superseded) Besford caldera (VandenBerg et al. 1998a).||Unit in Garden Creek Igneous Complex?||||11-FEB-13
30290|Besford Ignimbrite|68116|5|Briefly described|Appendix, Map 27.|Emsian|Emsian||||||Rhyolitic quartz ignimbrite: red, crystal-rich, with large quartz and feldspar phenocrysts and minor biotite in a welded groundmass.|
1539|Bete Bolong Granodiorite|23309|6|Mentioned|p424 App 1.|||(G57) - supersedes Bete Bolong Granite.||||||
1539|Bete Bolong Granodiorite|23938|6|Mentioned|p101|Early Devonian|Early Devonian|See also Bette Bolong Granodiorite.||||||25-SEP-08
1539|Bete Bolong Granodiorite|38367|5|Briefly described|Table 3, p95|||Comprises two elongated hornblende granodiorite plutons.||||||16-DEC-08
1539|Bete Bolong Granodiorite|44185|5|Briefly described|Map legend.|||I-type. Age uncertain: shown as SDg, ie Silurian-Devonian.||||||
1539|Bete Bolong Granodiorite|60542|5|Briefly described|p19 Fig. 3|Late Silurian|Late Silurian|Intrusive. See also Bete Bolong Granite - names used interchangeably. See also p23 Tb. 2, p26.||||||
1539|Bete Bolong Granodiorite|68116|5|Briefly described|Appendix.|Devonian|Silurian||||||Hornblende granodiorite: grey-green, medium to coarse-grained; I-type.|
1540|Bete Bolong Suite|23309|5|Briefly described|p345|||||||||
1540|Bete Bolong Suite|24551|6|Mentioned|p235|||Of the Kuark Province||||||
1540|Bete Bolong Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
1540|Bete Bolong Suite|42827|6|Mentioned|p431|||||||||
1540|Bete Bolong Suite|43312|5|Briefly described|Map Legend||Wenlock|||||||
1540|Bete Bolong Suite|43313|5|Briefly described|Map Legend||Wenlock|||||||
1540|Bete Bolong Suite|43314|5|Briefly described|Map Legend||Wenlock|||||||
1540|Bete Bolong Suite|43315|5|Briefly described|Map Legend||Wenlock|IncludesDysentery Tonalite, Feltis Farm Tonalite and Orbost Trondhjemite.||||||03-MAY-05
1540|Bete Bolong Suite|60541|5|Briefly described|p62|||Contains plutons Dysentery, Cooney Ridge and part of Feltis Farm on MURRUNGOWAR. Prominent on ORBOST. Geological Province: Lachlan Fold Belt.||||||12-JAN-06
1540|Bete Bolong Suite|60542|5|Briefly described|p44, p87, p90, p91|||All the granites of this suite have intruded the Lower Ordovician Pinnak Sandstone. ||||||
37798|Bethanga Gneissic Granite|23309|6|Mentioned|p448 Appendix 1|||Obsolete granite name.||||||
37798|Bethanga Gneissic Granite|68115|5|Briefly described|p7.|||Omeo Zone. Shown as granite by Keay et al. (1999), so has been re-named Bethanga Gneissic Granite accordingly. G175.||||||07-DEC-21
37798|Bethanga Gneissic Granite|68116|5|Briefly described|Appendix, Map 20.|Pridoli|Ludlow||||||Coarse-grained, well-foliated, heterogeneous cordierite-garnet granite: quartz, perthitic K-feldspar, plagioclase, reddish-brown biotite, muscovite, cordierite, and garnet, and accessory zircon, apatite, ilmenite and sillimanite; enclaves common.|
37798|Bethanga Gneissic Granite|70777|5|Briefly described|p2, p63, p81|Lochkovian|Pridoli|Lachlan Orogen. U-Pb zircon SHRIMP age.|419.9 +/- 3.4 Ma (Keay et al., 1999)|||||
77281|Bethgarno Amphibolite|68115|5|Briefly described|p4.|Silurian|Silurian|Formerly Bethgarno Gneiss (O'Shea 1976, 1979); called Spring Creek Amphibolite by Steele (1979) and Bolger (1984). Name is now changed to distinguish it from other gneisses in the region which are all quartzofeldspathic. The name Bethgarno has precedence.||||||
77281|Bethgarno Amphibolite|68116|5|Briefly described|Appendix, Map 20.|Llandovery|Early Ordovician||||||Finely banded amphibolite gneiss with hornblende-, biotite-, and quartz-feldspar-rich layers; contains hornblende, biotite, plagioclase, quartz and minor K-feldspar, and cummingtonite-quartz-plagioclase layers; variably foliated with mylonitic bands.|
1549|Betka Granodiorite|23309|6|Mentioned|p424, App1|||G8. Supersedes Betka Granite.||||||
1549|Betka Granodiorite|41850|6|Mentioned|p430|||||||||
1549|Betka Granodiorite|42827|5|Briefly described|p430|||Coarse, uneven-grained, large K-feldspars commonly rimmed with albite and appreciable amount of hornblende||||||30-NOV-04
1549|Betka Granodiorite|68116|5|Briefly described|Appendix, Map 46.|Early Devonian|Early Devonian||||||Biotite-hornblende granodiorite: coarse grained with large pink K-feldspars occasionally mantled by plagioclase; accessory sphene; I-type.|
31529|Betka Suite|24551|6|Mentioned|p235|||||||||
31529|Betka Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
1591|Big Hill Quartz Diorite|23309|5|Briefly described|p424, App1|||G152. Supersedes Blue Gums Tonalite. Age: K/Ar Biotite 398 +/- 2 Ma.||||||
1591|Big Hill Quartz Diorite|29711|6|Mentioned|Table 1|||||||||
1591|Big Hill Quartz Diorite|31800|5|Briefly described|p210|||||||||
1591|Big Hill Quartz Diorite|35278|5|Briefly described|p357|||||||||
1591|Big Hill Quartz Diorite|39860|4|Described|p19|||Age: 397 +/- 11 Ma (K/Ar). Consists of quartz, plagioclase, biotite and abundant hornblende.||||||30-NOV-04
1591|Big Hill Quartz Diorite|42089|6|Mentioned|p19|||||||||
1591|Big Hill Quartz Diorite|42791|5|Briefly described|p209, Fig.2 p206|||||||||
1591|Big Hill Quartz Diorite|42835|6|Mentioned|p249|||||||||
1591|Big Hill Quartz Diorite|42836|5|Briefly described|p252|||||||||
1591|Big Hill Quartz Diorite|43220|6|Mentioned|p11||Devonian|||||||
1591|Big Hill Quartz Diorite|44184|5|Briefly described|Map Legend||Early Devonian|||||||
1591|Big Hill Quartz Diorite|61160|3|Fully described|p76, p30 Tb. 5.2, p18|Early Devonian|Early Devonian|Assigned to Big Hill Suite. Hornblende-biotite quartz diorite; dark grey, with speckled appearance. Intrudes Cobungra Granite and migmatite, gneiss and leucogranite of Omeo Metamorphic Complex. Age: 401+/-16Ma (K-Ar). ||||||
1591|Big Hill Quartz Diorite|61161|5|Briefly described|p67|Early Devonian|Early Devonian|Age: 395 +- 16 Ma.||||||
1591|Big Hill Quartz Diorite|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Big Hill Suite. GSV map code: G152. Two unnamed phases: Hornblende-biotite quartz diorite: grey, coarse grained, equigranular, I-type intrusion, GSV map code: G152a; Biotite tonalite: grey, medium grained, equigranular, GSV map code: G152b.||||||28-SEP-05
1591|Big Hill Quartz Diorite|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Big Hill Suite. GSV map code: G152. Two unnamed phases: Hornblende-biotite quartz diorite: grey, coarse grained, equigranular, I-type intrusion, GSV map code: G152a; Biotite tonalite: grey, medium grained, equigranular, GSV map code: G152b.||||||28-SEP-05
1591|Big Hill Quartz Diorite|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Big Hill Suite. GSV map code: G152. Two unnamed phases: Hornblende-biotite quartz diorite: grey, coarse grained, equigranular, I-type intrusion, GSV map code: G152a; Biotite tonalite: grey, medium grained, equigranular, GSV map code: G152b.||||||28-SEP-05
1591|Big Hill Quartz Diorite|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Big Hill Suite. GSV map code: G152. Two unnamed phases: Hornblende-biotite quartz diorite: grey, coarse grained, equigranular, I-type intrusion, GSV map code: G152a; Biotite tonalite: grey, medium grained, equigranular, GSV map code: G152b.||||||07-FEB-11
1591|Big Hill Quartz Diorite|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Big Hill Suite. Two unnamed phases: hornblende-biotite quartz diorite: I-type, 395 +/- 8 Ma: K/Ar biotite, 401 +/- 16 Ma: K/Ar hornblende; highly magnetic; GSV map code: G152a; and, biotite tonalite: moderately magnetic; GSV map code: G152b.||||||05-OCT-05
1591|Big Hill Quartz Diorite|68116|5|Briefly described|Appendix, Map 27.|Early Devonian|Early Devonian||||||Hornblende-biotite quartz diorite: grey; coarse grained; equigranular; I-type; biotite tonalite; grey, medium grained; equigranular.|
1591|Big Hill Quartz Diorite|70910|4|Described|p49|||||||||
69708|Big Hill Suite|61160|4|Described|p76, p58-59 Fig. 6.8|Early Devonian|Early Devonian|Formerly called the Big Hill Series by Fagan (1979). Contains just one pluton, the Big Hill Quartz Monzodiorite. I-type granite. ||||||
69708|Big Hill Suite|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Big Hill Quartz Diorite.||||||
69708|Big Hill Suite|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Big Hill Quartz Diorite.||||||
69708|Big Hill Suite|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Big Hill Quartz Diorite.||||||
69708|Big Hill Suite|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Big Hill Quartz Diorite.||||||07-FEB-11
69708|Big Hill Suite|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Big Hill Quartz Diorite.||||||
1603|Big Valley Granodiorite|24551|6|Mentioned|p229|||Of the Tabberabbera Province. Low initial Sr ratios suggest affinities with Murmungee Granodiorite.||||||27-NOV-09
1603|Big Valley Granodiorite|42154|6|Mentioned|Table 1 p334|||||||||27-NOV-09
21254|Bimmarn Ignimbrite|23309|4|Described|p110 Table 2.40|||Maximum Thickness: 50m.  Of the Mount Dawson Subgroup.||||||
21254|Bimmarn Ignimbrite|23615|3|Fully described|p106|Early Devonian|Early Devonian|Of Mount Dawson Subgroup.  Overlain by Plumb Gully Ignimbrite, underlain by Doyle Gully Ignimbrite.||||||
21254|Bimmarn Ignimbrite|43206|5|Briefly described|map legend||Ludlow|Of Mount Dawson Subgroup.||||||
21254|Bimmarn Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Feldspar ignimbrite: dark with white euhedral feldspar phenocrysts.|
37525|Bindaree Formation|23309|4|Described| p160,175,182|Late Devonian|Late Devonian|Of the Wellington Volcanics. Maximum thickness ~700m.||||||21-FEB-13
37525|Bindaree Formation|24551|4|Described|p174||Late Devonian|Of the Wellington Volcanic Group.  Maximum Thickness: 700m.  Overlain by: Howitt Spur Formation ).||||||
37525|Bindaree Formation|66252|2|Defined|p209, p211 Fig.1, p212 Fig.2, p213 Fig.3|Frasnian|Frasnian|See also p214, p215-217 Figs.5-7, p219-225, p228-231. New name. Definition data given. Central Macalister Synclinorium. Unit in Avon River Group. Comprises three informal members : Boulder Conglomerate Unit (conglomerate, sandstone); Green Mudstone Unit (laminated green mudstone, siltstone, fine sandstone); Black Shale Unit (black shale, green mudstone). Thickness highly variable. Corresponds to Rose River Volcanics and Refrigerator Gap Dacite. Is overlain by Howitt Spur Formation. Detailed stratigraphic section and petrographic description.||||||
37525|Bindaree Formation|68115|6|Mentioned|p8.|||Tabberabbera Zone, near Mount Buller.||||||
37525|Bindaree Formation|68116|5|Briefly described|Appendix, Map 34.|Late Devonian|Late Devonian||||||Boulder conglomerate, green mudstone, black shale.|
26393|Bindi Granodiorite|22968|4|Described|P32, Table7, P173||Early Devonian|Intruded Pinnak Sandstone, surrounded by Cobungra Granite. Age of unit: 400+/-6 Ma. Of the Bullenbalong Supersuite.||||||08-MAR-07
26393|Bindi Granodiorite|23021|5|Briefly described|Map legend|Wenlock|Wenlock|Of the Bullenbalong Suite.||||||08-MAR-07
26393|Bindi Granodiorite|23029|5|Briefly described|Map legend|Wenlock|Wenlock|Of the Bullenbalong Suite. Biotite granodiorite and granite: S-type; pale grey, medium grained, massive; small biotite-rich enclaves common, enclaves of gneiss locally abundant.||||||08-MAR-07
26393|Bindi Granodiorite|23030|5|Briefly described|Map legend|Silurian|Silurian|Of the Bullenbalong Supersuite.  G121a: biotite granodiorite and granite: S-type; 400+/-6 Ma (K/Ar); nonmagnetic; moderate K, moderate to high Th, U. G121b: granite and leucogranite: nonmagnetic; high K, low Th, moderate U.||||||08-MAR-07
26393|Bindi Granodiorite|23309|5|Briefly described|p308,338.|Early Devonian|Early Devonian|G121. Supersedes Bindi Granite. Age:400+/-6Ma.  Of Cooma Supersuite?||||||
26393|Bindi Granodiorite|38145|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
26393|Bindi Granodiorite|38367|6|Mentioned|Fig.9|||||||||
26393|Bindi Granodiorite|39447|4|Described|p17|||||||||
26393|Bindi Granodiorite|42791|6|Mentioned|p215|||||||||
26393|Bindi Granodiorite|44185|5|Briefly described|Map legend.|Silurian|Silurian|S-type.||||||
26393|Bindi Granodiorite|60503|6|Mentioned|p48|||Juxtaposed against Early Devonian Buchan Group by the Bindi Fault.||||||07-SEP-05
26393|Bindi Granodiorite|68116|5|Briefly described|Appendix, Map 35.|Wenlock|Llandovery||||||Biotite granodiorite, granite: pale grey; medium-grained; massive; small biotite-rich enclaves common; enclaves of gneiss locally abundant.|
34834|Bingo Munjie Quartz Diorite|22968|5|Briefly described|P40, Table7, P210||Late Silurian|Age of unit is 417+/-17 Ma, intruded by Anglers Rest Granite, highly magnetic, parent is Bingo Munjie Suite||||||
34834|Bingo Munjie Quartz Diorite|23029|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is the Bingo Munjie Suite||||||
34834|Bingo Munjie Quartz Diorite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Bingo Munjie Suite||||||
34834|Bingo Munjie Quartz Diorite|23309|6|Mentioned|p425 App 1|||(G81) Supersedes Bingo Munjie Granite. Age: 417 +/- 7 Ma.||||||
34834|Bingo Munjie Quartz Diorite|60503|4|Described|p164, p43 Tb.2|Early Devonian|Early Devonian|Of the Bingo Munjie Suite (Boggy Plain Supersuite). Abundant lath-like plagioclase crystals with large crystals of hornblende and rarer biotite. Overlain by the Eight Mile Loop Rhyolite. Intruded by Anglers Rest Granite at northern end. ||||||
34834|Bingo Munjie Quartz Diorite|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Hornblende-biotite quartz diorite: I-type; medium grained, dark green; epidote alteration and mafic enclaves common.||||||
34834|Bingo Munjie Quartz Diorite|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Boggie Plain Supersuite. Hornblende-biotite quartz diorite: I-type; medium grained, dark green; epidote alteration and mafic enclaves common.||||||
34834|Bingo Munjie Quartz Diorite|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Hornblende-biotite quartz diorite: I-type; medium grained, dark green; epidote alteration and mafic enclaves common.||||||
34834|Bingo Munjie Quartz Diorite|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Boggie Plain Supersuite. Hornblende-biotite quartz diorite: I-type; medium grained, dark green; epidote alteration and mafic enclaves common.||||||07-OCT-04
34834|Bingo Munjie Quartz Diorite|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Bingo Munjie Suite. Hornblende-biotite quartz diorite: I-type; 417+/-7 Ma (U/Pb zircon); thin north trending non- and intensely (~1000 nT) magnetic sheets; low to moderate Th, low total count K, U||||||
34834|Bingo Munjie Quartz Diorite|68116|5|Briefly described|Appendix, Maps 27, 35.|Pragian|Ludlow||||||Hornblende-biotite quartz diorite: medium grained; dark green; epidote alteration; mafic enclaves common.|
34913|Bingo Munjie Suite|22968|5|Briefly described|P210||Late Silurian|Contains the Bingo Munjie Quartz Diorite, Post Office Granite and Charlestown Quartz Diorite, parent is Boggy Plain Supersuite||||||
34913|Bingo Munjie Suite|23021|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is Boggy Plain Supersuite||||||
34913|Bingo Munjie Suite|23029|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is Boggy Plain Supersuite||||||
34913|Bingo Munjie Suite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Boggy Plain Supersuite||||||
34913|Bingo Munjie Suite|23309|5|Briefly described|p344|||Of Boggy Plains Supersuite.  Consists of Bingo Munjie Quartz Diorite, Charlestown Creek Tonalite and Post Office Granite.||||||
34913|Bingo Munjie Suite|24551|6|Mentioned|p233|||||||||
34913|Bingo Munjie Suite|60503|4|Described|p159|||Of the Boggy Plains Supersuite. Includes Bingo Munjie Quartz Diorite and Charlestown Quartz Diorite.||||||01-SEP-05
34913|Bingo Munjie Suite|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Boggy Plains Supersuite. Includes: Post Office Granite, Charlestown Creek Quartz Diorite, Bingo Munjie Quartz Diorite.||||||08-NOV-04
1712|Bird Rock Member|23309|5|Briefly described|p54|||Of the Waratah Limestone.||||||
1712|Bird Rock Member|24551|5|Briefly described|p100|Early Ordovician|Early Ordovician|Of the Digger Island Marlstone.  Previously included as part of the Waratah Limestone||||||
1712|Bird Rock Member|30570|6|Mentioned|p4|||||||||
1712|Bird Rock Member|32583|6|Mentioned|p379|||Mb. of Waratah Limestone||||||
1712|Bird Rock Member|34926|6|Mentioned|p120|||||||||
1712|Bird Rock Member|34954|5|Briefly described|p194|||||||||
1712|Bird Rock Member|35274|5|Briefly described|p421|||||||||
1712|Bird Rock Member|41868|5|Briefly described|p575|||||||||
1712|Bird Rock Member|42577|5|Briefly described|p31|||Name abandoned? Synonym for "Lower Grinder Member"?||||||
1712|Bird Rock Member|42635|5|Briefly described|p24, 26|||||||||
1712|Bird Rock Member|42827|5|Briefly described|p575|||||||||
1712|Bird Rock Member|43530|14|Not recorded|p1029|||Part of Bell Point Limestone||||||
1712|Bird Rock Member|43537|14|Not recorded|p7||Siegenian|Member of Waratah Limestone||||||
1712|Bird Rock Member|61181|5|Briefly described|p69, p127|Early Devonian|Early Devonian|Lowermost member of the Waratah Limestone. Includes well bedded greyish brown dolomitic limestone and dolomite - generally fossiliferous. ||||||
1802|Black Mountain Ignimbrite|23309|4|Described|p110, 115, 123, Table 2.40|||Maximum Thickness: 750m.  Of the Berrmarr Subgroup.||||||
1802|Black Mountain Ignimbrite|23615|3|Fully described|p23, p102-104, 101|Early Devonian|Early Devonian|Replaces Black Mt. Rhyodacite. Of Berrmarr Subgp. Max. thick:600m.  Age:410-395Ma. Overlies Ballantyne Megabreccia, Wombargo Subgp.and pockets of Statham Ignim. in the northwest. In places overlain by Gelantipy Ignim. and patches of Wulgulmerang Ashstone.||||||10-SEP-18
1802|Black Mountain Ignimbrite|24551|5|Briefly described|p143|||Of the Berrmarr Subgroup||||||
1802|Black Mountain Ignimbrite|41585|5|Briefly described|p136|||||||||
1802|Black Mountain Ignimbrite|42827|5|Briefly described|p136|||||||||
1802|Black Mountain Ignimbrite|43206|5|Briefly described|map legend||Ludlow|Of Berrmarr Subgroup.||||||
1802|Black Mountain Ignimbrite|60542|6|Mentioned|p50|Early Devonian|Early Devonian|Name favoured over Black Mountain Rhyodacite in this study.||||||
1802|Black Mountain Ignimbrite|68116|5|Briefly described|Appendix, Maps 28, 36.|Pragian|Pragian||||||Quartz-feldspar ignimbrite: granular with large phenocrysts and abundant lithic clasts.|
28217|Black Range Granodiorite|22882|5|Briefly described|p 13||Devonian|||||||
28217|Black Range Granodiorite|22885|5|Briefly described|map|||||||||
28217|Black Range Granodiorite|22886|4|Described|Table.1|||||||||
28217|Black Range Granodiorite|23309|5|Briefly described|p165, 347, 350, 351.||Late Devonian|(G223) Intrudes both the Murrindindi Granodiorite and Archeron Cauldron Volcanics.||||||25-SEP-08
28217|Black Range Granodiorite|23938|6|Mentioned|p118|Late Devonian|Late Devonian|See also p124 Fig. 59.||||||25-SEP-08
28217|Black Range Granodiorite|32074|6|Mentioned|p186|||||||||
28217|Black Range Granodiorite|33607|6|Mentioned|Map legend|Devonian|Devonian|Porphyritic granite; porphyritic granodiorite; medium-grained granodiorite; porphyritic microgranodiorite.||||||29-NOV-04
28217|Black Range Granodiorite|40725|6|Mentioned|Fig.1|||||||||
28217|Black Range Granodiorite|44187|5|Briefly described|Map Legend||Late Devonian|G223 Unassigned.||||||
28217|Black Range Granodiorite|44197|5|Briefly described|Map Legend||Late Devonian|G223 Unassigned.||||||
28217|Black Range Granodiorite|68116|5|Briefly described|Appendix, Maps 33, 42.|Late Devonian|Late Devonian||||||Biotite granodiorite: generally porphyritic, biotite-bearing with occasional almandine, hypersthene and sillimanite; minor porphyritic microgranodiorite, aplite and pegmatite; S-type.|
28217|Black Range Granodiorite|70629|6|Mentioned|p986, p1000|||Melbourne Zone. Has a similar major element composition as the nearby Mo- and W-bearing granitic intrusions at Monkey Gully.||||||
83839|Black Range greenstone|73118|6|Mentioned|p14, 19|||Glenelg Zone, Western Victoria. Hosts VHMS style gold and base metal mineralisation.|||||Basaltic to andesitic meta-volcanics; greenschist facies and moderately to highly deformed.|
21264|Black Satin Ignimbrite|23309|4|Described|p110 Table 2.40|||Maximum Thickness: 500m.  Of the Marroo Subgroup.||||||
21264|Black Satin Ignimbrite|23615|3|Fully described|p100|Early Devonian|Early Devonian|Of Maroo Subgroup. Maximum thickness: 500m. Oldest unit in the Snowy River Volcanics. Unconformably overlain by the Little River Subgroup. Granular, brown to dark green quartz-feldspar ignimbrite with strongly welded vitricastic matrix.||||||
21264|Black Satin Ignimbrite|23938|6|Mentioned|p54 Tb. 4|||Of the Snowy River Volcanics?? See also p63-65 Figs. 23-24.||||||25-SEP-08
21264|Black Satin Ignimbrite|43206|5|Briefly described|map legend||Ludlow|Of Marroo Subgroup||||||
21264|Black Satin Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Quartz-feldspar ignimbrite: large phenocrysts, minor hornblende.|
34889|Blackfellows Flat Conglomerate|22968|4|Described|p122, p124, 128-130|Late Silurian|Late Silurian|Formalised unit, nonmagnetic unit, parent is Mount Tambo Group, maximum thickness is 1400m. Age 416+/-5 Ma from basal Vitric Ignimbrite Member.||||||10-SEP-18
34889|Blackfellows Flat Conglomerate|23021|5|Briefly described|Map legend|Ludlow|Ludlow|Parent is Mount Tambo Group, overlying unit is Shanahan Sandstone, underlying unit is Berrawan Conglomerate||||||
34889|Blackfellows Flat Conglomerate|23030|5|Briefly described|Map legend|Late Silurian|Late Silurian|Parent is the Mount Tambo Group||||||
34889|Blackfellows Flat Conglomerate|23309|5|Briefly described|p103, 126, 129.|||||||||
34889|Blackfellows Flat Conglomerate|24551|4|Described|p140|||Of the Mount Tambo Group.||||||
34889|Blackfellows Flat Conglomerate|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Mount Tambo Group. Fluvial sediments: conglomerate, sandstone, mudstone||||||
34889|Blackfellows Flat Conglomerate|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Mount Tambo Group. Fluvial sediments: conglomerate, sandstone, mudstone||||||
34889|Blackfellows Flat Conglomerate|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Mount Tambo Group. Fluvial sediments: conglomerate, sandstone, mudstone||||||
34889|Blackfellows Flat Conglomerate|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Mount Tambo Group. Fluvial sediments: conglomerate, sandstone, mudstone||||||
34889|Blackfellows Flat Conglomerate|68116|5|Briefly described|Appendix, Maps 27, 35.|Pragian|Ludlow||||||Conglomerate, sandstone, pebbly sandstone, mudstone: clasts well rounded, sandstones with high felsic volcanic component. Formation fines upward.|
1872|Blackwatch Volcaniclastic Member|22876|6|Mentioned|p22|||||||||
1872|Blackwatch Volcaniclastic Member|23309|5|Briefly described|p106 Table 2.39|||||||||
1872|Blackwatch Volcaniclastic Member|24551|5|Briefly described|p148|||Of Bungywarr Formation.||||||
1872|Blackwatch Volcaniclastic Member|41585|5|Briefly described|p140|||||||||
1872|Blackwatch Volcaniclastic Member|42577|6|Mentioned|p29|||||||||
1872|Blackwatch Volcaniclastic Member|42627|5|Briefly described|Map legend|Emsian|Pragian|||||||
1872|Blackwatch Volcaniclastic Member|42647|3|Fully described|p30||Pragian|Supersedes Blackwatch Volcanics, Blackwatch Transition Formation. Member of Bungywarr Formation.||||||
41183|Blair Atholl Granite|50154|2|Defined|p75, p80, p248 App. 5|Cambrian|Cambrian|Of the Glenelg Metamorphic Complex. Corresponds to part of the Wando Granodiorite of Wells (1956). Intrudes the Snake River Tonalite and the Brimboal Granodiorite.||||||15-SEP-04
41183|Blair Atholl Granite|50156|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite granite.||||||20-AUG-04
41183|Blair Atholl Granite|50157|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite granite.||||||20-AUG-04
41183|Blair Atholl Granite|50158|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite granite.||||||20-AUG-04
41183|Blair Atholl Granite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite granite.||||||20-AUG-04
41183|Blair Atholl Granite|50160|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite granite.||||||20-AUG-04
41183|Blair Atholl Granite|50161|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite granite.||||||20-AUG-04
41183|Blair Atholl Granite|50162|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite granite.||||||20-AUG-04
41183|Blair Atholl Granite|50163|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite granite.||||||20-AUG-04
41183|Blair Atholl Granite|50164|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Biotite-muscovite granite.||||||20-AUG-04
41183|Blair Atholl Granite|66002|6|Mentioned|p9 Tb.5|||G439. Defined by Kemp et al. 2002||||||
41183|Blair Atholl Granite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Biotite-muscovite granite: foliated, pale tan, coarse grained leucocratic, equigranular; accessory garnet; rare biotite-rich microgranitoid enclaves; enclaves of migmatite and biotite-rich schlieren common near southern margin; magnetic.|
1918|Blanchetown Clay|2967|5|Briefly described|p14, 48-53, 74, 155, 159, 166, 169, 205|Pleistocene|Pliocene|Firman (1965). Western Murray Basin. Up to 34m thick. See also p207, 280, 283, 285, 304, 318, 322, 327, 331, 333-334.||||Is separated from the underlying Parilla Sand by the Karoonda Surface. Is overlain locally by Tyrrell Beds.|Lacustrine sequence of olive-grey clay, silt and minor interbedded fine sand.|
1918|Blanchetown Clay|10010|5|Briefly described|p12 Fig. 3, p16|Pleistocene|Pleistocene|Fine-grained lacustrine deposits of Lake Bungunnia. Geological Province: Murray Basin.||||||13-AUG-07
1918|Blanchetown Clay|22773|5|Briefly described|Fig24.8p352|Early Pleistocene|Late Pliocene|||||||
1918|Blanchetown Clay|22799|2|Defined|p39|Late Pliocene|Late Pliocene|||||||
1918|Blanchetown Clay|22857|5|Briefly described|p352 Fig. 24.8|Early Pleistocene|Late Pliocene|Geological Province: Murray Basin.||||||
1918|Blanchetown Clay|22887|5|Briefly described|Fig.6 p13||Late Pliocene|||||||
1918|Blanchetown Clay|22893|3|Fully described|p52 table3||Pleistocene|Generally 2-5m thick, up to 20m.||||||
1918|Blanchetown Clay|22941|6|Mentioned|p289|||||||||
1918|Blanchetown Clay|23089|5|Briefly described|p649|||||||||
1918|Blanchetown Clay|23560|6|Mentioned|p165|||||||||
1918|Blanchetown Clay|23818|5|Briefly described|p210, p212 Fig.108|Middle Pleistocene|Early Pleistocene|Geological Province: Murray Basin.||||||
1918|Blanchetown Clay|23884|6|Mentioned|p153|||Geological Province: Murray Basin||||||
1918|Blanchetown Clay|24043|5|Briefly described|p525|||||||||
1918|Blanchetown Clay|24465|5|Briefly described|p351 Fig.1|Quaternary|Quaternary|||||||
1918|Blanchetown Clay|24566|5|Briefly described|p114|Pliocene|Pliocene|||||||
1918|Blanchetown Clay|24574|6|Mentioned|p706|||Geological Province: Murray Basin||||||
1918|Blanchetown Clay|29591|6|Mentioned|Table 20|||||||||
1918|Blanchetown Clay|29697|5|Briefly described|Table 1|||||||||
1918|Blanchetown Clay|30145|6|Mentioned|p183|||||||||
1918|Blanchetown Clay|30750|6|Mentioned|p1|||Pleistocene age||||||
1918|Blanchetown Clay|30751|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
1918|Blanchetown Clay|30753|4|Described|p15|||Lower Pleistocene age||||||
1918|Blanchetown Clay|30754|2|Defined|Appendix 1|early Pleistocene|early Pleistocene|See also P22,23,31,41,42||||||
1918|Blanchetown Clay|30755|6|Mentioned|p169|||Tectonic map.||||||
1918|Blanchetown Clay|30758|6|Mentioned|p66|||Stratigraphy||||||
1918|Blanchetown Clay|30807|6|Mentioned|p101|||Suggested map symbol.||||||
1918|Blanchetown Clay|30935|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
1918|Blanchetown Clay|30994|6|Mentioned|Fig. 1|||||||||
1918|Blanchetown Clay|30996|3|Fully described|p32|||Contains dolomite & limestone members.||||||03-FEB-09
1918|Blanchetown Clay|31240|5|Briefly described|p64|||Pleistocene||||||
1918|Blanchetown Clay|31319|5|Briefly described|p157|||Pleistocene||||||
1918|Blanchetown Clay|31345|6|Mentioned|p294|||||||||
1918|Blanchetown Clay|31554|6|Mentioned|p14|||||||||
1918|Blanchetown Clay|31741|6|Mentioned|p6|||||||||
1918|Blanchetown Clay|31745|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
1918|Blanchetown Clay|32007|4|Described|p159|||Palaeontology fully discussed||||||
1918|Blanchetown Clay|32099|6|Mentioned|p229|||||||||
1918|Blanchetown Clay|32323|6|Mentioned|p9|||Pleistocene||||||
1918|Blanchetown Clay|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
1918|Blanchetown Clay|32432|6|Mentioned|Fig.2|||See also Table 1||||||
1918|Blanchetown Clay|32433|6|Mentioned|p80|||See also Table 2||||||
1918|Blanchetown Clay|32439|6|Mentioned|p99|||||||||
1918|Blanchetown Clay|32861|5|Briefly described|Table 1|||Lithology||||||
1918|Blanchetown Clay|32862|5|Briefly described|Table 3|||Pleistocene||||||
1918|Blanchetown Clay|32864|6|Mentioned|Fig. 5|||||||||
1918|Blanchetown Clay|33048|6|Mentioned|p195|||See also P196||||||
1918|Blanchetown Clay|33051|6|Mentioned|p187|||||||||
1918|Blanchetown Clay|33725|6|Mentioned|p10|||Small sinkholes.||||||
1918|Blanchetown Clay|33826|6|Mentioned|p42|||Strat. table||||||
1918|Blanchetown Clay|34069|6|Mentioned|p1|||See also Fig.2. Pleist.||||||
1918|Blanchetown Clay|34114|4|Described|p50|||Pleistocene||||||
1918|Blanchetown Clay|34180|6|Mentioned|p212|||Lower - Middle Pleistocene.||||||
1918|Blanchetown Clay|34459|4|Described|p11|||||||||
1918|Blanchetown Clay|34460|4|Described|p164|||Lithology. Table 2||||||
1918|Blanchetown Clay|34461|5|Briefly described|p49|||Pleistocene||||||
1918|Blanchetown Clay|34536|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
1918|Blanchetown Clay|34690|6|Mentioned|p1|||||||||
1918|Blanchetown Clay|34758|6|Mentioned|p27|||||||||
1918|Blanchetown Clay|34933|6|Mentioned|p58|||||||||
1918|Blanchetown Clay|35029|6|Mentioned|p166|||||||||
1918|Blanchetown Clay|35071|6|Mentioned|Fig.4|||||||||
1918|Blanchetown Clay|35097|6|Mentioned|Fig.4|||||||||
1918|Blanchetown Clay|35131|6|Mentioned|p8|||||||||
1918|Blanchetown Clay|35200|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
1918|Blanchetown Clay|35232|5|Briefly described|Table.4|||||||||
1918|Blanchetown Clay|35272|4|Described|p283|||||||||
1918|Blanchetown Clay|35541|6|Mentioned|p13|||||||||
1918|Blanchetown Clay|37619|6|Mentioned|p2|||||||||
1918|Blanchetown Clay|37661|6|Mentioned|p8.2.1|||||||||
1918|Blanchetown Clay|37796|6|Mentioned|p161|||||||||
1918|Blanchetown Clay|37873|4|Described|p2|||||||||
1918|Blanchetown Clay|38068|6|Mentioned|p76|||||||||
1918|Blanchetown Clay|38605|6|Mentioned|p30|||||||||
1918|Blanchetown Clay|39322|6|Mentioned|p404|||||||||
1918|Blanchetown Clay|39329|6|Mentioned|Fig.1|||||||||
1918|Blanchetown Clay|40003|6|Mentioned|Table 8|||||||||
1918|Blanchetown Clay|40215|6|Mentioned|p56|||||||||
1918|Blanchetown Clay|40380|6|Mentioned|p221|||||||||
1918|Blanchetown Clay|40597|6|Mentioned|Fig.3|||||||||
1918|Blanchetown Clay|40779|6|Mentioned|Fig.2|||||||||
1918|Blanchetown Clay|40820|5|Briefly described|p141|||||||||
1918|Blanchetown Clay|41206|5|Briefly described|p370|||||||||
1918|Blanchetown Clay|41478|5|Briefly described|Table 1|||||||||
1918|Blanchetown Clay|41537|6|Mentioned|p350|||||||||
1918|Blanchetown Clay|41848|4|Described|p358|||Includes Bungunnia Limestone and Irymple Member. Age: Pleistocene.||||||20-OCT-08
1918|Blanchetown Clay|41868|6|Mentioned|p552|||||||||
1918|Blanchetown Clay|42125|5|Briefly described|p139|||||||||
1918|Blanchetown Clay|42130|6|Mentioned|Fig.3 P265|||||||||
1918|Blanchetown Clay|42131|5|Briefly described|p287|||||||||
1918|Blanchetown Clay|42132|6|Mentioned|p295|||||||||
1918|Blanchetown Clay|42134|6|Mentioned|Fig.3 P335|||||||||
1918|Blanchetown Clay|42137|6|Mentioned|Fig.2 P368|||||||||
1918|Blanchetown Clay|42389|5|Briefly described|p71|||||||||
1918|Blanchetown Clay|42443|6|Mentioned|p4|||||||||
1918|Blanchetown Clay|42499|5|Briefly described|Map legend|Pleistocene|Pliocene|||||||
1918|Blanchetown Clay|42509|5|Briefly described|p2|||||||||
1918|Blanchetown Clay|42510|5|Briefly described|p35|||||||||
1918|Blanchetown Clay|42512|6|Mentioned|p68|||||||||
1918|Blanchetown Clay|42513|6|Mentioned|p98|(IV) A||||||||13-MAY-13
1918|Blanchetown Clay|42514|6|Mentioned|p116|||||||||
1918|Blanchetown Clay|42515|6|Mentioned|p134|||||||||
1918|Blanchetown Clay|42516|6|Mentioned|p152|||||||||
1918|Blanchetown Clay|42518|5|Briefly described|p185|||||||||
1918|Blanchetown Clay|42519|6|Mentioned|p205|||||||||
1918|Blanchetown Clay|42592|6|Mentioned|p280|||||||||
1918|Blanchetown Clay|42717|5|Briefly described|map legend|Pleistocene||||||||
1918|Blanchetown Clay|42720|5|Briefly described|map legend|Pleistocene|Pliocene|||||||
1918|Blanchetown Clay|42813|5|Briefly described|p25|||||||||
1918|Blanchetown Clay|42827|4|Described|p358|||||||||
1918|Blanchetown Clay|42867|6|Mentioned|p13|||||||||
1918|Blanchetown Clay|42881|4|Described|Fig.3, P84|||||||||
1918|Blanchetown Clay|42966|1|Redefined|p205|Early Pleistocene|Late Pliocene|||||||
1918|Blanchetown Clay|43052|5|Briefly described|Table 2.1|||||||||
1918|Blanchetown Clay|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Sandy clay. Overlain by Bungunnia Limestone.||||||25-MAY-05
1918|Blanchetown Clay|43073|5|Briefly described|p17,Table 4|||||||||
1918|Blanchetown Clay|43258|5|Briefly described|Map Legend|Pleistocene|Pliocene|||||||
1918|Blanchetown Clay|43298|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
1918|Blanchetown Clay|43655|5|Briefly described|p40-846|||||||||
1918|Blanchetown Clay|43669|4|Described|p8-9|||||||||
1918|Blanchetown Clay|43682|6|Mentioned|p289|||||||||
1918|Blanchetown Clay|43791|6|Mentioned|p372, Fig1|||||||||
1918|Blanchetown Clay|43804|6|Mentioned|Fig.2,p49|||||||||
1918|Blanchetown Clay|44133|5|Briefly described|p252|Middle Pleistocene|Late Pliocene|Interfingers with Chowilla Sand. Thickness: 20m. Geological Province: Murray Basin. ||||||
1918|Blanchetown Clay|44188|5|Briefly described|Map Legend|Pleistocene|Pliocene|Geological province: Murray Basin. Lacustrine deposits - poorly cosolidated to friable, well-laminated, green-grey, red-brown clay; silty, sandy, calcareous and gypsiferous.||||||03-FEB-09
1918|Blanchetown Clay|44191|5|Briefly described|Map Legend|Late Pleistocene|Early Pleistocene|||||||
1918|Blanchetown Clay|49038|4|Described|Table 2|||Briefly described p32.||||||20-OCT-08
1918|Blanchetown Clay|49040|6|Mentioned|p12|||||||||
1918|Blanchetown Clay|60005|5|Briefly described|Map legend|Pleistocene|Pleistocene|Fluvial: clayey sand, sandstone, sand.||||||11-JAN-10
1918|Blanchetown Clay|60540|5|Briefly described|p1000 Fig.2,p1000,p1009 Fig.5,|Pleistocene|Pliocene||||||Lacustrine clay.|
1918|Blanchetown Clay|60953|5|Briefly described|Map Legend|Pleistocene|Pliocene|Sandy clay. Overlain by: Bungunnia Limestone.||||||
1918|Blanchetown Clay|61108|5|Briefly described|map legend|Pleistocene|Pliocene|Sandy clay. Underlies Bungunnia Limestone.||||||01-JUN-05
1918|Blanchetown Clay|61155|5|Briefly described|p18|Late Pliocene|Late Pliocene|Overlies Loxton-Parilla Sands in central area of basin. Variably overlain by Monoman Formation, Lowen Sand, Woorinen Formation and Shepparton Formation. Age: ~2.0Ma. Geological Province: Murray Basin.||||||03-MAR-10
1918|Blanchetown Clay|61207|5|Briefly described|p280 Fig. 2|Pleistocene|Late Pliocene|Lacustrine sediments. Overlies Loxton-Parilla Sands. Geological Province: Murray Basin.||||||
1918|Blanchetown Clay|61314|5|Briefly described|p129|Pleistocene|Pleistocene|Lacustrine clays. Geological Province: western Murray Basin.||||||
1918|Blanchetown Clay|61822|5|Briefly described|p107|Pleistocene|Pleistocene|Geological Province: Murray Basin.||||||
1918|Blanchetown Clay|61964|5|Briefly described|p161|||Overlies the Pliocene "Karoonda surface". Geological Province: Murray Basin.||||||
1918|Blanchetown Clay|63887|5|Briefly described|p20, p21 Fig. 1|Pleistocene|Late Miocene|Deposited in fluvio-lacustrine environment, within a shallow lake.||||||
1918|Blanchetown Clay|63893|5|Briefly described|p191, p185, p184|||Fluvial. With Loxton-Parilla Sands, underlies lowest units of Shepparton Formation. With Loxton-Parilla Sands, underlies bentonite deposits. Geol Prov: Murray Basin.||||||
1918|Blanchetown Clay|64961|5|Briefly described|p259|Quaternary|Quaternary|First formally defined by Firman (1973). Overlain by Bungunnia Limestone; unconformably overlies Karrona Surface over Loxton-Parilla Sand in central/eastern part of basin. Thickness is variable: <40m; typically 1-10m. Geol.province: Murray Basin.||||||10-NOV-10
1918|Blanchetown Clay|65552|5|Briefly described|p5 Fig.3, p6, p23 App.2|Late Pliocene|Late Pliocene|Murray Basin unit. Contains minor gypsum. Overlies Loxton Sands, Parilla Sand, Loxton-Parilla Sands and Norwest Bend Formation. Underlies surface aeolian-fluvio-lacustrine deposits (e.g. Woorinen Formation, Coonambidgal Formation, Molineaux-Lowan Sands).||||||
1918|Blanchetown Clay|65901|6|Mentioned|p181|||May be correlative with possible Pooraka Formation sediments at River Glen Marina, Murray River.||||||
1918|Blanchetown Clay|66002|5|Briefly described|p13 Tb.9|Neogene|Neogene|Defined by Firman 1973.||||||
1918|Blanchetown Clay|66287|5|Briefly described|p25 Fig. 2, p28, 31,33, 42, Fig 4,5,7|Late Pliocene|Late Pliocene|Palaeomag studies on clays from base of unit constrain minimum age for underlying Loxton-Parilla Sands to between 3.4 and 2.4 Ma. Part of the Lake Bungunnia sedimentary fill.||||Overlies the Loxton-Parilla Sands in places.||20-APR-12
1918|Blanchetown Clay|67179|4|Described|p581, p584|Calabrian|Gelasian|Deposited in a large freshwater lake (Lake Bungunnia) due to damming of ancient Murray River in the Late Pliocene (Brown and Stevenson 1991, Cupper et al. 2003). Late Pliocene-Quaternary.|ca 2.4 - 1.2 Ma (McLaren et al. 2009).|||Overlies the Loxton Sand in NW Murray Basin.||28-MAY-13
1918|Blanchetown Clay|67462|5|Briefly described|Map legend.|Pliocene|Pliocene|Murray Basin.||||||
1918|Blanchetown Clay|68116|5|Briefly described|Appendix, Maps 1-11, 14.|Pleistocene|Pliocene|Early Pleistocene minimum age.|||||Laminated greenish-grey and red-brown clay and silty clay, locally calcareous and gypsiferous; minor interbedded quartz sand, ostracod sand; contains calcareous, gypsiferous and siliceous nodules.|
1918|Blanchetown Clay|68189|6|Mentioned|p27 Tb.3.2|||||||Possibly overlain by the Shepparton Formation?||
1918|Blanchetown Clay|68194|6|Mentioned|p24|Pliocene|Pliocene|Murray Basin.||Unit in Wunghnu Group.||||
1918|Blanchetown Clay|68548|5|Briefly described|p13|Pleistocene|Pliocene|Late Pliocene to Early Pleistocene.||||Is overlain by Bungunnia Limestone.|Lacustrine clays.|
1918|Blanchetown Clay|68715|6|Mentioned|p31 Fig.5|Ionian|Zanclean|Murray Basin.||||||
1918|Blanchetown Clay|68716|6|Mentioned|p39 Fig.3|||||||Overlain by the Woorinen Formation. Underlain by the Loxton Sand. ||
1918|Blanchetown Clay|70718|5|Briefly described|p25, p26,  p129|Quaternary|Quaternary|Fine grained lacustrine deposits in Lake Bungunnia.||||Disconformably overlies Loxton Sand.||
1918|Blanchetown Clay|71248|2|Defined|p1,2||Pleistocene|||||||
1918|Blanchetown Clay|72445|5|Briefly described|App.7 p7 Fig.4, p7.|Quaternary|Pliocene|Shown in App 7 Fig 4 (from Brown & Stephenson 1991). Described, along with Loxton-Parilla Sands, Shepparton Formation, as fluvio lacustrine.||||Shown as unconformably overlying Loxton-Parilla Sands and partially equivalent to Bungunnia Limestone.||
1918|Blanchetown Clay|73188|6|Mentioned|p320|Pleistocene|Pleistocene|Murray Basin.|||||Alluvial and lacustrine clay.|
1918|Blanchetown Clay|73228|4|Described|p50-53, p55-57, p59, p62|Pleistocene|Late Pliocene|Murray Basin, Lake Bungunnia. Fluviolacustrine and coastal-shallow marine depositional environments. Identified in Cooltong 1, Loxton 1 and Overland Corner 1 drillholes. Capped by Bungunnia Limestone. Ooid-rich layers are commonly found in the upper portion; these sometimes define a transitional zone with the overlying unit.||||Underlain by Loxton Sand, Bookpurnong Formation, Karoonda Surface, upper Norwest Bend Formation, and Chowilla Sand.|Poorly laminated, or occasionally very finely laminated, clays and sandy clays, and minor quartz sand.|
1918|Blanchetown Clay|73229|5|Briefly described|p66-67, p70-72, p75|Pleistocene|Late Pliocene|Murray Basin. [Analysed using pXRF; see article].|||||Includes clay, greenish grey, sandy; limestone, thin; quartz sand; clay, green-grey, mottled, sandy.|
1918|Blanchetown Clay|73496|5|Briefly described|Map legend|Pleistocene|Pleistocene|||Wunghnu Group|||Lacustrine to fluvial silty or sandy clay; nonmagnetic; moderate to high K, Th, and U where not covered by other units; occupies distinct topographic lows typically less than 60 m ASL.|
1918|Blanchetown Clay|73505|4|Described|p2, p12-13, p36|Pliocene|Pliocene|Murray Basin. Deposited in Lake Bungunnia. Basal contact is partly erosional, upper contact is conformable. Low radiometric response. No detectable magnetic response.||Wunghnu Group||Overlies Parilla Sand, Calivil Formation|Lacustrine clay.|
31520|Blue Gum Suite|23549|5|Briefly described|p520|||Of Glenbog Supersuite.  Comprises Blue Gum and Buldah Gap plutons. Tonalite and granites.||||||05-APR-05
31520|Blue Gum Suite|24551|6|Mentioned|p235, 729 Table 8.12|||||||||
31520|Blue Gum Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31520|Blue Gum Suite|68592|6|Mentioned|p1674|Early Devonian|Early Devonian|||Unit in Glenbog Supersuite.||||
23395|Blue Gum Tonalite|22876|4|Described|p25|||Glenbog Suite||||||
23395|Blue Gum Tonalite|22877|5|Briefly described|map|Silurian|Silurian|Glenbog Supersuite. Porphyritic, weakly foliated. I-Type.||||||26-OCT-04
23395|Blue Gum Tonalite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Biotite-hornblende tonalite: greenish grey, medium to coarse grained, weakly foliated; hornblende crystals to 12mm long, abundant mafic inclusions.||||||06-OCT-04
23395|Blue Gum Tonalite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Biotite-hornblende tonalite: greenish grey, medium to coarse grained, weakly foliated; hornblende crystals to 12mm long, abundant mafic inclusions.||||||01-OCT-04
23395|Blue Gum Tonalite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Biotite-hornblende tonalite: highly to moderately magnetic. Moderate to high in K, Th and U||||||06-OCT-04
23395|Blue Gum Tonalite|23309|5|Briefly described|p425 App1||Early Devonian|G26. I-Type. Supersedes Blue Gums Tonalite. Age: 398 +/- 2 Ma K/Ar.||||||09-DEC-16
23395|Blue Gum Tonalite|24222|5|Briefly described|p14|||Of the Glenbog Supersuite.  Geological Province: Lachlan Fold Belt.||||||
23395|Blue Gum Tonalite|41850|6|Mentioned|p428|||||||||
23395|Blue Gum Tonalite|42827|5|Briefly described|p428|||of Glenbog Supersuite||||||
23395|Blue Gum Tonalite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|of Bega Batholith. I-type. Medium to coarse grained hornblende biotite tonalite.||||||22-OCT-04
23395|Blue Gum Tonalite|43315|5|Briefly described|Map Legend||Wenlock|Of  the Bega Batholith. I-type. medium- to coarse-grained hornblende biotite tonalite.||||||03-MAY-05
23395|Blue Gum Tonalite|60541|6|Mentioned|p65|||See also Blue Gums Tonalite which is probably misspelt - place name is Blue Gum (see Gazetteer).  Both attributed to Dodds (1980). See also p72 Tb. 2.||||||12-JAN-06
23395|Blue Gum Tonalite|68116|5|Briefly described|Appendix, Maps 37, 46.|Early Devonian|Llandovery||||||Biotite-hornblende tonalite (felsic and mafic phases): greenish grey, medium to coarse grained, weakly foliated; hornblende crystals to 12 mm long, abundant mafic enclaves; I-type.|
41777|Blue Rag pluton|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: low gravity response (-500 ums^-2); nonmagnetic, background is weakly magnetic (30 nT). GSV map code: G470.||||||21-SEP-05
41777|Blue Rag pluton|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: low gravity response (-500 ums^-2); nonmagnetic, background is weakly magnetic (30 nT). GSV map code: G470.||||||07-FEB-11
41777|Blue Rag pluton|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: low gravity response (-500 ums^-2); nonmagnetic, background is weakly magnetic (30 nT). GSV map code: G470.||||||21-SEP-05
41777|Blue Rag pluton|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: low gravity response (-500 ums^-2); nonmagnetic, background is weakly magnetic (30 nT). GSV map code: G470.||||||21-SEP-05
41777|Blue Rag pluton|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: low gravity response (-460 to -420 ums^-2); nonmagnetic, background is weakly magnetic (30 nT). GSV map code: G470.||||||
1999|Blue Range Formation|23229|5|Briefly described|p36|||||||||
1999|Blue Range Formation|24551|5|Briefly described|p164, p163 Fig. 6.4, 633|Late Devonian|Late Devonian|Of Taggery Subgroup, Marysville Igneous Complex||||||
1999|Blue Range Formation|35073|5|Briefly described|Table 2|||||||||
1999|Blue Range Formation|35186|4|Described|p3|||||||||
1999|Blue Range Formation|35277|4|Described|p87|||||||||
1999|Blue Range Formation|38327|6|Mentioned|p564|||||||||
1999|Blue Range Formation|39291|6|Mentioned|Table 1|||||||||
1999|Blue Range Formation|40995|6|Mentioned|p362|||||||||
1999|Blue Range Formation|41641|4|Described|p153|||Also P157 and mention on P192||||||
1999|Blue Range Formation|42827|5|Briefly described|p162|||||||||
1999|Blue Range Formation|64616|6|Mentioned|p155|Middle Devonian|Middle Devonian|Cerberean Cauldron. Among the oldest rocks to overlie unconformably Tabberabberan Orogeny-folded rocks. ||||||
1999|Blue Range Formation|68298|5|Briefly described|p230|Frasnian||Type locality is in this unit, near Taggerty, Victoria. Fauna includes species of Bothriolepis and Austrophyllolepis, rhipidistians, a palaeoniscoid, dipnoans and acanthodians. The Taggerty fish site is constrained by isotopically dated rhyolites giving a minimum age of 367 +/- 2 Ma (William et al, 1982). |367 +/- 2 Ma (William et al, 1982)|||||
1999|Blue Range Formation|68311|5|Briefly described|p273-274|Late Devonian|Late Devonian|Cerberean Cauldron, Central Victoria. Up to 120m thick. Pre-collapse phase.||Taggerty Subgroup.||Overlies Snobs Creek Volcanics. Is overlain by Torbreck Range Andesite.|Thin-bedded lacustrine sandstone and siltstone.|
2005|Blue Shirt Rhyolite Member|22968|5|Briefly described|P50, P111|||Intrudes Towanga Sandstone, parent is Thorkidaan Volcanics||||||
2005|Blue Shirt Rhyolite Member|23021|5|Briefly described|Map legend|Ludlow|Ludlow|Parent is Thorkidaan Volcanics||||||
2005|Blue Shirt Rhyolite Member|23309|5|Briefly described|p86 Table 2.32|||Was considered part of Thorkidaan Volcanics.||||||
2005|Blue Shirt Rhyolite Member|24551|5|Briefly described|p131, p135|||Included in Towanga Sandstone by Allen (1987), now included in Thorkidaan Volcanics.||||||
2005|Blue Shirt Rhyolite Member|41585|6|Mentioned|p127|||||||||
2005|Blue Shirt Rhyolite Member|42827|6|Mentioned|p127|||||||||
2013|Blueys Creek Formation|22968|4|Described|p14, Fig49, p104|Gisbornian|Gisbornian|Previously assigned to the Bendoc Group, unconformably overlain by Attunga Paringa Formation, parent is Kiandra Group||||||12-JAN-06
2013|Blueys Creek Formation|23021|5|Briefly described|Map legend|Late Ordovician|Late Ordovician|Parent is the Kiandra Group.||||||25-SEP-08
2013|Blueys Creek Formation|23309|5|Briefly described|p60|||||||||
2013|Blueys Creek Formation|23615|5|Briefly described|p20 Fig.6, p67|Late Ordovician|Late Ordovician|Of Bendoc Group. Includes Banksia Chert Member and Brumby Mafic Arenite Member. Overlain by Towanga Sandstone. Age within the 'deep marine Ordovician sedimentation' period : 500-438Ma. Intruded by the Thorkidaan Volcanics.||||||16-AUG-18
2013|Blueys Creek Formation|23938|5|Briefly described|p14 Tb. 1, p139 Tb.1 App.|Late Ordovician|Late Ordovician|Comprises thinly bedded chert, andesitic to basaltic sandstone turbidites, slate, mudstone, quartz sandstone and dacite to andesitic sills and lavas. Overthrust by Omeo Metamorphic Complex. See also p38-39 Tb. 2, p83.||||||
2013|Blueys Creek Formation|24266|5|Briefly described|p1482|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||09-MAR-05
2013|Blueys Creek Formation|24275|4|Described|p1695, p1698 Tb. 1|Ordovician|Ordovician|Deep marine thinly bedded cherts, cherty slates and mudstones, andesitic to basaltic sandstone turbidites, black mudstone, quartz sandstone turbidites, dacitic to andesitic sills and lavas, and fossiliferous cherts (conodonts). Geol. Prov: Lachlan Fold B.||||||
2013|Blueys Creek Formation|24551|4|Described|p106|Late Ordovician|Late Ordovician|Previously included in the Bendoc Group, now re-assigned to the Kiandra Group.||||||16-AUG-18
2013|Blueys Creek Formation|41585|6|Mentioned|p125|||||||||
2013|Blueys Creek Formation|43128|5|Briefly described|Fig.6,p476||Late Ordovician|||||||
2013|Blueys Creek Formation|43206|5|Briefly described|map legend||Gisbornian|Of Bendoc Group.||||||25-SEP-08
2013|Blueys Creek Formation|43770|5|Briefly described|p829||Late Ordovician|||||||
2013|Blueys Creek Formation|44093|5|Briefly described|p93|Late Ordovician|Late Ordovician|||||||
2013|Blueys Creek Formation|44184|5|Briefly described|Map Legend||Late Ordovician|||||||
2013|Blueys Creek Formation|44185|5|Briefly described|Map legend.|Late Ordovician|Late Ordovician||||||Marine: chert, volcaniclastic siltstone.|
2013|Blueys Creek Formation|60503|5|Briefly described|p64|Late Ordovician|Late Ordovician|Conformably/disconformably overlain by Towanga Sandstone. Geological Province: Limestone Creek Graben. ||||||
2013|Blueys Creek Formation|60541|5|Briefly described|p51, p54|Ordovician|Ordovician|See also Bluey Creek Formation. Of the Bendoc Group. Contains turbidites derived from an andesitic, volcanic source - probably from the Molong Volcanic Rise in New South Wales.||||||
2013|Blueys Creek Formation|61187|5|Briefly described|p24.|Late Ordovician|Late Ordovician|Limestone Creek Graben.||||Is conformably overlain by Towanga Sandstone.|Sandstones and shales.|
2013|Blueys Creek Formation|63278|4|Described|p157|Gisbornian|Darriwilian |Of the Kiandra Group. Geological Province: Kiandra Volcanic Belt, LFB.||||||07-FEB-11
2013|Blueys Creek Formation|63290|6|Mentioned|p394 Tb. 1|Gisbornian|Gisbornian|Geological Province: Kiandra Volcanic Belt. Contains Gisbornian conodonts.||||||11-DEC-07
2013|Blueys Creek Formation|67322|5|Briefly described|p26, p20 Fig.5|Sandbian|Darriwilian|Age is determined from p20 Fig.5 (Strat. column). Occurs in the Kiandra Volcanic Belt.||Of the Kiandra Group|Brumby Mafic Arenite Member, Banksia Chert Member|||21-FEB-18
2013|Blueys Creek Formation|68116|5|Briefly described|Appendix, Maps 35-36.|Katian|Sandbian|Age written as Gisbornian in text.|||||Quartz sandstone, siltstone, chert, black slate, dacite and andesite lava, mafic volcaniclastic sandstone.|
2018|Bluff Member|30570|6|Mentioned|p4|||||||||
2018|Bluff Member|34954|5|Briefly described|p194|||||||||
2018|Bluff Member|35274|5|Briefly described|p421|||||||||
2018|Bluff Member|41868|5|Briefly described|p575|||||||||
2018|Bluff Member|42577|6|Mentioned|p39|||of Bell Point Limestone||||||
2018|Bluff Member|42635|5|Briefly described|p26|||||||||
2018|Bluff Member|42827|5|Briefly described|p575|||||||||
2018|Bluff Member|43530|14|Not recorded|p1029|||Part of Bell Point Limestone||||||
2018|Bluff Member|61181|5|Briefly described|p127|Early Devonian|Early Devonian|Together with Kiln Member forms the uppermost section of Waratah Limestone. Hard, thick-bedded, fossiliferous, dark grey limestone. Thickness: 80m. See also the informal Bluff member.||||||
2057|Bochara Limestone Member|23909|5|Briefly described|p290 Fig.3|Early Miocene|Early Miocene|Geological Province: Otway Basin.||||||
2057|Bochara Limestone Member|35066|4|Described|p213|||||||||
2057|Bochara Limestone Member|42827|4|Described|Fig 8.9|||||||||
2057|Bochara Limestone Member|60785|5|Briefly described|p184 Fig.1, p186.  |Serravallian|Langhian|Of the Otway Basin. Has yielded one partial fossil cetacean skeleton.||Unit in Port Campbell Limestone.||Conformably underlies the Muddy Creek Marl Member.||
2057|Bochara Limestone Member|67061|6|Mentioned|p554 Fig.10.|Miocene||Otway Basin.||||Is overlain by Muddy Creek Marl Member.||
23399|Bodman Creek Formation|24551|6|Mentioned|p503|||||||||
23399|Bodman Creek Formation|38929|4|Described|p51|||See also Fig.6||||||
23399|Bodman Creek Formation|61336|5|Briefly described|p(xii)|||Comprise sands and clays. Graded laterally into Alberton Coal Measures.||||||07-FEB-11
2067|Boebuck Granodiorite|23309|5|Briefly described|p344|||Supersedes Boebuck Adamellite and Tonalite, and Mt Pinnibar Granodiorite.||||||
2067|Boebuck Granodiorite|24133|3|Fully described|p68|Silurian|Silurian|Formerly known as Pinnabar Adamellite.  Parent: Boggy Plain Supersuite.  Geological Province: Lachlan Fold Belt. G90a highly to intensely magnetic; moderate to low K, low Th, moderate patchy U. G90b intensely magnetic; low K, Th, U. G90c highly magnetic||||||31-JAN-06
2067|Boebuck Granodiorite|24142|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Boggy Plain Suite.  Geological Province: Lachlan Fold Belt.||||||
2067|Boebuck Granodiorite|24143|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||
2067|Boebuck Granodiorite|24144|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||
2067|Boebuck Granodiorite|24145|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt||||||
2067|Boebuck Granodiorite|24146|5|Briefly described|Map Legend|Devonian|Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||
2067|Boebuck Granodiorite|24551|6|Mentioned|p233|||See also Mount Pinnibar Granodiorite||||||
2067|Boebuck Granodiorite|39860|5|Briefly described|p21|||||||||
2067|Boebuck Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
2067|Boebuck Granodiorite|60503|4|Described|p155-156, p199|Early Devonian|Early Devonian|Of the Boggy Plains Supersuite. Named by Talent (1967), but also referred to as Pinnibar Adamellite by Wyborn et al (1987). Hornfels aureole - an excellent example of an Early Devonian granite intruding lower greenschist grade Pinnak Sandstone.||||||
2067|Boebuck Granodiorite|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Boggy Plains Supersuite. Hornblende-biotite quartz diorite: I-type; highly magnetic (300-500 nT) with east-west trends and nonmagnetic western margin; low total count, K, Th, moderate U, in southwest moderate K||||||
2067|Boebuck Granodiorite|61187|6|Mentioned|pp15-16.|||Mentioned as possibly prospective for copper-gold mineralisation, although may be less prospective than NSW mineralisation, having formed on continental crust.||Unit in Boggy Plains Supersuite.||||
2067|Boebuck Granodiorite|68116|5|Briefly described|Appendix, Maps 27, 28.|Early Devonian|Early Devonian|Informally subdivided into magnetic, highly magnetic, porphyritic diorite and porphyritic granite phases. Porphyritic diorite contains feldspar porphyry enclaves.|||||Hornblende granodiorite: pale grey, medium grained; I-type. Porphyritic diorite: pale pink and beige; medium grained, pinkish yellow plagioclase phenocrysts; I-type. Porphyritic granite: pale pink and beige; medium grained, K-feldspar rich.|08-DEC-16
37529|Boggy Creek Sandstone|23309|4|Described|p111 table 2.40|||Of Ninnie Subgroup.||||||22-FEB-10
37529|Boggy Creek Sandstone|24551|4|Described|p143|||Of Ninnie Subgroup.||||||
37529|Boggy Creek Sandstone|60542|3|Fully described|p56, p49|Early Devonian|Early Devonian|Of Ninnie Subgroup. Mass flows of crystal-vitric "sandstone". Consists largely of pyroclastics - lithic-rich feldspar ignimbrite. Conformably overlain by Nowa Nowa Conglomerate; conformably overlies Tomato Creek Ignimbrite.||||||
37529|Boggy Creek Sandstone|68116|5|Briefly described|Appendix, Map 45.|Pragian|Pragian||||||Feldspar ignimbrite and feldspathic volcanogenic sandstone: thick bedded, dark grey; vitric mudstone; primary and reworked pyroclastic deposits.|
2092|Boggy Plain Supersuite|22580|5|Briefly described|p94||Early Devonian|||||||
2092|Boggy Plain Supersuite|22638|6|Mentioned|p67|||||||||
2092|Boggy Plain Supersuite|22768|5|Briefly described|p157,178|||||||||
2092|Boggy Plain Supersuite|22778|4|Described|p 159|||||||||
2092|Boggy Plain Supersuite|22831|6|Mentioned|p 69|||||||||
2092|Boggy Plain Supersuite|22857|6|Mentioned|p128, p157|||||||||
2092|Boggy Plain Supersuite|22968|5|Briefly described|Fig89 P164, P207|Early Devonian|Late Silurian|||||||
2092|Boggy Plain Supersuite|22971|6|Mentioned|p 68|||||||||
2092|Boggy Plain Supersuite|23021|5|Briefly described|Map legend|Lochkovian|Lochkovian|Nonconformably and angular unconformably underlies the Mount Elizabeth Caldera Complex||||||
2092|Boggy Plain Supersuite|23028|5|Briefly described|Map legend|Lochkovian|Lochkovian|Unconformably and nonconformably underlies the Mount Elizabeth Caldera Complex||||||
2092|Boggy Plain Supersuite|23029|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
2092|Boggy Plain Supersuite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
2092|Boggy Plain Supersuite|23214|5|Briefly described|p85|||||||||
2092|Boggy Plain Supersuite|23245|6|Mentioned|p128|||||||||
2092|Boggy Plain Supersuite|23309|5|Briefly described|p21, 345, 388, 391, 398||Early Devonian|||||||
2092|Boggy Plain Supersuite|23439|5|Briefly described|p124 fig.1|||||||||
2092|Boggy Plain Supersuite|23548|4|Described|Table 1 p532|||I-Type granites. Also see p533.||||||
2092|Boggy Plain Supersuite|23549|5|Briefly described|p517 Fig 1, p523|||Consists of a belt of granite plutons and associated volcanic complexes. Includes the Boggy Plain Suite and Nallawa Suite. I-type granite. Geological Province: Lachlan Fold Belt.||||||14-DEC-05
2092|Boggy Plain Supersuite|23551|5|Briefly described|p493 & p490|||||||||
2092|Boggy Plain Supersuite|23967|5|Briefly described|p1342|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|24133|4|Described|p68|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|24142|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|24143|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|24144|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|24145|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt||||||
2092|Boggy Plain Supersuite|24146|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|24222|5|Briefly described|p5|||Formed from high temperature magmas. I-type. Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|24266|5|Briefly described|p1485|Early Devonian|Early Devonian|Age: 400+/-10 Ma. Geological Province: Lachlan Fold Belt.||||||07-DEC-04
2092|Boggy Plain Supersuite|24270|6|Mentioned|p1604|||Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|24417|6|Mentioned|p45|||No longer includes "Illunie Rhyolite".||||||
2092|Boggy Plain Supersuite|24512|6|Mentioned|p5|||Geological Province: Lachlan Orogen.||||||
2092|Boggy Plain Supersuite|24514|5|Briefly described|p28, p29|||Granites and volcanic rocks. Includes Mountain Creek Volcanics. Geological Province: Lachlan Fold Belt.||||||25-MAY-05
2092|Boggy Plain Supersuite|24515|5|Briefly described|p35|Paleozoic|Paleozoic|I-type granite. Geological Province: Lachlan Fold Belt.||||||07-NOV-08
2092|Boggy Plain Supersuite|24516|5|Briefly described|p39, p40|||High temperature suite. Includes felsic rhyolites. Geological Province: Lachlan Fold Belt.||||||28-MAY-13
2092|Boggy Plain Supersuite|24551|6|Mentioned|p230|||||||||
2092|Boggy Plain Supersuite|40882|4|Described|p22|||||||||
2092|Boggy Plain Supersuite|41133|4|Described|p1114|||||||||
2092|Boggy Plain Supersuite|42726|5|Briefly described|map legend||Early Devonian|Includes 15 named suites.||||||08-FEB-05
2092|Boggy Plain Supersuite|42791|5|Briefly described|p219|||||||||
2092|Boggy Plain Supersuite|42827|4|Described|p432|||||||||
2092|Boggy Plain Supersuite|44093|5|Briefly described|p93, p103, p188|Early Devonian|Silurian|See also p114.  Includes Bogong, Burrinjuck and Gocup Suites. Intrusions.||||||25-JAN-06
2092|Boggy Plain Supersuite|46524|6|Mentioned|p123|||||||||
2092|Boggy Plain Supersuite|46525|6|Mentioned|p146|||||||||
2092|Boggy Plain Supersuite|50087|6|Mentioned|p176|||Age is post-Ordovician.||||||
2092|Boggy Plain Supersuite|60267|5|Briefly described|p14|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|60423|6|Mentioned|p374|||Geological Province: Lachlan Fold Belt. ||||||
2092|Boggy Plain Supersuite|60503|4|Described|p15, p154|Early Devonian|Early Devonian|Includes several intrusions: Boebuck, Banimboola, Anglers Rest, Bingo Munjie, Post Office and Charlestown intrusions. Geological Province: Lachlan Fold Belt.||||||01-SEP-05
2092|Boggy Plain Supersuite|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Anglers Rest Granite, Banimboola Quartz Diorite, Boebuck Quartz Diorite, Bingo Munjie Quartz Diorite.||||||
2092|Boggy Plain Supersuite|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes: Anglers Rest Granite, Banimboola Quartz Diorite, Boebuck Quartz Diorite, Bingo Munjie Quartz Diorite.||||||
2092|Boggy Plain Supersuite|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes: Anglers Rest Granite, Banimboola Quartz Diorite, Boebuck Quartz Diorite, Bingo Munjie Quartz Diorite.||||||
2092|Boggy Plain Supersuite|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Anglers Rest Granite, Banimboola Quartz Diorite, Boebuck Quartz Diorite, Bingo Munjie Quartz Diorite.||||||
2092|Boggy Plain Supersuite|61160|4|Described|p78, 58-59 Fig. 6.8|Early Devonian|Early Devonian|Comprises Anglers Rest Granite and Banimboola Quartz Monzodiorite. Intrusive I-type granites and volcanic rocks. Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|61161|5|Briefly described|p105, p76-77 Fig 6.1|Early Devonian|Early Devonian|Includes Anglers Rest Granite, Phipps Granite, Dry Gully Granodiorite, Dougs pluton and Alpine Road pluton. I-type granitic and volcanic rocks.||||||
2092|Boggy Plain Supersuite|61163|6|Mentioned|p118|||||||||
2092|Boggy Plain Supersuite|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite and Banimboola Quartz Monzodiorite.||||||
2092|Boggy Plain Supersuite|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite and Banimboola Quartz Monzodiorite.||||||
2092|Boggy Plain Supersuite|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite and Banimboola Quartz Monzodiorite.||||||
2092|Boggy Plain Supersuite|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite and Banimboola Quartz Monzodiorite.||||||07-FEB-11
2092|Boggy Plain Supersuite|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite and Banimboola Quartz Monzodiorite.||||||
2092|Boggy Plain Supersuite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite, Phipps Granite, Dry Gully Granodiorite, Dougs pluton and Alpine Road pluton. ||||||
2092|Boggy Plain Supersuite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite, Phipps Granite, Dry Gully Granodiorite, Dougs pluton and Alpine Road pluton.||||||07-FEB-11
2092|Boggy Plain Supersuite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite, Phipps Granite, Dry Gully Granodiorite, Dougs pluton and Alpine Road pluton. ||||||
2092|Boggy Plain Supersuite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite, Phipps Granite, Dry Gully Granodiorite, Dougs pluton and Alpine Road pluton. ||||||
2092|Boggy Plain Supersuite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite, Phipps Granite, Dry Gully Granodiorite, Dougs pluton and Alpine Road pluton. ||||||
2092|Boggy Plain Supersuite|61783|5|Briefly described|p296|||Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|63287|6|Mentioned|p332|Early Devonian|Late Silurian|||||||07-FEB-11
2092|Boggy Plain Supersuite|63290|6|Mentioned|p405|||Is a proxy for the distribution of Ordovician subduction-related igneous rocks in the crust.||||||11-DEC-07
2092|Boggy Plain Supersuite|66713|6|Mentioned|p13|||Of Wyborn et al. (1987). Contains Yeoval Complex.||||||
2092|Boggy Plain Supersuite|67847|6|Mentioned|p79|||Benambra Terrane, Lachlan Orogen. Hosts porphyry style copper-gold mineralisation. ||||||
2092|Boggy Plain Supersuite|68592|2|Defined|p73 Tb.5,p222,p932-4,p1318-20,p1397-1465|Early Devonian|Early Devonian|Wyborn et al. (1987), after their type pluton the Boggy Plain Granitic Complex (described). Fractionated and oxidised high-temperature granites. Includes many plutons and extends 500 km from NE Victoria to Dubbo. Geochemistry detailed. Has geochemical/genetic affinities with Mountain Creek Volcanics. Geochemical differences with Gunning Suite are described. Conflicts between isotopic and palaeontological ages discussed. Thought to be comagmatic with Mountain Creek and Warrawong Volcanics. Some plutons are adjacent to mineralisation at Murringo Iron Prospect, Murringo Copper Prospect, and the Black Andrew Mine. Taemas and Yass structural zones: deformation described.|c.419-c.415 Ma.||Includes Gooramma, Karoopa, Childowla and Burrinjuck Suites.|Intrudes Black Range Group and Young Suite.|Predominantly granite to granodiorite, generally massive; several bodies also have quartz monzonite, monzodiorite and tonalitic phases; quartz monzonite, quartz monzodiorite to diorite dykes; a small gabbro intrusion. I-type.|
2092|Boggy Plain Supersuite|70297|4|Described|map legend, on side 2 of map sheet|Emsian|Emsian||||Broula Granite, Crowther Monzodiorite, Eugowra Granite, Gumble Granite, Lords Granite||Potassium-rich, oxidised I-type biotite-hornblende granite, leucogranite, monzodiorite and aplite.|18-MAY-16
2092|Boggy Plain Supersuite|70684|6|Mentioned|p11|Early Devonian|Early Devonian|Wyborn et al. (1987).||||||
2092|Boggy Plain Supersuite|71206|6|Mentioned|p379, 384-385|||Lachlan Fold Belt. Petrogenesis discussed.|||Burrinjuck, Yeoval, Jackson Granites.||I-type granite.|
2100|Bogong Creek beds|23710|14|Not recorded|p69|||Correlation.||||||
2100|Bogong Creek beds|34519|6|Mentioned|p42|||||||||
27716|Boisdale Formation|23238|5|Briefly described|Fig10-3.3p108, 108||Pliocene|||||||
27716|Boisdale Formation|23885|5|Briefly described|p163|Pliocene|Late Miocene|Geological Province: Gippsland Basin.||||||
27716|Boisdale Formation|24038|5|Briefly described|p439 Fig.2|Pliocene|Miocene|Geological Province: Gippsland Basin||||||
27716|Boisdale Formation|24468|5|Briefly described|p405 Fig.2|Pliocene|Miocene|Geological Province: Gippsland Basin||||||
27716|Boisdale Formation|24551|5|Briefly described|p327 Fig. 10.33, p733 Table 17.3, p504|Pliocene|Pliocene|Max thickness: 150m.||||||
27716|Boisdale Formation|32375|6|Mentioned|Table 1|||See also p6.||||||07-SEP-18
27716|Boisdale Formation|34843|4|Described|p10|||||||||
27716|Boisdale Formation|35271|6|Mentioned|p67|||||||||
27716|Boisdale Formation|37330|5|Briefly described|Table 4|||||||||
27716|Boisdale Formation|37530|4|Described|p12|||||||||
27716|Boisdale Formation|37585|6|Mentioned|p42|||||||||
27716|Boisdale Formation|37587|6|Mentioned|p35|||||||||
27716|Boisdale Formation|38973|6|Mentioned|p569|||||||||
27716|Boisdale Formation|41868|6|Mentioned|Fig.12.14|||See also p550.||||||07-SEP-18
27716|Boisdale Formation|42184|6|Mentioned|Fig.2 P348|||||||||
27716|Boisdale Formation|42827|3|Fully described|p336|||See also Fig 8.20.||||||07-SEP-18
27716|Boisdale Formation|45168|6|Mentioned|p6|||||||||
27716|Boisdale Formation|60538|5|Briefly described|p488 Fig. 27|||Geological province: Gippland Basin or Latrobe Valley.||||||
27716|Boisdale Formation|61155|5|Briefly described|p5, p18|Pliocene|Pliocene|Of the Sale Group. Overlies Jemmys Point Formation. Age: 3.5-2.0Ma. Thickness: 200m. Geological Province: Gippsland Basin.||||||
27716|Boisdale Formation|61336|5|Briefly described|p(v) Fig. 5|||Of Sale Group. Geological Province: Gippsland Basin.||||||07-FEB-11
27716|Boisdale Formation|63217|4|Described|p97, p112, 109.|||Lateral equivalent to Hazelwood Formation, and a paralic equivalent to the marine carbonates of the Bairnsdale Limestone Formation. Maximum thickness is 5m.|14.5 - 5.5 Ma.|||Overlies Wuk Wuk Marl Formation. Is overlain by Haunted Hills Formation.|Clays and sands.|07-SEP-18
27716|Boisdale Formation|65718|6|Mentioned|p10 Fig 3.2|Pliocene|Pliocene|||||||
27716|Boisdale Formation|69016|5|Briefly described|p89-101|Early Pliocene|Late Miocene|Of the Gippsland Basin. Depositional environment: Marine facies, marginal marine facies and non-marine facies.||Unit of Sale Group.|Includes Nuntin Clay and Wurruk Sand.||Sands, gravels, clays, coal and also middle Tertiary basalts, minor aquifer system consists of limestone and marls.|
27716|Boisdale Formation|73289|6|Mentioned|p765 Fig.2|Recent|Pliocene|||||Unconformably overlies Yallourn Formation.||
27716|Boisdale Formation|73488|6|Mentioned|p634 Fig.4|||||||||
26410|Bola Sandstone Member|23309|5|Briefly described|p106 Table 2.39|||||||||
26410|Bola Sandstone Member|24551|5|Briefly described|p148|||Of Bungywarr Formation.||||||
26410|Bola Sandstone Member|41585|5|Briefly described|p140|||||||||
26410|Bola Sandstone Member|42577|6|Mentioned|p29|||||||||
26410|Bola Sandstone Member|42627|5|Briefly described|Map legend|Pragian||||||||
26410|Bola Sandstone Member|42647|3|Fully described|p30|||of Bungywarr Formation. Supersedes Bola Creek Formation.||||||
26410|Bola Sandstone Member|42827|5|Briefly described|p140|||of Bungywarr Formation||||||
24743|Bolinda Shale|22885|5|Briefly described|map|Late Ordovician|Late Ordovician|||||||
24743|Bolinda Shale|22886|5|Briefly described|p12|Late Ordovician|Late Ordovician|||||||
24743|Bolinda Shale|23229|4|Described|Table3-2p21, 22|Bolindian|Bolindian|||||||
24743|Bolinda Shale|23272|5|Briefly described|p414, Fig14-4.1p415||Bolindian|||||||
24743|Bolinda Shale|23307|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
24743|Bolinda Shale|23309|5|Briefly described|p59, 270 Table 2.18|||||||||
24743|Bolinda Shale|24177|5|Briefly described|p50 Fig.22|Bolindian|Bolindian|Overlain by the Darraweit Guim Formation. Geological Province: Darraweit Guim Province.||||||25-JUN-13
24743|Bolinda Shale|24551|4|Described|p105|Late Ordovician|Late Ordovician|Of Sunbury Group. Conformably overlies Riddell Sandstone.||||||
24743|Bolinda Shale|24588|5|Briefly described|p29|||Of the Sunbury Group. Geological Province: Darraweit Guim Province. Overlies Riddell Sandstone? Overlain by Darraweit Guim Mudstone?||||||29-NOV-13
24743|Bolinda Shale|39980|2|Defined|p19|Late Ordovician|Late Ordovician|||||||
24743|Bolinda Shale|40126|6|Mentioned|p14|||||||||
24743|Bolinda Shale|40136|5|Briefly described|p18|||||||||
24743|Bolinda Shale|41570|4|Described|p87|||||||||
24743|Bolinda Shale|41585|6|Mentioned|Fig.4.1|||||||||
24743|Bolinda Shale|42560|6|Mentioned|p55|||||||||
24743|Bolinda Shale|42628|5|Briefly described|Map legend|Bolindian||||||||
24743|Bolinda Shale|42826|2|Defined|p33|Late Ordovician||||||||
24743|Bolinda Shale|42827|4|Described|p87|||see also Table 4.1||||||
24743|Bolinda Shale|44197|6|Mentioned|Map Legend||Late Ordovician|||||||
24743|Bolinda Shale|60599|5|Briefly described|p47 Fig. 19|Bolindian|Bolindian|Geological Province: Darraweit Guim Province, Melbourne Zone, Lachlan Fold Belt. ||||||
24743|Bolinda Shale|61185|5|Briefly described|p21 Fig. 6|Bolindian|Bolindian|Underlies Darraweit Guim Formation. Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||25-JUN-13
24743|Bolinda Shale|64612|6|Mentioned|p27|Early Llandovery|Early Llandovery|Overlain by Murrindindi Supergroup.||||||25-JUN-13
24743|Bolinda Shale|65715|5|Briefly described|p4 Tb.2|Ordovician|Ordovician|Of Sunbury Group. Formation rank.||||||
24743|Bolinda Shale|68116|5|Briefly described|Appendix, Map 32.|Late Ordovician|Late Ordovician||||||Black shale, siltstone, sandstone: thinly bedded; black shale and siltstone coarse-grained; micaceous; often richly graptolitic; sandstone pale grey; fairly well sorted; fine to medium-grained; sequences.|
2147|Bolwarra-Gorae Diatomite|34988|6|Mentioned|p291 Table 9.4|Pleistocene|Pliocene|~1.8 Ma?||||||16-DEC-14
23404|Bonang Granodiorite|22876|4|Described|p24|||Currawong Suite||||||
23404|Bonang Granodiorite|22877|5|Briefly described|map|Silurian|Silurian|Currowong Suite. Hornblende-biotite granodiorite. I-Type.||||||26-OCT-04
23404|Bonang Granodiorite|23309|6|Mentioned|p425 App1|||G52. I-Type. Supersedes Bonang Granitoid and Granite.||||||
23404|Bonang Granodiorite|42627|5|Briefly described|Map legend|Wenlock|Wenlock|Variation on Bonang Granite.||||||
23404|Bonang Granodiorite|42647|4|Described|p40|||||||||
23404|Bonang Granodiorite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Hornblende granodiorite: medium grained; grey; I-type.|
23404|Bonang Granodiorite|71206|6|Mentioned|p372|||Pre- or syn-deformation emplacement is indicated by strong foliation parallel to regional deformation. Presented as Bonang Complex [?].||||||
2167|Bondi Granite|22815|4|Described|p71|||||||||
2167|Bondi Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
2167|Bondi Granite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Wallagaraugh Suite.||||||
68350|Bonita Sandstone Member|13323|5|Briefly described|p393 Fig. 2|Maastrichtian|Maastrichtian|Of the Volador Formation (Emperor Subgroup, Latrobe Group). Geological Province: Gippsland Basin.||||||26-JUN-06
68350|Bonita Sandstone Member|24551|5|Briefly described|p268, p478 Fig 15.8||Maastrican|Of the Volador Formation.  Of the Halibut Subgroup.||||||
68350|Bonita Sandstone Member|61552|6|Mentioned|p583 Fig.2. |Late Maastrichtian|Late Maastrichtian|||Unit in Barracouta Formation.||||
68350|Bonita Sandstone Member|65717|5|Briefly described|p9 figure 2.2|Maastrichtian|Maastrichtian|||Barracouta Formation||Interbedded with Volador Formation|Interbedded sandstone, siltstone and shale.|
39338|Bonlta Sandstone Member|24090|5|Briefly described|p8 Fig.3|Maastrichtian|Maastrichtian|Of the Volador Formation.  Geological Province: Gippsland Basin.||||||06-APR-05
2203|Bookpurnong Formation|10010|5|Briefly described|p12 Fig. 3|Early Pliocene|Late Miocene|See also Bookpurnong beds. Geological Province: Murray Basin.||||||13-AUG-07
2203|Bookpurnong Formation|22773|5|Briefly described|Fig24.8p352,354|Pliocene|Miocene|||||||
2203|Bookpurnong Formation|22857|5|Briefly described|p352-3 Figs. 24.8 and 24.9, p354|Early Pliocene|Late Miocene|Passes laterally into the Loxton and Parilla Sands. Geological Province: Murray Basin.||||||
2203|Bookpurnong Formation|23226|6|Mentioned|p901|||May overlap Pata Formation depending upon geographic location.  Of Murray Basin.||||||
2203|Bookpurnong Formation|23768|5|Briefly described|p27, p33, p47|||Geological Province: Murray Basin. Overlain by Norwest Bend Formation.  see also p28 Fig. 5.||||||11-SEP-09
2203|Bookpurnong Formation|24551|6|Mentioned|p450|||Supersedes Bookpurnong Beds||||||
2203|Bookpurnong Formation|30996|4|Described|p30|||||||||
2203|Bookpurnong Formation|41511|5|Briefly described|p18|||See also mention p20.||||||29-JUL-08
2203|Bookpurnong Formation|42127|5|Briefly described|p222|||||||||
2203|Bookpurnong Formation|42966|6|Mentioned|p152|||Synonym for Bookpurnong beds||||||
2203|Bookpurnong Formation|44133|5|Briefly described|p161, 152 Fig. 10.2|Early Pliocene|Late Miocene|Geological Province: Murray Basin. ||||||
2203|Bookpurnong Formation|60540|5|Briefly described|p999,p1000 Fig.2,p1002 Fig.4,p1020 |Pliocene|Pliocene|Brown and Stephenson (1991), Rogers et al. (1995). Previously Bookpurnong Beds. Zanclean age, based on biostratigraphy? Low-energy, shallow-marine deposits.||||Conformably overlain by the Loxton Sand. Onlaps [overlies] the Murray Supergroup.|Variable fossiliferous, shallow marine, glauconitic clays and marls.|06-FEB-18
2203|Bookpurnong Formation|60785|6|Mentioned|p184 Fig.1, p196.  |Zanclean|Zanclean|South Australia. Has yielded fossil cetacean elements.||||||
2203|Bookpurnong Formation|61185|5|Briefly described|p58|Late Miocene|Late Miocene|Name used interchangeably with Bookpurnong Beds. Marine sediments. Geological Province: Murray Basin.||||||07-FEB-11
2203|Bookpurnong Formation|63887|5|Briefly described|p20, p21, p21 Fig. 1|Pleistocene|Late Miocene|Shallow marine depositional environment. Consists of clays with occasional sandy, silty, carbonaceous and calcareous beds.||||||
2203|Bookpurnong Formation|64237|5|Briefly described|p19 Fig.2b|Late Miocene|Late Miocene|Superseded Bookpurnong Beds of Lawrence (1961) - revised by Rogers et al (1995). Overlies the Murray Group.||||||29-JUL-08
2203|Bookpurnong Formation|66286|5|Briefly described|p179, pp189-190.|Pliocene|Miocene|Refers to the mud-rich sediments underlying the Loxton-Parilla sands. Deposited during a marine transgression-regression into the Murray Basin. Lacks high carbonate, fossil and glauconite content of other occurrences. 1.5 - 3m blanket under Wimmera Plain.||||Overlies Loddon River Group. Is overlain by or interfingers with Loxton-Parilla sands.|Shallow marine clays and marls; grey to brown muds; pinnate cracks filled with kaolinite common; local goethite-rich lenticular mottles.|
2203|Bookpurnong Formation|67462|5|Briefly described|Map legend.|Miocene|Miocene|Murray Basin.||||||
2203|Bookpurnong Formation|68548|5|Briefly described|p13|Pliocene|Miocene|Late Miocene to Early Pliocene.||||Overlain by the Loxton Sand.|Succession of variably fossiliferous, shallow marine, glauconitic clays and marls.|
2203|Bookpurnong Formation|68715|6|Mentioned|p31 Fig.5|Pliocene|Miocene|Murray Basin. Late Miocene maximum age.||||||
2203|Bookpurnong Formation|68716|5|Briefly described|p39 Fig.3, p40, p43, p44 Fig.7|||Aquitard - extremely low permeability.||||Overlain by the Loxton Sand and Monoman Formation. Underlain by the Pata Formation.||
2203|Bookpurnong Formation|71593|4|Described|p52-p54|Pliocene||This unit is only a few metres thick generally.||||Overlain by the Loxton Sand.|Clay to marl with occasional shell fragments or mica flakes.|
2203|Bookpurnong Formation|72445|5|Briefly described|App.1; App.2.|Pliocene||App.2 is a .csv format file . Identified in Stavely 09,11,14. Accidently assigned to Murray Group in Stavely 11? Shown as ungrouped elsewhere. Minimum age from overlying units.||||Overlain by Calivil Formation, Loxton Sand (sharp contact). Overlies Renmark Group (gradational contact), Murray Group (sharp contact).|Includes glauconitic marl, fine sand and silt; marl with lesser sand and mud; silt with marl and limestone.|
2203|Bookpurnong Formation|73188|6|Mentioned|p320|Pliocene|Pliocene|Murray Basin.|||||Marl, clay, sand.|
2203|Bookpurnong Formation|73228|4|Described|p50, p52-58, p62|Early Pliocene|Late Miocene|Murray Basin. Shallow marine, lower shoreface depositional environments. Identified in Cooltong 1, Berri North 1, Nadda 1, Loxton 1 and Overland Corner 1 drillholes. Outcrops are limited to a small area; type section near Loxton, SA. Subsurface thickness of up to 50 m. Subsurface distribution is a broad arc in the deeper, central sections of the Murray Basin. Considered to have formed on the lower-shoreface (offshore) following major marine inundation of the area.||||Underlain by Murray Group. Overlain by Loxton Sand and Blanchetown Clay.|Brown or greenish grey marl, silty clay and minor fine sand, with relatively high carbonate contents. Includes glauconite, shell/mollusc fragments and bryozoa.|
2203|Bookpurnong Formation|73229|5|Briefly described|p66-67, p70-72, p74-75|Early Pliocene|Late Miocene|Murray Basin. [Analysed using pXRF; see article]. Shallow marine.|||||Marl; silty clay; minor fine-grained sand, glauconitic.|
2211|Boola Formation|22570|6|Mentioned|p189|Pragian|Lochkovian|||||||
2211|Boola Formation|23229|4|Described|Table3-3p27, 32-3|Pragian|Lochkovian|||||||
2211|Boola Formation|23265|5|Briefly described|p341, 348, Fig13-4.10p350||Early Devonian|||||||
2211|Boola Formation|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Jordan River Group.||||||27-OCT-08
2211|Boola Formation|23309|4|Described|p143, 144, 151||Lochkovian|Overlain by Eildon Sandstone? Underlain by Whitelaw Siltstone?||||||17-NOV-08
2211|Boola Formation|24002|5|Briefly described|p234|Early Devonian|Early Devonian|||||||
2211|Boola Formation|24098|5|Briefly described|p27 Fig. 2|Early Devonian|Early Devonian|Of the Murrindindi Supergroup. Geological Province: Melbourne Zone, Lachlan Fold Belt.||||||19-APR-05
2211|Boola Formation|24177|5|Briefly described|p50 Fig.22|Lochkovian|Lochkovian|Geological Province: Mount Easton Province.||||||
2211|Boola Formation|24248|6|Mentioned|p59|Lochkovian|Lochkovian|||||||
2211|Boola Formation|24551|5|Briefly described|p123, p610 Fig. 22.6|||||||||
2211|Boola Formation|24588|5|Briefly described|p20, 30|||Pre-Walhalla Group. ?Of Jordan River Group||||||29-NOV-13
2211|Boola Formation|33601|2|Defined|p13|Early Devonian|Early Devonian|||||||
2211|Boola Formation|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
2211|Boola Formation|34815|6|Mentioned|p19|||||||||
2211|Boola Formation|35073|5|Briefly described|Table 1.|||||||||
2211|Boola Formation|38787|6|Mentioned|p127|||||||||
2211|Boola Formation|39551|6|Mentioned|Map legend|Pragian|Lochkovian|Pragian to Lochkovian||||||
2211|Boola Formation|39555|6|Mentioned|Map legend|Lochkovian|Lochkovian|||||||
2211|Boola Formation|41585|4|Described|p112|||See also p114.||||||17-NOV-08
2211|Boola Formation|41868|5|Briefly described|p574|||||||||
2211|Boola Formation|42051|6|Mentioned|p140|||||||||
2211|Boola Formation|42827|4|Described|p112|||see also Table 4.1||||||
2211|Boola Formation|42938|4|Described|p578|||see also Fig.3 p576.||||||17-NOV-08
2211|Boola Formation|44187|5|Briefly described|Map Legend||Early Devonian|||||||
2211|Boola Formation|60599|5|Briefly described|p47 Fig. 19|Lochkovian|Lochkovian|Geological Province: Mount Easton Province, Melbourne Zone, Lachlan Fold Belt.||||||
2211|Boola Formation|61138|5|Briefly described|p207-208, p210-211|||Coopers Creek and Tyers areas. Problems of the age of the fauna discussed.||||Overlain conformably by the Coopers Creek Limestone.||
2211|Boola Formation|61181|6|Mentioned|p126|Devonian|Devonian|Includes lenses of limestone. ||||||
2211|Boola Formation|61185|5|Briefly described|p37, p21 Fig. 6|Lochkovian|Lochkovian|Of Jordan River Group (Philip, 1962; VandenBerg, 1975). Overlies Whitelaw Siltstone; underlies Coopers Creek Limestone and Wilson Creek Shale. Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
2211|Boola Formation|64535|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Gp. Sitlstone, lithic sandstone, conglomerate and diamictite with mafic- meta-igneous, carbonate and chert grains and clasts; limestone olistoliths; rich shelly fauna in upper parts; deep-marine turbidite fan and hemipelagic fan deposits.||||||22-DEC-08
2211|Boola Formation|64539|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Gp. Sitlstone, lithic sandstone, conglomerate and diamictite with mafic- meta-igneous, carbonate and chert graines and clasts; limestone olistoliths; rich shelly fauna in upper parts; deep-marine turbidite fan and hemipelagic fan deposits.||||||22-DEC-08
2211|Boola Formation|64540|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Gp. Sitlstone, lithic sandstone, conglomerate and diamictite with mafic- meta-igneous, carbonate and chert grains and clasts; limestone olistoliths; rich shelly fauna in upper parts; deep-marine turbidite fan and hemipelagic fan deposits.||||||22-DEC-08
2211|Boola Formation|64605|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Jordan River Group. Siltstone, lithic sandstone, conglomerate, limestone lenses; deep-marine deposits; Dark to bright red and red-green in RGB.  Nonmagnetic.||||||17-NOV-08
2211|Boola Formation|64616|3|Fully described|p92, p155, p203 Fig.7.3, p253-254, p294|Pragian|Lochkovian|See also p304, p385 Tb.1, p386-387, p390. Of Jordan River Group. Conformable between Whitelaw Siltstone below and Wilson Creek Shale above, but also interfingering. Also irregular contact with overlying Coopers Creek Limestone. 200-900m thick. Interbedded siltstone, lithic sandstone, and lithic and fossiliferous conglomerate. Debris-slope deposit, including limestone lenses of high (97.4%) purity; quarried for lime. Contact metamorphosed by Baw Baw Granodiorite. Geophysical characteristics given. Trilobite fossils described.||||||
2211|Boola Formation|65900|6|Mentioned|p171||Devonian|Shallow marine strata, contains clasts of probable Cambrian mafic rocks.||||||10-MAY-12
2211|Boola Formation|68116|5|Briefly described|Appendix, Maps 43, 52.|Pragian|Lochkovian||||||Siltstone, intercalated with lithic sandstone, conglomerate, limestone lenses: siltstone well bedded to prominently slump-folded; sandstone and conglomerate with mafic meta-igneous, carbonate and chert grains and clasts; limestone olistoliths.|
21295|Boorabal Andesite|23309|4|Described|p108 Table 2.40|||Maximum Thickness: 150m.  Of the Little River Subgroup.||||||
21295|Boorabal Andesite|23615|3|Fully described|p29 Fig.9, p126|Early Devonian|Early Devonian|Of Little River Subgroup. Overlain by McRaes Ignimbrite.  Consists of andesite lava, lenses of basalt lava and breccia with minor intercalated sediments.  Max. thickness: 150m.  See also p213 App. 2.||||||
21295|Boorabal Andesite|24551|5|Briefly described|p145|||Of Little River Subgroup.||||||
21295|Boorabal Andesite|43206|5|Briefly described|map legend||Lochkovian|of Little River Subgroup.||||||
21295|Boorabal Andesite|60542|5|Briefly described|p60|Early Devonian|Early Devonian|Overlies the Balley Hooley Ignimbrite. ||||||
21295|Boorabal Andesite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Andesite lava, minor basalt lava lenses, breccia.|
69406|Boorgunyah Granite|61160|4|Described|p60, p32 Tb. 5.2|Silurian|Silurian|S-type. Medium-grained, equigranular, muscovite-biotite leucocratic granite with weak foliation and small clots of biotite-muscovite up to 2cm. See also p58-59 Fig. 6.8.||||||
69406|Boorgunyah Granite|61164|5|Briefly described|map legend|Early Silurian|Early Silurian|Muscovite-biotite leucogranite: medium grained; equigranular with clots of biotite-muscovite up to 2 cm; weak foliation; S-type intrusion. GSV map code: G170.||||||
69406|Boorgunyah Granite|61165|5|Briefly described|map legend|Early Silurian|Early Silurian|Muscovite-biotite leucogranite: medium grained; equigranular with clots of biotite-muscovite up to 2 cm; weak foliation; S-type intrusion. GSV map code: G170.||||||
69406|Boorgunyah Granite|61166|5|Briefly described|map legend|Early Silurian|Early Silurian|Muscovite-biotite leucogranite: medium grained; equigranular with clots of biotite-muscovite up to 2 cm; weak foliation; S-type intrusion. GSV map code: G170.||||||
69406|Boorgunyah Granite|61167|5|Briefly described|map legend|Early Silurian|Early Silurian|Muscovite-biotite leucogranite: medium grained; equigranular with clots of biotite-muscovite up to 2 cm; weak foliation; S-type intrusion. GSV map code: G170.||||||07-FEB-11
69406|Boorgunyah Granite|61168|5|Briefly described|map legend|Early Silurian|Early Silurian|Muscovite-biotite leucogranite: S-type; nonmagnetic (kv = 0-5 x10^-6 cg); low gravity (-420 to -425 ums ^-2); low to moderate total radioelement, high K, low Th, low to moderate U. GSV map code: G170.||||||
69406|Boorgunyah Granite|68116|5|Briefly described|Appendix, Map 27.|Silurian|Silurian||||||Muscovite-biotite leucogranite: medium-grained, equigranular with clots of biotite-muscovite up to 2 cm; weakly foliated; S-type.|
2277|Boorhaman Conglomerate|22971|4|Described|p12 Tb.1, p25|Permian|Carboniferous|Consists of grey diamictite(tillite), slump deposits and sandstone and siltstone.||||||19-JAN-06
2277|Boorhaman Conglomerate|23307|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
2277|Boorhaman Conglomerate|41637|6|Mentioned|p209|||||||||
2277|Boorhaman Conglomerate|42454|5|Briefly described|p11|||Permian||||||
2277|Boorhaman Conglomerate|42827|6|Mentioned|p209|||||||||
2277|Boorhaman Conglomerate|43841|4|Described|7|Early Permian|Late Carboniferous|Max. drilled thickness 176.2m||||||
2277|Boorhaman Conglomerate|60529|5|Briefly described|Map Legend|Permian|Carboniferous|Fluvial deposits; gravel and cobbles of quartz and lithic fragments, moderately to poorly sorted, unconsolidated.||||||15-JUN-06
2277|Boorhaman Conglomerate|61185|5|Briefly described|p53|Permian|Late Carboniferous|Does not outcrop on NAGAMBIE. Intersected in bore hole. Fine- to coarse-grained sand and gravel and cobbles of well-rounded quartz and rare sedimentary lithic fragments.||||||07-FEB-11
2277|Boorhaman Conglomerate|61701|5|Briefly described|Map Legend|Permian|Carboniferous|Fluvial deposits; gravel and cobbles of quartz and lithic fragments, moderately to poorly sorted, unconsolidated.||||||15-JUN-06
2277|Boorhaman Conglomerate|61702|5|Briefly described|Map Legend|Permian|Carboniferous|Fluvial deposits; gravel and cobbles of quartz and lithic fragments, moderately to poorly sorted, unconsolidated.||||||15-JUN-06
2277|Boorhaman Conglomerate|61703|5|Briefly described|Map Legend|Permian|Carboniferous|Fluvial deposits; gravel and cobbles of quartz and lithic fragments, moderately to poorly sorted, unconsolidated.||||||15-JUN-06
2277|Boorhaman Conglomerate|68116|5|Briefly described|Appendix, Maps 18, 19, 26.|Permian|Permian||||||Polymict conglomerate, pebbly sandstone, siltstone; fluvioglacial, marine.|
2277|Boorhaman Conglomerate|69798|5|Briefly described|p4 Fig.2, p14-16|Late Carboniferous|Late Carboniferous|Oaklands Basin. Marine (glaciogene) and fluvial.||||Is unconformably overlain by Urana Formation.||06-FEB-18
2376|Boulder Flat Limestone|22530|6|Mentioned|p698||Emsian|||||||
2376|Boulder Flat Limestone|22876|6|Mentioned|p17|||Errinunda Group.||||||25-SEP-08
2376|Boulder Flat Limestone|23309|5|Briefly described|p106, 125, 126  Table 2.39||Early Devonian|||||||
2376|Boulder Flat Limestone|23522|5|Briefly described|p247 Fig 3|Early Devonian|Early Devonian|||||||
2376|Boulder Flat Limestone|23938|5|Briefly described|p31-32 Fig. 12|Early Devonian|Early Devonian|See also p139 Tb. 1 Appendix.||||||25-SEP-08
2376|Boulder Flat Limestone|24551|4|Described|p148, 440, 455|||Of Errinundra Group.||||||
2376|Boulder Flat Limestone|40761|5|Briefly described|p233|||||||||
2376|Boulder Flat Limestone|41585|5|Briefly described|p140|||||||||
2376|Boulder Flat Limestone|41868|5|Briefly described|p575|||||||||
2376|Boulder Flat Limestone|42577|6|Mentioned|p29|||||||||
2376|Boulder Flat Limestone|42627|5|Briefly described|Map Legend|Emsian||||||||
2376|Boulder Flat Limestone|42647|2|Defined|p32|Emsian|Pragian|Of Errinundra Group.||||||25-SEP-08
2376|Boulder Flat Limestone|42827|4|Described|p140|||see also Table 4.1||||||
2376|Boulder Flat Limestone|43228|5|Briefly described|p10||Early Devonian|||||||
2376|Boulder Flat Limestone|61181|5|Briefly described|p13, p128|Devonian|Devonian|Contains a locally discordant but persistent barite-rich zone near its basal contact with ignimbrites. The mineralisation is 15-30m wide and is traced discontinuously for >3km. ||||||
2376|Boulder Flat Limestone|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Boulder Flat. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
2376|Boulder Flat Limestone|68116|5|Briefly described|Appendix, Map 36.|Early Devonian|Early Devonian||||||Limestone: massive, dark grey, recrystallized to stylobrecciated; black shale; minor dolomite.|
24756|Bouma B beds|41590|6|Mentioned|Fig.3|||||||||
28392|Bouma C beds|41590|6|Mentioned|p3|||||||||
2387|Boundary Creek Conglomerate|23309|4|Described|p108, Table 2.40|||Maximum Thickness: 100m.  Of the Little River Subgroup.||||||
2387|Boundary Creek Conglomerate|23615|3|Fully described|p126|Early Devonian|Early Devonian|Of Little River Subgroup. Previously included in the basal beds of Wulgulmerang Ashstone (Ringwood, 1955 a,b).  Now redefined and considered to post-date the Wulgulmerang Ashstone.  Overlies Wulgulmerang Ashstone.  Max. thickness:100m.||||||
2387|Boundary Creek Conglomerate|24551|5|Briefly described|p145|||Of Little River Subgroup.||||||
2387|Boundary Creek Conglomerate|33602|6|Mentioned|p32|||||||||
2387|Boundary Creek Conglomerate|33603|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
2387|Boundary Creek Conglomerate|33606|5|Briefly described|p64|||||||||
2387|Boundary Creek Conglomerate|34519|6|Mentioned|p44|||||||||
2387|Boundary Creek Conglomerate|35014|6|Mentioned|p363|||||||||
2387|Boundary Creek Conglomerate|35112|6|Mentioned|p285|||||||||
2387|Boundary Creek Conglomerate|35283|6|Mentioned|p49|||||||||
2387|Boundary Creek Conglomerate|36201|5|Briefly described|p5|||||||||
2387|Boundary Creek Conglomerate|37330|5|Briefly described|Table 2|||||||||
2387|Boundary Creek Conglomerate|41585|6|Mentioned|p136|||||||||
2387|Boundary Creek Conglomerate|42827|5|Briefly described|p136|||||||||
2387|Boundary Creek Conglomerate|43206|5|Briefly described|map legend||Lochkovian|of Little River Subgroup.||||||
2387|Boundary Creek Conglomerate|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Red conglomerate, gritstone and pebbly sandstone, red siltstone, mudstone.|
83445|Bourka pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G652.|||||Magnetic response to 150 nT but with nonmagnetic core; gravity low approximately 50 micrometres/second/second.|
83445|Bourka pluton|73505|5|Briefly described|p18, p21|||Newly named unit in Swan Hill and parts of Balranald and Deniliquin 1:250 000 map areas, (G652). Named after Bourka Parish. Subcircular intrusion about 5 km in diameter and 5km NW of Sea Lake, a second smaller intrusion is grouped with this pluton. Magnetic response to 150 nT but with nonmagnetic core. Gravity low, approximately 50 micrometres/second/second.|||||Granite.|
21305|Bowen Track Ignimbrite|23309|5|Briefly described|p123, 134  Table 2.47|||||||||
21305|Bowen Track Ignimbrite|23615|3|Fully described|p86, p96|Early Devonian|Early Devonian|Of White Monkey Subgroup. Extensive coarse-grained quartz and feldspar ignimbrite.  Underlain by Mackiesons Spur Ashstone.  Max. thickness: 600m.||||||
21305|Bowen Track Ignimbrite|24551|5|Briefly described|p149, p132 Fig.5.23|||Of White Monkey Volcanics||||||
21305|Bowen Track Ignimbrite|43206|5|Briefly described|map legend||Ludlow|OF White Monkey Subgroup.||||||
21305|Bowen Track Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Early Devonian|Early Devonian||||||Quartz-feldspar ignimbrite. Coarse, abundant white feldspar and large quartz grains set in a welded black glassy groundmass. Aggregates of feldspar are common. Minor small felsic lava or sedimentary lithics, occasional pumice clasts.|
39335|Bream Volcanics|13323|5|Briefly described|p393 Fig. 2|Middle Eocene|Middle Eocene|Basaltic volcanics. Geological Province: Gippsland Basin.||||||26-MAY-06
39335|Bream Volcanics|24090|5|Briefly described|p8 Fig.3|Eocene|Eocene|Geological Province: Gippsland Basin.||||||
39335|Bream Volcanics|24551|5|Briefly described|p262 Fig. 9.29, p478 Fig 15.8|Eocene|Eocene|||||||
39335|Bream Volcanics|61552|6|Mentioned|p583 Fig.2. |Eocene|Eocene|||||||
39335|Bream Volcanics|65717|5|Briefly described|p9 figure 2.2|Eocene|Eocene|||Halibut Subgroup||Associated with Barracouta Formation|Basaltic volcanics.|05-SEP-17
39335|Bream Volcanics|66181|6|Mentioned|p310 Fig.5|||Lithological identifier not used in figure, only in caption; an episode of volcanism in Gippsland Basin, presented as Bream.||||||
39335|Bream Volcanics|73471|6|Mentioned|p87|Eocene|Eocene|Gippsland Basin, Central Deep. Referred to as Bream Volcano p86.|46 Ma|||||
39335|Bream Volcanics|75065|5|Briefly described|p151|Eocene|Eocene|Gippsland Basin; offshore.||Halibut Subgroup.||Overlies Barracouta Formation. Is overlain unconformably by Traralgon Formation (Cobia Subgroup).||
24764|Bridgewater Bay Sands|34988|5|Briefly described|p295|||||||||
24764|Bridgewater Bay Sands|41848|3|Fully described|p366|Holocene|Holocene|Dune limestone of Mount Gambier coastal plains (Bridgewater Formation), not equivalent to Bridgewater Bay Sands||||||22-FEB-13
24764|Bridgewater Bay Sands|42827|5|Briefly described|p370|||||||||
2543|Bridgewater Formation|2967|6|Mentioned|p54|||Boutakoff (1963). A regressive coastal dune sequence.||||||
2543|Bridgewater Formation|10010|5|Briefly described|p14 Fig. 5f, p16|Quaternary|Quaternary|Carbonate-rich. Geological Province: Murray Basin.||||||13-AUG-07
2543|Bridgewater Formation|22489|5|Briefly described|p12||Pleistocene|||||||
2543|Bridgewater Formation|22552|6|Mentioned|p 32|||||||||
2543|Bridgewater Formation|22867|6|Mentioned|P27|||||||||
2543|Bridgewater Formation|22870|6|Mentioned|P32|||||||||
2543|Bridgewater Formation|22875|6|Mentioned|p86|||||||||
2543|Bridgewater Formation|23322|5|Briefly described|957 Fig.2|Pleistocene|Pliocene|Geological Province: Gambier Basin.||||||07-SEP-09
2543|Bridgewater Formation|23418|6|Mentioned|p14|||||||||
2543|Bridgewater Formation|23482|5|Briefly described|p9|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|23492|6|Mentioned|p7 Fig. 2.|||||||||
2543|Bridgewater Formation|23537|5|Briefly described|p 440|||||||||
2543|Bridgewater Formation|23560|5|Briefly described|p152|Cretaceous|Cretaceous|||||||
2543|Bridgewater Formation|23719|5|Briefly described|p30|||||||||
2543|Bridgewater Formation|23731|6|Mentioned|p29|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|23779|5|Briefly described|p621|||||||||
2543|Bridgewater Formation|23818|5|Briefly described|p213, 228|||Geological Province: Murray Basin. Underlying unit: Coomandook Formation and Nullarbor Limestone. Max. thickness: 250 ft.||||||
2543|Bridgewater Formation|23879|5|Briefly described|p20|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|23908|6|Mentioned|p6|Pleistocene|Pleistocene| Geological Province: Gawler Craton.||||||
2543|Bridgewater Formation|23921|5|Briefly described|p1109 Table 1, p1111|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
2543|Bridgewater Formation|23932|5|Briefly described|p687|Holocene|Pleistocene|||||||
2543|Bridgewater Formation|24038|5|Briefly described|p439 Fig.2|Pliocene|Pliocene|Geological Province: Port Phillip Basin||||||
2543|Bridgewater Formation|24358|5|Briefly described|p32 Fig.1|Pleistocene|Pleistocene|Geological Province: Eucla Basin. Maximum Thickness: 15m.||||||17-MAR-05
2543|Bridgewater Formation|24363|6|Mentioned|p37 Fig.1|Quaternary|Quaternary|||||||
2543|Bridgewater Formation|24410|5|Briefly described|p6|Pleistocene|Pleistocene|Includes bouldery conglomerate with flint.||||||24-NOV-09
2543|Bridgewater Formation|24508|5|Briefly described|p30|Quaternary|Quaternary|Consists of relict, calcareous sand dunes formed during the last interglacial period.  Geological Province: Gawler Craton.||||||23-DEC-09
2543|Bridgewater Formation|24551|6|Mentioned|p305, 306, 343, p734 Table 17.4|||Superseded by Bridgewater Group.  Max thickness: 200m.||||||
2543|Bridgewater Formation|24585|6|Mentioned|p33 (photo)|||||||||
2543|Bridgewater Formation|29591|6|Mentioned|p92|||||||||
2543|Bridgewater Formation|29664|6|Mentioned|p2|||||||||
2543|Bridgewater Formation|29665|6|Mentioned|p79|||||||||
2543|Bridgewater Formation|29697|6|Mentioned|p2|||||||||
2543|Bridgewater Formation|29825|5|Briefly described|p18|||||||||
2543|Bridgewater Formation|29829|6|Mentioned|p178|||||||||
2543|Bridgewater Formation|29866|6|Mentioned|p84|||||||||
2543|Bridgewater Formation|29891|5|Briefly described|p107|||||||||
2543|Bridgewater Formation|29892|6|Mentioned|p77|||||||||
2543|Bridgewater Formation|30514|6|Mentioned|p102|||||||||
2543|Bridgewater Formation|30522|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|30578|5|Briefly described|p14|||||||||
2543|Bridgewater Formation|30580|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
2543|Bridgewater Formation|30752|6|Mentioned|p5|||||||||
2543|Bridgewater Formation|30754|6|Mentioned|p20|||See also P22,24,27. Geological map||||||
2543|Bridgewater Formation|30756|6|Mentioned|p4|||||||||
2543|Bridgewater Formation|30758|6|Mentioned|p66|||Stratigraphy||||||
2543|Bridgewater Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
2543|Bridgewater Formation|30825|6|Mentioned|p32|||||||||
2543|Bridgewater Formation|30922|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|30928|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
2543|Bridgewater Formation|30932|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|31241|4|Described|p101|||Middle Pleistocene||||||
2543|Bridgewater Formation|31248|4|Described|p57|||||||||
2543|Bridgewater Formation|31312|6|Mentioned|p71|||||||||
2543|Bridgewater Formation|31320|6|Mentioned|p14|||Quaternary||||||
2543|Bridgewater Formation|31624|4|Described|p98|||Pleistocene. See also p131.||||||22-FEB-19
2543|Bridgewater Formation|31625|6|Mentioned|Fig. 5.2|||Pleistocene||||||
2543|Bridgewater Formation|31629|6|Mentioned|Fig. 5.1|||Recent to Pleistocene||||||
2543|Bridgewater Formation|31746|6|Mentioned|p197|||||||||
2543|Bridgewater Formation|31850|3|Fully described|p39|||||||||
2543|Bridgewater Formation|31920|6|Mentioned|p59|||See also Table 3-1. Pleistocene||||||
2543|Bridgewater Formation|31923|6|Mentioned|p16|||||||||
2543|Bridgewater Formation|32432|5|Briefly described|Table 1|||||||||
2543|Bridgewater Formation|32438|6|Mentioned|p42|||||||||
2543|Bridgewater Formation|32561|6|Mentioned|Fig.4|||||||||
2543|Bridgewater Formation|32767|6|Mentioned|p66|||||||||
2543|Bridgewater Formation|32859|5|Briefly described|p69|||See also Figs. 1,2.||||||
2543|Bridgewater Formation|33109|5|Briefly described|p83|||Main aquifer system P84||||||
2543|Bridgewater Formation|33160|6|Mentioned|p301|||See also P304||||||
2543|Bridgewater Formation|33224|6|Mentioned|Fig.32|||See also Fig.36. Photo.||||||
2543|Bridgewater Formation|33716|3|Fully described|p20|||See also Table 2.||||||
2543|Bridgewater Formation|33798|6|Mentioned|p98|||See also Fig.2||||||
2543|Bridgewater Formation|34180|6|Mentioned|p212|||Middle Pleistocene||||||
2543|Bridgewater Formation|34191|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|34658|5|Briefly described|p98|||||||||
2543|Bridgewater Formation|34758|6|Mentioned|Table 1|||||||||
2543|Bridgewater Formation|34827|6|Mentioned|p12|||||||||
2543|Bridgewater Formation|34954|5|Briefly described|p198|||||||||
2543|Bridgewater Formation|34988|3|Fully described|p291|||||||||
2543|Bridgewater Formation|35029|6|Mentioned|p168|||||||||
2543|Bridgewater Formation|35066|6|Mentioned|p218|||||||||
2543|Bridgewater Formation|35097|6|Mentioned|p15|||||||||
2543|Bridgewater Formation|35147|6|Mentioned|p127|||||||||
2543|Bridgewater Formation|35238|6|Mentioned|p86|||||||||
2543|Bridgewater Formation|35271|6|Mentioned|p67|||||||||
2543|Bridgewater Formation|35272|6|Mentioned|p283|||||||||
2543|Bridgewater Formation|35274|6|Mentioned|p424|||||||||
2543|Bridgewater Formation|35285|6|Mentioned|p414|||||||||
2543|Bridgewater Formation|35290|6|Mentioned|p45|||||||||
2543|Bridgewater Formation|35368|6|Mentioned|p69|||||||||
2543|Bridgewater Formation|35579|6|Mentioned|p67|||||||||
2543|Bridgewater Formation|35672|6|Mentioned|p11|||||||||
2543|Bridgewater Formation|35712|4|Described|p24|||||||||
2543|Bridgewater Formation|35722|6|Mentioned|p6|||Stratigraphy.||||||
2543|Bridgewater Formation|35772|4|Described|Table 1|||||||||
2543|Bridgewater Formation|36355|6|Mentioned|p132|||||||||
2543|Bridgewater Formation|36499|6|Mentioned|p51|||||||||
2543|Bridgewater Formation|36624|6|Mentioned|Fig.1|||||||||
2543|Bridgewater Formation|37500|6|Mentioned|p385|||||||||
2543|Bridgewater Formation|37548|6|Mentioned|p131|||||||||
2543|Bridgewater Formation|37850|6|Mentioned|Fig.2|||||||||
2543|Bridgewater Formation|37863|5|Briefly described|p195|||||||||
2543|Bridgewater Formation|38068|6|Mentioned|p76|||||||||
2543|Bridgewater Formation|38699|5|Briefly described|Fig.10|||||||||
2543|Bridgewater Formation|38932|5|Briefly described|p99|||See also Fig.4||||||
2543|Bridgewater Formation|39077|6|Mentioned|p25|||||||||
2543|Bridgewater Formation|39329|6|Mentioned|p485|||||||||
2543|Bridgewater Formation|39351|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
2543|Bridgewater Formation|39352|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|39839|6|Mentioned|p48|||||||||
2543|Bridgewater Formation|40003|5|Briefly described|p44|||||||||
2543|Bridgewater Formation|40226|6|Mentioned|p52|||||||||
2543|Bridgewater Formation|40230|6|Mentioned|p7|||||||||
2543|Bridgewater Formation|40440|5|Briefly described|p103|||||||||
2543|Bridgewater Formation|40442|6|Mentioned|p35|||||||||
2543|Bridgewater Formation|40445|5|Briefly described|p48|||||||||
2543|Bridgewater Formation|40448|5|Briefly described|p43|||||||||
2543|Bridgewater Formation|40521|6|Mentioned|Fig.2|||||||||
2543|Bridgewater Formation|40525|6|Mentioned|p172|||||||||
2543|Bridgewater Formation|40555|6|Mentioned|p51|||||||||
2543|Bridgewater Formation|40561|6|Mentioned|p8|||||||||
2543|Bridgewater Formation|40643|5|Briefly described|p145|||||||||
2543|Bridgewater Formation|40829|5|Briefly described|p14|||||||||
2543|Bridgewater Formation|40941|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|40942|4|Described|p20|||||||||
2543|Bridgewater Formation|40980|6|Mentioned|p335|||||||||
2543|Bridgewater Formation|41206|5|Briefly described|p367|||Mention P365||||||
2543|Bridgewater Formation|41499|6|Mentioned|p70|||||||||
2543|Bridgewater Formation|41511|6|Mentioned|p23|||||||||
2543|Bridgewater Formation|41521|3|Fully described|p241|||||||||
2543|Bridgewater Formation|41599|6|Mentioned|p192|||||||||
2543|Bridgewater Formation|41619|6|Mentioned|Map legend|Pleistocene||||||||
2543|Bridgewater Formation|41642|6|Mentioned|Fig.8.6|||||||||
2543|Bridgewater Formation|41769|6|Mentioned|p50|||||||||
2543|Bridgewater Formation|41848|3|Fully described|p366|||||||||
2543|Bridgewater Formation|41868|5|Briefly described|p549|||See also p554 and p578.||||||22-FEB-19
2543|Bridgewater Formation|41940|6|Mentioned|p38|||||||||
2543|Bridgewater Formation|42097|6|Mentioned|p40|||||||||
2543|Bridgewater Formation|42129|6|Mentioned|p254|||See also Fig.6||||||
2543|Bridgewater Formation|42292|5|Briefly described|p8|||See also Fig. 3 P12||||||
2543|Bridgewater Formation|42318|5|Briefly described|p8|||||||||
2543|Bridgewater Formation|42404|6|Mentioned|p32|||||||||
2543|Bridgewater Formation|42466|5|Briefly described|Map Legend|||||||||
2543|Bridgewater Formation|42475|4|Described|p23|||||||||
2543|Bridgewater Formation|42601|6|Mentioned|Fig.2 p15|||||||||
2543|Bridgewater Formation|42622|6|Mentioned|p15|||||||||
2543|Bridgewater Formation|42635|5|Briefly described|p94|||||||||
2543|Bridgewater Formation|42716|5|Briefly described|Map legend|Pleistocene||||||||
2543|Bridgewater Formation|42717|5|Briefly described|map legend|Pleistocene||||||||
2543|Bridgewater Formation|42738|5|Briefly described|map legend|Quaternary||||||||
2543|Bridgewater Formation|42827|4|Described|p366|||see also Table 9.3||||||
2543|Bridgewater Formation|42966|2|Defined|p223|Late Pleistocene|Early Pleistocene|||||||
2543|Bridgewater Formation|43026|5|Briefly described|Table 1,p586|||||||||
2543|Bridgewater Formation|43049|4|Described|p23|||||||||
2543|Bridgewater Formation|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Calcreted aeolianite.||||||25-MAY-05
2543|Bridgewater Formation|43071|5|Briefly described|p17|||||||||
2543|Bridgewater Formation|43073|5|Briefly described|Table 4|||||||||
2543|Bridgewater Formation|43195|5|Briefly described|Map Legend|Late Pleistocene|Early Pleistocene|see also commentary on back of map.||||||
2543|Bridgewater Formation|43231|6|Mentioned|p12|||||||||
2543|Bridgewater Formation|43258|5|Briefly described|Map Legend||Pleistocene|||||||
2543|Bridgewater Formation|43298|5|Briefly described|Map Legend||Pleistocene|||||||
2543|Bridgewater Formation|43590|4|Described|p35||Quaternary|||||||
2543|Bridgewater Formation|44133|5|Briefly described|p220 Fig. 11.2, 222|Pleistocene|Pleistocene|Geological Province: Eucla Basin. ||||||
2543|Bridgewater Formation|44864|5|Briefly described|Map Legend||Pleistocene|||||||
2543|Bridgewater Formation|46802|6|Mentioned|Table 1|||||||||
2543|Bridgewater Formation|46839|6|Mentioned|p86|||See also Fig.3||||||
2543|Bridgewater Formation|46909|6|Mentioned|p83|||See also Fig.2||||||
2543|Bridgewater Formation|48911|6|Mentioned|Chart 1|||||||||
2543|Bridgewater Formation|49038|4|Described|Table 2|||Briefly described P33||||||
2543|Bridgewater Formation|50154|2|Defined|p140||Late Pleistocene|Overlies the Whalers Bluff Formation. Age: oldest dunes dated at 0.69 Ma. Consists of poorly consolidated fine- to coarse- grained calcarenite.||||||15-MAY-13
2543|Bridgewater Formation|50155|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Palaeo-beach ridges; calcarenite||||||
2543|Bridgewater Formation|50156|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Stranded elongate beach ridges: calcareous sand, calcarenite; pale yellow, fine to coarse, fossiliferous, cross bedding common, poorly consolidated.||||||
2543|Bridgewater Formation|50157|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Overlies Whalers Bluff Formation. Stranded elongate beach ridges: calcareous sand, calcarenite; pale yellow, fine to coarse, fossiliferous, cross bedding common, poorly consolidated.||||||25-JUN-04
2543|Bridgewater Formation|50158|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Stranded elongate beach ridges: calcareous sand, calcarenite; pale yellow, fine to coarse, fossiliferous, cross bedding common, poorly consolidated.||||||
2543|Bridgewater Formation|50159|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Stranded elongate beach ridges: calcareous sand, calcarenite; pale yellow, fine to coarse, fossiliferous, cross bedding common, poorly consolidated.||||||24-JUN-04
2543|Bridgewater Formation|50160|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Calcareous sand, calcarenite||||||16-JUN-04
2543|Bridgewater Formation|50161|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Stranded elongate beach ridges: calcareous sand, calcarenite; pale yellow, fine to coarse, fossiliferous, cross bedding common, poorly consolidated.||||||24-JUN-04
2543|Bridgewater Formation|50162|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Stranded elongate beach ridges: calcareous sand, calcarenite; pale yellow, fine to coarse, fossiliferous, cross bedding common, poorly consolidated.||||||24-JUN-04
2543|Bridgewater Formation|50163|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Stranded elongate beach ridges: calcareous sand, calcarenite; pale yellow, fine to coarse, fossiliferous, cross bedding common, poorly consolidated.||||||24-JUN-04
2543|Bridgewater Formation|50164|5|Briefly described|Map Legend|Quaternary|Quaternary|Palaeo-beach ridges; calcarenite.||||||
2543|Bridgewater Formation|60707|5|Briefly described|p612 Fig. 1c|Pleistocene|Pleistocene|Calcarenites.||||||
2543|Bridgewater Formation|60953|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Calcreted aeolianite.||||||
2543|Bridgewater Formation|60958|5|Briefly described|Map Legend|Holocene|Pleistocene|Medium-grained, large scale cross-bedded calcarenite and calcareous aeolianite with numerous palaeosol horizons and capped by calcrete.||||||
2543|Bridgewater Formation|61070|5|Briefly described|Map Legend|Late Pleistocene|Middle Pleistocene|Soft, white to cream-fawn fine to medium-grained aeolian calcarenite. Multiple coalescing horizons of calcrete. Tabular foresets  with interbeds of silt. Underlies: Wiabuna Formation.||||||15-MAY-13
2543|Bridgewater Formation|61108|5|Briefly described|map legend|Pleistocene|Pleistocene|Calcreted aeolianite.||||||
2543|Bridgewater Formation|61121|5|Briefly described|Map legend|Pleistocene|Pleistocene|Medium-grained, large-scale calcarenite and calcareous aeolianite, numerous paleosol horizons;capped by thick laminar to powdery or bouldery calcrete. Cavernous in places with abundant rhizomorphs and solution pipes. Upper and lower members differentiated||||||07-JUN-05
2543|Bridgewater Formation|61155|5|Briefly described|p6, p17|Pleistocene|Pleistocene|Series of beach ridge/dune complexes. Overlies Coomandook Formation (Polda Basin and Aire Peninsula) and Wannaeue Formation in Melbourne area. Geological Province: Otway and Murray Basins/coastal margins; Polda Basin, Eyre Peninsula. See also p18.||||||03-MAR-10
2543|Bridgewater Formation|61181|5|Briefly described|p136, p183|Pleistocene|Pleistocene|Largely derived from Tertiary bryozoal limestone, siliceous sand and lime fixed by groundwater percolation. Composition and hardness vary from place to place. Underlies Malanganee Sands. ||||||
2543|Bridgewater Formation|61307|5|Briefly described|p34, p65 Fig. 29|Tertiary|Tertiary|Includes calcareous sandstones. See also p71-75 Figs. 32-36.||||||15-JAN-08
2543|Bridgewater Formation|62068|5|Briefly described|p136,p137,|||[Misspelling of Bridgewater Group?]||||Unconformably overlies Nelson Bay Formation. Appears to say this unit is?mid-?late Pliocene on p37, but they may be referring to the Hanson Plain Sands equivalent.|Series of consolidated cross-bedded dune sands.|
2543|Bridgewater Formation|62893|4|Described|Map Legend, p22-25, p38, p40|Pleistocene|Pleistocene|Reflects widespread coastal and inland dune and loess deposits. Forms spectacular cliffs near Sheringa and low undulating terrain inland. Maximum thickness of over 140 m, although much thinner (less than 1 m) away from the coast. Divided into [informal] lower and upper members. Calcarenite horizons constitute important freshwater aquifers. Overlies and blankets both Tertiary sediments and Archaean-Proterozoic basement. Intertongues with and is laterally equivalent to the Glanville Formation.||||Disconformably overlain by Semaphore Sand. Equivalent to Glanville Formation.|Calcareous aeolianite dunes and associated calcrete horizons.|
2543|Bridgewater Formation|62898|5|Briefly described|p197, p205|Pleistocene|Pleistocene|In Eyre Peninsula, S.A.||||||
2543|Bridgewater Formation|63124|5|Briefly described|p92, p93|||Unconformably overlies Green Point Member (Gambier Limestone). May overlie Camelback Member (Gambier Limestone) unconformably.  Geological Province: Otway Basin. ||||||
2543|Bridgewater Formation|63446|5|Briefly described|Map legend|Pleistocene|Pleistocene||||||Aeolian: dune deposits, calcarenite.|
2543|Bridgewater Formation|64282|5|Briefly described|Map legend|Pleistocene|Pleistocene|Medium-grained, lg.scale X-bedded calcarenite + calcareous aeolianite with numerous palaeosol horizons, capped by thick, laminar to powdery or bouldery calcrete; cavernous in places with abundant rhizomorphs and solution pipes; preserved dune morphology.||||||23-DEC-09
2543|Bridgewater Formation|65375|4|Described|p32, p38, pp40-41, p56.|Pleistocene|Pleistocene|Originally applied to Portland aeolianites and limestones; subsequently for calcareous dunes and bioclastic barrier shoreline complexes in S.A. Described in detail in Notes. Covers >90 % of Yorke Peninsula land area. Supplies town water for Warooka.|<0.78 Ma to 22,400 +/- 800 years.|||Unconformably overlies Cape Jervis Formation and Hindmarsh Clay. Is overlain by Saint Kilda Formation. Locally capped with calcrete.|Three units: medium-to coarse-grained, large-scale foreset bedded calcarenite with interlayered red-brown sandy clay paleosols; shells of the Glanville Formation; and an upper unit of fine- to medium-grained aeolianite and bioclastic calcarenite.|
2543|Bridgewater Formation|65376|5|Briefly described|p9 Fig.1.2. |Pleistocene|Pleistocene||||||Eolian calcareous sand, with calcrete.|
2543|Bridgewater Formation|65715|5|Briefly described|p15 Tb.8, p25|Neogene|Neogene|Six unnamed subunits recognised by Gill (1967, 1976) and elevated to group rank by Reeckman and Gill (1981). Here demoted to formation rank.||||||
2543|Bridgewater Formation|65921|5|Briefly described|p1, p2 (map legend).|Pleistocene|Pleistocene|Large coastal sand dunes. Occurs as a 50m cliff sequence at Pennington Bay. Contains over 30 caves: karren, sea caves and dolines are common.|||||Aeolian calcarenite variably cemented by pedogenic and vadose diagenetic processes and affected by karstic solution.|
2543|Bridgewater Formation|65922|5|Briefly described|p25 Tb. 4, p27|Pleistocene|Pleistocene|Pale yellow-cream calcareous gritty sandstone; aeolian calcarenite. Ripon Calcrete occurs within this unit.||||||
2543|Bridgewater Formation|66002|5|Briefly described|p13 Tb.9|Neogene|Neogene|Defined by Boutakoff and Sprigg 1953. Raised to Group in 1981, but reinstated as Formation herein.||||||
2543|Bridgewater Formation|66287|5|Briefly described|p35, 38, 40, Fig 11, 16|Pleistocene|Pleistocene|Forms a strandplain up to 100 km inland from the modern coastline; includes 13 coastal barriers.|||||Prograding calcareous sediments.|20-APR-12
2543|Bridgewater Formation|66761|5|Briefly described|p244, 246|Pleistocene|Pleistocene|26 m interval in PIRSA stratigraphic hole Investigator 1 where it overlies the White Point Conglomerate. Calcareous aeolianite.||||||14-MAR-12
2543|Bridgewater Formation|67462|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Saint Vincent Basin.||||||
2543|Bridgewater Formation|68116|5|Briefly described|Maps 29, 38, 47-48, 50, 54-55, 57.|Pleistocene|Pleistocene|Also occurs in the Appendix.|||||Calcarenite: medium to coarse grained shell fragments and minor quartz; consolidated, thin interbedded red palaeosols, minor hard calcrete capping, prominent dune cross-bedding; coastal dune deposits.|
2543|Bridgewater Formation|68131|5|Briefly described|p2 Fig.1, p7, p17, p42, p66, p71, p84|Pleistocene|Pleistocene|Aeolian sediments.|||||Calcareous sand, with calcrete.|
2543|Bridgewater Formation|68211|6|Mentioned|p28 Fig.1|Quaternary|Quaternary|||||||06-AUG-13
2543|Bridgewater Formation|68715|6|Mentioned|p31 Fig.5|Pleistocene|Pleistocene|St Vincent Basin.||||||
2543|Bridgewater Formation|68811|5|Briefly described|p67, p69, p112,113, p114, p130|Quaternary|Quaternary|See also p156 app 1, p170 tbl 31, p193 tbl 47. ||||Overlies the Uley Formation, Brighton Group and the Fyansford Formation. |Sandy sediments. |16-APR-20
2543|Bridgewater Formation|68990|6|Mentioned|p459|||Sheard (1978, 1990).|||||Sands.|
2543|Bridgewater Formation|68991|5|Briefly described|p465 Fig.2, pp467-469, p471 Fig.5|Pleistocene|Pleistocene|Upper Pleistocene age. ~ 0-100 m thick. Represents stacked coastal-dune deposits. Thermoluminescence dating of quartz grains and loess at Warrnambool gave ages ranging between 160-67 ka (Sherwood et al. 1994; Brooke 2001).|93 +/- 11 ka|||Disconformably underlain by the Port Campbell Limestone, Hesse Clay, Dog Trap Bay Sand and Cove Sand.|Comprises partially lithified, yellowish grey, cross-bedded medium-grained calcarenite of shell fragments and minor quartz grains.|20-JUL-15
2543|Bridgewater Formation|69048|6|Mentioned|p2|Cenozoic|Cenozoic|Southern Eyre Peninsula.||||||
2543|Bridgewater Formation|69297|6|Mentioned|p79|Pleistocene|Pleistocene|Otway Basin. ||||Unconformably overlies the Gambier Limestone and the Coomandook Formation. ||
2543|Bridgewater Formation|69372|6|Mentioned|p28 fig. 6, p34 fig. 12|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|70029|5|Briefly described|p151-153,156,158-159,161-163,165|Pleistocene|Pleistocene|First identified at Cape Bridgewater in western VIC (Boutakoff 1963). Represented by late early Pleistocene [Marine Isotope Stage (MIS) 23 at 933 ka] to Holocene barrier shoreline successions deposited during sea-level highstands. Up to nine morphologically distinct, relict coastal barrier landforms preserved in the Mount Gambier coastal plain that trend sub[parallel to the modern coastline. Can be correlated to barrier landforms in the Robe coastal plain, 100km NW of Mount Gambier based on lateral continuity.||||Underlain unconformably by Gambier Limestone and Coomandook/Werrikoo Limestone.|Cool water, temperate sedimentary carbonates.|
2543|Bridgewater Formation|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Holocene|Holocene|Otway Basin: Gambier Embayment and Voluta Trough, and Robe-Penola Trough.||||Overlies Coomandook Formation.||
2543|Bridgewater Formation|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Holocene|Holocene|Gambier Embayment and Voluta Trough.||||Overlies Coomandook Formation.||
2543|Bridgewater Formation|70337|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Shown as having two unnamed members in parts.|||||Bioclastic barrier shoreline deposits, silica-rich, with heavy minerals, shallow sub-tidal. Coastal, cross-bedded, aeolian calcarenite with paleosol horizons and capped by calcrete.|08-JAN-16
2543|Bridgewater Formation|70778|5|Briefly described|p4, p10|||Intersected in Nundroo 3 DDH.|||||Calc-arenite.|
2543|Bridgewater Formation|70893|6|Mentioned|p3 fig 1b|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|71419|5|Briefly described|p22|||Calcareous sandstone.||||Overlies Gellibrand Marl.||
2543|Bridgewater Formation|73026|6|Mentioned|p26|||||||||
2543|Bridgewater Formation|73027|6|Mentioned|p26, p31, p39|||Outcrops at Wanna.||||||
2543|Bridgewater Formation|73107|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Four constituent parts/facies, called members but obviously not intended as stratigraphic units, are described and mapped separately. The Glanville Formation separates the topmost from the third member.||||Is interbedded with the Glanville Formation.|Medium-grained, large-scale cross-bedded calcarenite and calcareous aeolianite with numerous paleosol horizons and capped by thick laminar to powdery or boulder calcrete. Cavernous in places. Preserved dune morphology.|
2543|Bridgewater Formation|73112|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Brownish aeolian calcarenite.|
2543|Bridgewater Formation|73122|5|Briefly described|p23, 27-28|Quaternary|Quaternary|Central Williams Island.|||||Travertine and calcareous aeolianite.|
2543|Bridgewater Formation|73228|4|Described|p50, p56-57, p60, p62|Pleistocene|Late Pliocene|Murray Basin. Outcrops as an extensive sequence of subparallel linear ridges in the southwest and is contiguous with sediments on the Gambier coastal plain. Consists of subtidal, intertidal and aeolian dune facies. Characterised by a sparse faunal assemblage comprising benthic and rare planktonic foraminifera, echinoderms, bivalves, bryozoans and articulated tidal bivalves. Variations in depositional environment are reflected in the degree of cross-bedding, from gentle (near-shore) to steep (aeolian).|||||Well-sorted, fine- to medium-grained bioclastic carbonate sand, commonly laminated and well cemented.|
2543|Bridgewater Formation|73229|6|Mentioned|p67|Pleistocene|Late Pliocene|Murray Basin.||||||
2543|Bridgewater Formation|73292|6|Mentioned|p955, p963|Pleistocene|Pleistocene||||||Eolianites of consolidated Quaternary sand dunes.|
2543|Bridgewater Formation|73302|6|Mentioned|p34|Pleistocene|Pleistocene|||||||
2543|Bridgewater Formation|73356|6|Mentioned|p3|Pleistocene|Pliocene|||||Unconformably underlain by Heytesbury Group.|Shallow marine sediments and basalts.|
2543|Bridgewater Formation|73383|5|Briefly described|p3|Pliocene|Pliocene|||||Overlies Heytesbury Group, underlies Newer Volcanics.|Sandstones.|
2543|Bridgewater Formation|73385|5|Briefly described|p3-5|Pleistocene|Pliocene|Otway Basin. Overlies late-Miocene unconformity.||||Unconformably overlies Heytesbury Group, Bridgewater Formation, underlies Newer Volcanics.|Shallow marine and nearshore sandstones.|
2543|Bridgewater Formation|73386|5|Briefly described|p2, p4-5, p7, p14, iii|Pleistocene|Pliocene|Otway Basin. Deposited following widespread tectonic uplift in the Pliocene.|||Albert Park Aeolianite, Armstrong Sand, Moyne Alluvium, Port Fairy Calcarenite, Sunnyside Sand, Warrnambool Aeolianite, Bats Ridge Member, Descartes Bay Member, Duquesne Member.|Overlies Heytesbury Group, underlies Newer Volcanics|Shallow marine sediments, sequence of relatively thin localised units.|
2543|Bridgewater Formation|73493|5|Briefly described|p715 Fig.2, p717, p718 Fig.5|Pleistocene|Pliocene|Cover sequence.||||Overlies Donington Suite|Includes calc-arenite.|
2543|Bridgewater Formation|73594|5|Briefly described|p4, p6|Pliocene|Pliocene|Otway Basin. See also Bridgewater Bay Group p6.||||Underlies Newer Volcanics|Shallow marine and nearshore sandstones.|
2543|Bridgewater Formation|73634|6|Mentioned|p7|||Williams Island, Jussieu Peninsula. Age given as Tertiary.||||||
2545|Bridgewater Granite|42726|5|Briefly described|map legend|Early Devonian||709. NOT variation on Bridgewater Formation. Invalid name.||||||
2545|Bridgewater Granite|65969|6|Mentioned|p6 Fig.2|||Magnetic. Peraluminous, high-Na chemistry. Contains hornblende, sphene and allanite or monazite, and strongly magnetic phases. Referred to as Loddon Vale pluton on p.15.||||||
35859|Bridle Track Granodiorite|23332|5|Briefly described|1109|||||||||
41182|Brimboal Granodiorite|50154|2|Defined|p75, p79, p248 App.5|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex. Corresponds to part of the Wando Granodiorite of Wells (1956). Replaces the Meissen Granodiorite of Anderson (1990), as the name has no geographic entity. Intrudes the Snake River Tonalite.||||||15-SEP-04
41182|Brimboal Granodiorite|50155|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Biotite-hornblende granodiorite||||||25-JUN-04
41182|Brimboal Granodiorite|50156|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-hornblende granodiorite||||||20-AUG-04
41182|Brimboal Granodiorite|50157|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-hornblende granodiorite||||||20-AUG-04
41182|Brimboal Granodiorite|50158|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-hornblende granodiorite||||||20-AUG-04
41182|Brimboal Granodiorite|50159|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-hornblende granodiorite||||||20-AUG-04
41182|Brimboal Granodiorite|50160|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-hornblende granodiorite||||||20-AUG-04
41182|Brimboal Granodiorite|50161|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-hornblende granodiorite||||||20-AUG-04
41182|Brimboal Granodiorite|50162|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-hornblende granodiorite||||||20-AUG-04
41182|Brimboal Granodiorite|50163|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-hornblende granodiorite||||||20-AUG-04
41182|Brimboal Granodiorite|50164|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Biotite-hornblende granodiorite||||||
41182|Brimboal Granodiorite|66002|6|Mentioned|p9 Tb.5|||G438. Defined by Morand et al. 2003.||||||
41182|Brimboal Granodiorite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Biotite-hornblende granodiorite: foliated to massive, bluish-grey, medium to coarse grained, equigranular; occasional biotite-rich microgranitoid enclaves; accessory magnetite; magnetic.|
37530|Bringalbert Gabbro|23309|4|Described|p26-27, Table 2.14, App 1|Early Cambrian|Early Cambrian|G440.  Age: 524+/-9Ma (SHRIMP U/Pb).||||||22-FEB-10
37530|Bringalbert Gabbro|24551|5|Briefly described|p78|Early Cambrian|Early Cambrian|||||||
37530|Bringalbert Gabbro|50154|5|Briefly described|p58|Cambrian|Cambrian|Age: 524 +/- 9 Ma (U/Pb; Maher et al., 1997)||||||
37530|Bringalbert Gabbro|71593|6|Mentioned|p19, p22|||Glenelg Zone.||||||
21330|Brissces Hut Andesite|23309|5|Briefly described|p36 Table 2.7|||Of the Jamieson Volcanics.||||||
21330|Brissces Hut Andesite|24551|5|Briefly described|p87|||Of Jamieson Volcanics (fig.3.15)||||||
21330|Brissces Hut Andesite|24576|6|Mentioned|p731|||Geological Province: Lachlan Fold Belt||||||
21330|Brissces Hut Andesite|61187|5|Briefly described|p50.|Early Cambrian|Early Cambrian|||Unit in Jamieson Volcanics.||Faulted against Warrambat Andesite Breccia.||
21330|Brissces Hut Andesite|68116|5|Briefly described|Appendix, Map 34.|Cambrian|Cambrian||||||Andesite lava, clinopyroxene-phyric; marine.|
27348|Broadford Formation|22885|5|Briefly described|map|Late Silurian|Late Silurian|||||||
27348|Broadford Formation|22886|5|Briefly described|p14|Devonian|Devonian|||||||
27348|Broadford Formation|23108|5|Briefly described|p518|Early Devonian|Early Devonian|||||||
27348|Broadford Formation|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
27348|Broadford Formation|23309|4|Described|p141, 153, 270  Figure 3.24|||Overlies the Dargile Formation.||||||
27348|Broadford Formation|24177|3|Fully described|p55, p50 Fig.22|Pridoli|Ludlow|Overlain by the Puckapunyal Formation. Overlies the Dargile Formation. Geological Province: Melbourne Trough. Maximum Thickness: 2km. Correlates with the McIvor Sandstone.||||||
27348|Broadford Formation|24328|5|Briefly described|Map legend|Late Silurian|Late Silurian|||||||
27348|Broadford Formation|24329|5|Briefly described|Map legend|Late Silurian|Late Silurian|||||||
27348|Broadford Formation|31654|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27348|Broadford Formation|33238|6|Mentioned|p642|||||||||
27348|Broadford Formation|35283|6|Mentioned|p53|||||||||
27348|Broadford Formation|39331|4|Described|p22|||See p23.Pragian||||||15-JAN-07
27348|Broadford Formation|44197|5|Briefly described|Map Legend||Late Silurian|||||||
27348|Broadford Formation|60083|5|Briefly described|Map legend|Early Devonian|Early Devonian|Interbedded siltstone and sandstone with minor greywacke-conglomerate intervals (turbidites).||||||
27348|Broadford Formation|60529|5|Briefly described|Map Legend|Lochkovian|Ludlow|Submarine channel and upper fan deposits: turbiditic sandstones; medium to thickly bedded, massive quartz arenite and quartz-lithic arenite, with current ripples, and polymitic conglomerate.||||||
27348|Broadford Formation|60591|5|Briefly described|Map Legend|Pridoli|Ludlow|Overlies the Dargile Foramtion. Overlain by the Puckapunyal Formation. Turbiditic sandstone, massive quartz arenite and quartz-lithic arenite||||||
27348|Broadford Formation|60592|5|Briefly described|Map Legend|Pridoli|Ludlow|Overlies the Dargile Foramtion. Overlain by the Puckapunyal Formation. Turbiditic sandstone, massive quartz arenite and quartz-lithic arenite.||||||03-FEB-09
27348|Broadford Formation|60593|5|Briefly described|Map Legend|Pridoli|Ludlow|Overlies the Dargile Foramtion. Overlain by the Puckapunyal Formation. Turbiditic sandstone, massive quartz arenite and quartz-lithic arenite||||||
27348|Broadford Formation|60595|5|Briefly described|Map Legend|Pridoli|Ludlow|Overlies the Dargile Foramtion. Overlain by the Puckapunyal Formation. Turbiditic sandstone, massive quartz arenite and quartz-lithic arenite||||||
27348|Broadford Formation|60596|5|Briefly described|Map Legend|Pridoli|Ludlow|Overlies the Dargile Foramtion. Overlain by the Puckapunyal Formation. Turbiditic sandstone, massive quartz arenite and quartz-lithic arenite||||||
27348|Broadford Formation|60597|5|Briefly described|Map Legend|Pridoli|Ludlow|Low magnetic responses, with weak magnetic linear features; low to moderate K and Th||||||
27348|Broadford Formation|60599|3|Fully described|p14, p24 Tb.4, p56, p68, p107, p99|Pridolian|Late Ludlow|Interfingers with Humevale Siltstone; probable lateral equivalent to McIvor Sst. Conformably overlies Dargile Fm. Gradationally overlain by Puckapunyal Fm, which also partly overlies Dargile Fm.  Max. thickness:<2km. Lithological details included.||||||
27348|Broadford Formation|61185|2|Defined|p26-31, p22, p23, p34, p24-25 Fig. 7|Pridolian|Late Ludlow|Massive sandstones (basal diamictite conglomerates) and interbedded turbidites. Conformably overlies Dargile Fm. Under/over/interfingers with Humevale Fm. Under Puckapunyal and Waranga Formations. Max. thickness: ~500m. Geol.Prov: LFB, Melbourne Zone.||||||07-FEB-11
27348|Broadford Formation|61701|5|Briefly described|Map Legend|Lochkovian|Ludlow|Submarine channel and upper fan deposits: turbiditic sandstones; medium to thickly bedded, massive quartz arenite and quartz-lithic arenite, with current ripples, and polymitic conglomerate.||||||25-JUL-06
27348|Broadford Formation|61702|5|Briefly described|Map Legend|Lochkovian|Ludlow|Submarine channel and upper fan deposits: turbiditic sandstones; medium to thickly bedded, massive quartz arenite and quartz-lithic arenite, with current ripples, and polymitic conglomerate.||||||25-JUL-06
27348|Broadford Formation|61703|5|Briefly described|Map Legend|Lochkovian|Ludlow|Submarine channel and upper fan deposits: turbiditic sandstones; medium to thickly bedded, massive quartz arenite and quartz-lithic arenite, with current ripples, and polymitic conglomerate.||||||25-JUL-06
27348|Broadford Formation|61704|6|Mentioned|Map legend|Silurian|Silurian|Low moderate K and Th, with bands of high K and Th.||||||27-OCT-08
27348|Broadford Formation|64612|6|Mentioned|p8|||||||||07-FEB-11
27348|Broadford Formation|65969|6|Mentioned|p17 Fig.7|||||||||
27348|Broadford Formation|66244|5|Briefly described|p3.|||Interfingers with Humevale Siltstone. Thins to south and southeast. In the Whittlesea area, is laterally equivalent to Clonbinane and Mount Phillipa Members. In the Flowerdale area, this unit is mapped as Killingworth Formation and Flowerdale Member on the Kinglake 1:63 360 sheet (Garratt 1977) where it occupies the cores of synclines.||||Interfingers with, and locally overlies, Humevale Siltstone.||
27348|Broadford Formation|66769|6|Mentioned|p127 Fig.8d, Fig 13|||Melbourne Zone. Is overlain by Puckapunyal Formation.||||||
27348|Broadford Formation|68116|5|Briefly described|Appendix, Maps 24-25, 32-33, 42.|Pridoli|Llandovery||||||Medium- to thickly-bedded, massive quartz arenite and quartz-litharenite with current ripples, and polymictic conglomerate; interbedded with thinly bedded fine-grained turbiditic sandstone, siltstone and claystone.|
27348|Broadford Formation|69089|5|Briefly described|Map legend|Late Silurian|Late Silurian||||||Marine: thin to thick bedded siltstone, sandstone, conglomerate.|
27348|Broadford Formation|70487|5|Briefly described|p8 Fig.1, p11 Fig5, p7-10, p12, p14|Lochkovian|Llandovery|Includes fossiliferous sandstone yielding brachiopods and bivalves. Fossils clearly indicate age in the Boucotia australis biozone of Garratt (1983a) for the localities examined in this paper. Definition regarded as deficient by Sandford (2002) who recommended that parts of the outcrop be assigned to Mount Ida Formation, on the basis of trilobites.|||Includes Flowerdale Member|Dargile Formation underlies, Humevale Siltstone interfingers + overlies. Overlain by Puckapunyal Formation, Wilson Creek Shale, Easts Lookout Siltstone. Correlated with Stoddart Member, Mount Ida Fm.|Interbedded siltstone and sandstone with minor greywacke-conglomerate intervals (turbidites).|
27348|Broadford Formation|73497|5|Briefly described|Map legend|Silurian|Silurian|Marine.||Murrindindi Supergroup|||Siltstone, sandstone, conglomerate: low magnetic responses, weak magnetic linear features of short strike length (up to 6 km); low-moderate K and Th, some weak bands (particularly K) are parallel to strike.|
72936|Broadmeadows Granite|61186|6|Mentioned|p51|||Probably a trade name for a diimension stone. Also referred to as Bulla (Broadmeadows) Granite.||||||17-DEC-07
23423|Brodribb Granodiorite|22876|4|Described|p24|||||||||
23423|Brodribb Granodiorite|22877|5|Briefly described|map|Silurian|Silurian|Currowong Suite. Biotite granodiorite. I-Type.||||||26-OCT-04
23423|Brodribb Granodiorite|23309|5|Briefly described|p344, 350.|Silurian|Silurian|G49.  Age: 414+/-3Ma||||||
23423|Brodribb Granodiorite|41850|6|Mentioned|p431|||||||||
23423|Brodribb Granodiorite|42627|5|Briefly described|Map legend|Wenlock||||||||
23423|Brodribb Granodiorite|42647|4|Described|p40|||||||||
23423|Brodribb Granodiorite|42827|5|Briefly described|p431|||||||||
23423|Brodribb Granodiorite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Biotite granodiorite: medium grained, greyish blue; I-type.|
37634|Broken Leg Granite|23309|6|Mentioned|p425, Appendix 1|||G46, I-type. Supersedes Pinnak Granite.||||||
37634|Broken Leg Granite|23938|6|Mentioned|p70 Tb. 6|||See also p75 Fig. 27.||||||25-SEP-08
37634|Broken Leg Granite|24551|6|Mentioned|p235|||See also Pinnack Granite||||||
37634|Broken Leg Granite|43312|5|Briefly described|Map Legend|Wenlock|Wenlock|G46. Hornblende-biotite granodiorite, grey-green, medium-grained, weathered, I-Type.||||||
37634|Broken Leg Granite|60542|4|Described|p91, p88 Tb. 4|||Previously Pinnak Granite. Occurs in a number of small outcrops near Mount Pinnak. Deeply weathered, forming flat pavements of decomposed quartz and seriicitised feldspar grains in a green clay-rich matrix.||||||
37634|Broken Leg Granite|61187|6|Mentioned|p123 Fig.8, p124.|||||||||
37634|Broken Leg Granite|68116|5|Briefly described|Appendix.|Devonian|Silurian||||||Hornblende-biotite granodiorite: grey-green, medium-grained, weathered; I-type.|
32563|Brookville Granite|22968|5|Briefly described|P186, P188||Early Devonian|New name, parent is Swifts Creek Igneous Complex||||||
32563|Brookville Granite|23020|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Swifts Creek Igneous Complex||||||
32563|Brookville Granite|23030|5|Briefly described|Map legend|Early Devonian|Late Silurian|Parent is the Swifts Creek Igneous Complex. G545: granite: I-type; nonmagnetic; moderate K, Th, low to moderate U. G545b: tonalite, quartz diorite, hornblendite: I-type; highly magnetic (300 nT); low K, Th, low to moderate U.||||||15-SEP-04
32563|Brookville Granite|23309|6|Mentioned|p425, App1|||G545. I-Type||||||
32563|Brookville Granite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Granite: pale pink to cream; medium-grained; massive; minor dark coarse-grained hornblendite and quartz diorite on southern and western margins.|
41868|Brothers Syenite|24551|5|Briefly described|p138|Triassic|Triassic|Geological province: Lachlan Fold Belt.  Its contact aureole encircles a limestone body known as Pyles deposit which lies directly on deformed Lower Ordovician Pinnak Sandstone.||||||05-FEB-15
41868|Brothers Syenite|60503|4|Described|p180, p41 Tb. 2|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Coarsely porphyritic syenite. Consists of rectangular phenocrysts of K-feldspar with plagioclase, quartz and hornblende, biotite and magnetite.||||||
41868|Brothers Syenite|60504|5|Briefly described|Map Legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Hornblende-biotite syenite: A-type; grey, coarsely porphyritic in the south and northeast, equigranular in the northwest, phenocrysts are orthoclase.||||||20-OCT-04
41868|Brothers Syenite|60505|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Hornblende-biotite syenite: A-type; grey, coarsely porphyritic in the south and northeast, equigranular in the northwest, phenocrysts are orthoclase.||||||21-OCT-04
41868|Brothers Syenite|60506|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Hornblende-biotite syenite: A-type; grey, coarsely porphyritic in the south and northeast, equigranular in the northwest, phenocrysts are orthoclase.||||||21-OCT-04
41868|Brothers Syenite|60507|5|Briefly described|Map Legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Hornblende-biotite syenite: A-type; grey, coarsely porphyritic in the south and northeast, equigranular in the northwest, phenocrysts are orthoclase.||||||21-OCT-04
41868|Brothers Syenite|60508|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Syenite: A-type; 232+/-5 Ma (K/Ar biotite); nonmagnetic and intensely magnetic (0-750 nT) northwest trends; high total count, K, Th, U in northwest.||||||
41868|Brothers Syenite|68116|5|Briefly described|Appendix, Map 27.|Triassic|Triassic||||||Hornblende-biotite syenite: grey, coarsely porphyritic in the south and northeast, equigranular in the northwest; phenocrysts are orthoclase.|
34698|Brucknell Member|22875|5|Briefly described|p26 Table1|||Of the Mepunga Formation.||||||31-JAN-07
34698|Brucknell Member|61182|4|Described|p25, p26, p172|Early Oligocene|Late Eocene|Equiv. to Brucknell Fm (Blake 1980). Unit of clayey silt separating upper and lower Mepunga sand units within Mepunga Fm (Nirranda Group). Dark brown, carbonaceous clayey silt to silty clay, often burrowed; richly fossiliferous in places. Max. thick: 36m.||||||
2706|Brumby Mafic Arenite Member|22968|5|Briefly described|P51, P104|||Parent is Blueys Creek Formation||||||
2706|Brumby Mafic Arenite Member|23021|5|Briefly described|Map legend|Late Ordovician|Late Ordovician|Parent is the Blueys Creek Formation||||||
2706|Brumby Mafic Arenite Member|23309|5|Briefly described|p60  Table 2.20|||Parent Kiandra Group.||||||
2706|Brumby Mafic Arenite Member|23615|5|Briefly described|p67|Late Ordovician|Late Ordovician|Of Blueys Creek Formation. Black cherty slate/mafic arenite turbidite.||||||
2706|Brumby Mafic Arenite Member|24551|5|Briefly described|p106|Late Ordovician|Late Ordovician|Of Blueys Creek Formation.||||||
2706|Brumby Mafic Arenite Member|41570|6|Mentioned|p92|||Of Blueys Creek Formation, Limestone Creek Graben.||||||
2706|Brumby Mafic Arenite Member|63278|4|Described|p157|Gisbornian|Darriwilian |Of Blueys Creek Formation, Kiandra Group. Underlain by Banksia Chert Member. Geological Province: Kiandra Volcanic Belt, LFB. Consists of cherts and volcaniclastic turbidites.||||||07-FEB-11
2706|Brumby Mafic Arenite Member|67322|6|Mentioned|p26|Sandbian|Darriwilian|Age is constrained by that of the parent Blueys Creek Formation.||Of the Blueys Creek Formation||||
2725|Brunton Avenue Breccia Member|29982|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
37257|Bryan Creek Granodiorite|24012|3|Fully described|p224 appendix 1|||||||||
37257|Bryan Creek Granodiorite|50154|2|Defined|p95, p247 App.5|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex. Thickness: 150-200m.||||||15-SEP-04
37257|Bryan Creek Granodiorite|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Biotite-muscovite granodiorite; S-type||||||
37257|Bryan Creek Granodiorite|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamoprhic Complex? Biotite-muscovite granodiorite||||||20-AUG-04
37257|Bryan Creek Granodiorite|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamoprhic Complex? Biotite-muscovite granodiorite||||||20-AUG-04
37257|Bryan Creek Granodiorite|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamoprhic Complex? Biotite-muscovite granodiorite||||||20-AUG-04
37257|Bryan Creek Granodiorite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamoprhic Complex? Biotite-muscovite granodiorite||||||20-AUG-04
37257|Bryan Creek Granodiorite|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamoprhic Complex? Biotite-muscovite granodiorite||||||20-AUG-04
37257|Bryan Creek Granodiorite|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamoprhic Complex? Biotite-muscovite granodiorite||||||20-AUG-04
37257|Bryan Creek Granodiorite|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamoprhic Complex? Biotite-muscovite granodiorite||||||20-AUG-04
37257|Bryan Creek Granodiorite|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamoprhic Complex? Biotite-muscovite granodiorite||||||20-AUG-04
37257|Bryan Creek Granodiorite|66002|6|Mentioned|p9 Tb.5|||G445. Defined by Kemp et al. 2002||||||
37257|Bryan Creek Granodiorite|68116|5|Briefly described|Appendix.|Early Ordovician|Middle Cambrian||||||Biotite-muscovite granodiorite: foliated, grey, medium grained, porphyritic with phenocrysts of plagioclase and alkali feldspar; accessory sillimanite; biotite, muscovite, and micaceous selvedges define foliation; enclaves of schist; non-magnetic.|
75714|Bryce Plain Basalt|66244|5|Briefly described|p6.|Oligocene|Eocene|New name. This unit occupies much of the Howitt Province of Wellman (1974) and Price et al. (2003). Consists mainly of erosional remnants on the Mount Howitt - Mount Tamboritha plateau.||||Overlies unconformably the Snowy Plains Formation.|Tholeiitic and alkali olivine basalts, with some hawaiite and rare nephelinite.|
75714|Bryce Plain Basalt|68115|5|Briefly described|p9.|Cenozoic|Cenozoic|Replaces Older Volcanic Group on the Howitt Plateau, and outliers at Mount Buller and north of Mirimbah. Described in Morand (2010).||||||
75714|Bryce Plain Basalt|68116|5|Briefly described|Appendix, Maps 34, 43.|Rupelian|Priabonian||||||Alkali olivine basalt, minor olivine tholeiite, minor hawaiite, rare nephelinite: lava flows and plugs, interbedded sedimentary rocks. Dense, blue-black, rarely vesicular, typically strongly jointed.|
24199|Bryo Gully Shale|23309|5|Briefly described|p52  Table 2.16, p42 Fig. 2.14|||||||||30-JAN-15
24199|Bryo Gully Shale|40136|5|Briefly described|p18|||||||||
24199|Bryo Gully Shale|41570|4|Described|p85|||||||||
24199|Bryo Gully Shale|42560|6|Mentioned|p51|||||||||
24199|Bryo Gully Shale|42628|5|Briefly described|Map legend|Lancefieldian||||||||
24199|Bryo Gully Shale|42790|5|Briefly described|Fig.14 P189|||||||||
24199|Bryo Gully Shale|42826|2|Defined|p27|Early Ordovician||of Romsey Group||||||
24199|Bryo Gully Shale|42827|5|Briefly described|p85|||see also Fig 3.8||||||
24199|Bryo Gully Shale|65715|5|Briefly described|p4 Tb.2|Ordovician|Ordovician|Of Romsey Subgroup. Formation rank.||||||
24199|Bryo Gully Shale|68116|5|Briefly described|Appendix, Map 32.|Floian|Tremadocian|Age written as Lancefieldian in text.|||||Siltstone, shale: black; generally thin-bedded; siliceous in basal portion; contains sporadic graptolites.|
23429|Buangor Granite|22756|5|Briefly described|P42|||||||||
23429|Buangor Granite|23309|5|Briefly described|p425 App1|||G377. I-Type||||||
23429|Buangor Granite|23810|5|Briefly described|Table 1, p886, p888||Devonian|Felsic I-Type. Age: 372+/-2 Ma (SHRIMP U-Pb age). Of Mt Cole Suite. Lachlan Fold Belt.||||||
23429|Buangor Granite|42726|5|Briefly described|map legend|Early Devonian||Reserved 1993.||||||
23429|Buangor Granite|43260|5|Briefly described|Map Legend||Early Devonian|Of the Mount Cole Suite. Hornblende-biotite granite: pale grey to pink; speckled appearance; porphyritic texture, with phenocrysts of perthitic K-feldspar. Granophyric intergrowths common. Rare mafic clots of hornblende and biotite.||||||27-OCT-04
23429|Buangor Granite|44186|5|Briefly described|Map Legend||Early Devonian|G377 I-type.||||||
23429|Buangor Granite|66002|5|Briefly described|p7 Tb.5|||Of Mount Cole Suite. G377.  Defined by Cayley and McDonald 1995.||||||
23429|Buangor Granite|67978|5|Briefly described|p496 Fig.1, p499 Tb.1|Famennian|Frasnian|Zircon dating by Bierlein et al. (2001b).|372 +/- 2 Ma, SIMS U-Pb|Of the Mount Cole Suite.||||19-SEP-14
23429|Buangor Granite|68116|5|Briefly described|Appendix, Map 31.|Early Devonian|Early Devonian||||||Hornblende-biotite granite: pale grey to pink; speckled appearance; porphyritic texture, with phenocrysts of perthitic K-feldspar; granophyric intergrowths common; rare mafic clots of hornblende and biotite.|
23429|Buangor Granite|75072|6|Mentioned|p250|||Has the least degree of zircon inheritance of the samples graphed (see Bierlein et al., 2001). Appears as Buangor Granodiorite.|||||I-type.|
2750|Buchan Caves Limestone|5178|6|Mentioned|p106, p113||Lower Devonian|||||||
2750|Buchan Caves Limestone|22520|6|Mentioned|p18|Emsian|Emsian|||||||
2750|Buchan Caves Limestone|22968|4|Described|P15, P32, P149|Devonian|Devonian|Lowest Formation in the Buchan Group, unconformably overlain by the Taravale Marlstone, underlying unit is Roadsend Formation, maximum thickness is 295m||||||
2750|Buchan Caves Limestone|23021|5|Briefly described|Map legend|Emsian|Pragian|Of the Buchan Group; overlying unit is the Taravale Limestone, underlying unit is the Snowy River Volcanics||||||30-JAN-07
2750|Buchan Caves Limestone|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Buchan Group.||||||30-JAN-07
2750|Buchan Caves Limestone|23229|6|Mentioned|p35||Pragian|||||||
2750|Buchan Caves Limestone|23275|6|Mentioned|p467||Early Devonian|||||||
2750|Buchan Caves Limestone|23308|6|Mentioned|Map Legend|||Mine name?||||||
2750|Buchan Caves Limestone|23309|4|Described|p114, 126-128, 132  Table 2.41|||Of the Buchan Group.||||||
2750|Buchan Caves Limestone|23522|5|Briefly described|p247 Fig 3|Early Devonian|Early Devonian|||||||
2750|Buchan Caves Limestone|23615|3|Fully described|p137, p84, p215,218 App. 2|Middle Devonian|Emsian|Formerly called Cave Limestone (Teichert, 1948; Hill, 1950). Same unit also named Gillingall, Butcher's Ridge, Basin and Jackson's Crossing Limestones - termed "Buchan Caves Limestone and Equivalents" in Teichert and Talent (1958). Of Buchan Group. Richly fossiliferous late Pragian? or Emsian age.||||||15-JAN-13
2750|Buchan Caves Limestone|23710|14|Not recorded|p74|||Stratigraphy.||||||
2750|Buchan Caves Limestone|23938|5|Briefly described|p11, p63-65 Figs. 23-24.|||Basal unit of the Buchan Group. Dolomite and dolomitic limestone. Overlies the Snowy River Volcanics. See also p54-55 Tb. 4, p96.||||||
2750|Buchan Caves Limestone|24551|4|Described|p147, p139 Fig. 5.30|Early Devonian|Early Devonian|Of Buchan Group. ||||||
2750|Buchan Caves Limestone|24598|5|Briefly described|p514|Early Devonian|Early Devonian|Max. thickness: 200m.  Geological Province: Lachlan Orogen.  See also p517.||||||
2750|Buchan Caves Limestone|29860|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
2750|Buchan Caves Limestone|29878|6|Mentioned|p71|||Middle Devonian||||||
2750|Buchan Caves Limestone|30245|6|Mentioned|p80|||||||||
2750|Buchan Caves Limestone|30574|6|Mentioned|p12|||||||||
2750|Buchan Caves Limestone|30597|6|Mentioned|p33|||Lower Devonian age. Conodonts||||||
2750|Buchan Caves Limestone|30938|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
2750|Buchan Caves Limestone|31060|6|Mentioned|p33|||Re - geology||||||
2750|Buchan Caves Limestone|31161|5|Briefly described|PA11|||||||||
2750|Buchan Caves Limestone|31331|6|Mentioned|p182|||||||||
2750|Buchan Caves Limestone|31334|6|Mentioned|p663|||||||||
2750|Buchan Caves Limestone|31502|5|Briefly described|p95|||Devonian corals. Age.||||||
2750|Buchan Caves Limestone|31503|6|Mentioned|p2|||||||||
2750|Buchan Caves Limestone|32623|6|Mentioned|p4|||Refers Philip & Pedder(1968), Philip(1966).||||||
2750|Buchan Caves Limestone|32892|6|Mentioned|p222|||||||||
2750|Buchan Caves Limestone|32984|6|Mentioned|p342|||Correlation chart||||||
2750|Buchan Caves Limestone|32985|6|Mentioned|Fig.2|||Correlation chart||||||
2750|Buchan Caves Limestone|33154|5|Briefly described|p6|||||||||
2750|Buchan Caves Limestone|33156|6|Mentioned|p132|||||||||
2750|Buchan Caves Limestone|33326|6|Mentioned|p435|||Fauna.||||||
2750|Buchan Caves Limestone|33393|6|Mentioned|p161|||||||||
2750|Buchan Caves Limestone|33434|6|Mentioned|p80|||||||||
2750|Buchan Caves Limestone|33481|6|Mentioned|Fig.1|||Couvinian ? See also p14.||||||30-JAN-07
2750|Buchan Caves Limestone|33602|6|Mentioned|p31|||||||||
2750|Buchan Caves Limestone|33603|6|Mentioned|Map legend|Devonian|Devonian|||||||
2750|Buchan Caves Limestone|33606|4|Described|p65|||||||||
2750|Buchan Caves Limestone|33732|5|Briefly described|Table III|||||||||
2750|Buchan Caves Limestone|34031|6|Mentioned|p277|||M.Dev.  See also pp282,284,285 and Fig.2.||||||30-JAN-07
2750|Buchan Caves Limestone|34250|6|Mentioned|p11|||||||||
2750|Buchan Caves Limestone|34403|6|Mentioned|p146|||||||||
2750|Buchan Caves Limestone|34519|6|Mentioned|p44|||||||||
2750|Buchan Caves Limestone|34926|6|Mentioned|p120|||||||||
2750|Buchan Caves Limestone|34954|6|Mentioned|Fig.34|||Analysis Fig.33.||||||
2750|Buchan Caves Limestone|34964|6|Mentioned|p452|||||||||
2750|Buchan Caves Limestone|35112|6|Mentioned|p285|||||||||
2750|Buchan Caves Limestone|35193|6|Mentioned|p20|||||||||
2750|Buchan Caves Limestone|35274|4|Described|p420|||||||||
2750|Buchan Caves Limestone|35283|6|Mentioned|p49|||||||||
2750|Buchan Caves Limestone|36201|4|Described|p5|||||||||
2750|Buchan Caves Limestone|37330|5|Briefly described|p12|||||||||
2750|Buchan Caves Limestone|37501|6|Mentioned|p411|||||||||
2750|Buchan Caves Limestone|37586|6|Mentioned|p12|||||||||
2750|Buchan Caves Limestone|38145|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
2750|Buchan Caves Limestone|38367|6|Mentioned|Fig.1, p83|||Contains interbedded volcanic rocks.||||||16-DEC-08
2750|Buchan Caves Limestone|38545|6|Mentioned|p114|||||||||
2750|Buchan Caves Limestone|38734|6|Mentioned|p10|||||||||
2750|Buchan Caves Limestone|38787|6|Mentioned|p143|||||||||
2750|Buchan Caves Limestone|39447|4|Described|p13|||||||||
2750|Buchan Caves Limestone|39860|5|Briefly described|p11|||||||||
2750|Buchan Caves Limestone|40728|6|Mentioned|Fig.1|||||||||
2750|Buchan Caves Limestone|40761|6|Mentioned|p233|||||||||
2750|Buchan Caves Limestone|40819|6|Mentioned|p23|||||||||
2750|Buchan Caves Limestone|41585|5|Briefly described|p138|||Mention p117 and p135.||||||30-JAN-07
2750|Buchan Caves Limestone|41755|6|Mentioned|p181|||||||||
2750|Buchan Caves Limestone|41804|6|Mentioned|p168|||||||||
2750|Buchan Caves Limestone|41868|5|Briefly described|p574|||||||||
2750|Buchan Caves Limestone|42015|6|Mentioned|p316|||||||||
2750|Buchan Caves Limestone|42033|6|Mentioned|p654|||||||||
2750|Buchan Caves Limestone|42141|6|Mentioned|p569|||||||||
2750|Buchan Caves Limestone|42577|3|Fully described|p27|||||||||
2750|Buchan Caves Limestone|42635|5|Briefly described|p27|||||||||
2750|Buchan Caves Limestone|42647|6|Mentioned|p32|||||||||
2750|Buchan Caves Limestone|42967|5|Briefly described|p76|||||||||
2750|Buchan Caves Limestone|43206|5|Briefly described|map legend||Pragian|Of Buchan Group.||||||25-SEP-08
2750|Buchan Caves Limestone|43228|5|Briefly described|p10||Early Devonian|approx. 200m thick.||||||
2750|Buchan Caves Limestone|43312|5|Briefly described|Map Legend||Pragian|Of Buchan Group..||||||30-JAN-07
2750|Buchan Caves Limestone|43313|5|Briefly described|Map Legend||Pragian|Of Buchan Group.||||||30-JAN-07
2750|Buchan Caves Limestone|43461|14|Not recorded|p627|Eifelian|Emsian|Late Emsian - Eifelian||||||
2750|Buchan Caves Limestone|43525|14|Not recorded|p130,Tb p131,132|||||||||
2750|Buchan Caves Limestone|43529|14|Not recorded|p235||Siegenian|||||||
2750|Buchan Caves Limestone|43530|14|Not recorded|p1028,1029,1031|Emsian|Siegenian|U.Siegenian-L.Emsian||||||
2750|Buchan Caves Limestone|43537|14|Not recorded|p17,20,28|||Late Siegenian or Emsian. Devonian tetracorals||||||
2750|Buchan Caves Limestone|43547|14|Not recorded|p151,Tb p153,154,161||Emsian|Part of Buchan Group. Brachs = Bell Point Limestone (U.Emsian)||||||
2750|Buchan Caves Limestone|43755|6|Mentioned|Fig.9,p556|||||||||
2750|Buchan Caves Limestone|44184|5|Briefly described|Map Legend||Early Devonian|||||||
2750|Buchan Caves Limestone|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Unit in Buchan Group.|||Marine: well-bedded, dark grey, recrystallised limestone, dolomite.|
2750|Buchan Caves Limestone|44215|14|Not recorded|p359|||||||||
2750|Buchan Caves Limestone|44216|14|Not recorded|p390|||||||||
2750|Buchan Caves Limestone|45075|6|Mentioned|p29|||Devonian||||||
2750|Buchan Caves Limestone|46053|14|Not recorded|p.444,447|||||||||
2750|Buchan Caves Limestone|48971|6|Mentioned|p9,11,14,15,19,21,23|||p24,27,42.||||||
2750|Buchan Caves Limestone|50077|5|Briefly described|p7|Early Devonian|Early Devonian|Predominantly calcarenites and calcisiltites with dolomites and dolomitic limestones.  Overlain by the Taravale Formation and Murrindal Limestone.||||||
2750|Buchan Caves Limestone|60542|3|Fully described|p78, p15|Middle Devonian (Emsian)|Early Devonian|Of Buchan Gp. Parts previously mapped as Taravale Fm. Limestone sands and muds. Conformably overlies Jellung Ignimbrite; and Moores Ford Andesite. Transitional with Taravale Marlstone. Age: in 395-385Ma age range. Max. thick: 280m?||||||16-AUG-18
2750|Buchan Caves Limestone|61181|5|Briefly described|p69, p127, p129 Tb. 32||Middle Devonian|Of Buchan Gp. Incl: v. pure dolomite sections (several metres thick), upwards into normal limest, dolomite progressively decreasing. Mid-grey/black calcarenite and calcilutite;lesser algal pisolite, coquina and coral limest.Max.thick:210m. In Buchan Basin||||||
2750|Buchan Caves Limestone|61186|5|Briefly described|p87|||Of the Buchan Group - source of Victorian dimension stone. Generally a pale grey colour and highly fossiliferous. ||||||
2750|Buchan Caves Limestone|61187|5|Briefly described|pp137-140, p142 Fig.3.|Early Devonian|Early Devonian|A 40 m  section at the base of this unit is dolomitised and associated with so-far uneconomic occurrences of gold, porphyry copper and base metals.||Unit in Buchan Group.||Overlies Spring Creek Member.||
2750|Buchan Caves Limestone|63594|5|Briefly described|p1032|||Of the Buchan Group. Contains Spring Creek Member.  Underlies Taravale Formation. See also Fig. 1.||||||04-OCT-07
2750|Buchan Caves Limestone|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Buchan. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
2750|Buchan Caves Limestone|66197|5|Briefly described|p635 Fig.5c|Emsian|Emsian|Buchan Basin. Shallow marine limestone. Underlies the Taravale Marlstone, overlies the Avonmore Subgroup.||||||13-MAR-12
2750|Buchan Caves Limestone|68116|5|Briefly described|Appendix, Maps 35-36, 45.|Emsian|Pragian||||||Limestone and dolomite: black to grey; thickly bedded, graded calcarenite to calcilutite, skeletal or peloidal grainstone and wackestone; base massive, becoming more fossiliferous upwards. Some volcaniclastic sediments near the base.|
2750|Buchan Caves Limestone|70901|14|Not recorded|p6|||Age of fauna discussed.||||||
2750|Buchan Caves Limestone|73143|6|Mentioned|p11, p18|Emsian|Pragian|Contains several rugose coral species.||||||
2754|Buchan Group|22628|6|Mentioned|p117,p118|||||||||
2754|Buchan Group|22768|6|Mentioned|p178|||||||||
2754|Buchan Group|22857|6|Mentioned|p178|||||||||
2754|Buchan Group|22968|4|Described|P37, P147|Devonian|Devonian|Conformably overlies the Snowy River Volcanics||||||
2754|Buchan Group|23020|5|Briefly described|Map legend|Early Devonian|Early Devonian|Overlain by Mount Leinster Igneous Complex.||||||08-MAR-07
2754|Buchan Group|23021|5|Briefly described|Map legend|Emsian|Pragian|Unconformably and nonconformably underlies the Mount Leinster Igneous Complex||||||
2754|Buchan Group|23028|5|Briefly described|Map legend|Emsian|Pragian|||||||
2754|Buchan Group|23029|5|Briefly described|Map legend|Emsian|Pragian|Angular unconformably and nonconformably underlies the Mount Leinster Igneous Complex||||||
2754|Buchan Group|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
2754|Buchan Group|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
2754|Buchan Group|23309|4|Described|p71, 106, 114  Table 2.41|Early Devonian|Early Devonian|||||||16-AUG-18
2754|Buchan Group|23615|3|Fully described|p137, p20 Fig.6|Middle Devonian|Early Devonian|Formerly known as Buchan Limestone, Buchan Series or series, Upper Buchan beds and Bindi Limestone. Composed of 3 formations: Buchan Caves Limestone, Taravale Marlstone and Murrindal Limestone.  Age: late Early to Middle Devonian ~395-385Ma. Underlain by Snowy River Volcanics.||||||16-AUG-18
2754|Buchan Group|23710|14|Not recorded|p72|||Faulting.||||||
2754|Buchan Group|23938|5|Briefly described|p31-32 Fig. 12|Early Devonian|Early Devonian|Includes the Spring Creek Member. Marlstone, limestone, dolomite.||||||
2754|Buchan Group|24002|5|Briefly described|p228 Fig.2|Devonian|Devonian|||||||
2754|Buchan Group|24004|5|Briefly described|p275 Fig.2|Devonian|Devonian|||||||
2754|Buchan Group|24098|5|Briefly described|p27 Fig. 2|Middle Devonian|Emsian| Geological Province: Lachlan Fold Belt.||||||
2754|Buchan Group|24164|6|Mentioned|p15 Fig.8|Devonian|Devonian|Shallow marine.||||||
2754|Buchan Group|24266|5|Briefly described|p1483|||Geological Province: Lachlan Fold Belt. Underlain by Snowy River Volcanics.||||||08-MAR-07
2754|Buchan Group|24275|6|Mentioned|p1696 Fig. 2|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
2754|Buchan Group|24551|3|Fully described|p147, p118 Fig. 5.1|Devonian|Devonian|||||||
2754|Buchan Group|24598|5|Briefly described|p514|Early Devonian|Early Devonian|Geological Province: Lachlan Orogen.||||||
2754|Buchan Group|29860|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
2754|Buchan Group|30814|6|Mentioned|Table.2|||||||||
2754|Buchan Group|32585|6|Mentioned|p211|||Mid. Dev.||||||
2754|Buchan Group|33238|5|Briefly described|p644|||||||||
2754|Buchan Group|33393|6|Mentioned|p161|||||||||
2754|Buchan Group|33437|6|Mentioned|p63|||Sil.-Dev. Conodont faunas.||||||
2754|Buchan Group|33602|6|Mentioned|Table 1|||||||||
2754|Buchan Group|33603|6|Mentioned|Map legend|Devonian|Devonian|||||||
2754|Buchan Group|33606|3|Fully described|p66|||||||||
2754|Buchan Group|33608|6|Mentioned|p45|||||||||
2754|Buchan Group|33732|6|Mentioned|p111|||||||||
2754|Buchan Group|34184|6|Mentioned|p7|||Conodonts. Refers Philip(1966).||||||
2754|Buchan Group|34287|6|Mentioned|p97|||||||||
2754|Buchan Group|34405|6|Mentioned|Fig.3.9|||||||||
2754|Buchan Group|34519|6|Mentioned|p44|||||||||
2754|Buchan Group|34954|6|Mentioned|Fig.34|||||||||
2754|Buchan Group|35112|6|Mentioned|Table 1|||||||||
2754|Buchan Group|35274|6|Mentioned|p420|||||||||
2754|Buchan Group|35278|6|Mentioned|p360|||||||||
2754|Buchan Group|35283|6|Mentioned|p49|||||||||
2754|Buchan Group|36201|6|Mentioned|p2|||Mentioned throughout article.||||||
2754|Buchan Group|37330|5|Briefly described|p15|||||||||
2754|Buchan Group|37501|6|Mentioned|p414|||||||||
2754|Buchan Group|37727|6|Mentioned|p33|||||||||
2754|Buchan Group|38145|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
2754|Buchan Group|38367|6|Mentioned|p11|||||||||
2754|Buchan Group|38545|6|Mentioned|p114|||||||||
2754|Buchan Group|38734|6|Mentioned|p10|||||||||
2754|Buchan Group|39447|4|Described|p13|||||||||
2754|Buchan Group|40728|6|Mentioned|p173|||||||||
2754|Buchan Group|40761|5|Briefly described|p230|||||||||
2754|Buchan Group|41570|6|Mentioned|p91|||||||||
2754|Buchan Group|41572|5|Briefly described|p21|||||||||
2754|Buchan Group|41585|5|Briefly described|p138|||||||||
2754|Buchan Group|41755|6|Mentioned|p168|||||||||
2754|Buchan Group|41868|6|Mentioned|p574|||||||||
2754|Buchan Group|42089|6|Mentioned|p10|||||||||
2754|Buchan Group|42577|6|Mentioned|p28|||||||||
2754|Buchan Group|42635|5|Briefly described|p27|||||||||
2754|Buchan Group|42791|5|Briefly described|Fig.9 P213|||||||||
2754|Buchan Group|42827|5|Briefly described|p138|||see also Table 4.1||||||
2754|Buchan Group|42967|4|Described|p76|||||||||
2754|Buchan Group|43206|5|Briefly described|map legend|Emsian|Pragian|||||||
2754|Buchan Group|43228|5|Briefly described|p10||Early Devonian|||||||
2754|Buchan Group|43312|5|Briefly described|Map Legend||Pragian|||||||
2754|Buchan Group|43313|5|Briefly described|Map Legend||Pragian|||||||
2754|Buchan Group|43431|14|Not recorded|p1262||Early Devonian|Lower Devonian. Previously regarded as Middle Devonian||||||
2754|Buchan Group|43461|14|Not recorded|p627, 628|||||||||
2754|Buchan Group|43530|14|Not recorded|p1025,1030-1,1034|Emsian|Siegenian|U.Siegenian-L.Emsian||||||
2754|Buchan Group|43547|14|Not recorded|p147,151,Tb p153-55|Eifelian|Emsian|U.Emsian-Eifelian.||||||
2754|Buchan Group|43770|6|Mentioned|p829||Early Devonian|||||||
2754|Buchan Group|44184|5|Briefly described|Map Legend||Early Devonian|||||||
2754|Buchan Group|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian||||Includes Buchan Caves and Murrindal Limestones, and Taravale Marlstone.|||
2754|Buchan Group|48971|6|Mentioned|p9|||||||||
2754|Buchan Group|50077|5|Briefly described|p7|Early Devonian|Early Devonian|Includes the Buchan Caves Limestone and Taravale Formation.||||||
2754|Buchan Group|60503|5|Briefly described|p27|Early Devonian|Early Devonian|Marine clastics and carbonates. ||||||
2754|Buchan Group|60542|4|Described|p78, p15|Middle Devonian|Early Devonian|Comprises Buchan Caves Limestone and Taravale Marlstone in ORBOST. Overlies Snowy River Volcanics conformably, unconformably and disconformably. Largest outcrop is in Murrindal Synclinorium. See also p25.||||||
2754|Buchan Group|61180|5|Briefly described|p7|Devonian|Devonian|Limestone units overlying Snowy River Volcanics. Base metal mineralisation is concentrated into lower parts of this sequence.||||||
2754|Buchan Group|61181|5|Briefly described|p13, p127|Devonian|Devonian|In the Buchan-Murrindal area this group forms a sequence of carbonate and calcareous mudstone, in which the limestones are Buchan Caves (lower) and Murrindal Limestones (upper). ||||||
2754|Buchan Group|61186|6|Mentioned|p87|||Includes Buchan Caves Limestone and Murrindal Limestone. ||||||
2754|Buchan Group|61187|5|Briefly described|p5 Fig.3, p26 Fig.2, p29 Fig.4,  pp137ff|Early Devonian|Early Devonian|Tabberabbera Zone, Benambra Terrane. Correlative of Wentworth Group (Tabberabbera Zone, Benambra Terrane), and Lilydale Limestone and Wilson Creek Shale (Melbourne Zone, Melbourne Terrane).|||Includes Buchan Caves Limestone, Taravale Formation and Murrindal Limestone.|Overlies Snowy River Volcanics.|Nonmagnetic limestones, dolomites and calcareous silts.|
2754|Buchan Group|63594|5|Briefly described|p1032|||Includes Buchan Caves Limestone and Taravale Formation. See also Fig. 1.||||||04-OCT-07
2754|Buchan Group|66498|6|Mentioned|p43|Emsian|Emsian|Contains vertebrate macro-remains.||||||
2754|Buchan Group|68297|5|Briefly described|p184, 192|Pragian|Lochkovian|Vic. Includes possible shark scales.||||||
2754|Buchan Group|68592|6|Mentioned|p1007|Early Devonian|Early Devonian|||||Correlated with Taemas Limestone (Murrumbidgee Group). ||
2754|Buchan Group|71040|5|Briefly described|p8, p12-13, p15|Emsian|Emsian|Bindi Syncline, NE Victoria. Post-rift shallow-marine carbonates. Shows 20-30% fold shortening and reactivation of faults, due to the Tabberabberan Orogeny.||||Overlies Snowy River Volcanics.||
24200|Buckeran Diorite|23309|6|Mentioned|p425 App1|||G394. I-Type. Supersedes Buckeran Granite.||||||
24200|Buckeran Diorite|23402|3|Fully described|p23, p7 Tb. 1|Cambrian|Cambrian|Intrudes the Glenthompson Sandstone.   Geological Province: Adelaide Fold Belt||||||
24200|Buckeran Diorite|40172|6|Mentioned|Map legend|Devonian|Devonian|||||||
24200|Buckeran Diorite|40887|2|Defined|p25|Early Devonian|Early Devonian|||||||
24200|Buckeran Diorite|50371|5|Briefly described|Map Legend|Cambrian|Cambrian|Diorite||||||03-SEP-04
24200|Buckeran Diorite|61187|5|Briefly described|p69, p74 Fig.6.|Devonian|Devonian|Glenelg Zone. High magnetic response; moderate K and high Th responses. Age given on p.69 as both Cambrian and Devonian.||||Intrudes Glenthompson Sandstone.||
24200|Buckeran Diorite|63599|4|Described|p976, p978, 981|||Forms part of the Bushy Creek Igneous Complex. Medium to dark grey rocks dominated by plagioclase, hornblende and minor quartz. See also Buckeran diorite. Note: a rock said to be a dacite from a greenstone belt (sample 7) p984, appears to be shown as from Buckeran Diorite in Fig on p 977.|?495+/-2 Ma MC-ICPMS on titanite.|||||08-DEC-16
24200|Buckeran Diorite|66002|6|Mentioned|p8 Tb.5|||G394. Defined in Buckland 1986.||||||
24200|Buckeran Diorite|68116|5|Briefly described|Appendix, Map 39.|Late Cambrian|Middle Cambrian||||||Hornblende-biotite diorite with clinopyroxene cores to the hornblende and rare orthopyroxene; medium to coarse grained, equigranular. The pluton is mostly magnetic, with a non-magnetic core; weakly to non-magnetic phase not exposed.|
24200|Buckeran Diorite|70211|5|Briefly described|p3, p5, p46|||Stavely region. Titanite U-Pb age.|495.0 +/- 2.0 Ma (Whelan et al.,2007).|||||08-DEC-16
24200|Buckeran Diorite|70877|4|Described|p2, p10, p109-p122, p169, p172, |Cambrian|Cambrian|See also p186, p200. Grampians-Stavely Zone. Ballarat 1:250k and Willaura 1:100k map sheets. SHRIMP ages derived from this study and represents the age of magmatic crystallisation. Also dated at 495 +/- 2 Ma (Whelan et al., 2007) and 501.8 +/- 2.6 Ma (SHRIMP, this study). Outcrops as small boulders and tors. Petrography, zircon morphology and SHRIMP U-Pb results are discussed in detail for two samples of this unit.|502.1 +/- 2.9 Ma (SHRIMP U-Pb)|||Intrudes the Glenthompson Sandstone.|Amphibole-rich, medium to coarse-grained, equigranular, plutonic diorite with a greenish colour.|
24200|Buckeran Diorite|70967|6|Mentioned|p28|||Stavely Belt.||||||
24200|Buckeran Diorite|71593|4|Described|p9, p19, p25, p35, p40|Late Cambrian|Late Cambrian|Delamerian Orogen, Grampians-Stavely Zone. Whelan (2007) grouped this unit with the Bushy Creek Granodiorite as the Bushy Creek Igneous Complex. See also p76, p118-p119, p163, p188.|c. 502-498 Ma (Lewis et al., 2016)|Bushy Creek Igneous Complex||Intrudes the Glenthompson Sandstone.||
2804|Buckrabanyule Granite|23309|5|Briefly described|p425|||G336 S-Type. Age: 398 +/- 6Ma,  407 +/- 6 Ma||||||
2804|Buckrabanyule Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
2804|Buckrabanyule Granite|60452|4|Described|p54-55|Early Devonian|Early Devonian|Medium-grained biotite-cordierite granite; aplite and pegmatite dykes are common. Cuts the Grieves and Barrakee Granites. Age: 398 +/-6Ma (K/Ar biotite) and 407 +/-6Ma (K/Ar muscovite). See also p16, p44.||||||
2804|Buckrabanyule Granite|60461|5|Briefly described|Map legend|Early Devonian|Early Devonian|Cordierite granite, medium-grained; contains enclaves of schistose hornfels and feldspar porphyry.||||||
2804|Buckrabanyule Granite|60462|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Granite: S-type, reduced; nonmagnetic; K, Th and U responses all higher than surrounds||||||
2804|Buckrabanyule Granite|60491|4|Described|p54|Devonian|Devonian|Intrudes the Barrakee Granite. Age: 398+/-6 Ma (K/Ar biotite), 407+/-6 Ma (K/Ar muscovite). S-type.||||||
2804|Buckrabanyule Granite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Cordierite granite: S-type, reduced; associated with large amounts of aplite and pegmatite||||||
2804|Buckrabanyule Granite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Granite: reduced S-type; non-magnetic. Age: 398 +/-6 Ma (Rb/Sr)||||||
2804|Buckrabanyule Granite|66002|6|Mentioned|p6 Tb.5|||G336. Defined in Bibby and Moore 1998.||||||
2804|Buckrabanyule Granite|68116|5|Briefly described|Appendix, Map 16.|Middle Devonian|Early Devonian||||||Cordierite granite: medium grained; contains enclaves of schistose hornfels and feldspar porphyry; S-type; nonmagnetic.|
2804|Buckrabanyule Granite|68189|6|Mentioned|p42 App.2|||||||||
30583|Buckwong Granodiorite|23309|5|Briefly described|p425 App 1|Early Silurian|Early Silurian|G87. Supersedes Buckwong Granite.||||||
30583|Buckwong Granodiorite|24551|6|Mentioned|p449|Early Silurian|Early Silurian|||||||
30583|Buckwong Granodiorite|43220|6|Mentioned|p10||Silurian|||||||
30583|Buckwong Granodiorite|44184|5|Briefly described|Map Legend||Early Silurian|Shown as Buckwong S-type.||||||
30583|Buckwong Granodiorite|60503|5|Briefly described|p44 Tb. 2|Silurian|Silurian|See also Buckwong granite and Buckwong granodiorite.||||||05-SEP-05
30583|Buckwong Granodiorite|68116|5|Briefly described|Appendix, Maps 27, 28.|Wenlock|Llandovery||||||Biotite granodiorite: dark grey; medium-grained; felsic northern phase locally foliated, pink in radiometrics.|
2847|Buldah Gap Granodiorite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Hornblende-biotite granodiorite: dark grey, medium to coarse grained, mostly massive; extensive pyritic marginal phase porphyritic in quartz & feldspar, equigranular interior; prominent quartz; rare pyroxene.||||||01-OCT-04
2847|Buldah Gap Granodiorite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Hornblende-biotite granodiorite: dark grey, medium to coarse grained, mostly massive; extensive pyritic marginal phase porphyritic in quartz & feldspar, equigranular interior; prominent quartz; rare pyroxene.||||||01-OCT-04
2847|Buldah Gap Granodiorite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Hornblende-biotite granodiorite: highly magnetic (300-320 nT) to moderately magnetic (80-110n T). Radiometric response variable, high to medium K, medium Th and U.||||||06-OCT-04
2847|Buldah Gap Granodiorite|23309|6|Mentioned|p426 App 1|||G22. I-Type. Supersedes Buldah Gap Granite.||||||
2847|Buldah Gap Granodiorite|41850|6|Mentioned|p428|||||||||
2847|Buldah Gap Granodiorite|42827|6|Mentioned|p428|||||||||
2847|Buldah Gap Granodiorite|68116|5|Briefly described|Appendix, Map 37.|Early Devonian|Llandovery||||||Hornblende-biotite granodiorite: dark grey, medium to coarse grained, mostly massive; extensive pyritic marginal phase porphyritic in quartz and feldspar, equigranular interior: prominent quartz; rare pyroxene; I-type.|
26432|Buldah Trail Granite|42726|5|Briefly described|map legend|Early Devonian||Assume NOT variation on Buldah Gap Granite/Granodiorite. Both Bega Batholith.||||||
37635|Bulgana Diorite|23309|6|Mentioned|p426, Appendix 1|||G388||||||
37635|Bulgana Diorite|60451|4|Described|p91, 219|Early Devonian|Early Devonian|Of the Stawell Pluton. Type section in text. Dark grey, fine grained quartz diorite, containing considerable hornblende and biotite.||||||
37635|Bulgana Diorite|60457|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Ararat Suite. Biotite-hornblende-quartz diorite: dark grey, fine grained, numerous darker diorite xenoliths, oxidised, highly magnetic.||||||15-OCT-04
37635|Bulgana Diorite|60459|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Ararat Suite. Biotite-hornblende-quartz diorite: oxidised.||||||
37635|Bulgana Diorite|66002|5|Briefly described|p7 Tb.5|||Of Ararat Suite in Stawell Pluton area. G388. Defined by Cayley and Taylor 2001.||||||
37635|Bulgana Diorite|68116|5|Briefly described|Appendix, Map 30.|Early Devonian|Early Devonian||||||Biotite-hornblende-quartz diorite: dark grey, fine grained; numerous darker diorite xenoliths; oxidised, highly magnetic.|
2878|Bull Run Gap Granite|23309|6|Mentioned|p426 App 1|||G62. Supersedes Bull Run Gap Adamellite.||||||
2878|Bull Run Gap Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Bull Run Gap Adamellite, Bull Run Granodiorite?||||||
2878|Bull Run Gap Granite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Felsic biotite granite: fine to medium grained; grey; S-type.|
26434|Bulla Granodiorite|22502|6|Mentioned|P251|||||||||
26434|Bulla Granodiorite|23309|6|Mentioned|p426 App 1|||Supersedes Bulla Granite and Adamellite. S-Type Granite||||||
26434|Bulla Granodiorite|23810|5|Briefly described|Table 1, p894||Devonian|Mafic S-Type. Age: 392+/-5 Ma (SHRIMP U-Pb age). Geological Province:  Lachlan Fold Belt.||||||18-SEP-07
26434|Bulla Granodiorite|24551|6|Mentioned|p717 Table 2.4, 718 Table 8.1|Late Devonian|Early Devonian|Age: 395 +/- 5Ma, 368 +/- 2Ma.||||||
26434|Bulla Granodiorite|32001|6|Mentioned|p78|||||||||
26434|Bulla Granodiorite|33604|5|Briefly described|p19|||||||||
26434|Bulla Granodiorite|33605|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26434|Bulla Granodiorite|35712|6|Mentioned|p15|||||||||
26434|Bulla Granodiorite|41641|6|Mentioned|Fig.5.1|||||||||
26434|Bulla Granodiorite|61723|5|Briefly described|p824|||S-type granite. Age: 395+/-5Ma. In Victoria. ||||||
26434|Bulla Granodiorite|67802|6|Mentioned|p29|Devonian|Devonian|SHRIMP zircon age.|392 +/- 5 Ma (Bierlein et al. 2001).|||||
26434|Bulla Granodiorite|67978|5|Briefly described|p496 Fig.1, p500 Tb.1|Givetian|Emsian|Zircon dating (Bierlein et al. 2001b).|392 +/- 5 Ma|||||19-SEP-14
26434|Bulla Granodiorite|68116|5|Briefly described|Appendix, Map 41.|Late Devonian|Late Devonian||||||Biotite-cordierite granodiorite and granite: coarse-grained; minor garnet.|
26434|Bulla Granodiorite|75061|6|Mentioned|p64|Devonian|Devonian|Central Victoria.|392 +/- 5 Ma (Bierlein et al., 2001).||||S-type.|
26434|Bulla Granodiorite|75062|6|Mentioned|p74|Devonian|Devonian|Melbourne Zone.|392 Ma.||||S-type.|
26434|Bulla Granodiorite|75072|5|Briefly described|p230, 233, 237, 245-246, 249, 251|Middle Devonian|Middle Devonian|Melbourne Zone. A very small pluton, just N of Melbourne. Zircon ages indicate thermal events; age ranges discussed; probability density distribution graph.|392 +/- 5 Ma (Bierlein et al., 2001).||||Monzogranite. S-type.|
31598|Bulla Suite|24551|6|Mentioned|p221|||||||||
31598|Bulla Suite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
39837|Bullabul Granodiorite|24178|4|Described|p19|Early Devonian|Early Devonian|Age: 393 +/- 4Ma (Pb-U, Bierlein et al, 1999)||||||
39837|Bullabul Granodiorite|61369|5|Briefly described|p383|Early Devonian|Early Devonian|Part of the oxidised I-type Tarnagulla pluton (White and Chappell 1988).  Medium- to coarse-grained, non-foliated granodiorite.  Age: 391+/-5My (K-Ar: Richards and Singleton 1981).||||||28-SEP-05
30446|Bullawin Porphyry|23309|6|Mentioned|p426 App1|||G403 A-Type.||||||
30446|Bullawin Porphyry|44929|5|Briefly described|Map Legend||Early Devonian|Part of Victoria Valley Batholith. Biotite hornblende dacite to rhyodacite.||||||14-JUN-06
30446|Bullawin Porphyry|44930|5|Briefly described|Map Legend||Early Devonian|Part of Victoria Valley Batholith. Biotite hornblende dacite to rhyodacite.||||||14-JUN-06
30446|Bullawin Porphyry|44932|5|Briefly described|Map Legend||Early Devonian|Part of Victoria Valley Batholith. Biotite hornblende dacite to rhyodacite.||||||14-JUN-06
30446|Bullawin Porphyry|44933|5|Briefly described|Map Legend||Early Devonian|Of the Victoria Valley Batholith. Biotite hornblende dacite to rhyodacite: small intrusive plugs; glassy to medium grained, somewhat porphyritic, greyish green; felsic, oxidised, I-type.||||||27-OCT-04
30446|Bullawin Porphyry|61183|4|Described|p60|Early Devonian|Early Devonian|Late stage small intrusive body of the Victoria Valley batholith. Glassy, fine- to medium-grained, greyish-green dacite to rhyodacite. 393+/-3 Rb/Sr whole rock isochron of 16 samples from many of the intrusive phases of the Victoria Valley batholith (C.Gray pers. comm. 1995) may give a maximum age to this unit.||||||05-OCT-10
30446|Bullawin Porphyry|63457|5|Briefly described|p124-137.|||Authors stress this is an intrusive rock. Apparently, formerly called Bare Hill Rhyodacite. Major and trace element data provided. Has significantly higher Na content than typical Lachlan Fold Belt I-types. A-type.|||||Fine- to medium-grained, greyish-green where fresh; pink alkali feldspar, long (to 1cm) needles of dark amphibole, euhedral plagioclase phenocrysts; locally more felsic variants with aplite-like "sugary" texture and biotite the dominant mafic phase.|
30446|Bullawin Porphyry|64541|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Victoria Valley Batholith. Biotite hornblende dacite to rhyodacite: small intrusive plugs; glassy to medium grained, somewhat porphyritic, greyish green; felsic, oxidised, I-type.||||||07-FEB-11
30446|Bullawin Porphyry|64610|5|Briefly described|Map legend|Early Devonian|Early Devonian|Part of Victoria Valley Batholith. Biotite hornblende dacite to rhyodacite: -small intrusive plugs, glassy to med.-gr., somewhat porphyritic; greyish-green; felsic, oxidised, I-type.||||||17-NOV-08
30446|Bullawin Porphyry|66002|5|Briefly described|p8 Tb.5|||In Victoria Valley Batholith area. G403. Defined by Cayley and Taylor (1997).||||||
30446|Bullawin Porphyry|68116|5|Briefly described|Appendix, Map 30.|Early Devonian|Early Devonian||||||Biotite hornblende dacite/rhyodacite: greyish green; glassy to medium-grained, sparse feldspar and quartz phenocrysts; oxidised; forms small stocks.|
30446|Bullawin Porphyry|70877|6|Mentioned|p13|Early Devonian|Late Silurian|||||Intrudes the Grampians Group.||
30446|Bullawin Porphyry|70967|6|Mentioned|p11|||Mount Stavely Belt.||||Intrudes Grampians Group. Co-magmatic with Rocklands Volcanic Group.||
30446|Bullawin Porphyry|72445|5|Briefly described|p10.|Early Devonian|Late Silurian|||||Intrudes Grampians Group. Comagmatic with Rocklands Volcanic Group.||
2895|Bullenbalong Suite|22606|6|Mentioned|P829, P830|||||||||
2895|Bullenbalong Suite|22768|6|Mentioned|p176|||||||||
2895|Bullenbalong Suite|22778|4|Described|p 162|||||||||
2895|Bullenbalong Suite|22815|4|Described|p43,55, fig19|Silurian|Silurian|Contains at least 17 seperate units.||||||
2895|Bullenbalong Suite|22857|5|Briefly described|p176|||Intrusive granite.||||||
2895|Bullenbalong Suite|22876|5|Briefly described|p27|||||||||
2895|Bullenbalong Suite|22877|5|Briefly described|map|Silurian|Silurian|||||||
2895|Bullenbalong Suite|22968|6|Mentioned|Fig49 P92|||||||||
2895|Bullenbalong Suite|23020|5|Briefly described|Map legend|Wenlock|Wenlock|||||||
2895|Bullenbalong Suite|23021|5|Briefly described|Map legend|Wenlock|Wenlock|Nonconformable and angular unconformably overlain by the Enano Group||||||
2895|Bullenbalong Suite|23028|5|Briefly described|Map legend|Wenlock|Wenlock|||||||
2895|Bullenbalong Suite|23029|5|Briefly described|Map legend|Wenlock|Wenlock|Angular unconformably and nonconformably underlies the Enano Group||||||
2895|Bullenbalong Suite|23309|6|Mentioned|p338|||||||||
2895|Bullenbalong Suite|23439|6|Mentioned|p127|||||||||
2895|Bullenbalong Suite|23547|5|Briefly described|p553|||||||||
2895|Bullenbalong Suite|23549|5|Briefly described|p521|||Of Bullenbalong Supersuite. Includes the Jillamatong pluton. Mafic rocks crowded with biotite and cordierite-rich enclaves. Geological Province:  Lachlan Fold Belt.||||||06-FEB-08
2895|Bullenbalong Suite|23615|3|Fully described|p152|Early Devonian|Early Silurian|Composed of several large batholiths - Campbells Knob, Amboyne, Suggan Buggan, Chiplin, Nunniong and Mellick Munjie Granodiorites and Barrabilly Adamellite.  Geological Province: Lachlan Fold Belt.||||||
2895|Bullenbalong Suite|24099|5|Briefly described|p47, p48 Fig. 3|||S-type granite in the Kosciusko Basement Terrane.||||||
2895|Bullenbalong Suite|24222|5|Briefly described|p11|||Chemistry of samples reported. S-type. See also Bullenbalong Supersuite. Geological Province: Lachlan Fold Belt.||||||06-FEB-08
2895|Bullenbalong Suite|24514|6|Mentioned|p31|||S-type.||||||
2895|Bullenbalong Suite|41563|6|Mentioned|p513|||||||||
2895|Bullenbalong Suite|41898|5|Briefly described|p1184|||||||||
2895|Bullenbalong Suite|41905|4|Described|p75|||||||||
2895|Bullenbalong Suite|41933|5|Briefly described|Map legend|Late Silurian||||||||
2895|Bullenbalong Suite|42726|5|Briefly described|map legend||Silurian|Of the Bullenbalong Supersuite.  Contains 19 granitic units and one volcanics unit.||||||08-FEB-05
2895|Bullenbalong Suite|42827|5|Briefly described|p431|||||||||
2895|Bullenbalong Suite|43159|6|Mentioned|p3|||Intrusive equivalent of Hawkins Suite of volcanics.||||||
2895|Bullenbalong Suite|43206|5|Briefly described|map legend||Wenlock|||||||
2895|Bullenbalong Suite|43233|5|Briefly described|Map Legend|Late Silurian||of Berridale Batholith.||||||
2895|Bullenbalong Suite|44093|5|Briefly described|p188 App. 1|Early Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||
2895|Bullenbalong Suite|62962|6|Mentioned|p2291|||Geological Province: Lachlan Fold Belt.||||||07-FEB-11
2895|Bullenbalong Suite|68592|6|Mentioned|p1225|||Named after its type pluton, the Bullenbalong Granodiorite.||Unit in Bullenbalong Supersuite.|Includes Bullenbalong Granodiorite.|||
2895|Bullenbalong Suite|69876|5|Briefly described|p316|||Lachlan Fold Belt. Discussed in relation to source rock.|||||S-type granite.|
2895|Bullenbalong Suite|72571|5|Briefly described|p90, p92, p99|||Of the Tasmanides of eastern Australia.|||Includes the Jillamatong Granodiorite.|||
28182|Bullengarook Gravel|24383|4|Described|p30, 70|Early Pliocene|Late Miocene|Underlain by Castlemaine Group. Max. Thickness: <5m. Geological Province: Lachlan Fold Belt||||||08-MAR-07
28182|Bullengarook Gravel|24384|5|Briefly described|Map legend|Pliocene|Miocene|Gravel, sand and silt; vein quartz pebbles and cobbles, moderately rounded and crudely to well stratified; moderately consolidated.||||||
28182|Bullengarook Gravel|24385|5|Briefly described|Map legend|Miocene|Miocene|Gravel, sand and silt; vein quartz pebbles and cobbles; moderately rounded and sorted; crudely to well stratified; moderately consolidated; alluvial braid plain||||||
28182|Bullengarook Gravel|24386|5|Briefly described|Map legend|Miocene|Miocene|Gravel, sand and silt: vein quartz pebbles and cobbles; moderately rounded and sorted; crudely to well stratified; moderately consolidated.||||||
28182|Bullengarook Gravel|24387|5|Briefly described|Map legend|Miocene|Miocene|Gravel, sand and silt; vein quartz pebbles and cobbles; moderately rounded and sorted; crudely to well stratified; moderately consolidated; alluvial braid plain.||||||
28182|Bullengarook Gravel|24388|5|Briefly described|Map legend|Pliocene|Pliocene|Gravel, sand and silt; nonmagnetic; low-moderate total radioelements, K, Th and U.||||||
28182|Bullengarook Gravel|33604|6|Mentioned|p16|||Pliocene - Miocene. Map legend||||||
28182|Bullengarook Gravel|33605|6|Mentioned|Map legend|Pliocene|Miocene|Miocene-Pliocene||||||
28182|Bullengarook Gravel|39865|4|Described|p44|||||||||
28182|Bullengarook Gravel|64619|5|Briefly described|Map legend|Pleistocene|Pliocene|Gravel, sand, silt. gravel is dominant - pale, rounding and sorting moderate-good; moderately consolidated; massive to trough cross-bedded; pebble gravel consists mostly of vein quartz; fluvial deposits.||||||30-OCT-08
28182|Bullengarook Gravel|65715|4|Described|p15 Tb.8, p25, p109-110|Neogene|Neogene|Called Bullengarook Gravels by Crawford (1940). Type locality in gravel quarry adjacent to Gisborne-Bacchus Marsh Road at Bullengarook (MGA reference given). Unconformably overlies Castlemaine Group.||||||10-FEB-15
28182|Bullengarook Gravel|68116|5|Briefly described|Appendix, Maps 32, 41.|Pliocene|Miocene||||||Gravel, sand, silt: gravel predominant; pale; rounding and sorting moderate to good; moderately consolidated; massive to trough cross-bedded; pebble gravel consists mostly of vein quartz.|
24785|Bullung Siltstone|22971|5|Briefly described|p 22|||of Jordan River Group||||||
24785|Bullung Siltstone|23229|4|Described|Table3-3p27, 32|Wenlock|Wenlock|||||||
24785|Bullung Siltstone|23265|5|Briefly described|p340||Silurian|||||||
24785|Bullung Siltstone|23309|5|Briefly described|p143  Table 2.53/2.54||Silurian|Age: Wenlock||||||
24785|Bullung Siltstone|24177|5|Briefly described|p50 Fig.22|Early Silurian|Early Silurian|Geological Province: Mount Easton Province.||||||
24785|Bullung Siltstone|24551|6|Mentioned|p619|||||||||
24785|Bullung Siltstone|24588|5|Briefly described|p12 Fig.3|Wenlock|Wenlock|Geological Province: Mount Easton Province. Of the Jordan River Group.||||||29-NOV-13
24785|Bullung Siltstone|33601|2|Defined|p7|Late Silurian|Early Silurian|Early to Late Silurian.||||||22-DEC-08
24785|Bullung Siltstone|33607|6|Mentioned|Map legend|Silurian|Silurian|||||||
24785|Bullung Siltstone|35073|6|Mentioned|p17|||See also Table 1.||||||
24785|Bullung Siltstone|35283|3|Fully described|p51|||||||||
24785|Bullung Siltstone|36389|6|Mentioned|p41|||||||||
24785|Bullung Siltstone|37727|4|Described|p41|||See also p9.||||||17-NOV-08
24785|Bullung Siltstone|38787|6|Mentioned|Fig.2|||||||||
24785|Bullung Siltstone|39551|6|Mentioned|Map legend|Ludlovian|Wenlockian|Wenlockian to Ludlovian||||||
24785|Bullung Siltstone|39555|6|Mentioned|Map legend|Ludlovian|Wenlockian|Ludlovian to Wenlockian||||||
24785|Bullung Siltstone|41585|4|Described|p112|||See also Fig.4.3||||||
24785|Bullung Siltstone|42827|5|Briefly described|Table 4.1|||||||||
24785|Bullung Siltstone|44187|5|Briefly described|Map Legend||Early Silurian|||||||
24785|Bullung Siltstone|60599|5|Briefly described|p47 Fig. 19|Ludlow|Wenlock|Geological Province: Mount Easton Province, Melbourne Zone, Lachlan Fold Belt.||||||
24785|Bullung Siltstone|61185|5|Briefly described|p37, p21 Fig. 6|Ludlow|Wenlock|Of Jordan River Group (VandenBerg, 1975). Overlies McAdam Sandstone; underlies Sinclair Valley Sandstone.Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
24785|Bullung Siltstone|64535|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp. Dk. grey siltstone, generally finely banded/bioturbated - uppermost portion with mass-flow deposits, pockets of comminuted shelly fossils; sandstone, thin-v.thin-bedded, pale, quartzitic; deep marine hemipelagic + turbidite deposits.||||||22-DEC-08
24785|Bullung Siltstone|64536|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp. Dk. grey siltstone, generally finely banded/bioturbated - uppermost portion with mass-flow deposits, pockets of comminuted shelly fossils; sandstone, thin-v.thin-bedded, pale, quartzitic; deep marine hemipelagic + turbidite deposits.||||||07-FEB-11
24785|Bullung Siltstone|64537|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp. Dk. grey siltstone, generally finely banded/bioturbated - uppermost portion with mass-flow deposits, pockets of comminuted shelly fossils; sandstone, thin-v.thin-bedded, pale, quartzitic; deep marine hemipelagic + turbidite deposits.||||||07-FEB-11
24785|Bullung Siltstone|64538|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp. Dk. grey siltstone, generally finely banded/bioturbated - uppermost portion with mass-flow deposits, pockets of comminuted shelly fossils; sandstone, thin-v.thin-bedded, pale, quartzitic; deep marine hemipelagic + turbidite deposits.||||||07-FEB-11
24785|Bullung Siltstone|64539|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp. Dk. grey siltstone, generally finely banded/bioturbated - uppermost portion with mass-flow deposits, pockets of comminuted shelly fossils; sandstone, thin-v.thin-bedded, pale, quartzitic; deep marine hemipelagic + turbidite deposits.||||||22-DEC-08
24785|Bullung Siltstone|64540|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp. Dk. grey siltstone, generally finely banded/bioturbated - uppermost portion with mass-flow deposits, pockets of comminuted shelly fossils; sandstone, thin-v.thin-bedded, pale, quartzitic; deep marine hemipelagic + turbidite deposits.||||||22-DEC-08
24785|Bullung Siltstone|64605|5|Briefly described|Map legend|Silurian|Silurian|Of the Jordan River Group. Siltstone, minor sandstone; deep-marine deposits. Dark to light green and speckled brown to pink-white in RGB. Nonmagnetic.||||||17-NOV-08
24785|Bullung Siltstone|64606|5|Briefly described|Map Legend|Silurian|Silurian|Of Jordan River Group. Siltstone, minor sandstone: deep-marine deposits. Dark to light green and speckled brown to pink-white in RGB. Nonmagnetic.||||||11-NOV-08
24785|Bullung Siltstone|64616|3|Fully described|p83, p162-163 Fig.6.9, p165|Ludlow|Llandovery|See also p183 Fig.6.29, p197 Fig.6.34, p286-287, p293, p305, p385 Tb.1, p386. Of Jordan River Group. Type section location given. Conformable between underlying McAdam Sandstone and overlying Sinclair Valley Sandstone. ~150-775m thick. Thick-bedded, dark grey, laminated siltstone, strongly cleaved, bioturbated; minor thin-bedded, pale, quartzitic sandstone. Fossil localities important in distinguishing this unit from Whitelaw Siltstone. Age inferred. Geophysical characteristics given.||||||
24785|Bullung Siltstone|68116|5|Briefly described|Appendix, Maps 25, 33-34, 43, 52.|Homerian|Telychian||||||Siltstone, minor sandstone: siltstone dark grey, generally finely banded and bioturbated, uppermost portion contains mass-flow deposits with pockets of comminuted shelly fossils; sandstone thin to very thin-bedded, pale, quartzitic.|
24785|Bullung Siltstone|70487|6|Mentioned|p13|Lochkovian|Pridoli|The lowest stratigraphic occurrence (of systematic palaeontology) recorded in Victoria is in the Bullung Siltstone.|||||Fossiliferous siltstone.|
2938|Bumberrah Member|41511|6|Mentioned|Fig.2|||||||||
2941|Bumble Creek Formation|41585|6|Mentioned|p128|||||||||
2941|Bumble Creek Formation|42827|5|Briefly described|p128|||||||||
69427|Bundara Munjie Quartz Diorite|61161|5|Briefly described|p96, p151, p92 Fig 6.11, p76-77 Fig 6.1|Early Devonian|Early Devonian|Of Rileys Creek Suite. Elongate, dyke-like bodies of fine-grained hornblende- and biotite-bearing quartz diorite. Intrude Omeo Metamorphic Complex. Weakly to highly magnetic. I-type. GSV map code: G467a diorite; G467b biotite-hornblende granodiorite.||||||
69427|Bundara Munjie Quartz Diorite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Subdivided into two informal phases: hornblende-biotite quartz diorite and biotite-hornblende granodiorite; GSV map code: G467a and G467b respectively; I-type intrusion.||||||
69427|Bundara Munjie Quartz Diorite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Subdivided into two informal phases: hornblende-biotite quartz diorite and biotite-hornblende granodiorite; GSV map code: G467a and G467b respectively; I-type intrusion.||||||07-FEB-11
69427|Bundara Munjie Quartz Diorite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Subdivided into two informal phases: hornblende-biotite quartz diorite and biotite-hornblende granodiorite; GSV map code: G467a and G467b respectively; I-type intrusion.||||||
69427|Bundara Munjie Quartz Diorite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Subdivided into two informal phases: hornblende-biotite quartz diorite and biotite-hornblende granodiorite; GSV map code: G467a and G467b respectively; I-type intrusion.||||||
69427|Bundara Munjie Quartz Diorite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Two informal phases: hornblende-biotite quartz diorite and biotite-hornblende granodiorite, with differing geophysical responses; GSV map code: G467a and G467b respectively.||||||
69427|Bundara Munjie Quartz Diorite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Silurian||||||Hornblende-biotite quartz diorite: fine to medium grained; porphyritic, large hornblende and biotite phenocrysts, lesser plagioclase, augite phenocrysts in groundmass of fine plagioclase, accessory quartz and magnetite; chlorite, epidote alteration.|
69426|Bundara Tonalite|61160|4|Described|p64, p33 Tb. 5.2, p58-59 Fig. 6.8|Silurian|Silurian|Of Pretty Valley Suite. Formerly included in Pretty Valley Series (Fagan 1979); grouped with Pretty Valley Tonalite by Beavis (1962). Foliated biotite tonalite and minor granodiorite, few enclaves; grey; equigranular; biotite-rich; local hornblende.||||||30-MAY-14
69426|Bundara Tonalite|61164|5|Briefly described|map legend|Early Silurian|Early Silurian|Of the Pretty Valley Suite. Biotite tonalite: grey; coarse to medium grained; equigranular; biotite-rich, local hornblende; minor enclaves; includes minor granodiorite types with orthoclase, no hornblende; foliated; I-type intrusion. GSV map code: G168.||||||
69426|Bundara Tonalite|61165|5|Briefly described|map legend|Early Silurian|Early Silurian|Of the Pretty Valley Suite. Biotite tonalite: grey; coarse to medium grained; equigranular; biotite-rich, local hornblende; minor enclaves; includes minor granodiorite types with orthoclase, no hornblende; foliated; I-type intrusion. GSV map code: G168.||||||
69426|Bundara Tonalite|61166|5|Briefly described|map legend|Early Silurian|Early Silurian|Of the Pretty Valley Suite. Biotite tonalite: grey; coarse to medium grained; equigranular; biotite-rich, local hornblende; minor enclaves; includes minor granodiorite types with orthoclase, no hornblende; foliated; I-type intrusion. GSV map code: G168.||||||
69426|Bundara Tonalite|61167|5|Briefly described|map legend|Early Silurian|Early Silurian|Of the Pretty Valley Suite. Biotite tonalite: grey; coarse to medium grained; equigranular; biotite-rich, local hornblende; minor enclaves; includes minor granodiorite types with orthoclase, no hornblende; foliated; I-type intrusion. GSV map code: G168.||||||07-FEB-11
69426|Bundara Tonalite|61168|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Pretty Valley Suite. Biotite tonalite: I-type; nonmagnetic (0-30 nT, kv = 0-20 x10^-6 cgs); slight gravity low (-430 ums^-2); moderate total radioelement, K, Th and U. GSV map code: G168.||||||
69426|Bundara Tonalite|68116|5|Briefly described|Appendix, Map 27.|Silurian|Silurian||||||Biotite tonalite: grey; coarse to medium grained; equigranular; biotite-rich, hornblende occurs locally; minor enclaves; includes minor granodiorite types with orthoclase and no hornblende; foliated; I-type.|
30293|Bung Bung Syenite|60503|3|Fully described|p183, p41 Tb. 2|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Syenite, medium to coarse-grained and pale grey, orthoclase crystals and small clots of hornblende and biotite. Contains few xenoltihs of trachyte. Intrudes Little Mount Tambo Trachyte Member.||||||16-NOV-09
30293|Bung Bung Syenite|68116|5|Briefly described|Appendix, Map 27.|Triassic|Triassic||||||Hornblende-biotite syenite: pale grey, medium to coarse grained, equigranular, porphyritic in the south.|
3001|Bungal granite|37385|6|Mentioned|p6|||Name refers to an outcrop area only.||||||
28414|Bungeet West Granite|23309|5|Briefly described|p426 App1|||G210 S-Type.||||||27-AUG-04
28414|Bungeet West Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
28414|Bungeet West Granite|68116|5|Briefly described|Appendix, Maps 18, 19.|Late Devonian|Late Devonian||||||Equigranular medium-grained, pinkish biotite granite with vermiculite, indicating some hydrothermal alteration; accessory muscovite, fluorite.|
3026|Bungunnia Limestone|10010|5|Briefly described|p12 Fig. 3|Pleistocene|Late Pliocene|Geological Province: Murray Basin.||||||13-AUG-07
3026|Bungunnia Limestone|22773|5|Briefly described|Fig24.8p352|Early Pleistocene|Late Pliocene|||||||
3026|Bungunnia Limestone|22799|5|Briefly described|p24 Fig.10|Pleistocene|Pleistocene|||||||
3026|Bungunnia Limestone|22857|5|Briefly described|p352 Fig. 24.8|Pleistocene|Late Pliocene|Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|22887|5|Briefly described|Fig.6 p13||Late Pliocene|||||||
3026|Bungunnia Limestone|22893|5|Briefly described|fig9p27|||||||||
3026|Bungunnia Limestone|23560|6|Mentioned|p152|||||||||
3026|Bungunnia Limestone|23818|5|Briefly described|p212 Fig.108|Middle Pleistocene|Middle Pleistocene|Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|23884|5|Briefly described|p155 Fig. 13.2|Late Pliocene|Late Pliocene|Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|24176|6|Mentioned|p20|Pleistocene|Pleistocene|Of Firman (1965).||||||
3026|Bungunnia Limestone|24551|5|Briefly described|p338 Fig. 11.2, 340, 609.|Middle Pleistocene|Early Pleistocene|||||||
3026|Bungunnia Limestone|30056|6|Mentioned|Table 2|||||||||
3026|Bungunnia Limestone|30177|6|Mentioned|p106|||Pleistocene age.||||||
3026|Bungunnia Limestone|30750|6|Mentioned|p1|||Pleistocene age||||||
3026|Bungunnia Limestone|30751|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
3026|Bungunnia Limestone|30753|4|Described|p15|||Middle Pleistocene age||||||
3026|Bungunnia Limestone|30754|2|Defined|Appendix 1|middle Pleistocene|middle Pleistocene|See also P22,31||||||
3026|Bungunnia Limestone|30807|6|Mentioned|p101|||Suggested map symbol||||||
3026|Bungunnia Limestone|30918|6|Mentioned|p84|||||||||
3026|Bungunnia Limestone|30996|6|Mentioned|p38|||Refers Roberts (1968), Firman (1971)||||||
3026|Bungunnia Limestone|31741|6|Mentioned|p6|||||||||
3026|Bungunnia Limestone|31745|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
3026|Bungunnia Limestone|31848|6|Mentioned|p12|||Quaternary||||||
3026|Bungunnia Limestone|32426|4|Described|p141|||See also P140||||||
3026|Bungunnia Limestone|32861|5|Briefly described|Table 1|||||||||
3026|Bungunnia Limestone|32862|5|Briefly described|Table 3|||Pleistocene||||||
3026|Bungunnia Limestone|33826|6|Mentioned|p42|||Strat. table||||||
3026|Bungunnia Limestone|34114|4|Described|p50|||Pleistocene||||||
3026|Bungunnia Limestone|34180|6|Mentioned|p212|||Middle Pleistocene.||||||
3026|Bungunnia Limestone|34459|4|Described|p11|||Pleistocene||||||
3026|Bungunnia Limestone|34461|5|Briefly described|p49|||||||||
3026|Bungunnia Limestone|34758|6|Mentioned|Table 1|||||||||
3026|Bungunnia Limestone|34954|6|Mentioned|p199|||||||||
3026|Bungunnia Limestone|35097|6|Mentioned|Fig.4|||||||||
3026|Bungunnia Limestone|35131|6|Mentioned|p8|||||||||
3026|Bungunnia Limestone|35200|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
3026|Bungunnia Limestone|35232|6|Mentioned|Table 4|||||||||
3026|Bungunnia Limestone|35272|4|Described|p284|||||||||
3026|Bungunnia Limestone|35274|6|Mentioned|p425|||||||||
3026|Bungunnia Limestone|37873|4|Described|p2|||||||||
3026|Bungunnia Limestone|38068|6|Mentioned|p76|||||||||
3026|Bungunnia Limestone|39329|6|Mentioned|Fig.1|||||||||
3026|Bungunnia Limestone|40380|6|Mentioned|p221|||||||||
3026|Bungunnia Limestone|40820|5|Briefly described|p142|||||||||
3026|Bungunnia Limestone|41848|5|Briefly described|p358|||At top of Blanchetown Clay sequence. Age Pleistocene||||||
3026|Bungunnia Limestone|41868|6|Mentioned|p579|||||||||
3026|Bungunnia Limestone|42125|6|Mentioned|p139|||||||||
3026|Bungunnia Limestone|42130|6|Mentioned|Fig.3 P265|||||||||
3026|Bungunnia Limestone|42134|6|Mentioned|Fig.3 P335|||||||||
3026|Bungunnia Limestone|42137|6|Mentioned|Fig.2 P368|||||||||
3026|Bungunnia Limestone|42592|6|Mentioned|p280|||||||||
3026|Bungunnia Limestone|42635|5|Briefly described|p94|||||||||
3026|Bungunnia Limestone|42717|6|Mentioned|map legend|Pleistocene||||||||
3026|Bungunnia Limestone|42813|6|Mentioned|p25|||||||||
3026|Bungunnia Limestone|42827|5|Briefly described|p359|||see also Table 9.1||||||
3026|Bungunnia Limestone|42881|4|Described|Fig.3, P84|||||||||
3026|Bungunnia Limestone|42966|1|Redefined|Table 34 p209|Early Pleistocene||||||||
3026|Bungunnia Limestone|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Lacustrine dolomitic limestone. Underlain by Blanchetown Clay.||||||
3026|Bungunnia Limestone|43073|5|Briefly described|Table 4|||||||||
3026|Bungunnia Limestone|43258|5|Briefly described|Map Legend|Pleistocene|Pliocene|||||||
3026|Bungunnia Limestone|43298|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
3026|Bungunnia Limestone|43655|5|Briefly described|p40-846|||||||||
3026|Bungunnia Limestone|43791|6|Mentioned|p372, Fig1|||||||||
3026|Bungunnia Limestone|43804|6|Mentioned|Fig.2,p49|||||||||
3026|Bungunnia Limestone|44133|5|Briefly described|p252|Middle Pleistocene|Late Pliocene|Thickness: 3m. At the top of the Chowilla Sand and the Blanchtown Clay. Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|49040|6|Mentioned|Fig.6|||||||||
3026|Bungunnia Limestone|60540|5|Briefly described|p1000 Fig.2,p1000,|Pleistocene|Pleistocene|||||Incised into the underlying Loxton Sand|Dolostone.|
3026|Bungunnia Limestone|60953|5|Briefly described|Map Legend|Pleistocene|Pliocene|Overlies: Blanchetown Clay. Lacustrine dolomitic limestone.||||||
3026|Bungunnia Limestone|61108|5|Briefly described|map legend|Pleistocene|Pliocene|Lacustrine dolomitic limestone. Overlies Blanchetown Clay.||||||01-JUN-05
3026|Bungunnia Limestone|61181|5|Briefly described|p137|Pleistocene|Pleistocene|Lacustrine deposits occur between ridges of Parilla Sand. Dolomitic limestone of this formation is interbedded with clay and sand. In the Mallee region.||||||
3026|Bungunnia Limestone|61207|5|Briefly described|p280 Fig. 2|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|61314|5|Briefly described|p129|Pleistocene|Pleistocene|Of the Wunghnu Group. Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|63887|5|Briefly described|p20, p21 Fig. 1|Pleistocene|Late Miocene|Variably dolomitic limestone.||||||
3026|Bungunnia Limestone|64961|5|Briefly described|p259, p269 Fig. 9|Quaternary|Quaternary|Overlies Blanchetown Clay. Geological province: Murray Basin. Thin, lacustrine carbonate unit, restricted in distribution. Indicated by 'BL' in Figure 9. ||||||
3026|Bungunnia Limestone|65552|5|Briefly described|p5 Fig. 3|Quaternary|Quaternary|Limestone of the central and western Murray Basin. Overlies Blanchetown Clay; underlies surface aeolian-fluvio-lacustrine deposits (e.g. Woorinen Formation, Coonambidgal Formation, Molineaux-Lowan Sands).||||||
3026|Bungunnia Limestone|66287|5|Briefly described|Fig 2,4,5|Late Pliocene|Late Pliocene|With the Blanchetown Clay and the Chowilla Sand, part of the Lake Bungunnia sedimentary fill.||||Underlies the Bakara Soil and overlies the Blanchetown Clay.||20-APR-12
3026|Bungunnia Limestone|68548|5|Briefly described|p13, p13 Fig.2|Pleistocene|Pleistocene|Early to Middle Pleistocene age.||||Overlies Blanchetown Clay.|Dolostones.|
3026|Bungunnia Limestone|71248|2|Defined|p1, 2|||||||||
3026|Bungunnia Limestone|72445|6|Mentioned|App.7 p7, p7 Fig.4.|Quaternary|Quaternary|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991).||||Shown as overlying and partially equivalent to Blanchetown Clay.|Shown as limestone.|
3026|Bungunnia Limestone|73188|6|Mentioned|p320|Pleistocene|Pleistocene|Murray Basin.|||||Lacustrine limestone.|
3026|Bungunnia Limestone|73228|4|Described|p50, p56-57, p59, p62|Pleistocene|Late Pliocene|Murray Basin. Thickness: 1-3 m. Caps the Blanchetown Clay.|||||Interlaminated calcite, dolomite and magnesite, including an abundance of pisolitic and ooid grainstones, as well as ostracod-rich sands.|
3026|Bungunnia Limestone|73229|6|Mentioned|p67|Pleistocene|Late Pliocene|Murray Basin.||||||
3028|Bungywarr Formation|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Errinundra Group||||||
3028|Bungywarr Formation|23309|5|Briefly described|p104  Table 2.39, 106|||||||||
3028|Bungywarr Formation|23522|5|Briefly described|p247 Fig 3|Early Devonian|Early Devonian|||||||
3028|Bungywarr Formation|24551|4|Described|p148|||Of Errinundra Group.||||||
3028|Bungywarr Formation|41585|5|Briefly described|p140|||||||||
3028|Bungywarr Formation|42577|5|Briefly described|p29|||||||||
3028|Bungywarr Formation|42627|5|Briefly described|Map legend|Emsian|Pragian|||||||
3028|Bungywarr Formation|42647|3|Fully described|p29|||of Errinundra Group||||||
3028|Bungywarr Formation|42827|4|Described|p140|||of Errinundra Group||||||
3028|Bungywarr Formation|43228|5|Briefly described|p10||Early Devonian|||||||
3028|Bungywarr Formation|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Boulder Flat. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
3028|Bungywarr Formation|68116|5|Briefly described|Appendix.|Early Devonian|Early Devonian||||||Sandstone and pebble conglomerate, including volcaniclastics; interbedded ignimbrite-like rocks are unwelded; minor rhyolitic lava is surrounded by hyaloclastite.|
3028|Bungywarr Formation|70601|5|Briefly described|p28|Pragian|Pragian|East Gippsland.||Errinundra Group.|||Felsic volcanics and detritus.|
3039|Bunroy Hut Granite|23309|6|Mentioned|p426 App 1|||G91||||||
3039|Bunroy Hut Granite|24133|3|Fully described|p75|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
3039|Bunroy Hut Granite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
3039|Bunroy Hut Granite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
3039|Bunroy Hut Granite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
3039|Bunroy Hut Granite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt||||||
3039|Bunroy Hut Granite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
3039|Bunroy Hut Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
3039|Bunroy Hut Granite|44184|5|Briefly described|Map Legend||Early Silurian|Shown as Bunroy Hut Unassigned.||||||
3039|Bunroy Hut Granite|68116|5|Briefly described|Appendix.|Pridoli|Wenlock|Informally subdivided into highly and moderately magnetic phases, as well as a leucocratic phase.|||||Biotite granodiorite: grey, medium to coarse grained and equigranular; occasional small ovoid microgranular mafic enclaves; I-type; low to highly magnetic. Leucogranite and biotite granite: grey, massive equigranular; I-type; moderately magnetic.|
37636|Burbibyong Granite|23309|6|Mentioned|p426,  App. 1|||G568, S-type.||||||09-SEP-04
37636|Burbibyong Granite|24133|3|Fully described|p62|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37636|Burbibyong Granite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37636|Burbibyong Granite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37636|Burbibyong Granite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37636|Burbibyong Granite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Biotite-cordierite granite: brownish grey, medium to fine grained; locally foliated; S-type; nonmagnetic||||||09-SEP-04
37636|Burbibyong Granite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Biotite-cordierite granite: S-type; nonmagnetic; variable K, Th, U.||||||09-SEP-04
37636|Burbibyong Granite|68116|5|Briefly described|Appendix, Map 20.|Pridoli|Wenlock||||||Biotite cordierite granite: brownish grey, medium to fine grained; locally foliated; S-type; nonmagnetic.|
30514|Burglar Gap Granite|22878|4|Described|p87|||||||||
30514|Burglar Gap Granite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Leucocratic granite: partly concealed, pale grey, fine to medium grained, massive, contains biotite and muscovite.||||||01-OCT-04
30514|Burglar Gap Granite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Leucocratic granite: partly concealed, pale grey, fine to medium grained, massive, contains biotite and muscovite.||||||01-OCT-04
30514|Burglar Gap Granite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Leucocratic granite: Highly magnetic (up to 300 nT) with moderately magnetic section (90-125 nT). High K, low Th and U.||||||06-OCT-04
30514|Burglar Gap Granite|23309|6|Mentioned|p426 App1|||G14 I-Type. Supersedes Buckle Trail Granite.||||||
30514|Burglar Gap Granite|68116|5|Briefly described|Appendix, Map 37.|Early Devonian|Llandovery||||||Leucocratic granite: pale grey, fine to medium grained, massive; contains biotite and muscovite; I-type.|
28416|Burlington Sandstone Member|35283|6|Mentioned|p53|||||||||
3088|Burnie Group|33220|6|Mentioned|Fig.2|||||||||
3088|Burnie Group|70025|6|Mentioned|p2,26|Neoproterozoic|Neoproterozoic|Burnie Group and correlatives deposited on thinned continental crust.||||||
3088|Burnie Group|73199|6|Mentioned|p520|Neoproterozoic|Neoproterozoic|||||||
3093|Burnley Basalt Flow|23267|5|Briefly described|p378|||||||||
3093|Burnley Basalt Flow|24551|5|Briefly described|p338 Fig. 11.2|Middle Pleistocene|Early Pleistocene|||||||
3093|Burnley Basalt Flow|41848|4|Described|p391|||||||||
3093|Burnley Basalt Flow|42827|4|Described|p391|||||||||
3093|Burnley Basalt Flow|71277|5|Briefly described|p301|Quaternary|Quaternary|Nielson and Jenkin (1967). Also referred to as the Burnley Basalt (p302, p303 Tb.1, p304-306, p307 Fig.6).|0.93-0.82 Ma (Heath, 2015; Page, 1968).|Yarra Delta Group.|||Very high strength, dark grey, jointed, vesicular basalt, weathered at the top.|
32302|Burong Formation|13323|5|Briefly described|p393 Fig. 2|Early Oligocene|Middle Eocene|Of the Cobia Subgroup (Latrobe Group). Fluvial-deltaic and paralic deposits. Geological Province: Gippsland Basin.||||||
32302|Burong Formation|24090|5|Briefly described|p8 Fig.3|Oligocene|Eocene|Geological Province: Gippsland Basin.||||||
32302|Burong Formation|24407|5|Briefly described|p13 Fig.2|Early Oligocene|Middle Eocene|Geological Province: Gippsland Basin||||||
32302|Burong Formation|24495|5|Briefly described|p10|||Of Cobia Sungroup.  Fluvial/coastal plain deposits.  Geological Province: Gippsland Basin.||||||
32302|Burong Formation|24551|5|Briefly described|p262 Fig. 9.29, 477.|Oligocene|Eocene|Of the Cobia Subgroup.||||||
32302|Burong Formation|61552|6|Mentioned|p583 Fig.2. |Early Oligocene|Middle Eocene|||Unit in Cobia Subgroup.||||
32302|Burong Formation|64876|5|Briefly described|p145 Fig.2|Oligocene|Eocene|Gippsland Basin.||Cobia Subgroup.||||
32302|Burong Formation|65717|5|Briefly described|p9 Fig.2.2, p11-12|Oligocene|Eocene|Partridge (1999). Coal-bearing lower coastal plain facies deposit. One of the Latrobe Group's top seals.||Cobia Subgroup||Unconformably overlies Kingfish Formation. Unconformably overlain by Lakes Entrance Formation, Balook Formation.|Interbedded sandstone, siltstone, shale and coal.|05-SEP-17
32302|Burong Formation|65718|5|Briefly described|p12, p16, p42 Fig 5.3|Oligocene|Eocene|Partridge (1999). Lower coastal plain facies which is reasonably well-developed across the eastern part of the onshore Gippsland Basin. Middle Eocene to Early Oligocene age.||Of the Cobia Subgroup.||||
32302|Burong Formation|65973|5|Briefly described|p16, p22, p171|Oligocene|Eocene|Gippsland Basin. Deposited as a lower coastal plain.||Cobia Subgroup|||Fine- to medium-grained glauconitic siliciclastics.|
32302|Burong Formation|70028|6|Mentioned|p79|Oligocene|Eocene|Onshore Gippsland Basin.||||||
32302|Burong Formation|70076|5|Briefly described|South-Eastern: Fig.2; p2|Priabonian|Lutetian|See also Regional: Fig.3; p3, p7. Lower-middle coastal plain sediments. Hydrocarbon reservoir.||Cobia Subgroup||Overlies Kingfish Formation. Is overlain by Gurnard Formation.|Coal-rich.|
32302|Burong Formation|73289|5|Briefly described|p764, 769|Eocene|Eocene|Gippsland Basin (offshore).||||Referred to as Traralgon Formation in onshore Gippsland Basin. Equivalent to Gurnard Formation.||
32302|Burong Formation|73471|5|Briefly described|p86|||Gippsland Basin.||Cobia Subgrop||Underlies Gurnard Formation|Fluvial-deltaic and paralic sandstones and siltstones with interbedded coal layers.|
32302|Burong Formation|73488|6|Mentioned|p632 Fig.2|Lutetian|Ypressian|Gippsland Basin.||||Underlies Traralgon Formation||
32302|Burong Formation|75065|5|Briefly described|p151|Oligocene|Eocene|Gippsland Basin; offshore. Fluvial-deltaic and paralic sediments.||Cobia Subgroup.||Unconformably overlies Kingfish Formation (Halibut Subgroup). Adjacent to Traralgon and Gurnard Formations. Is overlain locally by Gurnard Formation.|Sandstone, coal, shale.|
30461|Burramboot Formation|22886|4|Described|p10|Cambrian|Cambrian|||||||
30461|Burramboot Formation|61187|5|Briefly described|p103 Fig.3.|Cambrian|Cambrian|||Unit in Mount William Volcanics.||||
37637|Burrumbeep Granodiorite|23309|5|Briefly described|p426, Appendix 1|Devonian|Devonian|G381, I-type. Supersedes Burrumbeep Adamellite.||||||
37637|Burrumbeep Granodiorite|24551|6|Mentioned|p228, 722 Table 8.5|||||||||
37637|Burrumbeep Granodiorite|60451|4|Described|p87|Early Devonian|Early Devonian|I-Type. Of the Ararat Suite. Type section in text. Equigranular, fine to medium grained, pale speckled grey, inner parts porphyritic.||||||
37637|Burrumbeep Granodiorite|60454|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Ararat Suite. Hornblende-biotite granodiorite; pale grey; porphyritic; fine to medium grained; oxidised; I-Type.||||||
37637|Burrumbeep Granodiorite|60459|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Ararat Suite. Hornblende-biotite granodiorite; oxidised, I-Type.||||||
37637|Burrumbeep Granodiorite|63599|6|Mentioned|p976 Fig. 1|||Geological Province: Stawell Zone.||||||10-DEC-07
37637|Burrumbeep Granodiorite|66002|5|Briefly described|p7 Tb.5|||Of Ararat Suite. In Ararat Pluton area. G380. Defined by Cayley and Taylor 2001. Called Burrumbeet Granodiorite by White and Chappell (1988)||||||
37637|Burrumbeep Granodiorite|68116|5|Briefly described|Appendix, Map 30.|Middle Devonian|Early Devonian||||||Hornblende-biotite granodiorite; pale grey; porphyritic; fine to medium grained; miarolitic cavities, symplectic intergrowth textures; contact metamorphosed by enclosing Ararat Granodiorite; oxidised, I-type, very weakly to non-magnetic.|
37639|Burrungabugge Granodiorite|23309|5|Briefly described|p426, Appendix 1|Early Devonian|Early Devonian|G96, I-type. Supersedes Burrunabugge Tonalite. Age: 408+/-7Ma.||||||
37639|Burrungabugge Granodiorite|24133|3|Fully described|p70|Silurian|Silurian|Parent: Boggy Plain Supersuite.  Geological Province: Lachlan Fold Belt.||||||
37639|Burrungabugge Granodiorite|24142|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||
37639|Burrungabugge Granodiorite|24143|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||
37639|Burrungabugge Granodiorite|24144|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||
37639|Burrungabugge Granodiorite|24145|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt||||||
37639|Burrungabugge Granodiorite|24146|5|Briefly described|Map Legend|Devonian|Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||
37639|Burrungabugge Granodiorite|60503|3|Fully described|p167, p42 Tb. 2|Early Devonian|Early Devonian|Series of six small outcropping intrusions and one small outlying intrusion partly buried by the Murtagh Creek Ignimbrite. Each is highly magnetic I-type mainly of granodioritic composition; some gabbro. Also referred to as the Burrungabugge pluton.||||||17-FEB-10
37639|Burrungabugge Granodiorite|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Hornblende-biotite diorite: I-type; 408+/-7 Ma (U/Pb zircon); highly magnetic (400nT) northeast aligned 'bullseyes'; low total count, K, Th, U||||||
37639|Burrungabugge Granodiorite|68116|5|Briefly described|Appendix, Map 20, 27.|Early Devonian|Early Devonian||||||Hornblende-biotite granodiorite: dark green, medium-grained; epidote alteration common; highly magnetic.|
3162|Burrungule Member|22875|5|Briefly described|p26 Table1|||||||||
3162|Burrungule Member|23671|3|Fully described|p2|Middle Eocene|Middle Eocene|Carbonaceous clay with occasional silt and coarse sand interbeds. Disconformably overlain by Gambier Limestone. Max. thickness: ~90ft.||||||05-FEB-08
3162|Burrungule Member|23818|5|Briefly described|p174 Fig.84, p176|Middle Eocene|Middle Eocene|Of the Tartwaup Formation. Geological Province: Otway Basin. Max. thickness: 34 ft. Contains many small planktonic foraminifera.||||||
3162|Burrungule Member|24551|5|Briefly described|p292 Fig. 10.3|||Of the Wangerrip Group.||||||
3162|Burrungule Member|29355|6|Mentioned|p188|||||||||
3162|Burrungule Member|29591|6|Mentioned|p92|||||||||
3162|Burrungule Member|29697|6|Mentioned|Fig.11|||||||||
3162|Burrungule Member|30179|6|Mentioned|p32|||||||||
3162|Burrungule Member|30514|6|Mentioned|p108|||Late Eocene to early Middle Miocene age||||||
3162|Burrungule Member|30754|6|Mentioned|p12|||See also P14. Stratigraphic table.||||||
3162|Burrungule Member|30917|6|Mentioned|p54|||||||||
3162|Burrungule Member|31245|4|Described|p78|||See also p80. Fauna. Lithology||||||31-JAN-07
3162|Burrungule Member|31246|6|Mentioned|p56|||M. Eocene||||||
3162|Burrungule Member|31625|6|Mentioned|Fig. 5.2|||Eocene||||||
3162|Burrungule Member|31920|4|Described|p57|||See also Fig. 3-2, 3,4,5. Eocene||||||
3162|Burrungule Member|31922|6|Mentioned|Table 3|||||||||
3162|Burrungule Member|32116|6|Mentioned|p51|||||||||
3162|Burrungule Member|32117|6|Mentioned|Fig.2|||||||||
3162|Burrungule Member|32119|6|Mentioned|p483|||Eocene||||||
3162|Burrungule Member|32120|5|Briefly described|p275|||Eocene or fauna||||||
3162|Burrungule Member|33109|6|Mentioned|p84|||Refers aquifers||||||
3162|Burrungule Member|33224|6|Mentioned|p69|||Palynology||||||
3162|Burrungule Member|33716|6|Mentioned|p15|||||||||
3162|Burrungule Member|33938|6|Mentioned|p48|||Refs. McGowran et al (1971) & Harris (1971).||||||
3162|Burrungule Member|34295|6|Mentioned|p30|||Eocene. fauna||||||
3162|Burrungule Member|34308|5|Briefly described|p176|||U.Eocene. See Fig.84||||||
3162|Burrungule Member|35066|6|Mentioned|Fig.8.9|||||||||
3162|Burrungule Member|37548|5|Briefly described|p131|||||||||
3162|Burrungule Member|38068|6|Mentioned|Fig.7|||||||||
3162|Burrungule Member|38903|5|Briefly described|Table 2|||||||||
3162|Burrungule Member|39408|6|Mentioned|Fig.5|||||||||
3162|Burrungule Member|40003|5|Briefly described|p44|||See also Fig.10||||||
3162|Burrungule Member|40555|6|Mentioned|Fig.4|||||||||
3162|Burrungule Member|41517|6|Mentioned|p134|||||||||
3162|Burrungule Member|41520|5|Briefly described|Fig.12|||||||||
3162|Burrungule Member|41626|6|Mentioned|p63|||||||||
3162|Burrungule Member|41769|5|Briefly described|p25|||||||||
3162|Burrungule Member|41868|5|Briefly described|p535|||||||||
3162|Burrungule Member|42827|5|Briefly described|Fig 8.9|||||||||
3162|Burrungule Member|47054|6|Mentioned|p491|||||||||
3162|Burrungule Member|60538|5|Briefly described|p470, Fig. 10, 471 Fig. 10|Early Eocene|Early Eocene|Of the Dilwyn Formation. Geological Province: Otway Basin.||||||31-JAN-07
3162|Burrungule Member|61155|5|Briefly described|p18|Middle Eocene|Early Eocene|Of the Tartwaup Formation. Max. thickness: 300m. Geological Province: Otway Basin (Gambier Embayment).||||||03-MAR-10
3162|Burrungule Member|61182|6|Mentioned|p25|||Defined by Harris (1965) for the basal mudstone unit of Nirranda Group in the South Australian part of the Otway Basin. Significantly different in age and stratigraphic relationships to Burrungule Formation of Blake (1980) in Victoria. ||||||
3162|Burrungule Member|63124|6|Mentioned|p88|||Of Harris (1966). Of the Tartwaup Formation - a synonym of Pember Mudstone (Wangerrip Group). ||||||
26442|Bushy Creek Granodiorite|23309|5|Briefly described|p41, 47, 51, 332, 337||Cambrian|Supersedes Bushy Creek Granite.  Age: 489 +/- 7Ma, 500 +/- 2Ma.||||||
26442|Bushy Creek Granodiorite|23402|3|Fully described|p21, p7 Tb. 1|Cambrian|Cambrian|Age: 489+/-7Ma (U-Pb zircon).  Intrudes Glenthompson Sandstone and Glenelg River Complex.  Previously included in the Devonian Mafeking Suite (White, et al, 1988).Geological Province: Adelaide Fold Belt||||||14-MAY-15
26442|Bushy Creek Granodiorite|24551|6|Mentioned|p717 Table 2.4, 22|Early Ordovician|Late Cambrian|Age: 495 +/- 5Ma, 499 +/- 2Ma.||||||
26442|Bushy Creek Granodiorite|40172|6|Mentioned|Map legend|Devonian|Devonian|||||||
26442|Bushy Creek Granodiorite|40887|3|Fully described|p25|||||||||
26442|Bushy Creek Granodiorite|44186|5|Briefly described|Map Legend||Early Devonian|G395 I-type. Shown as Bushy Creek.||||||
26442|Bushy Creek Granodiorite|50154|5|Briefly described|p72|Late Cambrian|Late Cambrian|Age:490 Ma. Intrudes the Glenthompson Sandstone.||||||
26442|Bushy Creek Granodiorite|50371|5|Briefly described|Map Legend|Cambrian|Cambrian|Grey porphyritic hornblende granodiorite.||||||
26442|Bushy Creek Granodiorite|60412|6|Mentioned|p236-238, 243|||Appears throughout as Bushy Creek granodiorite.|500 +/- 2 Ma (40Ar-39Ar biotite).|||||
26442|Bushy Creek Granodiorite|60451|5|Briefly described|p20, 106, 125|Late Cambrian|Late Cambrian|||||||
26442|Bushy Creek Granodiorite|61183|5|Briefly described|p21, p23|Ordovician|Cambrian|Age: 495+/-5Ma (zircon, SHRIMP), 499+/-2Ma and 500+/-2Ma (Ar/Ar dates on biotite). See also p112.||||||
26442|Bushy Creek Granodiorite|61187|5|Briefly described|p69, p130 Fig.1.|Cambrian|Cambrian|Glenelg Zone. High magnetic response.||||Intrudes Glenthompson Sandstone.||
26442|Bushy Creek Granodiorite|61749|5|Briefly described|p13, p16|Early Ordovician|Cambrian|Age: 495+/-5 Ma (SHRIMP U-Pb, Stuart-Smith, in prep.)||||||21-JAN-10
26442|Bushy Creek Granodiorite|63457|5|Briefly described|p123, p136.|||Emplaced at end of the Delamerian Orogeny. Appears as Bushy Creek Suite in Fig.10.|495 Ma (Stuart-Smith and Black, 1999).|||||
26442|Bushy Creek Granodiorite|66002|6|Mentioned|p8 Tb.5|||G395.  Defined in Buckland 1986.||||||
26442|Bushy Creek Granodiorite|66769|6|Mentioned|117|Late Cambrian|Late Cambrian|Grampians-Stavely Zone. Post-tectonic; constrains timing of major deformation in the Delamerian Orogeny. Age: 489 +/- 7 Ma (magmatic zircon Pb-U; Stuart-Smith and Black 1999).||||||
26442|Bushy Creek Granodiorite|67978|6|Mentioned|p496 Fig.1|||||||||
26442|Bushy Creek Granodiorite|68116|5|Briefly described|Appendix, Map 39.|Late Cambrian|Middle Cambrian|Informally subdivided into equigranular and porphyritic phases.|||||Hornblende-biotite granodiorite: grey, equigranular; weakly magnetic; deeply weathered. Hornblende granodiorite phase: porphyritic with phenocrysts of quartz, plagioclase, alkali feldspar and hornblende; strongly magnetic.|
26442|Bushy Creek Granodiorite|68822|6|Mentioned|p346|Paibian|Paibian|Grampians-Stavely Zone.|ca. 497 Ma|||||
26442|Bushy Creek Granodiorite|70211|5|Briefly described|p3-5, p46|||Stavely region. Two other ages are given: 489 +/- 7 Ma and 499 +/- 7 Ma.|500.0 +/- 2.0 Ma.|||||
26442|Bushy Creek Granodiorite|70877|4|Described|p2, p109, p123-p152, p167|Cambrian|Cambrian|See also p169, p172-p173, p192, p200. Grampians-Stavely Zone.  Ballarat 1:250k and Willaura 1:100k map sheets. SHRIMP ages derived from this study and represent a maximum age of deposition.  Additional SHRIMP ages include 500 +/- 2.6 Ma and 499.6 +/- 2.5 Ma and 498.2 +/- 2.3 (SHRIMP, this study) . This unit is a poorly exposed, circular, magnetically zoned pluton `8km in diameter west of the Mount Stavely Volcanic Belt. Petrography, zircon morphology and SHRIMP U-Pb results are discussed in detail for four samples of this unit.|502.5 +/- 2.6 Ma Ma (SHRIMP U-Pb)|||Intrudes the Glenthompson Sandstone.|Coarse-grained and medium-coarse grained, equigranular, biotite-bearing granodiorites.|
26442|Bushy Creek Granodiorite|70967|6|Mentioned|p28|||Stavely Belt.||||||
26442|Bushy Creek Granodiorite|71593|4|Described|p9, p19, p25, p28, p35|Late Cambrian|Late Cambrian|Delamerian Orogen, Grampians-Stavely Zone. Whelan (2007) grouped this unit with the Buckeran Diorite as the Bushy Creek Igneous Complex. An additional SHRIMP U/Pb age of 489 +/- 7 Ma is provided from Stuart-Smith and Black 1999. See also p39-p40, p76, p99, p119, p137, p188.|c. 502-498 Ma (Lewis et al., 2016)|Bushy Creek Igneous Complex||Intrudes the Glenthompson Sandstone and the Chatsworth Basalt.||
26442|Bushy Creek Granodiorite|73430|5|Briefly described|p493, p518|Cambrian|Cambrian|Mount Stavely Belt. Post-tectonic, constrains cessation of deformation at Mount Stavely Volcanic Complex. Written as Bushy Ck.Granodiorite p493 and Bushy Creek granodiorite p518.|498+/-5 Ma|||||
73823|Bushy Creek Igneous Complex|63599|4|Described|p975|Middle Cambrian|Middle Cambrian|Includes Bushy Creek Pluton (granodiorite/granite)+ Buckeran Diorite .Ages: 500+/2Ma + 495+/-5Ma (Pb-U zircon). Intrudes Glenthompson Sst and Glenelg River Complex. 5 lithologies: greenstones, diorite (Bukeran Diorite), granodiorites, granites + aplites.||||||08-DEC-16
73823|Bushy Creek Igneous Complex|70211|6|Mentioned|p6, p45|||||||Intrudes Glenthompson Sandstone.||
73823|Bushy Creek Igneous Complex|70877|5|Briefly described|p1, p3, p12, p109, p167, p169-p170|Cambrian|Cambrian|Grampians-Stavely Zone. SHRIMP ages derived from this study and represents the age of magmatic crystallisation.|502.5 +/- 2.6 Ma (SHRIMP U-Pb)||Includes Buckeran Diorite and Bushy Creek Granodiorite.|Intrudes the Glenthompson Sandstone.||
73823|Bushy Creek Igneous Complex|70967|6|Mentioned|p9-10|Cambrian|Cambrian|Stavely Arc. Large, post-tectonic, sub-circular intrusions.|489 +/- 7 Ma (Stuart-Smith and Black, 1999).|||Intrudes Glenthompson Sandstone.||
73823|Bushy Creek Igneous Complex|71593|4|Described|p35, p40, p59|Cambrian|Cambrian|Interpreted to have been deposited during the Delamerian Orogen. Geochemical features suggest similarities with subduction related magmatism and may share a genetic link with the Mount Stavely Volcanic Complex. A granodiorite stock considered part of this complex hosts the Lexington Cu prospect. See also  p68, p71, p117, p136, p174.|c. 505-500 Ma||Includes the Buckeran Diorite and the Bushy Creek Granodiorite.|||
73823|Bushy Creek Igneous Complex|72445|5|Briefly described|p8-9.|Cambrian|Cambrian|Large, post-tectonic, sub-circular intrusions.|489 +/-7 Ma; Stuart-Smith and Black, 1999|||Intrudes Glenthompson Sandstone.||
38462|Butchers Block Tonalite|24133|6|Mentioned|p65|||Geological Province: Lachlan Fold Belt.||||||
38462|Butchers Block Tonalite|68115|5|Briefly described|p7.|||Omeo Zone. Shown as Tom Groggin Granite on the previous 1:250 000 map (VandenBerg 1997) but indicated correctly in White and Chappell (1988). Distinguished by its geophysical character: moderately magnetic and very dark in the radiometrics.||||||
38462|Butchers Block Tonalite|68116|5|Briefly described|Appendix, Map 28.|Early Devonian|Early Devonian||||||Tonalite; magnetic; I-type.|
74892|Buttercup Mudstone Member|64536|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Fm (Mansfield Gp).Mudstone, shale, minor sandstone: mudstone red and grey; shale green-grey, occasion'ly dolomitic; sandstone grey, fine-grained, micaceous; fossil wood fragments, small patches of malacjite, azurite+ U renrichment.Fluvial.||||||07-FEB-11
74892|Buttercup Mudstone Member|64537|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Fm (Mansfield Gp).Mudstone, shale, minor sandstone: mudstone red and grey; shale green-grey, occasion'ly dolomitic; sandstone grey, fine-grained, micaceous; fossil wood fragments, small patches of malacjite, azurite+ U renrichment.Fluvial.||||||07-FEB-11
74892|Buttercup Mudstone Member|64538|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Fm (Mansfield Gp).Mudstone, shale, minor sandstone: mudstone red and grey; shale green-grey, occasion'ly dolomitic; sandstone grey, fine-grained, micaceous; fossil wood fragments, small patches of malacjite, azurite+ U renrichment.Fluvial.||||||07-FEB-11
74892|Buttercup Mudstone Member|64606|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation. Mudstone, shale, minor sandstone: alluvial deposits. Pink in RGB with moderate to high Th, K and U. Nonmagnetic.||||||
74892|Buttercup Mudstone Member|64616|4|Described|p139, p253, p299|Early Carboniferous|Early Carboniferous|New Member of Snowy Plains Formation. Conformably overlies Home Station Sandstone Member. Is overlain conformably by Lanky Creek Sandstone Member in the north. 50-80m thick. Dark red to grey mudstone; green-grey shale, occasionally dolomitic; minor fine-grained, micaceous sandstone. Hosts small Cu-U-V-Ag occurrences. Geophysical characteristics given.||||||
37641|Buxton Granodiorite|23309|6|Mentioned|p426, Appendix 1|||G224, S-type. Supersedes Buxton Granite.||||||
37641|Buxton Granodiorite|24551|6|Mentioned|p223, 720 Table 8.3|||||||||
37641|Buxton Granodiorite|64536|5|Briefly described|Map legend|Late Devonian|Late Devonian|Biotite-garnet granodiorite and porphyry: greenish-grey, coarse-grained, porphyritic; in some places quartz-feldspar-garnet porphyry with same composition; S-type intrusion.||||||07-FEB-11
37641|Buxton Granodiorite|64537|5|Briefly described|Map legend|Late Devonian|Late Devonian|Biotite-garnet granodiorite and porphyry: greenish-grey, coarse-grained, porphyritic; in some places quartz-feldspar-garnet porphyry with same composition; S-type intrusion.||||||07-FEB-11
37641|Buxton Granodiorite|64538|5|Briefly described|Map legend|Late Devonian|Late Devonian|Biotite-garnet granodiorite and porphyry: greenish-grey, coarse-grained, porphyritic; in some places quartz-feldspar-garnet porphyry with same composition; S-type intrusion.||||||07-FEB-11
37641|Buxton Granodiorite|64606|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Biotite-garnet granodiorite and porphyry: S-type intrusive rock. Pink and light to dark green-blue in RGB. Nonmagnetic.||||||12-NOV-08
37641|Buxton Granodiorite|64616|4|Described|p131, p204-205, p301, p434-435|Late Devonian|Late Devonian|Of Marysville Igneous Complex. Occupies the discontinuous ring dyke that partly encircles the Cerberean Cauldron. Biotite K-Ar age of 358 +/- 10 Ma. Intrudes the Montys Hut Formation, which has been hornfelsed for 40m. See also Buxton Granite p289. Greenish-grey, coarse-grained biotite-garnet granodiorite and porphyry. Geophysical characteristics given.||||||
37641|Buxton Granodiorite|68116|5|Briefly described|Appendix, Maps 33-34, 42.|Late Devonian|Late Devonian||||||Biotite-garnet granodiorite and porphyry: greenish-grey; coarse-grained; porphyritic; in some places quartz-feldspar-garnet porphyry with same composition.|
27356|Byawatha Granite|22971|5|Briefly described|p 33|||||||||
27356|Byawatha Granite|23309|6|Mentioned|p426 App1|||G197 I-Type. Supersedes Byawatha Aplite.||||||
27356|Byawatha Granite|24551|6|Mentioned|p229|||Of the Tabberabbera Province.||||||
27356|Byawatha Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|Variation on Byawatha Aplite.||||||
27356|Byawatha Granite|68116|5|Briefly described|Appendix, Map 19.|Late Devonian|Late Devonian||||||Fine-grained to aplitic granite.|
3223|Bymue Member|35272|6|Mentioned|p286|||||||||
3223|Bymue Member|41848|5|Briefly described|p361|||Member of Woorinen Formation. Age 29750 +- 1450 yrs||||||
3223|Bymue Member|42264|6|Mentioned|Fig.5 P12|||||||||
3223|Bymue Member|42827|5|Briefly described|Table 9.1|||of Woorinen Formation||||||
3223|Bymue Member|42966|2|Defined|Table35 p236|Late Pleistocene||of Woorinen Formation||||||
3223|Bymue Member|44133|6|Mentioned|p253|Holocene|Middle Pleistocene|Of the Woorinen Formation. Geological Province: Murray Basin.||||||
3251|Cabanandra Granodiorite|22876|5|Briefly described|p28|||Dalgety Supersuite||||||
3251|Cabanandra Granodiorite|22877|5|Briefly described|map|Silurian|Silurian|Dalgety Supersuite. G67. Biotite granodiorite. S-Type.||||||26-OCT-04
3251|Cabanandra Granodiorite|23309|6|Mentioned|p426 App 1|||G67.||||||
3251|Cabanandra Granodiorite|41850|6|Mentioned|p431|||||||||
3251|Cabanandra Granodiorite|42627|5|Briefly described|Map legend|Wenlock||||||||
3251|Cabanandra Granodiorite|42647|3|Fully described|p46|||||||||
3251|Cabanandra Granodiorite|42827|5|Briefly described|p431|||||||||
3251|Cabanandra Granodiorite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Biotite granodiorite: medium grained, quartz phyric; grey; S-type.|
41192|Cadden Rhyolite|50154|2|Defined|p118, p244 App.5|Devonian|Devonian|Of the Rocklands Volcanic Group.||||||25-SEP-09
41192|Cadden Rhyolite|50155|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Rhyolite lava||||||
41192|Cadden Rhyolite|50156|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Rhyolite lava: cream coloured, fine grained, small phenocrysts of quartz and feldspar||||||
41192|Cadden Rhyolite|50157|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Rhyolite lava: cream coloured, fine grained, small phenocrysts of quartz and feldspar||||||
41192|Cadden Rhyolite|50158|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Rhyolite lava: cream coloured, fine grained, small phenocrysts of quartz and feldspar||||||
41192|Cadden Rhyolite|50159|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Rhyolite lava: cream coloured, fine grained, small phenocrysts of quartz and feldspar||||||
41192|Cadden Rhyolite|50160|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group.||||||
41192|Cadden Rhyolite|50161|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Rhyolite lava: cream coloured, fine grained, small phenocrysts of quartz and feldspar||||||24-JUN-04
41192|Cadden Rhyolite|50162|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Rhyolite lava: cream coloured, fine grained, small phenocrysts of quartz and feldspar||||||
41192|Cadden Rhyolite|50163|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Rhyolite lava: cream coloured, fine grained, small phenocrysts of quartz and feldspar||||||
41192|Cadden Rhyolite|66002|5|Briefly described|p6 Tb.4|Devonian|Devonian|Of Rocklands Volcanic Group. Defined in Morand et al. 2003.||||||
37253|Cairns Creek Granodiorite|23309|6|Mentioned|p337|||G432||||||
37253|Cairns Creek Granodiorite|24012|3|Fully described|p223 appendix 1|Ordovician|Cambrian|||||||
37253|Cairns Creek Granodiorite|24551|5|Briefly described|p77|||Of the Glenelg River Complex||||||
37253|Cairns Creek Granodiorite|50154|2|Defined|p103, p246 App.5|Ordovician|Ordovician|Intrudes the Chetwynd Tonalite.||||||15-SEP-04
37253|Cairns Creek Granodiorite|50155|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende biotite granodiorite; I-type||||||
37253|Cairns Creek Granodiorite|50156|5|Briefly described|Map Legend|Ordovician|Ordovician|Rim of hornblende-biotite granodiorite and core of biotite granodiorite||||||
37253|Cairns Creek Granodiorite|50157|5|Briefly described|Map Legend|Ordovician|Ordovician|Rim of hornblende-biotite granodiorite and core of biotite granodiorite||||||
37253|Cairns Creek Granodiorite|50158|5|Briefly described|Map Legend|Ordovician|Ordovician|Rim of hornblende-biotite granodiorite and core of biotite granodiorite||||||
37253|Cairns Creek Granodiorite|50159|5|Briefly described|Map Legend|Ordovician|Ordovician|Rim of hornblende-biotite granodiorite and core of biotite granodiorite.||||||
37253|Cairns Creek Granodiorite|50160|5|Briefly described|Map Legend|Ordovician|Ordovician|Rim of hornblende-biotite granodiorite and core of biotite granodiorite||||||
37253|Cairns Creek Granodiorite|50161|5|Briefly described|Map Legend|Ordovician|Ordovician|Rim of hornblende-biotite granodiorite and core of biotite granodiorite.||||||
37253|Cairns Creek Granodiorite|50162|5|Briefly described|Map Legend|Ordovician|Ordovician|Rim of hornblende-biotite granodiorite and core of biotite granodiorite.||||||
37253|Cairns Creek Granodiorite|50163|5|Briefly described|Map Legend|Ordovician|Ordovician|Rim of hornblende-biotite granodiorite and core of biotite granodiorite.||||||21-JUN-04
37253|Cairns Creek Granodiorite|50164|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-biotite granodiorite; I-type.||||||
37253|Cairns Creek Granodiorite|66002|6|Mentioned|p9 Tb.5|||G432. Defined by Kemp et al. 2002||||||
37253|Cairns Creek Granodiorite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Late Cambrian|Magnetic rim with a weakly magnetic core. The rim contains accessory magnetite, sphene and allanite, whilst the core has accessory magnetite and sphene.|||||Hornblende-biotite granodiorite. Rim: massive, pale greenish, coarse grained, porphyritic with plagioclase, biotite, hornblende and quartz phenocrysts. Core: massive, coarse grained, alkali feldspar-phyric to equigranular.|
3304|Caladenia Limestone Member|23309|6|Mentioned|p86|||||Towanga Sandstone||||31-OCT-14
3304|Caladenia Limestone Member|23710|5|Briefly described|p70|||||||||
3304|Caladenia Limestone Member|37727|6|Mentioned|p49|||||||||
3304|Caladenia Limestone Member|39447|6|Mentioned|p9|||||||||
3304|Caladenia Limestone Member|40328|6|Mentioned|p70|||||Towanga Formation||||23-DEC-14
3322|Calivil Formation|2967|4|Described|p14, p15 Fig.2.2, p17-20, 22-23, 26-37|Pliocene|Miocene|Macumber (1973). Eastern Murray Basin. The type section is from 77m to 95m in the Mines Department Calivil No. 2 bore. Locally, these sediments occupy valleys incised into Renmark Group units. A main regional aquifer (semi-confined). Misprinted as Cavil Formation twice on p110. Hydrochemistry (""salinity"") detailed. See also p40-41, 43, 45-46, 77-88, 90-91, 93-97, 101-102, 105, 108-113, 117, 128, 132, 135, 137, 139-152, 155, 178, 181, 336-337.||Wunghnu Group.||Is separated from the underlying Olney Formation (Renmark Group) by the Mologa Surface. Is overlain by Shepparton Formation, Parilla Sand and Yando Clay.|Valley-fill, fluviatile coarse-grained quartz gravel, pebbles.|
3322|Calivil Formation|10010|5|Briefly described|p12 Fig. 3, p17|Early Pliocene|Late Miocene|Of Wunghnu Group. Overlies upper part of Renmark Group. Grades upwards into Shepparton and Coonambidgal Formations. Geological Province: Murray Basin. Considered to be fluvial counterpart of Loxton-Parilla Sands.||||||13-AUG-07
3322|Calivil Formation|22756|3|Fully described|P13, P31||Tertiary|||||||
3322|Calivil Formation|22773|5|Briefly described|Fig24.8p352,354|||||||||
3322|Calivil Formation|22782|6|Mentioned|p15|||||||||
3322|Calivil Formation|22857|5|Briefly described|p352-3 Figs. 24.8 and 24.9, p354|Early Pliocene|Early Pliocene|Of the Wunghnu Group. A porous fluvio-lacustrine unit that is an important basin-wide aquifer. At the margins of the basin this unit contains conglomerate as well as sands. Geological Province: Murray Basin.||||||09-OCT-08
3322|Calivil Formation|22886|5|Briefly described|p36|Early Pliocene|Late Miocene|||||||
3322|Calivil Formation|22887|2|Defined|p34, Fig.6 p13|Pliocene|Late Miocene|||||||
3322|Calivil Formation|22893|3|Fully described|p29 fig9 table3|Pliocene|Late Miocene|||||||
3322|Calivil Formation|22971|4|Described|p26, p27|||Max. thickness: <25m. Geological Province: Murray Basin.||||||19-JAN-06
3322|Calivil Formation|23089|5|Briefly described|p649|||||||||
3322|Calivil Formation|23164|4|Described|p15|Oligocene|Eocene|||||||
3322|Calivil Formation|23252|5|Briefly described|Map Legend|||||||||11-JAN-10
3322|Calivil Formation|23300|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
3322|Calivil Formation|23302|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
3322|Calivil Formation|23303|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
3322|Calivil Formation|23304|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
3322|Calivil Formation|23305|4|Described|p52|||Of Macumber (1972). Overlain by Newer Volcanics. Geological Province: Lachlan Fold Belt. Max. thickness: 4 m.||||||09-OCT-08
3322|Calivil Formation|23884|5|Briefly described|p153, p155 Fig.13.2|||Geological Province: Murray Basin. Of the Wunghnu Group.||||||28-APR-05
3322|Calivil Formation|23921|4|Described|p1109, p1114|Pliocene|Pliocene|Geological Province: Murray Basin.||||||
3322|Calivil Formation|24043|5|Briefly described|p525|Pliocene|Pliocene|||||||
3322|Calivil Formation|24103|5|Briefly described|p139 Fig.3, p143 Fig.6|Tertiary|Tertiary|Middle Tertiary.||||||
3322|Calivil Formation|24105|5|Briefly described|p155|Miocene|Miocene|||||||
3322|Calivil Formation|24106|5|Briefly described|p185|Pliocene|Late Miocene|||||||
3322|Calivil Formation|24107|6|Mentioned|p224|||||||||
3322|Calivil Formation|24108|5|Briefly described|p242|Pliocene|Late Miocene|Geological Province: Murray Basin. Overlying Unit: Shepparton Formation.||||||
3322|Calivil Formation|24177|3|Fully described|p71|Late Miocene|Late Eocene|Interfingers with Parilla Sand. Overlies the Renmark Group. Overlain by the Newer Volcanics and Shepparton Volcanics. Interpretation of age varies. Geological Province: Murray Basin.||||||
3322|Calivil Formation|24219|5|Briefly described|p870|||||||||
3322|Calivil Formation|24232|5|Briefly described|p227, p231|Tertiary|Tertiary|||||||
3322|Calivil Formation|24328|5|Briefly described|Map legend|Neogene|Neogene|||||||
3322|Calivil Formation|24329|5|Briefly described|Map legend|Neogene|Neogene|||||||
3322|Calivil Formation|24383|4|Described|p10, 18|Pliocene|Oligocene|Age: 40 - 5Ma. Overlying Unit: Newer Volcanic Group. Underlying Unit: Castlemaine Group. Underlain by  White Hills Gravel, which provided source material for Calivil Formation. Geological Province: Lachlan Fold Belt||||||07-JUL-20
3322|Calivil Formation|24384|5|Briefly described|Map legend|Eocene|Eocene|Quartz cobble conglomerate.||||||
3322|Calivil Formation|24385|5|Briefly described|Map legend|Eocene|Eocene|Quartz cobble conglomerate.||||||
3322|Calivil Formation|24386|5|Briefly described|Map legend|Eocene|Eocene|Quartz cobble conglomerate||||||
3322|Calivil Formation|24387|5|Briefly described|Map legend|Eocene|Eocene|Quartz cobble conglomerate.||||||
3322|Calivil Formation|24388|5|Briefly described|Map legend|Eocene|Eocene|Quartz cobble conglomerate; nonmagnetic.||||||
3322|Calivil Formation|24439|5|Briefly described|p8, p23|||See also p9 Fig. 3. Author disputes presence of this unit in BENDIGO as defined by Macumber (1991) - see p. 37.  Fluvial deposits.||||||14-SEP-05
3322|Calivil Formation|24440|5|Briefly described|Map legend|||||||||
3322|Calivil Formation|24551|5|Briefly described|p322, 321, 421, 543|||Of the Murray Group.  Max thickness: 50m.||||||
3322|Calivil Formation|31713|6|Mentioned|p16|||||||||
3322|Calivil Formation|31746|6|Mentioned|p197|||In reference to Macumber (1972).||||||25-JUN-13
3322|Calivil Formation|31951|3|Fully described|p7|||||||||
3322|Calivil Formation|31953|6|Mentioned|p9|||||||||
3322|Calivil Formation|32232|6|Mentioned|p19|||||||||
3322|Calivil Formation|34735|6|Mentioned|p30|||||||||
3322|Calivil Formation|34757|6|Mentioned|p45|||||||||
3322|Calivil Formation|34813|5|Briefly described|p63|||Also mentioned on P62||||||
3322|Calivil Formation|35091|4|Described|p8|||Also p29.||||||07-JUL-20
3322|Calivil Formation|35172|4|Described|p127|||||||||
3322|Calivil Formation|35187|6|Mentioned|Table1|||||||||
3322|Calivil Formation|35242|6|Mentioned|p94|||||||||
3322|Calivil Formation|39329|6|Mentioned|p483|||||||||
3322|Calivil Formation|39330|6|Mentioned|p487|||||||||
3322|Calivil Formation|39446|6|Mentioned|p49|||||||||
3322|Calivil Formation|39967|6|Mentioned|p41|||||||||
3322|Calivil Formation|40520|6|Mentioned|Fig.5|||||||||
3322|Calivil Formation|40599|5|Briefly described|p19|||||||||
3322|Calivil Formation|40664|6|Mentioned|p248|||||||||
3322|Calivil Formation|40820|6|Mentioned|Fig.4|||||||||
3322|Calivil Formation|41068|5|Briefly described|p67|||||||||
3322|Calivil Formation|41765|4|Described|p36|||||||||
3322|Calivil Formation|41868|5|Briefly described|p551|||||||||
3322|Calivil Formation|42125|5|Briefly described|p137|||See also Fig.5||||||
3322|Calivil Formation|42126|6|Mentioned|p149,p151|||||||||
3322|Calivil Formation|42130|6|Mentioned|Fig.3 P265|||||||||
3322|Calivil Formation|42133|6|Mentioned|p302|||||||||
3322|Calivil Formation|42134|4|Described|p339|||||||||
3322|Calivil Formation|42137|6|Mentioned|p370|||||||||
3322|Calivil Formation|42138|6|Mentioned|p392|||||||||
3322|Calivil Formation|42454|4|Described|p11|early Pliocene|late Miocene|||||||
3322|Calivil Formation|42455|5|Briefly described|Map legend|early Pliocene|late Miocene|||||||
3322|Calivil Formation|42509|6|Mentioned|p4|||||||||
3322|Calivil Formation|42827|6|Mentioned|p271|||refers to Macumber (1972)||||||
3322|Calivil Formation|42881|4|Described|Fig.3, P84|||||||||
3322|Calivil Formation|42966|2|Defined|p179|Pliocene|Late Miocene|Of the Wunghnu Group.||||||09-OCT-08
3322|Calivil Formation|43198|5|Briefly described|Map Legend|Oligocene|Eocene|||||||
3322|Calivil Formation|43199|5|Briefly described|Map Legend|Oligocene|Eocene|||||||
3322|Calivil Formation|43211|4|Described|p4,Fig.5 p15,27-8|Oligocene|Eocene|||||||
3322|Calivil Formation|43260|5|Briefly described|Map Legend|Miocene|Oligocene|||||||
3322|Calivil Formation|43261|5|Briefly described|Map Legend|Oligocene|Eocene|||||||
3322|Calivil Formation|43493|4|Described|32|Oligocene|Eocene|||||||
3322|Calivil Formation|43601|6|Mentioned|p224||Early Pliocene|||||||
3322|Calivil Formation|43655|5|Briefly described|p40-846|||||||||
3322|Calivil Formation|43780|6|Mentioned|p6|||||||||
3322|Calivil Formation|43791|6|Mentioned|p372, Fig1|||||||||
3322|Calivil Formation|43804|6|Mentioned|Fig.2,p49|||||||||
3322|Calivil Formation|43846|5|Briefly described|14||Oligocene|||||||
3322|Calivil Formation|44188|5|Briefly described|Map Legend|Pliocene|Pliocene|Geological province: Murray Basin. Fluvial deposits- poorly consolidated pale grey, poorly sorted coarse to granular quartz sand, conglomerate with white kaolinitic matrix.||||||25-JUN-13
3322|Calivil Formation|44931|5|Briefly described|Map Legend|Tertiary|Tertiary|Alluvial clay and sand, and minor gravel.||||||14-JUN-06
3322|Calivil Formation|49038|4|Described|Table 2|||Briefly described p26||||||07-JUL-20
3322|Calivil Formation|49040|6|Mentioned|p12|||||||||
3322|Calivil Formation|50154|5|Briefly described|p133|Pliocene|Late Miocene|Overlies the Renmark Group. Geological Province: Murray Group.||||||
3322|Calivil Formation|60451|4|Described|p30, 95 Fig. 61, 98, 253|Pliocene|Eocene|Age: 40-6Ma, but not directly dated.  Palynology indicates max age. Overlain by Miocene-Pliocene units. Interfingers with the Renmark, Murray and Wunghnu Groups. Underlies: Parilla Sand, Shepparton Formation, Newer Volcanics.||||||24-JUN-14
3322|Calivil Formation|60452|4|Described|p35|Cenozoic|Cenozoic|First named by Macumber (1973), then called Calivil Sand (Lawrence, 1975) but reverted to original name of Calivil Formation (Tickell & Humphreys, 1980). Overlies Castlemaine Group, diconformably overlies Renmark Group. Overlain by Shepparton Formation.||||||19-NOV-08
3322|Calivil Formation|60454|5|Briefly described|Map Legend|Neogene|Paleogene|Pre-basaltic overbank, point bar and channel lag sequences.||||||07-NOV-08
3322|Calivil Formation|60456|5|Briefly described|Map Legend|Neogene|Paleogene|Pre-basaltic overbank, point bar and channel lag sequence; poorly sorted gravel, sand and minor kaolinitic clay.||||||07-NOV-08
3322|Calivil Formation|60457|5|Briefly described|Map Legend|Neogene|Paleogene|Pre-basaltic overbank, point bar and channel lag sequence also known as 'Older Gold Drift' and 'deep leads': often richly auriferous; poorly sorted gravel, sand and minor kaolinitic clay.||||||25-JUN-13
3322|Calivil Formation|60458|5|Briefly described|Map Legend|Neogene|Paleogene|Pre-basaltic overbank, point bar and channel lag sequence also known as 'Older Gold Drift' and 'deep leads'.||||||07-NOV-08
3322|Calivil Formation|60459|5|Briefly described|Map Legend|Neogene|Paleogene|Pre-basaltic alluvium now entirely buried beneath younger units.||||||07-NOV-08
3322|Calivil Formation|60461|5|Briefly described|Map legend|Miocene|Oligocene|Of the Murray Group.  River valley deposits - Powlett Plains deep lead and colluvium: interbedded clay, silty clay, silt and subangular to subrounded fine to coarse-grained quartz sand, reef quartz and metasediment gravel, minor ligneous clay.||||||28-SEP-04
3322|Calivil Formation|60462|5|Briefly described|Map Legend|Neogene|Neogene|Poorly sorted fine to coarse grained terrestrial sand: magnetic where ferruginised with responses to 20 nT; where cropping out thorium high.||||||15-SEP-04
3322|Calivil Formation|60491|4|Described|p16, p21|||Interfingers with the Parilla Sand. Consists of fluvial and fluviolacustrine quartzose sand and gravel.||||||
3322|Calivil Formation|60492|5|Briefly described|Map Legend|Miocene|Miocene|Alluvium: gravel, sand, silt, conglomerate.||||||
3322|Calivil Formation|60529|5|Briefly described|Map Legend|Pliocene|Miocene|Goulburn Valley deep lead river deposits: interbedded clay, silty-clay, silt, and sub-angular to sub-rounded fine to coarse grained sand, gravel; poorly sorted, unconsolidated.||||||
3322|Calivil Formation|60581|5|Briefly described|Map Legend|Pliocene|Eocene|Variably rounded gravels of vein quartz, minor bedrock and White Hills Gravel clasts with sand, silt, clay and plant material.||||||
3322|Calivil Formation|60582|5|Briefly described|Map Legend|Pliocene|Eocene|Variably rounded gravels of vein quartz, minor bedrock and White Hills Gravel clasts with sand, silt, clay and plant material.||||||23-NOV-04
3322|Calivil Formation|60583|5|Briefly described|Map Legend|Pliocene|Eocene|Variably rounded gravels of vein quartz, minor bedrock and White Hills Gravel clasts with sand, silt, clay and plant material.||||||
3322|Calivil Formation|60584|5|Briefly described|Map Legend|Pliocene|Eocene|Variably rounded gravels of vein quartz, minor bedrock and White Hills Gravel clasts with sand, silt, clay and plant material.||||||
3322|Calivil Formation|60585|4|Described|p28|Pliocene|Late Eocene|Disconformably overlain by the Moorabool Viaduct Sand. Consists of poorly to moderately sorted polymictic cobbles, pebbles, sand and clay that have been ferruginised or silicified.||||||
3322|Calivil Formation|60591|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and unconformably overlies the Urana Formation. Clay, silty clay, silt, and fine- to coarse-grained sand, gravel; poorly sorted, subangular to subrounded, unconsolidated.||||||
3322|Calivil Formation|60592|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and unconformably overlies the Urana Formation. Clay, silty clay, silt, and fine- to coarse-grained sand, gravel; poorly sorted, subangular to subrounded, unconsolidated.||||||25-NOV-04
3322|Calivil Formation|60593|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and unconformably overlies the Urana Formation. Clay, silty clay, silt, and fine- to coarse-grained sand, gravel; poorly sorted, subangular to subrounded, unconsolidated.||||||
3322|Calivil Formation|60595|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and unconformably overlies the Urana Formation. Clay, silty clay, silt, and fine- to coarse-grained sand, gravel; poorly sorted, subangular to subrounded, unconsolidated.||||||
3322|Calivil Formation|60596|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and unconformably overlies the Urana Formation. Clay, silty clay, silt, and fine- to coarse-grained sand, gravel; poorly sorted, subangular to subrounded, unconsolidated.||||||
3322|Calivil Formation|60597|5|Briefly described|Map Legend|Pliocene|Miocene|Deep lead fluvial deposits: no distinctive magnetic responses.||||||
3322|Calivil Formation|60599|5|Briefly described|p15, p85|Late Eocene|Middle Miocene|Of the Wunghnu Group. Fluvial sediments. Geological Province: Murray Basin.||||||09-OCT-08
3322|Calivil Formation|61160|5|Briefly described|p150|Pliocene|Miocene|Buried auriferous gravels or deep leads within this unit are present in valleys of the upper Ovens River and Morses Creek in BUFFALO. ||||||
3322|Calivil Formation|61163|6|Mentioned|p99|||Of Wunghnu Gp. Overlies Shepparton Fm. Poorly sorted gravels with abundance of sandstone clasts now fragile due to in-situ weathering; vein quartz clasts are subangular to subrounded. Economically important due to placer gold content. Geol Prov: LFB||||||05-JUL-07
3322|Calivil Formation|61174|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Gravel, sand, silt, clay: generally consolidated (in subsurface only). GSV map code: Nwc.||||||07-FEB-11
3322|Calivil Formation|61175|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Gravel, sand, silt, clay: generally consolidated (in subsurface only). GSV map code: Nwc.||||||
3322|Calivil Formation|61176|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Gravel, sand, silt, clay: generally consolidated (in subsurface only). GSV map code: Nwc.||||||
3322|Calivil Formation|61177|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Gravel, sand, silt, clay: generally consolidated (in subsurface only). GSV map code: Nwc.||||||
3322|Calivil Formation|61185|2|Defined|p57-62, p15, p64|Pliocene|Late Miocene|Of Macumber (1973). Of Wunghnu Gp. Reworked White Hills Gravel and colluvial seds. Under Shepparton Fm and Newer Volcanics; disconf. over Renmark Gp; conform. over/interfingers with Parilla Sand. Subsurface in NAGAMBIE. See Calivil Sand. Auriferous.||||||07-FEB-11
3322|Calivil Formation|61701|5|Briefly described|Map Legend|Pliocene|Miocene|Goulburn Valley deep lead river deposits: interbedded clay, silty-clay, silt, and sub-angular to sub-rounded fine to coarse grained sand, gravel; poorly sorted, unconsolidated.||||||15-JUN-06
3322|Calivil Formation|61702|5|Briefly described|Map Legend|Pliocene|Miocene|Goulburn Valley deep lead river deposits: interbedded clay, silty-clay, silt, and sub-angular to sub-rounded fine to coarse grained sand, gravel; poorly sorted, unconsolidated.||||||15-JUN-06
3322|Calivil Formation|61703|5|Briefly described|Map Legend|Pliocene|Miocene|Goulburn Valley deep lead river deposits: interbedded clay, silty-clay, silt, and sub-angular to sub-rounded fine to coarse grained sand, gravel; poorly sorted, unconsolidated.||||||15-JUN-06
3322|Calivil Formation|61822|6|Mentioned|p107|Neogene|Neogene|||||||
3322|Calivil Formation|61964|3|Fully described|p14 Fig. 4p141-143|Pliocene|Late Miocene|Of Murray Group? Fluvial gravels, sands and fine-grained sands  pale grey, poorly sorted medium- to coarse-grained quartz sand/sandstone with a white kaolinitic clay matrix. Unconformably overlies Olney Formation (Renmark Group). Geol. Prov: Murray Basin||||||09-OCT-08
3322|Calivil Formation|62370|5|Briefly described|p447, p452 Fig.4|Early Pliocene|Late Miocene|Fluvial deep-lead infill of sand and cobble conglomerate, and includes pallid clay and ferruginous clasts, recycled pebbles and locally eroded bedrock, in some areas has a magnetic ferricrete cap. Unconformably underlies Shepparton Formation.||||||
3322|Calivil Formation|62405|5|Briefly described|Map legend|Tertiary|Tertiary|Poorly consolidated to unconsolidated, cross-bedded, poorly sorted, medium- to coarse-grained quartz sand and sandstone, white clay-rich matrix;interbedded siltstone and claystone; silicified and ferruginised duricrust common.||||||13-MAY-13
3322|Calivil Formation|64314|5|Briefly described|p498 Fig. 3, p502 Fig. 7|Late Miocene|Late Eocene|Of Macumber (1973). Thickness: ~30m. Use also in the compound name Yaloak/Calivill Formation. See also p500 Fig. 5, p501.||||||
3322|Calivil Formation|64568|5|Briefly described|Map legend|Silurian|Silurian|Geol.Prov: Murray Basin. [Note: map symbol suggests Tertiary age]. Poorly consolidated to unconsolidated, cross-bedded, poorly sorted, medium- to coarse-grained quartz sand and sandstone, white clay-rich matrix; interbedded siltstone and claystone; silicified and ferruginised duricrust is common.||||||24-JUN-14
3322|Calivil Formation|64612|6|Mentioned|p28|Cainozoic|Cainozoic|||||||07-FEB-11
3322|Calivil Formation|64823|5|Briefly described|p1011|||Paleochannel deposits. Geological province: Murray Basin.||||||
3322|Calivil Formation|65552|5|Briefly described|p2, p5 Fig.3, p6-8, p13, p15, p19|Early Pliocene|Late Miocene|See also p24 App.3, p26 App.5. Of Wanghnu Group, eastern Murray Basin. Medium to coarse grained quartz sand/sandstone with locally thick kaolin lenses. Overlies Olney Formation (Renmark Group), conformably underlies Shepparton and Coonambidgal Formations.||||||
3322|Calivil Formation|65715|5|Briefly described|p11 Tb.7, p11-12, 14, 16, 26, 27|Miocene|Miocene|Included in Wunghnu Group by Lawrence (1975). Correlated with older Murray Group by Holdgate and Gallagher (2003). Overlies Werribee Formation. Underlies Newer Volcanics. Younger than White Hills Gravel. Distribution modified see p14.||||||06-FEB-15
3322|Calivil Formation|65969|5|Briefly described|p27 Tb.3.3, p30-1|Miocene|Oligocene|Murray Basin. Erosional contact with underlying Olney Formation. Of Murray Group. Typically clay and silt interbedded with sand and gravel. Fines to the north of the BENDIGO 1:250 000 sheet. Occurs in paleotopographic lows and fills paleovalleys. Up to 70 m thick. Extensively worked for gold near Bendigo. Minor areas have magnetic responses to 15 nT; no distinctive radiometric response.||||||
3322|Calivil Formation|66002|5|Briefly described|p10 Tb.7, p12|Paleogene|Paleogene|Correlative of (obsolete) Loddon River Group. Previously included in Wunghnu Group (1975), but shown to correlate with Murray Group (Holdgate & Gallagher 2003). See also Macumber 1991.||||||15-MAY-13
3322|Calivil Formation|67179|6|Mentioned|p581|Pliocene|Miocene|Fluvial valley fill east of study area.||||Interfingers with the Loxton Sand (lateral equivalent). ||
3322|Calivil Formation|68116|5|Briefly described|Appendix, Maps 22-24, 30-32, 40-41, 50.|Miocene|Oligocene||||||Conglomerate, sandstone, silt, clay: brown to pale colours; poorly sorted; clasts variably rounded; predominant vein quartz clasts; cross-bedding prominent.|
3322|Calivil Formation|68140|5|Briefly described|p1699|Pliocene|Pliocene|No outcrop. In hydraulic conductivity with the underlying Renmark Formation throughout much of the Riverine Province; they commonly form a single aquifer, and are referred to in this article as Calivil-Renmark Formation (see references p1698, p1699, p1702, pp1705-1708).||||Underlain by the Renmark Formation.|Sands.|09-FEB-18
3322|Calivil Formation|68189|5|Briefly described|p4, p26-29, p33|Miocene|Oligocene|River valley depositional environment. Upstream time equivalent of the younger part of the Olney Formation. Truncated by the Mologa Surface. Hosts alluvial Au won in ST ARNAUD in the near surface and where it forms deep leads.||||Nonconformably underlain by the White Hills Gravel.|Comprises mud, subangular to subrounded sand, reef quartz gravel.|
3322|Calivil Formation|68194|5|Briefly described|p9, p17, p21, p23, p25-26, p35-36, p40|Pliocene|Pliocene|See also p44, p55. Macumber (1972). Preserved on hills and rises, overlying weathered bedrock or Parilla Sand. Regolith and remote sensing profiles described. Age given as Eocene on p55.||Unit in Murray Group.||Lateral facies equivalent of Geera Clay.|Alluvial sands in paleovalleys, and gravels overlying bedrock highs.|
3322|Calivil Formation|68203|6|Mentioned|p11|Pliocene|Miocene|Deposition coincided with the first of two uplifts (~15-20m) of the Cadell Fault.||||||
3322|Calivil Formation|69162|5|Briefly described|Map legend|Tertiary|Tertiary|Murray Basin.|||||Poorly consolidated to unconsolidated, cross-bedded, poorly sorted, medium- to coarse-grained quartz sand and sandstone, white clay-rich matrix; interbedded siltstone and claystone; silicified and ferruginised duricrust common.|
3322|Calivil Formation|69163|5|Briefly described|Map legend|Tertiary|Tertiary|Murray Basin.|||||Poorly consolidated to unconsolidated, cross-bedded, poorly sorted, medium- to coarse-grained quartz sand and sandstone, white clay-rich matrix; interbedded siltstone and claystone; silicified and ferruginised duricrust common.|
3322|Calivil Formation|69164|5|Briefly described|Map legend|Tertiary|Tertiary|Murray Basin.|||||Poorly consolidated to unconsolidated, cross-bedded, poorly sorted, medium- to coarse-grained quartz sand and sandstone, white clay-rich matrix; interbedded siltstone and claystone; silicified and ferruginised duricrust common.|
3322|Calivil Formation|69798|6|Mentioned|p4 Fig.2|Pliocene|Pliocene|Murray Basin.||Wunghnu Group.||||
3322|Calivil Formation|70718|5|Briefly described|p17, p25|Cenozoic|Cenozoic|Is one of the primary aquifers in the Hay map sheet area. Misspellt as the Calival Formation on p25.||||Overlain by the Loxton Sand. Overlies the Upper Renmark Beds [Olney Formation]. Transitionally overlain by the Shepparton Formation.|Relatively coarse and poorly sorted fluvial sands and muddy overbank deposits.|30-MAY-19
3322|Calivil Formation|71419|5|Briefly described|p8 Fig 2, p14, p17-18.|Miocene|Miocene|Fluvial sediments derived from the Western Uplands. Source for later marine deposits i.e. Sandringham Sandstone.||||Overlain by Sandringham Sandstone.|Contains conglomerate consisting almost exclusively of vein quartz clasts.|02-FEB-18
3322|Calivil Formation|71593|5|Briefly described|p52, p54|||||Wunghu Group||||
3322|Calivil Formation|72445|5|Briefly described|App.1; App.2; App.7 p7-8, p7 Fig.4.|Pliocene|Miocene|Characterised by the organic-poor nature of the sands that are a major component of this formation. Said to be non-marine. App.2 is a .csv format file.  Identified in Stavely 05,07,11,12. Partially equivalent to Torrumbarry Clay, Bookpurnong beds/Formation.||Wunghnu Group ? Of Murray Group (App 2)||Underlies Woorinen Formation (gradational), Loxton Sand (sharp or gradational contact), Shepparton Formation. Overlies Olney, Bookpurnong Formations (sharp contacts).|Shown as including sand, gravel, lignite, mud and conglomerate.|
3322|Calivil Formation|73118|5|Briefly described|p81|Pliocene|Miocene|Extensive blanket underlies much of the Riverine Plain and N fringes of the Murray Basin. Deposited in valley-fill, alluvial-fan, fluviolacustrine and braided-channel environments.||Wunghnu Group.|||Poorly consolidated, pale grey, poorly sorted coarse to granular quartz sand, conglomerate, with white kaolinitic matrix; thick intercalations of carbonaceous clay.|
3322|Calivil Formation|73228|6|Mentioned|p56, p62|Pliocene|Late Miocene|Fluvial counterpart of the Loxton Sand.||||Underlain by upper Renmark Group.|Coarse and poorly sorted fluvial sands and muddy overbank deposits.|
3322|Calivil Formation|73496|6|Mentioned|Map legend|Miocene|Oligocene|||||||
3322|Calivil Formation|73497|5|Briefly described|Map legend|Pliocene|Miocene|||Wunghnu Group|||Fluvial deposits: no distinctive magnetic or radiometric response.|
3322|Calivil Formation|73505|4|Described|p2, p11, p13, p36|Miocene|Late Eocene|Murray Basin. Nonmarine, occurs in palaeotopographic lows. Lateral equivalents interfinger with the Geera Clay. Minor areas where channels have magnetic responses to 15 nT.||Murray Group||Overlies Olney Formation with erosional contacts, onshore equivalent to Geera Clay, underlies Parilla Sand, Blanchetown Clay|Fluvial sand and mud, gravel, coarsening to the south.|
34350|Callemondah Conglomerate|22729|2|Defined|p583,585,587|Devonian|Devonian|Upgrading of basal unit of Delatite Group.||||||22-DEC-08
34350|Callemondah Conglomerate|23309|4|Described|p173, 174, 180, 184  Table 2.65|||||||||22-FEB-10
34350|Callemondah Conglomerate|24551|4|Described|p168, 171.|||Maximum Thickness: 110m. Overlying Unit: Kevington Creek Formation. Of the Delatite Group.||||||22-DEC-08
34350|Callemondah Conglomerate|61161|5|Briefly described|p125|||Of Delatite Group. Mansfield Basin. Underlies Kevington Creek Formation.||||||
34350|Callemondah Conglomerate|64010|5|Briefly described|p258 Fig.1. |||||Of the Kevington Creek Formation.||||
34350|Callemondah Conglomerate|64536|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Of Delatite Group. Conglomerate, sandstone, mudstone: conglomerate polymictic, pebbles and cobbles of vein quartz, metasedimentary rock, chert, siltstone, imbricated - forms prominent bluffs. Sandstone and mudstone red, lithic. Fluvial deposits.||||||07-FEB-11
34350|Callemondah Conglomerate|64537|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Of Delatite Group. Conglomerate, sandstone, mudstone: conglomerate polymictic, pebbles and cobbles of vein quartz, metasedimentary rock, chert, siltstone, imbricated - forms prominent bluffs. Sandstone and mudstone red, lithic. Fluvial deposits.||||||07-FEB-11
34350|Callemondah Conglomerate|64538|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Of Delatite Group. Conglomerate, sandstone, mudstone: conglomerate polymictic, pebbles and cobbles of vein quartz, metasedimentary rock, chert, siltstone, imbricated - forms prominent bluffs. Sandstone and mudstone red, lithic. Fluvial deposits.||||||07-FEB-11
34350|Callemondah Conglomerate|64606|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Of Delatite Group. Conglomerate, sandstone, mudstone: alluvial deposits. Red-pink to blue-green in RGB. Nonmagnetic.||||||11-NOV-08
34350|Callemondah Conglomerate|64616|4|Described|p132, p187-189, p279, p301|Givetian|Givetian|Of Delatite Group. Unconformably overlies mainly Murrindindi Supergroup. Conformably overlain by Kevington Creek Formation. 110m thick in type section. Polymictic pebble and cobble conglomerate, red lithic sandstone and mudstone. Geophysical characteristics given.||||||
34350|Callemondah Conglomerate|68116|5|Briefly described|Appendix, Map 34.|Late Devonian|Late Devonian||||||Conglomerate, sandstone, mudstone: conglomerate is polymictic with imbricated pebbles and cobbles of vein quartz, metasedimentary rock, chert, siltstone; forms prominent bluffs. Sandstone and mudstone red; sandstone lithic.|
3361|Calton Hill Sandstone Member|22511|6|Mentioned|p661|||||||||
3361|Calton Hill Sandstone Member|22684|5|Briefly described|Fig.2 p746|Llandovery|Llandovery|See also Fig.5 p749||||||
3361|Calton Hill Sandstone Member|22886|6|Mentioned|p53|||||||||
3361|Calton Hill Sandstone Member|23309|5|Briefly described|p139  Table 2.50|||||||||
3361|Calton Hill Sandstone Member|42628|5|Briefly described|Map legend|Silurian||Variation on Calton Hill Conglomerate Member. Age: Silurian (Wenlock?)||||||
3361|Calton Hill Sandstone Member|42826|2|Defined|p41|Early Silurian||Of Springfield Sandstone.||||||14-APR-08
3361|Calton Hill Sandstone Member|63083|6|Mentioned|p218|Telychian|Telychian|Of the Springfield Formation.||||||07-FEB-11
31564|Campbell Knob Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
30562|Campbells Knob Granodiorite|23309|6|Mentioned|p338, 427|||(G66). S-Type||||||04-NOV-14
30562|Campbells Knob Granodiorite|23615|3|Fully described|p153, p32|Early Silurian|Early Silurian|Of Bullenbalong Suite. See also p204 Appendix 1. Coarse- to medium-grained, pale biotite-granodiorite. Non-conformably overlain and intruded by the Snowy River Volcanics.||||||25-SEP-08
30562|Campbells Knob Granodiorite|23938|6|Mentioned|p53|||See also p27.||||||25-SEP-08
30562|Campbells Knob Granodiorite|24551|5|Briefly described|p142 Fig. 5.34|||||||||
30562|Campbells Knob Granodiorite|43206|5|Briefly described|map legend||Wenlock|Of Bullenbalong Suite. Misspelling of Campbell Knob Granodiorite?||||||
30562|Campbells Knob Granodiorite|44185|5|Briefly described|Map legend.|Silurian|Silurian|Said to be I-type [in error?]||||||04-NOV-14
30562|Campbells Knob Granodiorite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Biotite granodiorite: medium grained; pale grey; abundant gneiss and biotite schist enclaves, aplite and Snowy River Volcanic dykes.|
37642|Camview Granite|23309|6|Mentioned|p427, Appendix 1|||G209, S-type. Formerly Katandra Granite.||||||
37642|Camview Granite|68116|5|Briefly described|Appendix, Map 18.|Late Devonian|Late Devonian||||||Biotite granite: varies from evenly medium grained to coarse grained and weakly porphyritic in both feldspars; tourmaline is present, both disseminated and in nodules.|
3452|Candelo Supersuite|22878|6|Mentioned|p82|||||||||
3452|Candelo Supersuite|22879|5|Briefly described|map|Early Devonian|Early Devonian|||||||
3452|Candelo Supersuite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Nungatta Granodiorite||||||01-OCT-04
3452|Candelo Supersuite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||06-OCT-04
3452|Candelo Supersuite|24551|5|Briefly described|p235|||||||||
3452|Candelo Supersuite|42726|5|Briefly described|map legend||Early Devonian|Includes the Belowra, Braidwood, Candelo, Hopping Joe, Jinden, Nungatta and Watch Box Suites.||||||09-FEB-05
3452|Candelo Supersuite|42827|5|Briefly described|p430|||||||||
3452|Candelo Supersuite|68592|6|Mentioned|p24|Early Devonian|Early Devonian|||||||
3452|Candelo Supersuite|69564|5|Briefly described|p3, p5|||Chappell et al. (1988); Chappell et al. (1991). Lachlan Orogen. Extends from near Wangarabell (Vic) to Lower Boro (NSW).|||Braidwood Suite.|||
3452|Candelo Supersuite|69801|6|Mentioned|p129|||Eastern Lachlan Orogen.|||Includes the Yurammie Granite.|||
3452|Candelo Supersuite|71069|6|Mentioned|p43|Early Devonian|Early Devonian|||||Intrudes the Bungonia and Bindook Groups.||
3452|Candelo Supersuite|71700|2|Defined|vi, CD|Early Devonian|Early Devonian|Named for the village of Candelo after which the type pluton, the Candelo Tonalite (Lewis et al. 1994) is named. See the Braidwood Suite for geomorphic expression, outcrop, lithology, structure, metamorphism and relationships. Distribution, geochemistry, geophysical characteristics, distinguishing features, economic geology and geological hazards are discussed. Age is derived from SHRIMP U-Pb zircon dates for Braidwood Granodiorite of the constituent Braidwood Suite.|||Includes the Braidwood Suite, Belowra Suite, Candelo Suite, Hopping Joe Suite, Jinden Suite, Nungatta Suite and Watch Box Suite.|||
3461|Cann Mountain Granodiorite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Biotite-minor hornblende granite: moderately magnetic (115-130n T). High K, low Th and U.||||||06-OCT-04
3461|Cann Mountain Granodiorite|23309|6|Mentioned|p427 App 1|||G25||||||
3461|Cann Mountain Granodiorite|41850|6|Mentioned|p428|||||||||
3461|Cann Mountain Granodiorite|42827|6|Mentioned|p428|||of Glenbog Suite||||||
3461|Cann Mountain Granodiorite|68116|5|Briefly described|Appendix, Map 37.|Early Devonian|Llandovery||||||Biotite - minor hornblende granite: pale yellow grey, coarse- grained, massive; prominent quartz; chloritised mafic minerals; I-type.|
83442|Cannie pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G655.|||||Strongly magnetic (response to 300 nT)  and shows distinct layering; gravity response probably a weak low, but obsured by more regional effects.|
83442|Cannie pluton|73505|5|Briefly described|p18, p21|||Newly named unit in Swan Hill and parts of Balranald and Deniliquin 1:250 000 map areas, (G655). Named after Cannie Parish. A 5 by 14 km wide intrusion about 5 km west of Quambatook, on eastern edge of Lalbert Batholith. Strongly magnetic (responses to 300 nT) and shows distinct layering. Probably a weak low gravity response, obscurred by regional effects.|||||Granite.|
3485|Cape Conran Granite|23309|5|Briefly described|p102, 314, 315.|||(G42)||||||
3485|Cape Conran Granite|24004|6|Mentioned|p281|||||||||
3485|Cape Conran Granite|24551|6|Mentioned|p49|||||||||
3485|Cape Conran Granite|41232|4|Described|p4|||||||||
3485|Cape Conran Granite|41321|6|Mentioned|p229|||||||||
3485|Cape Conran Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
3485|Cape Conran Granite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|I-type. Well foliated (pervasive S-C fabric) coarse grained, muscovite, biotite (hornblende) granite.||||||22-OCT-04
3485|Cape Conran Granite|43315|5|Briefly described|Map Legend||Wenlock|I-type granite. Well foliated, coarse-grained muscovite, biotite (hornblende) granite.||||||03-MAY-05
3485|Cape Conran Granite|60541|4|Described|p33, p74|||Intrusive within the Kuark Metamorphic Complex.  Composed of gneissic recrystallised aggregate of quartz, plagioclase, K-feldspar, muscovite and biotite with accessory zircon and torumaline.  Intrudes Pinnak Sst to the east.  See also Cape Conran granite.||||||
3485|Cape Conran Granite|65716|5|Briefly described|p25-31|Eifelian|Emsian|From Murrungowar and part of Conran 1:50k sheets. Syn-shearing granite. SHRIMP zircon U-Pb magmatic age of 397.8 +/- 2.8 Ma. Age constrains shearing in Pheasant Creek Shear Zone.||||||
3485|Cape Conran Granite|68116|5|Briefly described|Appendix.|Devonian|Silurian||||||Granite: composition variable; muscovite, biotite-(hornblende); coarse-grained; mylonitic; I-type.|
3535|Cape Woolamai Granite|23263|5|Briefly described|Fig13-2.1p312, 313-4||Late Devonian|||||||
3535|Cape Woolamai Granite|35278|5|Briefly described|p355|||||||||
3535|Cape Woolamai Granite|61186|5|Briefly described|p52|||Dimension stone found at southeastern end of Phillip Island. Coarse- to medium-grained, salmon-pink in colour with no xenoliths. ||||||
35501|Carapooee Granodiorite|23164|4|Described|p19|Early Devonian|Early Devonian|||||||
35501|Carapooee Granodiorite|23165|5|Briefly described|Map legend||Devonian|||||||
35501|Carapooee Granodiorite|23167|5|Briefly described|Map legend||Devonian|of Mount Cole Suite. G356. Mafic biotite granodiorite to syenogranite; pale grey to pink, fine-medium grained with porphyritic texture and large phenocrysts of plagioclase.||||||27-OCT-04
35501|Carapooee Granodiorite|23168|5|Briefly described|Map legend||Devonian|of Mount Cole Suite.||||||
35501|Carapooee Granodiorite|23169|5|Briefly described|Map legend||Devonian|of Mount Cole Suite.||||||
35501|Carapooee Granodiorite|23309|6|Mentioned|p232|||G356. Supersedes Carapooee Granite.||||||
35501|Carapooee Granodiorite|66002|5|Briefly described|p7 Tb.5|||Of Mount Cole Suite. G356. Includes Dalgenon Granite of Krokowski de Vickerod et al. (1997)||||||
35501|Carapooee Granodiorite|66769|6|Mentioned|p127 Fig.8b, p129 Fig.9|||Stawell Zone. Appears as Carapooee Granite in Fig.8.||||||
35501|Carapooee Granodiorite|68116|5|Briefly described|Appendix, Map 23.|Early Devonian|Early Devonian||||||Biotite granodiorite: variable texture and composition from medium grained granite to porphyritic granodiorite with large anhedral to subhedral weakly perthitic K-feldspar grains ~10 mm across.|
3573|Carawa Cobble Conglomerate|33020|5|Briefly described|p241|||Depositional characteristics||||||
3600|Cardinia Sand|31510|5|Briefly described|p25|||See also Table 1||||||
3600|Cardinia Sand|32002|6|Mentioned|p115|||||||||
3600|Cardinia Sand|35290|6|Mentioned|p48|||||||||
3618|Carisbrook tillite|39967|5|Briefly described|p37|||Variation of Carisbrooke?||||||
76936|Carrajung Volcanic Group|66244|5|Briefly described|p6.|Eocene|Paleocene|Formerly Carrajung Volcanics (Roberts 1981). Most flows are reversely magnetised. Apparently continuous in outcrop and magnetic data with Thorpdale Volcanic Group to the west, but has older K-Ar ages; their boundary is arbitrary.||||||
76936|Carrajung Volcanic Group|68116|5|Briefly described|Appendix, Maps 52, 57.|Ypresian|Thanetian||||||Basalt, tuff, siltstone, claystone: titanaugite basalt coarse-grained; olivine basalt fine-grained porphyritic; tuff weathered; bedded to cross-bedded.|
38035|Carrara Marble|24312|6|Mentioned|p1084|||||||||
34872|Carriage Range Ignimbrite|22968|4|Described|Fig49 P92, P140||Early Devonian|Lowest unit in the Avonmore Subgroup, type section location given of p141, parent is Avonmore Subgroup, overlying unit is Tin Pot Ignimbrite, underlying unit is Attunga Paringa Formation, maximum thickness is 80m||||||
34872|Carriage Range Ignimbrite|23021|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is the Snowy River Volcanics||||||
34872|Carriage Range Ignimbrite|23309|4|Described|p113 Table 2.40|||Of the Avonmore Subgroup.  Maximum thickness: ~80m.||||||22-FEB-10
34872|Carriage Range Ignimbrite|24551|5|Briefly described|p145, p139 Fig. 5.30|Early Devonian|Early Devonian|Of Avonmore Subgroup.||||||
34872|Carriage Range Ignimbrite|68116|5|Briefly described|Appendix, Map 35.|Pragian|Lochkovian||||||Quartz ignimbrite: range from coarse-grained with very high phenocryst content to finer, less crystal-rich rocks; high cognate lithic content gives rock a clastic appearance.|
33129|Carrigeen Granodiorite|23309|6|Mentioned|p335.|||(G414)||||||
33129|Carrigeen Granodiorite|23319|4|Described|p408 Fig. 1,  p412|Ordovician|Cambrian|Age: 487+/-6Ma (K-Ar, muscovite).||||||07-FEB-07
33129|Carrigeen Granodiorite|23991|5|Briefly described|p196|||||||||
33129|Carrigeen Granodiorite|24551|5|Briefly described|p77|||Of the Glenelg River Complex||||||
33129|Carrigeen Granodiorite|50154|2|Defined|p94, p247 App.5|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex||||||15-SEP-04
33129|Carrigeen Granodiorite|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Muscovite-biotite granodiorite; S-type||||||
33129|Carrigeen Granodiorite|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granodiorite.||||||20-AUG-04
33129|Carrigeen Granodiorite|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granodiorite.||||||20-AUG-04
33129|Carrigeen Granodiorite|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granodiorite.||||||20-AUG-04
33129|Carrigeen Granodiorite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granodiorite.||||||20-AUG-04
33129|Carrigeen Granodiorite|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granodiorite.||||||20-AUG-04
33129|Carrigeen Granodiorite|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granodiorite.||||||20-AUG-04
33129|Carrigeen Granodiorite|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granodiorite.||||||20-AUG-04
33129|Carrigeen Granodiorite|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granodiorite.||||||20-AUG-04
33129|Carrigeen Granodiorite|66002|6|Mentioned|p8 Tb.5|||G414. Defined by Kemp and Gray 1999.||||||
33129|Carrigeen Granodiorite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Muscovite-biotite granodiorite: massive to foliated, bluish-white, medium grained, equigranular; local accessory garnet; metasedimentary enclaves, microcline megacrysts and schlieric foliation become more abundant toward the periphery.|
37531|Carrolls Amphibolite|23309|5|Briefly described|p30, 64, 227|||Of Moornambool Metamorphic Complex.||||||
37531|Carrolls Amphibolite|24551|5|Briefly described|p82|||||||||
37531|Carrolls Amphibolite|60451|4|Described|p52, 63, 66, 111-113.|||Of the Moornambool Metamorphic Complex. Type section in text. Maximum Thickness: ~400m. Detailed lithology and mineralogy in text. Amphibolite grade rocks.||||||
37531|Carrolls Amphibolite|60454|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Hornblende-quartz-feldspar (+/-garnet+/-epidote+/-calc-silicate) schist; minor greenschist; mylonitic in places.||||||
37531|Carrolls Amphibolite|60456|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Hornblende-quartz-feldspar (+/-garnet+/-epidote+/-calc-silicate) schist; minor greenschist; mylonitic in places.||||||
37531|Carrolls Amphibolite|60457|5|Briefly described|Map Legend|Early Devonian|Silurian|Hornblende-quartz-feldspar (+/-garnet+/-epidote+/-calc-silicate) schist; minor greenschist; mylonitic in places; plagioclase phenocrysts, amygdales.||||||
37531|Carrolls Amphibolite|60458|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Hornblende-quartz-feldspar (+/-garnet+/-epidote+/-calc-silcate) schist; minor greenschist; mylonitic in places.||||||28-SEP-04
37531|Carrolls Amphibolite|60459|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Hornblende-quartz-feldspar (+/-garnet+/-epidote+/-calc-silicate) mafic and ultramafic schist; amphibolite grade.||||||
37531|Carrolls Amphibolite|61187|5|Briefly described|p82, p83 Fig.1, p84 Fig.2.|||Stawell Zone. Brought to the surface along the Moyston Fault. Interpreted to be a higher grade rock than its precursor, the Magdala Metabasalt. Has a distinctive low-K radiometric response. Especially magnetic where contact metamorphosed by Stawell and Ararat Granites. Susceptibility measures given.||||Is intercalated with Lexington Schist. Is intruded and contact metamorphosed by Stawell and Ararat Granites.|Basic tholeiitic lavas.|
37531|Carrolls Amphibolite|61752|5|Briefly described|p6 Fig. 2|Cambrian|Cambrian|||||||07-FEB-11
37531|Carrolls Amphibolite|66002|5|Briefly described|p5 Tb.2|Cambrian|Cambrian|Of Moornambool Metamorphic Complex. Defined by Cayley and Taylor 2001.||||||
37531|Carrolls Amphibolite|66769|5|Briefly described|116|Cambrian|Cambrian|Stawell zone. Unit in Moornambool Metamorphic Complex. Also spelt Carrols, same page. Altered, sheared amphibolite: hornblende, almandine garnet, fibrous quartz. Thrust over Glenthompson Sandstone.||||||
37531|Carrolls Amphibolite|68116|5|Briefly described|Appendix p3, Map 30.|Late Cambrian|Late Cambrian|Moderately to highly magnetic within Devonian contact aureoles. From Magdala Volcanics precursor.|||||Hornblende-quartz-feldspar (+/-garnet+/-epidote+/-calc-silicate) schist; minor greenschist; mylonitic; plagioclase phenocrysts, amygdales, and thin layers of plagioclase, diopside, garnet, quartz-calcareous layers within the basaltic protolith.|14-NOV-16
37531|Carrolls Amphibolite|71593|5|Briefly described|p36|||||Moornambool Metamorphic Complex||||
37531|Carrolls Amphibolite|72445|5|Briefly described|App.1; App.2.|||App.2 is a .csv format file.||Moornambool Metamorphic Complex|||Includes foliated and deformed amphibolite. More intensely veined and deformed from 209m in Stavely 01.|
69407|Carruno Tonalite|61160|3|Fully described|p75, p58-59 Fig. 6.8.|Early Devonian|Early Devonian|See also Carruno Granodiorite, names used interchangeably. Of Falls Creek Suite. I-type. Medium-grained, equigranular biotite tonalite with no foliation. Intrudes Cobungra Granite and migmatite, gneiss and biotite granodiorite of Omeo Metamorphic Complex.||||||
69407|Carruno Tonalite|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Falls Creek Suite. Biotite tonalite: grey; medium grained; equigranular; I-type intrusion. GSV map code: G164.||||||
69407|Carruno Tonalite|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Falls Creek Suite. Biotite tonalite: grey; medium grained; equigranular; I-type intrusion. GSV map code: G164.||||||
69407|Carruno Tonalite|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Falls Creek Suite. Biotite tonalite: grey; medium grained; equigranular; I-type intrusion. GSV map code: G164.||||||
69407|Carruno Tonalite|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Falls Creek Suite. Biotite tonalite: grey; medium grained; equigranular; I-type intrusion. GSV map code: G164.||||||07-FEB-11
69407|Carruno Tonalite|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Falls Creek Suite. Biotite tonalite: I-type; highly magnetic in S (200-500 nT), moderately magnetic in N (0-100 nT; kv = 0-600 x10^-6 cgs); slight gravity low (-420 to -430 ums^-2), very low total radiolement, K, Th and U. GSV map code: G164.||||||
69407|Carruno Tonalite|68116|5|Briefly described|Appendix, Map 27.|Early Devonian|Early Devonian||||||Biotite tonalite: grey; medium grained; equigranular; I-type.|
21462|Carson Creek Ignimbrite|23309|4|Described|p109.  Table 2.40|||Maximum Thickness: 600m.  Of the Little River Subgroup. Eqivalent to Detavica Ignimbrite.||||||
21462|Carson Creek Ignimbrite|23615|3|Fully described|p118|Early Devonian|Early Devonian|Of Little River Subgroup.  Parts of this unit originally assigned to Gelantipy Rhyodacite (Fletcher, 1963).  Subsequently described in detail by Sielecki (1980) but not formally named.  Age: Early Devonian ~410-395Ma. Approx. 600m at type section.||||||16-AUG-18
21462|Carson Creek Ignimbrite|24551|5|Briefly described|p144|||Of Little River Subgroup.||||||
21462|Carson Creek Ignimbrite|43206|5|Briefly described|map legend||Lochkovian|of Little River Subgroup.||||||
21462|Carson Creek Ignimbrite|43312|5|Briefly described|Map Legend||Early Devonian|of Little River Group.||||||
21462|Carson Creek Ignimbrite|43313|5|Briefly described|Map Legend||Early Devonian|of Little River Group||||||
21462|Carson Creek Ignimbrite|60542|4|Described|p60, p22 Tb. 2|Devonian|Devonian|Of Little River Subgroup. Feldspar ignimbrite with minor interbedded sediments; phenocrysts and coarse-grained with a feldspar:quartz ratio of ~5:1. Conformably overlain by Fairy Sandstone. Max. thickness: 600m.||||||
21462|Carson Creek Ignimbrite|63594|5|Briefly described|p1032 Fig. 1|||Of the Snowy River Volcanics.||||||
21462|Carson Creek Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Feldspar ignimbrite: pumiceous, commonly with well developed eutaxitic foliation, grey; thin breccia and sandstone lenses; pyroclastic and epiclastic deposits.|
37643|Case Granite|23309|6|Mentioned|p427, Appendix 1|||G513, I-type.||||||
37643|Case Granite|43312|5|Briefly described|Map Legend|Wenlock|Wenlock|G513. Leucocratic granite, medium grained, very poorly exposed and altered, I-Type.||||||
37643|Case Granite|44185|5|Briefly described|Map legend.|Middle Devonian|Middle Devonian|I-type.||||||
37643|Case Granite|60542|4|Described|p96, p19 Fig. 3|Late Silurian|Late Silurian|Deeply weathered and covered by thick residual soil. Strongly altered and fractured, producing a blotchy green/pink appearance; consists of interlocking aggregate of plagioclase, quartz and K-feldspar.||||||30-MAY-14
37643|Case Granite|68116|5|Briefly described|Appendix, Map 45.|Middle Devonian|Middle Devonian||||||Leucocratic granite: medium-grained, very poorly exposed and altered; I-type.|
3744|Casterton Formation|12781|6|Mentioned|p385-386, 402|Early Cretaceous|Jurassic|Penola Trough, W Otway Basin. A thin (up to 60m) and ""rather enigmatic"" unit, difficult to correlate seismically or stratigraphically.||||Unconformably overlies Kanmantoo Group (basement). Is overlain unconformably by Pretty Hill Formation (Crayfish Group).||
3744|Casterton Formation|22674|4|Described|p718, Fig.2 p719|Early Cretaceous|Late Jurassic|||||||
3744|Casterton Formation|22686|6|Mentioned|Fig3p745|Berriasian|Tithonian| Geological Province: Otway Basin.||||||17-JAN-06
3744|Casterton Formation|22875|3|Fully described|p31|Early Cretaceous|Early Cretaceous|Otway Group.||||||22-DEC-08
3744|Casterton Formation|22930|6|Mentioned|50|||||||||
3744|Casterton Formation|23356|5|Briefly described|26 Tab.2|Early Cretaceous|Late Jurassic|||||||
3744|Casterton Formation|23427|6|Mentioned|Table 11.2 p418.|||Possibly informal.||||||
3744|Casterton Formation|23911|4|Described|p95 Fig. 9B|Tithonian|Tithonian|Geological Province: Otway Basin.  Overlying Unit: Crayfish Subgroup. Of the Otway Group.||||||
3744|Casterton Formation|24164|6|Mentioned|p16|Jurassic|Jurassic|Near Otway Basin (western Victoria) age typically about 160 Ma (Mitchell et al. 1997)|||||Basalt|
3744|Casterton Formation|24209|5|Briefly described|p152|Berriasian|Late Jurassic|Geological Province: Penola Trough (Otway Basin).||||||
3744|Casterton Formation|24314|5|Briefly described|p61 Fig.2|Late Jurassic|Late Jurassic|Geological Province: Otway Basin. Max. Thickness ?500m.||||||30-NOV-04
3744|Casterton Formation|24323|5|Briefly described|p135|Late Jurassic|Late Jurassic|Geological Province: Otway Basin||||||
3744|Casterton Formation|24453|4|Described|p808, p809 Fig.2|Early Cretaceous|Late Jurrasic|Fluvial sandstones, conglomerates and minor siltstones, coals, tuffs and basalt. Of Otway Group. Geological Province: Otway Basin.||||||27-JUN-14
3744|Casterton Formation|24551|5|Briefly described|p240, Fig. 9.2, 241|Early Cretaceous|Late Jurassic|Maximum Thickness: 230m.  Of the Otway Group.||||||
3744|Casterton Formation|24562|5|Briefly described|p8 Fig. 2|Berriasian|Late Jurassic|Of the Otway Supergroup.  Geological Province: Otway Basin.||||||
3744|Casterton Formation|41726|5|Briefly described|p420|||||||||
3744|Casterton Formation|42153|5|Briefly described|p352|||See also Fig.2||||||
3744|Casterton Formation|42361|6|Mentioned|p4|||Used 1989, but Casterton beds preferred herein.||||||
3744|Casterton Formation|43171|5|Briefly described|2-8|Tithonian|Kimmeridgian|)f Otway Supergroup. Age: 150Ma.||||||22-DEC-08
3744|Casterton Formation|43195|5|Briefly described|Map Legend||Late Jurassic|See also commentary on back of map.||||||
3744|Casterton Formation|43208|5|Briefly described|map legend|Berriasian|Oxfordian|Of Otway Group.||||||
3744|Casterton Formation|43219|5|Briefly described|Fig.3,p6.|Tithonian|Oxfordian|Of Otway Group.||||||22-DEC-08
3744|Casterton Formation|43590|4|Described|p7|Early Cretaceous|Late Jurassic|||||||
3744|Casterton Formation|43744|6|Mentioned|Fig.3,p3|||||||||
3744|Casterton Formation|43937|5|Briefly described|Map Legend|Aptian|Kimmeridgian|||||||
3744|Casterton Formation|44133|5|Briefly described|p142, 94 Fig. 9.2|Cretaceous|Jurassic|Geological Province: Otway Basin. Previosly recorded as 'Unit T', 'Basal Unit', 'Casterton Group undifferentiated'.||||||
3744|Casterton Formation|50154|5|Briefly described|p123, p131||Jurassic|Geological Province: Otway Basin. Age: ~150 Ma. Units that have been described range from Jurassic well into the Early Cretaceous. In need of revision due to uncertain age and status.||||||
3744|Casterton Formation|60126|4|Described|p4-8|Valanginian|Valanginian|Predominantly composed of carbonaceous shales with minor interbedded sltst. sst, volcaniclastics, basalt flows.  Age based on spore-pollen content of samples from Sawpit-1 well, incl. Gagiella mutabilis, a dinoflagellate which occurs precisely in this era||||||
3744|Casterton Formation|61017|5|Briefly described|p5 Fig. 2, p6|Tithonian|Callovian|Of the Otway Group. Non-marine lacustrine to fluvial sediments, with potential as excellent source rocks for hydrocarbons. Geological Province: Otway Basin.||||||07-FEB-11
3744|Casterton Formation|61182|3|Fully described|p11, p82-83|||Formerly Casterton Beds. Base of the Otway Group. Unconformably overlain by Pretty Hill Formation. Basalt with minor pyroclastics and sediments. Max. thickness: 536m. Geological Province: Otway Basin.||||||
3744|Casterton Formation|61470|5|Briefly described|p28 Fig. 5|Tithonian|Callovian|Of the Otway Group. Geological Province: Otway Basin.||||||
3744|Casterton Formation|61528|5|Briefly described|p819|Berriasian|Kimmeridgian|Overlain by Crayfish Group rocks or Eumeralla Formation. Age: ~146-134 Ma. Max. thickness: >1000m. Geological Province: Otway Basin.||||||
3744|Casterton Formation|61547|6|Mentioned|p461. |Berriasian|Kimmeridgian|Lacustrine sediments; the initial sediments in the Penola Trough. ||||Is overlain by Pretty Hill Formation.||
3744|Casterton Formation|61622|4|Described|p436, p436 Fig. 2, p438 Fig. 4|Early Cretaceous|Late Jurrasic|Of Crayfish Group. Thickness: 60 to 500m.  Geological Province: Otway Basin. Lacustrine carbonaceous mudstones, sandstones and minor coals and volcaniclastics.||||||07-FEB-11
3744|Casterton Formation|61623|6|Mentioned|p447, p449 Fig. 4|Late Jurassic|Late Jurassic|Geological Province: Otway Basin.||||||07-APR-09
3744|Casterton Formation|61626|5|Briefly described|p486 Fig. 2|Jurassic|Jurassic|Of Otway Group. Geological Province: Otway Basin.||||||07-APR-09
3744|Casterton Formation|61627|5|Briefly described|p500 Fig. 2|Late Jurassic|Late Jurassic|Includes Pretty Hill and Laria Formations, Katnooke Sandstone. Geological Province: Otway Basin.||||||07-FEB-11
3744|Casterton Formation|61628|5|Briefly described|p509 Fig. 3|Early Cretaceous|Jurassic|Of Otway Group. Geological Province: Otway Basin.||||||07-APR-09
3744|Casterton Formation|63122|5|Briefly described|p17 Fig. 4.3|Late Jurassic|Late Jurassic|Max. thickness: 60m. Geological Province: Otway Basin.||||||13-DEC-07
3744|Casterton Formation|63124|5|Briefly described|p55-57, p48 Fig. 5.1, p49 Fig. 5.2|Early Cretaceous|Late Jurassic|Originally Casterton Beds, then C.Formation, C.Beds, C.Group, C.beds; now established as Casterton Fm. Unconformable below Crayfish Group; unconformably overlain by Pretty Hill Formation. Age: 150-142Ma. Max.thick: 500m. Geol.Prov:Otway Basin.See also p55||||||
3744|Casterton Formation|63125|5|Briefly described|p104, p116 Tb. 7.6|||Overlain by Pretty Hill Formation. Geological Province: Otway Basin||||||
3744|Casterton Formation|63130|5|Briefly described|p141|||Geological Province: Otway Basin.||||||31-JAN-08
3744|Casterton Formation|63150|5|Briefly described|p95|||Plant microfossils are abundant in claystone and coal, and only absent in any sandstone sections. Geological province: Otway Basin.||||||
3744|Casterton Formation|63267|5|Briefly described|p485 Fig.2, p486 Fig.3, p489-492, p497|Early Cretaceous|Late Jurassic|Penola Trough, Otway Basin. Lacustrine-fluvial deposits. Hydrocarbon source potential (elaborated).||||Is overlain unconformably by Pretty Hill Formation.||
3744|Casterton Formation|63269|5|Briefly described|p603-606, p616, p618, p622, p624|Early Cretaceous|Early Cretaceous|Otway Basin. Lacustrine deposits. Became overmature for gas generation from Late Cretaceous onwards. Details of oils and oil stains in named wells tabulated. Oil-source correlation. Biomarker diagram.||Otway Group.||Is overlain unconformably by Pretty Hill Formation.|Mainly carbonaceous shales, with minor interbedded volcanics and sandstone.|
3744|Casterton Formation|63431|5|Briefly described|p676, p677 Fig. 2|Late Jurassic|Late Jurassic|Overlain by Crayfish Group. Lacustrine. Geological Province: Penola Trough/Otway Basin. See also p680.||||||07-FEB-11
3744|Casterton Formation|64570|5|Briefly described|p852|Middle Jurassic|Middle Jurassic|Age: 170-160Ma (K-Ar). Geological Province: Otway Basin. Basaltic lavas.||||||22-DEC-08
3744|Casterton Formation|66245|5|Briefly described|p6 Fig.5, p42.|Berriasian|Kimmeridgian|Oldest sediments in the Otway Basin: locally-derived sands, and muds from a more distant source, deposited in locally deep lakes that eventually formed a through-going rift.||Basal unit in Otway Group.|||Fluvial sandstones, floodplain and lacustrine claystones; some coals.|
3744|Casterton Formation|67367|5|Briefly described|p131 Fig.2, pp131-132.|Late Jurassic|Middle Jurassic|Fluvio-lacustrine shales. Hydrocarbon source rock. Assigned to the Austral 1 petroleum sub-system.||Unit in Otway Group.|||Interbedded carbonaceous mudstones.|
3744|Casterton Formation|68135|5|Briefly described|p52 fig 2b |Early Cretaceous|Kimmeridgian|South Australian margin and Tasmania. Plant macrofossils present.|||||Interbedded siltstone and sandstone.|14-SEP-17
3744|Casterton Formation|68189|5|Briefly described|p19 Fig.8, p25|Jurassic|Jurassic|Upper Jurassic age.||Of the Otway Group.|||Comprises basalt and mafic volcaniclastic material.|
3744|Casterton Formation|69297|5|Briefly described|p79, p98-p100, p104, p400|Valanginian|Valanginian|Torquay Sub-basin, Otway Basin.  Deposited in a fluvio-lacustrine environment. Interpreted to be thermally overmature for oil and gas generation.  ||Crayfish Subgroup||Overlain by the Sawpit Shale and Sawpit Sandstone. |Mudstone and shale. |
3744|Casterton Formation|69651|5|Briefly described|p10, p50|Early Cretaceous|Late Jurassic|Fluvio-lacustrine deposits.||Otway Group.||Is overlain unconformably by Pretty Hill Formation (Crayfish Subgroup).|Shales.|
3744|Casterton Formation|70077|5|Briefly described|Nelson:Fig.2. Regional:Fig.4;p4,p6-7,p9|Early Cretaceous|Early Cretaceous|Otway Basin: Port Campbell Embayment and Robe-Penola Trough. Source rocks of the Austral 1 Petroleum System.||Otway Group.||Is overlain by Pretty Hill Formation or Sawpit Shale/Sawpit Sandstone.|Lacustrine sediments and interbedded flow basalts.|
3744|Casterton Formation|70379|5|Briefly described|p717, p719, p721, p724-732|Early Cretaceous|Early Cretaceous|Central Otway Basin. Distribution was restricted to rapidly subsiding, structurally controlled depocentres in the W of the Basin. Isopach map. Relationship of tectonic activity to sediment accumulation discussed in detail. Berriasian to early Valanginian.|c. 152-139 Ma.|Crayfish Group.||Is overlain by Sawpit Shale (equivalent) and McEachern Sandstone.|Volcaniclastic and lacustrine deposits.|
3744|Casterton Formation|70880|6|Mentioned|p77|Berriasian|Tithonian|Otway Basin.||||||
3744|Casterton Formation|71266|6|Mentioned|p614 Fig.3|Berriasian|Tithonian|Otway Basin.||||||
3744|Casterton Formation|73356|5|Briefly described|p. 1-2, 4-6, 8-11, 13-16, 19-21,24-27,29|Berriasian|Tithonian|Otway Basin. Upper boundary is unconformable in many instances (cf. Warrong Trough) but is shown to be conformable in the Sawpit-1 well (Penola Trough).||Otway Group||Overlain by Sawpit Formation (conformably), including McEachern Member (disconformably), and Pretty Hill Formation (unconformably) (all of Crayfish Subgroup).||
3744|Casterton Formation|73357|5|Briefly described|p15-16, p45, p47|Berriasian|Berriasian|Otway Basin. Sparse, poorly preserved palynomorph assemblages, or barren of palynomorphs. Assigned to the Ruffordiaspora australiensis Spore-Pollen Zone, wholly terrestrial palynofloras with common fern spores and moderately frequent freshwater algae. May be entirely represented by R. australiensis zone.||Of Otway Group.||Underlies Pretty Hill Formation.|Contains sandy lithologies.|
3744|Casterton Formation|73383|5|Briefly described|p3, p7-8, p11-12, p15, p27, p38, p45|Berriasian|Tithonian|Otway Basin. Approximately equivalent to chemostratigraphic Sequence S0, subdivided into five packages. Defined by high Nb values (generally 20 ppm and above), mixed terrigenous clastic and alkaline volcanic composition. Likely includes coal in parts, and some intervals have high Mo and S concentrations interpreted as deposition in anoxic conditions or in a marine environment/marine incursion. Lithologies based on geochemistry using the ChemLith classification includes calcareous and argillaceous sandstones, limestone, calcareous limestone and igneous rock; and using the Herron classification (1988) includes shale, Fe-shale, Fe-sand, lith-arenite and wacke. See also iii, vi, p55-58, p65-66, p103-106, p112-117, p167, p176, p187-190, p198, p233-236, p241-246, p295, p322, p342-343.||Otway Group||Unconformably underlies Pretty Hill Formation, Crayfish Subgroup|Lacustrine mudstones and alluvial sandstones with initial basaltic volcanics.|
3744|Casterton Formation|73385|5|Briefly described|p3, p5|Berriasian|Tithonian|Otway Basin. Deposited in predominantly NW-SE grabens and half-grabens of limited extent, deposition facilited by a series of lakes within individual depocentres, that became linked to an active fluvio-lacustrine system.||Otway Group||Underlies Pretty Hill Formation.|Lacustrine mudstones and alluvial sandstones with initial basaltic volcanics. Primarily comprised of locally derived sands and far-sourced muds.|
3744|Casterton Formation|73386|4|Described|p2, p4, p6-8, Attachment A1|Berriasian|Tithonian|Otway Basin. Oldest sedimentary unit in basin, unconformably overlies Paleozoic basement. Deposited in half graben structures, distribution restricted to Early Cretaceous depocentres. Conformably underlies Crayfish Subgroup and Sawpit Formation in the western Victorian Otway Basin, unconformable in the central basin. Type section defined between 2220 m and 2450 m in Casterton-1 (Morton et al., 1994). Basalt and tuff deposits dominant in the central Otway Basin, carbonaceous facies are more common in the west. Belongs to the Retriletes watherooensis Spore-Pollen Zone and Lower Ruffordiaspora australiensis Spore-Pollen Subzone of Partridge (2006), corresponds to the S0 chemostratigraphic sequence of Forbes et al. (2020).||Otway Group||Underlies Crayfish Subgroup, Sawpit Formation, McEachern Member|Characterised by lacustrine shales with interbeds of sandstone and siltstone, with much of the sediment associated with basaltic volcanics, includes initial basaltic volcanics.|
3744|Casterton Formation|73594|5|Briefly described|p3-4, p8, p38, p41, p44, p49-55, p66-67|Berriasian|Tithonian|Otway Basin. Deposited in isolated freshwater lakes, stratigraphy is likely to be unique in each half-graben. Up to 500m thick. Restricted to the area west of Warrnambool. See also p45 Fig.5.19, p59.||Otway Group||Underlies Pretty Hill Formation, Crayfish Subgroup|Carbonaceous shales, coals, siltstones and sandstones with minor basalt and trachyte.|
80012|Casterton Volcanics|69297|6|Mentioned|p79|Oxfordian|Bajocian|Otway Basin. Shown as Coleraine and Casterton - 1 Volcanics. Shown as unconformably underlying the Cretaceous Casterton Formation.||||||19-SEP-17
3760|Castleburn Granite|23309|6|Mentioned|p427 App1.|||(G142).  Same unit as Castleburn Tonalite?||||||01-OCT-08
3760|Castleburn Granite|42726|5|Briefly described|map legend|||||||||
3760|Castleburn Granite|68116|5|Briefly described|Appendix, Map 44.|Devonian|Silurian||||||Biotite granite: grey, medium-grained, equigranular, massive.|
36202|Castlemaine Group|12100|5|Briefly described|p819|Middle Ordovician|Early Ordovician|Upward fining succession with an upward decrease in lithic content; 2-3 km thick; took approximately 30 million years to be deposited.||||||08-MAY-12
36202|Castlemaine Group|23300|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
36202|Castlemaine Group|23302|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
36202|Castlemaine Group|23303|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
36202|Castlemaine Group|23304|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
36202|Castlemaine Group|23305|3|Fully described|p39|Chewtonian|Lancefieldian|Probably a misspelling of Castlemaine Supergroup, but spelling is consistent within this publication. Cas & Vanden Berg (1988). Underlying unit St Arnaud Group. Geological Province: Lachlan Fold Belt. Max. thickness: 6000 m.||||||03-FEB-09
36202|Castlemaine Group|23309|4|Described|p49, 51-58, 155, 241, 242, 258|||||||||22-FEB-10
36202|Castlemaine Group|23814|5|Briefly described|p746 Fig. 5|Early Ordovician|Early Ordovician|||||||
36202|Castlemaine Group|24002|5|Briefly described|p244 Fig.1|Ordovician|Ordovician|||||||
36202|Castlemaine Group|24004|5|Briefly described|p277|||||||||
36202|Castlemaine Group|24037|6|Mentioned|p423|||Geological Province: Lachlan Fold Belt.||||||21-OCT-08
36202|Castlemaine Group|24098|5|Briefly described|p27 Fig. 2|Late Ordovician|Early Ordovician|Geological Province: Lachlan Fold Belt. See also Castlemaine Group.||||||
36202|Castlemaine Group|24103|5|Briefly described|p137|Ordovician|Ordovician|||||||
36202|Castlemaine Group|24104|5|Briefly described|p151|Ordovician|Ordovician|Overlying unit: White Hills Gravel.||||||
36202|Castlemaine Group|24134|5|Briefly described|p7|Middle Ordovician|Early Ordovician|||||||
36202|Castlemaine Group|24177|4|Described|p45, p84|Middle Ordovician|Early Ordovician|Overlies Knowsley East Shale. Geological Province: Bendigo Zone. Can be subdivided biostratigraphically using graptolites. Intruded by the Baringhup and Harcourt Granodiorites, Crosbie Granite and Commissioners Flat Diorite.||||||11-MAY-04
36202|Castlemaine Group|24178|5|Briefly described|p15 Fig.2, p18|Ordovician|Ordovician|Age: 490 - 450Ma.||||||21-OCT-08
36202|Castlemaine Group|24180|5|Briefly described|Map Legend|Ordovician|Ordovician|Deep marine deposits; sandstones, siltstones, mudstones and black shales; dominantly sand-rich turbidite facies.||||||09-MAY-13
36202|Castlemaine Group|24276|4|Described|p1723|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt. Max. thickness: 2000 m.||||||
36202|Castlemaine Group|24326|5|Briefly described|Map legend|Ordovician|Ordovician|||||||
36202|Castlemaine Group|24328|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|||||||
36202|Castlemaine Group|24329|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|||||||
36202|Castlemaine Group|24383|4|Described|p7, 15, 58|Ordovician|Ordovician|Overlying Unit: Calivil Formation (unconformable). Max Thickness: 3700m. Geological Province: Lachlan Fold Belt.||||||03-FEB-09
36202|Castlemaine Group|24384|5|Briefly described|Map legend|Middle Ordovician|Early Ordovician|Sandstone, slate; moderately to well sorted, variably rounded quartz with minor feldspar and lithic grains in quartz silt or clay matrix; minor quartz granule conglomerate; thin to very thick bedded; black fossiliferous shales.||||||25-JUN-13
36202|Castlemaine Group|24385|5|Briefly described|Map legend|Middle Devonian|Early Devonian|||||||
36202|Castlemaine Group|24386|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Sandstone, slate; moderately to well sorted, variably rounded quartz with minor feldspar and lithic grains in quartz silt or clay matrix; minor quartz granule conglomerate, thin to very thickly bedded; black fossiliferous shale.||||||
36202|Castlemaine Group|24387|5|Briefly described|Map legend|Middle Ordovician|Early Ordovician|Sandstone, slate; moderately to well sorted, variably rounded quartz with minor feldspar and lithic grains in quartz silt or clay matrix; minor quartz granule conglomerate; thin to very thickly bedded; black fossiliferous shales.||||||
36202|Castlemaine Group|24388|5|Briefly described|Map legend|Ordovician|Ordovician|Sandstone, slate; non-weakly magnetic; moderate-high K, low-moderate Th, U and total radioelements; moderately high magnetic response.||||||03-FEB-09
36202|Castlemaine Group|24438|5|Briefly described|p4, p20|Early Ordovician|Early Ordovician|Bendigo Zone of Lachlan Fold Belt|||||deep marine turbidites|
36202|Castlemaine Group|24439|4|Described|p28, p9 Fig. 3|Ordovician|Ordovician|See also p8, p7 Fig. 2.  Geological Province: Lachlan Fold Belt.||||||
36202|Castlemaine Group|24440|5|Briefly described|Map legend|||||||||
36202|Castlemaine Group|24551|3|Fully described|p99, 606|Darriwilian|Lancefieldian|Upgraded to Castlemaine Supergroup by Cas & VandenBerg (1988) but relegated to group status by VandenBerg et al (2000). Overlies Goldie Chert and Knowsley East Shale.||||||30-JAN-15
36202|Castlemaine Group|50092|5|Briefly described|p361, 362|Early Ordovician|Early Ordovician|Contains fossil conodont Oepikodus evae in a black chert and black shale interval.||||||24-FEB-05
36202|Castlemaine Group|60451|5|Briefly described|p21 Fig. 7, 23|Early Ordovician|Early Ordovician|||||||
36202|Castlemaine Group|60452|4|Described|p22|Ordovician|Ordovician|Thick sequence of quartz-rich turbidites with graptolite fauna. Graptolites are of Lancefieldian age.||||||
36202|Castlemaine Group|60461|5|Briefly described|Map legend|Lancefieldian|Lancefieldian|Overlies the Saint Arnaud Group.  Age: 490-486Ma.||||||28-SEP-04
36202|Castlemaine Group|60462|5|Briefly described|Map Legend|Lancefieldian|Lancefieldian|Marine turbiditic sandstone with minor mudstone and carbonaceous siltstone.||||||21-OCT-08
36202|Castlemaine Group|61161|6|Mentioned|p167|||Host rock of goldfields in Bendigo Zone of Central Victoria. Similarity drawn to Pinnak Sandstone, DARGO (host basement rocks in Tabberabbera Zone).||||||
36202|Castlemaine Group|61186|5|Briefly described|p98|||Castlemaine Slate occurs within bands in this group as well as in the metamorphic aureole of the Harcourt Granite - slate from the latter being harder. ||||||
36202|Castlemaine Group|61187|6|Mentioned|p4.|||||||Is conformably overlain by Sunbury Group.||
36202|Castlemaine Group|62099|5|Briefly described|p331|Middle Ordovician|Early Ordovician|Dominated by turbidites / a series of overlapping lenticular sandstone packages . Max. thickness: 5km. In the Bendigo Zone of the Lachlan Orogen. ||||||
36202|Castlemaine Group|62100|5|Briefly described|p344|Early Ordovician|Early Ordovician|Turbiditic sandstone and mudstone sequences.  Host to the vast majority of orogenic lode gold deposits in the western Lachlan Orogen. In the Bendigo Zone of Lachlan Orogen.||||||23-MAR-09
36202|Castlemaine Group|62370|6|Mentioned|p447|||||||||
36202|Castlemaine Group|62742|5|Briefly described|p699 Fig. 2|Devonian|Silurian|In the Heathcote Greenstone Belt. ||||||
36202|Castlemaine Group|62744|5|Briefly described|p709 Fig. 2|Devonian|Silurian|Geological Province: Heathcote Greenstone Belt.||||||
36202|Castlemaine Group|64312|6|Mentioned|p442, p443|||Contains turbidites. See also p443 Fig. 5. ||||||
36202|Castlemaine Group|64314|5|Briefly described|p495 Fig. 2a|Ordovician|Ordovician|||||||
36202|Castlemaine Group|64611|5|Briefly described|Map legend + Excursion Localities list|Darriwilian|Lancefieldian|Contains the Romsey Subgroup of sandstones, siltstones and shale of Lancefieldian, Bendigonian, Chewtonian, Castlemainian, Yapeenian, and Darriwilian ages.||||||03-DEC-12
36202|Castlemaine Group|64612|2|Defined|p34-36, p25 Fig. 5.1, p27, p33, p42|Ordovician|Cambrian|Includes many units. Overlain by Sunbury Group. Thick: 5000m. Geological Province: Bendigo Zone. Turbidite-mudstone sequence and shows upward fining, deep marine setting.||||||09-MAY-13
36202|Castlemaine Group|64616|6|Mentioned|p343 Fig.23|||||||||
36202|Castlemaine Group|64619|5|Briefly described|Map legend|Middle Ordovician|Early Ordovician|Includes the Romsey Subgroup and Middle Ordovician undifferentiated sandstone/siltstone/shale which is sparsely fossiliferous and has origins as deep-water turbiditic fan and hemipelagic deposits.||||||
36202|Castlemaine Group|65665|6|Mentioned|p1160 Fig.14|||Turbidites.|Deposited from ca 490 - 455 Ma.|||||10-MAY-12
36202|Castlemaine Group|65715|5|Briefly described|p4 Tb.2, p5-6, p10, p12, p18, p26, 27|Ordovician|Ordovician|Includes Romsey Subgroup. Subdivided into 8 biostratigraphic units ranging in age from Darriwilian to Lancefieldian based on graptolite zones. Overlain by White Hills Gravel, Bullengarook Gravel.||||||
36202|Castlemaine Group|65719|5|Briefly described|p7|Ordovician|Ordovician|||||Overlies Heathcote Volcanic Group.||10-MAY-12
36202|Castlemaine Group|65905|5|Briefly described|p260||Ordovician|Discussion of turbidite sequence in lower and middle parts of the Group, that host gold deposits. Lithology: mudstone and sandstone, quartz-carbonate veins present in the mudstone, Bendigo Zone.||||||29-APR-11
36202|Castlemaine Group|65969|5|Briefly described|p3,p13,p17 Fig.7,p26 Fig.13,p31,p36-37|Ordovician|Ordovician|Bendigo Zone. Overlies Goldie Chert. Upwards-fining metaturbidites with decreasing lithic material. Deformed at c.445 +/- 10 Ma and again at c.415 +/- 10 Ma. Largely non-magnetic. Contains graptolites allowing very fine chronostratigraphic division.||||||
36202|Castlemaine Group|65974|6|Mentioned|p4, p6, p9, p12, p16, p19, p22, p24, p27|Ordovician|Ordovician|See also p29, p32, p35, p41, p44, p47, p49, p52, p54. It is assumed a folded and faulted Cambrian stratigraphy of approximately 5-8km underlies the Ordovician Castlemaine Group west of the Whitelaw and Drummartin faults. [This observation is repeated in every page reference].|||||Comprises a folded and faulted turbidite sequence.|07-FEB-18
36202|Castlemaine Group|66182|5|Briefly described|p319|Early Ordovician||Lachlan Fold Belt. Maximum deformation age 455-440 Ma.|||||Quartz-wacke deep marine turbidite sequence, occasional black shale units.|11-MAY-12
36202|Castlemaine Group|66769|5|Briefly described|117-120, 130, 133, 145|Early Ordovician|Early Ordovician|Bendigo Zone. Extensive, thick package (c.3000m) of turbiditic sandstone and mudstone (now slate). Bedding-parallel quartz veins. Low seismic reflectivity.||||||
36202|Castlemaine Group|67322|5|Briefly described|p13|Ordovician|Ordovician|Age and stratigraphy based on detailed graptolite zonation, allowing correlation throughout Lachlan Orogen. Also appears in the same paragraph as Castlemaine Supergroup.||||||21-FEB-18
36202|Castlemaine Group|67847|6|Mentioned|p10 fig 2.3, p14 fig 2.9|Ordovician|Ordovician|||||||
36202|Castlemaine Group|68116|5|Briefly described|Maps 16-17, 23-24, 31-32, 40-41, 50-51.|Dapingian|Tremadocian|Also occurs in the Appendix. Age written as Lancefieldian to Yapeenian in text. Contains six informal subdivisions based on age: Yapeenian, Lancefieldian, Darriwilian, Chewtonian, Castlemainian, and Bendigonian.|||||Undifferentiated: sandstone, siltstone, black shale; sparsely fossiliferous; deep marine turbidite and hemipelagic deposits.|
36202|Castlemaine Group|68189|6|Mentioned|p3, p14, p15 Fig.6, pp17-20, p33|Ordovician|Ordovician|See also Castlemaine Group"". Turbidite fan deposit. Contains graptolites.||||||
36202|Castlemaine Group|68314|5|Briefly described|p754, p756, p759||Ordovician|Cas (1983). Heathcote Greenstone Belt.|||||Quartz-rich flysch (sandstone, conglomerate and mudstone).|
36202|Castlemaine Group|68822|5|Briefly described|p324, p351, p352, p353 Fig.16|Middle Ordovician|Lower Ordovician|Bendigo Zone. Graptolite-rich. The youngest graptolite in shale is Darriwilian 3 (VandenBerg and Cooper 1992). Contains syndepositional disturbed strata, although mudstone intraclasts and scouring features are present.|||||Quartz-rich turbidites.|
36202|Castlemaine Group|68823|6|Mentioned|p406|||Middle Ordovician deformation of this unit provided detritus for Late Ordovician Sunbury Group.||||||
36202|Castlemaine Group|69002|6|Mentioned|p13|||Of the Bendigo Zone.||||||
36202|Castlemaine Group|69541|5|Briefly described|p652|Early Ordovician|Early Ordovician|Top of the Group is latest Darriwilian. There is no overlying black shale equivalent to the Bendoc Group, which overlies the Adaminaby and Wagga Groups.||||Is overlain by Sunbury Group. Possibly correlated with Girilambone Group.||
36202|Castlemaine Group|70601|5|Briefly described|p44|Bendigonian|Lancefieldian|Kilmore/Heathcote area.||||Overlies Goldie Chert.||
36202|Castlemaine Group|70629|6|Mentioned|p986|Late Ordovician|Early Ordovician|Melbourne Zone.||||||
36202|Castlemaine Group|70684|6|Mentioned|p7 Fig.1|||||||||
36202|Castlemaine Group|70718|4|Described|p38|Darriwilian|Lancefieldian|Marine turbidite deposits. Deformed and metamorphosed during the Benambran Orogeny.|490-450 Ma|||Intruded by the Pyramid Hill Granite and Lake Boga Granite.|Turbiditic sandstone, mudstone and black shale with minor granule conglomerate.|
36202|Castlemaine Group|71419|6|Mentioned|p18 Fig 19|Ordovician|Ordovician|Deep marine sedimentation. Subsequently underwent folding and faulting.||||||02-FEB-18
36202|Castlemaine Group|72445|6|Mentioned|App.7 p6 Fig.3.|Ordovician|Ordovician|Shown only on the geological map covering the Stavely Project area (from Geology of Victoria 2003: 21).||||||
36202|Castlemaine Group|73140|5|Briefly described|p495|Gisbornian|Late Cambrian|Proposed to be incorporated into a new Lachlan Supergroup.||Lachlan Supergroup|||Terrigenous turbiditic sequence.|
36202|Castlemaine Group|73177|5|Briefly described|p1113-1114|Ordovician|Ordovician|Lachlan Orogen. Bendigo Zone, western Victoria.||||||
36202|Castlemaine Group|73186|6|Mentioned|p229, Fig.2, p230, p237|Sandbian|Early Ordovician|Bendigo Zone.|||||Turbidites with lesser pelitic black shale.|
36202|Castlemaine Group|73264|6|Mentioned|p1390 Fig.12|Early Ordovician|Early Ordovician|Lachlan Orogen, Bendigo Terrane.|||||Turbidites.|
36202|Castlemaine Group|73496|5|Briefly described|Map legend|Ordovician|Ordovician||||||Sandstone, mudstone, black shale, strongly layered; deep marine turbidite. No magnetic response, or magnetic response to 5 nT with weak magnetic linear features in parts.|
36202|Castlemaine Group|73497|5|Briefly described|Map legend|Ordovician|Ordovician||||||Marine turbiditic sandstone with minor mudstone and carbonaceous siltstone: magnetic responses to less than 1 nT; or weakly magnetic responses 1 to 15 nT.|
36202|Castlemaine Group|73505|5|Briefly described|p2, p6, p14, p28|Ordovician|Ordovician|||||Overlies Dja Dja Wrung Supergroup, equivalent to Tueloga beds||
36202|Castlemaine Group|73576|5|Briefly described|p803 Fig.1, p804, p810, p811-815|Ordovician|Ordovician|||||Overlies Dja Dja Wrung Supergroup, hosts Tarnagulla Granodiorite, Moliagul Granodiorite.|Deep marine turbidite sequences. Includes hornfels.|
36202|Castlemaine Group|75072|6|Mentioned|p233, 240|||Bendigo Zone. Zircon age distribution.|474 +/- 1 Ma (Wilkinson et al., 1995).||||Metagreywacke.|
36860|Castor Oil Lava|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Snowy River Volcanics||||||
36860|Castor Oil Lava|23309|5|Briefly described|p106,113|||||||||
36860|Castor Oil Lava|24551|5|Briefly described|p142|||Not a formal stratigraphic name.||||||
36860|Castor Oil Lava|60542|4|Described|p74, p14|Early Devonian|Early Devonian|Large lava body mostly of glassy rhyolite lava but in a few places includes andesite lava and clastic rocks.||||||
36860|Castor Oil Lava|68115|5|Briefly described|p4.|Devonian|Devonian|Contains two un-named members, one mafic and one felsic. These were interchanged on the map (Hendrickx et al. 1996c) but now corrected, with the larger felsic member labelled Dspb and the smaller mafic member labelled Dspa.||Unit in Snowy River Volcanic Group.||||
36860|Castor Oil Lava|68116|5|Briefly described|Appendix, Map 45.|Pragian|Pragian||||||Rhyolite, andesite and basalt: lava dome/cryptodome.|
3787|Cathedral 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
3787|Cathedral Group|22768|6|Mentioned|p188|||||||||
3787|Cathedral Group|22857|5|Briefly described|p188|Devonian|Devonian|Non-marine unit. Unconformably overlain by Marysville Igneous Complex; underlain by Walhalla Group.||||||
3787|Cathedral Group|23229|5|Briefly described|p25-6, 31, 35|Middle Devonian|Zlichovian|||||||
3787|Cathedral Group|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
3787|Cathedral Group|23309|5|Briefly described|p147, 154  Table 2.56|Middle Devonian|Early Devonian|||||||
3787|Cathedral Group|23522|5|Briefly described|p247 Fig 3|Devonian|Early Devonian|||||||
3787|Cathedral Group|24002|5|Briefly described|p228 Fig.2|Devonian|Devonian|||||||
3787|Cathedral Group|24098|5|Briefly described|p27 Fig. 2|Middle Devonian|Middle Devonian|Of the Murrindindi Supergroup. Geological Province: Melbourne Zone, Lachlan Fold Belt.||||||19-APR-05
3787|Cathedral Group|24177|5|Briefly described|p13, p50 Fig.22, p60|Devonian|Devonian|Overlies the Walhalla Group. Geological Province: Mount Easton Province, Melbourne Trough.||||||
3787|Cathedral Group|24588|5|Briefly described|p12, 13, 15, 30, 33|Middle Devonian|Emsian|Conformably overlies Walhalla Group. Max Thickness: >2.5 km. Geological Province: Mount Easton Province. Unconformably underlies Marysville Igneous Complex.||||||29-NOV-13
3787|Cathedral Group|33238|4|Described|p642|||||||||
3787|Cathedral Group|35283|6|Mentioned|p46|||||||||
3787|Cathedral Group|40761|5|Briefly described|p234|||Mention P226||||||
3787|Cathedral Group|41585|4|Described|p115|||Mention p103, Fig 4.1.||||||06-JUN-06
3787|Cathedral Group|42827|4|Described|p115|||see also Table 4.1||||||
3787|Cathedral Group|44187|5|Briefly described|Map Legend||Middle Devonian|||||||
3787|Cathedral Group|60599|6|Mentioned|p14|Middle Devonian||Overlies Walhalla Group. ||||||
3787|Cathedral Group|61185|5|Briefly described|p14, p47, p24-25 Fig. 7, p21 Fig. 6|||Fluvial sediments. Overlies Montys Hut Formation (Walhalla Group).||||||07-FEB-11
3787|Cathedral Group|64612|6|Mentioned|p27|Middle Devonian|Early Devonian|Fluvial sandstones.||||||07-FEB-11
3787|Cathedral Group|64616|6|Mentioned|p156 Fig.6.5|Middle Devonian|Early Devonian|Overlies Walhalla Group.||||||
3787|Cathedral Group|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Walhalla. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
3787|Cathedral Group|67804|5|Briefly described|p64|Early Devonian|Early Devonian|||||Overlies Jordan and Walhalla Groups conformably.||
3787|Cathedral Group|68116|5|Briefly described|Appendix, Maps 33, 42.|Emsian|Emsian||||||Fluvial: red and green sandstone, siltstone, conglomerate.|
3787|Cathedral Group|70629|6|Mentioned|p986|Middle Devonian|Early Devonian|Melbourne Zone. Mis-spelt as Cathederal Group in Fig.1.||||||
3787|Cathedral Group|70742|5|Briefly described|p161-163|||Non-marine deposits.||Murrindindi Supergroup.||Overlies Walhalla Group. Is overlain by Marysville Igneous Complex.||
3787|Cathedral Group|71040|6|Mentioned|p26|||Youngest unit in the Melbourne Zone to be deformed by the Tabberabberan Orogeny, but it lacks fossils for dating.||||||
35645|Catherine Sandstone (VIC)|23109|6|Mentioned|p512 Fig.3|||||||||
77283|Cattleyard Granite|68115|6|Mentioned|p6.|||G701. Although it has not been observed in the field, radiometric data shows that this unit outcrops, hence it now has a formal name.||||||17-OCT-12
77283|Cattleyard Granite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Granitic rock; moderately magnetic, low K, low Th, moderate U.|
40602|Cauldron Volcanics|23309|5|Briefly described|p5 Fig 1.3|Carboniferous|Early Devonian|||||||
37235|Caupaul Igneous Complex|23991|6|Mentioned|p188|||||||||
37235|Caupaul Igneous Complex|24012|3|Fully described|p209|Ordovician|Cambrian|See also page 222 Appendix 1.||||||
37235|Caupaul Igneous Complex|24551|5|Briefly described|p76|||||||||
37235|Caupaul Igneous Complex|50154|2|Defined|p36, p81, p248 App.5|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex. Includes the Ferres Creek Tonalite and the Kooreelah Gabbro-Diorite.||||||16-MAY-13
37235|Caupaul Igneous Complex|50156|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Includes: Kooreelah Gabbro-Diorite and Ferres Creek Tonalite||||||20-AUG-04
37235|Caupaul Igneous Complex|50157|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Includes: Kooreelah Gabbro-Diorite and Ferres Creek Tonalite||||||20-AUG-04
37235|Caupaul Igneous Complex|50158|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Includes: Kooreelah Gabbro-Diorite and Ferres Creek Tonalite||||||20-AUG-04
37235|Caupaul Igneous Complex|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Includes: Kooreelah Gabbro-Diorite and Ferres Creek Tonalite||||||20-AUG-04
37235|Caupaul Igneous Complex|50160|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Includes: Kooreelah Gabbro-Diorite and Ferres Creek Tonalite||||||20-AUG-04
37235|Caupaul Igneous Complex|50161|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Includes: Kooreelah Gabbro-Diorite and Ferres Creek Tonalite||||||20-AUG-04
37235|Caupaul Igneous Complex|50162|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Includes: Kooreelah Gabbro-Diorite and Ferres Creek Tonalite||||||20-AUG-04
37235|Caupaul Igneous Complex|50163|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Includes: Kooreelah Gabbro-Diorite and Ferres Creek Tonalite||||||20-AUG-04
37235|Caupaul Igneous Complex|50164|5|Briefly described|Map Legend|||Includes: Kooreelah Gabbro-Diorite and Ferres Creek Tonalite||||||20-AUG-04
37235|Caupaul Igneous Complex|66002|5|Briefly described|p8 Tb.5|||Includes Ferres Creek Tonalite and Kooreelah Diorite. Defined by Kemp et al. 2002, modified from unpublished Caupaul Monzonite of Ferguson 1993.||||||
3837|Cave Hill Sandstone|22530|6|Mentioned|p698|||||||||
3837|Cave Hill Sandstone|23229|5|Briefly described|Table3-3p26, 26, 31|Pragian|Pragian|||||||
3837|Cave Hill Sandstone|23268|5|Briefly described|Fig14-2.1p388, 397||Early Devonian|||||||
3837|Cave Hill Sandstone|23309|5|Briefly described|p141, 148  Table 2.52, 150||Devonian|||||||
3837|Cave Hill Sandstone|24177|5|Briefly described|p50 Fig.22|Emsian|Emsian|Geological Province: Darraweit Guim Province||||||11-MAY-04
3837|Cave Hill Sandstone|24551|6|Mentioned|p128|||||||||
3837|Cave Hill Sandstone|24588|5|Briefly described|p12 Fig.3|Late Devonian|Late Devonian|Geological Province: Darraweit Guim Province.||||||29-NOV-13
3837|Cave Hill Sandstone|32074|6|Mentioned|Table 1|||Section. See also P180||||||
3837|Cave Hill Sandstone|32076|4|Described|p203|||See also stratigraphy p201.||||||14-JAN-09
3837|Cave Hill Sandstone|32077|5|Briefly described|p35|||||||||
3837|Cave Hill Sandstone|33238|6|Mentioned|p642|||||||||
3837|Cave Hill Sandstone|33598|6|Mentioned|Map legend|Emsian|Emsian|||||||
3837|Cave Hill Sandstone|33599|4|Described|p6|||Devonian.||||||14-JAN-09
3837|Cave Hill Sandstone|33601|6|Mentioned|p34|||||||||
3837|Cave Hill Sandstone|33604|5|Briefly described|p18|||||||||
3837|Cave Hill Sandstone|33606|6|Mentioned|p69|||||||||
3837|Cave Hill Sandstone|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
3837|Cave Hill Sandstone|33732|6|Mentioned|p107|||||||||
3837|Cave Hill Sandstone|34954|6|Mentioned|Fig.34|||||||||
3837|Cave Hill Sandstone|35073|6|Mentioned|p6|||||||||
3837|Cave Hill Sandstone|35283|6|Mentioned|p55|||||||||
3837|Cave Hill Sandstone|41585|4|Described|p111|||||||||
3837|Cave Hill Sandstone|42827|5|Briefly described|p111|||||||||
3837|Cave Hill Sandstone|43461|14|Not recorded|p627|||U/C on Lilydale Limestone.||||||27-OCT-08
3837|Cave Hill Sandstone|43525|14|Not recorded|Table p132||Emsian|||||||
3837|Cave Hill Sandstone|43547|14|Not recorded|Table p152||Emsian|||||||
3837|Cave Hill Sandstone|60599|5|Briefly described|p47 Fig. 19|Emsian|Emsian|Geological Province: Darraweit Guim Province, Melbourne Zone, Lachlan Fold Belt.||||||
3837|Cave Hill Sandstone|61120|6|Mentioned|p4.|||Has an undescribed brachiopod fauna at the base. Replaces Cave Hill Formation.||||Unconformably overlies Lilydale Limestone.||22-SEP-14
3837|Cave Hill Sandstone|61185|5|Briefly described|p21 Fig. 6|Emsian|Emsian|Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
3837|Cave Hill Sandstone|68116|5|Briefly described|Appendix, Map 42.|Early Devonian|Early Devonian||||||Quartzitic sandstone, conglomerate.|
3837|Cave Hill Sandstone|70933|14|Not recorded|Table 1|Devonian|Silurian|Generalised east west section Silurian and Devonian,Victoria refers to Talent 1965.||||||
39640|Central Sandstone|24088|6|Mentioned|p355 Fig. 4||| Geological Province: Lachlan Fold Belt.||||||
3873|Cerberean Volcanics|22451|5|Briefly described|p24|Late Devonian||||||||
3873|Cerberean Volcanics|23229|6|Mentioned|p37|||||||||
3873|Cerberean Volcanics|23309|5|Briefly described|p161 Table 2.60|Devonian|Devonian|||||||
3873|Cerberean Volcanics|29786|6|Mentioned|p85|||||||||
3873|Cerberean Volcanics|31161|5|Briefly described|PA11|||||||||
3873|Cerberean Volcanics|32074|6|Mentioned|Table 3|||See also p184||||||30-AUG-22
3873|Cerberean Volcanics|33238|6|Mentioned|p643|||||||||
3873|Cerberean Volcanics|33732|5|Briefly described|Table III|||||||||
3873|Cerberean Volcanics|35186|4|Described|p6|||||||||
3873|Cerberean Volcanics|35277|3|Fully described|p87|||||||||
3873|Cerberean Volcanics|35278|6|Mentioned|p360|||||||||
3873|Cerberean Volcanics|35283|6|Mentioned|p54|||||||||
3873|Cerberean Volcanics|35526|6|Mentioned|p97|||Discussion of ages.||||||
3873|Cerberean Volcanics|37727|6|Mentioned|p27|||||||||
3873|Cerberean Volcanics|38327|6|Mentioned|p558|||||||||
3873|Cerberean Volcanics|38367|6|Mentioned|Fig.1|||||||||
3873|Cerberean Volcanics|38787|6|Mentioned|p143|||||||||
3873|Cerberean Volcanics|39291|6|Mentioned|p210|||See also Table 1||||||
3873|Cerberean Volcanics|40995|6|Mentioned|Fig.31|||||||||
3873|Cerberean Volcanics|41385|6|Mentioned|p363|||||||||
3873|Cerberean Volcanics|41585|6|Mentioned|Fig.4.5|||||||||
3873|Cerberean Volcanics|41641|4|Described|p157|||See also p160.||||||30-AUG-22
3873|Cerberean Volcanics|41868|6|Mentioned|p485|||||||||
3873|Cerberean Volcanics|42827|4|Described|p157|||see also Fig 5.2 and p160||||||30-AUG-22
3873|Cerberean Volcanics|43461|14|Not recorded|p628|||||||||
3873|Cerberean Volcanics|43547|14|Not recorded|p150|||||||||
3873|Cerberean Volcanics|48894|6|Mentioned|p92|||See also pp93-95. 365+-90my.||||||30-AUG-22
3873|Cerberean Volcanics|64571|5|Briefly described|p827, p828|Late Devonian|Late Devonian|Age: 367+/-2Ma (K/Ar and Rb/Sr). Victoria.||||||15-DEC-08
3873|Cerberean Volcanics|68311|5|Briefly described|p273, 276, 278|Late Devonian|Late Devonian|Cerberean Cauldron, Central Victoria.|375.0 +/- 2 Ma (SIMS U-Pb; Compston, 2004).|||Overlies Snobs Creek Volcanics.|S-type.|
3873|Cerberean Volcanics|70933|14|Not recorded|p98||Late Devonian|Table of Upper Devonian cauldron sequences.||||||
37265|Ceres Gabbro|23309|5|Briefly described|p23,359|Neoproterozoic|Neoproterozoic|||||||
37265|Ceres Gabbro|24002|5|Briefly described|p235|||Correlated with Mesoproterozoic Wickham Metamorphics that underlie the Neoproterozoic Currie Group on King Island (Tas).||||||07-JUL-11
37265|Ceres Gabbro|24098|5|Briefly described|p27 Fig. 2|Cambrian|Cambrian|Geological Province: Melbourne Zone, Lachlan Fold Belt (Darraweit Guim).||||||25-JUN-13
37265|Ceres Gabbro|24551|5|Briefly described|p90|||Probably should be Ceres Metagabbro||||||
37265|Ceres Gabbro|65715|5|Briefly described|p4 Tb.1, p10|Cambrian|Cambrian|Formation rank.||||||
37265|Ceres Gabbro|68116|5|Briefly described|Appendix, Map 50.|Cambrian|Neoproterozoic||||||Metagabbro: weakly deformed to mylonitic; amphibolite facies, with hornblende, plagioclase and relict igneous clinopyroxene.|
75780|Changue East Diorite|68115|5|Briefly described|p8.|||Tabberabbera Zone; near Mount Buller. Formerly Bindaree Diorite on earlier maps (Chappell et al. 1991), but this conflicts with the nearby Bindaree Formation. Named after the parish of Changue East.||||||
75780|Changue East Diorite|68116|5|Briefly described|Appendix, Map 34.|Middle Devonian|Middle Devonian||||||Diorite, gabbro: medium grained, dark green-grey.|
69124|Charlestown Tonalite|68116|5|Briefly described|Appendix, Map 27.|Early Devonian|Early Devonian||||||Hornblende-biotite-(pyroxene) quartz diorite: dark bluish to greenish grey; medium-grained.|
80553|Chatsworth Basalt|71593|4|Described|p8-p9, p12, p27-p28, p102|Late Cambrian||Has geochemical similarities to dykes dated c. 510 Ma which intrude the Kanmantoo Group. Recrystallised by contact metamorphism with later granite intrusion. See also p121-p123, p126, p133, p172, p188, p198.||||Intrudes the Glenthompson Sandstone. Intruded by the Bushy Creek Granodiorite.|Fine-grained basalt to microgabbro occuring as dykes, sills and some possible lava flows.|
3947|Cheltenham Member|42371|6|Mentioned|p33, p36|Cheltenhamian||||||||
30176|Chepstowe Granodiorite|23309|6|Mentioned|p427 App1|||G310 I-Type||||||
30176|Chepstowe Granodiorite|60581|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Beckworth Suite. Biotite granodiorite: medium to coarse grained, pale pinkish-grey, fresh to weathered, topographically recessive, mafic oxidised I-type pluton.||||||23-NOV-04
30176|Chepstowe Granodiorite|60582|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Beckworth Suite. Biotite granodiorite: medium to coarse grained, pale pinkish-grey, fresh to weathered, topographically recessive, mafic oxidised I-type pluton.||||||
30176|Chepstowe Granodiorite|60583|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Beckworth Suite. Biotite granodiorite: medium to coarse grained, pale pinkish-grey, fresh to weathered, topographically recessive, mafic oxidised I-type pluton.||||||
30176|Chepstowe Granodiorite|60584|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Beckworth Suite. Biotite granodiorite: medium to coarse grained, pale pinkish-grey, fresh to weathered, topographically recessive, mafic oxidised I-type pluton.||||||
30176|Chepstowe Granodiorite|60585|4|Described|p24|Late Devonian|Late Devonian|See also Chepstowe granodiorite. Medium to coarse grained, pale-pinkish grey; oxidised, mafic I-type biotite granodiorite.||||||
30176|Chepstowe Granodiorite|66002|5|Briefly described|p6 Tb.5|||Of Beckworth Suite. G310. Defined in Taylor et al. 1995.||||||16-MAY-13
30176|Chepstowe Granodiorite|68116|5|Briefly described|Appendix, Map 40.|Late Devonian|Middle Devonian||||||Biotite granodiorite: medium to coarse grained, pale pinkish-grey; oxidised mafic I-type; magnetic.|
74886|Cherrytree Gap Sandstone Member|64536|5|Briefly described|Map legend|Silurian|Silurian|Of Donnellys Creek Siltstone (Jordan River Group). Medium to thick bedded sandstone;Tbc and lesser Tabc turbidites; quartzitic, interbedded siltstone laminated and bioturbated. Deep marine turbidite fan and hemipelagic deposits.||||||07-FEB-11
74886|Cherrytree Gap Sandstone Member|64537|5|Briefly described|Map legend|Silurian|Silurian|Of Donnellys Creek Siltstone (Jordan River Group). Medium to thick bedded sandstone;Tbc and lesser Tabc turbidites; quartzitic, interbedded siltstone laminated and bioturbated. Deep marine turbidite fan and hemipelagic deposits.||||||07-FEB-11
74886|Cherrytree Gap Sandstone Member|64538|5|Briefly described|Map legend|Silurian|Silurian|Of Donnellys Creek Siltstone (Jordan River Group). Medium to thick bedded sandstone;Tbc and lesser Tabc turbidites; quartzitic, interbedded siltstone laminated and bioturbated. Deep marine turbidite fan and hemipelagic deposits.||||||07-FEB-11
74886|Cherrytree Gap Sandstone Member|64606|5|Briefly described|Map Legend|Late Ordovician|Middle Ordovician|Of Donellys Creek Siltstone (Jordan River Group). Sandstone, siltstone: deep-marine deposits. Yellow in RGB. Nonmagnetic.||||||12-NOV-08
74886|Cherrytree Gap Sandstone Member|64616|4|Described|p305|Llandovery|Llandovery|Unit in Donnellys Creek Siltstone. See also Cherry Tree Sandstone Member (p80). Medium- to thick-bedded quartzitic sandstone, interbedded with laminated and bioturbated siltstone. Geophysical characteristics given.||||||
3963|Chesney Vale Granite|22971|5|Briefly described| p 35|||||||||
3963|Chesney Vale Granite|23309|6|Mentioned|p427 App 1|||G211 S-Type.||||||
3963|Chesney Vale Granite|24551|6|Mentioned|p58|||||||||
3963|Chesney Vale Granite|30906|6|Mentioned|Map legend|Silurian|Silurian|||||||
3963|Chesney Vale Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
3963|Chesney Vale Granite|68116|5|Briefly described|Appendix, Map 19.|Late Devonian|Late Devonian||||||Small intrusions of fine to medium-grained pinkish granophyre, contains tourmaline nodules; consists of quartz, plagioclase, K-feldspar, biotite, zircon, tourmaline, opaques.|
37248|Chetwynd Tonalite|24012|3|Fully described|p223 appendix 1|Ordovician|Cambrian|Intruded by Cairns Creek Granodiorite and Glengoyne Adamellite.||||||
37248|Chetwynd Tonalite|50154|2|Defined|p36, p89-90, p247 App.5|Cambrian|Cambrian|Of the Glenelg Metamorphic Complex. Intruded by Cairns Creek Granodiorite.||||||15-SEP-04
37248|Chetwynd Tonalite|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Biotite tonalite; I-type||||||
37248|Chetwynd Tonalite|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite tonalite.||||||20-AUG-04
37248|Chetwynd Tonalite|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite tonalite.||||||20-AUG-04
37248|Chetwynd Tonalite|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite tonalite.||||||20-AUG-04
37248|Chetwynd Tonalite|50159|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite tonalite.||||||20-AUG-04
37248|Chetwynd Tonalite|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite tonalite.||||||20-AUG-04
37248|Chetwynd Tonalite|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite tonalite.||||||20-AUG-04
37248|Chetwynd Tonalite|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite tonalite.||||||20-AUG-04
37248|Chetwynd Tonalite|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite tonalite.||||||20-AUG-04
37248|Chetwynd Tonalite|50164|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Biotite tonalite; I-type||||||
37248|Chetwynd Tonalite|66002|6|Mentioned|p9 Tb.5|||G433.  Defined by Kemp et al. 2002||||||
37248|Chetwynd Tonalite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Biotite tonalite: massive, bluish-grey, coarse grained with quartz phenocrysts; accessory magnetite and rare allanite; uncommon mafic biotite-rich microgranitoid enclaves; magnetic to non-magnetic.|
25842|Childers Formation|23238|6|Mentioned|p107|||Geol. Province: Western Port Basin.||||||22-DEC-08
25842|Childers Formation|23264|5|Briefly described|Fig13-3.1p324, 331, 335||Oligocene|||||||
25842|Childers Formation|23265|5|Briefly described|Fig13-4.9p349||Paleocene|||||||
25842|Childers Formation|23307|5|Briefly described|Map Legend|Eocene|Eocene|||||||
25842|Childers Formation|24053|5|Briefly described|p37|Miocene|Eocene|Of Latrobe Group. Geological Basin: Gippsland Basin.||||||22-DEC-08
25842|Childers Formation|24551|6|Mentioned|p575, p733 Table 17.3||Tertiary|Max thickness: 40m.||||||
25842|Childers Formation|29821|6|Mentioned|p2|||||||||
25842|Childers Formation|29822|6|Mentioned|p11|||||||||
25842|Childers Formation|30084|4|Described|p9|||||||||
25842|Childers Formation|30930|6|Mentioned|Map legend|Paleocene|Paleocene|||||||
25842|Childers Formation|31045|6|Mentioned|p139|||||||||
25842|Childers Formation|31242|5|Briefly described|p7|||Refers hydrology.||||||17-NOV-08
25842|Childers Formation|31254|2|Defined|p140|Paleocene|Paleocene|See also p141-142.||||||17-NOV-08
25842|Childers Formation|31352|6|Mentioned|p133|||See also Fig. 3. Eocene||||||
25842|Childers Formation|31508|6|Mentioned|Table 1|||Tertiary||||||
25842|Childers Formation|32229|6|Mentioned|p32|||||||||
25842|Childers Formation|32230|6|Mentioned|p34|||||||||
25842|Childers Formation|32232|6|Mentioned|p20|||||||||
25842|Childers Formation|32233|6|Mentioned|p22|||||||||
25842|Childers Formation|32375|6|Mentioned|Table 1|||See also P8||||||
25842|Childers Formation|32679|6|Mentioned|p94|||Stratigraphic diagram||||||
25842|Childers Formation|33156|6|Mentioned|p135|||||||||
25842|Childers Formation|33159|6|Mentioned|p21|||Coal Seams.||||||22-DEC-08
25842|Childers Formation|33237|5|Briefly described|p64|||||||||
25842|Childers Formation|33458|6|Mentioned|p13|||||||||
25842|Childers Formation|33459|6|Mentioned|p10|||Stratigraphy.||||||
25842|Childers Formation|33462|4|Described|p14|||See also p25. Re hydrogeology.||||||17-NOV-08
25842|Childers Formation|33929|6|Mentioned|p70|||See also P71.||||||
25842|Childers Formation|34558|4|Described|p19|||Fig.2||||||
25842|Childers Formation|34815|6|Mentioned|p19|||||||||
25842|Childers Formation|34842|4|Described|p19|||||||||
25842|Childers Formation|34843|4|Described|p9|||||||||
25842|Childers Formation|34991|6|Mentioned|p379|||||||||
25842|Childers Formation|35273|4|Described|p266|||||||||
25842|Childers Formation|35276|6|Mentioned|p244|||||||||
25842|Childers Formation|35285|6|Mentioned|p415|||||||||
25842|Childers Formation|36197|4|Described|p8|||||||||
25842|Childers Formation|37065|4|Described|p42|||||||||
25842|Childers Formation|37127|5|Briefly described|p347|||||||||
25842|Childers Formation|37366|4|Described|p4|||||||||
25842|Childers Formation|37530|6|Mentioned|p5|||||||||
25842|Childers Formation|37809|6|Mentioned|p7|||||||||
25842|Childers Formation|38928|6|Mentioned|Fig.14|||||||||
25842|Childers Formation|38935|5|Briefly described|Fig.2|||||||||
25842|Childers Formation|38973|6|Mentioned|Fig.2|||||||||
25842|Childers Formation|39551|6|Mentioned|Map legend|Miocene|Miocene|||||||
25842|Childers Formation|39555|6|Mentioned|Map legend|Miocene|Miocene|||||||
25842|Childers Formation|40114|6|Mentioned|p4|||||||||
25842|Childers Formation|40523|6|Mentioned|p210|||||||||
25842|Childers Formation|40527|6|Mentioned|p129|||||||||
25842|Childers Formation|41171|6|Mentioned|Fig.6|||||||||
25842|Childers Formation|41318|6|Mentioned|p188|||||||||
25842|Childers Formation|41868|6|Mentioned|p520|||||||||
25842|Childers Formation|42827|3|Fully described|p340|||see also Fig 8.24.||||||17-NOV-08
25842|Childers Formation|61155|5|Briefly described|p18|Late Oligocene|Early Oligocene|Of the LaTrobe Group. Overlain by Thorpdale Volcanics and by Morwell Formation. Age: 35-28Ma. Thickness: 40m. Geological Province: Gippsland Basin (LaTrobe Valley). Not related to Childers Volcanics in the Bundaberg-Gladstone region.||||||
25842|Childers Formation|61302|5|Briefly described|p13|Eocene|Eocene|Alluvial fans, braided streams and point bar sand deposits. Often directly overlies the Strzelecki Group. Geological Province: western margin of Gippsland Basin.||||||
25842|Childers Formation|61336|5|Briefly described|p(ix) Fig. 9|Late Oligocene|Early Oligocene|Geological Province: Gippsland Basin.||||||07-FEB-11
25842|Childers Formation|64535|5|Briefly described|Map legend|Paleogene|Paleogene|Sandstone, conglomerate, clay, sand, gravel; fluvial deposits. ||||||
25842|Childers Formation|64539|5|Briefly described|Map legend|Paleogene|Paleogene|Sandstone, conglomerate, clay, sand, gravel; fluvial deposits. ||||||
25842|Childers Formation|64540|5|Briefly described|Map legend|Paleogene|Paleogene|Sandstone, conglomerate, clay, sand, gravel; fluvial deposits. ||||||
25842|Childers Formation|64605|5|Briefly described|Map legend|Paleogene|Paleogene|Sandstone, conglomerate, clay, sand, gravel; alluvial deposits. Speckled green to blue-black in RGB. Nonmagnetic. Indistinguishable from the overlying Haunted Hills Gravel in TMI and RGB.||||||17-NOV-08
25842|Childers Formation|64616|3|Fully described|p144, p298|Oligocene|Oligocene|Outcrops mainly S of Erica as small erosional remnants on ridges and hills. Unconformably overlies Jordan River and Walhalla Groups. Is overlain by Older Volcanics Group or Haunted Hills Gravel, both disconformably. 10-40m thick. Type area near Childers. Quartzose sandstone, siliceous conglomerate, sand, gravel, silt, clay and brown coal. Geophysical characteristics given.||||||
25842|Childers Formation|66181|6|Mentioned|p297|||A broad plain of fluvial sediments.||||||
25842|Childers Formation|68116|5|Briefly described|Appendix, Maps 43, 51-52, 56-57.|Eocene|Eocene||||||Sandstone, conglomerate, clay, sand, gravel; fluvial deposits.|
25842|Childers Formation|69016|5|Briefly described|p88-89,91,93-101|Early Oligocene|Late Oligocene|Of the Gippsland Basin. Major Early Tertiary aquifer. Thickness: up to 40m.||||Interfingers with Thorpdale Formation.|Terrestrial sandstones, conglomerates and clays.|
25842|Childers Formation|71202|14|Not recorded|p195-196|||Stratigraphy.||||||
25842|Childers Formation|73289|5|Briefly described|p767|Oligocene|Oligocene|Thorpdale-Moe area, Gippsland Basin.||||Is overlain by Thorpdale Volcanics.||
25842|Childers Formation|73488|6|Mentioned|p632 Fig.2|Oligocene|Oligocene|Gippsland Basin.||||Underlies Thorpdale Volcanics||
25842|Childers Formation|75065|5|Briefly described|p151|Oligocene|Oligocene|Gippsland Basin; onshore.||Cobia Subgroup.||Overlies Traralgon Formation. Is overlain unconformably by Morwell Formation (Latrobe Valley Group).|Non-marine conglomerate, sandstone, siltstone.|
30561|Chilpin Granodiorite|23309|6|Mentioned|p427 App1|||S-Type G76.||||||
30561|Chilpin Granodiorite|23615|3|Fully described|p155|Early Silurian|Early Silurian|Of Bullenbong Suite.  Together with Suggan Buggan Granodiorite forms the Suggan Buggan Pluton. Intrudes Bendoc and Yalmy Groups.  Non-conformably overlain by Snowy River Volcanics.  See also p205 App. 1.||||||
30561|Chilpin Granodiorite|43206|5|Briefly described|map legend||Wenlock|Of Bullenbalong Suite. Biotite granodiorite: dark grey; fine grained; massive||||||08-SEP-04
30561|Chilpin Granodiorite|44185|5|Briefly described|Map legend.|Silurian|Silurian|S-type.||||||
30561|Chilpin Granodiorite|68116|5|Briefly described|Appendix, Maps 28, 36.|Wenlock|Llandovery||||||Biotite granodiorite: very fine to medium grained; S-type.|
32309|Chimaera Formation|13323|5|Briefly described|p393 Fig. 2|Campanian|Santonian|Of Golden Beach Subgroup. Fluvial-deltaic and paralic deposits - shales and siltstones, sandstone. Overlain by and interfingers with Anenome Formation; overlies Kipper Shale. Geological Province: Gippsland Basin.||||||
32309|Chimaera Formation|13324|5|Briefly described|p98|||Of Lowry and Longley (1991). Part of extensive fluvial system. Unit expected to be developed regionally.||?Of Golden Beach Subgroup|||Sandstones and minor shales.|
32309|Chimaera Formation|24090|5|Briefly described|p8 Fig.3|Campanian|Santonian|Geological Province: Gippsland Basin.||||||
32309|Chimaera Formation|24407|5|Briefly described|p13 Fig.2|||Geological Province: Gippsland Basin||||||
32309|Chimaera Formation|24551|6|Mentioned|p476|||Of the Golden Beach Subgroup.||||||
32309|Chimaera Formation|61552|6|Mentioned|p583 Fig.2. |Late Cretaceous|Late Cretaceous|||Unit in Golden Beach Subgroup.||||
32309|Chimaera Formation|64876|5|Briefly described|p145 Fig.2|Campanian|Santonian|Gippsland Basin.||Golden Beach Subgroup.||||
32309|Chimaera Formation|65717|5|Briefly described|p9 Fig.2.2, p10-11|Campanian|Santonian|Formerly known as Chimaera Sandstone (Lowry and Longley, 1991). Non-marine succession comprising coarse-grained alluvial/fluvial sediments and fine-grained floodplain deposits.||Golden Beach Subgroup||Intruded by Campanian Volcanics|Sandstone interbedded with coal, siltstone and shale.|05-SEP-17
32309|Chimaera Formation|65718|6|Mentioned|p10 Fig 3.2, p11|Campanian|Coniacian|||Of the Golden Beach Subgroup.||||
32309|Chimaera Formation|65973|4|Described|p15, p29, p40-44, p61-62, p66|Campanian|Campanian|Gippsland Basin. Deposited as an upper coastal plain facies and a braided stream facies. The braided stream facies hosts the majority of hydrocarbon reserves in the Gummy field. Intersected Omeo-1,-2, Kipper-2, Kipper-1, East Pilchard-1 , Judith-1 , East Pilchard-1, Shark-1 and Perch-1 drillholes. Petroleum resource characteristics are discussed. Marine dinoflagellates are present in some horizons. See also p71, p74, p78-79, p82, p85-86, p90, p106-108, p124, p126-127, p129-131, p135, p138-139, p171.||Golden Beach Subgroup|||Coarse-grained sediments including sandstone, conglomerates and fine-grained floodplain deposits including shale and coal.|
32309|Chimaera Formation|70028|6|Mentioned|p79|Campanian|Santonian|||||||
32309|Chimaera Formation|70076|5|Briefly described|South-Eastern:Fig.2;p2.Regional:Fig.3;p7|Campanian|Santonian|Fluvial and coastal plain sediments. Hydrocarbon reservoir, sealed by Campanian volcanics, Emperor Subgroup shales or intraformational mudstones.||Golden Beach Subgroup||Overlies Kipper Shale, Admiral Formation or Kersop Arkose. Is overlain by Anemone, Volador or Barracouta Formation and locally by Campanian Volcanics. Locally encloses Campanian Volcanics.||
32309|Chimaera Formation|73471|5|Briefly described|p86|||Gippsland Basin. Overlies Longtom Unconformity, underlies Seahorse Unconformity.||Golden Beach Subgroup|||Fluvial-deltaic and paralic sandstones and siltstones with interbedded coal layers.|
32309|Chimaera Formation|75065|5|Briefly described|p151, 154, 163-164|Campanian|Turonian|Gippsland Basin; offshore. Fluvial-deltaic and paralic sediments. Contains potential reservoir sandstones.||Golden Beach Subgroup.||Unconformably overlies Curlip Formation (Emperor Subgroup). Is overlain by and abuts Anemone Formation. Is overlain unconformably by Barracouta and Volador Formations (Halibut Subgroup).|Sandstone, siltstone, shale, coal.|
37646|Chin Chap Meladiorite|23309|6|Mentioned|p329 Table 4.1|||I-type. See also Chin Chap Hornblendite.||||||16-MAY-13
37646|Chin Chap Meladiorite|50154|2|Defined|p109, p245 App.5|Cambrian|Cambrian|Intrudes the Kassingbrook Granodiorite.||||||15-SEP-04
37646|Chin Chap Meladiorite|50155|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-rich diorite to gabbro; I-type: nonmagnetic; high K, low Th, U due to surrounding G417 (Kassingbrook Granodiorite).||||||03-SEP-04
37646|Chin Chap Meladiorite|50156|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-rich diorite to gabbro: massive, black, coarse grained; minor biotite, plagioclase and clinopyroxene||||||
37646|Chin Chap Meladiorite|50157|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-rich diorite to gabbro: massive, black, coarse grained; minor biotite, plagioclase and clinopyroxene||||||
37646|Chin Chap Meladiorite|50158|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-rich diorite to gabbro: massive, black, coarse grained; minor biotite, plagioclase and clinopyroxene||||||
37646|Chin Chap Meladiorite|50159|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-rich diorite to gabbro: massive, black, coarse grained; minor biotite, plagioclase and clinopyroxene||||||24-JUN-04
37646|Chin Chap Meladiorite|50160|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-rich diorite to gabbro||||||
37646|Chin Chap Meladiorite|50161|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-rich diorite to gabbro: massive, black, coarse grained; minor biotite, plagioclase and clinopyroxene||||||24-JUN-04
37646|Chin Chap Meladiorite|50162|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-rich diorite to gabbro: massive, black, coarse grained; minor biotite, plagioclase and clinopyroxene||||||24-JUN-04
37646|Chin Chap Meladiorite|50163|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-rich diorite to gabbro: massive, black, coarse grained; minor biotite, plagioclase and clinopyroxene||||||24-JUN-04
37646|Chin Chap Meladiorite|66002|6|Mentioned|p9 Tb.5|||G435. Defined by Morand et al. 2003.||||||
28232|Chintin Formation|22511|4|Described|p660, p661||Silurian|||||||
28232|Chintin Formation|22542|6|Mentioned|p663|||||||||
28232|Chintin Formation|22628|6|Mentioned|fig1p108|Silurian|Silurian|||||||
28232|Chintin Formation|22684|4|Described|p749, Fig.2 p746|Llandovery|Llandovery|See also Fig.5 p749.||||||15-JAN-09
28232|Chintin Formation|22886|4|Described|p12|Wenlock|Llandovery|||||||
28232|Chintin Formation|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
28232|Chintin Formation|23309|4|Described|p134, 139, 149, 150, 151.||Silurian|Age: Upper Telychian/Llandovery. Possible Wenlock. Overlain by Kilmore Siltstone?||||||15-JAN-09
28232|Chintin Formation|24177|5|Briefly described|p50 Fig.22|Llandovery|Llandovery|Geological Province: Darraweit Guim Province||||||
28232|Chintin Formation|24551|6|Mentioned|p606|Silurian|Silurian|||||||
28232|Chintin Formation|24588|5|Briefly described|p12 Fig.3|Wenlock|Wenlock|Geological Province: Darraweit Guim Province.||||||29-NOV-13
28232|Chintin Formation|33604|6|Mentioned|p17|||Correlation chart.Sil||||||
28232|Chintin Formation|37727|4|Described|p46|||See also p9.||||||15-JAN-09
28232|Chintin Formation|38787|6|Mentioned|p131|||||||||
28232|Chintin Formation|39331|6|Mentioned|Table 2-1|||||||||
28232|Chintin Formation|41585|4|Described|p105|||Mention p121.||||||15-JAN-09
28232|Chintin Formation|42628|5|Briefly described|Map legend|Ludlow|Wenlock|||||||
28232|Chintin Formation|42790|5|Briefly described|Fig.14 P189|||||||||
28232|Chintin Formation|42826|2|Defined|p41|Early Silurian||||||||
28232|Chintin Formation|42827|4|Described|p105|||||||||
28232|Chintin Formation|44197|6|Mentioned|Map Legend||Early Silurian|||||||
28232|Chintin Formation|60083|5|Briefly described|Map legend|Late Silurian|Silurian|Laminated and current-bedded sandstone, minor interbedded mudstone and shale. Overlies Springfield Formation.||||||14-APR-08
28232|Chintin Formation|60599|5|Briefly described|p47 Fig. 19|Llandovery|Llandovery|Geological Province: Darraweit Guim Province, Melbourne Zone, Lachlan Fold Belt.||||||
28232|Chintin Formation|61185|5|Briefly described|p21 Fig. 6|Llandovery|Llandovery|Presented as Chintin Fm. Overlies Springfield Sandstone; underlies Kilmore Siltstone. See also Chintin Beds.||||||07-FEB-11
28232|Chintin Formation|61187|5|Briefly described|p5 Fig.3. |Early Silurian|Early Silurian|Melbourne Zone, Melbourne Terrane. Correlative of Seldom Seen Conglomerate, Towanga Formation and Yalmy Group in the Benambra Terrane.||||||
28232|Chintin Formation|62469|5|Briefly described|p6, p5 Fig. 2|Llandovery|Llandovery|Overlies Springfield Sandstone. Geological Province: Darraweit Guim Province. See also p20 Fig. 11, p43, p45.||||||07-FEB-11
28232|Chintin Formation|63083|5|Briefly described|p215, p216 Tb. 1|Wenlock|Llandovery|Overlies Springfield Formation. Sandstones including diverse trilobite faunas. See also p220, p230 Fig. 9.||||||07-FEB-11
28232|Chintin Formation|64611|5|Briefly described|Map legend|Ludlow|Wenlock|Of Murrindindi Supergroup. Sandstone, pebbly sst, pebbly siltstone+siltst:  thick bedded sst with coarse micaceous sandy siltst.; pebbly lithologies poorly sorted; chaotic slump folding+shelly fossils common. Deep-marine mass-flow deposits.||||||16-DEC-08
28232|Chintin Formation|64612|2|Defined|p27, p37, p38|Ludlow|Late Llandovery|Of Murrindindi Supergroup. Underlain conformably by Springfield Sandstone, overlian conformably by Kilmore Siltstone (gradational). Thickness: 150m. Massive to laminated micaceous sandy siltstone to silty sandstone. Abundant shelly fossils.||||||07-FEB-11
74148|Chitts Creek Conglomerate|61329|5|Briefly described|p121|||Of Strzelecki Group. Geological Province: Gippsland Basin.||||||
4038|Chocolyn Silts|31511|6|Mentioned|p305|||||||||
4038|Chocolyn Silts|41848|5|Briefly described|p382|||||||||
4038|Chocolyn Silts|42827|6|Mentioned|p382|||||||||
4042|Chowilla Sand|23818|5|Briefly described|p212 Fig.108|Early Pleistocene|Early Pleistocene|Geological Province: Murray Basin. Of the Blanchetown Clay.||||||18-APR-05
4042|Chowilla Sand|24551|5|Briefly described|p338 Fig. 11.2, 340|Middle Pleistocene|Late Pliocene|||||||
4042|Chowilla Sand|30145|6|Mentioned|p183|||||||||
4042|Chowilla Sand|30754|2|Defined|Appendix 1|early Pleistocene|early Pleistocene|See stratigraphic table on p22.||||||31-MAR-09
4042|Chowilla Sand|30994|6|Mentioned|Fig. 1|||||||||
4042|Chowilla Sand|30996|3|Fully described|p39|||Refers Firman (1971).||||||31-MAR-09
4042|Chowilla Sand|31345|6|Mentioned|p294|||||||||
4042|Chowilla Sand|31385|6|Mentioned|Table 4|||||||||
4042|Chowilla Sand|31745|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
4042|Chowilla Sand|32007|6|Mentioned|Fig. 2|||Pleistocene||||||
4042|Chowilla Sand|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
4042|Chowilla Sand|32861|5|Briefly described|Table 1|||||||||
4042|Chowilla Sand|33048|6|Mentioned|p197|||||||||
4042|Chowilla Sand|33826|6|Mentioned|p42|||Strat. table||||||
4042|Chowilla Sand|34180|6|Mentioned|p212|||Lower Pleistocene.||||||
4042|Chowilla Sand|34459|4|Described|p11|||Pleistocene||||||
4042|Chowilla Sand|34758|6|Mentioned|Table 1|||||||||
4042|Chowilla Sand|35232|6|Mentioned|p15|||||||||
4042|Chowilla Sand|37873|4|Described|p2|||||||||
4042|Chowilla Sand|38068|5|Briefly described|p76|||||||||
4042|Chowilla Sand|40003|6|Mentioned|Table 8|||||||||
4042|Chowilla Sand|41537|6|Mentioned|p350|||||||||
4042|Chowilla Sand|41848|6|Mentioned|p353|||Only on stratigraphic table p353, not in text||||||
4042|Chowilla Sand|42125|5|Briefly described|p138|||||||||
4042|Chowilla Sand|42443|6|Mentioned|p4|||||||||
4042|Chowilla Sand|42827|5|Briefly described|Table 9.1|||||||||
4042|Chowilla Sand|42966|1|Redefined|Table 31 p199|Pleistocene||||||||
4042|Chowilla Sand|44133|5|Briefly described|p252|Middle Pleistocene|Late Pliocene|Thickness: 10m. Geological Province: Murray Basin. Equivalent to Irymple Member. Interfingers with Blanchetown Clay.||||||20-NOV-17
4042|Chowilla Sand|64961|5|Briefly described|p260|||Name used interchangeably with Chowilla Sand Member. Of Blanchetown Clay. Well-sorted sand unit considered as, etc; sand is possibly reworked Loxton-Parilla Sand (see p260).||||||21-APR-09
4042|Chowilla Sand|66287|5|Briefly described|p28,31, Fig 4-5,10|Late Pliocene|Late Pliocene|Similar in appearance to the Loxton-Parilla Sands, but occupies a higher stratigraphic level. With the Blanchetown Clay and the Bungunnia Limestone, part of the Lake Bungunnia sedimentary fill. Included in the Blanchetown Clay by Firman (1965, 1973).||||||25-FEB-13
4042|Chowilla Sand|73228|6|Mentioned|p50, p56, p59|Pleistocene|Late Pliocene|Murray Basin, Lake Bungunnia. Fluvial.||||Unconformably underlain by Karoonda Surface. Overlain by Blanchetown Clay.|Dark-yellow to pale-yellow fine quartz-sand.|
4042|Chowilla Sand|73229|6|Mentioned|p67|Pleistocene|Late Pliocene|Murray Basin.||||||
75110|Chowilla Sand Member|64961|5|Briefly described|p260|Late Pliocene|Late Pliocene|Name used interchangeably with Chowilla Sand. Sand-dominated package at base of Blanchetown Clay. Comprises lower and upper sand separated by a non-calcareous green clay;  Total thickness: 13.15m.||Blanchetown Clay||Said (Brown & Stephenson,1991) to be equivalent to Irymple Member of Lawrence (1975)||25-FEB-13
4081|Claire Creek Limestone Member|24551|6|Mentioned|p614||Devonian|Of the Cowombat Siltstone.||||||31-JAN-06
4081|Claire Creek Limestone Member|37727|5|Briefly described|p51|||||||||
4081|Claire Creek Limestone Member|39447|6|Mentioned|p8|||||||||
4081|Claire Creek Limestone Member|40328|6|Mentioned|p70|||||||||
4081|Claire Creek Limestone Member|41585|6|Mentioned|p128|||||||||
4081|Claire Creek Limestone Member|42827|6|Mentioned|p128|||||||||
4112|Clarkes Hill Basalt|30370|6|Mentioned|p26|||||||||
4112|Clarkes Hill Basalt|43282|6|Mentioned|p67|||Informal name.||||||
26481|Cliffy Island Granite|23309|6|Mentioned|p427 App1|||G251 S-Type.||||||
26481|Cliffy Island Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
26481|Cliffy Island Granite|68116|5|Briefly described|Appendix, Map 57.|Middle Devonian|Middle Devonian||||||Granite, S-type.|
4157|Clifton Formation|22674|5|Briefly described|Fig.2 p719|Early Miocene|Early Oligocene|||||||
4157|Clifton Formation|22875|5|Briefly described|p65|Early Miocene|Early Oligocene|Heytesbury Group.||||||24-JUL-08
4157|Clifton Formation|22944|5|Briefly described|Fig3|||||||||
4157|Clifton Formation|23230|5|Briefly described|Table4-1p40||Oligocene|||||||
4157|Clifton Formation|23249|5|Briefly described|p147 Fig.2||Late Oligocene|Equivalent to middle Gambier Limestone. Plankton fossil assemblage is the age determinant. In the Otway Basin.||||||16-MAY-13
4157|Clifton Formation|23307|5|Briefly described|Map Legend|Miocene|Miocene|Of Heytesbury Group||||||
4157|Clifton Formation|23322|5|Briefly described|957 Fig.2|Late Oligocene|Late Oligocene|Of the Heytesbury Group. Geological Province: Otway Basin.||||||07-SEP-09
4157|Clifton Formation|23402|3|Fully described|p32, p31 fig. 18, p7 Tb. 1|Miocene|Miocene|Thickness: 15m. Geological Province: Otway Basin.||||||24-JUL-08
4157|Clifton Formation|23768|5|Briefly described|p28 Fig.5, p69|Early Miocene|Early Miocene|Geological Province: Otway Basin.  See also p78 Fig. 22, p81.||||||11-SEP-09
4157|Clifton Formation|24056|5|Briefly described|p84 Fig. 2|Miocene|Oligocene|Of Heytesbury Group.  Geological Basin: Otway Basin.||||||
4157|Clifton Formation|24551|5|Briefly described|p246, 304|Miocene|Oligocene|Of the Heytesbury Group.||||||
4157|Clifton Formation|24562|5|Briefly described|p8 Fig. 2|Miocene|Oligocene|Of the Heytesbury Group.  Geological Province: Otway Basin.||||||
4157|Clifton Formation|29823|5|Briefly described|p14|||||||||
4157|Clifton Formation|29856|6|Mentioned|p36|||||||||
4157|Clifton Formation|30576|5|Briefly described|Table 2|||||||||
4157|Clifton Formation|30578|5|Briefly described|p12|||||||||
4157|Clifton Formation|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
4157|Clifton Formation|30675|5|Briefly described|p253|||Lithology & radioactivity||||||
4157|Clifton Formation|30932|6|Mentioned|Map legend|Miocene|Oligocene|Part of Gellibrand Marl. Oligocene-Miocene.||||||19-SEP-18
4157|Clifton Formation|31036|1|Redefined|p211|Oligocene|Oligocene|See also p199, 209, Table 9-1. Unit of Heytesbury Group.||||||04-APR-07
4157|Clifton Formation|31372|6|Mentioned|Fig. 2|||||||||
4157|Clifton Formation|31396|6|Mentioned|p1185|||||||||
4157|Clifton Formation|31424|4|Described|p14|||Description is from a core.||||||
4157|Clifton Formation|31625|6|Mentioned|Fig. 5.2|||Oligocene - Miocene||||||
4157|Clifton Formation|31922|6|Mentioned|Fig.2|||||||||
4157|Clifton Formation|32120|6|Mentioned|p279|||Oligocene fauna.||||||19-SEP-18
4157|Clifton Formation|32220|6|Mentioned|p9|||||||||
4157|Clifton Formation|32852|6|Mentioned|Fig. 2|||||||||
4157|Clifton Formation|33155|4|Described|p122|||||||||
4157|Clifton Formation|33229|6|Mentioned|p246|||||||||
4157|Clifton Formation|33940|6|Mentioned|p414|||||||||
4157|Clifton Formation|34954|6|Mentioned|Fig.35|||||||||
4157|Clifton Formation|35066|3|Fully described|p210|||Described p222.||||||04-APR-07
4157|Clifton Formation|35274|6|Mentioned|p423|||||||||
4157|Clifton Formation|36305|6|Mentioned|p358|||||||||
4157|Clifton Formation|36913|6|Mentioned|p81|||||||||
4157|Clifton Formation|38444|6|Mentioned|p302|||||||||
4157|Clifton Formation|38625|6|Mentioned|Table 2|||||||||
4157|Clifton Formation|41016|5|Briefly described|Table 1|||||||||
4157|Clifton Formation|41185|6|Mentioned|Fig.4|||||||||
4157|Clifton Formation|41269|5|Briefly described|p246|||||||||
4157|Clifton Formation|41398|6|Mentioned|p3|||||||||
4157|Clifton Formation|41639|5|Briefly described|p11|||||||||
4157|Clifton Formation|41642|6|Mentioned|Fig.8.6|||||||||
4157|Clifton Formation|41701|6|Mentioned|Map legend|Oligocene||||||||
4157|Clifton Formation|41704|6|Mentioned|Fig.3|||||||||
4157|Clifton Formation|41714|6|Mentioned|Fig.2|||||||||
4157|Clifton Formation|41726|6|Mentioned|Fig.5|||||||||
4157|Clifton Formation|41769|4|Described|p30|||||||||
4157|Clifton Formation|41868|5|Briefly described|p578|||||||||
4157|Clifton Formation|42079|6|Mentioned|Fig.2 p264|||See also Fig.10, p272||||||19-SEP-18
4157|Clifton Formation|42318|6|Mentioned|Fig.2 p10|||||||||19-SEP-18
4157|Clifton Formation|42452|5|Briefly described|Map legend|early Miocene|late Oligocene|||||||
4157|Clifton Formation|42453|4|Described|p17|||Superseded Kawarren limestone in 1974.||||||
4157|Clifton Formation|42524|5|Briefly described|Fig.3 P27|||||||||
4157|Clifton Formation|42635|6|Mentioned|p91|||||||||
4157|Clifton Formation|42827|3|Fully described|p284|||||||||
4157|Clifton Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
4157|Clifton Formation|43171|6|Mentioned|5-8|||Of Heytesbury Group. Age: 15-30Ma||||||
4157|Clifton Formation|43208|5|Briefly described|map legend|Early Miocene|Late Oligocene|Of Heytesbury Group.||||||
4157|Clifton Formation|43590|4|Described|p24|Early Miocene|Early Oligocene|||||||
4157|Clifton Formation|43604|6|Mentioned|p145|||||||||
4157|Clifton Formation|43660|6|Mentioned|Fig.6,p15||Oligocene|||||||
4157|Clifton Formation|43702|6|Mentioned|p407|Miocene|Oligocene|||||||
4157|Clifton Formation|43733|6|Mentioned|Fig.2.11,p65|Miocene|Oligocene|||||||
4157|Clifton Formation|43744|6|Mentioned|Fig.3,p3|||||||||
4157|Clifton Formation|43937|5|Briefly described|Map Legend|Early Oligocene|Middle Eocene|||||||
4157|Clifton Formation|46802|6|Mentioned|Table 1|||||||||
4157|Clifton Formation|48581|14|Not recorded|p14|||||||||
4157|Clifton Formation|48911|6|Mentioned|Chart 1|||Correlation||||||
4157|Clifton Formation|50154|5|Briefly described|p135|||Of Heytesbury Group.||||||
4157|Clifton Formation|50371|5|Briefly described|Map Legend|Tertiary|Tertiary|Swamp and strand-line deposits; quartz, sand, clay and calcarenite.||||||11-JUN-04
4157|Clifton Formation|60421|5|Briefly described|p417|Early Miocene|Late Oligocene|Of the Heytesbury Group.||||||
4157|Clifton Formation|60538|5|Briefly described|p471 Fig. 10|||||||||
4157|Clifton Formation|60563|6|Mentioned|p47|||||||||
4157|Clifton Formation|60581|5|Briefly described|Map Legend|Miocene|Oligocene|Of the Heytesbury Group. Shallow marine deposits: medium to coarse grained calcarenite of bryozoan and shell fragments in quartz sand matrix, moderately sorted, thin to medium bedded.||||||
4157|Clifton Formation|60582|5|Briefly described|Map Legend|Miocene|Oligocene|Of the Heytesbury Group. Shallow marine deposits: medium to coarse grained calcarenite of bryozoan and shell fragments in quartz sand matrix, moderately sorted, thin to medium bedded.||||||
4157|Clifton Formation|60583|5|Briefly described|Map Legend|Miocene|Oligocene|Of the Heytesbury Group. Shallow marine deposits: medium to coarse grained calcarenite of bryozoan and shell fragments in quartz sand matrix, moderately sorted, thin to medium bedded.||||||
4157|Clifton Formation|60584|5|Briefly described|Map Legend|Miocene|Oligocene|Of the Heytesbury Group. Shallow marine deposits: medium to coarse grained calcarenite of bryozoan and shell fragments in quartz sand matrix, moderately sorted, thin to medium bedded.||||||
4157|Clifton Formation|60585|4|Described|p30|Early Miocene|Late Oligocene|Of the Heytesbury Group. Disconformably overlain by the Gellibrand Marl. Medium to coarse grained sandy calcarenite.||||||
4157|Clifton Formation|60785|5|Briefly described|p184 Fig.1, pp188-189.  |Chattian|Chattian|Eastern margin of Port Campbell Embayment, Otway Basin. Below unnamed nodule horizon, shell Sr/Sr age of 27.4 Ma (Holdgate and Gallagher, 2003). Sr/Sr age of 24.0 Ma immediately above the nodule layer. Foraminifera zone P21b-P22. Has yielded well-preserved isolated fossil cetacean elements: teeth, ribs and bone fragments.|||||Medium coarse-grained calcarenite, with about 10% quartz and limonite sand. At the Kawarren quarry, consists of friable, pale yellow limestone interbedded with harder crystalline bands. All fossils from the more friable calcarenite layers.|
4157|Clifton Formation|61155|5|Briefly described|p3, p18|Early Miocene|Late Oligocene|Of the Heytesbury Group. Coals and clastics deposits. Overlain by Gellibrand Marl. Max. thickness: 90m. Geological Province: Gippsland Basin and Otway Basin (Tyrendarra and Port Campbell Embayments).||||||25-JUN-13
4157|Clifton Formation|61182|3|Fully described|p28, p26, p33|Early Miocene|Early Oligocene|Of Heytesbury Group. Formerly Clifton beds. Calder River Limestone (Aire district) is incorporated. Disconformable over Narrawaturk Marl and Demons Bluff Fm; grades up into Gellibrand Marl. Medium to coarse-grained calcarenite, bryozoans, shell fragments.||||||04-FEB-08
4157|Clifton Formation|61623|6|Mentioned|p449 Fig. 4|Miocene|Oligocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-APR-09
4157|Clifton Formation|61624|5|Briefly described|p465, p466, p466 Fig. 2, p467, p471|Oligocene|Oligocene|Of Haytesbury Group. Overlain by Gellibrand Marl and Port Campbell Limestone. Geological Province: Otway Basin.||||||16-MAY-13
4157|Clifton Formation|61626|6|Mentioned|p486 Fig. 2|Miocene|Oligocene|Geological Province: Otway Basin.||||||07-APR-09
4157|Clifton Formation|61628|5|Briefly described|p509 Fig. 3|Early Miocene|Early Oligocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-APR-09
4157|Clifton Formation|62896|6|Mentioned|p88|||||||||07-FEB-11
4157|Clifton Formation|63269|5|Briefly described|p605|Miocene|Oligocene|Otway Basin.||Heytesbury Group.||||
4157|Clifton Formation|63740|5|Briefly described|p88|||Geological province: Otway Basin.||||||07-FEB-11
4157|Clifton Formation|65316|5|Briefly described|p598,603|Aquitanian|Chattian|Thought to be a correlative of the Point Addis Limestone and Jan Juc Marl; in the Otway Basin. Age from strontium isotope stratigraphy on forams.| 27.8  - 22.4 Ma.|Basal unit of the Heytesbury Group.||||23-APR-12
4157|Clifton Formation|65715|5|Briefly described|p14 Tb.8|Miocene|Oligocene|Of Heytesbury Group.||||||
4157|Clifton Formation|66002|4|Described|p12, p13 Tb.9, p16, p26 Fig.7, p69-74|Neogene|Neogene|Of Heytesbury Group. Defined by Glenie 1971. Impure limestone. Outcrops around the Glenaire flats. Calcarenite, generally medium- to coarse-grained fragments of bryozoans, molluscs and echinoids, minor quartz and limonite sand. Moderately well bedded. Cementation variable||||||
4157|Clifton Formation|66012|3|Fully described|p17-18|Oligocene|Oligocene|Of Heytesbury Group. Littoral to shallow-marine sandy unit. Overlain by Gellibrand Marl. Laterised quartz sand, fossiliferous calcarenite, and brown sandy and silty clay. Strandline deposits. Up to 15m thick| | | | | |13-JUN-13
4157|Clifton Formation|66245|5|Briefly described|p6 Fig.5. |Burdigalian|Rupelian|||Unit in Heytesbury Group.||Is overlain by Gellibrand Marl.||
4157|Clifton Formation|67061|6|Mentioned|p546 Fig.3.|Oligocene|Oligocene|||Unit in Heytesbury Group.||||
4157|Clifton Formation|67366|5|Briefly described|p103 Fig.2. |Oligocene|Oligocene|||Unit in Heytesbury Group.||Unconformably overlies Narrawaturk Marl. Is overlain by Gellibrand Marl.|Shallow marine calcareous sandstone and limestone.|
4157|Clifton Formation|67367|5|Briefly described|p131 Fig.2. |Late Miocene|Middle Miocene|||Unit in Heytesbury Group.||||
4157|Clifton Formation|68116|5|Briefly described|Appendix, Maps 39-40, 49, 55.|Miocene|Oligocene||||||Calcarenite: generally medium to coarse grained, fragments of bryozoans, molluscs and echinoids, minor quartz and limonite sand; moderately bedded, alternating poorly and well-cemented beds; shallow marine and minor beach and near shore deposits.|
4157|Clifton Formation|68991|5|Briefly described|p465, p465 Fig.2|Miocene|Oligocene|Lower Miocene minimum age. < 20 m thick and of shallow-marine origin.|||||Comprises medium- to coarse-grained calcarenite.|
4157|Clifton Formation|69297|5|Briefly described|p79, p98|Chattian|Chattian|Otway Basin. ||Heytesbury Group||Unconformably overlies the Narrawaturk Marl, Upper. Overlain by the Gellibrand Marl. |Limestones. |
4157|Clifton Formation|69651|5|Briefly described|p10|Miocene|Oligocene|||Heytesbury Group.||Unconformably overlies Narrawaturk Marl, Mepunga and Demons Bluff Formations. Is overlain by Gellibrand Marl.||
4157|Clifton Formation|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Oligocene|Oligocene|Otway Basin: Port Campbell Embayment.||Heytesbury Group.||Overlies Narrawaturk Marl. Is overlain by Gellibrand Marl.||
4157|Clifton Formation|70880|6|Mentioned|p77|Miocene|Oligocene|Otway Basin.||||||
4157|Clifton Formation|70942|4|Described|p126, 119|||||||||17-FEB-17
4157|Clifton Formation|71437|4|Described|Fig. 1 opp 154, p155, p160-161|Oligocene|Oligocene|of Baker (1953). Transgressive sand deposit.||Base of Heytesbury Group.||Sharp or transitional to overlying Gellibrand Marl.|Limonitic sandy limestone to glauconitic limestone, limonitic quartz sand.|
4157|Clifton Formation|73357|5|Briefly described|p30, p44, p46, p48|Chattian|Chattian|Otway Basin. Correlated with Proteacidites tuberculatus Spore-Pollen Zone and Operculodinium Dinocyst Superzone, nearshore to offshore marine depositional environments.||Of Heytesbury Group.||Overlies Narrawaturk Marl, underlies Gellibrand Marl.||
4157|Clifton Formation|73383|5|Briefly described|p3, p10 Tb.3.8, p25, p28, p164, p236|Miocene|Oligocene|Otway Basin. Approximately equivalent to chemostratigraphic package S6-P2 which has lower Ti/Cr values than the underlying or overlying packages. Lithologies based on geochemistry using the ChemLith classification includes calcareous limestone and calcareous sandstone, and using the Herron classification (1988) includes Fe-shale, Fe-sand. See also vi, p11 Tb.3.9, p34, p107, p117, p131, p137, p246, p258, p264.||Heytesbury Group||Overlies Nirranda Group, underlies Gellibrand Marl|Limestones.|
4157|Clifton Formation|73385|5|Briefly described|p5|Miocene|Oligocene|Otway Basin.||Heytesbury Group||Overlies Narrawaturk Marl, underlies Gellibrand Marl.|Shallow to open marine limestones.|
4157|Clifton Formation|73386|4|Described|p4, p6, p14, Attachment A1|Chattian|Chattian|Otway Basin. Clastics in sandy facies around the margin of the basin supplied by rivers to the north and east. Depositional environment transitions from paralic coastal environments to high-energy outer shelf environments where clastic poor limestones were deposited in the south and west. Associated with the Middle Proteacidites tuberculatus Spore-Pollen Subzone.||Heytesbury Group||Overlies Narrawaturk Marl, Nirranda Group, underlies Gelilbrand Marl|Sandy limestone, which may be dolomitic or contain thin horizons of phosphate and limonite nodules, limestone and ferruginous sandy marl.|
4157|Clifton Formation|73486|6|Mentioned|p511 Fig.2, p516|Burdigalian|Chattian|Otway Basin.||Heytesbury Group||||
4157|Clifton Formation|73594|5|Briefly described|p4|Miocene|Oligocene|Otway Basin.||Heytesbury Group||Underlies Gellibrand Marl|Marine limestones.|
73495|Clifton Springs Tuff|65715|3|Fully described|p14 Tb.8, p15, p56 Fig.50|Neogene|Neogene|Paper says newly defined here, but does not meet all definition criteria. Of Bellarine Volcanic Group. Overlies Murraduc Basalt. Overlain by Gellibrand Marl. Well-bedded mafic tuffs. Predominantly sand-sized but also include clay and lapilli. Type section at Curlewis (MGA ref given).||||||
4179|Clonbinane Member|13996|6|Mentioned|p147|||See also references to Clonbinane Sandstone Member (p146-147).||||||
4179|Clonbinane Member|23229|5|Briefly described|Table3-3p26, 29|Pridolian|Ludlow|||||||
4179|Clonbinane Member|24177|5|Briefly described|p50 Fig.22|Pridolian|Pridolian|Of the Humevale Siltstone. Geological Province: Darraweit Guim Province||||||
4179|Clonbinane Member|31852|6|Mentioned|p720|||See also Fig.5. Upper Silurian -Lower Devonian.||||||14-JAN-09
4179|Clonbinane Member|33394|6|Mentioned|p75|||||||||
4179|Clonbinane Member|35283|6|Mentioned|p49|||||||||
4179|Clonbinane Member|37727|5|Briefly described|p97|||See also p71.||||||14-JAN-09
4179|Clonbinane Member|41585|6|Mentioned|p109|||||||||
4179|Clonbinane Member|43282|6|Mentioned|p92||Silurian|||||||
4179|Clonbinane Member|43547|14|Not recorded|p148|||||||||
4179|Clonbinane Member|60599|5|Briefly described|p47 Fig. 19|Pridolian|Pridolian|Abbreviation of Clonbinane Sandstone Member? Geological Province: Darraweit Guim Province, Melbourne Zone, Lachlan Fold Belt.||||||
4179|Clonbinane Member|61185|6|Mentioned|p21 Fig. 6, p24-25 Fig. 7|||Williams (1964). Of Humevale Siltstone. See Clonbinane Sandstone Member.||||||07-FEB-11
4179|Clonbinane Member|66244|5|Briefly described|pp2-3.|||Mapped in the Merriang Syncline. This article does not make clear of which Formation this unit was a Member; but it appears it is now part of the Humevale Siltstone. Lateral  equivalent of Broadford Formation in the Whittlesea area.||Unit in Humevale Siltstone.||Overlies Yan Yean Formation. Is overlain by Humevale Siltstone.|A thin sandy unit, with length along strike of 10 km.|
4179|Clonbinane Member|70904|14|Not recorded|p 35|||Stratigraphy.||||||
37252|Cloven Hills Granodiorite|24012|3|Fully described|p223 appendix 1|Ordovician|Cambrian|||||||
37252|Cloven Hills Granodiorite|50154|2|Defined|p75, p102-103, p246 App.5|Ordovician|Ordovician|Corresponds to part of the Wando Granodiorite of Wells (1956)||||||15-SEP-04
37252|Cloven Hills Granodiorite|50155|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite-hornblende granodiorite; I-type||||||
37252|Cloven Hills Granodiorite|50156|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite-hornblende granodiorite: massive, light buff, medium to coarse grained, equigranular; accessory magnetite, sphene, allanite and epidote.||||||
37252|Cloven Hills Granodiorite|50157|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite-hornblende granodiorite: massive, light buff, medium to coarse grained, equigranular; accessory magnetite, sphene, allanite and epidote.||||||
37252|Cloven Hills Granodiorite|50158|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite-hornblende granodiorite: massive, light buff, medium to coarse grained, equigranular; accessory magnetite, sphene, allanite and epidote.||||||
37252|Cloven Hills Granodiorite|50159|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite-hornblende granodiorite: massive, light buff, medium to coarse grained, equigranular; accessory magnetite, sphene, allanite and epidote.||||||24-JUN-04
37252|Cloven Hills Granodiorite|50160|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite-hornblende granodiorite||||||
37252|Cloven Hills Granodiorite|50161|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite-hornblende granodiorite: massive, light buff, medium to coarse grained, equigranular; accessory magnetite, sphene, allanite and epidote.||||||24-JUN-04
37252|Cloven Hills Granodiorite|50162|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite-hornblende granodiorite: massive, light buff, medium to coarse grained, equigranular; accessory magnetite, sphene, allanite and epidote.||||||24-JUN-04
37252|Cloven Hills Granodiorite|50163|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite-hornblende granodiorite: massive, light buff, medium to coarse grained, equigranular; accessory magnetite, sphene, allanite and epidote.||||||24-JUN-04
37252|Cloven Hills Granodiorite|50164|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite-hornblende granodiorite; I-type||||||
37252|Cloven Hills Granodiorite|66002|6|Mentioned|p8 Tb.5|||G418. Defined by Kemp et al. 2002||||||
37252|Cloven Hills Granodiorite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Late Cambrian||||||Biotite-hornblende granodiorite: massive, light buff, medium to coarse grained, equigranular; accessory magnetite, sphene, allanite and epidote; magnetic.|
73148|Clover Hill Complex|61896|5|Briefly described|p61, p62 Fig. 10|||A tuff ring that forms an enclosed basin.||||||19-DEC-07
4250|Cobargo Supersuite|22878|6|Mentioned|p83|||||||||
4250|Cobargo Supersuite|22879|5|Briefly described|map|Early Devonian|Early Devonian|||||||
4250|Cobargo Supersuite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Wangarabell Granodiorite||||||01-OCT-04
4250|Cobargo Supersuite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||06-OCT-04
4250|Cobargo Supersuite|24551|5|Briefly described|p236|||Consists of: Wangarabell Suite||||||
4250|Cobargo Supersuite|42726|5|Briefly described|map legend||Early Devonian|Includes the Brogo, Cobargo, Merricumbene and Wangrah Suites.||||||09-FEB-05
4250|Cobargo Supersuite|42827|6|Mentioned|p430|||||||||
4250|Cobargo Supersuite|68592|6|Mentioned|p24|Early Devonian|Early Devonian|||||||
38292|Cobaw Suite|24383|5|Briefly described|p9 Fig.1|||Geological Province: Lachlan Fold Belt||||||
38292|Cobaw Suite|24384|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes Pyalong Granite and Baynton Granodiorite.||||||
38292|Cobaw Suite|24385|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes the Pyalong Granite and the Baynton Granodiorite.||||||
38292|Cobaw Suite|24386|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes the Pyalong Granite and the Baynton Granodiorite.||||||23-MAR-07
38292|Cobaw Suite|24387|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes the Pyalong Granite and the Baynton Granodiorite.||||||
38292|Cobaw Suite|24388|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes the Pyalong Granite and the Baynton Granodiorite.||||||
32459|Cobbannah Group|22832|4|Described|Fig.1b p634|||?Early Silurian turbidite strata, probably equivalents of the Yalmy Group. See also p637.||||||
32459|Cobbannah Group|22968|6|Mentioned|P94||Silurian|||||||
32459|Cobbannah Group|22971|5|Briefly described|p 21||Silurian|||||||
32459|Cobbannah Group|23309|5|Briefly described|p75, 83, 87, 88, 282|Early Silurian|Early Silurian|Correlates with Yalmy Group.||||||21-OCT-08
32459|Cobbannah Group|23860|5|Briefly described|p944|Silurian||||||||
32459|Cobbannah Group|24004|5|Briefly described|p278|Early Silurian|Early Silurian|||||||
32459|Cobbannah Group|24037|6|Mentioned|p432|Early Silurian|Early Silurian|Geological Province: Lachlan Fold Belt||||||
32459|Cobbannah Group|24551|4|Described|p133, p98|Early Silurian|Early Silurian|||||||
32459|Cobbannah Group|24575|5|Briefly described|p711|Early Silurian|Early Silurian|Geological Province: Lachlan Fold Belt||||||
32459|Cobbannah Group|24576|5|Briefly described|p727|Late Silurian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||21-OCT-08
32459|Cobbannah Group|24600|5|Briefly described|p485|Early Silurian|Early Silurian|Geological Province: Lachlan Fold Belt.||||||
32459|Cobbannah Group|44185|5|Briefly described|Map legend.|Early Silurian|Early Silurian||||||Marine: sandstone, mudstone.|
32459|Cobbannah Group|44187|5|Briefly described|Map Legend||Early Silurian|||||||
32459|Cobbannah Group|60536|6|Mentioned|p552|Silurian|Silurian|Age: ca. 440-430 Ma.||||||
32459|Cobbannah Group|61160|6|Mentioned|p48|||Concordantly overlies the Bendoc Group (west and south).||||||
32459|Cobbannah Group|61161|5|Briefly described|p82-83, p76-78, p5-6|Early Silurian|Early Silurian|Includes Dandongadale Siltstone overlying Moornapa Sandstone. Deep marine; quartzite and minor siltstone; no fossils. Faulted against Pinnak Sandstone and Bendoc Group; unconformably underlies Avon Supergroup. GSV map code: Sc.||||||
32459|Cobbannah Group|61163|4|Described|p85, p10 Fig. 31|Early Silurian|Early Silurian|Comprises Dandongadale Siltstone (upper) and Moornapa Sandstone (lower). Marine sedimentary rocks - thick sequence of turbiditic sandstone and mudstone. Geological Province: Lachlan Fold Belt (Tabberabbera Zone). See also p14 Fig. 3.2, p27, p38 Tb. 6.2.||||||
32459|Cobbannah Group|61169|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Moornapa Sandstone.||||||
32459|Cobbannah Group|61170|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Moornapa Sandstone.||||||07-FEB-11
32459|Cobbannah Group|61171|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Moornapa Sandstone.||||||
32459|Cobbannah Group|61172|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Moornapa Sandstone.||||||
32459|Cobbannah Group|61173|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Moornapa Sandstone.||||||
32459|Cobbannah Group|61174|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Dandongadale Siltstone.||||||07-FEB-11
32459|Cobbannah Group|61175|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Dandongadale Siltstone.||||||
32459|Cobbannah Group|61176|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Dandongadale Siltstone.||||||
32459|Cobbannah Group|61177|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Dandongadale Siltstone.||||||
32459|Cobbannah Group|61178|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Dandongadale Siltstone.||||||
32459|Cobbannah Group|64312|5|Briefly described|p442|Silurian|Silurian|Age is Silurian? ||||||
32459|Cobbannah Group|65900|5|Briefly described|p162, p167||Early Silurian|Lower Silurian. Turbidite, intruded by I-type granites.||||Overlies the Pinnak Sandstone.||10-MAY-12
32459|Cobbannah Group|66769|6|Mentioned|137, 142|Silurian|Ordovician|Tabberabbera Zone. Has a thin-skinned fold style.||||||
32459|Cobbannah Group|67322|6|Mentioned|p16-17|Early Silurian|Early Silurian|The New Country Sandstone is viewed as the local transition into the Yalmy or Cobbannah Group sandstones of the Early Silurian.||||||21-FEB-18
32459|Cobbannah Group|67802|6|Mentioned|p29||Early Silurian|In Benambra Terrane.|||||Turbiditic quartz-rich sandstone and siltstone.|
32459|Cobbannah Group|68116|5|Briefly described|Appendix, Maps 18-19, 26, 34-35, 44.|Wenlock|Llandovery||||||Sandstone, siltstone: sandstone quartzitic, thick to thin bedded, fine to coarse grained, pale grey; siltstone massive to bedded, commonly bioturbated, grey to pale colours.|
32459|Cobbannah Group|70601|5|Briefly described|p52, p56|Early Silurian|Early Silurian|Tabberabbera Zone, western margin of the Albury-Bega Terrane. Deposition preceded deformation similar to that in the Narooma Terrane. Includes at least seven broken-formation zones. Variously mis-spelt: Cobannnah (p52), Cabbannah (p52), Cobbanah (p56).|||||Melange containing Howqua Chert fragments and blocks.|
32459|Cobbannah Group|70629|6|Mentioned|p986|Early Devonian|Silurian|Melbourne Zone.||||||
32459|Cobbannah Group|70718|4|Described|p43|Early Silurian|Early Silurian|Tabberabbera Zone, Murray Basin. Deposited in a deep marine setting.|c. 440-430 Ma||||Quartzite and minor siltstone.|
77308|Cobbledick Basalt|65715|5|Briefly described|p13|||Limited distribution. Thought by Holdgate et al. (2002) to separate Werribee and Yaloak Formations.||||||
37535|Cobbler Rhyolite|23309|4|Described|p169, 181, 185.|Late Devonian|Late Devonian|Formerly Mine Creek Rhyolite.||||||22-FEB-10
37535|Cobbler Rhyolite|24551|4|Described|p166, 174|||Of the Tolmie Igneous Complex.  Of the Rose River Volcanics. Maximum Thickness: 200m.||||||
37535|Cobbler Rhyolite|61163|6|Mentioned|p95|||Lowest unit in Rose River Volcanics at Mount Cobbler. Has been equated with the former "Mine Creek Rhyolite" (Gaul 1982) by Vandenburg et al (2000). Relationship with Cobbler Lava unclear - this is probably an informal reference to the rhyolite?||||||05-JUL-07
37535|Cobbler Rhyolite|66252|2|Defined|p211 Fig.1, p215 Fig.5, p216, p217|Frasnian|Frasnian|See also p219-220, p230-231. Definition data given. Lower Member of Rose River Volcanics, along NW margins of Macalister Synclinorium. Flow banded, phenocryst-poor rhyolite and rhyolite breccia. Thickness highly variable: 0-200m. Unconformably overlies both Ordovician metasedimentary rocks and Mid-Devonian Stirling Granodiorite. Is overlain by Staircase Ignimbrite. Detailed stratigraphic section.||||||
37535|Cobbler Rhyolite|68116|5|Briefly described|Appendix, Map 34.|Late Devonian|Late Devonian||||||Rhyolitic lava with garnet phenocrysts, and lava breccia that is probably resedimented.|
21512|Cobbs Spur Andesite Breccia|23309|5|Briefly described|p36.  Table 2.7|||Of the Licola Volcanics.||||||
21512|Cobbs Spur Andesite Breccia|24551|5|Briefly described|p88 Fig. 3.15|||Of Licola Volcanics (Fig. 3.15).||||||22-DEC-08
21512|Cobbs Spur Andesite Breccia|64535|5|Briefly described|Map legend|Cambrian|Cambrian|Of Licola Volcanic Group. Andesite breccia, volcanogenic sandstone, phophatic shale, limestone megaclasts; marine mass-flow deposits.||||||
21512|Cobbs Spur Andesite Breccia|64539|5|Briefly described|Map legend|Cambrian|Cambrian|Of Licola Volcanic Group. Andesite breccia, volcanogenic sandstone, phophatic shale, limestone megaclasts; marine mass-flow deposits.||||||
21512|Cobbs Spur Andesite Breccia|64540|5|Briefly described|Map legend|Cambrian|Cambrian|Of Licola Volcanic Group. Andesite breccia, volcanogenic sandstone, phophatic shale, limestone megaclasts; marine mass-flow deposits.||||||
21512|Cobbs Spur Andesite Breccia|64605|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Licola Volcanic Group. Andesite breccia, volcanogenic sandstone, phosphatic shale, limestone megaclasts; marine lavas and sedimentary rocks. Red-black in RGB. Non-magnetic.||||||
21512|Cobbs Spur Andesite Breccia|64616|4|Described|p61, 60, p14 Table 1.1, p184-185, p307|Late Cambrian|Middle Cambrian|Of Licola Volcanic Group. Conformably overlies Tobacco Creek Andesite. In faulted contact with Whisky Knob Rhyolite. Poor to moderately sorted, clast-supported monomictic/polymictic breccia, interbedded with finer grained volcaniclastics. Includes phosphatic shale and limestone olistoliths. Appears on p61 also as Cobbs Spur Volcanic Breccia. Geophysical characteristics given.||||||
21512|Cobbs Spur Andesite Breccia|66244|5|Briefly described|p2.|Cambrian|Cambrian|Formerly a unit in Licola Volcanic Group (VandenBerg et al. 1995) which has been made redundant.||Unit in Jamieson Volcanic Group.||||
21512|Cobbs Spur Andesite Breccia|68116|5|Briefly described|Appendix, Maps 34, 43.|Cambrian|Cambrian||||||Andesite breccia, volcanogenic sandstone, phosphatic shale, limestone megaclasts.|
38161|Cobden basalt|24344|5|Briefly described|p78 Fig.8|||Informal. Age: <2Ma.||||||
32306|Cobia Subgroup|13323|5|Briefly described|p393 Fig. 2|Early Oligocene|Middle Eocene|Of the Latrobe Group. Non-marine to paralic clastics; marine clastics. Geological Province: Gippsland Basin. See also p394 Fig. 3.||||||
32306|Cobia Subgroup|24090|5|Briefly described|p8 Fig.3|Oligocene|Eocene|Of Latrobe Group. Geological Province: Gippsland Basin.||||||
32306|Cobia Subgroup|24164|6|Mentioned|p3, 26-27 Figs.16-17, 28-29, 41 Tb.2, 44|||Gippsland Basin||||||
32306|Cobia Subgroup|24407|5|Briefly described|p13 Fig.2, p14|Eocene|Eocene|Of the  Latrobe Group. Geological Province: Gippsland Basin||||||20-FEB-08
32306|Cobia Subgroup|24495|5|Briefly described|p9|||Of Latrobe Group.  Includes Burong and Gurnard Formations.  Geological Province: Gippsland Basin.||||||
32306|Cobia Subgroup|24551|5|Briefly described|p262 Fig. 9.29, 477|Early Oligocene|Middle Eocene|Of the Latrobe Group.||||||
32306|Cobia Subgroup|61552|5|Briefly described|p581, p583 Fig.2, p595.  |Early Oligocene|Middle Eocene|Slower margin sag-phase characterised by declining sediment supply, widespread transgressions on the basin margins and the commencement of compression and structural growth.||Unit in Latrobe Group.|Includes Burong, Gurnard and Turrum Formations.|||
32306|Cobia Subgroup|64876|5|Briefly described|p145 Fig.2|Oligocene|Eocene|Gippsland Basin.||Latrobe Group.|Burong, Gurnard, Turrum Formations.|Overlies Halibut Subgroup (Marlin Unconformity). Is overlain by Seaspray Group (Latrobe Unconformity and Marshall Paraconformity).||
32306|Cobia Subgroup|65717|5|Briefly described|p9 Fig.2.2, p11, p13, p28|Oligocene|Eocene|Formerly the Cobia Group of Thompson (1986).||Latrobe Group|Includes Burong Formation, Gurnard Formation, Turrum Formation|Unconformably overlies Halibut Subgroup, unconformably overlain by Seaspray Group.||05-SEP-17
32306|Cobia Subgroup|65718|5|Briefly described|p8, p10 Fig 3.2, p12, p43 Fig 5.4, p52|Oligocene|Eocene|Gippsland Basin. Middle Eocene minimum age. Formerly the Cobia Group of Thompson (1986). Comprises lower coastal plain and shallow to open marine facies.||Of the Latrobe Group.|Includes the Burong Formation and the Gurnard Formation.|||
32306|Cobia Subgroup|65973|5|Briefly described|p14, p16, p27, p57, p78, p82, |Oligocene|Eocene|Gippsland Basin. Intersected in including Leatherjacket-1,  Kipper-1, Kipper-2, Judith-1, East Pilchard-1, Longtom-1, Longtom-1/ST-1, Longtom-2/ST-1, Sweep-1 and many more drillholes (see appendix). See also p84-85, p90, p93, p97, p100, p102, p112, p114, p123, p126-127, p130-134, p136, p141-143, p171.||Latrobe Group|Includes the Burong Formation, Gurnard Formation.|||
32306|Cobia Subgroup|66181|5|Briefly described|p310 Fig.5|Eocene||Non marine to paralic clastics, in the Latrobe Group. Unconformably overlies the Halibut Subgroup.||||||
32306|Cobia Subgroup|70028|6|Mentioned|p79|Oligocene|Eocene|Gippsland Basin.||Latrobe Group.||Unconformably overlies Halibut Subgroup. Is overlain unconformably by Seaspray Group.||
32306|Cobia Subgroup|70076|5|Briefly described|South-Eastern:Fig.2;p2.Regional:Fig.3;p5|Rupelian|Lutetian|Hydrocarbon source rocks and a major hydrocarbon reservoir.||Latrobe Group.|Turrum, Gurnard, Burong Formations.|Overlies Halibut Subgroup. Is overlain by Angler Subgroup (Seaspray Group).|Includes coals and carbonaceous shales (hydrocarbon sources) and marine near-shore barrier and shoreface sandstones (reservoirs).|
32306|Cobia Subgroup|70331|5|Briefly described|p69|Oligocene|Eocene|Gippsland Basin (western).||Latrobe Group.||Unconformably overlies Halibut Subgroup. Is overlain by Seaspray Group.|Onshore: paralic siltstone, shale, coal. Offshore: marine clastics.|
32306|Cobia Subgroup|73471|5|Briefly described|p86-90, p91 Fig.4|Rupelian|Lutetian|Gippsland Basin. Coastal-plain-dominated siliciclastic sag-phase deposits. Overlies the Marlin Unconformity, underlies the Latrobe Unconformity.|46.5-32 Ma|Latrobe Group|Gurnard Formation, Burong Formation|Unconformably overlies Halibut Subgroup, underlies Seaspray Group||
32306|Cobia Subgroup|75065|5|Briefly described|p151, 154, 166|Oligocene|Eocene|Gippsland Basin.||Latrobe Group.|Traralgon, Burong, Gurnard, Turrum, Childers Formations.|Unconformably overlies Halibut Subgroup. Is overlain unconformably by Latrobe Valley and Seaspray Groups.||
4268|Cobram Sand|24177|4|Described|p77|Quaternary|Quaternary|Source bordering dunes related to the Coonambidgal Formation. Geological Province: Murray Basin||||||
4268|Cobram Sand|35272|5|Briefly described|p287|||||||||
4268|Cobram Sand|41848|5|Briefly described|p362|||||||||
4268|Cobram Sand|42827|6|Mentioned|p362|||||||||
4268|Cobram Sand|60452|4|Described|p41||Quaternary|"Source-bordering dunes" first named by Lawrence (1975) consisting mostly of reworked Shepparton Formation material. Lie uncomformably on the Shepparton Formation.||||||
4268|Cobram Sand|60599|5|Briefly described|p96-97|Recent|Quaternary|Part of Coonambidgal Formation. Source-bordering dunes first described/named by Lawrence (1975). Occur mainly along banks of larger streams - many dunes still actively forming today. ||||||
4268|Cobram Sand|61185|5|Briefly described|p69-71|Recent|Recent|Source-bordering dunes defined by Lawrence (1975) but here considered part of Coonambidgal Fm. Quartz sand, minor silt and clay forming clusters of low (10m max), narrow (up to 100m) crescentic dunes extending 1-2km. Actively depositing today.||||||07-FEB-11
34840|Cobungra Granite|22968|4|Described|P59, P163||Early Silurian|In the Omeo Metamorphic Complex.||||||05-NOV-07
34840|Cobungra Granite|23021|5|Briefly described|Map legend|Wenlock|Wenlock|Of Omeo Metamorphic Compex.||||||16-NOV-05
34840|Cobungra Granite|23028|5|Briefly described|Map legend|Wenlock|Llandovery|Of Omeo Metamorphic Complex.||||||16-NOV-05
34840|Cobungra Granite|23029|5|Briefly described|Map legend|Wenlock|Wenlock|Of Omeo Metamorphic Complex. Heterogenus bodies with variable muscovite-biotite-cordierite-sillimanite: abundant K-feldspar phenocrysts; abundant metasedimentary, gneissic enclaves; dark grey; fine to course grained; massive to strongly foliated.||||||16-NOV-05
34840|Cobungra Granite|23030|5|Briefly described|Map legend|Silurian|Silurian|Parent is the Omeo Metamorphic Complex. Heterogenus bodies with variable muscovite-biotite-cordierite-sillimanite: S-type; nonmagnetic; moderate to high K, Th, U (no distinctive magnetic and radiometric responses).||||||13-SEP-04
34840|Cobungra Granite|23309|5|Briefly described|p338|||(G549 - S-Type)||||||
34840|Cobungra Granite|24551|5|Briefly described|p56, p232,|||Of the Omeo Metamorphic Complex. S-type granite in the Omeo Zone - with both massive and foliated phases; high grade metamorphics.||||||
34840|Cobungra Granite|61160|3|Fully described|p52, p34 Tb. 5.2|Llandovery|Llandovery|In the Omeo Met.Complex (OMC).Classic S-type (red-brown biotite, cordierite, sillimanite) from partial melting of metasediments in Omeo Zone; gradational into migmatite of the OMC. Formerly combined with OMC migmatite as High Plains Gneiss.||||||05-NOV-07
34840|Cobungra Granite|61161|5|Briefly described|p89, p86, p76-77 Fig 6.1|||Nonmagnetic, grey, medium to coarse-grained, unfoliated to strongly foliated or mylonitic, bio-musc S-type granite. Intruded by High Tops Tonalite and Anglers Rest Granite. See High Plains Gneiss and High Plains Gneissic Adamellite. GSV map code: G549.||||||
34840|Cobungra Granite|61164|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Omeo Metamorhpic Complex. Biotite-muscovite granite: with K-feldspar phenocrysts; accessory cordierite; biotite-sillimanite enclaves; common migmatite, gneiss and vein quartz enclaves; variably foliated; S-type intrusion. GSV map code: G549.||||||
34840|Cobungra Granite|61165|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Omeo Metamorhpic Complex. Biotite-muscovite granite: with K-feldspar phenocrysts; accessory cordierite; biotite-sillimanite enclaves; common migmatite, gneiss and vein quartz enclaves; variably foliated; S-type intrusion. GSV map code: G549.||||||
34840|Cobungra Granite|61166|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Omeo Metamorhpic Complex. Biotite-muscovite granite: with K-feldspar phenocrysts; accessory cordierite; biotite-sillimanite enclaves; common migmatite, gneiss and vein quartz enclaves; variably foliated; S-type intrusion. GSV map code: G549.||||||
34840|Cobungra Granite|61167|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Omeo Metamorhpic Complex. Biotite-muscovite granite: with K-feldspar phenocrysts; accessory cordierite; biotite-sillimanite enclaves; common migmatite, gneiss and vein quartz enclaves; variably foliated; S-type intrusion. GSV map code: G549.||||||07-FEB-11
34840|Cobungra Granite|61168|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Omeo Metamorhpic Complex. Biotite-muscovite granite: S-type; nonmagnetic; gravity higher between Kiewa and Nelse shear zones, lower N of Tawonga Fault; moderate to high total radioelement, K, Th and U. GSV map code: G549.||||||
34840|Cobungra Granite|61169|5|Briefly described|map legend|Silurian|Silurian|Of Omeo Metamorphic Complex. Granite, granodiorite: abundant K-feldspar phenocrysts and metasedimentary enclaves, variable muscovite-biotite-cordierite-sillimanite content; S-type intrusion. GSV map code: G549.||||||16-NOV-05
34840|Cobungra Granite|61170|5|Briefly described|map legend|Silurian|Silurian|Of Omeo Metamorphic Complex. Granite, granodiorite: abundant K-feldspar phenocrysts and metasedimentary enclaves, variable muscovite-biotite-cordierite-sillimanite content; S-type intrusion. GSV map code: G549.||||||07-FEB-11
34840|Cobungra Granite|61171|5|Briefly described|map legend|Silurian|Silurian|Of Omeo Metamorphic Complex. Granite, granodiorite: abundant K-feldspar phenocrysts and metasedimentary enclaves, variable muscovite-biotite-cordierite-sillimanite content; S-type intrusion. GSV map code: G549.||||||16-NOV-05
34840|Cobungra Granite|61172|5|Briefly described|map legend|Silurian|Silurian|Of Omeo Metamorphic Complex. Granite, granodiorite: abundant K-feldspar phenocrysts and metasedimentary enclaves, variable muscovite-biotite-cordierite-sillimanite content; S-type intrusion. GSV map code: G549.||||||16-NOV-05
34840|Cobungra Granite|61173|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Omeo Metamorphic Complex. Granite, granodiorite: low to moderate gravity response (-400 to -380 ums^-2); nonmagnetic (k up to 5 x10^-6 cgs); moderate K, U and total radioelements, moderate to high Th. GSV map code: G549.||||||
34840|Cobungra Granite|68116|5|Briefly described|Appendix, Maps 27, 35.|Wenlock|Llandovery||||||Granite, granodiorite: dark grey; fine to coarse-grained; massive to very foliated; K-feldspar phenocrysts and clots of biotite+sillimanite; variable muscovite-biotite-cordierite-sillimanite content; metasedimentary enclaves; grades into migmatite.|
37647|Cochranes Creek Granodiorite|23309|6|Mentioned|p428, Appendix 1|||G341.  Supersedes Bealiba Granodiorite?||||||26-AUG-05
34860|Cocks Break Granodiorite|22968|5|Briefly described|P87, P216||Late Silurian|New name, type locality location given on p216.||||||21-FEB-07
34860|Cocks Break Granodiorite|23028|5|Briefly described|Map legend||Late Silurian|||||||
34860|Cocks Break Granodiorite|23030|5|Briefly described|Map legend|Early Devonian|Late Silurian|||||||
34860|Cocks Break Granodiorite|23309|6|Mentioned|p428 App 1|||G527 I-Type.||||||
34860|Cocks Break Granodiorite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Granodiorite: grey; medium-grained; porphyritic in biotite.|
75876|Cod Formation|70028|6|Mentioned|p79|Miocene|Miocene|Offshore Gippsland Basin.||||||
75876|Cod Formation|70076|5|Briefly described|South-Eastern: Fig.2; Regional: Fig.3|Miocene|Miocene|||Albacore Subgroup.||Overlies Conger Formation. Is overlain by Whiting Formation.||
4303|Cohuna Silt|2967|5|Briefly described|p67 Fig.3.8, p68, p71 Fig.3.10|||Thorne and Macumber (1969). Kow Swamp, northern Victoria,|10,879 +/- 100 BP.||||Lacustrine sandy silt, fine sand; shell band.|
4303|Cohuna Silt|31954|4|Described|p10|||||||||
4303|Cohuna Silt|31955|6|Mentioned|p289|||||||||
4303|Cohuna Silt|31957|6|Mentioned|p309|||||||||
4303|Cohuna Silt|32232|6|Mentioned|p19|||||||||
4303|Cohuna Silt|33486|6|Mentioned|p316|||||||||
4303|Cohuna Silt|41848|6|Mentioned|p364|||Radiocarbon age 13200 BP. Kow Swamp sediments||||||
4303|Cohuna Silt|42827|5|Briefly described|Table 9.2|||||||||
4303|Cohuna Silt|42966|5|Briefly described|p264|||||||||
77309|Coimadai Shale|65715|3|Fully described|p15 Tb.8, p17, p96-102|Pliocene|Pliocene|Paper says newly defined here, but does not meet all definition criteria. Formation rank. Replaces Coimaidai limestone, Coimaidai beds and Coimaidai series of Officer and Hogg (1897). Variable composition ranging from well laminated dolomite to basaltic tuffs. Lacustrine with air-fall tuff. Type locality in Alkemade's Quarrry (MGA ref given).||||||10-FEB-15
77309|Coimadai Shale|68116|5|Briefly described|Appendix, Map 41.|Pliocene|Pliocene||||||Dolomite, clay, sand, tuff: dolomite: white to yellow; clay variable; laminated to varved; tuff basaltic; sandsized; graded.|
37710|Colbinabbin Diorite|23309|6|Mentioned|p428, App. 1|||G297.||||||
37710|Colbinabbin Diorite|24177|4|Described|p43|Early Cambrian|Early Cambrian|Intrudes Sheoak Gully Boninite. Inferred age - represents final phase of Heathcote Volcanics (Lower Cambrian).||||||27-OCT-08
37710|Colbinabbin Diorite|24328|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|||||||
37710|Colbinabbin Diorite|60591|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Diorite: highly magnetic, fine- to medium-grained, subophitic growths of plagioclase and augite.||||||
37710|Colbinabbin Diorite|60592|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Diorite: highly magnetic, fine- to medium-grained, subophitic growths of plagioclase and augite.||||||
37710|Colbinabbin Diorite|60593|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Diorite: highly magnetic, fine- to medium-grained, subophitic growths of plagioclase and augite.||||||
37710|Colbinabbin Diorite|60595|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Diorite: highly magnetic, fine- to medium-grained, subophitic growths of plagioclase and augite.||||||
37710|Colbinabbin Diorite|60596|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Diorite: highly magnetic, fine- to medium-grained, subophitic growths of plagioclase and augite.||||||
37710|Colbinabbin Diorite|60597|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Intensely magnetic (up to 600 nT); low K, Th and U.||||||27-OCT-08
37710|Colbinabbin Diorite|60599|4|Described|p24 Tb. 4, p101|Early Cambrian|Early Cambrian|Intrusive at Cornella East identified by Bailey (1979). Single large diorite sill which intrudes Sheoak Gully Boninite. Ferro-diorite, grey-green in outcrop, variably weathered. ||||||
37710|Colbinabbin Diorite|65715|6|Mentioned|p8 Tb.4|||G297. Of Edwards et al (1998) p101.||||||
37710|Colbinabbin Diorite|68116|5|Briefly described|Appendix, Map 24.|Cambrian|Cambrian||||||Quartz diorite: grey-green; fine- to medium-grained; subophitic growths of plagioclase and augite, with hornblende commonly replacing augite.|
37710|Colbinabbin Diorite|73497|5|Briefly described|Map legend|Cambrian|Cambrian|G297.|||||Diorite: intensely magnetic (up to 600 nT); low K, Th and U.|
4316|Coldstream Rhyolite|23268|6|Mentioned|Fig14-2.2(b)p389, 397||Early Paleozoic|||||||07-NOV-08
4316|Coldstream Rhyolite|23269|4|Described|p402-4, Fig14-3.3p405||Late Devonian|||||||
4316|Coldstream Rhyolite|23309|5|Briefly described|p166.  Table 2.62|||Of the Dandenong Volcanics?||||||
4316|Coldstream Rhyolite|24551|5|Briefly described|p161|Devonian|Devonian|Part of the Dandenong Ranges Igneous Complex.||||||
4316|Coldstream Rhyolite|29652|6|Mentioned|Table 4|||||||||
4316|Coldstream Rhyolite|29653|6|Mentioned|p4|||||||||
4316|Coldstream Rhyolite|30867|6|Mentioned|p16|||See also Fig.2. Late Devonian. Unaffected by Yeringberg Fault.||||||
4316|Coldstream Rhyolite|30931|6|Mentioned|Map legend|Late Devonian|Late Devonian|`Upper' and `Lower' Toscanites||||||
4316|Coldstream Rhyolite|32077|6|Mentioned|p35|||||||||
4316|Coldstream Rhyolite|33157|4|Described|p39|||||||||
4316|Coldstream Rhyolite|33158|4|Described|p39|||||||||
4316|Coldstream Rhyolite|33598|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
4316|Coldstream Rhyolite|33599|4|Described|p7|||Dev.||||||
4316|Coldstream Rhyolite|34956|5|Briefly described|p82|||||||||
4316|Coldstream Rhyolite|35012|5|Briefly described|p430|||||||||
4316|Coldstream Rhyolite|35277|4|Described|p93|||||||||
4316|Coldstream Rhyolite|38146|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
4316|Coldstream Rhyolite|39291|6|Mentioned|Fig.13|||||||||
4316|Coldstream Rhyolite|41641|4|Described|p163|||||||||
4316|Coldstream Rhyolite|42827|5|Briefly described|p163|||see also Fig 5.5||||||
4316|Coldstream Rhyolite|44197|5|Briefly described|Map Legend||Late Devonian|||||||
4316|Coldstream Rhyolite|60083|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Mount Dandenong Volcanics Group.  Rhyolite ("dellenite").||||||
4316|Coldstream Rhyolite|68116|5|Briefly described|Appendix, Map 42.|Late Devonian|Late Devonian||||||Rhyolite lava: coherent flow-banded to autobrecciated; dark greenish to bluish grey, with occasional phenocrysts of andesine in a cryptocrystalline matrix of oligoclase and orthoclase, chloritised biotite, little quartz.|
41194|Coleraine Volcanic Group|50154|2|Defined|p25, p107, p130|Late Jurassic|Early Jurassic|Overlies the Hassall Creek Granodiorite, Bacchus Marsh Formation and the Glenelg River Metamorphic Complex. Disconformably overlain by the Otway Group, Parilla Sand and Lowan Sand. Intrudes the Bacchus Marsh Formation. Max. Thickness: 75m.||||||25-SEP-09
41194|Coleraine Volcanic Group|50155|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Hypatia Formation and Den Hills Formation||||||
41194|Coleraine Volcanic Group|50156|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Den Hills Formation, Hypatia Formation.||||||
41194|Coleraine Volcanic Group|50157|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Den Hills Formation, Hypatia Formation.||||||
41194|Coleraine Volcanic Group|50158|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Den Hills Formation, Hypatia Formation.||||||
41194|Coleraine Volcanic Group|50159|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Den Hills Formation, Hypatia Formation.||||||
41194|Coleraine Volcanic Group|50160|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Den Hills Formation, Hypatia Formation.||||||
41194|Coleraine Volcanic Group|50161|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Den Hills Formation, Hypatia Formation.||||||22-JUN-04
41194|Coleraine Volcanic Group|50162|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes Hypatia Formation and Den Hills Formation||||||
41194|Coleraine Volcanic Group|50163|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Den Hills Formation, Hypatia Formation.||||||16-MAY-13
41194|Coleraine Volcanic Group|50164|5|Briefly described|Map Legend|Jurassic|Jurassic|Includes: Den Hills Formation, Hypatia Formation.||||||
41194|Coleraine Volcanic Group|60421|5|Briefly described|p408 Fig. 1, 409, 418 Fig. 5|Jurassic|Jurassic|Alkalic volcanics.||||||
41194|Coleraine Volcanic Group|64612|6|Mentioned|p28|Mesozoic|Mesozoic|||||||07-FEB-11
41194|Coleraine Volcanic Group|66002|5|Briefly described|p9 Tb.6|Mesozoic|Mesozoic|Includes Den Hills Formation and Hypatia Formation.  Defined by Morand et al. 2003. Previously called Coleraine trachyte by Hogg (1899)||||||
41194|Coleraine Volcanic Group|68116|5|Briefly described|Appendix, Maps 38-39.|Jurassic|Jurassic||||||Trachyte and basalt: lava flows, lava domes and laccoliths.|
32062|Coliban Basalt|24103|6|Mentioned|p139 Fig.3|||Superseded by the Coliban River Volcanic Flow.||||||
32062|Coliban Basalt|24177|4|Described|p73|Early Pliocene|Late Miocene|Of the Newer Volcanics. Partly covered by Shepparton Formation and overlies White Hills Gravel and Calivil Formation. Maximum Thickness: 30m.||||||
32062|Coliban Basalt|24439|5|Briefly described|p8|Quaternary|Cenozoic|Of Edwards et al (1998).  Of the Newer Volcanic Group.||||||19-NOV-08
32062|Coliban Basalt|60591|5|Briefly described|Map Legend|Pliocene|Miocene|Of the Newer Volcanics. Lava flow: olivine basalt; iddingsitised olivine, plagioclase and clinopyroxene phenocrysts; fine-grained, moderately vesicular||||||
32062|Coliban Basalt|60592|5|Briefly described|Map Legend|Pliocene|Miocene|Of the Newer Volcanics. Lava flow: olivine basalt; iddingsitised olivine, plagioclase and clinopyroxene phenocrysts; fine-grained, moderately vesicular||||||
32062|Coliban Basalt|60593|5|Briefly described|Map Legend|Pliocene|Miocene|Of the Newer Volcanics. Lava flow: olivine basalt; iddingsitised olivine, plagioclase and clinopyroxene phenocrysts; fine-grained, moderately vesicular||||||
32062|Coliban Basalt|60595|5|Briefly described|Map Legend|Pliocene|Miocene|Of the Newer Volcanics. Lava flow: olivine basalt; iddingsitised olivine, plagioclase and clinopyroxene phenocrysts; fine-grained, moderately vesicular||||||
32062|Coliban Basalt|60596|5|Briefly described|Map Legend|Pliocene|Miocene|Of the Newer Volcanics. Lava flow: olivine basalt; iddingsitised olivine, plagioclase and clinopyroxene phenocrysts; fine-grained, moderately vesicular||||||
32062|Coliban Basalt|60599|2|Defined|p27, p90-91|Early Pliocene|Late Miocene|Former "Coliban-Campaspe River flows" (Cherry and Wilkinson 1994). At least 2 lava flows - fine-gr.mod'ly weathered, variably vesicular, black to grey olivine basalt. Disconform.on White Hills Gravel; overlain by thin Shepparton Fm. Max.thickness: >30m.||||||
32062|Coliban Basalt|65969|5|Briefly described|p30|Zanclean|Tortonian|Olivine basalt. K/Ar dates range from 7.1+/-0.7 Ma to 4.85+/-0.05 Ma (McKenzie et al., 1984).||||||
79023|Collins Quarry Sandstone Member|62469|6|Mentioned|p5 Fig. 2|Lochkovian|Lochkovian|Of Puckapunyal Formation. Shown as overlying Humevale Siltstone, in Springfield-Kinglake West area. Laterally equivalent to Yeringberg Sandstone Member of Humevale Siltstone in Melbourne-Lilydale area.||||||12-FEB-15
4367|Colongulac Loess|31511|6|Mentioned|p305|||||||||
4367|Colongulac Loess|36370|6|Mentioned|p148|||||||||
4367|Colongulac Loess|41848|5|Briefly described|p383|||||||||
4367|Colongulac Loess|42827|6|Mentioned|p383|||||||||
4369|Colquhoun Granite|23309|6|Mentioned|p428 App. 1|||G130, I-type.||||||
4369|Colquhoun Granite|42726|5|Briefly described|map legend|Middle Devonian||582. NOT variation on Colquhoun Sandstone, Gravel.||||||
4369|Colquhoun Granite|43284|5|Briefly described|Map Legend||Middle Devonian|||||||
4369|Colquhoun Granite|43312|5|Briefly described|Map Legend||Wenlock|G130. Biotite granite, coarse to medium grained, pink, I-Type.||||||26-OCT-04
4369|Colquhoun Granite|43313|5|Briefly described|Map Legend||Wenlock|||||||
4369|Colquhoun Granite|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|I-type.||||||
4369|Colquhoun Granite|60542|4|Described|p95, p19 Fig. 3|Late Devonian|Middle Devonian|Coarse to medium-grained pink granite; contains large quartz and perthitic K-feldspar crystals, plagioclase and <5% biotite; accessory minerals include magnetite, apatite and zircon. Type section is in BAIRNSDALE.||||||19-DEC-07
4369|Colquhoun Granite|61186|5|Briefly described|p52|||Victorian dimension stone. Possibly named for the quarry locality. Fine-grained rock, warm red colour. See also p45 Fig. 14.||||||
4369|Colquhoun Granite|68116|5|Briefly described|Appendix, Map 44.|Middle Devonian|Early Devonian||||||Biotite granite: coarse to medium-grained, pink.|
4371|Colquhoun Sandstone Member|35273|4|Described|p257|||||||||
4371|Colquhoun Sandstone Member|42827|5|Briefly described|p331|||||||||
4371|Colquhoun Sandstone Member|62899|5|Briefly described|p37 Fig. 2|||Geological province: Lakes Entrance Platform.||||||
4371|Colquhoun Sandstone Member|63739|5|Briefly described|p37 Fig. 2|||Of Lakes Entrance Formation. Geological province: Gippsland Basin.||||||01-JUL-08
4371|Colquhoun Sandstone Member|65717|6|Mentioned|p11|Oligocene|Oligocene|Onshore.||Lakes Entrance Formation||||05-SEP-17
4371|Colquhoun Sandstone Member|65718|5|Briefly described|p12, p18|Miocene|Oligocene|||||Of the Lakes Entrance Formation.||
26487|Combyingbar Formation|22530|6|Mentioned|p697||Late Devonian|||||||
26487|Combyingbar Formation|22628|6|Mentioned|fig1p108|Devonian|Devonian|||||||
26487|Combyingbar Formation|22876|5|Briefly described|p15|Late Devonian|Late Devonian|Age: 375-360Ma.||||||07-NOV-07
26487|Combyingbar Formation|22878|3|Fully described|p39|Late Devonian|Late Devonian|||||||
26487|Combyingbar Formation|22879|5|Briefly described|map|Late Devonian|Late Devonian|||||||
26487|Combyingbar Formation|22880|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Sandstone (fine to coarse grained), mudstone and minor pebbly sandstone and conglomerate: fluvial succession, quartzose composition with minor lithic component, mostly red colour, contains plant and rare fish fossils.||||||01-OCT-04
26487|Combyingbar Formation|23309|5|Briefly described|p186-187, p5 Fig. 1.3.|Late Devonian|Late Devonian|||||||05-APR-05
26487|Combyingbar Formation|23938|5|Briefly described|p31-32 Fig. 12|Late Devonian|Late Devonian|Fluvial: conglomerate, sandstone, mudstone. See also p139 Tb. 1 Appendix.||||||
26487|Combyingbar Formation|24004|5|Briefly described|p275 Fig.2|Devonian|Devonian|||||||
26487|Combyingbar Formation|24133|5|Briefly described|p20 Fig. 8|Carboniferous|Late Devonian|Geological Province: Lachlan Fold Belt.||||||
26487|Combyingbar Formation|24551|6|Mentioned|p189|||||||||
26487|Combyingbar Formation|24580|6|Mentioned|p828 Fig.1|||Formation is Fm in text. Geological Province: Eastern Lachlan Fold Belt.||||||
26487|Combyingbar Formation|42627|5|Briefly described|Map legend|Late Devonian|Late Devonian|Variation on Combyingbar Beds.||||||
26487|Combyingbar Formation|42647|4|Described|p33||Late Devonian|||||||
26487|Combyingbar Formation|43228|5|Briefly described|p10||Late Devonian|||||||
26487|Combyingbar Formation|43314|5|Briefly described|Map Legend||Late Devonian|||||||
26487|Combyingbar Formation|43315|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Includes the Mount Puggaree Conglomerate Member. Sandstone, coarse-grained, pebbly sandstone, yellow to grey, generally thick bedded, and mudstone, massive, red-purple, with abundant interbedded sandstone.||||||03-MAY-05
26487|Combyingbar Formation|60503|5|Briefly described|p28 Fig. 9|Late Devonian|Late Devonian|Incorrectly included in the Mount Tambo Group.||||||25-SEP-08
26487|Combyingbar Formation|60541|3|Fully described|p58-59, p37, p134, p17 Tb. 1.|Late Devonian|Late Devonian|Supersedes Combienbar River and Cann River Beds. Incl: basal Mount Puggarree Mbr, overlain by upward-fining sequence of dominantly arenaceous facies to mainly red mudstone (argillaceous). Unconform. on Pinnak Sst, Bendoc Gp  in N.and E. Age:375-360Ma. LFB||||||20-JUN-05
26487|Combyingbar Formation|60542|5|Briefly described|p11 Fig. 2|Late Devonian|Late Devonian|||||||
26487|Combyingbar Formation|61187|6|Mentioned|p5 Fig.3.|Late Devonian|Late Devonian|Mallacoota Zone, Benambra Terrane.||||||
26487|Combyingbar Formation|63605|5|Briefly described|p1002-3|||Superseded Genoa River beds. Outcrops at the NSW-Victoria border in Genoa River area. Includes a basal conglomerate Mount Puggaree Member. Contains the first evidence of land animals in the Devonian of Gondwanaland - in the form of tetrapod trackways.||||||07-FEB-11
26487|Combyingbar Formation|67847|6|Mentioned|p79|||Hosts red-bed copper, uranium, vanadium and silver deposits. ||||||
26487|Combyingbar Formation|68116|5|Briefly described|Appendix, Maps 36-37, 45.|Late Devonian|Late Devonian||||||Sandstone: coarse grained, pebbly sandstone; yellow to grey, generally thick bedded; and mudstone, massive, red-purple, with abundant interbedded sandstone; fluvial deposits.|
26487|Combyingbar Formation|71040|5|Briefly described|p13, p21|Late Devonian|Late Devonian|Boulder Flat Graben, E Victoria. Forms three apparently en echelon synclines with a N to NNE trend.||||Unconformably overlies Errinundra Group.||
34915|Commins Track Leucogranite|22968|5|Briefly described|P215||Early Devonian|New name||||||
34915|Commins Track Leucogranite|23028|5|Briefly described|Map legend||Late Silurian|||||||
34915|Commins Track Leucogranite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|parent is unassigned||||||
34915|Commins Track Leucogranite|23309|6|Mentioned|p428 App1|||G540 S-Type.||||||
34915|Commins Track Leucogranite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Leucogranite: grey to pink; medium to coarse-grained; equigranular to porphyritic.|
37711|Commissioners Flat Granodiorite|23309|6|Mentioned|p428, App. 1|||G286, I-type.||||||
37711|Commissioners Flat Granodiorite|24177|4|Described|p61|Late Devonian|Late Devonian|Overlain by White Hills Gravel. Intrudes Lazy Bar Andesite and Castlemaine Group sediments.||||||25-JUN-13
37711|Commissioners Flat Granodiorite|24328|5|Briefly described|Map legend|Late Devonian|Late Devonian|||||||
37711|Commissioners Flat Granodiorite|24329|5|Briefly described|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
37711|Commissioners Flat Granodiorite|24551|6|Mentioned|p222|||See also Heathcote Granodiorite.  Of the Strathbogie Province.||||||
37711|Commissioners Flat Granodiorite|60591|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Leucogranite: non-magnetic, I-type; fine- to medium-grained, equigranular; composed of quartz, feldspar, hornblende, alkali feldspar.||||||14-JAN-09
37711|Commissioners Flat Granodiorite|60592|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Leucogranite: non-magnetic, I-type; fine- to medium-grained, equigranular; composed of quartz, feldspar, hornblende, alkali feldspar.||||||14-JAN-09
37711|Commissioners Flat Granodiorite|60593|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Leucogranite: non-magnetic, I-type; fine- to medium-grained, equigranular; composed of quartz, feldspar, hornblende, alkali feldspar.||||||14-JAN-09
37711|Commissioners Flat Granodiorite|60595|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Leucogranite: non-magnetic, I-type; fine- to medium-grained, equigranular; composed of quartz, feldspar, hornblende, alkali feldspar.||||||14-JAN-09
37711|Commissioners Flat Granodiorite|60596|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Leucogranite: non-magnetic, I-type; fine- to medium-grained, equigranular; composed of quartz, feldspar, hornblende, alkali feldspar.||||||14-JAN-09
37711|Commissioners Flat Granodiorite|60597|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Leucogranite; I-type: non-magnetic; moderate to high K, low Th and U.||||||27-OCT-08
37711|Commissioners Flat Granodiorite|60599|4|Described|p24 Tb. 4, p83, p101, p19|Late Devonian|Late Devonian|Formerly known as "Heathcote Granite", an unsuitable name due to preoccupation by Heathcote Volcanics. Intrudes Lazy Bar Andesite. Fine- to med.gr., holocrystalline, altered granodiorite, grey-green in fresh outcrop, weathering to white and pink.||||||
37711|Commissioners Flat Granodiorite|65715|5|Briefly described|p7 Tb.4|||G286. Formerly named Heathcote Granite by Thomas et al. (1976).||||||
37711|Commissioners Flat Granodiorite|68116|5|Briefly described|Appendix, Map 24.|Late Devonian|Late Devonian||||||Hornblende-biotite granodiorite: fine- to medium-grained, equigranular; leucocratic; contains alteration assemblage of albite, chlorite and sericite.|
37711|Commissioners Flat Granodiorite|69089|5|Briefly described|Map legend|Late Devonian|Late Devonian|I-type.||||||
41873|Concongella Gritstone Member|60451|4|Described|p62|Late Cambrian|Late Cambrian|Of the Warrak Formation. Type section in text. Maximum Thickness: 60m+. Magdala Volcanics probably protolith.||||||18-OCT-04
41873|Concongella Gritstone Member|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Warrak Formation. Defined by Cayley and Taylor 2001.||||||
73150|Cones Suite|61896|5|Briefly described|p15|||Part of the Newer Volcanics Province. Alkaline basalts. See also Cones Series basalts and Cones basalts.||||||19-DEC-07
83448|Congupna pluton|73497|5|Briefly described|Map legend|Late Devonian|Late Devonian|G752.|||||Nonmagnetic; 20 micrometres/second/second gravity low.|
34841|Connleys Track Granodiorite|22968|5|Briefly described|P60, Table7, P179|Late Silurian|Early Silurian|Age of unit is 424+/-5Ma, New name, intrudes Cobungra Granite, intruded by Bingo Munjie Quartz Diorite||||||
34841|Connleys Track Granodiorite|23029|5|Briefly described|Map legend|Wenlock|Wenlock|Parent is unassigned||||||
34841|Connleys Track Granodiorite|23030|5|Briefly described|Map legend|Silurian|Silurian|||||||
34841|Connleys Track Granodiorite|23309|5|Briefly described|p338|||(G117) S-Type. Age: U/Pb  425 +/- 5 Ma. Supersedes Mount Sam Granodiorite.||||||29-MAR-05
34841|Connleys Track Granodiorite|24551|6|Mentioned|p717 Table 2.4|Wenlock|Wenlock|Age: ~425Ma.||||||
34841|Connleys Track Granodiorite|61160|5|Briefly described|p120|Early Silurian|Early Silurian|Pluton on OMEO. Age: 424+/-5Ma.||||||09-JAN-07
34841|Connleys Track Granodiorite|68116|5|Briefly described|Appendix, Map 35.|Ludlow|Wenlock||||||Biotite-muscovite granodiorite: grey; medium-grained; equigranular; massive to moderately foliated.|
34845|Connors Creek Tonalite|22968|5|Briefly described|P60, P202||Late Silurian|Parent is the Ensay Suite. G135a: highly magnetic; low to moderate K, moderate Th, low U. G135b: weakly to moderately magnetic; moderate K, Th low to moderate U. G135c: weakly to moderately magnetic; moderate to high K, low to moderate Th, U||||||14-SEP-04
34845|Connors Creek Tonalite|23020|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Ensay Suite||||||
34845|Connors Creek Tonalite|23021|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Ensay Suite||||||
34845|Connors Creek Tonalite|23028|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Ensay Suite||||||
34845|Connors Creek Tonalite|23029|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Ensay Suite||||||
34845|Connors Creek Tonalite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Ensay Suite||||||
34845|Connors Creek Tonalite|23309|5|Briefly described|p428 App1|||G135 I-Type. Supersedes Ensay South-Swifts Creek Tonalite, Ensay Tonalite and Ensay South Tonalite.||||||
34845|Connors Creek Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Biotite-hornblende tonalite: medium to coarse-grained, massive to moderately foliated.|
28285|Coode Island Silt|23237|5|Briefly described|p103-4|||||||||
28285|Coode Island Silt|23537|5|Briefly described|p 448|||||||||
28285|Coode Island Silt|24551|5|Briefly described|p338 Fig. 11.2|Holocene|Late Pleistocene|||||||
28285|Coode Island Silt|29982|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
28285|Coode Island Silt|30986|5|Briefly described|p197|||Holocene. See also P198,201.||||||
28285|Coode Island Silt|31009|6|Mentioned|M3|||||||||
28285|Coode Island Silt|33604|5|Briefly described|p25|||||||||
28285|Coode Island Silt|35011|3|Fully described|p313|||||||||
28285|Coode Island Silt|41848|4|Described|p391|||Age approx 8500 yrs||||||
28285|Coode Island Silt|42827|4|Described|p391|||of Yarra Delta Group||||||
28285|Coode Island Silt|44197|5|Briefly described|Map Legend||Pleistocene|||||||
28285|Coode Island Silt|60083|5|Briefly described|Map legend|Recent|Pleistocene|Silty clay, sometimes fossiliferous; sands, minor gravel of the Yarra delta.||||||
28285|Coode Island Silt|68116|5|Briefly described|Appendix, Maps 41-42.|Pleistocene|Pleistocene||||||Black silt, clay: lagoon deposits.|
28285|Coode Island Silt|71203|14|Not recorded|p207|||River Terraces.||||||
28285|Coode Island Silt|71277|4|Described|p301-309, p311-316|Quaternary|Quaternary|Lucas (1887). A widespread component of the Yarra Delta, infilling river-cut valleys of the Yarra and Maribyrnong Rivers. Thickness averages 20-25m in two main depocentres (isopach map). The unit is a major problem for construction foundations because of its poor load-bearing strength and high pyrite content/acid groundwater effects. Numerous carbon-14 ages given.|15,399 - 6,555 yrs BP (14C analyses).|Yarra Delta Group.||Overlies Fishermens Bend Silt, the Batman Avenue Gravels beneath the Yarra River, and Werribee Formation.|Very soft to firm, dark grey-brown silty clays with some sand. Variably fossiliferous (shell layers). Tends to be carbonaceous, with plant debris and woody material towards the base.|
37249|Coojar Granodiorite|24012|3|Fully described|p223 appendix 1|||||||||
37249|Coojar Granodiorite|50154|5|Briefly described|p85|||Included here in the Tuloona Granodiorite as they are very similar and occur adjacent to each other.||||||
4563|Coolungoolun coal|37127|5|Briefly described|p349|||||||||
4583|Coomandook Formation|23322|5|Briefly described|957 Fig.2|Pleistocene|Pliocene|Geological Province: Gambier Basin.||||||07-SEP-09
4583|Coomandook Formation|23818|5|Briefly described|p212 Fig.108, p213|Early Pleistocene|Early Pleistocene|Geological Province: Otway Basin. Overlying unit: Bridgewater Formation. Underlying unit: Parilla Sand.||||||
4583|Coomandook Formation|23921|5|Briefly described|p1109 Table 1|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
4583|Coomandook Formation|29591|6|Mentioned|p92|||||||||
4583|Coomandook Formation|29697|6|Mentioned|p22|||||||||
4583|Coomandook Formation|29892|6|Mentioned|p79|||||||||
4583|Coomandook Formation|30754|2|Defined|Appendix 1|early Pleistocene|early Pleistocene|See also Stratigraphic table p22. p24,28.||||||04-SEP-19
4583|Coomandook Formation|31241|4|Described|p101|||Lower Pleistocene||||||
4583|Coomandook Formation|32116|4|Described|p45|||||||||
4583|Coomandook Formation|32859|4|Described|p69|||L.Pleist.||||||
4583|Coomandook Formation|33566|6|Mentioned|p373|||See also p379.||||||01-NOV-22
4583|Coomandook Formation|33798|6|Mentioned|p98|||Fig.2||||||
4583|Coomandook Formation|34180|5|Briefly described|p212|||Lower Pleistocene.||||||
4583|Coomandook Formation|34191|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
4583|Coomandook Formation|34758|6|Mentioned|Table 1|||||||||
4583|Coomandook Formation|35066|6|Mentioned|p218|||||||||
4583|Coomandook Formation|35097|6|Mentioned|p123|||||||||
4583|Coomandook Formation|38068|6|Mentioned|p76|||||||||
4583|Coomandook Formation|38699|6|Mentioned|p29|||||||||
4583|Coomandook Formation|38932|4|Described|p99|||See also Fig.4||||||
4583|Coomandook Formation|39077|6|Mentioned|p27|||||||||
4583|Coomandook Formation|40003|5|Briefly described|p44|||See also Table 10||||||
4583|Coomandook Formation|41511|6|Mentioned|p24|||||||||
4583|Coomandook Formation|41520|5|Briefly described|Fig.12|||||||||
4583|Coomandook Formation|41599|6|Mentioned|p192|||||||||
4583|Coomandook Formation|42129|6|Mentioned|p254|||See also Fig.6||||||
4583|Coomandook Formation|42717|5|Briefly described|map legend|Pleistocene||||||||
4583|Coomandook Formation|42827|5|Briefly described|Fig 8.9|||||||||
4583|Coomandook Formation|42966|1|Redefined|p210|Early Pleistocene|Pliocene|||||||
4583|Coomandook Formation|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Shallow marine, fossiliferous sandy limestone and calcareous sand.||||||25-MAY-05
4583|Coomandook Formation|43073|4|Described|p13,Table 4|||||||||
4583|Coomandook Formation|43195|5|Briefly described|Map Legend||Early Pleistocene|see also commentary on back of map.||||||
4583|Coomandook Formation|43258|5|Briefly described|Map Legend||Pleistocene|||||||
4583|Coomandook Formation|43298|5|Briefly described|Map Legend||Pleistocene|||||||
4583|Coomandook Formation|44133|5|Briefly described|p220-222|Early Pleistocene|Early Pleistocene|Maximum Thickness: 75m. ||||||
4583|Coomandook Formation|46839|6|Mentioned|Fig.3|||||||||
4583|Coomandook Formation|49038|4|Described|Table 2|||Briefly described P33||||||
4583|Coomandook Formation|60953|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Shelly and gravelly beach deposits.||||||
4583|Coomandook Formation|61108|5|Briefly described|map legend|Pleistocene|Pleistocene|Marine strandline gravel and shellbeds.||||||
4583|Coomandook Formation|61155|5|Briefly described|p18|Pleistocene|Pleistocene|Overlies Whalers Bluff Formation; overlain by Bridgewater Formation. Geological Province: Otway Basin (Gambier Embayment).||||||03-MAR-10
4583|Coomandook Formation|63124|6|Mentioned|p93|||Unconformably overlies Green Point Member (Gambier Limestone). ||||||
4583|Coomandook Formation|67462|5|Briefly described|Map legend.|Pliocene|Pliocene|Murray Basin.||||||
4583|Coomandook Formation|68715|6|Mentioned|p31 Fig.5|Ionian|Zanclean|Murray Basin.||||||
4583|Coomandook Formation|69297|6|Mentioned|p79|Pleistocene|Pliocene|Otway Basin. ||||Unconformably overlies the Narracoorle Limestone Member. Unconformably overlain by the Bridgewater Formation. |Sandstone. |
4583|Coomandook Formation|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Pleistocene|Pliocene|Otway Basin: Gambier Embayment and Voluta Trough.||||Overlies Gambier Limestone. Is overlain by Bridgewater Formation.||
4583|Coomandook Formation|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Holocene|Pliocene|Gambier Embayment and Voluta Trough.||||Overlies Gambier Limestone (Heytesbury Group). Is overlain by Bridgewater Formation.||
4583|Coomandook Formation|73228|6|Mentioned|p50, p56-57, p59|Pleistocene|Late Pliocene|Murray Basin, Lake Bungunnia.||||Unconformably underlain by Karoonda Surface.||
4583|Coomandook Formation|73229|6|Mentioned|p67|Pleistocene|Late Pliocene|Murray Basin.||||||
4595|Coombool Member|22773|5|Briefly described|Fig24.5p350|Early Cretaceous|Early Cretaceous|||||||
4595|Coombool Member|22799|3|Fully described|p21|Albian|Aptian|Monash Formation||||||
4595|Coombool Member|22857|5|Briefly described|p548 App.1 Tb.A1.12|Albian|Aptian|Of the Monash Formation. Green-grey chloritic volcanolithic siltstone, sandstone and shale. Max. thickness: >150m. Geological Province: Berri Basin. See also p350 Fig. 24.5.||||||
4595|Coombool Member|22887|4|Described|Table 5 p31|Early Cretaceous|Early Cretaceous|See also Fig.5 p12. Renmark Trough||||||
4595|Coombool Member|22893|5|Briefly described|table5 fig4||Early Cretaceous|||||||
4595|Coombool Member|24551|6|Mentioned|p270|||Of the Monash Formation||||||
4595|Coombool Member|33488|2|Defined|p10|Early Cretaceous|Early Cretaceous|See also p11.||||||01-NOV-22
4595|Coombool Member|33490|4|Described|p10|||See also p25. Albian||||||01-NOV-22
4595|Coombool Member|35232|6|Mentioned|Table.2|||||||||
4595|Coombool Member|39211|6|Mentioned|p38|||Fig.23||||||
4595|Coombool Member|42966|1|Redefined|Table 7 p67|Albian|Aptian|of Monash Formation||||||
4595|Coombool Member|43052|5|Briefly described|Table 2.1|||of Monash Formation.||||||01-NOV-22
4595|Coombool Member|43218|4|Described|Fig.3,p22|Albian|Albian|Of Monash Formation,||||||
4595|Coombool Member|44191|5|Briefly described|Map Legend||Early Cretaceous|||||||
4595|Coombool Member|49038|5|Briefly described|p23|||||||||
4595|Coombool Member|49040|6|Mentioned|p8|||||||||
4595|Coombool Member|61314|5|Briefly described|p123, p129|Albian|Albian|Upper part of the Monash Formation. A terrestrial sequence of rocks - consisting of lithic sandstone, shale and siltstone. Overlies the Merreti Member. Geological Province: western Murray Basin.||||||
4595|Coombool Member|68189|6|Mentioned|p25, p33|Aptian|Albian|Of the Murray Basin.||Of the Monash Formation.||||
4595|Coombool Member|73228|5|Briefly described|p50-54|Early Cretaceous|Early Cretaceous|Berri Basin. Fluvial lacustrine depositional environment. Identified in Cooltong 1, Berri North 1, Nadda 1, and Loxton 1 drillholes. Distribution is more widespread than Pyap Member, overlapping older sediments and intervening basement ridges.||Monash Formation||Underlain by Merreti Member. Overlain by Warina Sand, Renmark Group.|Fluviolacustrine claystone and siltstone with minor interbeds of highly lithic sandstone.|
4595|Coombool Member|73229|5|Briefly described|p66-68, p70-72, p74|Early Cretaceous|Early Cretaceous|Berri Basin. [Analysed using pXRF; see article].||Monash Formation.|||Fluviolacustrine claystone and siltstone with minor interbeds of highly lithic sandstone.|01-NOV-22
4598|Coonambidgal Formation|2967|5|Briefly described|p40, 107|||Lawrence (1966, 1975). Murray Basin.|||||Brown and grey clays; a terrace with large wavelength meander scroll.|
4598|Coonambidgal Formation|10010|5|Briefly described|p16|Quaternary|Pliocene|Grades downwards into Calivil Formation  Geological Province: Murray Basin.||||||20-FEB-09
4598|Coonambidgal Formation|22531|5|Briefly described|p22|||||||||
4598|Coonambidgal Formation|22532|5|Briefly described|map legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|22756|6|Mentioned|P39|||||||||
4598|Coonambidgal Formation|22782|6|Mentioned|p15|||||||||
4598|Coonambidgal Formation|22799|3|Fully described|p58|Holocene|Late Pleistocene|Age: <14 000 years BP.||||||21-MAY-08
4598|Coonambidgal Formation|22887|2|Defined|p47|Holocene|Holocene|||||||
4598|Coonambidgal Formation|22893|3|Fully described|p62,63 table3,11||Holocene|Unconsolidated. Broken up into older and younger alluvial terraces.||||||
4598|Coonambidgal Formation|23164|5|Briefly described|p16|||||||||
4598|Coonambidgal Formation|23166|5|Briefly described|Map legend||Quaternary|||||||
4598|Coonambidgal Formation|23167|5|Briefly described|Map legend||Quaternary|||||||
4598|Coonambidgal Formation|23168|5|Briefly described|Map legend||Quaternary|||||||
4598|Coonambidgal Formation|23169|5|Briefly described|Map legend||Quaternary|||||||
4598|Coonambidgal Formation|23252|5|Briefly described|Map Legend|||||||||11-JAN-10
4598|Coonambidgal Formation|23603|5|Briefly described|p12|||||||||
4598|Coonambidgal Formation|23604|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|23605|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|23606|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|23607|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|23818|5|Briefly described|p212 Fig.108|Recent|Recent|Geological Province: Murray Basin.||||||
4598|Coonambidgal Formation|23921|5|Briefly described|p1109 Table 2|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
4598|Coonambidgal Formation|24103|6|Mentioned|p139 Fig.3|||||||||
4598|Coonambidgal Formation|24107|6|Mentioned|p224|||||||||
4598|Coonambidgal Formation|24133|6|Mentioned|p51|||Geological Province: Murray Basin.||||||
4598|Coonambidgal Formation|24177|3|Fully described|p77|Recent|Recent|Defined by Lawrence (1966) from type locality in NSW. Disconformably overlies the Shepparton Formation. Geological Province: Murray Basin.||||||17-JUN-09
4598|Coonambidgal Formation|24178|6|Mentioned|p18|Devonian|Ordovician|||||||
4598|Coonambidgal Formation|24232|5|Briefly described|p226 Fig.2, p227|||||||||
4598|Coonambidgal Formation|24326|5|Briefly described|Map legend|Recent|Pleistocene|||||||
4598|Coonambidgal Formation|24439|5|Briefly described|p8, p18|Quaternary|Quaternary|Fluvial sediments of Lawrence (1966).  Diachronous with Shepperton Formation.  See also p47 Fig. 22, Appendix 2.||||||
4598|Coonambidgal Formation|24440|5|Briefly described|Map legend|||||||||
4598|Coonambidgal Formation|24551|5|Briefly described|p338 Fig. 11.2, 342|Holocene|Late Pleistocene|Of the Wunghnu Group.||||||
4598|Coonambidgal Formation|29860|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|29898|6|Mentioned|p213|||||||||
4598|Coonambidgal Formation|30581|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|30750|6|Mentioned|p4|||||||||
4598|Coonambidgal Formation|30751|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|30753|4|Described|p14|||Recent age||||||
4598|Coonambidgal Formation|30754|2|Defined|Fig.33|Recent|Recent|||||||
4598|Coonambidgal Formation|30755|6|Mentioned|p169|||Tectonic map||||||
4598|Coonambidgal Formation|30758|6|Mentioned|p66|||Riverine||||||
4598|Coonambidgal Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
4598|Coonambidgal Formation|30906|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|30934|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|30935|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|30936|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|30996|3|Fully described|p48|||Age discussed.||||||21-MAY-08
4598|Coonambidgal Formation|31654|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|31713|5|Briefly described|p17|||||||||
4598|Coonambidgal Formation|31741|6|Mentioned|p6|||||||||
4598|Coonambidgal Formation|31742|5|Briefly described|p6|||Upper Cainozoic||||||
4598|Coonambidgal Formation|31745|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|31746|6|Mentioned|p197|||||||||
4598|Coonambidgal Formation|31747|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|32007|6|Mentioned|Fig. 2|||||||||
4598|Coonambidgal Formation|32432|6|Mentioned|Fig.2|||Table 1||||||
4598|Coonambidgal Formation|34180|6|Mentioned|p212|||Recent||||||
4598|Coonambidgal Formation|34735|4|Described|p41|||Also mention p8||||||
4598|Coonambidgal Formation|34758|6|Mentioned|p27|||||||||
4598|Coonambidgal Formation|34986|6|Mentioned|p339|||||||||
4598|Coonambidgal Formation|35091|4|Described|p18|||||||||
4598|Coonambidgal Formation|35097|6|Mentioned|Fig.4|||||||||
4598|Coonambidgal Formation|35111|6|Mentioned|p2|||||||||
4598|Coonambidgal Formation|35174|6|Mentioned|p167|||||||||
4598|Coonambidgal Formation|35187|6|Mentioned|Table1|||||||||
4598|Coonambidgal Formation|35200|6|Mentioned|Map legend|Holocene|Holocene|||||||
4598|Coonambidgal Formation|35232|5|Briefly described|Table.4|||||||||
4598|Coonambidgal Formation|35272|3|Fully described|p280|||||||||
4598|Coonambidgal Formation|37871|4|Described|p13|||||||||
4598|Coonambidgal Formation|37873|4|Described|p4|||||||||
4598|Coonambidgal Formation|37881|6|Mentioned|p16|||||||||
4598|Coonambidgal Formation|37882|4|Described|p7|||||||||
4598|Coonambidgal Formation|37883|6|Mentioned|p11|||||||||
4598|Coonambidgal Formation|37884|6|Mentioned|p14|||||||||
4598|Coonambidgal Formation|37885|5|Briefly described|p6|||||||||
4598|Coonambidgal Formation|38068|5|Briefly described|p79|||||||||
4598|Coonambidgal Formation|38879|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|39858|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|39860|5|Briefly described|p33|||||||||
4598|Coonambidgal Formation|40226|6|Mentioned|p51|||||||||
4598|Coonambidgal Formation|40522|6|Mentioned|Fig.2|||||||||
4598|Coonambidgal Formation|41765|4|Described|p42|||||||||
4598|Coonambidgal Formation|41848|3|Fully described|p355|||Use of name has been varied. Here basal "Monoman Formation is not distinguished.||||||
4598|Coonambidgal Formation|41849|6|Mentioned|p409|||Age Pleistocene-Recent||||||
4598|Coonambidgal Formation|41868|6|Mentioned|p552|||||||||
4598|Coonambidgal Formation|42125|6|Mentioned|p139|||||||||
4598|Coonambidgal Formation|42128|5|Briefly described|p227|||See also Fig.2||||||
4598|Coonambidgal Formation|42184|6|Mentioned|Fig.2 P348|||||||||
4598|Coonambidgal Formation|42264|4|Described|p9|||See also Fig.3||||||
4598|Coonambidgal Formation|42454|5|Briefly described|p12|||Maximum age: 25 000BP.||||||20-OCT-08
4598|Coonambidgal Formation|42455|5|Briefly described|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|42827|3|Fully described|p356|||see also Table 9.1||||||
4598|Coonambidgal Formation|42966|1|Redefined|p276|Holocene|Late Pleistocene|Of Wunghnu Group.||||||13-AUG-07
4598|Coonambidgal Formation|43053|5|Briefly described|Map Legend|Holocene|Holocene|||||||25-MAY-05
4598|Coonambidgal Formation|43258|5|Briefly described|Map Legend||Holocene|||||||
4598|Coonambidgal Formation|43261|5|Briefly described|Map Legend||Holocene|||||||
4598|Coonambidgal Formation|43298|5|Briefly described|Map Legend||Holocene|||||||
4598|Coonambidgal Formation|43493|5|Briefly described|32-38|Recent|Pleistocene|Radiocarbon date: 25 000 years BP.||||||20-OCT-08
4598|Coonambidgal Formation|43655|5|Briefly described|p40-846|||||||||
4598|Coonambidgal Formation|44133|5|Briefly described|p254 Fig. 11.28|Holocene|Holocene|||||||
4598|Coonambidgal Formation|44185|5|Briefly described|Map legend.|Holocene|Holocene||||||Fluvial, lacustrine: clay, sand, sandy clay.|
4598|Coonambidgal Formation|44186|5|Briefly described|Map Legend||Holocene|||||||
4598|Coonambidgal Formation|44187|5|Briefly described|Map Legend||Holocene|||||||
4598|Coonambidgal Formation|44188|5|Briefly described|Map Legend|Holocene|Pleistocene|Geological province: Murray Basin. Fluvial/alluvial deposits.||||||20-OCT-08
4598|Coonambidgal Formation|44191|5|Briefly described|Map Legend|Holocene|Late Pleistocene|||||||
4598|Coonambidgal Formation|46909|6|Mentioned|Fig.2|||||||||
4598|Coonambidgal Formation|49038|4|Described|Table 2|||Briefly described p32.||||||20-OCT-08
4598|Coonambidgal Formation|60005|5|Briefly described|Map legend|Holocene|Holocene|Fluvial, lacustrine: clay, sand, sandy clay.||||||11-JAN-10
4598|Coonambidgal Formation|60452|4|Described|p41-42|Quaternary|Quaternary|Alluvial deposits.||||||
4598|Coonambidgal Formation|60461|5|Briefly described|Map legend|Pleistocene|Pleistocene|Alluvial flood plain and fan deposits, channel sands and clay playettes; clay, silt, fine to coarse-grained sand, gravel.||||||
4598|Coonambidgal Formation|60491|4|Described|p23|Quaternary|Quaternary|Deposited by modern day streams and consists of unconsolidated grey-brown silt, clay, gravel and sand.||||||22-NOV-04
4598|Coonambidgal Formation|60492|5|Briefly described|Map Legend|Pleistocene|Pliocene| Alluvium of modern day streams and recent ancestors: sand, silt, clay.||||||30-SEP-04
4598|Coonambidgal Formation|60529|5|Briefly described|Map Legend|Recent|Pliocene|Alluvial flood plain, scroll deposits and source bordering dunes: clay, silt, fine to coarse grained sand, gravel: moderately sorted, unconsolidated.||||||14-JUN-06
4598|Coonambidgal Formation|60591|5|Briefly described|Map Legend|Recent|Pliocene|Overlies the Shepparton Formation. Clay, silt, fine-to coarse grained sand, gravel, moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|60592|5|Briefly described|Map Legend|Recent|Pliocene|Overlies the Shepparton Formation. Clay, silt, fine-to coarse grained sand, gravel, moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|60593|5|Briefly described|Map Legend|Recent|Pliocene|Overlies the Shepparton Formation. Clay, silt, fine-to coarse grained sand, gravel, moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|60595|5|Briefly described|Map Legend|Recent|Pliocene|Overlies the Shepparton Formation. Clay, silt, fine-to coarse grained sand, gravel, moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|60596|5|Briefly described|Map Legend|Recent|Pliocene|Overlies the Shepparton Formation. Clay, silt, fine-to coarse grained sand, gravel, moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|60597|5|Briefly described|Map Legend|Recent|Pliocene|Nonmagnetic with dendritic, moderately magnetic responses (10-20 nT) coinciding with present and prior streams; low K, Th, and variable U.||||||
4598|Coonambidgal Formation|60599|2|Defined|p24 Tb. 4, p95-96|Quaternary|Quaternary|Of Wunghnu Group. Includes Cobram Sand. Pale grey-brown silt +clay or fine- to coarse-g.qtz+ lithic sand, silt/clay; parts contain well-rounded qtz pebbles + ironstone fragments. Disconformable on Shepparton Formation; unconformable on Newer Volcanics. ||||||
4598|Coonambidgal Formation|60953|5|Briefly described|Map Legend|Holocene|Holocene|Stream alluvium in Murray River valley.||||||11-MAY-05
4598|Coonambidgal Formation|61108|5|Briefly described|map legend|Holocene|Holocene|Stream alluvium in Murray River valley.||||||
4598|Coonambidgal Formation|61163|5|Briefly described|p99, p109|||Term often used to include all the Quaternary alluvium in the Riverine Plains, but it is in fact a geomorphic unit and not primarily defined from its lithology.||||||
4598|Coonambidgal Formation|61185|2|Defined|p20 Fig. 5, p57, p64, p69-73|Recent|Pliocene|Of Lawrence (1966). Considered to now include Cobram Sand (Lawrence 1975). Deposits of existing streams cut into older Shepparton Formation sediments. Nonconformable on Strathbogie Granite. Actively deposited today.||||||07-FEB-11
4598|Coonambidgal Formation|61701|5|Briefly described|Map Legend|Recent|Pliocene|Alluvial flood plain, scroll deposits and source bordering dunes: clay, silt, fine to coarse grained sand, gravel: moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|61702|5|Briefly described|Map Legend|Recent|Pliocene|Alluvial flood plain, scroll deposits and source bordering dunes: clay, silt, fine to coarse grained sand, gravel: moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|61703|5|Briefly described|Map Legend|Recent|Pliocene|Alluvial flood plain, scroll deposits and source bordering dunes: clay, silt, fine to coarse grained sand, gravel: moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|61704|6|Mentioned|Map legend|Quaternary|Quaternary|From stream deposits derived from Strathbogie Granite; high K, variable Th; sediments deposited by the Goulburn River have moderate to high K, low Th.||||||12-FEB-15
4598|Coonambidgal Formation|61964|5|Briefly described|p143, p177|Quaternary|Quaternary|Of the Wunghnu Group. Associated with the Shepparton Formation. Geological Province: Murray Basin.||||||
4598|Coonambidgal Formation|64612|6|Mentioned|p56|||Name no longer used. Lawrence (1966).||||||07-FEB-11
4598|Coonambidgal Formation|65552|5|Briefly described|p2,p5-7,p12-13,p17,p19; p24,27 App.3,6 |Quaternary|Early Pliocene|Of Wanghnu Group. Poorly consolidated, mottled, variegated clay and silty lenses of sand and gravel. Hosts silica sand and minor clay deposits. With Shepparton Formation, overlies Calivil Formation and is the uppermost sequence in the Murray Basin.||||||
4598|Coonambidgal Formation|65715|6|Mentioned|p17|||Lapsed into disuse by GSV.||||||
4598|Coonambidgal Formation|65969|5|Briefly described|p27 Tb.3.3, p30|Quaternary|Quaternary|Fluvial mud and sand. Conformably overlies other units. Underlain by Karoonda Surface. Fills current river valleys and debouchments onto the Murray Valley. No magnetic response; mostly Th-rich but variable radiometric response, depending on source rocks.||||||
4598|Coonambidgal Formation|66002|6|Mentioned|p18|||Disused name. Use extended beyond type section and lithology, to all modern-day alluvial sediments N of Great Dividing Range, so GSV has dropped name.||||||
4598|Coonambidgal Formation|66287|6|Mentioned|p30 Fig. 8|Holocene|Pleistocene|||||||
4598|Coonambidgal Formation|67179|5|Briefly described|p580 Fig.1b, p581, 582|Holocene|Pleistocene|Laid down under arid climate by 'ancestral streams' that are precursors to current rivers in the region. See VandenBerg (1997d) and Macumber (1991).||||Conformably overlies the Shepparton Formation.||
4598|Coonambidgal Formation|68194|5|Briefly described|p24, p35|Holocene|Pleistocene|Butler (1958); Lawrence (1966). Channel and floodplain sediments, including alluvial sediments currently being deposited in the south of the map area. Appears as Coonambigil on p35.||||Overlies Shepparton Formation.||
4598|Coonambidgal Formation|68716|6|Mentioned|p39 Fig.3, p40|||||||Underlain by the Monoman Formation.||
4598|Coonambidgal Formation|69089|5|Briefly described|Map legend|Holocene|Holocene||||||Fluvial, lacustrine: clay, sand, sandy clay.|
4598|Coonambidgal Formation|70718|5|Briefly described|p25|||Alluvial fan formation. See also misspelling Coonabidgal Formation p23.||||Overlies Calivil Formation gradationally.||
4598|Coonambidgal Formation|70961|14|Not recorded|p133|||Refers to Lawrence (1966).||||||
4598|Coonambidgal Formation|73188|6|Mentioned|p320|Holocene|Holocene|Murray Basin.|||||Sand, clay, gravel, loam.|
4598|Coonambidgal Formation|73228|6|Mentioned|p62|Quaternary|Pliocene|||||||
4598|Coonambidgal Formation|73496|5|Briefly described|Map legend|Holocene|Pleistocene|[misspelt in map legend as Coornambidgal]||Wunghnu Group|||Nonmagnetic; high total count, K, Th, U; occupies regional topographic lows.|
4598|Coonambidgal Formation|73505|5|Briefly described|p2, p12-13|Quaternary|Quaternary|Murray Basin. Conformably overlies other units. Fills active river valleys. Often high K, Th radiometric response. No detectable magnetic response.|||||Fluvial mud and sand.|
37712|Cooney Ridge Granodiorite|23309|6|Mentioned|p428,  App 1|||G512, I-type. Supersedes Cooney Ridge Granite.||||||
37712|Cooney Ridge Granodiorite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|G512. I-type. Medium-coarse grained hornblende, biotite granodiorite||||||
37712|Cooney Ridge Granodiorite|43315|5|Briefly described|Map Legend|Wenlock|Wenlock|G512. I-type. Medium-coarse grained hornblende, biotite granodiorite.||||||03-MAY-05
37712|Cooney Ridge Granodiorite|60541|6|Mentioned|p16, p17 Tb. 1, p63|Silurian|Silurian|See also Cooney Ridge Granite - names used interchangeably.  Previously mapped as part of Orbost Granodiorite (Beams and Hough 1979).  Medium- to coarse-grained mafic rocks dominated by euhedral twinned and zoned plagioclase.  Geol.Province: LFB||||||12-JAN-06
37712|Cooney Ridge Granodiorite|68116|5|Briefly described|Appendix, Map 45.|Wenlock|Llandovery||||||Hornblende-biotite granodiorite: medium to coarse-grained; I-type.|
4615|Coongulmerang Formation|24468|5|Briefly described|p405 Fig.2|Pliocene|Pliocene|Geological Province: Gippsland Basin||||||
4615|Coongulmerang Formation|35273|6|Mentioned|p263|||||||||
4615|Coongulmerang Formation|37330|5|Briefly described|Table 4|||||||||
4615|Coongulmerang Formation|42827|4|Described|p337|||Of Sale Group.||||||01-JUL-08
4615|Coongulmerang Formation|62899|5|Briefly described|p37 Fig. 2|||Geological province: Lakes Entrance Platform.||||||
4615|Coongulmerang Formation|63739|5|Briefly described|p37 Fig. 2|||Overlain by Haunted Hill Gravel. Geological province: Gippsland Basin.||||||01-JUL-08
4615|Coongulmerang Formation|70076|5|Briefly described|Regional: Fig.3|Pleistocene|Pliocene|||Seaspray Group.||Overlies Jemmys Point Formation. Is overlain by Haunted Hills Formation.||
23508|Coonooer Granite|23164|4|Described|p19|Early Devonian|Early Devonian|||||||
23508|Coonooer Granite|23165|5|Briefly described|Map legend||Devonian|||||||
23508|Coonooer Granite|23166|5|Briefly described|Map legend||Devonian|of Mount Cole Suite.||||||
23508|Coonooer Granite|23167|5|Briefly described|Map legend||Devonian|Of Mount Cole Suite. G359. Muscovite-biotite granite: pale grey to pink, medium to coarse grained, muscovite and microline more common than biotite and plagioclase respectively. Granoblastic texture.||||||16-MAY-13
23508|Coonooer Granite|23168|5|Briefly described|Map legend||Devonian|Of Mount Cole Suite.||||||16-MAY-13
23508|Coonooer Granite|23169|5|Briefly described|Map legend||Devonian|of Mount Cole Suite.||||||
23508|Coonooer Granite|23309|5|Briefly described|p232, 342.|||G359. Of Coonooer Suite.  S-type granite.||||||
23508|Coonooer Granite|24551|6|Mentioned|p229|||Of the Charlton Province.||||||
23508|Coonooer Granite|42726|5|Briefly described|map legend|Early Devonian||Reserved 1976. NLR 1982.||||||
23508|Coonooer Granite|60491|4|Described|p45|||Of the Coonooer Suite. S-type.||||||
23508|Coonooer Granite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Coonooer Suite. Muscovite biotite granite: S-type, reduced; weakly porphyritic, with fine grained aplitic and pegmatite phases; occasional large rafts of weathered micaceous hornfels.||||||
23508|Coonooer Granite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of the Coonooer Suite. S-type; gravity response the deepest part of a regional low. G359a: weakly magnetic outer edge, high K moderate Th, U. G359b: moderately magnetic; moderate K, high Th, U. G359c: nonmagnetic inner part; high K, moderate Th, low U.||||||30-SEP-04
23508|Coonooer Granite|61750|6|Mentioned|p19|||S-type.||||||
23508|Coonooer Granite|66002|5|Briefly described|p6 Tb.5|||Of Coonooer Suite. G359. Defined in Bibby and Moore 1998.||||||
23508|Coonooer Granite|66769|6|Mentioned|p127 Fig.8b|||Stawell Zone.||||||
23508|Coonooer Granite|68116|5|Briefly described|Appendix, Maps 16, 23.|Middle Devonian|Early Devonian|Comprises a nonmagnetic core and weakly magnetic rim.|||||Muscovite-biotite granite: pale grey to pink, weakly porphyritic, coarse to fine grained, contains aplite and pegmatite; muscovite > biotite and microcline > plagioclase, granoblastic texture, weak flow foliation in places; S-type; reduced.|
23508|Coonooer Granite|68189|6|Mentioned|p17 Fig.7, p31 Fig.16|||||||||27-JUN-14
37536|Coonooer Suite|23309|5|Briefly described|p342|||Consists of Carapooee Granodiorite, Berrimal Granite and Coonooer Granite. Weekly Magnetic Plutons.||||||
37536|Coonooer Suite|60452|5|Briefly described|p51|||See also Coonooer suite. Component outcrop plutons: Barrakee, Berrimal, Grieves and Narrewillock.||||||
37536|Coonooer Suite|60461|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes the Barrakee, Grieves and Berrimal Granites, and the Narrewillock pluton.||||||
37536|Coonooer Suite|60462|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
37536|Coonooer Suite|60491|5|Briefly described|p26, p45|||Includes the north-south trending granites.||||||22-NOV-04
37536|Coonooer Suite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Barrakee Granite, Nardoo Granite, Yeungroon Granite, Richmond Granite, Coonooer Granite, Berrimal Granite.||||||
37536|Coonooer Suite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Includes: Barrakee Granite, Nardoo Granite, Yeungroon Granite, Richmond Granite, Coonooer Granite, Berrimal Granite.||||||30-SEP-04
37536|Coonooer Suite|66002|5|Briefly described|p6 Tb.5|||Includes Grieves Granite, Barrakee Granite, Berrimal Granite, Coonooer Granite, Richmond Granite and Yeungroon Granite. Defined in Bibby and Moore 1998.||||||
37536|Coonooer Suite|68189|6|Mentioned|p15 Fig.6||||||||granites|
24873|Coopers Creek Limestone|5178|6|Mentioned|p105, p106, p107 Table 2|Pragian|Pragian|Fossiliferous parts of this unit are mid-Pragian||||||
24873|Coopers Creek Limestone|22520|6|Mentioned|p17|Early Devonian|Early Devonian|||||||
24873|Coopers Creek Limestone|22570|6|Mentioned|p189|Emsian|Pragian|||||||
24873|Coopers Creek Limestone|23229|4|Described|Table3-3p27, 28, 33|Pragian|Pragian|||||||
24873|Coopers Creek Limestone|23308|6|Mentioned|Map Legend|||Mine name?||||||
24873|Coopers Creek Limestone|23309|5|Briefly described|p150, 151, 154.|Lochkovian|Devonian|||||||
24873|Coopers Creek Limestone|23522|5|Briefly described|p247 Fig 3|Early Devonian|Early Devonian|||||||
24873|Coopers Creek Limestone|24002|5|Briefly described|p234|Early Devonian|Early Devonian|||||||
24873|Coopers Creek Limestone|24177|5|Briefly described|p50 Fig.22|Early Devonian|Early Devonian|Geological Province: Mount Easton Province.||||||
24873|Coopers Creek Limestone|24551|5|Briefly described|p126, 614|Emsian|Pragian|Of the Jordan River Group?||||||
24873|Coopers Creek Limestone|24588|6|Mentioned|p30|||Forms a calcareous part of the Boola Fan.||||||
24873|Coopers Creek Limestone|24611|6|Mentioned|p209|||||||||
24873|Coopers Creek Limestone|24612|5|Briefly described|p12|Pragian|Pragian|Contains Carlinastraea fauna.||||||06-APR-05
24873|Coopers Creek Limestone|31502|5|Briefly described|p95|||Devonian corals. See also p108.||||||21-MAY-08
24873|Coopers Creek Limestone|33601|6|Mentioned|p14|||P16||||||
24873|Coopers Creek Limestone|33602|6|Mentioned|Fig.7|||||||||
24873|Coopers Creek Limestone|34815|6|Mentioned|p20|||||||||
24873|Coopers Creek Limestone|35112|6|Mentioned|Fig.9|||||||||
24873|Coopers Creek Limestone|38787|6|Mentioned|p141|||||||||
24873|Coopers Creek Limestone|39331|6|Mentioned|Table 2-1|||||||||
24873|Coopers Creek Limestone|39551|6|Mentioned|Map legend|Pragian|Pragian|||||||
24873|Coopers Creek Limestone|41317|6|Mentioned|p173|||||||||
24873|Coopers Creek Limestone|41585|4|Described|p112|||||||||
24873|Coopers Creek Limestone|41868|5|Briefly described|p574|||||||||
24873|Coopers Creek Limestone|42033|6|Mentioned|p654|||||||||
24873|Coopers Creek Limestone|42635|5|Briefly described|Fig.10 P32|||||||||
24873|Coopers Creek Limestone|42827|5|Briefly described|p112|||||||||
24873|Coopers Creek Limestone|42938|4|Described|p578|||see also Fig.3 p576.||||||21-MAY-08
24873|Coopers Creek Limestone|43530|14|Not recorded|p1028-30||Siegenian|See also Lexicon. L.Siegenian||||||
24873|Coopers Creek Limestone|44447|6|Mentioned|p135|Early Devonian|Early Devonian|||||||
24873|Coopers Creek Limestone|60599|5|Briefly described|p14|Late Emsian|Pragian|Chert and limestone turbidites. Geological Province: Melbourne Zone, Lachlan Fold Belt. ||||||
24873|Coopers Creek Limestone|61138|5|Briefly described|p207, p210-211|||Contains early Pragian conodont assemblages.||||Conformably overlies the Boola Formation.||
24873|Coopers Creek Limestone|61185|5|Briefly described|p37, p39, p21 Fig. 6|Emsian|Lochkovian|Of Jordan River Group (Philip, 1962; VandenBerg, 1975). Interfingers with Wilson Creek Shale; overlies Boola Formation. Geological Province:Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
24873|Coopers Creek Limestone|61186|5|Briefly described|p45 Fig. 14, p90|Early Devonian|Early Devonian|Victorian dimension stone - includes limestones and silty limestones, medium to dark grey in colour and partly consisting of comminuted fossil fragments. ||||||
24873|Coopers Creek Limestone|62070|5|Briefly described|p36, p37|Emsian|Pragian|Includes coral Favosites gothlandicus, Squameofavosites squamuliferus.||||||
24873|Coopers Creek Limestone|64296|6|Mentioned|p91|||Age is Late Pragian to early Emsian based on the unit spanning the 'sulcatus' and 'dehiscens' conodont range.||||||05-NOV-14
24873|Coopers Creek Limestone|64535|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Group. Limestone, mid to very dark grey, bedded to massive; stylobrecciated; minor chert conglomerate, mudstone; deep-marine mass flow deposits. ||||||
24873|Coopers Creek Limestone|64539|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Group. Limestone, mid to very dark grey, bedded to massive; stylobrecciated; minor chert conglomerate, mudstone; deep-marine mass flow deposits. ||||||
24873|Coopers Creek Limestone|64540|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Group. Limestone, mid to very dark grey, bedded to massive; stylobrecciated; minor chert conglomerate, mudstone; deep-marine mass flow deposits. ||||||
24873|Coopers Creek Limestone|64605|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Jordan River Group. Limestone; deep-marine deposits. Blue-green in RGB.  Nonmagnetic.||||||17-NOV-08
24873|Coopers Creek Limestone|64616|3|Fully described|p99, p164, p294, p304, p385 Tb.1, p386|Emsian|Pragian|Of Jordan River Group. Replaces the limestone facies in the former Coopers Creek Formation (see p92, p254) of Philip (1962). Only in Tyers Anticline. Irregular contact with underlying Boola Formation. Faulted contact with Walhalla Group in west. Thickness uncertain. Rich, diverse shelly fauna. Conodonts give age. Dark grey, bedded to massive, stylobrecciated limestone; minor basal chert conglomerate, mudstone. Geophysical characteristics given.||||||
24873|Coopers Creek Limestone|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Walhalla. Appears in text as Coopers Ck Limestone. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
24873|Coopers Creek Limestone|65900|6|Mentioned|p171||Devonian|Shallow marine strata, contains clasts of probable Cambrian mafic rocks.||||||10-MAY-12
24873|Coopers Creek Limestone|65940|6|Mentioned|p204|Pragian|Pragian|Typers, VIC. Contains Phillipsastrea maculosa (perbonus-gronbergi Zone, Mawson and Talent, 2000), Cyathophyllum cresswelli (Sterictophyllum sp.) (Pragian, sulcatus to possibly dehiscens Zones; Mawson and Talent, 2000).||||||
24873|Coopers Creek Limestone|66498|6|Mentioned|p43|||Tyers-Boola region, VIC. Has a diverse assemblage with acanthodian taxa.||||||
24873|Coopers Creek Limestone|68116|5|Briefly described|Appendix, Map 52.|Emsian|Pragian||||||Limestone: mid- to very dark grey; bedded to massive; stylobrecciated; minor chert conglomerate, mudstone; lower well-bedded facies of biomicrite and sparite overlain by upper facies of massive wackestone; fossiliferous.|
24873|Coopers Creek Limestone|68297|5|Briefly described|p189|Devonian|Devonian|Vic. Includes acanthodian scales now known to be common from the Late Silurian to Early Devonian. See also Coopers Creek Beds, same page, Coopers Creek Formation p191.||||||
24873|Coopers Creek Limestone|73143|6|Mentioned|p11-12|Emsian|Pragian|Minimum age of basal Emsian. Contains Favosites allani tabulate coral (Philip, 1962) and F. grandipora (Chapman, 1921).||||||
30515|Coopracambra Tonalite|22878|4|Described|p73|||||||||
30515|Coopracambra Tonalite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Hornblende-biotite tonalite: dark grey green, coarse grained, massive; strongly porphyritic in quartz and feldspar; strongly altered.||||||01-OCT-04
30515|Coopracambra Tonalite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Hornblende-biotite tonalite: dark grey green, coarse grained, massive; strongly porphyritic in quartz and feldspar; strongly altered.||||||01-OCT-04
30515|Coopracambra Tonalite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Hornblende-biotite tonalite: Non-magnetic. High K, low Th and U||||||06-OCT-04
30515|Coopracambra Tonalite|23309|6|Mentioned|p428 App1|||G533.||||||
30515|Coopracambra Tonalite|68116|5|Briefly described|Appendix, Map 37.|Early Devonian|Early Devonian||||||Hornblende-biotite tonalite: dark grey green, coarse grained, massive; strongly porphyritic in quartz and feldspar; strongly altered.|
30515|Coopracambra Tonalite|68592|6|Mentioned|p1674|Early Devonian|Early Devonian|||Unit in Glenbog Supersuite.||||
4633|Coorabin Coal Measures|22773|5|Briefly described|Fig24.5p350|Late Permian|Late Permian|||||||
4633|Coorabin Coal Measures|22857|5|Briefly described|p518 App.1 Tb.A1.9||Late Permian|Includes the Nowranie Creek, Loughmore and Narrow Plain Formations. Geological Province: Ovens Graben of the Tasman Epicratonic Province. See also p350 Fig.24.5..||||||
4633|Coorabin Coal Measures|22893|6|Mentioned|fig4 p9|Late Permian|Late Permian|||||||
4633|Coorabin Coal Measures|23836|5|Briefly described|p93|Late Permian|Late Permian|Geological Province: Murray Basin.||||||
4633|Coorabin Coal Measures|24551|6|Mentioned|p212|Late Permian|Late Permian|||||||
4633|Coorabin Coal Measures|32315|6|Mentioned|Fig. 2|||||||||
4633|Coorabin Coal Measures|34418|5|Briefly described|p502|||||||||
4633|Coorabin Coal Measures|35498|3|Fully described|p142|||New units defined on P144||||||
4633|Coorabin Coal Measures|35767|6|Mentioned|p31|||||||||
4633|Coorabin Coal Measures|36172|6|Mentioned|Appendix|||||||||
4633|Coorabin Coal Measures|36329|6|Mentioned|p62|||||||||
4633|Coorabin Coal Measures|37065|6|Mentioned|p35|||||||||
4633|Coorabin Coal Measures|37101|4|Described|p261|||||||||
4633|Coorabin Coal Measures|38293|4|Described|p20|||||||||
4633|Coorabin Coal Measures|39929|6|Mentioned|p276|||||||||
4633|Coorabin Coal Measures|40324|6|Mentioned|p53|||||||||
4633|Coorabin Coal Measures|40520|6|Mentioned|Fig.5|||||||||
4633|Coorabin Coal Measures|41226|6|Mentioned|Table 1|||||||||
4633|Coorabin Coal Measures|42454|6|Mentioned|p19|||Oaklands Basin.||||||
4633|Coorabin Coal Measures|42547|5|Briefly described|p83|||||||||
4633|Coorabin Coal Measures|42648|5|Briefly described|p39|||||||||
4633|Coorabin Coal Measures|42966|4|Described|p64|||||||||
4633|Coorabin Coal Measures|43218|5|Briefly described|p27||Late Permian|Ovens Graben.||||||
4633|Coorabin Coal Measures|43841|4|Described|8||Late Permian|Unconformable over Urana Fm, unconformable under Jerilderie Fm. Mostly coal that totals up to 20m.||||||
4633|Coorabin Coal Measures|44340|14|Not recorded|p.3,4||Permian|I/55-14.||||||
4633|Coorabin Coal Measures|44341|14|Not recorded|map legend||Permian|Shale and mudstone with coal sandstone bands.||||||
4633|Coorabin Coal Measures|49040|6|Mentioned|p12|||||||||
4633|Coorabin Coal Measures|61314|5|Briefly described|p128|Late Permian|Late Permian|Upward-fining sequence of conglomerate, sandstone, siltstone, mudstone, carbonaceous clay and coal. Overlain by the Jerilderie Formation. Geological Province: Murray Basin.||||||
4633|Coorabin Coal Measures|69798|5|Briefly described|p4, p7, p11-18|Late Permian|Early Permian|Oaklands Basin. Seismic profiles. Late Permian. Fine-grained units in the upper part provide a seal for lower reservoirs. Fluvial-point bar depositional environment.|||Nowranie Creek, Loughmore, Narrow Plain, Formations.|Unconformably overlies the Urana Formation. Is overlain disconformably by Jerilderie Formation.||06-FEB-18
4633|Coorabin Coal Measures|70125|5|Briefly described|p396|Permian|Permian|Oaklands Basin. 80m thick.||||Overlies Urana Formation. Is overlain by Jerilderie Formation.||
4688|Copperhead Volcaniclastic Member|22968|6|Mentioned|P111|||Of the Thorkidaan Volcanics.||||||05-SEP-05
4688|Copperhead Volcaniclastic Member|23021|5|Briefly described|Map legend|Ludlow|Ludlow|Of the Thorkidaan Volcanics. Overlain by Cowombat Siltstone.||||||17-APR-07
4688|Copperhead Volcaniclastic Member|23309|5|Briefly described|p92 Table 2.31|||||||||
4688|Copperhead Volcaniclastic Member|24551|5|Briefly described|p135|||Of the Thorkidaan Volcanics.||||||
4688|Copperhead Volcaniclastic Member|41585|6|Mentioned|p127|||||||||
4688|Copperhead Volcaniclastic Member|42827|6|Mentioned|p127|||||||||
4688|Copperhead Volcaniclastic Member|60503|5|Briefly described|p108, p15, p28 Fig. 9|Silurian|Silurian|Of the Thorkidaan Volcanics. Comprises an assortment of polymict clasts and matrix-supported rhyolite breccia, sandstone, siltstone and minor cobble conglomerate with clasts mainly of lava fragments but with lesser component of pumiceous debris. ||||||
4688|Copperhead Volcaniclastic Member|60504|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Thorkidaan Volcanics (Enano Group). Polymict breccia, pebbly sandstone, siltstone and minor conglomerate with clasts of rhyolite lava; rhyolitic pyroclastics and quartzite.||||||05-SEP-05
4688|Copperhead Volcaniclastic Member|60505|5|Briefly described|Map legend|Ludlow|Ludlow|Of the Thorkidaan Volcanics (Enano Group). Polymict breccia, pebbly sandstone, siltstone and minor conglomerate with clasts of rhyolite lava; rhyolitic pyroclastics and quartzite.||||||05-SEP-05
4688|Copperhead Volcaniclastic Member|60506|5|Briefly described|Map legend|Ludlow|Ludlow|Of the Thorkidaan Volcanics (Enano Group). Polymict breccia, pebbly sandstone, siltstone and minor conglomerate with clasts of rhyolite lava; rhyolitic pyroclastics and quartzite.||||||05-SEP-05
4688|Copperhead Volcaniclastic Member|60507|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Thorkidaan Volcanics (Enano Group). Polymict breccia, pebbly sandstone, siltstone and minor conglomerate with clasts of rhyolite lava; rhyolitic pyroclastics and quartzite.||||||05-SEP-05
37266|Corduroy Creek Gabbro|23309|5|Briefly described|p25, 28, Table 2.1/2.4|Cambrian|Cambrian|Underlies: Digger Island Marlstone (Unconformably).||||||
37266|Corduroy Creek Gabbro|24002|5|Briefly described|p231|Cambrian||||||||
37266|Corduroy Creek Gabbro|24098|5|Briefly described|p27 Fig. 2, p30|Early Cambrian|Proterozoic|Unconformably underlies Bear Gully Chert and Digger Island Marlstone. Geological Province: Melbourne Zone, Lachlan Fold Belt (Waratah Bay Platform).||||||19-APR-05
37266|Corduroy Creek Gabbro|24551|5|Briefly described|p89|||||||||
30575|Cornella Member|23309|5|Briefly described|p138||Early Devonian|||||||
30575|Cornella Member|24177|4|Described|p54, p50 Fig.22|Lochkovian|Lochkovian|Of the Mount Ida Formation. Overlain by the Dealba Member. Geological Province: Darraweit Guim Province.||||||
30575|Cornella Member|24329|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent: Mount Ida Formation.||||||27-OCT-08
30575|Cornella Member|24551|6|Mentioned|p615|||||||||
30575|Cornella Member|60591|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Mount Ida Formation. Overlain by the Dealba Member. Overlies McIvor Sandstone. Consists of fine-grained sandstone, siltstone; shelly fossils.||||||14-APR-08
30575|Cornella Member|60592|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Mount Ida Formation. Overlain by the Dealba Member. Overlies McIvor Sandstone. Consists of fine-grained sandstone, siltstone; shelly fossils||||||25-NOV-04
30575|Cornella Member|60593|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Mount Ida Formation. Overlain by the Dealba Member. Overlies McIvor Sandstone. Consists of fine-grained sandstone, siltstone; shelly fossils.||||||27-OCT-08
30575|Cornella Member|60595|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Mount Ida Formation. Overlain by the Dealba Member. Overlies McIvor Sandstone. Consists of fine-grained sandstone, siltstone; shelly fossils.||||||14-APR-08
30575|Cornella Member|60596|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Mount Ida Formation. Overlain by the Dealba Member. Overlies McIvor Sandstone. Consists of fine-grained sandstone, siltstone; shelly fossils.||||||14-APR-08
30575|Cornella Member|60599|2|Defined|p31 Fig. 9, p61|Early Devonian|Early Devonian|Of Mount Ida Fm. Encompasses early Spirifer Beds (Thomas 1937). Thickly bedded turbidite sequence - fine-gr.sst+siltst. beds, many heavily iron-stained and variably quartz cemented; claystone beds also. Conf.on McIvor Sst; underlies Dealba Sst Mbr.||||||10-NOV-08
30575|Cornella Member|61185|5|Briefly described|p21 Fig. 6|Lochkovian|Lochkovian|Of Mount Ida Formation. Underlies Dealba Member. Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
30575|Cornella Member|62469|5|Briefly described|p5 Fig. 2, p16, p15|Pridoli|Ludlow|Of the Mount Ida Formation. Geological Province: Darraweit Guim Province.||||||12-FEB-15
4755|Corryong Granite|23309|5|Briefly described|p338, 346||Silurian|G92 - S-Type.  Age: 404 Ma, 429 Ma, 421+/-3 Ma.||||||
4755|Corryong Granite|24133|3|Fully described|p59|Silurian|Silurian|Age: 421+/-3Ma.  Geological Province: Lachlan Fold Belt.||||||
4755|Corryong Granite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
4755|Corryong Granite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
4755|Corryong Granite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
4755|Corryong Granite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Two-mica cordierite granite: grey, medium to very course grained; equigranular to strongly porphyritic in K-feldspar; locally contains sillimanite or andalusite.||||||09-SEP-04
4755|Corryong Granite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Age: 421 +/- 3 Ma (K/Ar). Biotite-muscovite-cordierite granite: S-type, nonmagnetic; high K, high Th, moderate to high U.||||||09-SEP-04
4755|Corryong Granite|24551|6|Mentioned|p445, 464|||S-Type||||||
4755|Corryong Granite|29860|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
4755|Corryong Granite|29953|4|Described|p3|||||||||
4755|Corryong Granite|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
4755|Corryong Granite|29994|6|Mentioned|Map legend|Silurian|Silurian|||||||
4755|Corryong Granite|31800|5|Briefly described|p207|||||||||
4755|Corryong Granite|33004|6|Mentioned|p167|||||||||
4755|Corryong Granite|33874|5|Briefly described|p6|||||||||
4755|Corryong Granite|34544|6|Mentioned|p183|||||||||
4755|Corryong Granite|35278|4|Described|p358|||||||||
4755|Corryong Granite|37029|6|Mentioned|p48|||||||||
4755|Corryong Granite|37529|6|Mentioned|Fig.1|||||||||
4755|Corryong Granite|38367|5|Briefly described|p153|Silurian|Silurian|Age: 430m.y. Grey granite.||||||16-DEC-08
4755|Corryong Granite|38782|6|Mentioned|p43|||||||||
4755|Corryong Granite|39291|6|Mentioned|Fig.20|||||||||
4755|Corryong Granite|39331|5|Briefly described|p27|||||||||
4755|Corryong Granite|39860|5|Briefly described|p17|||See also p22.||||||26-MAY-08
4755|Corryong Granite|40328|6|Mentioned|p204|||||||||
4755|Corryong Granite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
4755|Corryong Granite|40498|6|Mentioned|p364|||||||||
4755|Corryong Granite|41572|6|Mentioned|p19|||||||||
4755|Corryong Granite|41868|6|Mentioned|p569|||||||||
4755|Corryong Granite|42089|6|Mentioned|p19|||||||||
4755|Corryong Granite|42726|5|Briefly described|map legend|Silurian||||||||
4755|Corryong Granite|42827|5|Briefly described|p19|||||||||
4755|Corryong Granite|44184|5|Briefly described|Map Legend||Early Silurian|||||||
4755|Corryong Granite|45087|5|Briefly described|p27|||Chem. analyses.||||||
4755|Corryong Granite|50542|6|Mentioned|p91, p96|Silurian|Silurian|||||||07-FEB-11
4755|Corryong Granite|60085|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
4755|Corryong Granite|64571|6|Mentioned|p825|Early Silurian|Early Silurian|||||||
4755|Corryong Granite|68116|5|Briefly described|Appendix, Map 20.|Pridoli|Wenlock||||||Two-mica cordierite granite: grey, medium to very coarse grained; equigranular to strongly porphyritic in K-feldspar; locally contains sillimanite or andalusite; S-type.|
4755|Corryong Granite|70910|6|Mentioned|p47|||Example of gneissic granite p43.||||||
4769|Costerfield Siltstone|22511|5|Briefly described|p660, p661||Silurian|||||||
4769|Costerfield Siltstone|22542|6|Mentioned|p664|||||||||
4769|Costerfield Siltstone|22684|4|Described|p750, Fig.2 p746|Wenlock|Wenlock|||||||
4769|Costerfield Siltstone|22886|6|Mentioned|p12|||||||||
4769|Costerfield Siltstone|23229|4|Described|Table3-3p26, 28|Llandovery|Llandovery|||||||
4769|Costerfield Siltstone|23309|5|Briefly described|p137, Table2.49, p150|Wenlock|Wenlock| Maximum thickness >600m.||||||14-APR-08
4769|Costerfield Siltstone|24177|4|Described|p48, p50 Fig. 52|Early Silurian|Late Ordovician|Overlain by the Wapentake Formation. Geological Province: Melbourne Trough. Includes the "Illaenus Band" at the top of the formation.||||||
4769|Costerfield Siltstone|24328|5|Briefly described|Map legend|Early Silurian|Early Silurian|||||||
4769|Costerfield Siltstone|24329|5|Briefly described|Map legend|Early Silurian|Early Silurian|||||||
4769|Costerfield Siltstone|24551|6|Mentioned|p447|Early Silurian|Early Silurian|||||||
4769|Costerfield Siltstone|24588|5|Briefly described|p12 Fig.3|Llandovery|Llandovery|Geological Province: Darraweit Guim Province.||||||29-NOV-13
4769|Costerfield Siltstone|33604|6|Mentioned|p17|||Correlation chart. Sil.||||||
4769|Costerfield Siltstone|35283|4|Described|p47|||||||||
4769|Costerfield Siltstone|37727|4|Described|p48|||Formerly Costerfield Beds.||||||14-APR-08
4769|Costerfield Siltstone|38378|6|Mentioned|Fig.1|||||||||
4769|Costerfield Siltstone|39331|6|Mentioned|Table 2-1|||||||||
4769|Costerfield Siltstone|41585|5|Briefly described|p105|||||||||
4769|Costerfield Siltstone|42827|5|Briefly described|p105|||see also Table 4.1||||||
4769|Costerfield Siltstone|60599|6|Mentioned|p20, p24 Tb. 4, p47-49, p13|Llandovery|Llandovery|Supersedes Costerfield beds, Costerfield Formation. Includes Illaenus Band at top. Burrowed siltstone, laminated to thinly bedded. Gradationally overlain by Wapentake Formation. Thickness: >600m.||||||27-OCT-08
4769|Costerfield Siltstone|61185|5|Briefly described|p10, p13, p21 Fig. 6|Llandovery|Llandovery|Includes Illaenus Band at top. Dark grey and extensively bioturbated mud-dominated sediments containing burrowing organisms. Also mentioned in text as informal "Costerfield and Deep Creek siltstones".||||||07-FEB-11
4769|Costerfield Siltstone|62469|5|Briefly described|p5 Fig. 2, p15|Wenlock||Geological Province: Darraweit Guim Province.||||||12-FEB-15
4769|Costerfield Siltstone|63083|5|Briefly described|p215, p216 Tb. 1|Llandovery|Llandovery|Underlies Wapentake Formation. Supersedes Costerfield Sandstone. Only one fossil recorded - a poorly preserved thorax specimen of Dalmanitina. See also p230 Fig. 9.||||||07-FEB-11
4769|Costerfield Siltstone|64612|5|Briefly described|p27, p38|Early Llandovery|Early Llandovery|Of Murrindindi Supergroup. Contains burrows.||||||07-FEB-11
4769|Costerfield Siltstone|68116|5|Briefly described|Appendix, Map 24.|Sheinwoodian|Telychian||||||Monotonous sequence of laminated to thinly bedded siltstone, minor sandstone towards top, in part pyritic; intensely bioturbated; sparse fossils include crinoid ossicles and a trilobite fragment; deep-marine hemipelagic deposit.|
4769|Costerfield Siltstone|69089|5|Briefly described|Map legend|Early Silurian|Early Silurian||||||Marine: siltstone, thin-bedded; minor sandstone, conglomerate.|
4769|Costerfield Siltstone|73497|5|Briefly described|Map legend|Silurian|Silurian|Marine.||Murrindindi Supergroup|||Siltstone, minor sandstone: weakly magnetic; high K and U, and moderate-high Th.|
4785|Council Trench Formation|22886|5|Briefly described|p16|Triassic|Triassic|||||||
4785|Council Trench Formation|23258|5|Briefly described|Fig12-3.1p214, 215||Triassic|||||||
4785|Council Trench Formation|24551|6|Mentioned|p565||Late Triassic|||||||
4785|Council Trench Formation|39865|4|Described|p22|||||||||
4785|Council Trench Formation|44197|5|Briefly described|Map Legend||Triassic|||||||
4785|Council Trench Formation|62897|4|Described|p113-114, p115 Fig. 1|Triassic|Triassic|Of Roberts (1984). Corresponds to "upper beds at Bald Hill" assigned Triassic age by Chapman (1927). Disconformable on Bacchus Marsh Sst; overlain by Pentland Hills Volcs+Werribee Fm. Max. thick: ~12m. Conglom./sst/conglom. Includes detailed lithology.||||||18-MAR-08
4785|Council Trench Formation|63741|2|Defined|p113-127|Triassic|Triassic|Of Roberts (1984) here defined by authors. Disconformable on Bacchus Marsh Sst; overlain by Pentland Hills Volcs+Werribee Fm. Once known as "upper beds at Bald Hill" (Chapman 1927). Max.thickness: ~12m. Type section. Interbedded ssts, congloms., siltsts.||||||
4785|Council Trench Formation|64532|6|Mentioned|p375 fig 1|Triassic|Triassic|||||||
4785|Council Trench Formation|65715|5|Briefly described|p9 Tb.6|Mesozoic|Mesozoic|Map symbol implies probable Triassic age.||||||
4785|Council Trench Formation|68116|5|Briefly described|Appendix, Map 41.|Jurassic|Triassic||||||Sandstone, conglomerate: cream to brown; sandstone feldspathic; contains conglomerate as lenses to pebble trains; pebbles of dark grey quartz and minor lithic material; fragmentary plant fossils.|
77691|Cove Sand|68991|4|Described|p465 Fig.2, pp468-469, p471 Fig.5|Pleistocene|Pleistocene|Middle Pleistocene age. Named after Childers Cove Road. ~ 0-5 m thick. Proposed in this study to have a dominantly eolian origin with minor alluvial input. Type section details given.|203 +/- 16 ka|||Disconformably underlain by the Dog Trap Bay Sand.|Comprises poorly consolidated, red, fine to medium quartz sand, with well frosted quartz grains and minor subangular fine and coarse quartz sands.|
25864|Cowombat Siltstone|22968|4|Described|P84, Fig49, P113||Late Silurian|Parent is Enano Group, maximum thickness is 800m, conformable to disconfomably underlain by the Thorkidaan Volcanics.||||||25-SEP-08
25864|Cowombat Siltstone|23021|5|Briefly described|Map legend|Pridoli|Ludlow|Parent is Enano Group, overlying unit is Gibsons Folly Formation, underlying unit is Thorkidaan Volcanics||||||
25864|Cowombat Siltstone|23030|5|Briefly described|Map legend|Late Silurian|Late Silurian|Parent is the Enano Group.||||||25-SEP-08
25864|Cowombat Siltstone|23309|6|Mentioned|p92, 307|||||||||
25864|Cowombat Siltstone|23615|3|Fully described|p82, p20 Fig.6|Pridoli|Ludlow|Includes the Lobelia, Farquhar and Caladenia Limestone lenses.||||||
25864|Cowombat Siltstone|23938|5|Briefly described|p14 Tb. 1, p139 Tb.1 App.|Late Silurian|Middle Silurian|Of Enano Gp. Marine lithology. Overlies the Thorkidaan Vols, conformably to disconformably; conformably overlain by Gibsons Folly Fm. In Limestone Creek Graben. See also p38-39 Tb. 2, p77, p82.||||||
25864|Cowombat Siltstone|24275|4|Described|p1695, p1697 Fig. 3, p1698 Tb. 1|Late Silurian|Silurian|Of the Enano group. Fossiliferous grey, black and green siltstone; minor conglomerate, limestone and sandstone composed of mixed rhyolite, limestone and quartz sandstone debris.  Conformably overlain by Gibsons Folly Formation. Geol.Prov: LFB.||||||15-SEP-05
25864|Cowombat Siltstone|24551|4|Described|p128, p135|Late Silurian|Late Silurian|Of Enano Group. Includes Mount Walterson Conglomerate Member.||||||
25864|Cowombat Siltstone|33606|6|Mentioned|p64|||||||||
25864|Cowombat Siltstone|35283|6|Mentioned|p49|||||||||
25864|Cowombat Siltstone|38145|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
25864|Cowombat Siltstone|38151|6|Mentioned|Table 1|||||||||
25864|Cowombat Siltstone|38367|6|Mentioned|Fig.9.|||||||||
25864|Cowombat Siltstone|39447|2|Defined|p8|Silurian|Silurian|See also p24||||||16-AUG-18
25864|Cowombat Siltstone|39860|6|Mentioned|p10|||See also P30||||||
25864|Cowombat Siltstone|40761|6|Mentioned|p227|||||||||
25864|Cowombat Siltstone|41585|4|Described|p128|||Mention Fig.4.5||||||
25864|Cowombat Siltstone|42827|4|Described|p128|||Of Enano Group.||||||25-SEP-08
25864|Cowombat Siltstone|43128|5|Briefly described|Fig.6,p476|||||||||
25864|Cowombat Siltstone|43206|5|Briefly described|map legend||Wenlock|Of Enano Group||||||
25864|Cowombat Siltstone|43770|5|Briefly described|p831|||||||||
25864|Cowombat Siltstone|44092|5|Briefly described|map legend|Late Silurian|Late Silurian|Ss4||||||
25864|Cowombat Siltstone|44184|5|Briefly described|Map Legend||Late Silurian|||||||
25864|Cowombat Siltstone|44185|5|Briefly described|Map legend.|Late Silurian|Late Silurian|||Unit in Enano Group.|||Marine: siltstone, laminated, minor sandstone, limestone lenses.|
25864|Cowombat Siltstone|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
25864|Cowombat Siltstone|60504|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Enano Group.||||||
25864|Cowombat Siltstone|60505|5|Briefly described|Map legend|Pridoli|Ludlow|Of the Enano Group.||||||25-SEP-08
25864|Cowombat Siltstone|60506|5|Briefly described|Map legend|Pridoli|Ludlow|Of the Enano Group.||||||
25864|Cowombat Siltstone|60507|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Enano Group.||||||07-OCT-04
25864|Cowombat Siltstone|60508|5|Briefly described|Map legend|Late Silurian|Late Silurian|Of the Enano Group. Siltstone, sandstone, limestone, conglomerate: nonmagnetic cut by northeast, north and west-northwest weakly magnetic (10-20 nT) trends; moderate to high total count K, Th, low U||||||21-OCT-04
25864|Cowombat Siltstone|61181|5|Briefly described|p122, p172|Silurian|Silurian|Of the Enano Group. Interbedded with lenses of Enano Group limestones. ||||||
25864|Cowombat Siltstone|61187|5|Briefly described|p24, p26 Fig.2, p28, p29 Fig.4. |Silurian|Silurian|Thickness to 500 m. Radiometric response varies considerably along strike.||Unit in Enano Group.|||Four facies in decreasing abundance: siltstone and mudstone; sandstone and breccia; limestone; conglomerate.|
25864|Cowombat Siltstone|66197|5|Briefly described|p635 Fig.5c|Late Silurian||Buchan Basin. Deep marine shale. Underlies the Gibsons Folly Formation, overlies the Thorkidaan Volcanics. Age: Pridoli?||||||14-MAR-12
25864|Cowombat Siltstone|68116|5|Briefly described|Appendix, Maps 27-28, 35-36.|Pridoli|Pridoli||||||Siltstone: grey, black and green; interbedded with subordinate sandstone, conglomerate and lenses of limestone.|
37713|Coynallan Tonalite|23309|6|Mentioned|p428, App 1|||G579, I-type.||||||
37713|Coynallan Tonalite|24133|3|Fully described|p73|Early Devonian|Late Silurian|Parent: Surveyors Creek Suite.  Geological Province: Lachlan Fold Belt.||||||
37713|Coynallan Tonalite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Of Surveyors Creek Suite. Geological Province: Lachlan Fold Belt.||||||
37713|Coynallan Tonalite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Of Surveyors Creek Suite. Geological Province: Lachlan Fold Belt.||||||
37713|Coynallan Tonalite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Of Surveyors Creek Suite. Geological Province: Lachlan Fold Belt.||||||
37713|Coynallan Tonalite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Of Surveyors Creek Suite.  Geological Province: Lachlan Fold Belt. Hornblende tonalite: medium grained equigranular to coarse and porphyritic; massive to foliated; numerous round mafic enclaves to several metres across; I-type||||||10-SEP-04
37713|Coynallan Tonalite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Of Surveyors Creek Suite. Geological Province: Lachlan Fold Belt. Hornblende tonalite: I-type; weakly to moderately magnetic; low K, Th, U.||||||10-SEP-04
37713|Coynallan Tonalite|68116|5|Briefly described|Appendix.|Pridoli|Wenlock||||||Hornblende tonalite: medium grained equigranular to coarse and porphyritic; massive to foliated; numerous round mafic enclaves to several metres across; I-type; weakly to moderately magnetic.|
29915|Crabhole Creek Limestone|43314|5|Briefly described|Map Legend||Llandovery|||||||
29915|Crabhole Creek Limestone|43315|5|Briefly described|Map Legend|Llandovery|Llandovery|Of the Yalmy Group. Undifferentiated limestone, pale grey (drill core only).||||||03-MAY-05
29915|Crabhole Creek Limestone|60541|4|Described|p56, p94|||Strongly foliated and predominantly composed of fine- to medium-grained calcite; typically impure with crenulated pelitic layers present; weakly carbonaceous in parts.||||||
4844|Cranbourne Sand|23262|5|Briefly described|Fig13-1.1p290, 292||Pleistocene|||||||
4844|Cranbourne Sand|23274|5|Briefly described|p449||Quaternary|||||||
4844|Cranbourne Sand|24551|6|Mentioned|p354|||||||||
4844|Cranbourne Sand|30929|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
4844|Cranbourne Sand|31510|6|Mentioned|Table 1|||On P5.||||||
4844|Cranbourne Sand|32002|6|Mentioned|p116|||||||||
4844|Cranbourne Sand|33237|6|Mentioned|p61|||||||||
4844|Cranbourne Sand|35290|6|Mentioned|p47|||||||||
4844|Cranbourne Sand|35366|6|Mentioned|p40|||||||||
4868|Crawford Member|31624|6|Mentioned|p129|||Unit of Whalers Bluff Fm.||||||
4868|Crawford Member|32767|6|Mentioned|p66|||||||||
4868|Crawford Member|33160|6|Mentioned|p304|||||||||
4868|Crawford Member|35066|6|Mentioned|p217|||||||||
4868|Crawford Member|42827|6|Mentioned|p291|||Of Whalers Bluff Formation.||||||01-JUL-08
4868|Crawford Member|48911|6|Mentioned|Chart 1|||||||||
4868|Crawford Member|63739|5|Briefly described|p54|Pleistocene|Late Pliocene|Of Whalers Bluff Formation. Contains ostracod assemblages (Loxoconcha sp.) at Myaring bridge.||||||01-JUL-08
4874|Crayfish Subgroup|22944|5|Briefly described|Fig3|||||||||
4874|Crayfish Subgroup|23911|4|Described|p93, p95 Fig. 9B|||Geological Province: Otway Basin.  Max. Thickness: >4500m. Underlain by Casterton Formation. Overlain by  Eumeralla Formation. Of the Otway Group.||||||14-APR-08
4874|Crayfish Subgroup|24453|4|Described|p808, p809 Fig.2|Hauterivian|Berriasian|Fluvial sandstones, conglomerates and minor silstones, coals, tuffs and basalt. Of Otway Group. Geological Province: Otway Basin.||||||07-FEB-11
4874|Crayfish Subgroup|24551|6|Mentioned|p245|||||||||
4874|Crayfish Subgroup|42361|4|Described|p4|||||||||
4874|Crayfish Subgroup|42545|5|Briefly described|Fig.4 P15|||||||||
4874|Crayfish Subgroup|43660|5|Briefly described|p14,Fig.6,p15||Early Cretaceous|||||||
4874|Crayfish Subgroup|43747|5|Briefly described|p5||Early Cretaceous|||||||
4874|Crayfish Subgroup|43814|6|Mentioned|Fig.3,p115|||||||||
4874|Crayfish Subgroup|50154|5|Briefly described|p44, p169|||Also known as Pretty Hill Formation. Of the Otway Group. Geological Province: Otway Basin.||||||24-AUG-04
4874|Crayfish Subgroup|61017|5|Briefly described|p5|Barremian|Bernasian|Of the Otway Group. Non-marine lacustrine to fluvial sediments. Unconformably overlain by Eumeralla Formation. Province: Otway Basin.||||||07-FEB-11
4874|Crayfish Subgroup|61182|6|Mentioned|p12|||May have superseded Crayfish Group?||||||18-FEB-08
4874|Crayfish Subgroup|61470|5|Briefly described|p28 Fig. 5|Barremian|Berriasian|Of the Otway Group.  Includes Pretty Hill and Laira Formations and the Katnook Sandstone. Geological Province: Otway Basin.||||||12-OCT-05
4874|Crayfish Subgroup|61628|5|Briefly described|p509 Fig. 3|Early Cretaceous|Early Cretaceous|Includes Katnook Sandstone, Pretty Hill and Laira Formations. Geological Province: Otway Basin.||||||
4874|Crayfish Subgroup|63269|5|Briefly described|p605|Early Cretaceous|Early Cretaceous|Otway Basin.||Otway Group.|Pretty Hill, Laira Formations; Katnook Sandstone.|||
4874|Crayfish Subgroup|65715|6|Mentioned|p10|||Includes conglomerate similar to Ballark Conglomerate.||||||
4874|Crayfish Subgroup|66245|5|Briefly described|p6 Fig.5, p42.|Barremian|Berriasian|Among the oldest sediments in the Otway Basin: locally-derived sands, and muds from a more distant source.||Unit in Otway Group.|Includes Pretty Hill and Laira Formations and Katnook Sandstone.|||
4874|Crayfish Subgroup|67367|5|Briefly described|p131 Fig.2, pp131-132. |Early Cretaceous|Early Cretaceous|Hydrocarbon source rocks, deposited in rifted half-grabens, for virtually all onshore hydrocarbons in South Australia. Assigned to the Austral 1 petroleum sub-system. ||Unit in Otway Group.|Includes Laira and Pretty Hill Formations, and Katnook Sandstone.|||
4874|Crayfish Subgroup|69297|6|Mentioned|p79|Aptian|Valanginian|Otway Basin. ||Otway Group|Includes the Casterton Formation, Sawpit Shale, Sawpit Sandstone, Pretty Hill Formation, Laira Formation and the Katnook Sandstone. |||
4874|Crayfish Subgroup|69651|5|Briefly described|p10|Early Cretaceous|Early Cretaceous|||Otway Group.|Pretty Hill, Laira Formations; Katnook Sandstone.|Unconformably overlies Casterton Formation. Is overlain unconformably by Eumeralla Formation.||
4874|Crayfish Subgroup|70077|5|Briefly described|Regional: Fig.4; p9|Early Cretaceous|Early Cretaceous|Otway Basin: Robe-Penola Trough. Source rocks of the Austral 1 Petroleum System.||Otway Group.|Sawpit Shale, Sawpit Sandstone, Pretty Hill and Laira Formations, Katnook Sandstone.|||
4874|Crayfish Subgroup|73356|6|Mentioned|p. v-2, p4, p11, p17, p29|||Otway Basin. Basal boundary is unconformable in many instances (cf. Warrong Trough) but is shown to be conformable in the Sawpit-1 well (Penola Trough).||Otway Group|Sawpit Formation, Pretty Hill Formation, Laira Formation, Katnook Sandstone|Underlain by Casterton Formation. Unconformably overlain by Windermere Sandstone.||
4874|Crayfish Subgroup|73357|6|Mentioned|p17, p43, p45, p47|Barremian|Berriasian|Otway Basin.||Otway Group|Includes Pretty Hill Formation|||
4874|Crayfish Subgroup|73383|4|Described|p3-4, p6, p7 Tb.3.1, p15-16, p25, p27|Barremian|Berriasian|Otway Basin. Approximately equivalent to chemostratigraphic Sequence S1, defined by generally higher Cr/Mg and lower Y/Nb and Ti/Cr values than the overlying Sequence S2. Significant lateral variation in lithology. May contain intra-formation unconformities based on large and abrupt geochemical changes. Lithologies based on geochemistry using the ChemLith classification includes mudstone, argillaceous and calcareous sandstone, limestone, calcareous limestone; and using the Herron classification (1988) includes shale, Fe-sand, Fe-shale, wacke, lith-arenite. See also vi, p1, p8, p11, p126-129, p253-256.||Otway Group|Pretty Hill Formation, Laira Formation, Katnook Sandstone|Overlies Casterton Formation, unconformably underlies Eumeralla Formation|Includes fluvial channel sandstones, lacustrine mudstones and alluvial sandstone. Both arkosic and lithic-rich.|
4874|Crayfish Subgroup|73385|5|Briefly described|p3, p5-6, p9, p12 Fig.4.9, p16|Barremian|Valanginian|Otway Basin. Deposited in predominantly NW-SE grabens and half-grabens of limited extent, deposition facilited by a series of lakes within individual depocentres, that became linked to a fluvio-lacustrine system. Crayfish Subgroup isopach grid used to define Early Cretaceous depocentres and highs. Location in text includes p15 Fig.4.13.||Otway Group|Laira Formation, Pretty Hill Formation, Katnook Sandstone|Overlies Casterton Formation, underlies Eumeralla Formation, Windermere Sandstone.|Includes fluvial channel sandstones, lacustrine mudstones and alluvial sandstone. Primarily comprised of locally derived sands and far-sourced muds.|
4874|Crayfish Subgroup|73386|4|Described|p1-2, p4-9, v, Attachment A1|Barremian|Berriasian|Otway Basin. Latest Berriasian maximum age. Conformable with Casterton Formation in the western Victorian Otway Basin, unconformable in the central basin. Primarily of fluvial and lacustrine depositional environments, syn-rift sequence and deposited in half grabens in the northern and western onshore Otway Basin. Limited available evidence suggests it is unlikely the Crayfish Subgroup is present offshore beyond areas adjacent to the coast. Corresponds to the Upper Ruffordiaspora australiensis to Upper Foraminisporis wonthaggiensis Spore-Pollen subzones of Partridge (2006), and the S1 chemostratigraphic sequence (Forbes et al., 2020).||Otway Group|Laira Formation, Pretty Hill Formation, Sawpit Formation, Katnook Sandstone|Overlies Casterton Formation, unconformably underlies Eumeralla Formation, Windermere Sandstone, equivalent to the Crayfish Group in South Australia|Sequence of sandstones, siltstones and shales.|
4874|Crayfish Subgroup|73594|4|Described|p3-4, p36, p38, p41-46, p49-50, p52|Barremian|Berriasian|Otway Basin. Deposited in a series of half-grabens with the stratigraphy of each depocentre likely unique. Low-relief erosional surface forms the boundary with the Eumeralla Formation. Originally Crayfish Group (Kopsen and Scholefield (1990), renamed by Morton (1990) to Crayfish Subgroup and divided into four sub-ubits based on seismic character.||Otway Group|Katnook Sandstone, Pretty Hill Formation, Laira Formation|Overlies Casterton Formation, unconformably underlies Eumeralla Formation, Windermere Sandstone|Fluvial channel sandstones, lacustrine mudstones and alluvial sandstones.|
4874|Crayfish Subgroup|75065|6|Mentioned|p157|||Otway Basin.||||Correlates with Tyers River Subgroup.||
73284|Crayfish Supersequence|63134|2|Defined|101|||||||||
73284|Crayfish Supersequence|63269|5|Briefly described|p605, p609, p616, p618, p622-624|Early Cretaceous|Early Cretaceous|Otway Basin. Oil-source correlation.|||Casterton Formation and Crayfish Subgroup.|Is overlain by Eumeralla Supersequence.||
73284|Crayfish Supersequence|69297|6|Mentioned|p77, p80, p81, p82, p96-p100, p110|Lower Cretaceous|Upper Jurassic|Nelson Sub-basin of the Otway Basin. Deposited in a fluvial or lacustrine environment. Interpreted from seismic data. ||||||
73284|Crayfish Supersequence|69651|5|Briefly described|p6, p10, p12-15, p17-19, p23, p25, p31||Early Cretaceous|See also p36-38, p40, p42-44, p47, p49-50. Krassay et al. (2004). Otway Basin. Part of the Otway Supergroup. Potential source rocks. Fluvial to lacustrine deposits. Modelling diagrams.||||Is overlain by Eumeralla Supersequence.|Argillaceous sandstone with interbedded claystone.|
73284|Crayfish Supersequence|70077|5|Briefly described|Nelson:p1. Regional: Fig.4; p3-4, p6, p9|Early Cretaceous|Early Cretaceous|Non-marine, fluvio-lacustrine deposits (shales and coals). A thick growth wedge in the ENE-trending Nerita Trough. Good potential source rocks.||||||
73284|Crayfish Supersequence|70078|6|Mentioned|Regional: Fig.4; p3-4|Early Cretaceous|Early Cretaceous|Hosts Austral 1 and part of Austral 2 petroleum systems.||||||
73284|Crayfish Supersequence|70880|5|Briefly described|p75-77, 82-83|Barremian|Tithonian|Otway Basin. Australia-Antarctica rifting produced E-W to NW-SE striking faults bounding horst-and-graben structures. Syn-rift deposition. Maximum thicknesses up to 5000m in northern onshore Basin.||||Is overlain unconformably by Eumeralla Supersequence.|Contains organic-rich mudstones, sandstones and some basalts.|
73284|Crayfish Supersequence|71266|5|Briefly described|p613-615, p617, p620, p622 Fig.10|Barremian|Tithonian|Contains the oldest known stratigraphic units in the Otway Basin. Syn-rift deposition. Up to 5000m thick in the northern, onshore part of the Basin. Affected by faults; their growth is discussed in great detail.||||Is overlain by Eumeralla Supersequence.|Organic-rich mudstones, sandstones and basalts.|
83251|Cretaceous/Paleogene boundary shale|73386|4|Described|p4-5, p12|Danian|Maastrichtian|Otway Basin. Formally referred to as the Massacre Shale, type section defined between 892 m and 917 m in Langley-1 (Partridge, 2001). Appears as Cretaceous/Paleogene Boundary Shale, p12. Represents first marine flooding over the Sherbrook Group. Late Maastrichtian to Danian in age, Upper Forcipites longus to Lower Lygistepollenites balmei spore-pollen subzones. Sharp boundary with underlying Timboon Sandstone.||Wangerrip Group||Unconformably overlies Timboon Sandstone, Sherbrook Group, underlies Pebble Point Formation.|Thin unit of silty shale to argillaceous fine-grained sandstone.|
4910|Croajingalong Granite|23309|5|Briefly described|p346||Early Devonian|G5 - I-Type.  Supersedes Croajingalong Adamellite||||||
4910|Croajingalong Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Croajingalong Adamellite, Vic.||||||
4910|Croajingalong Granite|68116|5|Briefly described|Appendix, Maps 37, 46.|Early Devonian|Early Devonian||||||Biotite granite: pink, coarse, porphyritic; rare microgranitoid enclaves.|
29708|Crohn Granite|23309|6|Mentioned|p428 App1|||G515.||||||
29708|Crohn Granite|23938|6|Mentioned|p55 Tb. 4|||||||||
29708|Crohn Granite|43312|5|Briefly described|Map Legend||Wenlock|G515. Tonalite, medium grained, porphyritic, green-grey, I-Type.||||||26-OCT-04
29708|Crohn Granite|43313|5|Briefly described|Map Legend||Wenlock|||||||
29708|Crohn Granite|60542|5|Briefly described|p96, p23 Tb. 2|Late Silurian|Late Silurian|The rock has been described both as a hornblende granite and as a quartz syenite. In the east is nonconformably overlain by Tara Range Subgroup ignimbrites. Type section is along Granite Creek.||||||
29708|Crohn Granite|68116|5|Briefly described|Appendix, Map 45.|Wenlock|Wenlock||||||Tonalite: medium-grained, porphyritic, green-grey.|
4939|Crosbie Granite|23309|6|Mentioned|p428 App 1|||G289 I-Type.||||||
4939|Crosbie Granite|24177|4|Described|p61, p35|Late Devonian|Late Devonian|Overlain by the Wild Duck Formation. Intrudes Castlemaine Group.||||||
4939|Crosbie Granite|24328|5|Briefly described|Map legend|Devonian|Devonian|||||||
4939|Crosbie Granite|24329|5|Briefly described|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
4939|Crosbie Granite|24551|6|Mentioned|p85|||||||||
4939|Crosbie Granite|35281|6|Mentioned|p21|||||||||
4939|Crosbie Granite|39676|6|Mentioned|p164|||||||||
4939|Crosbie Granite|41571|5|Briefly described|p47|||||||||
4939|Crosbie Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
4939|Crosbie Granite|42827|5|Briefly described|Fig 2.4|||||||||
4939|Crosbie Granite|60591|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Biotite granite: non-magnetic; medium- to coarse-grained, equigranular; composed of quartz, orthoclase, biotite.||||||27-OCT-08
4939|Crosbie Granite|60592|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Biotite granite: non-magnetic; medium- to coarse-grained, equigranular; composed of quartz, orthoclase, biotite.||||||27-OCT-08
4939|Crosbie Granite|60593|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Biotite granite: non-magnetic; medium- to coarse-grained, equigranular; composed of quartz, orthoclase, biotite.||||||27-OCT-08
4939|Crosbie Granite|60595|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Biotite granite: non-magnetic; medium- to coarse-grained, equigranular; composed of quartz, orthoclase, biotite.||||||27-OCT-08
4939|Crosbie Granite|60596|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Biotite granite: non-magnetic; medium- to coarse-grained, equigranular; composed of quartz, orthoclase, biotite.||||||27-OCT-08
4939|Crosbie Granite|60597|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Biotite granite: nonmagnetic, discontinuous moderately magnetic metamorphic aureole (10 nT); high K, low Th and U.||||||27-OCT-08
4939|Crosbie Granite|60599|4|Described|p24 Tb. 4, p102-103, p80, p83,p20, p35|Late Devonian|Late Devonian|Highly weathered, brown to grey, medium- to coarse-grained, equigranular, undeformed leucocratic granite. Contact metamorphic aureole developed in Knowsley East Shale and all formations of Heathcote Volcanics. Unconformably underlies Wild Duck Formation.||||||
4939|Crosbie Granite|61187|6|Mentioned|p103. |||The Mount Camel Copper Show lies within the aureole of this unit.||||||
4939|Crosbie Granite|65715|6|Mentioned|p7 Tb.4|||G289.||||||
4939|Crosbie Granite|65969|6|Mentioned|p19|||Non-magnetic. Hosts minor gold-stibnite mineralisation.||||||
4939|Crosbie Granite|68116|5|Briefly described|Appendix, Map 24.|Late Devonian|Late Devonian||||||Biotite granite: medium- to coarse-grained, equigranular; composed of quartz, orthoclase, plagioclase and biotite.|
4939|Crosbie Granite|73497|5|Briefly described|Map legend|Late Devonian|Late Devonian|G289.|||||Biotite granite: nonmagnetic, moderately magnetic metamorphic aureole (10 nT); high K, low Th and U; gravity low of 30 micrometres/second/second.|
30361|Cross Granite|23165|5|Briefly described|Map legend||Devonian|||||||
4959|Crowstick Diorite|39860|5|Briefly described|p22|||||||||
4959|Crowstick Diorite|68116|5|Briefly described|Appendix, Map 28.|Early Devonian|Llandovery||||||Hornblende-bearing quartz diorite.|
37537|Cudgewa Falls Volcanics|23309|6|Mentioned|p121|||||||||
37537|Cudgewa Falls Volcanics|24133|3|Fully described|p41|Devonian|Devonian|Parent: Mount Burrowa Volcanic Group.  Geological Province: Lachlan Fold Belt.||||||
37537|Cudgewa Falls Volcanics|24142|5|Briefly described|Map Legend|Devonian|Devonian|Of Mount Burrowa Volcanic Group. Geological Province: Lachlan Fold Belt.||||||
37537|Cudgewa Falls Volcanics|24143|5|Briefly described|Map Legend|Devonian|Devonian|Of Mount Burrowa Volcanic Group. Geological Province: Lachlan Fold Belt.||||||
37537|Cudgewa Falls Volcanics|24144|5|Briefly described|Map Legend|Devonian|Devonian|Of Mount Burrowa Volcanic Group. Geological Province: Lachlan Fold Belt.||||||
37537|Cudgewa Falls Volcanics|24145|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of Mount Burrowa Volcanic Group. Geological Province: Lachlan Fold Belt||||||
37537|Cudgewa Falls Volcanics|24551|5|Briefly described|p149|||Included as part of the Mount Burrowa Cauldron Complex.||||||
37537|Cudgewa Falls Volcanics|68116|5|Briefly described|Appendix, Map 20.|Middle Devonian|Early Devonian||||||Lava domes/flows and ignimbrite: dark crystal poor lava, massive to flow banded rhyolite; pale green and grey ignimbrite with variable pumice and crystal content; includes fine bands of pyroclastic surge deposits with abundant accretionary lapilli.|
5032|Cunninghame Greensand Member|24551|5|Briefly described|p327 Fig. 10.33|Oligocene|Oligocene|||||||
5032|Cunninghame Greensand Member|35273|4|Described|p258|||||||||
5032|Cunninghame Greensand Member|42827|6|Mentioned|p331|||of Lakes Entrance Formation||||||
5032|Cunninghame Greensand Member|61302|5|Briefly described|p5|Oligocene|Oligocene|Glauconitic sandstone; hosts crude oil. Capped by Lakes Entrance Formation. Geological Province: Gippsland Basin.||||||
5032|Cunninghame Greensand Member|65718|5|Briefly described|p10 Fig 3.2, p22, p43|Oligocene|Oligocene|||Of the Lakes Entrance Formation.||||
39339|Curlip Formation|13323|5|Briefly described|p393 Fig. 2|Turonian|Turonian|Youngest unit of Emperor Subgroup (Latrobe Group).  Alluvial, fluvial sandstones and thin fine-grained clastic beds that interfinger with and overlie Kipper Shale. Geological Province: Gippsland Basin.||||||26-JUN-06
39339|Curlip Formation|24090|5|Briefly described|p8 Fig.3|Cretaceous|Cretaceous|Geological Province: Gippsland Basin.||||||
39339|Curlip Formation|24407|5|Briefly described|p13 Fig.2|||Geological Province: Gippsland Basin||||||
39339|Curlip Formation|24551|5|Briefly described|p262 Fig. 9.29, 267|Late Cretaceous|Late Cretaceous|Of the Emperor Subgroup.  Overlies: Kipper Shale.||||||
39339|Curlip Formation|61552|6|Mentioned|p583 Fig.2. |Late Cretaceous|Late Cretaceous|||Unit in Emperor Subgroup.||||
39339|Curlip Formation|64876|5|Briefly described|p145 Fig.2|Turonian|Turonian|Gippsland Basin.||Emperor Subgroup.||||
39339|Curlip Formation|65717|5|Briefly described|p9 Fig.2.2, p10|Turonian|Cenomanian|Bernecker and Partridge (2001). Gippsland Basin.||Emperor Subgroup||Conformably overlies Admiral Formation, Kipper Shale (also interfingers with the latter).|Sandstones and conglomerates interbedded with thin shales and minor coals.|05-SEP-17
39339|Curlip Formation|65718|5|Briefly described|p11|Coniacian|Turonian|Bernecker and Partridge (2001). Fluvial-deltaic formation. Can exceed 300 m in thickness.||Of the Emperor Subgroup.||Underlain by and interfingered with the Kipper Shale.|Consists of sandstones and conglomerates that are interbedded with thin shales and minor coals.|
39339|Curlip Formation|65973|4|Described|p15, p28, p57-58, p76, p80|||Gippsland Basin. Deposited in a fluvial and partly lacustrine environment. Misspelt on p58 as the Curlip Arkose. Intersected in numerous drillholes including Kipper-1,  Hammerhead-1, Shark-1, Sole-1. See also p82, p86, p108, p110, p123, p125, p128-p130, p139-140, p171.||Emperor Subgroup.||Overlies and interfingers with the Kipper Shale.|Sandstones and conglomerates interbedded with thin shales and minor coals.|
39339|Curlip Formation|70028|6|Mentioned|p79|Turonian|Turonian|||||||
39339|Curlip Formation|70076|6|Mentioned|Regional: p2|||||||Overlies and interfingers with Kipper Shale.||
39339|Curlip Formation|73471|5|Briefly described|p86|||Gippsland Basin. Underlies Longtom Unconformity.||Emperor Subgroup|||Alluvial and fluvial sandstones and siltstones.|
39339|Curlip Formation|75065|5|Briefly described|p151|Turonian|Turonian|Gippsland Basin; offshore. Alluvial/fluvial deposits. Appears as Culip Formation on p151. Is overlain unconformably by Chimaera Formation (Golden Beach Subgroup).||Emperor Subgroup.||Overlies Admiral Formation, Kipper Shale and Kersop Arkose conformably; and Korumburra Subgroup (Strzelecki Group) unconformably. See more in COMMENTS.|Fluvial sandstones with interbedded mudstones and some very thin coals.|
21593|Currie Creek Ignimbrite|23309|4|Described|p110  Table 2.40|||Of Maroo Subgroup.  Maximum Thickness: 700m.||||||
21593|Currie Creek Ignimbrite|23615|3|Fully described|p100|||Of Marroo Subgroup.  Parts previously included in Ringwood's (1955a, b) Black Mountain Ignimbrite.  Overlain by Ballantyne Megabreccia.  Green to grey granular quartz-feldspar ignimbrite, with abundant phenocrysts and lithic clasts.||||||
21593|Currie Creek Ignimbrite|24551|5|Briefly described|p144|||||||||
21593|Currie Creek Ignimbrite|43206|5|Briefly described|map legend||Ludlow|Of Marroo Subgroup||||||
21593|Currie Creek Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Quartz-feldspar ignimbrite: green with abundant lithic clasts.|
37271|Currie Group|23309|5|Briefly described|p24, 359|Neoproterozoic|Neoproterozoic|||||||
37271|Currie Group|24002|5|Briefly described|p228 Fig. 2, p235|Neoproterozoic|Neoproterozoic|Includes picritic rocks. On King Island.||||||05-APR-07
37271|Currie Group|24098|6|Mentioned|p27 Fig. 2|Proterozoic|Proterozoic|Geological Province: Lachlan Fold Belt (King Island, Tasmania).||||||
37271|Currie Group|69841|6|Mentioned|p18|||This name was wrongly applied to the Grassy Group by VandenBerg et al. (2000) and Cayley et al. (2002).||||||
5085|Currowong Suite|22719|6|Mentioned|p485|||||||||
5085|Currowong Suite|22815|5|Briefly described|p57|Silurian|Silurian|||||||
5085|Currowong Suite|22877|5|Briefly described|map|Silurian|Silurian|||||||
5085|Currowong Suite|23549|5|Briefly described|p518, p524|||Geological Province:  Berridale Batholith.||||||05-APR-05
5085|Currowong Suite|24551|6|Mentioned|p235, 729 Table 8.12|||Of the Kuark Province||||||
5085|Currowong Suite|41933|5|Briefly described|Map legend|Late Silurian||||||||
5085|Currowong Suite|42627|5|Briefly described|Map legend|Wenlock||||||||
5085|Currowong Suite|42726|5|Briefly described|map legend||Silurian|Of the Currowong Supersuite.  Includes the Currowong, Bimbimbie, Iona, Bonang and Brodribb Granites.||||||09-FEB-05
5085|Currowong Suite|42827|5|Briefly described|p431|||||||||
5085|Currowong Suite|43233|5|Briefly described|Map Legend|Late Silurian||of Berridale Batholith.||||||
5085|Currowong Suite|67060|5|Briefly described|p503, p505 Table 1.|||Southern Berridale Batholith. I-type. Includes the compositionally-similar Iona, Currowong and Bimbimbie plutons.|c.417 Ma.|||||15-MAR-12
5085|Currowong Suite|72571|6|Mentioned|p88, p90-91, 94, 97, 99-101,103,105-107|||Of the Tasmanides of eastern Australia. I-type. Exhibits petrographic features and preserves geochemical and isotopic compositions that do not lend themselves to a simple restite or magma mixing model.|||Includes the Bimbimbie Granodiorite.|||
5087|Currowong Supersuite|42726|5|Briefly described|map legend|||Includes the Currowong, Goongerah, and Jungke Creek Suites.||||||09-FEB-05
5087|Currowong Supersuite|42827|5|Briefly described|p431|||||||||
37538|Curtis Diorite|23309|6|Mentioned|p229|||G386||||||
37538|Curtis Diorite|60451|4|Described|p89, 218|Early Devonian|Early Devonian|I-Type. Of the Ararat Suite. Type section in text. Fine to medium grained, melanocratic. Intruded by several dykes.||||||
37538|Curtis Diorite|60454|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Ararat Suite. Hornblende-biotite diorite: dark grey to black; quartz poor, oxidised.||||||
37538|Curtis Diorite|60459|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Ararat Suite. Hornblende-biotite diorite: oxidised.||||||
37538|Curtis Diorite|66002|5|Briefly described|p7 Tb.5|||Of Ararat Suite. In Ararat Pluton area. G386. Defined by Cayley and Taylor 2001.||||||
37538|Curtis Diorite|68116|5|Briefly described|Appendix, Map 30.|Early Devonian|Early Devonian||||||Hornblende-biotite diorite: dark grey to black; quartz poor; feldspar and hornblende phenocrysts; oxidised, highly magnetic.|
37714|Cut-throat Diorite|23309|6|Mentioned|p429, App 1|||G390.||||||
37714|Cut-throat Diorite|60458|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Quartz diotite; pale grey; fine grained; porphyritic; oxidised.||||||
37714|Cut-throat Diorite|60459|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Ararat Suite. Quartz diorite: oxidised, highly weathered.||||||
30443|Daahl Sandstone Member|23309|5|Briefly described|p79, 82  Table 2.27|||Maximum Thickness: 20m. Of the Wartook Sandstone.||||||
30443|Daahl Sandstone Member|24551|5|Briefly described|p122|||Of Mount Difficult Subgroup. Also referred to as Daahl Sandstone in text.||||||
30443|Daahl Sandstone Member|44929|5|Briefly described|Map Legend|Silurian|Ordovician|Of Wartook Sandstone. Quartz sandstone, pale, medium-grained, well-sorted.||||||25-JUL-06
30443|Daahl Sandstone Member|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Of Wartook Sandstone (Mount Difficult Sub-Group, Grampians Group). Quartz sandstone, pale, medium-grained.||||||13-JUN-06
30443|Daahl Sandstone Member|44932|5|Briefly described|Map Legend|Silurian|Ordovician|Of Wartook Sandstone. Quartz sandstone, pale, medium-grained, well-sorted.||||||25-JUL-06
30443|Daahl Sandstone Member|44933|5|Briefly described|Map Legend|Silurian|Ordovician|Of Wartook Sandstone. Quartz sandstone, pale, medium-grained, well-sorted.||||||25-JUL-06
30443|Daahl Sandstone Member|61183|4|Described|p49-50|||Of the Wartook Sandstone (Grampians Group). Interval of clean, medium-grained quartz sandstone that forms a prominent marker in the Black Range. Max. thickness: 20m. See also the abbreviated version Daahl Sandstone.||||||16-MAY-13
30443|Daahl Sandstone Member|64541|5|Briefly described|Map Legend|Silurian|Silurian|Of Wartook Sandstone, Mount Difficult Sub-group. Quartz sandstone: pale, medium grained, well sorted; with very large scale wedge-shaped cross-beds sets.||||||07-FEB-11
30443|Daahl Sandstone Member|64610|5|Briefly described|Map legend|Silurian|Silurian|Of Wartook Sandstone (Mount Difficult Subgroup, Grampians Gp). Sandstone: pale, medium-grained, well-sorted; with very large scale wedge-shaped cross-bed sets.||||||
30443|Daahl Sandstone Member|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Wartook Sandstone.  Defined by Cayley & Taylor, 1997. ||||||
5143|Dalgety Suite|22815|5|Briefly described|p56|Silurian|Silurian|Consists of 7 plutons.||||||18-FEB-08
5143|Dalgety Suite|24222|5|Briefly described|p11|||Chemistry of samples reported. S-type granite, felsic.  Geological Province: Berridale Batholith, Lachlan Fold Belt.||||||
5143|Dalgety Suite|24551|6|Mentioned|p234, 728 Table 8.11|||||||||
5143|Dalgety Suite|41563|6|Mentioned|p512|||||||||
5143|Dalgety Suite|41905|6|Mentioned|p42|||||||||
5143|Dalgety Suite|41933|5|Briefly described|Map legend|||||||||
5143|Dalgety Suite|42726|5|Briefly described|map legend||Silurian|Of the Dalgety Supersuite.  Includes nine 'granite' units.||||||09-FEB-05
5143|Dalgety Suite|42827|6|Mentioned|p431|||||||||
5143|Dalgety Suite|43233|5|Briefly described|Map Legend|Late Silurian||Of Berridale Batholith.||||||18-FEB-08
5143|Dalgety Suite|44093|5|Briefly described|p190 App. 1|Early Devonian|Silurian|||||||
5143|Dalgety Suite|67060|5|Briefly described|p503, p505 Table 1.|||Includes two S-type, N-S trending plutons: the granodioritic Dalgety pluton and the granitic Numbla Vale pluton.|435 +/- 4.4 Ma.|||||15-MAR-12
5143|Dalgety Suite|68592|5|Briefly described|p1253-4, p1264|||A discontinuous string of 9 plutons stretching 100km south from Lake Eucumbene into Victoria.||Unit in Wyangala Supersuite.|||Equigranular, non-fractionated granitoids.|
5143|Dalgety Suite|72571|6|Mentioned|p90, p92, p97, p100|||Of the Tasmanides of eastern Australia.||||||
5145|Dalgety Supersuite|22876|5|Briefly described|p28|||||||||
5145|Dalgety Supersuite|22877|5|Briefly described|map|Silurian|Silurian|||||||
5145|Dalgety Supersuite|42627|5|Briefly described|Map legend|Wenlock|Wenlock|||||||18-FEB-08
5145|Dalgety Supersuite|42726|5|Briefly described|map legend|||Includes the Dalgety Suite, containing 9 'granite' units.||||||09-FEB-05
5145|Dalgety Supersuite|42827|6|Mentioned|p431|||||||||
21613|Dandan Andesite|23309|4|Described|p109  Table 2.40|||Of the Little River Subgroup.  Maximum Thickness: 300m.||||||
21613|Dandan Andesite|23615|3|Fully described|p117|Early Devonian|Early Devonian|Of Little River Subgroup.  Restricted to two lenses of hornblende andesite.  Max. thickness in northern lens: 40m; southern lens estimated to be ~300m thick.  Overlies Mount McLeod Tonalite in northern lens, and underlain by Monkan Ignimbrite.||||||
21613|Dandan Andesite|24551|5|Briefly described|p144|||Of Little River Subgroup.||||||
21613|Dandan Andesite|43206|5|Briefly described|map legend||Lochkovian|of Little River Subgroup.||||||
21613|Dandan Andesite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Andesite lava, minor andesite breccia with carbonate-filled vughs.|
37539|Dandenong Ranges Igneous Complex|23309|4|Described|p166, 259|||||||||22-FEB-10
37539|Dandenong Ranges Igneous Complex|24551|4|Described|p161|||Supersedes Dandenongs Igneous Complex.||||||
37539|Dandenong Ranges Igneous Complex|75062|6|Mentioned|p74 Fig.2|Devonian|Devonian|Melbourne Zone.||||Is intruded by Lysterfield Granodiorite.|S-type.|
35513|Dandongadale Siltstone|61161|5|Briefly described|p83, p14, p32|||Of Cobbannah Group. Overlies Moornapa Sandstone. Mudstone-dominated. Not present in DARGO.||||||
35513|Dandongadale Siltstone|61163|4|Described|p85, p38 Tb. 6.2|Early Silurian|Early Silurian|Of the Cobbannah Group. Dominated by mudstone; finely laminated siltstone exposed along the Dandongadale River. Thickness: ~3000m. Geological Province: Lachlan Fold Belt.||||||
35513|Dandongadale Siltstone|61174|5|Briefly described|map legend|Early Silurian|Early Silurian|Of the Cobbannah Group. Siltstone, minor sandstone: siltstone massive to bedded, commonly bioturbated, laminated; sandstone thick to thin-bedded; turbiditic and non-turbiditic sandstone. Deep-marine hemipelagic and turbidite deposits. GSV map code: Scd.||||||07-FEB-11
35513|Dandongadale Siltstone|61175|5|Briefly described|map legend|Early Silurian|Early Silurian|Of the Cobbannah Group. Siltstone, minor sandstone: siltstone massive to bedded, commonly bioturbated, laminated; sandstone thick to thin-bedded; turbiditic and non-turbiditic sandstone. Deep-marine hemipelagic and turbidite deposits. GSV map code: Scd.||||||
35513|Dandongadale Siltstone|61176|5|Briefly described|map legend|Early Silurian|Early Silurian|Of the Cobbannah Group. Siltstone, minor sandstone: siltstone massive to bedded, commonly bioturbated, laminated; sandstone thick to thin-bedded; turbiditic and non-turbiditic sandstone. Deep-marine hemipelagic and turbidite deposits. GSV map code: Scd.||||||
35513|Dandongadale Siltstone|61177|5|Briefly described|map legend|Early Silurian|Early Silurian|Of the Cobbannah Group. Siltstone, minor sandstone: siltstone massive to bedded, commonly bioturbated, laminated; sandstone thick to thin-bedded; turbiditic and non-turbiditic sandstone. Deep-marine hemipelagic and turbidite deposits. GSV map code: Scd.||||||
35513|Dandongadale Siltstone|61178|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Cobbannah Group. Siltstone, minor sandstone, often quartzitic (turbidite): nonmagnetic except where hydrothermally(?) altered; gravity high; low to moderate radioelement, K and Th, low U. GSV map code: Scd.||||||
5213|Dargile Formation|5252|6|Mentioned|p66.|Lochkovian||Unit 4 contains representatives of Monograptus dubius type which went extinct before the Lochkovian.||||||
5213|Dargile Formation|13996|5|Briefly described|p138, p142, p146-147|Wenlock|Wenlock|Heathcote area. A new species of conulariid mentioned. Bivalve taxa distribution Table. Gastropods mentioned. Echinoderm taxa Table.||||Overlies Wapentake Formation.||
5213|Dargile Formation|22542|6|Mentioned|p663|||?Superseded by Dargile Group.||||||27-OCT-08
5213|Dargile Formation|22628|6|Mentioned|fig1p108|Silurian|Silurian|||||||
5213|Dargile Formation|22882|4|Described|p 11||Silurian|||||||
5213|Dargile Formation|22885|5|Briefly described|map|Late Silurian|Late Silurian|||||||
5213|Dargile Formation|22886|5|Briefly described|p13|Silurian|Silurian|||||||
5213|Dargile Formation|23108|5|Briefly described|p518|Late Silurian|Late Silurian|||||||
5213|Dargile Formation|23229|4|Described|Table3-3p26, 27, 29-31|Ludlow|Wenlock|||||||
5213|Dargile Formation|23267|4|Described|Fig14-1.1p374, 375-6, 380||Ludlovian|Max Age: 405 Ma.||||||
5213|Dargile Formation|23268|5|Briefly described|Fig14-2.2(a)p389, 390, 392|Silurian|Silurian|||||||
5213|Dargile Formation|23269|5|Briefly described|p401-2||Late Silurian|||||||
5213|Dargile Formation|23273|5|Briefly described|p434, Fig14-5.1p435, 437|Late Silurian|Silurian|Age: 405-410 Ma.||||||
5213|Dargile Formation|23276|5|Briefly described|Fig14-8.1p476, 477, 483||Late Silurian|||||||
5213|Dargile Formation|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
5213|Dargile Formation|23309|5|Briefly described|p138-152  Table 2.49||Silurian|Age: early Ludlow||||||
5213|Dargile Formation|24177|3|Fully described|p51, p50 Fig. 22|Late Silurian|Silurian|Overlain by the McIvor Sandstone. Overlies the Wapentake Formation. Geological Province: Melbourne Trough.||||||
5213|Dargile Formation|24224|5|Briefly described|p263|Late Silurian|Ludlow|Geological Province: Turtons Creek Inlier.||||||
5213|Dargile Formation|24328|5|Briefly described|Map legend|Late Silurian|Late Silurian|||||||
5213|Dargile Formation|24329|5|Briefly described|Map legend|Late Silurian|Late Silurian|||||||
5213|Dargile Formation|24551|5|Briefly described|p120, 606|Late Silurian|Late Silurian|||||||
5213|Dargile Formation|24588|5|Briefly described|p19-21, p12 Fig.3, p27, 28|Ludlow|Wenlock|Geological Province: Darraweit Guim Province. Shown as Dargile Sandstone in Table 5 p27.||||||29-NOV-13
5213|Dargile Formation|29982|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
5213|Dargile Formation|30867|6|Mentioned|Fig.2|||See also p15,16. Early Devonian to Early Silurian.||||||21-OCT-22
5213|Dargile Formation|30931|6|Mentioned|Map legend|Silurian|Silurian|||||||
5213|Dargile Formation|31161|5|Briefly described|PA10|||||||||
5213|Dargile Formation|31654|6|Mentioned|Map legend|Ludlovian|Ludlovian|||||||
5213|Dargile Formation|31852|6|Mentioned|p719|||See also Fig.5. Ludlovian||||||
5213|Dargile Formation|32074|6|Mentioned|p179|||||||||
5213|Dargile Formation|32077|5|Briefly described|p33|||||||||
5213|Dargile Formation|33315|6|Mentioned|Fig.1|||U.Sil.||||||
5213|Dargile Formation|33326|6|Mentioned|p431|||Fauna.||||||
5213|Dargile Formation|33394|5|Briefly described|p74|||||||||
5213|Dargile Formation|33462|6|Mentioned|p10|||Strat.table.||||||
5213|Dargile Formation|33464|6|Mentioned|Fig.2|||||||||
5213|Dargile Formation|33598|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
5213|Dargile Formation|33599|4|Described|p3|||Ludlovian.||||||
5213|Dargile Formation|33601|6|Mentioned|p36|||||||||
5213|Dargile Formation|33604|4|Described|p17|||||||||
5213|Dargile Formation|33605|6|Mentioned|Map legend|Silurian|Silurian|||||||
5213|Dargile Formation|33607|6|Mentioned|Map legend|Silurian|Silurian|||||||
5213|Dargile Formation|35011|6|Mentioned|Fig. 9.5b|||||||||
5213|Dargile Formation|35283|3|Fully described|p47|||||||||
5213|Dargile Formation|35712|6|Mentioned|Table 6|||||||||
5213|Dargile Formation|37013|6|Mentioned|p38|||||||||
5213|Dargile Formation|37727|4|Described|p53|||See also p6.||||||23-SEP-18
5213|Dargile Formation|37752|6|Mentioned|p115|||||||||
5213|Dargile Formation|38070|6|Mentioned|Fig.8 p96|||||||||21-OCT-22
5213|Dargile Formation|38146|6|Mentioned|Map legend|Silurian|Silurian|||||||
5213|Dargile Formation|38378|6|Mentioned|p134|||||||||
5213|Dargile Formation|38787|6|Mentioned|p124|||||||||
5213|Dargile Formation|39331|4|Described|p21|||See also Table 2-1||||||
5213|Dargile Formation|40725|6|Mentioned|p1|||See also Fig.1||||||
5213|Dargile Formation|41585|4|Described|p107|||||||||
5213|Dargile Formation|41848|6|Mentioned|p392|||Age Silurian||||||
5213|Dargile Formation|42033|5|Briefly described|p649|||||||||
5213|Dargile Formation|42790|5|Briefly described|Fig.8 P183|||||||||
5213|Dargile Formation|42826|6|Mentioned|p45|||||||||
5213|Dargile Formation|42827|4|Described|p107|||see also Table 4.1||||||
5213|Dargile Formation|43871|14|Not recorded|p11 Fig.1,12-55|||Fauna||||||
5213|Dargile Formation|48971|6|Mentioned|p9|||See also p12 and p17.||||||21-OCT-22
5213|Dargile Formation|60083|5|Briefly described|Map legend|Late Silurian|Late Silurian|Laminated and current-bedded sandstone, minor interbedded mudstone and shale.  Overlain by Humevale Formation.||||||19-JUL-04
5213|Dargile Formation|60529|5|Briefly described|Map Legend|Ludlow|Ludlow|Deep water hemipelagic sediment: mudstone, minor very fine grained sandstone; laminated to thinly bedded, minor current ripples: shelly fossils.||||||
5213|Dargile Formation|60591|5|Briefly described|Map Legend|Ludlow|Wenlock|Deep water sediment: mudstone, minor very fine-grained sandstone; laminated to thinly bedded, minor current ripples; shelly fossils.||||||
5213|Dargile Formation|60592|5|Briefly described|Map Legend|Ludlow|Wenlock|Deep water sediment: mudstone, minor very fine-grained sandstone; laminated to thinly bedded, minor current ripples; shelly fossils.||||||
5213|Dargile Formation|60593|5|Briefly described|Map Legend|Ludlow|Wenlock|Deep water sediment: mudstone, minor very fine-grained sandstone; laminated to thinly bedded, minor current ripples; shelly fossils.||||||
5213|Dargile Formation|60595|5|Briefly described|Map Legend|Ludlow|Wenlock|Deep water sediment: mudstone, minor very fine-grained sandstone; laminated to thinly bedded, minor current ripples; shelly fossils.||||||26-NOV-04
5213|Dargile Formation|60596|5|Briefly described|Map Legend|Ludlow|Wenlock|Deep water sediment: mudstone, minor very fine-grained sandstone; laminated to thinly bedded, minor current ripples; shelly fossils.||||||
5213|Dargile Formation|60597|5|Briefly described|Map Legend|Ludlow|Wenlock|Low magnetic response, with weak magnetic linear features; moderate K and Th, high U.||||||26-NOV-04
5213|Dargile Formation|60599|1|Redefined|p13, p24 Tb. 4, p51,  p125, p106|Late Silurian|Early Silurian|Supersedes Dargile Beds; contains units 1 and 2 (of Thomas 1937). Sandstone+conglomerates (basal); with abundant graptolites. Conformable on Wapentake Formation; conformable beneath McIvor Sandstone. Max. thickness: ~1900m. Geol.Prov: Melbourne Zone/LFB.||||||27-OCT-08
5213|Dargile Formation|61185|2|Defined|p19, p22, p21 Fig 6, p11, p13|Pragian|Late Ludlow|Incl: lower 2 faunal units of Dargile Beds (Thomas 1937) and part/all of Chintin Beds (Talent and Thomas 1967); Clonbinane Sandstone and Mount Phillipa Members formerly of Humevale Siltstone. Relationships in text p22 error. Thick:~1900m. Geol.Prov: LFB||||||07-FEB-11
5213|Dargile Formation|61187|6|Mentioned|p5 Fig.3.|Silurian|Silurian|Melbourne Zone, Melbourne Terrane.||||||
5213|Dargile Formation|61701|5|Briefly described|Map Legend|Ludlow|Ludlow|Deep water hemipelagic sediment: mudstone, minor very fine grained sandstone; laminated to thinly bedded, minor current ripples: shelly fossils.||||||
5213|Dargile Formation|61702|5|Briefly described|Map Legend|Ludlow|Ludlow|Deep water hemipelagic sediment: mudstone, minor very fine grained sandstone; laminated to thinly bedded, minor current ripples: shelly fossils.||||||
5213|Dargile Formation|61703|5|Briefly described|Map Legend|Ludlow|Ludlow|Deep water hemipelagic sediment: mudstone, minor very fine grained sandstone; laminated to thinly bedded, minor current ripples: shelly fossils.||||||
5213|Dargile Formation|61704|6|Mentioned|Map legend|Silurian|Silurian|Low moderate K and Th, high U.||||||14-JUN-06
5213|Dargile Formation|64611|5|Briefly described|Map legend|Ludlow|Wenlock|Of Murrindindi Supergroup. Mudstone, minor sandstone and conglomerate: laminated to thinly bedded siltstone with minor current ripples and shelly fossils; fine-grained quartz sandstone and oligomictic cobble conglomerate. Deep-water marine deposits.||||||15-DEC-08
5213|Dargile Formation|64612|2|Defined|p27, p39-40, p54|Late Ludlow|Early Ludlow|Of Murrindindi Supergroup. Conformably between Wapentake Formation (underlying) and overlying McIvor Sandstone, both contacts gradational. Thick: 2500m. Massive to thinly bedded laminated siltstone. Very varied shelly fauna in unit.||||||07-FEB-11
5213|Dargile Formation|65900|6|Mentioned|p167|||Western Melbourne Zone.||||Overlies the Mount Easton Shale.||10-MAY-12
5213|Dargile Formation|66244|4|Described|p2.|||Defined by Edwards et al. (1998); formerly the lower mudstone-rich part of the Dargile Beds of Thomas (1937). A probable time-equivalent of the Humevale Siltstone. The sandstone-rich unit mapped as Dargile Formation in the Melbourne area is now considered to be the Melbourne Formation. Also now restricted to west of the Moormbool Fault.||||||11-FEB-15
5213|Dargile Formation|68116|5|Briefly described|Appendix, Maps 24, 32.|Pridoli|Llandovery||||||Mudstone, minor sandstone and conglomerate: laminated to thinly bedded siltstone with minor current ripples and shelly fossils; fine-grained quartz sandstone and oligomictic cobble conglomerate; deep water marine sediments.|
5213|Dargile Formation|69089|5|Briefly described|Map legend|Late Silurian|Late Silurian||||||Marine: siltstone, thin-bedded sandstone.|
5213|Dargile Formation|70487|5|Briefly described|p8-9, p11 Fig.5|Pridoli|Wenlock|Synonymised with the Humevale Siltstone in the Bailieston area enabling a maximum age from graptolite dating.||||Considered to be underlying the Broadford Formation (Edwards et al. 1997).|Includes siltstone.|
5213|Dargile Formation|70904|4|Described|p 34|||||||||
5213|Dargile Formation|70933|14|Not recorded|p93||Early Ludlow|Graptolitic.||||||
5213|Dargile Formation|73497|5|Briefly described|Map legend|Silurian|Silurian|Marine.||Murrindindi Supergroup|||Siltstone, sandstone, minor conglomerate: low magnetic response with weak magnetic linear features of short strike length (3km); moderate K and Th, and high U radiometric trends follow strike.|
69701|Dargo Tonalite|61161|5|Briefly described|p101-103, p8, p76-77 Fig 6.1|Early Devonian|Early Devonian|Magnetite-rich and poor tonalite (G140a) surrounds magnetic, medium-grained granite (G140b) core. Granite interpreted to have intruded into core of surrounding tonalite. Age: K/Ar biotite 387+-15 and 402 +-16Ma, hornblende 400+-16 and 399+-16Ma. I-type.||||||
69701|Dargo Tonalite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Subdivided into two informal phases: biotite-hornblende tonalite and granite. GSV map code: G140a and G140b respectively; I-type intrusion.||||||
69701|Dargo Tonalite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Subdivided into two informal phases: biotite-hornblende tonalite and granite. GSV map code: G140a and G140b respectively; I-type intrusion.||||||07-FEB-11
69701|Dargo Tonalite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Subdivided into two informal phases: biotite-hornblende tonalite and granite. GSV map code: G140a and G140b respectively; I-type intrusion.||||||
69701|Dargo Tonalite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Subdivided into two informal phases: biotite-hornblende tonalite and granite. GSV map code: G140a and G140b respectively; I-type intrusion.||||||
69701|Dargo Tonalite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Subdivided into two informal phases: biotite-hornblende tonalite and granite. GSV map code: G140a and G140b respectively. Both subdivided into 2 units of differing geophysical responses. K/Ar ages for G140b - beta unit.||||||
69701|Dargo Tonalite|68116|5|Briefly described|Appendix, Maps 35, 44.|Early Devonian|Early Devonian||||||Granite: grey, medium-grained, equigranular to porphyritic in K-feldspar; massive; biotite-hornblende tonalite: grey, medium-grained, equigranular to porphyritic in hornblende, massive.|
5222|Darley Gravel|33604|5|Briefly described|p25|||||||||
5222|Darley Gravel|33605|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
5222|Darley Gravel|39865|6|Mentioned|p46|||||||||
5222|Darley Gravel|65715|4|Described|p15 Tb.8, p17, p110-112|Quaternary|Pliocene|Called Darley Gravels by Thomas and Baragwanath (1950). Post-basaltic outwash aprons of gravel, sand and silt along Rowsley and Coimadai fault scarps. Fluvial.  Overlies Newer Volcanic Group and Werribee Formation. Formation rank.||||||31-JAN-18
5222|Darley Gravel|68116|5|Briefly described|Appendix, Maps 41, 50.|Pleistocene|Neogene||||||Gravel, sand, silt: gravel red to pale colours; rounding and sorting moderate to good; moderately consolidated; massive to trough cross-bedded; gravel clasts of vein quartz, sandstone, basalt, ironstone in proportions that reflect the local source.|
5222|Darley Gravel|71419|5|Briefly described|p18 Fig 19|Recent|Pliocene|Dissected fluvial and colluvial deposits.||||||
27308|Darraweit Guim Mudstone|13995|5|Briefly described|p86, p109|Late Ordovician|Late Ordovician|Contains late Ashgill-aged, cool-water, "Hirnantia" fauna trilobites.||||Is overlain by Deep Creek Siltstone.||
27308|Darraweit Guim Mudstone|22684|5|Briefly described|Fig.2 p746|Late Ordovician|Late Ordovician|See also Fig.5 p749||||||
27308|Darraweit Guim Mudstone|22886|5|Briefly described|p12|Late Ordovician|Late Ordovician|||||||
27308|Darraweit Guim Mudstone|23229|4|Described|Table3-2p21, 23|Bolindian|Bolindian|||||||
27308|Darraweit Guim Mudstone|23307|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
27308|Darraweit Guim Mudstone|23309|4|Described|p59, 60, 139, 261, 266, 270, Table 2.18|Late Ordovician|Late Ordovician|Of Sunbury Group. Middle Bolindian. Underlying unit: Bolinda shale.||||||
27308|Darraweit Guim Mudstone|24002|5|Briefly described|p247|Late Ordovician|Late Ordovician|||||||
27308|Darraweit Guim Mudstone|24551|4|Described|p105, 606|Late Ordovician|Late Ordovician|Of Sunbury Group.||||||
27308|Darraweit Guim Mudstone|24588|5|Briefly described|p29|||Overlies Bolinda Shale. Is overlain by Deep Creek Siltstone of Murrindindi Supergroup. Geological Province: Darraweit Guim Province.||||||29-NOV-13
27308|Darraweit Guim Mudstone|39980|2|Defined|p19|Late Ordovician|Late Ordovician|||||||
27308|Darraweit Guim Mudstone|40761|6|Mentioned|p225|||||||||
27308|Darraweit Guim Mudstone|41570|3|Fully described|p87|||||||||
27308|Darraweit Guim Mudstone|41585|6|Mentioned|p105|||||||||
27308|Darraweit Guim Mudstone|42628|5|Briefly described|Map legend|Bolindian||||||||
27308|Darraweit Guim Mudstone|42826|2|Defined|p33|Late Ordovician||||||||
27308|Darraweit Guim Mudstone|42827|4|Described|p87|||||||||
27308|Darraweit Guim Mudstone|62099|5|Briefly described|p331|Late Ordovician|Late Ordovician|Dominated by black shale. In the Melbourne Zone of the Lachlan Orogen. .||||||
27308|Darraweit Guim Mudstone|65715|5|Briefly described|p4 Tb.2|Ordovician|Ordovician|Of Sunbury Group. Formation rank.||||||
5230|Darriman limestone|34815|6|Mentioned|p20|||||||||
5234|Darriwil granite|37385|6|Mentioned|p6|||Name refers to an outcrop area only.||||||
5235|Darriwilian Slate|31706|6|Mentioned|p637|||Ordovician correlation chart||||||
23534|Dart River Volcanic Breccia|23309|5|Briefly described|p89, 122, 133.|||||||||
23534|Dart River Volcanic Breccia|24133|5|Briefly described|p45|Devonian|Devonian|Parent: Dartella Volcanic Group.  Geological Province: Lachlan Fold Belt.||||||
23534|Dart River Volcanic Breccia|24551|5|Briefly described|p149|Devonian|Devonian|Supersedes the Dart River Formation? Of Dartella Volcanics.||||||
23534|Dart River Volcanic Breccia|39221|6|Mentioned|p270|||||||||
23534|Dart River Volcanic Breccia|44184|5|Briefly described|Map Legend||Early Devonian|||||||
23534|Dart River Volcanic Breccia|60503|3|Fully described|p41 Tb. 2, p115|Early Devonian|Early Devonian|Of the Dartella Volcanics. Originally had member status within Sheevers Spur Rhyodacite. Now a formation. Purple-brown to grey sedimentary breccias and conglomerates; abundant clasts. Overlain by Murtagh Creek Ignimbrite. Max. thickness<100m.||||||16-NOV-09
23534|Dart River Volcanic Breccia|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Dartella Volcanic Group. Scree deposits: breccia, poorly sorted, with clasts of Ordovician bedrock, ignimbrite, andesite, granite and limestone||||||
23534|Dart River Volcanic Breccia|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Scree deposits: breccia, poorly sorted, with clasts of Ordovician bedrock, ignimbrite, andesite, granite and limestone||||||
23534|Dart River Volcanic Breccia|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Scree deposits: breccia, poorly sorted, with clasts of Ordovician bedrock, ignimbrite, andesite, granite and limestone||||||
23534|Dart River Volcanic Breccia|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Scree deposits: breccia, poorly sorted, with clasts of Ordovician bedrock, ignimbrite, andesite, granite and limestone||||||07-OCT-04
23534|Dart River Volcanic Breccia|68116|5|Briefly described|Appendix, Map 27.|Early Devonian|Early Devonian||||||Breccia, poorly sorted, with clasts and occasional megaclasts of Ordovician bedrock, ignimbrite, andesite, granite and limestone.|
23535|Dartella Volcanic Group|22487|6|Mentioned|p201|Early Devonian|Early Devonian|||||||
23535|Dartella Volcanic Group|22768|5|Briefly described|p167,178||Early Devonian|||||||
23535|Dartella Volcanic Group|22857|5|Briefly described|p167, p178|Early Devonian|Early Devonian|Unconformably overlies the Wombat Formation.||||||
23535|Dartella Volcanic Group|24133|4|Described|p45|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
23535|Dartella Volcanic Group|24142|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
23535|Dartella Volcanic Group|24143|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
23535|Dartella Volcanic Group|24144|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
23535|Dartella Volcanic Group|24145|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Geological Province: Lachlan Fold Belt||||||
23535|Dartella Volcanic Group|24146|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
23535|Dartella Volcanic Group|39221|2|Defined|p263|Devonian|Devonian|||||||
23535|Dartella Volcanic Group|40761|5|Briefly described|p230|||||||||
23535|Dartella Volcanic Group|41572|6|Mentioned|p18|||See also p19||||||05-SEP-05
23535|Dartella Volcanic Group|41585|4|Described|p132|||||||||
23535|Dartella Volcanic Group|41868|6|Mentioned|p584|||||||||
23535|Dartella Volcanic Group|42089|6|Mentioned|p18|||||||||
23535|Dartella Volcanic Group|42726|5|Briefly described|map legend|Early Devonian||||||||
23535|Dartella Volcanic Group|42827|4|Described|p132|||||||||
23535|Dartella Volcanic Group|43220|5|Briefly described|p10||Devonian|||||||
23535|Dartella Volcanic Group|60503|3|Fully described|p112|Early Devonian|Early Devonian|Name used interchangeably with Dartella Volcanics. Formerly interpreted as the northern part of the Mitta Mitta Volcanics.||||||16-NOV-09
23535|Dartella Volcanic Group|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Tabor Volcanics, Dart River Volcanic Breccia, Murtagh Creek Ignimbrite, Larsen Creek Ignimbrite, Sheevers Spur Ignimbrite.||||||
23535|Dartella Volcanic Group|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes: Tabor Volcanics, Dart River Volcanic Breccia, Murtagh Creek Ignimbrite, Larsen Creek Ignimbrite, Sheevers Spur Ignimbrite.||||||
23535|Dartella Volcanic Group|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes: Tabor Volcanics, Dart River Volcanic Breccia, Murtagh Creek Ignimbrite, Larsen Creek Ignimbrite, Sheevers Spur Ignimbrite.||||||
23535|Dartella Volcanic Group|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Tabor Volcanics, Dart River Volcanic Breccia, Murtagh Creek Ignimbrite, Larsen Creek Ignimbrite, Sheevers Spur Ignimbrite.||||||
23535|Dartella Volcanic Group|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes: Tabor Volcanics, Dart River Volcanics Breccia, Murtagh Creek Ignimbrite, Larsen Creek Ignimbrite, Sheevers Spur Ignimbrite, Eight Mile Loop Rhyolite, Besford Ignimbrite.||||||
23535|Dartella Volcanic Group|68116|5|Briefly described|Appendix, Map 20.|Middle Devonian|Early Devonian|Dyke|||||Hornblende-feldspar porphyry dyke: dark green, fine grained; plagioclase phenocrysts up to 3 mm long; highly magnetic.|
23536|Dartmouth Granite|22628|6|Mentioned|fig1p108|Silurian|Silurian|||||||
23536|Dartmouth Granite|23309|5|Briefly described|p69, 338|||G109 - S-Type.||||||
23536|Dartmouth Granite|39221|3|Fully described|p266|||||||||
23536|Dartmouth Granite|41572|6|Mentioned|p18|||||||||
23536|Dartmouth Granite|42726|5|Briefly described|map legend|Silurian||||||||
23536|Dartmouth Granite|42827|6|Mentioned|p18|||||||||
23536|Dartmouth Granite|60503|3|Fully described|p142, p45 Tb. 2|Silurian|Silurian|Two types of granite: main part is gneissic two-mica granite; other is of foliated grey granite. In faulted contact with Larsen Creek Ignimbrite. Unconformably overlain by Murtagh Creek Ignimbrite. Within the Omeo Metamorphic Complex.||||||08-DEC-16
23536|Dartmouth Granite|60504|5|Briefly described|Map Legend|Wenlock|Wenlock|Granite, gneissic granite: S-type; varies from strongly banded gneiss to homogeneous granite with abundant sedimentary enclaves; various grey colours, medium grained.||||||
23536|Dartmouth Granite|60505|5|Briefly described|Map legend|Wenlock|Wenlock|Granite, gneissic granite: S-type; varies from strongly banded gneiss to homogeneous granite with abundant sedimentary enclaves; various grey colours, medium grained.||||||
23536|Dartmouth Granite|60506|5|Briefly described|Map legend|Wenlock|Wenlock|Granite, gneissic granite: S-type; varies from strongly banded gneiss to homogeneous granite with abundant sedimentary enclaves; various grey colours, medium grained.||||||
23536|Dartmouth Granite|60507|5|Briefly described|Map Legend|Wenlock|Wenlock|Granite, gneissic granite: S-type; varies from strongly banded gneiss to homogeneous granite with abundant sedimentary enclaves; various grey colours, medium grained.||||||13-OCT-04
23536|Dartmouth Granite|60508|5|Briefly described|Map legend|Early Silurian|Early Silurian|Granite, gneissic granite: S-type; 497+/-7Ma (U/Pb zircon); nonmagnetic (0-5 nT), similar magnetic response to Pinnak Sandstone; high total count, K, Th, U in Mitta Mitta River Valley, low radiometric response elsewhere.||||||21-OCT-04
23536|Dartmouth Granite|61160|5|Briefly described|p78|||Intruded by Banimboola Quartz Monzodiorite. ||||||
23536|Dartmouth Granite|61187|5|Briefly described|p5 Fig.3.|Early Silurian|Late Ordovician|Tabberabbera Zone, Benambra Terrane. Age interpreted from Fig.3.|c.440 Ma.|||||
23536|Dartmouth Granite|68116|5|Briefly described|Appendix, Map 27.|Wenlock|Llandovery||||||Biotite granite, gneissic granite: varies from strongly banded gneiss to homogeneous granite with abundant sedimentary enclaves; various grey colours, medium-grained.|
37540|Davidsons Lane Formation|23309|4|Described|p112, Table 2.40|||Of Timbarra Subgroup.  Maximum Thickness: ~750m.||||||22-FEB-10
37540|Davidsons Lane Formation|24551|4|Described|p142|||Of the Timbarra Subgroup.||||||
37540|Davidsons Lane Formation|60542|4|Described|p14, p52|Early Devonian|Early Devonian|Of Timbarra Subgroup. Previously mapped as undifferentiated Timbarra Subgroup. Sedolithic pebble and boulder conglomerates with a sandy matrix. Conformable on Johnson Mudstone.||||||
37540|Davidsons Lane Formation|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Sedolithic and volcanolithic conglomerate, sandstone, mudstone: mostly massive and clast supported; fluvial deposits.|
34900|Day Hill Syenite|22968|5|Briefly described|P156, P222|Triassic|Triassic|New name, intruded the Tea Pot Creek Formation||||||
34900|Day Hill Syenite|23029|5|Briefly described|Map legend|Triassic|Triassic|Parent is the Mount Leinster Igneous Complex||||||
34900|Day Hill Syenite|23030|5|Briefly described|Map legend|Triassic|Triassic|Parent is the Mount Leinster Igneous Complex||||||
34900|Day Hill Syenite|68116|5|Briefly described|Appendix, Map 35.|Triassic|Triassic||||||Biotite syenite, quartz syenite: leucocratic; equigranular coarse-grained.|
34862|Dead Bird Suite|22968|5|Briefly described|p211, P89, Fig48, Fig89||Early Devonian|New name, strongly magnetic, Age of unit is 411+/-5 Ma||||||
34862|Dead Bird Suite|23020|5|Briefly described|Map legend|Lochkovian|Lochkovian|Overlying unit is Mount Elizabeth Caldera Complex||||||
34862|Dead Bird Suite|23021|5|Briefly described|Map legend|Lochkovian|Lochkovian|Nonconformably and angular unconformably underlies the Mount Elizabeth Caldera Complex||||||
34862|Dead Bird Suite|23028|5|Briefly described|Map legend|Lochkovian|Lochkovian|Unconformably and nonconformably underlies the Mount Elizabeth Caldera Complex||||||
34862|Dead Bird Suite|23029|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
34862|Dead Bird Suite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
34862|Dead Bird Suite|23309|6|Mentioned|p429 App1|||G543 I-Type.||||||
34862|Dead Bird Suite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Hornblende-biotite diorite/granodiorite: dark grey-green, fine to medium-grained, equigranular; often strong epidote-chlorite alteration; plugs.|
5297|Dead Bull Member|23309|5|Briefly described|p104  Table 2.38||Early Devonian|||||||
5297|Dead Bull Member|24551|5|Briefly described|p138, 620||Late Pragian|Of the Tabberabbera Formation.||||||
5297|Dead Bull Member|33326|6|Mentioned|p433|||Fauna.||||||
5297|Dead Bull Member|33606|6|Mentioned|p68|||||||||
5297|Dead Bull Member|37330|5|Briefly described|p17|||||||||
5297|Dead Bull Member|41585|6|Mentioned|Fig.4.9|||||||||
5297|Dead Bull Member|42033|6|Mentioned|p653|||||||||
5297|Dead Bull Member|61161|5|Briefly described|p118|||Of Tabberabbera Formation. At base of formation; limited distribution. Underlies Kilgower Member and Roaring Mag Member. Mudstone.||||||
21630|Dead Cattle Gully Ignimbrite|23309|4|Described|p110  Table 2.70|||Maximum Thickness: 700m.  Of the Mount Dawson Subgroup.||||||
21630|Dead Cattle Gully Ignimbrite|23615|3|Fully described|p104|Early Devonian|Early Devonian|Lowermost formation in the Mount Dawson Subgroup.  Dark grey to black feldspar-rich ignimbrite.  Overlies Statham Ignimbrite.||||||
21630|Dead Cattle Gully Ignimbrite|43206|5|Briefly described|map legend||Ludlow|Of Mount Dawson Subgroup.||||||
21630|Dead Cattle Gully Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Feldspar ignimbrite: grey to black with small quartz, ferromagnesian minerals and red pumice.|
74735|Dealba Sandstone Member|60599|2|Defined|p63|Early Devonian|Early Devonian|Of Mount Ida Fm. Corresponds to Pentamerus Beds (Thomas 1937). Well-sorted, thickly bedded quartzite, weathering into sugary textured rock; predominantly fine- to med.-gr.sst. Conformable below Stoddart Mbr; conformable on Cornella Mbr. Thickness: ~700m.||||||27-OCT-08
39642|Deborah Back Sandstone|24088|6|Mentioned|p355 Fig. 4||| Geological Province: Lachlan Fold Belt.||||||
5313|Deddick Rhyodacite|23615|5|Briefly described|p131, p85|Early Devonian|Early Devonian|Superseded by Deddick Lava.||||||
5313|Deddick Rhyodacite|33603|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
5313|Deddick Rhyodacite|33606|5|Briefly described|p64|||||||||
5313|Deddick Rhyodacite|35283|6|Mentioned|p49|||||||||
5313|Deddick Rhyodacite|36201|4|Described|p4|||||||||
5313|Deddick Rhyodacite|37330|6|Mentioned|p14|||See also Table 2.||||||
5313|Deddick Rhyodacite|39447|5|Briefly described|p12|||||||||
5313|Deddick Rhyodacite|41585|5|Briefly described|p136|||||||||
5313|Deddick Rhyodacite|60542|6|Mentioned|p50|||Deddick Lava name preferred in this study.||||||
5313|Deddick Rhyodacite|68115|5|Briefly described|p4, p6.|Devonian|Devonian|Originally of Ringwood (1955a, b); subsequently VandenBerg (1976); changed to Deddick Lava by Orth et al. (1993); since it is intrusive, this latter name is untenable and is replaced by the compositional term.||Unit in Snowy River Volcanic Group.||||
5313|Deddick Rhyodacite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Porphyry dykes; quartz-feldspar (hornblende) porphyry.|
69408|Dederang Granite|61160|3|Fully described|p85, p32 Tb. 5.2, p58-59 Fig. 6.8|Early Devonian|Early Devonian|S-type. Originally mapped as part of Kergunyah Adamellite. Fine- to medium-grained, equigranular biotite granite; few enclaves, and a few small biotite-rich clots of 1cm length; cordierite present in some samples.  ||||||
69408|Dederang Granite|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Muscovite-biotite granite: grey; equigranular; medium grained; much of it is foliated and mylonitized by the Kiewa Fault. GSV map code: G169.||||||
69408|Dederang Granite|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Muscovite-biotite granite: grey; equigranular; medium grained; much of it is foliated and mylonitized by the Kiewa Fault. GSV map code: G169.||||||
69408|Dederang Granite|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Muscovite-biotite granite: grey; equigranular; medium grained; much of it is foliated and mylonitized by the Kiewa Fault. GSV map code: G169.||||||
69408|Dederang Granite|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Muscovite-biotite granite: grey; equigranular; medium grained; much of it is foliated and mylonitized by the Kiewa Fault. GSV map code: G169.||||||07-FEB-11
69408|Dederang Granite|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Muscovite-biotite granite: I-type; subdivided into linear dyke-like magnetic highs and non- to slightly magnetic; both have: gravity low; moderate total radioelement, high K, low Th and U. GSV map code: G169.||||||
69408|Dederang Granite|68116|5|Briefly described|Appendix, Maps 20, 27.|Early Devonian|Silurian||||||Muscovite-biotite granite: grey; equigranular; medium grained; much of it is foliated and mylonitized by the Kiewa Shear Zone.|
37541|Deenicull Schist|23309|5|Briefly described|p65 Tb 2.23, p30|||Of Moornambool Metamorphic Complex.||||||
37541|Deenicull Schist|24551|5|Briefly described|p82|||Of the Moornambool Metamorphic Complex.||||||
37541|Deenicull Schist|60451|4|Described|p57, 63, 111, 206|||Of the Moornambool Metamorphic Complex. Warrak Formation and Magdala Volcanics probably protoliths of this unit. Greenschist grade. Underlies Saint Arnaud Group.||||||
37541|Deenicull Schist|60454|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-chlorite (+/-tremolite+/-actinolite+/-biotite) schist; strongly schistose; polydeformed.||||||
37541|Deenicull Schist|60457|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-chlorite (+/-tremolite+/-actinolite+/-biotite) schist; strongly schistose; polydeformed; numerous thin quartz veins.||||||
37541|Deenicull Schist|60458|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-chlorite (+/-tremolite+/-actinolite+/-biotite) schist; strongly schistose; polydeformed; numerous thin quartz veins.||||||
37541|Deenicull Schist|60459|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-chlorite (+/-tremolite+/-actinolite+/-biotite) mafic schist, with some ultramafic igneous and pelitic components. Greenschist grade.||||||
37541|Deenicull Schist|61187|6|Mentioned|p82, p83 Fig.1, p84 Fig.2.|||Part of this unit may have the Magdala Metabasalt as precursor. Susceptibility measures given.||||||
37541|Deenicull Schist|66002|5|Briefly described|p5 Tb.2|Cambrian|Cambrian|Of Moornambool Metamorphic Complex. Defined by Cayley and Taylor 2001.||||||
37541|Deenicull Schist|68116|5|Briefly described|Appendix, Map 30.|Late Cambrian|Late Cambrian||||||Quartz-chlorite (+/-tremolite+/-actinolite+/-biotite) schist; strongly schistose; polydeformed; numerous thin quartz veins; formed from a mix of Magdala Volcanics and Albion and Leviathan Formation precursors? low to highly magnetic.|
5327|Deep Creek Siltstone|13995|5|Briefly described|p109|||Contains the graptolite ?G. persculptus in basal layers.||||Overlies Darraweit Guim Mudstone.||
5327|Deep Creek Siltstone|22511|6|Mentioned|p661|||||||||
5327|Deep Creek Siltstone|22530|6|Mentioned|p696||Ashgill|||||||
5327|Deep Creek Siltstone|22542|6|Mentioned|p664|||||||||
5327|Deep Creek Siltstone|22684|4|Described|p747, Fig.2 p746|Llandovery|Late Ordovician|See also Fig.5 p749.||||||14-APR-08
5327|Deep Creek Siltstone|22885|5|Briefly described|map|Early Silurian|Early Silurian|||||||
5327|Deep Creek Siltstone|22886|4|Described|p12|Llandovery|Llandovery|||||||
5327|Deep Creek Siltstone|23229|4|Described|Table3-2p21, 28|Llandovery|Bolindian|||||||
5327|Deep Creek Siltstone|23272|5|Briefly described|p414, Fig14-4.1p415, 419||Early Silurian|||||||
5327|Deep Creek Siltstone|23309|5|Briefly described|p134, 139, 150-152.||Late Ordovician|||||||
5327|Deep Creek Siltstone|24177|5|Briefly described|p50 Fig.22|Llandovery|Bolindian|Geological Province: Darraweit Guim Province.||||||
5327|Deep Creek Siltstone|24551|5|Briefly described|p98|||Of the Murrindindi Supergroup.||||||
5327|Deep Creek Siltstone|24588|5|Briefly described|p18-19, p12 Fig.3, p13, 21|Wenlock|Llandovery|Geological Province: Darraweit Guim Province. Basal unit of Murrindindi Supergroup. Overlies Darraweit Guim Mudstone of Sunbury Group. Overlain by Springfield Sandstone. Creek is Ck in text.||||||29-NOV-13
5327|Deep Creek Siltstone|29608|6|Mentioned|p46|||[Originally enterd for Tas. CEBMar95]||||||
5327|Deep Creek Siltstone|33125|6|Mentioned|p15|||Correlation chart.||||||14-APR-08
5327|Deep Creek Siltstone|33604|6|Mentioned|p17|||Correlation chart.Sil.||||||
5327|Deep Creek Siltstone|35118|6|Mentioned|p426|||||||||
5327|Deep Creek Siltstone|35283|3|Fully described|p46|||||||||
5327|Deep Creek Siltstone|37727|3|Fully described|p54|||See also P11.||||||
5327|Deep Creek Siltstone|38787|6|Mentioned|p128|||||||||
5327|Deep Creek Siltstone|39331|6|Mentioned|Table 2-1|||||||||
5327|Deep Creek Siltstone|39980|2|Defined|p20|Silurian|Silurian|Base near Ordovician-Silurian boundary and top in Llandovery.||||||14-JAN-09
5327|Deep Creek Siltstone|40126|6|Mentioned|p14|||||||||
5327|Deep Creek Siltstone|41570|6|Mentioned|p87|||||||||
5327|Deep Creek Siltstone|41585|4|Described|p105|||Mention P120.||||||14-APR-08
5327|Deep Creek Siltstone|42628|5|Briefly described|Map legend|Llandovery|Bolindian|||||||
5327|Deep Creek Siltstone|42790|5|Briefly described|Fig.14 P189|||||||||
5327|Deep Creek Siltstone|42826|2|Defined|p36|Early Silurian|Late Ordovician|||||||
5327|Deep Creek Siltstone|42827|4|Described|p105|||see also Table 4.1||||||
5327|Deep Creek Siltstone|44197|5|Briefly described|Map Legend||Early Silurian|||||||
5327|Deep Creek Siltstone|60599|5|Briefly described|p47 Fig. 19, p13|Llandovery|Bolindian|Supersedes Deep Creek Beds. Geological Province: Darraweit Guim Province, Melbourne Zone, Lachlan Fold Belt.||||||
5327|Deep Creek Siltstone|61185|5|Briefly described|p13, p21 Fig. 6|Llandovery|Bolindian|Overlies Darraweit Gum Formation. Mentioned in text as informal "Costerfield and Deep Creek siltstones": mud-dominated sediments, intensely bioturbated by bottom fauna. Shown on p21 Fig 6. as Deep Ck Siltstone.||||||07-FEB-11
5327|Deep Creek Siltstone|63083|5|Briefly described|p216 Tb. 1|Llandovery|Llandovery|||||||07-FEB-11
5327|Deep Creek Siltstone|64612|5|Briefly described|p27, p37|Early Llandovery|Early Llandovery|Of Murrindindi Supergroup. Basal unit. Contains burrows.||||||07-FEB-11
5327|Deep Creek Siltstone|68116|5|Briefly described|Appendix, Maps 32, 41.|Rhuddanian|Katian|Maximum age written as Bolindian in text.|||||Siltstone and sandstone: siltstone: dark grey-green, thin to thick-bedded, strongly bioturbated; sandstone: interbedded with siltstone; thin to very thin, commonly with ripple marks; rare conglomerate and diamictite; contains rare graptolites.|
72942|Deer Park basalt|61186|6|Mentioned|p45 Fig. 14|||Informal name for Victorian dimension stone. Probably named for the quarry locality.||||||
21636|Delatite Group|22559|6|Mentioned|p590|||||||||
21636|Delatite Group|22628|6|Mentioned|fig1p108|Devonian|Devonian|||||||
21636|Delatite Group|22729|4|Described|p583,591|Carboniferous|Late Devonian|Overlies Mansfield Group.||||||21-AUG-07
21636|Delatite Group|22971|6|Mentioned|p18||Carboniferous|||||||19-JAN-06
21636|Delatite Group|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
21636|Delatite Group|23309|4|Described|p171-184.||Devonian|||||||
21636|Delatite Group|23456|6|Mentioned|p60|||||||||
21636|Delatite Group|24004|5|Briefly described|p275 Fig.2|Devonian|Devonian|||||||
21636|Delatite Group|24177|6|Mentioned|p14, p78|||||||||
21636|Delatite Group|24551|5|Briefly described|p88 Fig. 3.15|Late Devonian|Late Devonian|Of the Avon Supergroup.||||||
21636|Delatite Group|44187|5|Briefly described|Map Legend||Late Devonian|||||||
21636|Delatite Group|60503|5|Briefly described|p28 Fig. 9|Carboniferous|Late Devonian|||||||
21636|Delatite Group|60599|6|Mentioned|p14||Middle Devonian|Post Tabberabberan deformation.||||||
21636|Delatite Group|61161|5|Briefly described|p125, p76-77 Fig 6.1|||Of Avon Supergroup. Includes: Kevington Creek Fm overlying Callemondah Conglomerate in Mansfield Basin; elsewhere only Moroka Glen Formation recognised. Underlies Wellington Volcanic Group and Mansfield Group. Fluvial sedimentary rocks. GSV map code: Dad.||||||
21636|Delatite Group|61163|6|Mentioned|p97|||Oldest group in the Avon Supergroup. Not present on the BUFFALO sheet.||||||
21636|Delatite Group|61169|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Includes Moroka Glen Formation.||||||
21636|Delatite Group|61170|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Includes Moroka Glen Formation.||||||07-FEB-11
21636|Delatite Group|61171|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Includes Moroka Glen Formation.||||||
21636|Delatite Group|61172|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Includes Moroka Glen Formation.||||||
21636|Delatite Group|61173|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Includes Moroka Glen Formation.||||||
21636|Delatite Group|61187|6|Mentioned|p5 Fig.3.|Late Devonian|Late Devonian|Melbourne Zone, Melbourne Terrane.||||||
21636|Delatite Group|64010|5|Briefly described|p258 Fig.1, p259. |||||Of the Avon Supergroup.|Includes the Kevington Creek Formation.|Is overlain by Wellington Volcanic Group.||
21636|Delatite Group|64536|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Of the Avon Supergroup. Includes Callemondah Conglomerate and Kevington Creek. Consists of a lower conglomerate/sandstone/mudstone unit, a middle sandstone unit and an upper formation of mudstone.minor sandstone/occasional conglomerate.||||||07-FEB-11
21636|Delatite Group|64537|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Of the Avon Supergroup. Includes Callemondah Conglomerate and Kevington Creek. Consists of a lower conglomerate/sandstone/mudstone unit, a middle sandstone unit and an upper formation of mudstone.minor sandstone/occasional conglomerate.||||||07-FEB-11
21636|Delatite Group|64538|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Of the Avon Supergroup. Includes Callemondah Conglomerate and Kevington Creek. Consists of a lower conglomerate/sandstone/mudstone unit, a middle sandstone unit and an upper formation of mudstone.minor sandstone/occasional conglomerate.||||||07-FEB-11
21636|Delatite Group|64606|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Of Avon Supergroup. Includes Kevington Creek Formation and Callemondah Conglomerate.||||||11-NOV-08
21636|Delatite Group|64616|4|Described|p132,p157,p182, p186-190, p301, p434-435|Givetian|Givetian|Of Avon Supergroup. Comprises Callemondah Conglomerate and Kevington Creek Formation. FT age of 197 +/- 18 Ma. Givetian age based on fossil fish fauna in Kevington Creek Formation. Folded and eroded in Late Devonian. Unconformably overlain by Highton Volcanics. Geophysical characteristics given.||||||05-SEP-18
21636|Delatite Group|67804|6|Mentioned|p65|Late Devonian|Middle Devonian|Of Mansfield Basin. Hosts the Gannons gold prospect.||||||
21636|Delatite Group|68116|5|Briefly described|Appendix, Map 34.|Late Devonian|Late Devonian||||||Red siltstone, minor sandstone, conglomerate.|
21636|Delatite Group|70629|6|Mentioned|p986|Late Devonian|Late Devonian|Melbourne Zone.||||||
5348|Delburn sandstones|42827|6|Mentioned|p340|||refers to Wright (1894)||||||
5352|Delegate River Mudstone|13996|6|Mentioned|p149|||||||||
5352|Delegate River Mudstone|22768|6|Mentioned|p177|Ludlow||||||||
5352|Delegate River Mudstone|22815|2|Defined|p38|Ludlow|Llandovery|||||||
5352|Delegate River Mudstone|22857|4|Described|p177, p466 App.1 Tb.A1.6|Ludlovian|Wenlockian|Of the Bredbo Group. Fissile mudstone, occasional siltstone, sandstone and limestone; fossiliferous. Max. thickness: 200m. Geological Province: Quidong Basin. ||||||
5352|Delegate River Mudstone|23329|5|Briefly described|1042|Late Silurian|Silurian|||||||
5352|Delegate River Mudstone|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
5352|Delegate River Mudstone|32672|6|Mentioned|p672|||||||||
5352|Delegate River Mudstone|34692|6|Mentioned|p187|||||||||
5352|Delegate River Mudstone|37727|4|Described|p55|||See also P19.||||||
5352|Delegate River Mudstone|38151|6|Mentioned|Table 1|||||||||
5352|Delegate River Mudstone|40328|3|Fully described|p87|||||||||
5352|Delegate River Mudstone|41869|6|Mentioned|p9|||||||||
5352|Delegate River Mudstone|43233|5|Briefly described|Map Legend||Ludlow|of Bredbo Group||||||
5352|Delegate River Mudstone|46574|5|Briefly described|Map Legend|Late Silurian|Silurian|Of the Yass-Canberra Rise. Geological Province: Lachlan Pre-Cratonic Province.  Mudstone, siltstone, sandstone, limestone.||||||09-NOV-04
5352|Delegate River Mudstone|60988|5|Briefly described|p143-146 |Late Silurian|Middle Silurian|Quidong Basin. Contains brachiopods which were compared with those in the Silverdale Formation.||||Conformably overlies the Quidong Limestone.||
24913|Dellicknora Granite|23309|5|Briefly described|p313|Silurian||(G70) - S-Type.  Supersedes Dellicknora Adamellite.||||||
24913|Dellicknora Granite|42726|5|Briefly described|map legend|Silurian||Variation on Dellicknora Adamellite.||||||
24913|Dellicknora Granite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Biotite-cordierite granite: medium grained, quartz pyhric; grey; S-type.|
37523|Demon Ridge Andesite Porphyry|61163|4|Described|p123, p36 Tb. 6.2|Late Devonian|Late Devonian|Float of contact-metamorphosed hornblende andesite surrounded by hornfels derived from Pinnak Sandstone.||||||
37523|Demon Ridge Andesite Porphyry|61174|5|Briefly described|map legend|Early Devonian|Early Devonian|Andesite porphyry: abundant hornblende phenocrysts, plagioclase glomerocrysts, rare quartz in a fine-grained recrystallised granoblastic groundmass of biotite, feldspar and quartz. I-type intrusion. GSV map code: G190.||||||07-FEB-11
37523|Demon Ridge Andesite Porphyry|61175|5|Briefly described|map legend|Early Devonian|Early Devonian|Andesite porphyry: abundant hornblende phenocrysts, plagioclase glomerocrysts, rare quartz in a fine-grained recrystallised granoblastic groundmass of biotite, feldspar and quartz. I-type intrusion. GSV map code: G190.||||||
37523|Demon Ridge Andesite Porphyry|61176|5|Briefly described|map legend|Early Devonian|Early Devonian|Andesite porphyry: abundant hornblende phenocrysts, plagioclase glomerocrysts, rare quartz in a fine-grained recrystallised granoblastic groundmass of biotite, feldspar and quartz. I-type intrusion. GSV map code: G190.||||||
37523|Demon Ridge Andesite Porphyry|61177|5|Briefly described|map legend|Early Devonian|Early Devonian|Andesite porphyry: abundant hornblende phenocrysts, plagioclase glomerocrysts, rare quartz in a fine-grained recrystallised granoblastic groundmass of biotite, feldspar and quartz. I-type intrusion. GSV map code: G190.||||||
37523|Demon Ridge Andesite Porphyry|61178|5|Briefly described|map legend|Early Devonian|Early Devonian|Hornblende-bearing andesite porphyry (I-type): small circular magnetic highs (30-70 nT); no discernible gravity response; moderate total radioelement, K, Th and U. GSV map code: G190.||||||
37523|Demon Ridge Andesite Porphyry|68116|5|Briefly described|Appendix, Map 26.|Devonian|Silurian||||||Andesite porphyry: abundant phenocrysts of hornblende, glomerocrysts of plagioclase, rare quartz in a finegrained recrystallised granoblastic groundmass of biotite, feldspar and quartz; hornblende partly replaced by actinolite and biotite.|
36796|Demons Bluff Group|23778|4|Described|p660|Oligocene|Eocene|Replaces Demons Bluff Formation. Overlain by Torquay Group. Underlain by Eastern View Group. In the Torquay Basin.||||||11-APR-07
36796|Demons Bluff Group|24038|5|Briefly described|p439 Fig.2|Oligocene|Eocene|Misspelt? - see Demons Bluff Formation. Geological Province: Torquay Basin||||||11-APR-07
36796|Demons Bluff Group|24551|5|Briefly described|p473 Fig. 15.4, p308|||||||||
36796|Demons Bluff Group|24562|6|Mentioned|p132|Oligocene|Eocene|Geological Province: Otway Basin.||||||
36796|Demons Bluff Group|61553|6|Mentioned|p614.|||Regional highstand sealing facies.||||||12-NOV-12
36796|Demons Bluff Group|62370|6|Mentioned|p455|||Geological Province: Torquay Basin||||||
36796|Demons Bluff Group|65316|4|Described|p595-7, p597 Fig 2, p601|Oligocene|Eocene|Torquay Basin. Probably correlates with Nirranda Group and Traralgon Formation. Originally defined as Demons Bluff Formation.|||Includes Angahook Formation and Anglesea Sand.|Overlain by Jan Juc Marl and Point Addis Limestone; overlies Eastern View Group.|Terrestrial and paralic sediments.|23-APR-12
36796|Demons Bluff Group|65715|5|Briefly described|p11 Tb.7|Paleogene|Paleogene|Previously called Demons Bluff Formation by Raggatt and Crespin (1955). Raised to group status by Trupp et al. (1994).||||||
36796|Demons Bluff Group|66002|5|Briefly described|p10 Tb.7|Paleogene|Paleogene|Called Demons Bluff Formation by Raggatt and Crespin (1955)||||||
36796|Demons Bluff Group|67061|5|Briefly described|pp545-546, p551.|Oligocene|Eocene|Terrestrial and paralic. Thickness from c.285-420 m. Rests on a mid-Eocene unconformity, above the Eastern View Group, dated c.40-39 Ma.|||Includes the basal Boonah Formation, Anglesea Siltstone and Angahook Formation at the top.|Unconformably overlies Eastern View Group. Is unconformably overlain by the Torquay Group.||16-MAR-12
36796|Demons Bluff Group|68116|5|Briefly described|Appendix, Maps 49-50, 55.|Oligocene|Eocene||||||Carbonaceous pyritic silt to fine sand, clay, and clayey sand; contains occasional shelly fossils and glauconite.|
36796|Demons Bluff Group|69297|6|Mentioned|p97, p145|Upper Oligocene|Eocene|Torquay Sub-basin of the Otway Basin and Bass Basin. Deposited in a shelfal marine environment. |||Includes the Boonah Formation, Salt Creek Formation, the Addiscot Formation, the Angahook Formation and the Anglesea Formation. |Unconformably overlies the Eastern View Formation. Overlain by the Torquay Group. ||
36796|Demons Bluff Group|70077|5|Briefly described|Regional: p5|Oligocene|Eocene|Bass Basin and Torquay Sub-basin. Marine shelfal sediments.|||Boonah and Anglesea Formations.|Unconformably overlies Eastern View Formation. Is overlain by Torquay Group.||
36796|Demons Bluff Group|73217|5|Briefly described|p1007, 1017, 1019, 1022|Cenozoic|Cenozoic|Eastern Otway Basin.|c.54-28 Ma.||Boonah, Anglesea, Angahook Formations.|Overlies Eastern View Formation. Is overlain by Torquay Group.||
41196|Den Hills Formation|50154|2|Defined|p127-131|Middle Jurassic|Middle Jurassic|Overlain by the Otway Group and Parilla Sand. Overlies Glenelg River Metamorphic Complex. Intrudes the Bacchus Marsh Formation. Locally interbedded with the Hypatia Formation. Thickness at type section: 100m. Age: 163 +/- 3 Ma (K/Ar), 156 +/- 2 Ma (K/Ar).||||||25-SEP-09
41196|Den Hills Formation|50155|5|Briefly described|Map Legend|Jurassic|Jurassic|Lava flows; trachyte, phonolite. Domes, laccoliths; trachyte, phonolite, microsyenite||||||
41196|Den Hills Formation|50156|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Domes and laccoliths: trachyte, phonolite and microsyenite; cream to dark grey equigranular to sanidine-phyric. Lava flows: trachyte, phonolite; cream to dark grey, fine grained; small phenocrysts of sanidine locally abundant.||||||
41196|Den Hills Formation|50157|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Domes and laccoliths: trachyte, phonolite and microsyenite; cream to dark grey equigranular to sanidine-phyric. Lava flows: trachyte, phonolite; cream to dark grey, fine grained; small phenocrysts of sanidine locally abundant.||||||
41196|Den Hills Formation|50158|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Domes and laccoliths: trachyte, phonolite and microsyenite; cream to dark grey equigranular to sanidine-phyric. Lava flows: trachyte, phonolite; cream to dark grey, fine grained; small phenocrysts of sanidine locally abundant.||||||
41196|Den Hills Formation|50159|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Domes and laccoliths: trachyte, phonolite and microsyenite; cream to dark grey equigranular to sanidine-phyric. Lava flows: trachyte, phonolite; cream to dark grey, fine grained; small phenocrysts of sanidine locally abundant.||||||24-JUN-04
41196|Den Hills Formation|50160|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Domes and laccoliths: trachyte, phonolite and microsyenite; cream to dark grey equigranular to sanidine-phyric. Lava flows: trachyte, phonolite; cream to dark grey, fine grained; small phenocrysts of sanidine locally abundant.||||||24-JUN-04
41196|Den Hills Formation|50161|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Overlies Bacchus Marsh Formation and Glenelg River Metamorphic Complex.  Domes and laccoliths: trachyte, phonolite and microsyenite. Lava flows: trachyte, phonolite; small phenocrysts of sanidine locally abundant.||||||25-JUN-04
41196|Den Hills Formation|50162|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Domes and laccoliths: trachyte, phonolite and microsyenite; cream to dark grey equigranular to sanidine-phyric. Lava flows: trachyte, phonolite; cream to dark grey, fine grained; small phenocrysts of sanidine locally abundant.||||||24-JUN-04
41196|Den Hills Formation|50163|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Domes and laccoliths: trachyte, phonolite and microsyenite; cream to dark grey equigranular to sanidine-phyric. Lava flows: trachyte, phonolite; cream to dark grey, fine grained; small phenocrysts of sanidine locally abundant.||||||24-JUN-04
41196|Den Hills Formation|50164|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Lava flows; trachyte, phonolite.||||||16-MAY-13
41196|Den Hills Formation|66002|5|Briefly described|p9 Tb.6|Mesozoic|Mesozoic|Of Coleraine Volcanic Group.  Defined by Morand et al. 2003.||||||
41196|Den Hills Formation|68116|5|Briefly described|Appendix, Maps 29, 38.|Jurassic|Jurassic|Informally subdivided into domes and laccoliths, and lava flows. Flow foliation common.|||||Domes and laccoliths: trachyte, phonolite and microsyenite; cream to dark grey, equigranular to sanidine-phyric; random felty texture. Lava flows: trachyte, phonolite; cream to dark grey, fine-grained; small phenocrysts of sanidine locally abundant.|
35340|Denicull Formation|24105|5|Briefly described|p158, 159|||Of the Loddon River Group.||||||
5377|Dennington Sand|31003|6|Mentioned|p41|||||||||
5377|Dennington Sand|31004|6|Mentioned|p395|||||||||
5377|Dennington Sand|34993|4|Described|p300|||||||||
5377|Dennington Sand|35722|6|Mentioned|Table 2|||Quaternary stratigraphic units and nature of components.||||||
5377|Dennington Sand|41769|6|Mentioned|p53|||||||||
5377|Dennington Sand|41848|4|Described|p375|||||||||
5377|Dennington Sand|42827|4|Described|p375|||see also Fig 9.2||||||
27389|Dergholm Granite|22531|6|Mentioned|p17|||||||||
27389|Dergholm Granite|23275|5|Briefly described|p473||Ordovician|||||||
27389|Dergholm Granite|23306|6|Mentioned|Map legend|||||||||
27389|Dergholm Granite|23309|5|Briefly described|p45, 47-48, 332, 337.|Ordovician|Ordovician|G424 A-Type. Age: 453+/-6Ma, 488+/-5Ma, 479+/-6 Ma, 484+/-24Ma, 452+/-22 Ma, 443+/-7 Ma. Supersedes Dergholm leucocratic Granite.||||||
27389|Dergholm Granite|24551|5|Briefly described|p20, 77|Early Ordovician|Early Ordovician|Now divided into Baileys Rocks Granite, Dergholm Granite and Poolaijelo Granite.  Age: 485 +/- 5Ma.||||||
27389|Dergholm Granite|30928|6|Mentioned|Map legend|Devonian|Ordovician|Ordovician - Devonian||||||
27389|Dergholm Granite|31624|6|Mentioned|p108|||||||||
27389|Dergholm Granite|31625|6|Mentioned|Fig. 5.2|||Palaeozoic||||||
27389|Dergholm Granite|31629|6|Mentioned|Fig. 5.1|||||||||
27389|Dergholm Granite|33236|6|Mentioned|p24|||||||||
27389|Dergholm Granite|33602|6|Mentioned|Fig.2|||||||||
27389|Dergholm Granite|34735|6|Mentioned|p12|||||||||
27389|Dergholm Granite|35112|6|Mentioned|Fig.9|||||||||
27389|Dergholm Granite|35278|5|Briefly described|p352|||||||||
27389|Dergholm Granite|37501|6|Mentioned|p416|||||||||
27389|Dergholm Granite|41850|6|Mentioned|p437|||||||||
27389|Dergholm Granite|42275|6|Mentioned|p468|||||||||
27389|Dergholm Granite|42827|5|Briefly described|p437|||||||||
27389|Dergholm Granite|42889|4|Described|p286|||age of 485 +/- 5 Ma, see also Fig.1 P276||||||
27389|Dergholm Granite|42971|6|Mentioned|p152|||||||||
27389|Dergholm Granite|43627|5|Briefly described|p15|||On HAMILTON.||||||28-OCT-04
27389|Dergholm Granite|44133|6|Mentioned|p55|||||||||
27389|Dergholm Granite|50154|2|Defined|p24, p107-109, p144|Late Ordovician|Early Ordovician|A-type. Subdivided into Baileys Rocks Granite, Dergholm Adamellite, Taltjeri Adamellite & Poolaijelo Adamellite by Kemp et al (2002), however considered here to be part of the one pluton.  Age: 490Ma to 450Ma. Geological Province: Delamerian Fold Belt.||||||15-SEP-04
27389|Dergholm Granite|50156|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite granite: massive, pink, medium to coarse grained, leucogranite; equigranular to weakly porphyritic in alkali feldspar; accessory magnetite and fluorite||||||
27389|Dergholm Granite|50157|5|Briefly described|Map Legend|Ordovician|Ordovician|Overlain by Duddo Limestone, Hypatia Formation and Eumeralla Formation. Biotite granite: massive, pink, medium to coarse grained, leucogranite; equigranular to weakly porphyritic in alkali feldspar; accessory magnetite and fluorite||||||25-JUN-04
27389|Dergholm Granite|50158|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite granite: massive, pink, medium to coarse grained, leucogranite; equigranular to weakly porphyritic in alkali feldspar; accessory magnetite and fluorite||||||
27389|Dergholm Granite|50159|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite granite: massive, pink, medium to coarse grained, leucogranite; equigranular to weakly porphyritic in alkali feldspar; accessory magnetite and fluorite||||||24-JUN-04
27389|Dergholm Granite|50160|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite granite||||||
27389|Dergholm Granite|50161|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite granite: massive, pink, medium to coarse grained, leucogranite; equigranular to weakly porphyritic in alkali feldspar; accessory magnetite and fluorite||||||24-JUN-04
27389|Dergholm Granite|50162|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite granite: massive, pink, medium to coarse grained, leucogranite; equigranular to weakly porphyritic in alkali feldspar; accessory magnetite and fluorite||||||24-JUN-04
27389|Dergholm Granite|50163|5|Briefly described|Map Legend|Ordovician|Ordovician|Overlain by Duddo Limestone. Biotite granite: massive, pink, medium to coarse grained, leucogranite; equigranular to weakly porphyritic in alkali feldspar; accessory magnetite and fluorite||||||25-JUN-04
27389|Dergholm Granite|50164|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite granite. Age: 485 +/- 5 Ma (K-Ar)||||||
27389|Dergholm Granite|61186|5|Briefly described|p54|||Med.- to coarse-gr.granite, slightly porphyritic red rock, shows distinct green tinge on polished surfaces. Phenocrystic feldspars, orange-pink with coarse to med-gr. groundmass of green and pink feldspars; intersecting joints and occasional xenoliths.||||||
27389|Dergholm Granite|63446|5|Briefly described|Map legend|Ordovician|Ordovician|No lithology given: is listed as Dergholm. G424.|||||A-type granite.|12-JUN-15
27389|Dergholm Granite|66002|5|Briefly described|p8 Tb.5|||G424. Defined by Wells 1956. See also Morand et al. 2003 who included Baileys Rocks Granite, Taltjeri Adamellite and Poolaijelo Adamellite of Kemp et al. (2002)||||||16-MAY-13
27389|Dergholm Granite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Early Ordovician||||||Biotite granite: massive, pink, medium to coarse grained, leucogranite; equigranular to weakly porphyritic in alkali feldspar; accessory magnetite and fluorite; magnetic to nonmagnetic.|
27389|Dergholm Granite|71593|4|Described|p23|Ordovician|Cambrian||c. 490-480 Ma (Morand et al., 2003)||||Post-tectonic, A-type granite.|
27389|Dergholm Granite|72313|6|Mentioned|p459 Table 2|||Delamerian Orogen. A-type.  Hf isotope data included.|488 Ma|||||
27389|Dergholm Granite|73118|5|Briefly described|p15, 42|||Western Victoria. Delamerian age. This age places an Early Ordovician age on the last regional deformation. A-type.|488 +/- 5 Ma (K-Ar: Turner et al., 1993).||||Undeformed granite.|
27389|Dergholm Granite|73430|6|Mentioned|p503|Cambrian|Cambrian|||||||
30530|Derndang Granite|22878|4|Described|p87|||||||||
30530|Derndang Granite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Leucocratic granite: largely concealed, pink, medium grained, massive; minor biotite, K-feldspar rich.||||||01-OCT-04
30530|Derndang Granite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Leucocratic granite: largely concealed, pink, medium grained, massive; minor biotite, K-feldspar rich.||||||01-OCT-04
30530|Derndang Granite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Leucocratic granite: Very highly magnetic (up to 500 nT). High K, low Th and U.||||||06-OCT-04
30530|Derndang Granite|23309|6|Mentioned|p429 App1|||G17 I-Type.||||||
30530|Derndang Granite|68116|5|Briefly described|Appendix, Maps 37, 46.|Early Devonian|Early Devonian||||||Leucocratic granite: pink, medium grained, massive; minor biotite, rich in K-feldspar.|
78965|Descartes Bay Member|73386|6|Mentioned|p14|||||Bridgewater Formation||||
24916|Detarka Ignimbrite|23309|4|Described|p109, Table 2.40|||Equiv of Carson Creek Ignimbrite.  Of the Little River Subgroup.  Max. Thickness: 120m.||||||
24916|Detarka Ignimbrite|23615|3|Fully described|p118|Early Devonian|Early Devonian|Of Little River Subgroup.  Fine grained mainly feldspathic ignimbrite, dark green but may vary in colour.  Age: Early Devonian ~410-395Ma. Maximum thickness:120m.||||||16-AUG-18
24916|Detarka Ignimbrite|23938|6|Mentioned|p55 Tb. 4|||Of the Snowy River Volcanics. See also p63-65 Figs. 23-24.||||||25-SEP-08
24916|Detarka Ignimbrite|24551|5|Briefly described|p144|||Of Little River Subgroup.||||||
24916|Detarka Ignimbrite|41585|5|Briefly described|p136|||Reserved as Detarka in June 1987.||||||
24916|Detarka Ignimbrite|43206|5|Briefly described|map legend||Lochkovian|Of Little River Subgroup.||||||25-SEP-08
24916|Detarka Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Feldspar ignimbrite: vitric with small compressed pumice fragments.|
23545|Deutgam Silt|37385|6|Mentioned|p18|||||||||
23545|Deutgam Silt|65715|4|Described|p15 Tb.8, p17|Neogene|Neogene|Formation rank. >30 m of reddish-brown, poorly-bedded silty and sandy clay with minor sand and gravel. Overlies Newer Volcanic Group. Flood plain deposit. Exposed along low bluffs on the coastline and along the Werribee River.||||||
23545|Deutgam Silt|68116|5|Briefly described|Appendix, Maps 41, 50.|Pleistocene|Pliocene||||||Silt, minor sand and gravel.|
29205|Devils Den Conglomerate|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Snowy River Volcanics||||||
29205|Devils Den Conglomerate|23309|4|Described|p109, 131  Table 2.40|||Maximum Thickness: 500m.||||||22-FEB-10
29205|Devils Den Conglomerate|23615|2|Defined|p108|Early Devonian|Early Devonian|Discussed by Howitt (1878) in his description of the Snowy River "Porphyries". Of Snowy River Volcanics. Overlies Glen Sheil Ignimbrite.  Thickness varies from 200-500m. Age: Early Devonian ~410-395Ma.||||||16-AUG-18
29205|Devils Den Conglomerate|23938|6|Mentioned|p63-65 Figs. 23-24.|||||||||
29205|Devils Den Conglomerate|24551|5|Briefly described|p144, p141 Fig.  5.32|||Of Snowy River Volcanics.||||||
29205|Devils Den Conglomerate|41585|4|Described|p136|||||||||
29205|Devils Den Conglomerate|43206|5|Briefly described|map legend||Ludlow|Of Snowy River Volcanics||||||
29205|Devils Den Conglomerate|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Unit in Snowy River Volcanics.|||Fluvial: conglomerate, sandstone, minor mudstone.|
29205|Devils Den Conglomerate|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Conglomerate, breccia, sandstone, minor siltstone, shale.|
74895|Devils Plain Siltstone Member|64536|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Fm (Mansfield Group). Mudstone, minor sandstone: mudstone is red, well bedded, ripple marks + mudcracks common; sandstone is thin bedded, fine-grained, feldspathic, lithic, micaceous, laterally extensive. Sst forms ledges,cuestas. Fluvial.||||||07-FEB-11
74895|Devils Plain Siltstone Member|64537|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Fm (Mansfield Group). Mudstone, minor sandstone: mudstone is red, well bedded, ripple marks + mudcracks common; sandstone is thin bedded, fine-grained, feldspathic, lithic, micaceous, laterally extensive. Sst forms ledges,cuestas. Fluvial.||||||07-FEB-11
74895|Devils Plain Siltstone Member|64538|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Fm (Mansfield Group). Mudstone, minor sandstone: mudstone is red, well bedded, ripple marks + mudcracks common; sandstone is thin bedded, fine-grained, feldspathic, lithic, micaceous, laterally extensive. Sst forms ledges,cuestas. Fluvial.||||||07-FEB-11
74895|Devils Plain Siltstone Member|64606|5|Briefly described|Map Legend|Neogene|Neogene|Of Snowy Plains Formation. Mudstone, minor sandstone: alluvial deposits. Speckled pink and green in RGB with locally moderate Th in regolith and red-pink and yellow near Mt Battery. Nonmagnetic.||||||
74895|Devils Plain Siltstone Member|64616|3|Fully described|p141, p299|Early Carboniferous|Early Carboniferous|Uppermost Member of Snowy Plains Formation. Type section details given. Conformably overlies Hearns Mudstone Member. ~600m thick. Red, well-bedded siltstone with minor fine-grained interbedded sandstone. Geophysical characteristics given.||||||
30557|Dicks Creek Ignimbrite|23309|4|Described|p112 Table 2.40|||Of the Timbarra Subgroup.  Maximum Thickness:>200m.||||||22-FEB-10
30557|Dicks Creek Ignimbrite|23615|4|Described|p92|Early Devonian|Early Devonian|Of Timbarra Subgroup.  Overlies Scorpion Creek Sandstone in the south and the Windarra Formation in the north.  Maximum thickness: 250m.||||||
30557|Dicks Creek Ignimbrite|24551|5|Briefly described|p142|||Of the Timbarra Subgroup.||||||
30557|Dicks Creek Ignimbrite|43206|5|Briefly described|map legend||Ludlow|Timbarra Subgroup||||||
30557|Dicks Creek Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Feldspar ignimbrite: pink vitric matrix with minor quartz phenocrysts; wispy pumice fragments.|
37267|Digger Island Marlstone|23309|4|Described|p54-58, p32 Fig. 2.7|Ordovician|Ordovician|Age: Lancefieldian.  Overlies: Corduroy Creek Gabbro (Unconformably).  Overlying unit: Bear Gully Chert Bed.||||||22-FEB-10
37267|Digger Island Marlstone|24002|5|Briefly described|p231|Early Ordovician|Early Ordovician|||||||
37267|Digger Island Marlstone|24098|5|Briefly described|p27 Fig. 2, p30|Early Ordovician|Early Ordovician|Unconformably overlies Maitland Beach Volcanics and Corduroy Creek Gabbro. Geological Province: Melbourne Zone, Lachlan Fold Belt (Waratah Bay Platform).||||||19-APR-05
37267|Digger Island Marlstone|24551|4|Described|p100, 605|Early Ordovician|Early Ordovician|Also referred to as Digger Island Formation and Digger Island Limestone in text.||||||
37267|Digger Island Marlstone|64616|6|Mentioned|p192, p343 Fig.23|Ordovician|Ordovician|Shallow marine. Richly fossiliferous.||||||
37267|Digger Island Marlstone|68116|5|Briefly described|Appendix, Maps 56-57.|Early Ordovician|Early Ordovician||||||Limestone, calcareous siltstone; basal conglomerate with chert and igneous rock fragments overlain by thick bedded dolomites with 'brecciated' tops, interbedded with breccia; most of the formation consists of thinly bedded, muddy limestone.|
37267|Digger Island Marlstone|70684|6|Mentioned|p7 Fig.1|||||||||
37267|Digger Island Marlstone|75070|5|Briefly described|p175, 179|Early Ordovician|Early Ordovician|Waratah Bay, southern Victoria. See also reference to Diggers Island Marl (p178).|||Bear Gully Chert Bed.|Overlies Bear Gully Chert Bed.|Fossiliferous marl.|
5489|Dilwyn Formation|12781|6|Mentioned|p386|Eocene|Eocene|Otway Basin. Maximum thickness 593m.||Wangerip Group.||Overlies Pember Mudstone, locally unconformably. Is overlain unconformably by Narrawaturk Marl.||
5489|Dilwyn Formation|22587|6|Mentioned|p79 Fig.7|Early Eocene|Late Paleocene|Of the Wangerrip Group.||||||16-APR-07
5489|Dilwyn Formation|22674|5|Briefly described|Fig.2 p719|Early Eocene|Early Eocene|||||||
5489|Dilwyn Formation|22875|3|Fully described|p14|Early Eocene|Early Eocene|Of Wangerrip Group.||||||16-APR-07
5489|Dilwyn Formation|22944|5|Briefly described|Fig3|Eocene|Paleocene|||||||
5489|Dilwyn Formation|23230|4|Described|Table4-1p40, 41|Eocene||||||||
5489|Dilwyn Formation|23238|5|Briefly described|p106||Tertiary|||||||
5489|Dilwyn Formation|23242|6|Mentioned|Fig11-4.1p158||Paleocene|||||||
5489|Dilwyn Formation|23307|5|Briefly described|Map Legend|Paleocene|Paleocene|Of Wangerrip Group.||||||16-APR-07
5489|Dilwyn Formation|23322|5|Briefly described|957 Fig.2|Middle Eocene|Late Paleocene|Of the Wangerrip Group. Geological Province: Gambier Basin.||||||07-SEP-09
5489|Dilwyn Formation|23402|5|Briefly described|p31|Early Eocene|Late Paleocene|||||||
5489|Dilwyn Formation|23778|5|Briefly described|p668|||Geological Province: Otway Basin.||||||
5489|Dilwyn Formation|24038|5|Briefly described|p439 Fig.2|Paleocene|Paleocene|Geological Province: Torquay Basin||||||12-JAN-10
5489|Dilwyn Formation|24056|5|Briefly described|p85|Paleocene|Paleocene|Of Wangerrip Group. Geological Basin: Otway Basin.||||||24-JUL-08
5489|Dilwyn Formation|24202|5|Briefly described|p313 Fig 2|Middle Eocene|Late Paleocene|Of the Wangerrip Group.  Geological Province: Gambier Sub-basin.||||||
5489|Dilwyn Formation|24314|5|Briefly described|p61 Fig.2|Eocene|Eocene|Geological Province: Otway Basin. Max. Thickness 593m. Of the Wangerrip Group.||||||30-NOV-04
5489|Dilwyn Formation|24397|5|Briefly described|p245|||Overlain by Sturgess Point Member. Geological Province: Otway Basin.||||||
5489|Dilwyn Formation|24455|5|Briefly described|p327|Early Eocene|Late Paleocene|Composed mainly of dark brown, carbonaceous sandy clay and silt, interbedded with fine- to medium-grained, clean to clayey sand , with minor coarse sand and gravel. Conformably overlies the Pebble Point Formation. Max. thickness: 150 See also p321 Fig. 1.||||||22-MAR-05
5489|Dilwyn Formation|24551|5|Briefly described|p246, 295, p732 Table 17.2|Eocene|Paleocene|Of the Wangerrip Group. Underlain by Pember Mudstone Member. Overlain by Burrungule Member. Max thickness: 1000m.||||||16-APR-07
5489|Dilwyn Formation|24562|5|Briefly described|p8 Fig. 2|Eocene|Eocene|Of the Wangerrip Group.  Geological Province: Otway Basin.||||||
5489|Dilwyn Formation|29355|6|Mentioned|p188|||||||||
5489|Dilwyn Formation|29823|6|Mentioned|p14|||||||||
5489|Dilwyn Formation|29824|4|Described|p16|||||||||
5489|Dilwyn Formation|29825|5|Briefly described|p18|||||||||
5489|Dilwyn Formation|29856|6|Mentioned|p36|||||||||
5489|Dilwyn Formation|30576|6|Mentioned|Table 1|||||||||
5489|Dilwyn Formation|30578|4|Described|p8|||||||||
5489|Dilwyn Formation|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
5489|Dilwyn Formation|30675|5|Briefly described|p253|||Lithology and radioactivity.||||||16-APR-07
5489|Dilwyn Formation|30676|5|Briefly described|p12|||||||||
5489|Dilwyn Formation|30905|6|Mentioned|p149|||||||||
5489|Dilwyn Formation|30932|6|Mentioned|Map legend|Eocene|Paleocene|Equivalent Dartmoor Formation, Palaeocene to Eocene.||||||22-SEP-18
5489|Dilwyn Formation|31036|1|Redefined|p208|Paleocene|Paleocene|See also p199. Table 9-1. Unit of Wangerrip Group.||||||16-APR-07
5489|Dilwyn Formation|31245|5|Briefly described|p68|||Middle Palaeocene. Unit of Wangerrip Group. See also p82.||||||16-APR-07
5489|Dilwyn Formation|31246|6|Mentioned|p56|||See also p57.||||||22-SEP-18
5489|Dilwyn Formation|31372|4|Described|p11|||See also p2, p9.||||||16-APR-07
5489|Dilwyn Formation|31424|4|Described|p14|||See also p7. Described from core.||||||16-APR-07
5489|Dilwyn Formation|31534|6|Mentioned|p363|||See also Table 19-3||||||
5489|Dilwyn Formation|31624|5|Briefly described|p105|||Lithology||||||
5489|Dilwyn Formation|31625|6|Mentioned|Fig. 5.2|||Palaeocene||||||
5489|Dilwyn Formation|31920|6|Mentioned|p60|||||||||
5489|Dilwyn Formation|31922|6|Mentioned|p166|||||||||
5489|Dilwyn Formation|32115|4|Described|p1|||Early Tertiary. See also Fig.1||||||
5489|Dilwyn Formation|32117|6|Mentioned|Fig.2|||||||||
5489|Dilwyn Formation|32120|6|Mentioned|p274|||Palaeocene fauna||||||
5489|Dilwyn Formation|32220|6|Mentioned|p9|||||||||
5489|Dilwyn Formation|32227|6|Mentioned|p26|||||||||
5489|Dilwyn Formation|32232|6|Mentioned|p19|||||||||
5489|Dilwyn Formation|32234|6|Mentioned|p26|||||||||
5489|Dilwyn Formation|32235|6|Mentioned|p34|||||||||
5489|Dilwyn Formation|32240|6|Mentioned|p26|||||||||
5489|Dilwyn Formation|32852|6|Mentioned|p10|||||||||
5489|Dilwyn Formation|32898|6|Mentioned|p29|||See also Table 2-1||||||
5489|Dilwyn Formation|33319|6|Mentioned|p167|||Fauna||||||
5489|Dilwyn Formation|33938|6|Mentioned|p48|||Refers Harris (1965).||||||
5489|Dilwyn Formation|33940|6|Mentioned|p414|||||||||
5489|Dilwyn Formation|34063|6|Mentioned|p2|||Paleocene. Table||||||
5489|Dilwyn Formation|34343|5|Briefly described|p97|||||||||
5489|Dilwyn Formation|34360|6|Mentioned|p11|||||||||
5489|Dilwyn Formation|34988|6|Mentioned|Table 9.4|||||||||
5489|Dilwyn Formation|35066|3|Fully described|p205|||||||||
5489|Dilwyn Formation|35285|6|Mentioned|p414|||||||||
5489|Dilwyn Formation|35722|6|Mentioned|p4|||Stratigraphy.||||||
5489|Dilwyn Formation|36305|6|Mentioned|p358|||||||||
5489|Dilwyn Formation|36366|6|Mentioned|p5|||||||||
5489|Dilwyn Formation|36913|6|Mentioned|p81|||||||||
5489|Dilwyn Formation|37548|4|Described|p129|||||||||
5489|Dilwyn Formation|38625|6|Mentioned|Table 2|||||||||
5489|Dilwyn Formation|38663|6|Mentioned|Fig.1|||||||||
5489|Dilwyn Formation|38932|5|Briefly described|p97|||See also Fig.4||||||
5489|Dilwyn Formation|39408|6|Mentioned|Fig.2|||||||||
5489|Dilwyn Formation|39446|6|Mentioned|p34|||||||||
5489|Dilwyn Formation|40003|5|Briefly described|p44|||||||||
5489|Dilwyn Formation|40230|6|Mentioned|p6|||||||||
5489|Dilwyn Formation|40521|6|Mentioned|Fig.2|||||||||
5489|Dilwyn Formation|40555|6|Mentioned|p51|||||||||
5489|Dilwyn Formation|40796|6|Mentioned|p218|||||||||
5489|Dilwyn Formation|41016|5|Briefly described|p214|||||||||
5489|Dilwyn Formation|41043|6|Mentioned|p95|||See also p99.||||||22-SEP-18
5489|Dilwyn Formation|41185|6|Mentioned|p178|||See also Fig.4||||||
5489|Dilwyn Formation|41269|5|Briefly described|p246|||||||||
5489|Dilwyn Formation|41517|6|Mentioned|p134|||||||||
5489|Dilwyn Formation|41642|6|Mentioned|p219|||||||||
5489|Dilwyn Formation|41701|6|Mentioned|Map legend|Eocene||||||||
5489|Dilwyn Formation|41704|6|Mentioned|Fig.3|||||||||
5489|Dilwyn Formation|41714|6|Mentioned|p301|||||||||
5489|Dilwyn Formation|41726|6|Mentioned|p421|||See also p427.||||||16-APR-07
5489|Dilwyn Formation|41769|4|Described|p22|||See also p23.||||||16-APR-07
5489|Dilwyn Formation|41868|4|Described|p535|||See also p548.||||||16-APR-07
5489|Dilwyn Formation|42079|6|Mentioned|Fig.2 P264|||||||||
5489|Dilwyn Formation|42152|6|Mentioned|p15|||||||||
5489|Dilwyn Formation|42318|5|Briefly described|p8|||||||||
5489|Dilwyn Formation|42361|6|Mentioned|p16|||||||||
5489|Dilwyn Formation|42453|6|Mentioned|p11|||Port Campbell Embayment||||||
5489|Dilwyn Formation|42524|5|Briefly described|Fig.3 p27|||||||||22-SEP-18
5489|Dilwyn Formation|42555|5|Briefly described|Fig.2 p285|||||||||22-SEP-18
5489|Dilwyn Formation|42599|5|Briefly described|Fig.3 p614|||||||||22-SEP-18
5489|Dilwyn Formation|42827|3|Fully described|p279|||Of Wangerrip Group.||||||16-APR-07
5489|Dilwyn Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
5489|Dilwyn Formation|43171|6|Mentioned|5-8|||Of Wangerrip Group. Age: 45-65Ma||||||
5489|Dilwyn Formation|43195|5|Briefly described|Map Legend|Eocene|Paleocene|See also commentary on back of map. Of Wangerrip Group.||||||16-APR-07
5489|Dilwyn Formation|43208|5|Briefly described|map legend||Early Eocene|Of Wangerrip Group.||||||16-APR-07
5489|Dilwyn Formation|43219|5|Briefly described|Fig.3,p6.||Eocene|Of Wangerrip Group.||||||16-APR-07
5489|Dilwyn Formation|43590|4|Described|p18||Early Eocene|||||||
5489|Dilwyn Formation|43660|6|Mentioned|Fig.6,p15|Eocene|Paleocene|||||||
5489|Dilwyn Formation|43733|6|Mentioned|Fig.2.11,p65||Eocene|||||||
5489|Dilwyn Formation|43744|6|Mentioned|Fig.3,p3|||||||||
5489|Dilwyn Formation|43797|5|Briefly described|p201||Eocene|||||||
5489|Dilwyn Formation|43799|5|Briefly described|p185|||||||||
5489|Dilwyn Formation|43814|6|Mentioned|Fig.3,p115|||||||||
5489|Dilwyn Formation|43937|5|Briefly described|Map Legend|Paleocene|Santonian|||||||
5489|Dilwyn Formation|44133|5|Briefly described|p154, 152 Fig. 10.2|Middle Eocene|Late Paleocene|Of the Wangerrip Group. Geological Province: Gambier Basin. Interfingers with Pember Mudstone. Thickness: 740m. ||||||
5489|Dilwyn Formation|47054|6|Mentioned|p490|||||||||
5489|Dilwyn Formation|48911|3|Fully described|p25|||||||||
5489|Dilwyn Formation|48977|6|Mentioned|Fig.5|||||||||
5489|Dilwyn Formation|60538|5|Briefly described|p470, 471 Fig. 10, 474 Fig. 13|Early Eocene|Early Eocene|Includes: Burrungule Member at top (but may? be base of Mepunga Sand Formation above). Geological Province: Otway Basin.||||||31-JAN-07
5489|Dilwyn Formation|60563|6|Mentioned|p45|||||||||16-JUN-05
5489|Dilwyn Formation|61017|5|Briefly described|p5 Fig. 2|Lutetian|thanetian|Of the Wangerrip Group. Geological Province: Otway Basin.||||||07-FEB-11
5489|Dilwyn Formation|61155|5|Briefly described|p3, p18|Middle Eocene|Late Paleocene|Of the Wangerrip (Knight) Group. Thick paralic sequences of sediments. Overlies Pebble Point Formation; interfingers with Eastern View Formation and Pember Mudstone. Max. thickness: 500m. Geological Province: Otway Basin.||||||03-MAR-10
5489|Dilwyn Formation|61181|6|Mentioned|p183|||Contains relatively pure sands for various forms of silica. Geological Province: Otway Basin. ||||||
5489|Dilwyn Formation|61182|3|Fully described|p19, p22-23, p32|Early Eocene|Early Eocene|Formerly Dilwyn Clay. Of Wangerrip Gp. Geol.Prov: Otway Basin. Considered by some to include Pember Mudstone which here is treated as a separate formation. Conformably overlies Pember Mudstone and Eumeralla Fm; overlain by Nirranda Gp. Lithology included.||||||06-JAN-10
5489|Dilwyn Formation|61470|5|Briefly described|p28 Fig. 5|Lutetian|Thanetian|Of the Wangerrip Group. Overlies and interfingers with Pember Mudstone.  Geological Province: Otway Basin.||||||12-OCT-05
5489|Dilwyn Formation|61547|6|Mentioned|p461 Fig.2. |Eocene|Eocene|||Unit in Wangerrip Group.||Overlies Pember Mudstone.||
5489|Dilwyn Formation|61622|5|Briefly described|p436 Fig. 2|Eocene|Eocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-FEB-11
5489|Dilwyn Formation|61623|6|Mentioned|p449 Fig. 4|Eocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-APR-09
5489|Dilwyn Formation|61626|5|Briefly described|p486, p486 Fig. 2|Eocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-APR-09
5489|Dilwyn Formation|61627|5|Briefly described|p500 Fig. 2|Eocene|Eocene|Of Wangerrip Group. Underlain by Pember Mudstone. Geological Province: Otway Basin.||||||07-FEB-11
5489|Dilwyn Formation|61628|5|Briefly described|p509 Fig. 3|Middle Eocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-APR-09
5489|Dilwyn Formation|62896|5|Briefly described|p88, p89|Early Eocene|Late Paleocene|Of the Wangerrip Group. Consists predominantly of quartz sand, often silty or clayey, sandy silt and clay, mudstone and clay.||||||07-FEB-11
5489|Dilwyn Formation|63122|5|Briefly described|p17 Fig. 4.3|Middle Eocene|Early Eocene|Of the Wangerrip Group. Max. thickness: 593m. Geological Province: Otway Basin. ||||||
5489|Dilwyn Formation|63124|3|Fully described|p49 Fig. 5.2, p87 Fig. 5.29, p89|Middle Eocene|Early Eocene|Supersedes Dilwyn "Clay", "Dartmoor Formation",  Knight Fm. Prob.syn.with Tartwaup Fm. Of Wangerrip Gp. Overlies Sherbrook Gp and Pember Sst. Over Narrawaturk + Gellibrand Marls + Greenways and Camelback Mbrs (Gambier Lst). Age: ~55-~48Ma. Max.thick: 593m||||||
5489|Dilwyn Formation|63129|6|Mentioned|p139|||Geological Province: Otway Basin. May contain potential reservoirs.||||||30-JAN-08
5489|Dilwyn Formation|63130|5|Briefly described|p146|||Overlain by Narrawaturk Marl. Geological Province: Otway Basin.||||||06-FEB-08
5489|Dilwyn Formation|63150|5|Briefly described|p99|||Contains plant microfossils. Geological province: Otway Basin.||||||
5489|Dilwyn Formation|63269|5|Briefly described|p605|Eocene|Eocene|Otway Basin.||Wangerrip Group.||||
5489|Dilwyn Formation|63431|5|Briefly described|p677 Fig. 2|Eocene|Eocene|Topmost unit of the Wangerrip Group. Geological Province: Penola Trough/Otway Basin.||||||26-JUN-13
5489|Dilwyn Formation|63740|5|Briefly described|p88|Early Eocene|Late Paleocene|Of Wangerrip Group. Geological province: Otway Basin. Consists predominantly of quartz sand, often silty or clayey, sandy silt and clay, mudstone and shale.||||||07-FEB-11
5489|Dilwyn Formation|65715|5|Briefly described|p11 Tb.7|Paleogene|Paleogene|Of Wangerrip Group. Includes Pember Mudstone Member. Called Dilwyn Clay by Baker (1953).||||||
5489|Dilwyn Formation|66002|4|Described|p10 Tb.7, p10 Tb.8, p11, p16, p26 Fig.7|Eocene|Eocene|Of Wangerrip Group. Called Dilwyn Clay by Baker (1953). Outcrops indistinguishable from Wiridjil Gravel or Moomowroong Sand. VandenBerg (2009) recommends that inland outcrops be mostly reassigned to Wiridjil Gravel. Overlies Gellibrand Marl. Sandy clay and silt||||||28-MAY-13
5489|Dilwyn Formation|66012|4|Described|p4, p6, p10 Tb.1, p17, p27, p30 Tb.3|Eocene|Paleocene|Seen in water bores. Channel gravel deposits and clean quartz sand, with thin interbeds of clayey sand and brown coal. Unconformably overlain by Heytesbury Group. 40m thick. Fluvial and swamp deposit. Northern extension of Wangerrip Group and probably Olney Formation| | | | | |16-FEB-15
5489|Dilwyn Formation|66245|5|Briefly described|p6 Fig.5. |Lutetian|Thanetian|||Unit in Wangerrip Group.||Overlies Pember Mudstone and Eastern View Formation.||
5489|Dilwyn Formation|67061|6|Mentioned|p546 Fig.3.|Eocene|Eocene|||Unit in Wangerrip Group.||||
5489|Dilwyn Formation|67366|5|Briefly described|p103 Fig.2. |Eocene|Eocene|||Unit in Wangerrip Group.||Overlies Pember Mudstone. Is unconformably overlain by Mepunga Formation.|Shallow to nearshore marine sandstone and shale.|
5489|Dilwyn Formation|67367|5|Briefly described|p131 Fig.2. |Middle Eocene|Early Eocene|||Unit in Wangerrip Group.||||
5489|Dilwyn Formation|68211|6|Mentioned|p28 Fig.1|Neogene|Paleogene|||||||
5489|Dilwyn Formation|68811|5|Briefly described|p110, p130, p156 app 1, p192 tbl 46|Tertiary|Tertiary|Hosts a confined aquifer. Up to 800m thick.  ||||Overlain by Gambier Limestone.|Interbedded quartz sand, finer grained sediment and clay horizons. |16-APR-20
5489|Dilwyn Formation|69297|5|Briefly described|p79, p98|Lutetian|Ypresian|Otway Basin.||Wangerrip Group||Overlies the Pember Mudstone. Unconformably overlain by the Mepunga Formation. |Siltstone and shale. |
5489|Dilwyn Formation|69651|5|Briefly described|p10|Eocene|Eocene|||Wangerrip Group.||Overlies Pember Mudstone. Is overlain unconformably by Mepunga, Demons Bluff and Eastern View Formations. Locally abuts Eastern View Formation.||
5489|Dilwyn Formation|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4; p5|Eocene|Eocene|Otway Basin.||Wangerrip Group.||Partly equivalent to and partly overlies Pember Mudstone. Is overlain by Mepunga Formation.||
5489|Dilwyn Formation|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Eocene|Eocene|Gambier Embayment and Voluta Trough.||Wangerrip Group.||Overlies Pember Mudstone. Is overlain by Mepunga Formation (Nirranda Group).||
5489|Dilwyn Formation|70193|6|Mentioned|p285 fig 3|||||||||
5489|Dilwyn Formation|70880|6|Mentioned|p77|Eocene|Eocene|Otway Basin.||||||
5489|Dilwyn Formation|71266|6|Mentioned|p614 Fig.3|Eocene|Eocene|Otway Basin.||||||
5489|Dilwyn Formation|71437|4|Described|Fig. 1 opp 154, p155, p159-161|Paleocene|Paleocene|[After Dilwyn Clay of Baker (1953)] Mainly of near-shore to lagoonal, brackish to fresh-water environment.||Upper unit of Wangerrip Group.|Includes Pember Mudstone Member, Dartmoor Sand Member.|Transitional or interfingering with Dartmoor Sand Member.|Laminated micaceous shales with minor layers of dolomite and clean to silty well-sorted quartz sands.|
5489|Dilwyn Formation|73357|5|Briefly described|p24, p28-29, p44, p46, p48|Bartonian|Ypressian|Otway Basin. Correlated with multiple biozones including Malvacipollis diversus Spore-Pollen Zone in lower part, Achilleodinium biformoides Dinocyst Zone in upper part. Often marginal to nearshore marine depositional environments, and Nothofagidites asperus Spore-Pollen Zone in upper part with variable non-marine to nearshore marine depositional environments.||Of Wangerrip Group?||Overlies Pember Mudstone, underlies Mepunga Formation.||
5489|Dilwyn Formation|73383|5|Briefly described|p3, p10 Tb.3.7, p24-25, p213, p246-247|Eocene|Eocene|Otway Basin. Approximately equivalent to chemostratigraphic package S5-P9 which has low Th/Sc values and high Si/Al values, Fe and P concentrations decrease upwards. Lithologies based on geochemistry using the ChemLith classification includes calcareous and argillaceous sandstones, and using the Herron classification (1988) includes quartz arenite, Fe-sand, sub-litharenite and subarkose. See also vi, p11 Tb.3.9, p82, p118, p131, p137-138, p258, p264-265.||Wangerrip Group||Overlies Pember Mudstone, underlies Nirranda Group, Mepunga Formation|Quartz-rich sandstone.|
5489|Dilwyn Formation|73385|5|Briefly described|p5|Eocene|Eocene|Otway Basin.||Wangerrip Group||Overlies Pember Mudstone, underlies Nirranda Group, Mepunga Formation.|Shallow marine and nearshore sandstones.|
5489|Dilwyn Formation|73386|4|Described|p4, p6, p12-13, Attachment A1|Bartonian|Ypressian|Otway Basin. Fluvial-deltaic to shallow-marine (inner shelf) depositional environment. Exhibits a stacked, aggradational stratal geometry that is thickest in the Portland Trough. Lower Malvacipollis diversus to Lower Nothofagidites asperus spore-pollen subzones.||Wangerrip Group||Overlies Pember Mudstone, underlies Mepunga Formation, Nirranda Group|Sandstones and mudstones, characterised by a sequence of clean, blocky marginal marine sandstones which transition upwards to a series of prograding parasequence sets.|
5489|Dilwyn Formation|73594|5|Briefly described|p4|Eocene|Eocene|Otway Basin.||Wangerrip Group||Overlies Pember Mudstone|Shallow marine and nearshore sandstones.|
35519|Dimboola Igneous Complex|23309|4|Described|p27-29, 25.  Table 2.1|Cambrian|Cambrian|||||||22-FEB-10
35519|Dimboola Igneous Complex|24311|5|Briefly described|p1060 Fig. 3|Cambrian|Cambrian|||||||
35519|Dimboola Igneous Complex|24551|5|Briefly described|p78|||||||||
35519|Dimboola Igneous Complex|50154|5|Briefly described|p17, p159|Cambrian|Cambrian|||||||
35519|Dimboola Igneous Complex|60451|4|Described|p21 Fig. 7, 23, 25, 41, 123|Early Cambrian|Early Cambrian|Includes: Williamson Road serpentinite. Ultramafic rocks.||||||
35519|Dimboola Igneous Complex|60454|5|Briefly described|Map Legend|Cambrian|Cambrian|Includes: Williamsons Road Serpentinite. Geological Province: Delamerian Fold Belt.||||||07-JUL-11
35519|Dimboola Igneous Complex|60456|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt. Includes: Williamsons Road Serpentinite.||||||27-JUL-15
35519|Dimboola Igneous Complex|60457|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delarmerian Fold Belt. Includes: Williamsons Road Serpentinite.||||||
35519|Dimboola Igneous Complex|60458|5|Briefly described|Map Legend|Cambrian|Cambrian|Includes: Williamsons Road Sepentinite.||||||
35519|Dimboola Igneous Complex|60459|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delarmerian Fold Belt. Includes: Williamsons Road Serpentinite. Mafic boninitic lava.||||||29-SEP-04
35519|Dimboola Igneous Complex|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Includes Williamson Road Serpentinite. Defined by VandenBerg et al. 2000.||||||
35519|Dimboola Igneous Complex|66769|6|Mentioned|p117|Cambrian|Cambrian|Oceanic and forearc rocks.||||||
35519|Dimboola Igneous Complex|67103|5|Briefly described|p613 Fig.6, 614, 617-618, 621-622|||Western Victoria. Not well imaged offshore due to sedimentary cover.||||Equivalent to Glasgow Volcanics (ANT).|NW-trending belt of mafic-ultramafic rocks: variably sheared and strongly magnetised island-arc tholeiitic basalts, boninitic lavas and boninitic cumulate-derived ultramafites and serpentinites.|
35519|Dimboola Igneous Complex|67104|6|Mentioned|p633, p635, p637|Middle Cambrian|Early Cambrian|?Early-Middle Cambrian age. May correlate in part with the Glasgow Volcanics of Antarctica.|||||Ophiolite.|
35519|Dimboola Igneous Complex|67105|6|Mentioned|p651-652|Middle Cambrian|Middle Cambrian|Western Victoria.|||||Calc-alkaline volcanics.|
35519|Dimboola Igneous Complex|68116|5|Briefly described|Appendix, Map 30.|Cambrian|Cambrian||||||Mafic and ultramafic lava including low-Ti boninite, tholeiite and cumulate gabbro, dolerite, diorite, granophyre; volcaniclastics; greenschist facies metamorphic overprint.|
35519|Dimboola Igneous Complex|68822|5|Briefly described|p317 Fig.1, p323, p331, pp344-355|Ediacaran|Ediacaran|~ 300 km long, magnetically prominent central zone that comprises km-wide fault slices within the Grampians-Stavely Zone.|ca. 600 Ma||||Comprises a deep element alkaline to MORB rift volcanics (c. 600 Ma) plus a shallower component of calkalkaline, tholeiitic-boninitic rocks.|
35519|Dimboola Igneous Complex|68823|6|Mentioned|p372 Fig.1.|||Delamerian Orogen.||||||
35519|Dimboola Igneous Complex|70744|6|Mentioned|p940|||W Victoria.||||||
35519|Dimboola Igneous Complex|70877|5|Briefly described|p10|||Grampians-Stavely Zone.|||||Ultramafic-tholeiite boninite.|
35519|Dimboola Igneous Complex|70967|6|Mentioned|p3, 6, 10, 12-14, 18-19|||NW Victoria.||||||
35519|Dimboola Igneous Complex|71593|5|Briefly described|p24, p31, p130, p167-p168|||Intersected by Mineral exploration drillholes in the vicinity of Dimboola; these intersected serpentinites form the type locality for this complex. Based on similarities between rocks of this unit and the Mount Stavely Volcanic Complex this 'Complex' is now considered redundant and all constituent rocks included within the latter.|||||Serpentinites.|
35519|Dimboola Igneous Complex|72445|6|Mentioned|p2, p9, p11-13, p17-19; App.7 p6 Fig.3.|Cambrian|Cambrian|Extends into far north-west Victoria. Associated with a highly magnetic package of igneous rocks of unresolved affinity that lies entirely under younger cover (VandenBerg et al., 2000; Crawford et al., 2003; Figure 1.2).||||||
35519|Dimboola Igneous Complex|73264|6|Mentioned|p1382 Fig.6, p1384 Fig.7, p1385 Fig.8|Cambrian Stage 3|Cambrian Stage 3|Delamerian Orogen, Grampians-Stavely Zone.|||||Includes Boninitic volcanics.|
21665|Dingo Hill Lava|23309|5|Briefly described|p106.   Fig 2.75|||||||||
21665|Dingo Hill Lava|23615|4|Described|p28, p133|Early Devonian|Early Devonian|Of Snowy River Volcanics.  Composed of pale red to greyish-orange or pink rhyolite lava with quartz and altered orange feldspar phenocrysts in a glassy groundmass.  Unconformably overlies the Devils Den Conglomerate.  See also p85 Fig. 46.||||||
21665|Dingo Hill Lava|24551|5|Briefly described|p142|||Not a formal stratigraphic name.||||||
21665|Dingo Hill Lava|43206|5|Briefly described|map legend||Lochkovian|||||||
21665|Dingo Hill Lava|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Extrusive, intrusive: rhyolite lava with quartz and feldspar phenocrysts; flow banded to autobrecciated.|
21666|Dinner Hill Gap Lava|23309|4|Described|p112. Table 2.40|||Of the Timbarra Subgroup.  Maximum Thickness: ~120m.||||||
21666|Dinner Hill Gap Lava|23615|3|Fully described|p25 Fig.7, p92|Early Devonian|Early Devonian|Of Timbarra Subgroup.  Composed of small rhyolite bodies and flanking breccia. Maximum thickness :120m.||||||
21666|Dinner Hill Gap Lava|24551|5|Briefly described|p142|||Of the Timbarra Subgroup.||||||
21666|Dinner Hill Gap Lava|43206|5|Briefly described|map legend||Ludlow|Timbarra Subgroup||||||
21666|Dinner Hill Gap Lava|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Rhyolite lava and rhyolite breccia.|
69409|Dinner Plain Tonalite|61160|3|Fully described|p74, p31 Tb. 5.2|Early Devonian|Early Devonian|Of Falls Creek Suite. I-type. Light grey, medium- to coarse-grained, equigranular biotite tonalite. Intrudes migmatite of Omeo Metamorphic Complex and the Cobungra Granite. See also p58-59 Fig. 6.8.||||||
69409|Dinner Plain Tonalite|61161|5|Briefly described|p92-93, p76-77 Fig 6.1|Early Devonian|Early Devonian|Of Falls Creek Suite. I-type. Light grey, fine to medium-grained, equigranular biotite tonalite: quartz, plagioclase, biotite, muscovite, and accessory apatite, zircon, opaques. Variable magnetic response. Age: inferred Early Devonian. GSV map code: G167.||||||
69409|Dinner Plain Tonalite|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Falls Creek Suite. Biotite tonalite: light grey; medium to coarse grained; equigranular; I-type intrusion. GSV map code: G167.||||||
69409|Dinner Plain Tonalite|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Falls Creek Suite. Biotite tonalite: light grey; medium to coarse grained; equigranular; I-type intrusion. GSV map code: G167.||||||
69409|Dinner Plain Tonalite|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Falls Creek Suite. Biotite tonalite: light grey; medium to coarse grained; equigranular; I-type intrusion. GSV map code: G167.||||||
69409|Dinner Plain Tonalite|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Falls Creek Suite. Biotite tonalite: light grey; medium to coarse grained; equigranular; I-type intrusion. GSV map code: G167.||||||07-FEB-11
69409|Dinner Plain Tonalite|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Falls Creek Suite. Biotite tonalite: I-type; highly magnetic in E (50-200 nT; kv = 20-50 X 10^-6 cgs), lower in W (0-40 nT); very low total radioelement, K, Th and U. GSV map code: G167.||||||
69409|Dinner Plain Tonalite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Falls Creek Suite. Biotite tonalite: light grey, medium to coarse-grained, equigranular; unfoliated; variably magnetic; I-type intrusion. GSV map code: G167.||||||
69409|Dinner Plain Tonalite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Falls Creek Suite. Biotite tonalite: light grey, medium to coarse-grained, equigranular; unfoliated; variably magnetic; I-type intrusion. GSV map code: G167.||||||07-FEB-11
69409|Dinner Plain Tonalite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Falls Creek Suite. Biotite tonalite: light grey, medium to coarse-grained, equigranular; unfoliated; variably magnetic; I-type intrusion. GSV map code: G167.||||||
69409|Dinner Plain Tonalite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Falls Creek Suite. Biotite tonalite: light grey, medium to coarse-grained, equigranular; unfoliated; variably magnetic; I-type intrusion. GSV map code: G167.||||||
69409|Dinner Plain Tonalite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Falls Creek Suite. Biotite tonalite: insufficient gravity data; weakly magnetic (0 to 20 nT, k < 1 x10^-6 cgs) and highly magnetic (110 to 300 nT, k up to 1610 x10^-6 cgs); low K, Th and total radioelements, moderate U. GSV map code: G167.||||||
69409|Dinner Plain Tonalite|68116|5|Briefly described|Appendix, Maps 27, 35.|Early Devonian|Early Devonian||||||Biotite tonalite: light grey, medium to coarse-grained, equigranular; unfoliated; variably magnetic.|
5530|Discovery Bay Sands|34988|5|Briefly described|p295|||||||||
5530|Discovery Bay Sands|41848|5|Briefly described|p370|||||||||
5530|Discovery Bay Sands|42827|4|Described|p370|||||||||
39124|Dja Dja Wrung Supergroup|64612|2|Defined|p29|Early Cambrian|Early Cambrian|Includes Heathcote Volcanic Group. Moore (2004) introduced the name to include all basaltic ocean floor rock units that were erupted and intruded during the Rodinian break-up event.||||||07-FEB-11
39124|Dja Dja Wrung Supergroup|65715|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Includes Heathcote Volcanic Group.||||||
39124|Dja Dja Wrung Supergroup|68189|6|Mentioned|p14, p38 and p40 in App.1||||||Includes the Magdala Volcanics and the Pitfield Volcanics.|||
39124|Dja Dja Wrung Supergroup|73496|5|Briefly described|Map legend|Cambrian|Cambrian||||Pitfield volcanics, Magdala volcanics||Tholeiitic to andesitic basalt, includes Pitfield volcanics and Magdala volcanics, magnetic responses typically 10 to 50 nT.|
39124|Dja Dja Wrung Supergroup|73497|5|Briefly described|Map legend|Cambrian|Cambrian||||Heathcote Volcanic Group||Includes basalt with pyritic shale, black shale, chert, jasper, dolerite sills; andesite with volcanic sediment; boninite with volcanic sediment; tholeiitic basalt to andesite; undifferentiated bands of highly magnetic and nonmagnetic rocks.|
39124|Dja Dja Wrung Supergroup|73505|5|Briefly described|p2, p5, p28|Cambrian|Cambrian|Present along major faults. More magnetic near granites, apparently due to contact metamorphism.||||Underlies the Saint Arnaud Group and Castlemaine Group in the south and west, Tueloga beds in the northeast. Conformably underlies Knowsley East Shale along the Mount William Fault.|Ocean floor basalts.|
39124|Dja Dja Wrung Supergroup|73576|5|Briefly described|p804|Cambrian|Cambrian|Lachlan Orogen, Bendigo Zone. Crops out along the Heathcote Fault.||||Underlies Castlemaine Group.|Mafic igneous volcanics.|
34820|Doctors Flat Tonalite|22968|5|Briefly described|P16, P200|Early Devonian|Late Silurian|Ages of unit are 412+/-13 Ma and 413+/-16 Ma, Parent is Ensay Suite||||||
34820|Doctors Flat Tonalite|23020|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Ensay Suite||||||
34820|Doctors Flat Tonalite|23028|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Ensay Suite||||||
34820|Doctors Flat Tonalite|23029|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Ensay Suite||||||
34820|Doctors Flat Tonalite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||14-SEP-04
34820|Doctors Flat Tonalite|23309|5|Briefly described|p.295, 296, 343|Early Devonian|Silurian|G517 I-Type.  Age: 413+/-16Ma, 412+/-13 Ma. Supersedes Doctors Flat Granite.||||||
34820|Doctors Flat Tonalite|24004|6|Mentioned|p283|||||||||
34820|Doctors Flat Tonalite|24551|6|Mentioned|p717 Table 2.4|Early Devonian|Silurian|Age: 412 +/- 13Ma.||||||
34820|Doctors Flat Tonalite|61161|6|Mentioned|p150|||Contact metamorphism - cordierite isograd follows shape of this unit. In ENSAY.||||||
34820|Doctors Flat Tonalite|68116|5|Briefly described|Appendix, Map 35,|Early Devonian|Early Devonian||||||Biotite-hornblende tonalite and granodiorite: grey; medium to coarse-grained; rare phenocrysts; massive to foliated; sporadic small mafic igneous enclaves.|
77690|Dog Trap Bay Sand|68991|3|Fully described|p465 Fig.2, pp467-472|Pleistocene|Pleistocene|Proposed name for channel deposits originally included in the Hanson Plain Sand by Shoemaker and Uhlherr (1995); this study considers these units to be stratigraphically and sedimentologically distinct. Type section details given. Named after Dog Trap Bay.|420-230 ka|||Disconformably overlain by the Cove Sand. Disconformably overlain by the Bridgewater Formation. Disconformably overlain by the Sturgess Sand.|Comprises consolidated but readily eroded, pale yellowish grey to pale and dark grey and brown, clayey, medium quartz sand, with minor coarse and fine quartz grains and some prominent more clayey bands commonly 2-5 cm thick.|20-JUL-15
5574|Dolodrook Limestone|22857|5|Briefly described|p89 Fig. 14.7A|Late Cambrian|Middle Cambrian|Of the Garvey Gully Sandstone.||||||11-JUL-11
5574|Dolodrook Limestone|22858|6|Mentioned|Fig14.7ap88-9|Late Cambrian|Late Cambrian|||||||
5574|Dolodrook Limestone|31572|6|Mentioned|Fig.|||Correlation chart 1. U.Cambrian||||||
5574|Dolodrook Limestone|33154|6|Mentioned|p1|||Cambrian||||||
5574|Dolodrook Limestone|33602|6|Mentioned|p22|||||||||
5574|Dolodrook Limestone|35073|6|Mentioned|p2|||||||||
5574|Dolodrook Limestone|35112|6|Mentioned|p280|||||||||
5574|Dolodrook Limestone|35274|6|Mentioned|Table.12.8|||||||||
5574|Dolodrook Limestone|35281|5|Briefly described|p17|||||||||
5574|Dolodrook Limestone|40746|5|Briefly described|p359|||||||||
5574|Dolodrook Limestone|40761|5|Briefly described|Table 1|||||||||
5574|Dolodrook Limestone|41571|4|Described|p54|||||||||
5574|Dolodrook Limestone|42827|5|Briefly described|p54|||||||||
5574|Dolodrook Limestone|45012|14|Not recorded|p32,|||early Upper Cambrian fauna.||||||
5574|Dolodrook Limestone|45130|6|Mentioned|p61|||||||||
5574|Dolodrook Limestone|46053|14|Not recorded|p.440|Late Cambrian|Middle Cambrian|Middle-early U.Cambrian.||||||
5574|Dolodrook Limestone|70901|14|Not recorded|p1|||Trilobite-brachipod assemblage.||||||
5597|Doncaster Siltstone|33020|5|Briefly described|p232|||Wenlockian. Semi-logarithmic plot.||||||
5607|Donna Buang Rhyodacite|23229|6|Mentioned|p37|||||||||
5607|Donna Buang Rhyodacite|23269|6|Mentioned|p406|||||||||
5607|Donna Buang Rhyodacite|23309|5|Briefly described|p165-167|Carboniferous|Devonian|See also Donna Buang Ignimbrite.||||||
5607|Donna Buang Rhyodacite|24551|5|Briefly described|p166|Devonian|Devonian|Of Acheron Volcanics Subgroup, Marysville Igneous Complex||||||
5607|Donna Buang Rhyodacite|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
5607|Donna Buang Rhyodacite|35073|6|Mentioned|p9|||See also Table 2.||||||
5607|Donna Buang Rhyodacite|35277|6|Mentioned|p91|||||||||
5607|Donna Buang Rhyodacite|39291|6|Mentioned|Table 1|||||||||
5607|Donna Buang Rhyodacite|40725|6|Mentioned|Fig.1|||||||||
5607|Donna Buang Rhyodacite|41641|6|Mentioned|p162|||||||||
5607|Donna Buang Rhyodacite|42154|6|Mentioned|Table 1 P334|||||||||
5607|Donna Buang Rhyodacite|44187|5|Briefly described|Map Legend||Late Devonian|||||||
5607|Donna Buang Rhyodacite|68116|5|Briefly described|Appendix, Map 42.|Late Devonian|Late Devonian||||||Rhyodacite: light to dark grey according to degree of crystallization; phenocrysts of plagioclase, biotite, enstatite, rare quartz and K-feldspar; groundmass coarsens towards the top; contains large lithic fragments of underlying rhyodacite.|
27761|Donnellys Creek Siltstone|23309|4|Described|p143, 145, 146, 152.  Table 2.53/2.54||Silurian|Age: Llandovery.||||||15-JAN-09
27761|Donnellys Creek Siltstone|24177|5|Briefly described|p50 Fig.22|Early Devonian|Late Silurian|Geological Province: Mount Easton Province.||||||
27761|Donnellys Creek Siltstone|24214|6|Mentioned|p788 Fig. 2|||||||||
27761|Donnellys Creek Siltstone|24551|5|Briefly described|p88 Fig. 3.15|Silurian|Silurian|Of Jordan River Group.||||||27-OCT-08
27761|Donnellys Creek Siltstone|38787|6|Mentioned|p139|||||||||
27761|Donnellys Creek Siltstone|41585|4|Described|p118|||||||||
27761|Donnellys Creek Siltstone|42827|5|Briefly described|p118|||||||||
27761|Donnellys Creek Siltstone|44187|5|Briefly described|Map Legend||Early Silurian|||||||
27761|Donnellys Creek Siltstone|60599|5|Briefly described|p47 Fig. 19|Lochkovian|Pridolian|Geological Province: Melbourne Zone, Lachlan Fold Belt.||||||
27761|Donnellys Creek Siltstone|64535|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Dark grey to green grey, finely banded and bioturbated siltstone; rare sandstone, very thinly bedded; deep marine hemipelagic and mass flow deposits. ||||||
27761|Donnellys Creek Siltstone|64536|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Includes Cherrytree Gap Sandstone Member. Dark grey to green grey, finely banded and bioturbated siltstone; rare sandstone, very thinly bedded; deep marine hemipelagic and mass flow deposits.||||||07-FEB-11
27761|Donnellys Creek Siltstone|64537|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Includes Cherrytree Gap Sandstone Member. Dark grey to green grey, finely banded and bioturbated siltstone; rare sandstone, very thinly bedded; deep marine hemipelagic and mass flow deposits.||||||07-FEB-11
27761|Donnellys Creek Siltstone|64538|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Includes Cherrytree Gap Sandstone Member. Dark grey to green grey, finely banded and bioturbated siltstone; rare sandstone, very thinly bedded; deep marine hemipelagic and mass flow deposits.||||||07-FEB-11
27761|Donnellys Creek Siltstone|64539|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Dark grey to green grey, finely banded and bioturbated siltstone; rare sandstone, very thinly bedded; deep marine hemipelagic and mass flow deposits. ||||||
27761|Donnellys Creek Siltstone|64540|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Dark grey to green grey, finely banded and bioturbated siltstone; rare sandstone, very thinly bedded; deep marine hemipelagic and mass flow deposits. ||||||
27761|Donnellys Creek Siltstone|64605|5|Briefly described|Map legend|Silurian|Silurian|Of the Jordan River Group. Siltstone, rare sandstone; deep-marine deposits. Yellow-white to speckled pink-blue-brown in RGB. Nonmagnetic.||||||17-NOV-08
27761|Donnellys Creek Siltstone|64606|5|Briefly described|Map Legend|Early Silurian|Middle Ordovician|Of Jordan River Group. Siltstone, minor sandstone: deep-marine deposits. Blue-brown to white in RGB. Nonmagnetic.||||||17-NOV-08
27761|Donnellys Creek Siltstone|64616|3|Fully described|p80, p175-176, p183 Fig.6.29, p184-185|Llandovery|Llandovery|See also p189, p197 Fig.6.34, p201 Tb.7.1, p291, p305. Of Jordan River Group. Includes Cherrytree Gap Sandstone Member. Conformably overlies Lazarini Siltstone. Conformably underlies McAdam Sandstone. Type section location given. 375-900m thick. Dark grey to green-grey, finely banded and bioturbated siltstone;  rare, very thinly-bedded sandstone. Age inferred from relationships. Geophysical characteristics given.||||||
27761|Donnellys Creek Siltstone|68116|5|Briefly described|Appendix, Maps 33-34, 43, 52.|Aeronian|Rhuddanian||||||Siltstone, rare sandstone: siltstone dark grey to green-grey; finely banded and bioturbated; sandstone very thinly bedded.|
37545|Dookie Igneous Complex|23309|5|Briefly described|p25, 28, 32, 33. Table 2.1,2.4|Cambrian|Cambrian|||||||
37545|Dookie Igneous Complex|24551|6|Mentioned|p90|||||||||
37545|Dookie Igneous Complex|64616|6|Mentioned|p313 Fig.2|||||||||
37545|Dookie Igneous Complex|65969|5|Briefly described|p11, p18 Fig.8|||Basalt, gabbro and chert. In WANGARATTA 1:250 000 sheet.||||||
37545|Dookie Igneous Complex|66769|5|Briefly described|136-138, 156|Cambrian|Cambrian|Stratigraphic and structural equivalent to the Lickhole Volcanic Group. Includes Cambrian tholeiitic basalt and gabbro. Basal succession to the 'Tabberabbera Zone'.||||||
37545|Dookie Igneous Complex|68116|5|Briefly described|Appendix, Map 18.|Cambrian|Cambrian||||||Basalt, microgabbro, gabbro, pyroxenite; affected by low-grade regional metamorphism, with development of albite, actinolite, chlorite, epidote and sericite.|
37545|Dookie Igneous Complex|70601|5|Briefly described|p47|||Correlates with tholeiite of Lickhole Volcanics. Underlies Howqua Chert.|ID-TIMS zircon 502 +/- 0.7 Ma.|||Is overlain by Howqua Chert.|Tholeiitic: gabbro pegmatite, gabbro, basalts.|
37545|Dookie Igneous Complex|73497|5|Briefly described|Map legend|Cambrian|Cambrian|||||Overlies Mount William Metabasalt|Undifferentiated: highly magnetic boninite, gabbro and basalt (up to 400 nT), nonmagnetic chert and possibly dolerite and boninite; gravity response to 120 micrometres/second/second above the regional.|
21683|Doonarlik Ignimbrite|23309|4|Described|p110.  Table 2.40|||Maximum Thickness: ~130m.  Of the Mount Dawson Subgroup.||||||
21683|Doonarlik Ignimbrite|23615|3|Fully described|p105|Early Devonian|Early Devonian|Of Mount Dawson Subgroup.  Overlain by Doyle Gully Ignimbrite, overlies Dead Cattle Gully Ignimbrite. Maximum thickness: 130m.  A distinctive lithology, with euhedral and broken white to light green feldspar crystals set in dark welded groundmass.||||||
21683|Doonarlik Ignimbrite|43206|5|Briefly described|map legend||Ludlow|Of Mount Dawson Subgroup.||||||
21683|Doonarlik Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Feldspar ignimbrite: dark; white to green euhedral feldspar phenocrysts.|
37716|Double Bull Granodiorite|23309|6|Mentioned|p429, Appendix 1|||G56, I-Type.  Supersedes Double Bull Granite.||||||17-MAY-06
37716|Double Bull Granodiorite|23938|5|Briefly described|p70 Tb. 6|Devonian|Devonian|See also p111 Fig. 51.||||||25-SEP-08
37716|Double Bull Granodiorite|24551|6|Mentioned|p439|||||||||
37716|Double Bull Granodiorite|44185|5|Briefly described|Map legend.|||I-type. Age uncertain: shown as SDg, ie Silurian-Devonian.||||||
37716|Double Bull Granodiorite|60542|4|Described|p88, p19 Fig. 3|Late Silurian|Late Silurian|Of Bete Bolong Suite. See also Double Bull Granite. Less mafic than Bete Bolong Granite, therefore separately named - large honrblende crystals. Intruded the Pinnak Sandstone.||||||04-JUN-14
37716|Double Bull Granodiorite|61187|5|Briefly described|p114, p122, p123 Fig.8.|||Cu mineralisation was found at the northern end of this pluton, and the Stringers Knob Prospect at the southern end. Written as Double Bull Creek Granite in Fig.8.||Unit in Bete Belong Suite.||||
37716|Double Bull Granodiorite|68116|5|Briefly described|Appendix.|Devonian|Silurian||||||Hornblende granodiorite: grey-green, coarse-grained, weathered; I-type.|
5658|Doughboy Island Granite|23309|6|Mentioned|p429, App1|||G250 S-Type.||||||
5658|Doughboy Island Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
21688|Douglas Ignimbrite|23309|5|Briefly described|p123, 134.  Table 2.47|||||||||
21688|Douglas Ignimbrite|23615|3|Fully described|p97|Early Devonian|Early Devonian|Of White Monkey Subgroup.  Overlies Bass Camp Ignimbrite.  Previously included in the Black Mountain Rhyodacite of Ringwood (1955a). Maximum thickness: ~180m.||||||
21688|Douglas Ignimbrite|24551|5|Briefly described|p149, p132 Fig.5.23|||Of White Monkey Volcanics||||||
21688|Douglas Ignimbrite|43206|5|Briefly described|map legend||Ludlow|OF White Monkey Subgroup.||||||
21688|Douglas Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Early Devonian|Early Devonian||||||Feldspar ignimbrite: brown with minor quartz phenocrysts and abundant red pumice fragments.|
5678|Doutta Galla Silt|24551|6|Mentioned|p348, 609|Holocene|Pleistocene|||||||
5678|Doutta Galla Silt|30995|5|Briefly described|p31|||||||||
5678|Doutta Galla Silt|32008|5|Briefly described|p63|||Age. Fossil mammals||||||
5678|Doutta Galla Silt|41848|5|Briefly described|p386|||||||||
5678|Doutta Galla Silt|42827|5|Briefly described|p386|||||||||
5678|Doutta Galla Silt|71203|14|Not recorded|p207|||River Terraces.||||||
21692|Doyle Gully Ignimbrite|23309|4|Described|p110.  Table 2.40|||Maximum Thickness:~200m.  Of the Mount Dawson Subgroup.||||||
21692|Doyle Gully Ignimbrite|23615|3|Fully described|p105|Early Devonian|Early Devonian|Of Mount Dawson Subgroup.  Overlain by Bimmarn Ignimbrite, overlies Doonarlik Ignimbrite.  Consistently feldspathic with minor visible quartz, containing distinctive angular, green clasts and abundance of lithic fragments, variable in colour.||||||04-JUN-14
21692|Doyle Gully Ignimbrite|43206|5|Briefly described|map legend||Ludlow|Of Mount Dawson Subgroup.||||||
21692|Doyle Gully Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Early Devonian|Silurian||||||Feldspar ignimbrite with small quartz and angular altered green lithic clasts.|
5705|Dromana Granite|23234|6|Mentioned|p91|||||||||
5705|Dromana Granite|23274|5|Briefly described|p446, 457||Late Devonian|||||||
5705|Dromana Granite|23275|5|Briefly described|p471|||||||||
5705|Dromana Granite|23309|5|Briefly described|p170, 343|||G262. Intrudes Late devonian volcanics.||||||
5705|Dromana Granite|24551|5|Briefly described|p162|||||||||
5705|Dromana Granite|31080|5|Briefly described|p48|||||||||
5705|Dromana Granite|31510|5|Briefly described|p9|||See also Table 1.||||||
5705|Dromana Granite|33237|6|Mentioned|p53|||||||||
5705|Dromana Granite|35277|6|Mentioned|p97|||||||||
5705|Dromana Granite|35278|5|Briefly described|p355|||||||||
5705|Dromana Granite|35290|5|Briefly described|p21|||See also P20.||||||
5705|Dromana Granite|35712|6|Mentioned|Table 6|||||||||
5705|Dromana Granite|41641|6|Mentioned|p167|||||||||
5705|Dromana Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
5705|Dromana Granite|42827|6|Mentioned|p167|||||||||
5705|Dromana Granite|61186|6|Mentioned|p41, p55|||Green-brown dimension stone used in the church in Wangaratta. Granite is medium-grained with no xenoliths; variable in colour. ||||||
5705|Dromana Granite|63445|5|Briefly described|Map legend.|Late Devonian|Late Devonian||||||I-type granite.|
5705|Dromana Granite|64769|6|Mentioned|p26|||VIC.||||||05-MAY-09
5705|Dromana Granite|68116|5|Briefly described|Appendix, Maps 50-51.|Late Devonian|Late Devonian||||||Biotite granite: greenish, medium-grained, equigranular granite containing quartz, greenish orthoclase, perthite, oligoclase and biotite with accessory sphene, zircon, ilmenite and apatite; intruded by dykes of porphyry and aplite.|
5705|Dromana Granite|71205|14|Not recorded|p215||Upper Devonian|Probable Upper Devonian age.||||||
5706|Dromana Suite|24551|6|Mentioned|p225, 709|||||||||
5706|Dromana Suite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
5706|Dromana Suite|42827|5|Briefly described|p435|||||||||
26527|Drummer Granodiorite|22878|6|Mentioned|p8|||||||||
26527|Drummer Granodiorite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Of the Bemboka Supersuite. Biotite-hornblende granodiorite: grey, medium to coarse grained, massive; compositionally zoned with two biotite granite phases.||||||01-OCT-04
26527|Drummer Granodiorite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Bemboka Supersuite. Biotite-hornblende granodiorite: grey, medium to coarse grained, massive; compositionally zoned with two biotite granite phases.||||||01-OCT-04
26527|Drummer Granodiorite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Bemboka Supersuite. Biotite-hornblende granodiorite: Highly magneitc (150-175 nT). High K over fresh outcrop and low K and U where the granodiorite is weathered.||||||06-OCT-04
26527|Drummer Granodiorite|23309|6|Mentioned|p430 App1|||G16 I-Type. Supersedes Drummer Granite.||||||
26527|Drummer Granodiorite|30574|5|Briefly described|p10|||||||||
26527|Drummer Granodiorite|30938|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
26527|Drummer Granodiorite|35278|6|Mentioned|p359|||||||||
26527|Drummer Granodiorite|41850|6|Mentioned|p430|||||||||
26527|Drummer Granodiorite|42827|5|Briefly described|p430|||||||||
26527|Drummer Granodiorite|68116|5|Briefly described|Appendix, Maps 37, 46.|Early Devonian|Early Devonian||||||Biotite-hornblende granodiorite: grey, medium to coarse grained massive; compositionally zoned with two biotite granite phases; I-type.|
5712|Drummer Suite|22878|6|Mentioned|p77|||||||||
5712|Drummer Suite|24551|6|Mentioned|p235|||||||||
5712|Drummer Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Bemboka Supersuite.  Includes the Drummer and Future Trail Granites.||||||07-FEB-05
5712|Drummer Suite|42827|5|Briefly described|p430|||||||||
69423|Dry Gully Granodiorite|61161|5|Briefly described|p107-108, p151, p76-77 Fig 6.1|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Intrudes dykes of Bundara Munjie Quartz Diorite. Fine to medium grained, porphyritic, biotite-bearing granodiorite. Non- to moderately magnetic. Age: inferred Early Devonian. GSV map code: G468.||||||
69423|Dry Gully Granodiorite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite granodiorite: fine to medium-grained, porphyritic; with large euhedral plagioclase phenocrysts in a groundmass of quartz, plagioclase, K-feldspar, biotite, muscovite; I-type intrusion. GSV map code: G468.||||||
69423|Dry Gully Granodiorite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite granodiorite: fine to medium-grained, porphyritic; with large euhedral plagioclase phenocrysts in a groundmass of quartz, plagioclase, K-feldspar, biotite, muscovite; I-type intrusion. GSV map code: G468.||||||07-FEB-11
69423|Dry Gully Granodiorite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite granodiorite: fine to medium-grained, porphyritic; with large euhedral plagioclase phenocrysts in a groundmass of quartz, plagioclase, K-feldspar, biotite, muscovite; I-type intrusion. GSV map code: G468.||||||
69423|Dry Gully Granodiorite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite granodiorite: fine to medium-grained, porphyritic; with large euhedral plagioclase phenocrysts in a groundmass of quartz, plagioclase, K-feldspar, biotite, muscovite; I-type intrusion. GSV map code: G468.||||||
69423|Dry Gully Granodiorite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Biotite granodiorite: low gravity response (-430 ums^-2); weakly magnetic (50 nT) with moderately magnetic margins (100 nT, k up to 110 x10^-6 cgs); moderate K, Th and total radioelements, low U. GSV map code: G468.||||||
69423|Dry Gully Granodiorite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Silurian||||||Biotite granodiorite; fine to medium-grained, porphyritic; with large euhedral plagioclase phenocrysts in a groundmass of quartz, plagioclase, K-feldspar, biotite, muscovite.|
34852|Dry Hill Granodiorite|22968|5|Briefly described|P71, P197||Late Silurian|Parent is Polar Star Suite||||||
34852|Dry Hill Granodiorite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Polar Star Suite.||||||
34852|Dry Hill Granodiorite|23309|6|Mentioned|p430 App1|||G147 I-Type.||||||
34852|Dry Hill Granodiorite|24551|6|Mentioned|p230|||||||||
34852|Dry Hill Granodiorite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Biotite granodiorite: grey; medium-grained; massive to strongly foliated; minor fine-grained granodiorite.|
37546|Duchembegarra Granite|23309|5|Briefly described|p44|Devonian|Devonian|Age: 404+6Ma. Also referred to as Duchembegarra granite and Duchembegarra Tonalite throughout text.||||||
37546|Duchembegarra Granite|70877|6|Mentioned|p13|Early Devonian|Late Silurian|||||Intrudes the Grampians Group.||
37546|Duchembegarra Granite|70967|6|Mentioned|p11|||Mount Stavely Belt.||||Intrudes Grampians Group. Co-magmatic with Rocklands Volcanic Group.||
37546|Duchembegarra Granite|72445|5|Briefly described|p10.|Early Devonian|Late Silurian|||||Intrudes Grampians Group. Comagmatic with Rocklands Volcanic Group.||
37546|Duchembegarra Granite|73118|5|Briefly described|p6, 19-20, 34, 73-74, 237-238|Early Devonian|Early Devonian|Glenelg Zone, Western Victoria. Drill core summary log.|404 +/- 6 Ma (tonalite phase).|||Has metamorphosed the Grampians Group locally (Mt. Arapiles).|Includes a late-stage mafic tonalite.|
40269|Duck Bay Volcanics|23911|4|Described|p95 Fig. 9B|Tithonian|Tithonian|Geological Province: Gippsland Basin.  Overlying Unit: Tyers Subgroup.  Of the Strzelecki Group.||||||
40269|Duck Bay Volcanics|24164|6|Mentioned|p15 Fig.8|Jurassic|Jurassic||||||Mafic|
40269|Duck Bay Volcanics|24551|5|Briefly described|p262 Fig. 9.29|Early Cretaceous|Jurassic|Of the Strzelecki Group.||||||
40269|Duck Bay Volcanics|61302|5|Briefly described|p11 Fig.4|Late Jurassic|Late Jurassic|Of the Strzelecki Group. Geological Province: Gippsland Basin.||||||
40269|Duck Bay Volcanics|65718|6|Mentioned|p10 Fig 3.2|Jurassic|Jurassic|||||||
40269|Duck Bay Volcanics|75065|6|Mentioned|p156|Tithonian|Tithonian|Gippsland Basin. Marks the onset of rifting in the Basin.||Strzelecki Group.||||
5752|Duddo Limestone|2967|5|Briefly described|p14, p15 Fig.2.2, p24, 29, 42, 155-156|Miocene|Oligocene|Lawrence (1966). Western Murray Basin. Up to 130m thick. A major (water) aquifer. See also p158.||Murray Group.||Overlies Ettrick Marl conformably and diachronously. Is separated from the unconformably overlying Bookpurnong beds by the Mologa Surface. Grades laterally into Winnambool Formation.|Buff-coloured, bryozoal calcarenite, with interbedded layers of calcisiltite and calcilutite.|
5752|Duddo Limestone|10010|5|Briefly described|p12 Fig. 3||Early Miocene|Of the Murray Group. Geological Province: Murray Basin.||||||13-AUG-07
5752|Duddo Limestone|22773|5|Briefly described|Fig24.8p352+24.9p353|||||||||
5752|Duddo Limestone|22799|2|Defined|p32|Middle Miocene|Late Oligocene|||||||
5752|Duddo Limestone|22857|5|Briefly described|p352 Fig.24.8, p353 Fig. 24.9|Early Miocene|Late Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||
5752|Duddo Limestone|22887|5|Briefly described|Fig.6 p13||Early Miocene|||||||
5752|Duddo Limestone|22893|6|Mentioned|p27 fig9|Miocene|Miocene|||||||
5752|Duddo Limestone|23179|6|Mentioned|Fig.2|Middle Miocene|Late Oligocene|Murray Supergroup||||||
5752|Duddo Limestone|23226|6|Mentioned|p889|||Of Murray Group.||||||
5752|Duddo Limestone|23417|6|Mentioned|p6|||||||||
5752|Duddo Limestone|23884|5|Briefly described|p155 Fig. 13.2|Early Miocene|Early Miocene|Geological Province: Murray Basin. Of the Murray Group.||||||
5752|Duddo Limestone|23909|6|Mentioned|p298|||||||||
5752|Duddo Limestone|24551|5|Briefly described|p322 Fig. 10.29, 520, p731 Table 17.1|||Of the Murray Group.  Geological Province: Murray Basin.  Max thickness: 130m.||||||
5752|Duddo Limestone|29591|6|Mentioned|Table 20|||||||||
5752|Duddo Limestone|29898|6|Mentioned|p216|||||||||
5752|Duddo Limestone|30581|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
5752|Duddo Limestone|30754|6|Mentioned|p13|||Used in deeper parts of basin where Morgan & Mannum indistinguishable||||||
5752|Duddo Limestone|30934|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene & Miocene||||||
5752|Duddo Limestone|31625|6|Mentioned|Fig. 5.2|||Miocene||||||
5752|Duddo Limestone|31745|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene - Miocene||||||
5752|Duddo Limestone|31746|3|Fully described|p195|||||||||
5752|Duddo Limestone|34360|6|Mentioned|p11|||||||||
5752|Duddo Limestone|34813|6|Mentioned|p62|||||||||
5752|Duddo Limestone|35285|5|Briefly described|p413|||||||||
5752|Duddo Limestone|37809|6|Mentioned|p7|||||||||
5752|Duddo Limestone|37873|6|Mentioned|p1|||||||||
5752|Duddo Limestone|39329|6|Mentioned|Fig.1|||||||||
5752|Duddo Limestone|39929|6|Mentioned|Fig.3|||||||||
5752|Duddo Limestone|40820|6|Mentioned|Fig.4|||||||||
5752|Duddo Limestone|41511|6|Mentioned|p20|||||||||
5752|Duddo Limestone|41537|6|Mentioned|Fig.2|||||||||
5752|Duddo Limestone|41868|5|Briefly described|p551|||||||||
5752|Duddo Limestone|42125|6|Mentioned|p136|||||||||
5752|Duddo Limestone|42134|6|Mentioned|Fig.3 P335|||||||||
5752|Duddo Limestone|42137|6|Mentioned|p369|||||||||
5752|Duddo Limestone|42827|3|Fully described|p269|||Of the Murray Group.||||||29-JUL-08
5752|Duddo Limestone|42881|4|Described|Fig.3, P84|||||||||
5752|Duddo Limestone|42966|2|Defined|Table 23, p139|Middle Miocene|Late Oligocene|Of the Murray Group.||||||29-JUL-08
5752|Duddo Limestone|43655|5|Briefly described|p40-846|||||||||
5752|Duddo Limestone|43791|6|Mentioned|p372, Fig1|||||||||
5752|Duddo Limestone|43804|6|Mentioned|Fig.2,p49|||||||||
5752|Duddo Limestone|44191|5|Briefly described|Map Legend|Middle Miocene|Late Oligocene|||||||
5752|Duddo Limestone|46909|6|Mentioned|Fig.2|||||||||
5752|Duddo Limestone|49038|5|Briefly described|p26|||||||||
5752|Duddo Limestone|49040|6|Mentioned|p11|||||||||
5752|Duddo Limestone|50154|2|Defined|p129, p135-136|Early Miocene|Late Oligocene|Of the Murray Group. Max. thickness: 127m. Lies conformably over and interfingers with Ettrick Marl. Disconformably overlain by Parilla Sand or Bookpurnong beds. Nonconformably overlies the Glenelg River Metamorphic Complex in parts.||||||15-SEP-04
5752|Duddo Limestone|50155|5|Briefly described|Map Legend|Miocene|Oligocene|Calcarenite, bryozoal limestone||||||
5752|Duddo Limestone|50156|5|Briefly described|Map Legend|Miocene|Oligocene|Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||
5752|Duddo Limestone|50157|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Overlies Ettrick Marl and Dergholm Granite. Overlain by Parilla Sand and Whalers Bluff Formation. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||25-JUN-04
5752|Duddo Limestone|50158|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||
5752|Duddo Limestone|50159|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||
5752|Duddo Limestone|50160|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Overlain by Lowan Sand. Overlies Glenelg River Metamorphic Complex and Hypatia Formation. Marine deposit of bryozoal limestone and calcarenite||||||25-JUN-04
5752|Duddo Limestone|50161|5|Briefly described|Map Legend|Miocene|Oligocene|Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous. Of the Murray Group.||||||26-AUG-04
5752|Duddo Limestone|50162|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||22-JUN-04
5752|Duddo Limestone|50163|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Overlies Ferres Creek Tonalite, Glenelg River Metamorphic Complex, Dergholm Granite and Nangeela Formation. Overlain by Shepparton Formation, Parilla and Lowan Sands. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||25-JUN-04
5752|Duddo Limestone|50164|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||24-JUN-04
5752|Duddo Limestone|60421|5|Briefly described|p409, 413 Fig. 3, 414 Fig. 4|Middle Miocene|Late Oligocene|Underlies: Dorodong Sands. Overlies: Bacchus Marsh Formation.||||||
5752|Duddo Limestone|61314|5|Briefly described|p129|Miocene|Miocene|Of the Murray Group. Geological Province: western part of Murray Basin.||||||
5752|Duddo Limestone|63460|5|Briefly described|p838, p839 Fig. 2b|Middle Miocene|Late Oligocene|Of Lawrence and Abele (1976).Max.thickness:130m. Suggested here that this Victoria nomenclature be replaced by the South Australia mappable units of Mannum, Finniss, Glensforlan, Bryant Creek and Pata Fm, as they are recognisable in subsurface Victoria.  ||||||
5752|Duddo Limestone|64237|5|Briefly described|p17, p18, p19|Early Miocene|Early Miocene|Of Lawrence (1966). Retained as formal unit through the Lawrence (1975) and Lawrence and Abele(1988) name revisions where it overlay Netherby Marl. Appears to have been excluded from the Murray Supergp...........................reinstated in SA Murray Gp||||||15-JUL-08
5752|Duddo Limestone|65552|6|Mentioned|p5 Fig. 3|Miocene|Oligocene|Of Murray Group (western Murray Basin).||||||
5752|Duddo Limestone|66002|5|Briefly described|p10 Tb.7|Paleogene|Paleogene|Of Murray Group. Defined by Lawrence 1966.||||||
5752|Duddo Limestone|66286|5|Briefly described|pp178-179, pp188-189.|Miocene|Oligocene|Contains a variety of goethite-replaced marine fossils including bryozoans, echinoids and foraminifera. 1 - 2 m thick. Open marine shelf or shallow marine deposit.||Unit in Murray Group.|||Limestones of skeletal debris admixed with varying proportions of quartz sand, micrite, and calcareous clay. Well-indurated, fossiliferous, dusky-brown to yellow goethite-rich laminated duricrust with c.10% pisoliths and ooliths.|
5752|Duddo Limestone|66287|6|Mentioned|p30 Fig. 8, p31|Middle Miocene|Middle Miocene|Victorian equivalent of the Murray Group Limestones of South Australia.||||Underlies Bookpurnong Beds.||20-APR-12
5752|Duddo Limestone|67179|6|Mentioned|p579|||||||||
5752|Duddo Limestone|68116|5|Briefly described|Appendix, Maps 29, 38.|Langhian|Chattian||||||Calcarenite, bryozoal limestone.|
5752|Duddo Limestone|68189|6|Mentioned|p29|||||Of the Murray Group.||||
5752|Duddo Limestone|70961|14|Not recorded|p136|||Geological section.||||||
5752|Duddo Limestone|71593|4|Described|p52, p54|Miocene|Oligocene|Murray Basin.||Murray Group||Interfingered with the Ettrick Formation and the Winnambool Formation. Unconformably overlain by the Loxton Sand and Bookpurnong Formation. |Pale bioclastic limestone.|
5752|Duddo Limestone|72445|5|Briefly described|App.6 p2 Fig.1; App.7 p7 Fig.4.|Middle Miocene|Late Oligocene|Of Lawrence and Abele (1976). See also Duddo Limestone Member, App.7 p7 text.||Murray Group||Unconformably overlies Renmark Group and is laterally equivalent with Winnambool Formation.|Includes marl and marly limestone.|
5752|Duddo Limestone|73118|6|Mentioned|p17, 21, 24, 34|||Drill core summary logs.||||Overlies Ettrick Formation. Is overlain by Loxton-Parilla Sands, and Shepparton Formation.||
5752|Duddo Limestone|73496|6|Mentioned|Map legend|Miocene|Oligocene|||||||
30285|Duggan Creek Granite|60503|4|Described|p184, p40 Tb. 2|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Grey rock comprising equigranular, medium-grained feldspar and quartz with small flakes of biotite. Age is inferred. Intrudes Marengo Granodiorite. ||||||
30285|Duggan Creek Granite|60504|5|Briefly described|Map Legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Biotite granite: A-type; grey, equigranular.||||||
30285|Duggan Creek Granite|60505|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Biotite granite: A-type; grey, equigranular.||||||
30285|Duggan Creek Granite|60506|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Biotite granite: A-type; grey, equigranular.||||||
30285|Duggan Creek Granite|60507|5|Briefly described|Map Legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Biotite granite: A-type; grey, equigranular.||||||
30285|Duggan Creek Granite|60508|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Biotite granite: A-type; nonmagnetic (0-5 nT); high K, low total count Th, U||||||
30285|Duggan Creek Granite|68116|5|Briefly described|Appendix, Map 27.|Triassic|Triassic||||||Biotite granite: grey, equigranular.|
39631|Dukes Basalt|24087|6|Mentioned|p336 Fig. 8||| Geological Province: Lachlan Fold Belt.||||||
39631|Dukes Basalt|62749|5|Briefly described|p722 Fig. 1b|||Informal name. Forms the Dukes Nose structure within the Magdala Basalt. Composed of 2 sub-lithologies: massive basalt, and pillow basalt.||||||
37359|Duluth Gabbro|24037|6|Mentioned|p428|||||||||
37359|Duluth Gabbro|64647|6|Mentioned|p41|||Reference zircons.||||||
28518|Dundas Surface|38982|6|Mentioned|p68|||||||||
28518|Dundas Surface|39967|4|Described|p19|||||||||
28518|Dundas Surface|61183|5|Briefly described|p20, p67|Tertiary|Tertiary|Widespread deep weathering profile comprising a major regolith unit across the map area of the Grampians Group - with well-developed ferricrete duricrust. This unit characterises the Dundas Tableland. Thickness: may exceed 50m. See also p122.||||||
28518|Dundas Surface|61207|5|Briefly described|p280 Fig. 2|Late Pliocene|Late Pliocene|Geological Province: onshore Otway Basin.||||||
28518|Dundas Surface|66012|5|Briefly described|p18|Pleistocene|Pliocene|Ferricrete and magnetic pisolitic ironstone developed on Miocene sand dunes prior to Newer Volcanic Group basalt flows.||||||
21708|Dundonnell Granite|23309|6|Mentioned|p430, App1|||G303 I-Type.||||||
74890|Dungeon Gully Sandstone Member|64010|5|Briefly described|p258 Fig.1. |Tournaisian|Tournaisian|||Of the Snowy Plains Formation.||||
74890|Dungeon Gully Sandstone Member|64536|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation (Mansfield Group). Sandstone, minor conglomerate: sandstone is red, quartz-lithic+quartzarenite, med. To thick bedded, through x-bedded, occasional v. thick conglomerate towards base; forms bold outcrops+strike ridges. Fluvial.||||||07-FEB-11
74890|Dungeon Gully Sandstone Member|64537|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation (Mansfield Group). Sandstone, minor conglomerate: sandstone is red, quartz-lithic+quartzarenite, med. To thick bedded, through x-bedded, occasional v. thick conglomerate towards base; forms bold outcrops+strike ridges. Fluvial.||||||07-FEB-11
74890|Dungeon Gully Sandstone Member|64538|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation (Mansfield Group). Sandstone, minor conglomerate: sandstone is red, quartz-lithic+quartzarenite, med. To thick bedded, through x-bedded, occasional v. thick conglomerate towards base; forms bold outcrops+strike ridges. Fluvial.||||||07-FEB-11
74890|Dungeon Gully Sandstone Member|64606|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation. Sandstone, minor conglomerate: alluvial deposits. Blue-black to green-yellow in RGB. Nonmagnetic.||||||
74890|Dungeon Gully Sandstone Member|64616|3|Fully described|p138, p190, p300|Early Carboniferous|Early Carboniferous|Basal new member of Snowy Plains Formation. Conformable over Mount Kent Conglomerate, unconformable on Delatite Group. Conformably overlain by Ashwin Siltstone Member. ~400m thick. Red sandstone, quartz-lithic and quartzarenite, medium- to thick-bedded; minor conglomerate. Geophysical characteristics given.||||||
33134|Dunmore Leucotonalite|23309|5|Briefly described| p335|||G416 S-Type||||||
33134|Dunmore Leucotonalite|23319|4|Described|p408 Fig. 1,  p414-415|Ordovician|Cambrian|Dominated by coarse pale green plagioclase laths and quartz, with minor interstitial microcline; rare biotite. Hosts numerous metasedimentary enclaves and muscovite-rich selvages. Enveloped by migmatitic rocks.||||||07-FEB-07
33134|Dunmore Leucotonalite|23991|5|Briefly described|p196|||||||||
33134|Dunmore Leucotonalite|24551|5|Briefly described|p77|||Of the Glenelg River Complex||||||
33134|Dunmore Leucotonalite|50154|2|Defined|p36, p95, p247 App.5|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex. Intruded by Marn Mering Granodiorite.||||||15-SEP-04
33134|Dunmore Leucotonalite|50155|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Muscovite leucotonalite; S-type||||||25-JUN-04
33134|Dunmore Leucotonalite|50156|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite tonalite.||||||20-AUG-04
33134|Dunmore Leucotonalite|50157|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite tonalite.||||||20-AUG-04
33134|Dunmore Leucotonalite|50158|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite tonalite.||||||20-AUG-04
33134|Dunmore Leucotonalite|50159|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite tonalite.||||||20-AUG-04
33134|Dunmore Leucotonalite|50160|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite tonalite.||||||20-AUG-04
33134|Dunmore Leucotonalite|50161|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite tonalite.||||||20-AUG-04
33134|Dunmore Leucotonalite|50162|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite tonalite.||||||20-AUG-04
33134|Dunmore Leucotonalite|50163|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite tonalite.||||||20-AUG-04
33134|Dunmore Leucotonalite|66002|6|Mentioned|p8 Tb.5|||G416. Defined by Kemp and Gray 1999.||||||
33134|Dunmore Leucotonalite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Muscovite tonalite: foliated, white to pale green, coarse grained, equigranular with rare biotite; pervasive schlieric foliation; abundant enclaves of gneiss and migmatite.|
21713|Dunneworthy Granodiorite|22756|5|Briefly described|P44|||||||||
21713|Dunneworthy Granodiorite|23309|6|Mentioned|p430 App1|||G383 I-Type.||||||
21713|Dunneworthy Granodiorite|43260|5|Briefly described|Map Legend||Early Devonian|Of the Mount Cole Suite. Biotite granodiorite: pale grey; medium grained; strongly kaolinised in places.||||||27-OCT-04
21713|Dunneworthy Granodiorite|44186|5|Briefly described|Map Legend||Early Devonian|G383 Unassigned.||||||
21713|Dunneworthy Granodiorite|60451|6|Mentioned|p153|||||||||
21713|Dunneworthy Granodiorite|66002|5|Briefly described|p7 Tb.5|||Of Mount Cole Suite. G383.  Defined by Cayley and McDonald 1995.||||||
21713|Dunneworthy Granodiorite|68116|5|Briefly described|Appendix, Map 31.|Early Devonian|Early Devonian||||||Biotite granodiorite: pale grey; medium grained; strongly kaolinised in places.|
78700|Duquesne Member|73386|6|Mentioned|p14|||||Bridgewater Formation||||
75538|Dwyer Granite|66002|5|Briefly described|p3, p8 Tb.5, p9|||In Victoria Valley Batholith area. G399. Name replaces Victoria Valley Granite. Name taken from Dwyer Creek which drains the southeastern side of the pluton||||||
75538|Dwyer Granite|68116|5|Briefly described|Appendix, Map 30.|Early Devonian|Early Devonian||||||Hornblende-biotite granite: reddish to pale pinkish grey; fine to medium-grained, generally porphyritic, commonly granophyric, miarolitic cavities, flow-folded rhyolitic dykes; oxidised.|
75538|Dwyer Granite|70877|6|Mentioned|p13|Early Devonian|Late Silurian|||||Intrudes the Grampians Group.||
75538|Dwyer Granite|70967|6|Mentioned|p11|||Mount Stavely Belt.||||Intrudes Grampians Group. Co-magmatic with Rocklands Volcanic Group.||
75538|Dwyer Granite|71593|4|Described|p148|Early Devonian|Early Devonian|Hosts Quartz-molybdenite-pyrite veinlets.|||||K-feldspar-sericite-chlorite-epidote altered granite.|
75538|Dwyer Granite|72445|5|Briefly described|p10.|Early Devonian|Late Silurian|||||Intrudes Grampians Group. Comagmatic with Rocklands Volcanic Group.||
34706|Dysentery Tonalite|22876|4|Described|p25|||||||||
34706|Dysentery Tonalite|23309|6|Mentioned|p430 App1|||G48 I-Type.||||||
34706|Dysentery Tonalite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|Of the Bete Bolong Suite. G48. I-type. Coarse grained, hornblende, biotite tonalite with abundant mafic inclusions.||||||
34706|Dysentery Tonalite|43315|5|Briefly described|Map Legend|Wenlock|Wenlock|G48. Of the Bete Bolong Suite.  I-type. Coarse grained, hornblende, biotite tonalite with abundant mafic inclusions.||||||03-MAY-05
34706|Dysentery Tonalite|60541|4|Described|p62, p14|Silurian|Silurian|Previously mapped as Orbost Granodiorite (Beams and Hough 1979). Eastern-most pluton of Bete Belong Suite. Green-grey, medium-grained and consists of large hornblende prisms up to 1.5cm long; interlocking plagioclase crystals ... . See also p17 Tb. 1, p93||||||20-JUN-05
34706|Dysentery Tonalite|68116|5|Briefly described|Appendix.|Devionian|Silurian||||||Hornblende-biotite tonalite: coarse-grained; abundant mafic inclusions; I-type.|
5892|Eagle Point Sand Member|24468|5|Briefly described|p405 Fig.2|Pleistocene|Pliocene|Geological Province: Gippsland Basin||||||
5892|Eagle Point Sand Member|24551|5|Briefly described|p327 Fig. 10.33|Pliocene|Pliocene|||||||
5892|Eagle Point Sand Member|35273|4|Described|p263|||||||||
5892|Eagle Point Sand Member|42827|6|Mentioned|p337|||see also Fig 8.21||||||
5892|Eagle Point Sand Member|61207|5|Briefly described|p280 Fig. 2|Quaternary|Quaternary|Geological Province: onshore Gippsland Basin.||||||12-JAN-06
5892|Eagle Point Sand Member|62899|5|Briefly described|p37 Fig. 2|||Of Haunted Hill Gravel. Geological province: Lakes Entrance Platform.||||||
5892|Eagle Point Sand Member|63739|5|Briefly described|p37 Fig. 2|||Of the Haunted Hill Gravel. Geological province: Gippsland Basin.||||||01-JUL-08
37551|Eagles Peak Basalt|23309|5|Briefly described|p32, p 28 Table 2.4|||Of Lickhole Volcanic Group||||||
37551|Eagles Peak Basalt|24551|5|Briefly described|p90|||Of the Lickhole Volcanic Group. Overlies Malcolm Creek Hyaloclastite||||||
37551|Eagles Peak Basalt|70601|4|Described|p43-45, p47-48|Drumian|Drumian|1.5 - 2 km thick. Age consistent with age of Dookie gabbro. Informal term to avoid confusion with "Seamount Basalt".|502 +/- 1 Ma.|Uppermost Lickhole Volcanics.||Conformably underlies Howqua Chert.|Tholeiitic pillow basalt, intruded by dolerite and gabbro; weakly deformed in prehnite-pumpellyite metamorphic facies.|
5900|East Kiewa Granodiorite|29711|6|Mentioned|Table 1|||||||||
5900|East Kiewa Granodiorite|39860|5|Briefly described|p15|||||||||
5900|East Kiewa Granodiorite|42089|6|Mentioned|p19|||||||||
5900|East Kiewa Granodiorite|42791|6|Mentioned|p209|||||||||
5900|East Kiewa Granodiorite|61160|3|Fully described|p70, p31 Tb. 5.2, p58-59 Fig. 6.8|Early Devonian|Early Devonian|Of Falls Creek Suite. Grey, biotite granodiorite to tonalite; even-grained, some porphyritic. Unconformably under Older Volcanic Gp. basalt at Basalt Hill. Intrudes Omeo Met. Complex migmatite and Cobungra Granite. Ages: 411 and 422Ma, and 410+16Ma. ||||||
5900|East Kiewa Granodiorite|61161|5|Briefly described|p153, p92, p91|Silurian|Silurian|Of Falls Creek Suite. On BOGONG. Age: K/Ar (biotite) 417+-9 Ma, Richards & Singleton (1981). GSV map code: G151.||||||
5900|East Kiewa Granodiorite|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Falls Creek Suite. Biotite granodiorite: grey; medium grained; equigranular; some muscovite-bearing phases; I-type intrusion. GSV map code: G151.||||||
5900|East Kiewa Granodiorite|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Falls Creek Suite. Biotite granodiorite: grey; medium grained; equigranular; some muscovite-bearing phases; I-type intrusion. GSV map code: G151.||||||
5900|East Kiewa Granodiorite|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Falls Creek Suite. Biotite granodiorite: grey; medium grained; equigranular; some muscovite-bearing phases; I-type intrusion. GSV map code: G151.||||||
5900|East Kiewa Granodiorite|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Falls Creek Suite. Biotite granodiorite: grey; medium grained; equigranular; some muscovite-bearing phases; I-type intrusion. GSV map code: G151.||||||07-FEB-11
5900|East Kiewa Granodiorite|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Falls Creek Suite. Biotite granodiorite: I-type; 413 +/- 15 Ma K/Ar biotite, 398 +/- 16 Ma K/Ar muscovite, 416 +/- 17 Ma Rb/Sr biotite; moderate to highly magnetic and non- to moderately magnetic subdivisions. GSV map code: G151.||||||
5900|East Kiewa Granodiorite|68116|5|Briefly described|Appendix, Map 27a.|Early Devonian|Early Devonian||||||Biotite granodiorite: grey, medium grained, equigranular; some muscovite-bearing phases; I-type.|
5924|Eastern View Formation|22756|6|Mentioned|P30|||||||||
5924|Eastern View Formation|22875|3|Fully described|p55|Early Eocene|Early Eocene|Of the Wangerrip Group.||||||30-JAN-07
5924|Eastern View Formation|22886|6|Mentioned|p17|||||||||
5924|Eastern View Formation|22944|5|Briefly described|Fig3|Eocene|Paleocene|||||||
5924|Eastern View Formation|23230|4|Described|Table4-1p40, 40-1, 43|Eocene|Late Cretaceous|Present in the Torquay Basin.||||||
5924|Eastern View Formation|23234|5|Briefly described|p88|||||||||
5924|Eastern View Formation|23240|5|Briefly described|p120-1|Eocene|Paleocene|||||||
5924|Eastern View Formation|23307|5|Briefly described|Map Legend|Paleocene|Paleocene|Of Wangerrip Group||||||
5924|Eastern View Formation|23322|5|Briefly described|957 Fig.2|Eocene|Paleocene|Of the Wangerrip Group.  Geological Province: Otway Basin.||||||07-SEP-09
5924|Eastern View Formation|23778|5|Briefly described|p660|||Replaced by Eastern View Group. Geological Province: Torquay Basin.||||||10-AUG-15
5924|Eastern View Formation|24038|5|Briefly described|p449|||||||||
5924|Eastern View Formation|24056|4|Described|p85|Late Cretaceous|Late Cretaceous|Geological Basin: Otway Basin.||||||
5924|Eastern View Formation|24105|5|Briefly described|p158|Eocene|Paleocene|||||||
5924|Eastern View Formation|24551|6|Mentioned|p295|||||||||
5924|Eastern View Formation|24562|5|Briefly described|p8 Fig. 2|Eocene|Paleocene|Of the Wangerrip Group.  Geological Province: Otway Basin.||||||
5924|Eastern View Formation|29355|6|Mentioned|p179|||||||||
5924|Eastern View Formation|30576|6|Mentioned|Table 2|||||||||
5924|Eastern View Formation|30905|6|Mentioned|Table 7.3|||||||||
5924|Eastern View Formation|30929|6|Mentioned|Map legend|Paleocene|Paleocene|||||||
5924|Eastern View Formation|31242|6|Mentioned|p12|||Refers hydrogeology||||||
5924|Eastern View Formation|31922|6|Mentioned|Fig.2|||||||||
5924|Eastern View Formation|34987|6|Mentioned|p170|||||||||
5924|Eastern View Formation|34991|6|Mentioned|p386|||||||||
5924|Eastern View Formation|35013|4|Described|p394|||||||||
5924|Eastern View Formation|35066|3|Fully described|p220|||||||||
5924|Eastern View Formation|35262|6|Mentioned|Fig.3|||||||||
5924|Eastern View Formation|35276|3|Fully described|p230|||||||||
5924|Eastern View Formation|35285|6|Mentioned|p415|||||||||
5924|Eastern View Formation|35290|4|Described|p26|||See also p25.||||||30-JAN-07
5924|Eastern View Formation|35712|6|Mentioned|Table 6|||||||||
5924|Eastern View Formation|36499|3|Fully described|p35|||See also Fig.9.||||||
5924|Eastern View Formation|37129|5|Briefly described|p359|||||||||
5924|Eastern View Formation|37385|6|Mentioned|p8|||||||||
5924|Eastern View Formation|39211|6|Mentioned|Fig.45|||||||||
5924|Eastern View Formation|41043|6|Mentioned|p96|||||||||
5924|Eastern View Formation|41185|6|Mentioned|Fig.4|||||||||
5924|Eastern View Formation|41642|4|Described|p243|||||||||
5924|Eastern View Formation|41704|6|Mentioned|Fig.3|||||||||
5924|Eastern View Formation|41868|5|Briefly described|p544|||||||||
5924|Eastern View Formation|42184|6|Mentioned|p350|||||||||
5924|Eastern View Formation|42318|5|Briefly described|p6|||||||||
5924|Eastern View Formation|42452|5|Briefly described|Map legend|late Eocene|Early Paleocene|||||||07-NOV-08
5924|Eastern View Formation|42453|3|Fully described|p11|late Eocene|Paleocene|Defined 1955 Raggatt and Crespin, as Eastern View Coal Measures. Informally subdivided here into lower, middle and upper parts.||||||09-FEB-15
5924|Eastern View Formation|42524|5|Briefly described|Fig.3 P27|||||||||
5924|Eastern View Formation|42555|5|Briefly described|Fig.2 P285|||||||||
5924|Eastern View Formation|42648|5|Briefly described|p45|||||||||
5924|Eastern View Formation|42827|3|Fully described|p294, p304|||||||||
5924|Eastern View Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
5924|Eastern View Formation|43171|6|Mentioned|5-8|||Of Wangerrip Group. Age: 55-75Ma||||||
5924|Eastern View Formation|43590|6|Mentioned|p15|||||||||
5924|Eastern View Formation|43660|6|Mentioned|Fig.6,p15|Eocene|Paleocene|||||||
5924|Eastern View Formation|43702|6|Mentioned|Fig.2,p398|Middle Eocene|Late Cretaceous|||||||
5924|Eastern View Formation|43733|6|Mentioned|Fig.2.11,p65||Eocene|||||||
5924|Eastern View Formation|43744|6|Mentioned|Fig.3,p3|||||||||
5924|Eastern View Formation|43937|5|Briefly described|Map Legend|Paleocene|Santonian|||||||
5924|Eastern View Formation|60421|5|Briefly described|p409, 411, 418 Fig. 5|Eocene|Paleocene|Of the Wangerrip Group.||||||07-NOV-08
5924|Eastern View Formation|60451|5|Briefly described|p95 Fig. 61|Eocene|Paleocene|Interfingers with Wangerrip and Nirranda Groups.||||||
5924|Eastern View Formation|60563|5|Briefly described|p47|||Coal bearing time equivalent of Wangerrip Group and Mepunga Formation.||||||
5924|Eastern View Formation|60599|5|Briefly described|p84|Late Cretaceous|Late Cretaceous|Of the Wangerrip Group. Geological Province:Otway  Basin.||||||
5924|Eastern View Formation|61181|6|Mentioned|p183|||Contains relatively pure sands for various forms of silica. Geological Province: Otway Basin. ||||||
5924|Eastern View Formation|61182|3|Fully described|p19, p23, p89|Late Eocene|Paleocene|Largely non-marine, graded laterally from the marine Wangerrip Group - included in the Wangerrip Group, although upper part is younger in deeper part of basin. Unconformable over Eumeralla Fm; overlain by Demons Bluff Fm. Max.thick: 360m. In Otway Basin.||||||07-NOV-08
5924|Eastern View Formation|61185|5|Briefly described|p57|Tertiary|Tertiary|Of the Wangerrip Group. Contain large river-rounded lithic cobbles. Age: ~65Ma. Geol. Prov: Otway Basin.||||||07-FEB-11
5924|Eastern View Formation|61628|5|Briefly described|p509 Fig. 3|Middle Eocene|Paleocene|Geological Province: Otway Basin.||||||07-APR-09
5924|Eastern View Formation|63124|5|Briefly described|p88|||An easterly condensed sandy sequence, equivalent to the Wangerrip and lower Nirranda Groups (of South Australia) has been named Eastern View Formation in Victoria.||||||
5924|Eastern View Formation|63269|5|Briefly described|p605|Eocene|Late Cretaceous|Otway Basin.||Wangerrip Group.||||
5924|Eastern View Formation|63445|5|Briefly described|Map legend.|Paleocene|Paleocene||||||Fluvial: gravel, sand, clay, brown coal.|
5924|Eastern View Formation|64314|5|Briefly described|p501, p502 Fig. 7|Eocene|Late Paleocene|Geological province: Otway Basin. Non-marine sediments - sands, silts, coals.||||||
5924|Eastern View Formation|65715|5|Briefly described|p13, p25 Fig.1a|Paleogene|Paleogene|Said to be unconformably overlain by Boonah Sandstone in Anglesea brown coal mine. Elevated to group status by Holdgate et al. (2001). Demoted to formation rank in this paper. Name derived from Eastern View Coal Measures. Combined with Boonah Sandstone in Fig.1a.||||||
5924|Eastern View Formation|66245|6|Mentioned|p6 Fig.5. |Priabonian|Maastrichtian|Shown in Fig.6 as a unit in both the Wangerrip and Nirranda Groups.||||||
5924|Eastern View Formation|68116|5|Briefly described|Appendix, Maps 49-50.|Eocene|Paleocene|Contains lignite lenses. Detrital sediments poorly consolidated to strongly cemented. Shown in combination with Boonah Formation.|||||Mudstone, sandstone, conglomerate, lignite: mudstone pale brown; sandstone fine-grained to granule size; consists of quartz, poorly to moderately sorted; conglomerate uncommon; lignite black to brownish black; commonly impure.|
5924|Eastern View Formation|69297|5|Briefly described|p97, p99-p102, p145|Lower Eocene|Santonian|Otway and Bass Basins. Deposited in a lower coastal plain, fluvial plain or deltaic environment. Hydrocarbon source rock in the Bass Basin.  ||||Unconformably overlain by the Demons Bluff Group. |Sandstones, siltstones and coals. |
5924|Eastern View Formation|69651|5|Briefly described|p10|Eocene|Late Cretaceous|Shown as a unit in two Groups.||Nirranda, Wangerrip Groups[?].||Unconformably overlies Timboon Sandstone and Dilwyn Formation. Is overlain by Demons Bluff Formation and (locally) Dilwyn Formation.||
5924|Eastern View Formation|70077|5|Briefly described|Regional: p5, p7-9|Eocene|Campanian|Hydrocarbon source in the Bass Basin but thermally immature in the Torquay Sub-basin. Fair to excellent reservoir properties with intraformational seals.||||Is overlain unconformably by Demons Bluff Group.|Lower coastal plain sandstones, siltstones and coals.|
5924|Eastern View Formation|70880|6|Mentioned|p77|Eocene|Maastrichtian|Otway Basin.||||||
5924|Eastern View Formation|71266|6|Mentioned|p614 Fig.3|Eocene|Late Cretaceous|Otway Basin.||||||
5924|Eastern View Formation|73217|5|Briefly described|p1008 Fig.1, 1009, 1022|||Eastern Otway Basin. Fluvial to coastal plain sediments deposited after Late Cretaceous basin extension.|65-55 Ma.|||Overlies Eumeralla Formation. Is overlain by Boonah Formation (Demons Bluff Group).|Fluvial sandstone.|
5924|Eastern View Formation|73357|5|Briefly described|p25-28, p44|Lutetian|Paleocene|Otway Basin. Lower contact not penetrated. Correlated with multiple biozones, including Alisocysta circumtabulata Dinocyst Zone in lower part, Proteacidites asperopolus Spore-Pollen Zone in upper part. Typically marginal marine depositional environments. Eastern View Formation or its equivalents are correlated with Lygistepollenites balmei Spore-Pollen Zone.||||Underlies Demons Bluff Formation.||
5924|Eastern View Formation|73486|6|Mentioned|p511 Fig.2|Priabonian|Lutetian|Otway Basin.||Nirranda Group||||
74887|Easts Lookout Siltstone|64535|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Siltstone - dark green-grey to occasionally black, thinly bedded, shaly; pale grey, thin to occasionally medium bedded sandstone, v. fine to med.-gr., well sorted, quartz-rich; minor black shale: Deep-marine hemipelagic deposits.||||||22-DEC-08
74887|Easts Lookout Siltstone|64536|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Siltstone - dark green-grey to occasionally black, thinly bedded, shaly; pale grey, thin to occasionally medium bedded sandstone, v. fine to med.-gr., well sorted, quartz-rich; minor black shale: Deep-marine hemipelagic deposits.||||||07-FEB-11
74887|Easts Lookout Siltstone|64537|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Siltstone - dark green-grey to occasionally black, thinly bedded, shaly; pale grey, thin to occasionally medium bedded sandstone, v. fine to med.-gr., well sorted, quartz-rich; minor black shale: Deep-marine hemipelagic deposits.||||||07-FEB-11
74887|Easts Lookout Siltstone|64538|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Siltstone - dark green-grey to occasionally black, thinly bedded, shaly; pale grey, thin to occasionally medium bedded sandstone, v. fine to med.-gr., well sorted, quartz-rich; minor black shale: Deep-marine hemipelagic deposits.||||||07-FEB-11
74887|Easts Lookout Siltstone|64539|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Siltstone - dark green-grey to occasionally black, thinly bedded, shaly; pale grey, thin to occasionally medium bedded sandstone, v. fine to med.-gr., well sorted, quartz-rich; minor black shale: Deep-marine hemipelagic deposits.||||||22-DEC-08
74887|Easts Lookout Siltstone|64540|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Siltstone - dark green-grey to occasionally black, thinly bedded, shaly; pale grey, thin to occasionally medium bedded sandstone, v. fine to med.-gr., well sorted, quartz-rich; minor black shale: Deep-marine hemipelagic deposits.||||||22-DEC-08
74887|Easts Lookout Siltstone|64605|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Siltstone, sandstone, minor shale; deep-marine deposits; Speckled pink-blue in RGB, yellow north and northwest of Eildon. Low to moderate magnetic response.||||||17-NOV-08
74887|Easts Lookout Siltstone|64606|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Siltstone, sandstone, minor shale: deep-marine deposits. Speckled pink-blue in RGB, yellow north and northwest of Eildon. Low to moderate magnetic response.||||||
74887|Easts Lookout Siltstone|64616|3|Fully described|p183 Fig.6.29, p197 Fig.6.34, p288, p290|||See also p303. Unit in Walhalla Group. See also Easts Lookout Formation (p106, p160 Fig.6.7, p162-163, p172, p179, p181-183, p282, p286) [which appears to be the authors' preferred name for this unit]. Type section described on p288. Dark green-grey to black, thinly bedded siltstone; pale grey, thinly bedded, very fine- to medium-grained quartz-rich sandstone; minor shale. Geophysical characteristics given.||||||
74887|Easts Lookout Siltstone|68116|5|Briefly described|Appendix, Maps 25, 33-34, 42-43.|Emsian|Pragian|Shown separately on the maps (code Dne) and locally in combination with Wilson Creek Shale (Dne-Sji).|||||Siltstone, sandstone, minor shale: siltstone dark green-grey to occasionally black; thinly bedded, shaley; minor black shale; sandstone pale grey; thin- to occasionally medium-bedded; very fine to medium-grained; well sorted; quartz-rich.|
74887|Easts Lookout Siltstone|70487|6|Mentioned|p9, p11 Fig.5|Emsian|Pragian|Welch et al. (2011) interpreted as immediately overlying Broadford Formation.||||Overlies Broadford Formation in Yea area. Shown as overlying Wilson Creek Shale (Earp 2015) and underlying Norton Gully Sandstone.|Siltstone.|
5940|Eccles basalt|34988|4|Described|p293|||||||||
5940|Eccles basalt|35722|6|Mentioned|p5|||Stratigraphy.||||||
5940|Eccles basalt|41848|5|Briefly described|p368|||||||||
5946|Eckersley Volcanics|32852|6|Mentioned|p10|||||||||
30952|Eight Mile Loop Rhyolite|23309|5|Briefly described|p123, 290.|||||||||
30952|Eight Mile Loop Rhyolite|24551|5|Briefly described|p151|||||||||
30952|Eight Mile Loop Rhyolite|60503|4|Described|p128, p42 Tb. 2|Early Devonian|Early Devonian|Scattered outcrops of rhyolite which are part of a small lava body; generally massive but shows flow-banding - very fine-grained matrix of plagioclase with some quartz. Overlies the Ludrik Munjie, Bingo Munjie and Post Office intrusions.  ||||||
30952|Eight Mile Loop Rhyolite|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Rhyolite lava: grey to light brown; flow banded||||||
30952|Eight Mile Loop Rhyolite|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Rhyolite lava: grey to light brown; flow banded||||||
30952|Eight Mile Loop Rhyolite|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Rhyolite lava: grey to light brown; flow banded||||||
30952|Eight Mile Loop Rhyolite|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Rhyolite lava: grey to light brown; flow banded||||||
30952|Eight Mile Loop Rhyolite|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Dartella Volcanic Group. Rhyolite: nonmagnetic response complicated by underlying granites; low total count, K, Th, U||||||
30952|Eight Mile Loop Rhyolite|68116|5|Briefly described|Appendix, Map 27.|Early Devonian|Early Devonian||||||Rhyolite: grey to light brown; sparse quartz and feldspar phenocrysts in very fine-grained matrix; flow banded.|
6016|Eildon Sandstone|22971|6|Mentioned|p 22|||Jordan River Group.||||||22-DEC-08
6016|Eildon Sandstone|23229|4|Described|Table3-3p27, 32|Pragian|Lochkovian|||||||
6016|Eildon Sandstone|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Jordan River Group.||||||27-OCT-08
6016|Eildon Sandstone|23309|4|Described|p144, 152-154  Table 2.53/2.54||Devonian|Age: Lochkovian||||||
6016|Eildon Sandstone|24177|5|Briefly described|p50 Fig.22|Early Devonian|Early Devonian|Geological Province: Mount Easton Province.||||||
6016|Eildon Sandstone|24551|5|Briefly described|p129, 614|||||||||
6016|Eildon Sandstone|24588|5|Briefly described|p20, p12 Fig.3, p22, p25-28|Lochkovian|Lochkovian|Geological Province: Mount Easton Province. Overlies Whitelaw Siltstone conformably. Overlain conformably by Wilson Creek Shale.||||||29-NOV-13
6016|Eildon Sandstone|32074|6|Mentioned|p179|||||||||
6016|Eildon Sandstone|33238|5|Briefly described|p642|||||||||
6016|Eildon Sandstone|33601|2|Defined|p11|Early Devonian|Early Devonian|||||||
6016|Eildon Sandstone|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
6016|Eildon Sandstone|35073|5|Briefly described|Table 1.|||||||||
6016|Eildon Sandstone|35283|4|Described|p54|||||||||
6016|Eildon Sandstone|36389|6|Mentioned|p41|||||||||
6016|Eildon Sandstone|38787|6|Mentioned|p125|||||||||
6016|Eildon Sandstone|41585|4|Described|p114|||||||||
6016|Eildon Sandstone|42827|4|Described|p114|||see also Table 4.1||||||
6016|Eildon Sandstone|42938|5|Briefly described|p576 Fig.3|||||||||
6016|Eildon Sandstone|44187|5|Briefly described|Map Legend||Early Devonian|||||||
6016|Eildon Sandstone|60599|5|Briefly described|p47 Fig. 19|Lochkovian|Lochkovian|Geological Province: Mount Easton Province, Melbourne Zone, Lachlan Fold Belt.||||||
6016|Eildon Sandstone|61185|5|Briefly described|p37, p21 Fig. 6|Lochkovian|Lochkovian|Of Jordan River Group (Thomas,1947). Overlies Whitelaw Siltstone; underlies Wilson Creek Shale. Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
6016|Eildon Sandstone|62099|5|Briefly described|p331|Early Devonian|Early Devonian|In eastern Melbourne Zone of the Lachlan Orogen. ||||||
6016|Eildon Sandstone|64536|5|Briefly described|Map legend|Early Devonian|Early Devonian|Pale grey sandstone, thick-thin bedded, med.-fine-gr.often poorly sorted; Tabc, Tbc and Tc turbidite beds (convolute lamination); grey siltstone, thin-thick bedded, banded-bioturbated; rare black shale . Deep-marine turbidite fan and hemipelagic deposits.||||||07-FEB-11
6016|Eildon Sandstone|64537|5|Briefly described|Map legend|Early Devonian|Early Devonian|Pale grey sandstone, thick-thin bedded, med.-fine-gr.often poorly sorted; Tabc, Tbc and Tc turbidite beds (convolute lamination); grey siltstone, thin-thick bedded, banded-bioturbated; rare black shale . Deep-marine turbidite fan and hemipelagic deposits.||||||07-FEB-11
6016|Eildon Sandstone|64538|5|Briefly described|Map legend|Early Devonian|Early Devonian|Pale grey sandstone, thick-thin bedded, med.-fine-gr.often poorly sorted; Tabc, Tbc and Tc turbidite beds (convolute lamination); grey siltstone, thin-thick bedded, banded-bioturbated; rare black shale . Deep-marine turbidite fan and hemipelagic deposits.||||||07-FEB-11
6016|Eildon Sandstone|64606|5|Briefly described|Map Legend|Early Devonian|Silurian|Of Jordan River Group. Sandstone, siltstone: deep-marine deposits. Blue-pink to yellow in RGB. Nonmagnetic.||||||
6016|Eildon Sandstone|64616|3|Fully described|p88, p159, p162-163 Fig.6.9, p166|Early Devonian|Early Devonian|See also p169 Fig.6.16, p183 Fig.6.29, p197 Fig.6.34, p201 Tb.7.1, p205, p285-288, p295, p304. Of Jordan River Group. Conformable between Whitelaw Siltstone below and Wilson Creek Shale above. 325-500m thick. Age inferred from relationships and correlation with Boola Formation. Interbedded sandstone and siltstone. Locally hornfelsed by Woods Point Dyke Swarm. Geophysical characteristics given.||||||
6016|Eildon Sandstone|66769|6|Mentioned|135, fig 13|Devonian||Older than Norton Gully Sandstone. North dipping and younging.||||||
6016|Eildon Sandstone|68116|5|Briefly described|Appendix, Maps 25, 33.|Pragian|Lochkovian||||||Sandstone, siltstone: sandstone mid- to pale grey; thick to thin-bedded; medium to fine-grained; poorly sorted; turbidite beds with convolute lamination; siltstone mid- to dark grey; thin to thick-bedded; banded to bioturbated; rare black shale.|
6016|Eildon Sandstone|70933|14|Not recorded|p93|||Section.||||||
37718|Eleven Bob Granodiorite|23309|6|Mentioned|p430, Appendix 1|||G55, I-Type. Supersedes Eleven Bob Granite.||||||
37718|Eleven Bob Granodiorite|44185|5|Briefly described|Map legend.|||I-type. Age uncertain: shown as SDg, ie Silurian-Devonian.||||||
37718|Eleven Bob Granodiorite|68116|5|Briefly described|Appendix.|Devonian|Silurian||||||Hornblende-biotite granodiorite: grey-green, medium-grained, extremely weathered where exposed; northern margin is altered; I-type.|
6071|Elizabeth Street Formation|29982|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
6095|Ellery Granite|23309|5|Briefly described|p313, 344, 345.||Early Devonian|Supersedes Ellery Adamellite.  G37.  Age: 386+/-3 Ma.||||||
6095|Ellery Granite|33602|6|Mentioned|p37|||||||||
6095|Ellery Granite|35112|6|Mentioned|p289|||||||||
6095|Ellery Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
6095|Ellery Granite|68116|5|Briefly described|Appendix, Map 36.|Early Devonian|Early Devonian||||||Biotite-amphibole granite: coarse to medium grained, porphyritic.|
6095|Ellery Granite|71206|6|Mentioned|p373, 377, 379, 384|||Lachlan Fold Belt. Contains both abundant brick-red K-feldspar and cream-white K-feldspar. Geochemistry graphs.||Ellery Suite.|||Unfractionated aluminous A-type granite.|
6097|Ellery Suite|22876|4|Described|p25|||||||||
6097|Ellery Suite|22877|5|Briefly described|map|Silurian|Silurian|||||||
6097|Ellery Suite|42627|5|Briefly described|Map legend|Wenlock|Wenlock|Used at 'Group' level in stratigraphic sense. NOT variation on Ellery Adamellite.||||||
6097|Ellery Suite|42726|5|Briefly described|map legend||Middle Devonian|||||||
6097|Ellery Suite|42827|6|Mentioned|p429|||||||||
6097|Ellery Suite|60541|6|Mentioned|p69|||Includes all A-types west of the Bega Batholith.||||||
6097|Ellery Suite|71206|6|Mentioned|p373, 377, 387|||Lachlan Fold Belt. Sr/Nd plot.|||Ellery Granite.||Aluminous A-type granite.|
21743|Elmhurst Granite|22756|5|Briefly described|P45|||||||||
21743|Elmhurst Granite|23309|6|Mentioned|p430 App1|||G373 I-Type.||||||
21743|Elmhurst Granite|43260|5|Briefly described|Map Legend||Early Devonian|of Mount Cole Suite. Biotite granite: pale grey; felsic; fine to medium grained.||||||27-OCT-04
21743|Elmhurst Granite|44186|5|Briefly described|Map Legend||Early Devonian|G373 I-type.||||||
21743|Elmhurst Granite|66002|5|Briefly described|p7 Tb.5|||Of Mount Cole Suite. G373.  Defined by Cayley and McDonald 1995.||||||
21743|Elmhurst Granite|68116|5|Briefly described|Appendix, Map 31.|Early Devonian|Early Devonian||||||Biotite granite: pale grey; felsic; fine to medium grained.|
32290|Emperor Subgroup|13323|4|Described|p394, p393 Fig. 2|Coniacian|Turonian|Of Latrobe Group. Comprises Admiral and Curlip Formations, Kipper Shale, and Kersop Arkose. Non-marine to paralic clastics. Overlies Strzelecki Group. Max. thickness: <1500m. Geol. Prov: Gippsland Basin.||||||
32290|Emperor Subgroup|13324|5|Briefly described|p94 Fig. 4, Fig.5, p98|Coniacian|Cenomanian|Gippsland Basin. Formerly included in Golden Beach Group of Lowry and Longley (1991). Includes coarse-grained alluvial fan and fluvial deposits and mud-dominated lacustrine deposits.||Of Latrobe Group|Includes Kipper Shale?|Overlain unconformably by Golden Beach Subgroup.||
32290|Emperor Subgroup|24090|5|Briefly described|p8 Fig.3|Late Cretaceous|Late Cretaceous|Of the Latrobe Group. See also page 17. Geological Province: Gippsland Basin.||||||06-APR-05
32290|Emperor Subgroup|24164|6|Mentioned|p11,18,20,24-25,32,37,39-41,44 and more|Albian||Horizon top of this unit was mapped from seismic data. Believe sediment was deposited in and around deep, narrow lakes (Bernecker et al. 2001). Misspelt once as Emporer Group (p25). Included in Figs.10,12,15,22,26, Tb.2.||Latrobe Group|||Sediments|
32290|Emperor Subgroup|24407|5|Briefly described|p13 Fig.2, p14|||Parent: Latrobe Group. Geological Province: Gippsland Basin||||||
32290|Emperor Subgroup|24495|6|Mentioned|p11, p12 Fig. 5|||Geological Province: Gippsland Basin.||||||
32290|Emperor Subgroup|24551|5|Briefly described|p267, 475|Turonain|Turonian|Of the Latrobe Group.  Underlies the Golden Beach Subgroup.||||||
32290|Emperor Subgroup|61212|5|Briefly described|p301 Fig. 2|Coniacian|Cenomanian|Geological Province: Gippsland Basin.||||||
32290|Emperor Subgroup|61469|6|Mentioned|p33|||Contains gas-producing sandstones. Geological Province: Gippsland Basin.||||||
32290|Emperor Subgroup|61552|5|Briefly described|p583. |Late Cretaceous|Late Cretaceous|Represents the initial rift phase of tectonic extension.||Unit in Latrobe Group.|Includes Admiral and Curlip Formations, Kersop Arkose and Kipper Shale.|||
32290|Emperor Subgroup|64876|5|Briefly described|p145 Fig.2|Turonian|Turonian|Gippsland Basin.||Latrobe Group.|Admiral, Curlip Formations; Kipper Shale, Kersop Arkose.|Overlies Korumburra Subgroup, Strzelecki Group (Otway Unconformity). Is overlain by Golden Beach Subgroup (Longtom Unconformity) .||
32290|Emperor Subgroup|65717|5|Briefly described|p9 Fig.2.2, p10, p12|Santonian|Cenomanian|Bernecker and Partridge (2001). Gippsland Basin. Comprises coarse grained alluvial fan/plain as well as lacustrine facies. Includes intraformational seals.||Latrobe Group|Curlip Formation, Admiral Formation, Kipper Shale, Kersop Arkose.|Unconformably overlain by Golden Beach Subgroup, Unconformably overlies Strzelecki Group||05-SEP-17
32290|Emperor Subgroup|65718|5|Briefly described|p11, pp40-43, p48|Late Cretaceous|Late Cretaceous|Bernecker and Partridge (2001). Oldest depositional unit of the Latrobe Group. Comprises coarse-grained alluvial fan/plain as well as lacustrine facies associations.||Of the Latrobe Group.|Includes the Kipper Shale and the Curlip Formation.|Unconformably underlain by the Strzelecki Group.|Includes coarse to layered sandstone with rip-up clasts.|
32290|Emperor Subgroup|65973|5|Briefly described|p14-15, p23, p27, p29, p32-34, |||Gippsland Basin. Hosts a subeconomic gas column which was intersected in Longtom/ST-1. Only intersected around the basin margins. Intersected in numerous drillholes including Leatherjacket-1, Judith-1, Hammerhead-1, Longtom/ST-1,  Longtom-1, Longtom-2/ST-1, Shark-1  and many more drillholes (see appendix). See also p57-58, p80, p82, p86, p93, p96-97, p100, p108-110, p123, p125, p128-130, p132-134, p139-140, p171, p180-182, p184.||Latrobe Group|Includes the Kersop Arkose, Admiral Formation, Kipper Shale, Curlip Formation.|Unconformably overlies the Strzelecki Group. Unconformably overlain by the Golden Beach Subgroup.||
32290|Emperor Subgroup|66181|5|Briefly described|p310 Fig.5|Campanian|Turonian|Unconformably underlies the Golden Beach Subgroup, in the Latrobe Group. Marine clastics.||||||
32290|Emperor Subgroup|69297|5|Briefly described|p400, p415, p431, p434|||Gippsland Basin.|||||Mudstone and marine shales. |
32290|Emperor Subgroup|69879|5|Briefly described|p417, p428|Turonian|Turonian|Gippsland Basin. Deposited during renewed continental rifting. Faulted and folded.||Latrobe Group|||Synrift deposits: arkose, fluvial sandstone and then lacustrine shale.|
32290|Emperor Subgroup|70028|5|Briefly described|p79-80, 82|Coniacian|Turonian|Gippsland Basin.||Latrobe Group.||Unconformably overlies Strzelecki Group. Is overlain unconformably by Latrobe Group.|Coarse-grained alluvial fan and lacustrine plain sediments.|
32290|Emperor Subgroup|70076|5|Briefly described|South-Eastern: Fig.2; p2-3|Coniacian|Turonian|See also Regional: Fig.3; p2, p7-8. Dominantly freshwater lacustrine sediments. Hosts the Longtom gas discovery.||Latrobe Group.|Kipper Shale, Kersop Arkose, Admiral Formation and Wombat Volcanics.|Overlies Korumburra Subgroup (Strzelecki Group). Is overlain by Golden Beach Subgroup.||
32290|Emperor Subgroup|70331|5|Briefly described|p69|Late Cretaceous|Late Cretaceous|Gippsland Basin (western).||Latrobe Group.||Unconformably overlies Strzelecki Group. Is overlain unconformably by Golden Beach Subgroup.|Fluvial sandstone (onshore); lacustrine shale (offshore).|
32290|Emperor Subgroup|73471|5|Briefly described|p85-88, p89-91, p102, p104, p108|Turonian|Cenomanian|Gippsland Basin. Incorporated into the post-rift mega-sequence. Overlies Otway Unconformity, underlies Longtom Unconformity. Intruded by igneous sills, dykes and funnels. Contains hydrocarbon source rocks.|95-90 Ma|Latrobe Group|Curlip Formation, Kipper Shale|Unconformably overlies Strzelecki Group, Upper Strzelecki Subgroup, unconformably underlies Golden Beach Subgroup|Includes lacustrine shales.|
32290|Emperor Subgroup|75065|5|Briefly described|p149, 151, 154-155, 160, 162, 172|Santonian|Cenomanian|Gippsland Basin; offshore. Pervasive lakes and shallow inland seas. Contains reservoirs and potential petroleum source rocks.||Latrobe Group.|Kersop Arkose, Kipper Shale, Curlip Formation, Admiral Formation.|Unconformably overlies Strzelecki Group. Is overlain unconformably by Golden Beach Subgroup.|Coarse siliciclastics (from the W), volcaniclastics (from the E), organic-rich black mudstones and sapropelic coals.|
34857|Emu Vale Tonalite|22968|5|Briefly described|P79, P204|Early Devonian|Late Silurian|New name, parent is Ensay Suite||||||
34857|Emu Vale Tonalite|23028|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Ensay Suite||||||
34857|Emu Vale Tonalite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Ensay Suite||||||
34857|Emu Vale Tonalite|23309|5|Briefly described|p296|||G124 I-Type||||||
34857|Emu Vale Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Hornblende-biotite tonalite: grey, altered to pink or green; medium-grained; porphyritic in wafer-thin hornblende which defines weak magmatic foliation.|
24268|Enano Group|22628|6|Mentioned|p115,p118||Silurian|||||||
24268|Enano Group|22968|5|Briefly described|p12, p111||Late Silurian|Unconformably overlies the Towanga Sandstone.||||||16-AUG-18
24268|Enano Group|23020|5|Briefly described|Map legend|Pridoli|Ludlow|||||||
24268|Enano Group|23021|5|Briefly described|Map legend|Pridoli|Ludlow|Nonconformably and angular unconformably overlies the Bullenbalong Suite.||||||25-SEP-08
24268|Enano Group|23028|5|Briefly described|Map legend|Pridoli|Ludlow|||||||
24268|Enano Group|23029|5|Briefly described|Map legend|Pridoli|Ludlow|||||||
24268|Enano Group|23030|5|Briefly described|Map legend|Late Silurian|Late Silurian|||||||
24268|Enano Group|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
24268|Enano Group|23309|4|Described|p89-100, 304.  Table 2.31|Late Silurian|Late Silurian|||||||
24268|Enano Group|23522|5|Briefly described|p247 Fig 3|Silurian|Silurian|||||||
24268|Enano Group|23615|3|Fully described|p78, p21|Ludlow|Wenlock|Replaced Cowombat Group of Talent (1965).  Defined by VandenBerg (1981,1984) to include Towanga Sandstone, Cowombat Siltstone, and Gibsons Folly F; redefined (Allen 1987,1988) to exclude Towanga Sandstone and include Thorkidaan Volcanics. Age: ~425-410Ma.||||||16-AUG-18
24268|Enano Group|23938|5|Briefly described|p14 Tb. 1|Late Silurian|Middle Silurian|Includes Gibsons Folly Formation, Cowombat Siltstone and Thorkidaan Volcanics. ||||||
24268|Enano Group|24002|5|Briefly described|p228 Fig.2|Silurian|Silurian|||||||
24268|Enano Group|24004|5|Briefly described|p275 Fig.2|Silurian|Silurian|||||||
24268|Enano Group|24098|5|Briefly described|p27 Fig. 2|Pridolian|Ludlovian|Geological Province: Lachlan Fold Belt.||||||
24268|Enano Group|24266|6|Mentioned|p1482|||Geological Province: Lachlan Fold Belt.||||||
24268|Enano Group|24275|4|Described|p1695|Late Silurian|Silurian|Trends form abundant silicic volcanics to subordinate subaqueous mafic to intermediate volcanics, to shallow and deep marine sediments. Thickness: 1200m.  Formed in Cowombat Rift.  Overlies Towanga Sandstone basement.  Geol. Province: Lachlan Fold Belt.||||||
24268|Enano Group|37501|6|Mentioned|p413|||||||||
24268|Enano Group|38145|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
24268|Enano Group|38151|6|Mentioned|Table 1|||||||||
24268|Enano Group|38367|6|Mentioned|Fig.9.|||||||||
24268|Enano Group|39447|2|Defined|p6|Late Silurian|Late Silurian|||||||
24268|Enano Group|39860|4|Described|p9|||||||||
24268|Enano Group|40761|6|Mentioned|p227|||||||||
24268|Enano Group|41572|6|Mentioned|p19|||||||||
24268|Enano Group|41585|4|Described|p127|||||||||
24268|Enano Group|41868|5|Briefly described|p572|||||||||
24268|Enano Group|42089|5|Briefly described|p18|||See also Fig.62||||||
24268|Enano Group|42791|5|Briefly described|p216|||||||||
24268|Enano Group|42827|4|Described|p127|||||||||
24268|Enano Group|43128|5|Briefly described|p473|||||||||
24268|Enano Group|43206|5|Briefly described|map legend||Wenlock|||||||
24268|Enano Group|43220|5|Briefly described|p9||Silurian|||||||
24268|Enano Group|43766|6|Mentioned|p921|Late Silurian|Early Silurian|(M.Sil.-L.Sil.)||||||
24268|Enano Group|44184|5|Briefly described|Map Legend||Late Silurian|||||||
24268|Enano Group|44185|5|Briefly described|Map legend.|Late Silurian|Late Silurian||||Includes Gibsons Folly Formation and Cowombat Siltstone.|||
24268|Enano Group|60503|4|Described|p108, p15, p28 Fig. 9|Late Silurian|Late Silurian|Includes Thorkidaan Volcanics, Cowombat Siltstone and Gibsons Folly Formation. Submarine volcanics and clastics deposited as turbidites and mass flows. Overlies the Thorkidaan Volcanics. Max. thickness: ?3km.Geological Province: Limestone Creek Graben. ||||||
24268|Enano Group|60504|5|Briefly described|Map Legend|Pridoli|Ludlow|Includes: Thorkidaan Volcanics, Cowombat Siltstone, Gibsons Folly Formation.||||||25-SEP-08
24268|Enano Group|60505|5|Briefly described|Map legend|Pridoli|Ludlow|Includes: Thorkidaan Volcanics, Cowombat Siltstone, Gibsons Folly Formation.||||||25-SEP-08
24268|Enano Group|60506|5|Briefly described|Map legend|Pridoli|Ludlow|Includes: Thorkidaan Volcanics, Cowombat Siltstone, Gibsons Folly Formation.||||||25-SEP-08
24268|Enano Group|60507|5|Briefly described|Map Legend|Pridoli|Ludlow|Includes: Thorkidaan Volcanics, Cowombat Siltstone, Gibsons Folly Formation.||||||
24268|Enano Group|60508|5|Briefly described|Map legend|Late Silurian|Late Silurian|Includes Gibsons Folly Formation and Cowombat Siltstone.||||||25-SEP-08
24268|Enano Group|60541|5|Briefly described|p11 Fig. 2|Late Silurian|Late Silurian|||||||
24268|Enano Group|60542|5|Briefly described|p11 Fig. 2|Late Silurian|Late Silurian|||||||
24268|Enano Group|61181|5|Briefly described|p122, p172|Late Silurian|Middle Silurian|Incl:Thorkidaan Volcs, Cowombat Siltst and Gibsons Folly Fm. Ranges thro' rhyolite-dacite-andesite-basalt; rhyolite dominant in Thorkidaan Volcs. As lenses interbedded with siltst. and sst (Cowombat Siltst),strongly crystallised; platy cleavage in places.||||||20-DEC-07
24268|Enano Group|61187|5|Briefly described|p5, pp23-24, p26 Fig.2, p29 Fig.4.|Late Silurian|Middle Silurian|Buchan and Mallacoota Zones, Benambra Terrane. Correlative of Humevale, McIvor and Mount Ida Formations, Melbourne Zone, Melbourne Terrane. Dominantly volcanics. Hosts the Wilga and Currawong VHMS Zn-Cu deposits.|||Includes Thorkidaan Volcanics, Cowombat Siltstone and Gibsons Folly Formation.||Interbedded sediments and dacitic-andesitic volcanics.|
24268|Enano Group|66197|5|Briefly described|p634|Late Silurian|Late Silurian|Limestone Creek Graben. Thick lower unit of silicic volcanics, followed by deep marine sedimentary and volcanic rocks.||||||14-MAR-12
24268|Enano Group|71040|5|Briefly described|p8|Late Silurian|Late Silurian|Limestone Creek Graben, NE Victoria. Affected by the Bindian (=Bowning) Orogeny; has undergone intense shortening.||||Is overlain unconformably by Snowy River Volcanics.|Strongly folded and foliated metavolcanic and metasedimentary rocks.|
6183|Enfield Granite|23309|6|Mentioned|p430 App 1|||(G40) I-Type.||||||
6183|Enfield Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
6183|Enfield Granite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|I-type. Medium grained hornblende, biotite granite.||||||22-OCT-04
6183|Enfield Granite|43315|5|Briefly described|Map Legend||Wenlock|I-type granite. medium-grained hornblende, biotite granite.||||||03-MAY-05
6183|Enfield Granite|60541|4|Described|p18 Tb. 1, p48|Silurian|Silurian|I-type granite. Intrudes Kuark Metamorphic Complex. Grey rock when fresh but easily weathers to orange-red with abundant mica flakes; coarse-grained and foliated with abundant large K-feldspars in a matrix of medium-grained quartz, K-feldspar and biotite.||||||
6183|Enfield Granite|68116|5|Briefly described|Appendix, Map 45.|Wenlock|Wenlock||||||Hornblende-biotite granite: medium-grained; I-type.|
31575|Enfield Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31575|Enfield Suite|44093|5|Briefly described|p188 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
34902|Ensay Suite|22968|5|Briefly described|Fig89 P164, P199|Devonian|Silurian|Strongly magnetic plutons||||||
34902|Ensay Suite|23020|5|Briefly described|Map legend|Lochkovian|Pridoli|||||||
34902|Ensay Suite|23021|5|Briefly described|Map legend|Lochkovian|Pridoli|||||||
34902|Ensay Suite|23028|5|Briefly described|Map legend|Lochkovian|Pridoli|||||||
34902|Ensay Suite|23029|5|Briefly described|Map legend|Lochkovian|Pridoli|||||||
34902|Ensay Suite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
34902|Ensay Suite|23309|5|Briefly described|p344|||||||||
34902|Ensay Suite|24551|6|Mentioned|p230|||||||||
34902|Ensay Suite|61160|6|Mentioned|p70|||Formerly a part of Fagan's (1979) Falls Creek Series. Now probably an obsolete name? Restricted to 4 plutons in the Ensay Shear Zone. ||||||
34902|Ensay Suite|61161|5|Briefly described|p91|||I-type. See also Ensay suite.||||||
6218|Epacris Hills Granite|23309|6|Mentioned|p430 App 1|||G397 I-Type. Supersedes Stony Creek Granite.||||||
6218|Epacris Hills Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
6218|Epacris Hills Granite|44186|5|Briefly described|Map Legend||Early Devonian|G397 I-type. Shown as Epacris Hills.||||||
6218|Epacris Hills Granite|60451|4|Described|p87, 220|Early Devonian|Early Devonian|Of the Mafeking Suite. Previously known as Stony Creek granite (Spencer-Jones, 1965). Previously considered part of Mackenzie River Granite (Cayley & Taylor, 1997).||||||
6218|Epacris Hills Granite|60456|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Mafeking Suite. Unit does not appear on this map.||||||
6218|Epacris Hills Granite|60458|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Mafeking Suite. Hornblende-biotite granite; felsic, oxidised, I-Type.||||||
6218|Epacris Hills Granite|60459|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Mafeking Suite. Hornblende-biotite granodiorite, oxidised, I-Type.||||||29-SEP-04
6218|Epacris Hills Granite|63446|5|Briefly described|Map legend|Early Devonian|Early Devonian|No lithology given: is listed as Epacris Hills. G397.|||||I-type granite.|12-JUN-15
6218|Epacris Hills Granite|63599|6|Mentioned|p976 Fig. 1|||Geological Province: Grampians-Stavely Zone.||||||10-DEC-07
6218|Epacris Hills Granite|66002|5|Briefly described|p8 Tb.5|||Of Mafeking Suite. G397. Replaces Stony Creek Granodiorite of Spencer-Jones (1965)||||||
6218|Epacris Hills Granite|68116|5|Briefly described|Appendix, Map 30.|Early Devonian|Early Devonian||||||Hornblende-biotite granite: pale pinkish grey; medium to coarse-grained; equigranular to porphyritic.|
6227|Ercildoun Granite|23300|5|Briefly described|Map Legend|Devonian|Devonian|Of Beckworth Suite||||||
6227|Ercildoun Granite|23301|5|Briefly described|Map Legend|Devonian|Devonian|Of Beckworth Suite. Age: 360 +/- 4 Ma (K-Ar), 364 +/- 10 Ma (Rb-Sr).||||||13-SEP-04
6227|Ercildoun Granite|23302|5|Briefly described|Map Legend|Devonian|Devonian|Of Beckworth Suite||||||
6227|Ercildoun Granite|23303|5|Briefly described|Map Legend|Devonian|Devonian|Of Beckworth Suite||||||
6227|Ercildoun Granite|23304|5|Briefly described|Map Legend|Devonian|Devonian|Of Beckworth Suite||||||
6227|Ercildoun Granite|23305|4|Described|p45. Table 6, 7||Late Devonian|Now defined after White and Chappell (1988) and extended to include Bolton and Beckworth granites of White and Chappell and Misery Granite of Egan (1981). Age: 359+/-4 to 364+/-40 Ma K-Ar. Of Beckworth Suite. Central Victorian Magmatic Province.||||||
6227|Ercildoun Granite|23309|5|Briefly described|p430 App 1|Late Devonian|Late Devonian|G312 I-Type. Age: 360 +/- 4Ma, 363 +/- 4Ma, and 359 +/- 4 Ma, 364 +/- 10Ma.||||||
6227|Ercildoun Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
6227|Ercildoun Granite|44186|5|Briefly described|Map Legend||Early Devonian|G312 I-type.||||||
6227|Ercildoun Granite|65715|5|Briefly described|p8 Tb.4|||G312. Includes Bolton and Beckworth granites of White and Chappell (1988).||||||
6227|Ercildoun Granite|65974|6|Mentioned|p28|||Modelled with a larger lateral extent than mapped at the surface, indicating granite at shallow depths proximal to the known contact.||||||
6227|Ercildoun Granite|66002|5|Briefly described|p6 Tb.5|||Of Beckworth Suite. G312. Defined in Taylor et al. 2000. Includes the Bolton and Beckworth Granites of White and Chappell (1988)||||||16-MAY-13
6227|Ercildoun Granite|68116|5|Briefly described|Appendix, Map 31.|Late Devonian|Late Devonian||||||Biotite granite: medium grained; commonly porphyritic in quartz, plagioclase and K-feldspar; leucocratic; nonmagnetic reduced.|
6227|Ercildoun Granite|75061|5|Briefly described|p60-61, 63-64, 70|Late Devonian|Late Devonian|Bendigo Zone, Lachlan Fold Belt.|370.9 +/- 6.5 Ma.||||I-type. Weakly peraluminous biotite monzogranite.|
6227|Ercildoun Granite|75072|5|Briefly described|p230 Fig.2, 233-234, 241, 249, 253|Late Devonian|Late Devonian|Mount Bolton pluton, near Addington. Bendigo Zone. Zircon age spectra graph. Zircon age peaks discussed.|369.8 +/- 5.6 Ma (Clemens et al., 2022).||||Weakly peraluminous, porphyritic biotite micromonzogranite. I-type.|
30464|Erindale Granite|23309|6|Mentioned|p430 App1|||G296.||||||
30464|Erindale Granite|24177|4|Described|p61|Late Devonian|Late Devonian|Overlain by the Wild Duck Formation. Intrudes Castlemaine Group sediments.||||||
30464|Erindale Granite|24328|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|||||||
30464|Erindale Granite|24329|5|Briefly described|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
30464|Erindale Granite|60591|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Leucogranite: non-magnetic, medium-grained, equigranular; consists of quartz, muscovite pseudomorphing biotite, sericite.||||||
30464|Erindale Granite|60592|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Leucogranite: non-magnetic, medium-grained, equigranular; consists of quartz, muscovite pseudomorphing biotite, sericite.||||||
30464|Erindale Granite|60593|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Leucogranite: non-magnetic, medium-grained, equigranular; consists of quartz, muscovite pseudomorphing biotite, sericite.||||||
30464|Erindale Granite|60595|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Leucogranite: non-magnetic, medium-grained, equigranular; consists of quartz, muscovite pseudomorphing biotite, sericite.||||||
30464|Erindale Granite|60596|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Leucogranite: non-magnetic, medium-grained, equigranular; consists of quartz, muscovite pseudomorphing biotite, sericite.||||||
30464|Erindale Granite|60597|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Leucogranite: nonmagnetic.||||||
30464|Erindale Granite|60599|4|Described|p24 Tb. 4, p103, p80|Late Devonian|Late Devonian|The weathered rock is pale grey, medium-grained porphyritic leucogranite, with quartz up to 5mm across. Unconformably overlain by Wild Duck Formation. Assumed to intrude Castlemaine Supergroup sediments at depth. ||||||
30464|Erindale Granite|65715|6|Mentioned|p8 Tb.4|||G296. Of Edwards et al (1998) p103.||||||
30464|Erindale Granite|68116|5|Briefly described|Appendix, Map 24.|Late Devonian|Late Devonian||||||Leucogranite: nonmagnetic; medium-grained, equigranular; consists of quartz, muscovite pseudomorphing biotite, sericite.|
30464|Erindale Granite|73497|5|Briefly described|Map legend|Late Devonian|Late Devonian|G296.|||||Leucogranite: nonmagnetic.|
26538|Ernebank Granite|42726|5|Briefly described|map legend|Early Devonian||555. Variation on Ernebank Adamellite.||||||
28537|Errinundra Group|22530|6|Mentioned|p697||Early Devonian|||||||
28537|Errinundra Group|22628|6|Mentioned|fig1p108|Devonian|Devonian|||||||
28537|Errinundra Group|22876|4|Described|p15|Early Devonian|Early Devonian|Age: 400-390Ma.||||||13-NOV-08
28537|Errinundra Group|22877|5|Briefly described|map|Devonian|Devonian|||||||
28537|Errinundra Group|22968|6|Mentioned|P135||Early Devonian|||||||
28537|Errinundra Group|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
28537|Errinundra Group|23309|4|Described|p104-106, 129.  Table 2.39|Early Devonian|Early Devonian|||||||
28537|Errinundra Group|23615|5|Briefly described|p84|Early Devonian|Early Devonian|||||||
28537|Errinundra Group|24004|5|Briefly described|p275 Fig.2|Devonian|Silurian|||||||
28537|Errinundra Group|24266|5|Briefly described|p1483|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
28537|Errinundra Group|24551|3|Fully described|p148|||||||||
28537|Errinundra Group|40761|5|Briefly described|p233|||See also p234.||||||13-NOV-08
28537|Errinundra Group|41572|6|Mentioned|p23|||||||||
28537|Errinundra Group|41585|5|Briefly described|p140|||Mention Fig.4.7||||||
28537|Errinundra Group|41868|6|Mentioned|Table 12.3|||See also p585.||||||13-NOV-08
28537|Errinundra Group|42577|5|Briefly described|p29|||||||||
28537|Errinundra Group|42627|5|Briefly described|Map legend|Emsian|Pragian|||||||
28537|Errinundra Group|42647|3|Fully described|p29-|||||||||10-SEP-18
28537|Errinundra Group|42827|4|Described|p140|||||||||
28537|Errinundra Group|43228|5|Briefly described|p10||Early Devonian|||||||
28537|Errinundra Group|60503|5|Briefly described|p28 Fig. 9|Early Devonian|Early Devonian|||||||
28537|Errinundra Group|60541|6|Mentioned|p13, p11 Fig. 2|Early Devonian|Early Devonian|No known outcrops in Murrungowar area.  Also informally referred to as Errinundra Group Volcanics. See also p43, p116.||||||12-JAN-06
28537|Errinundra Group|60542|5|Briefly described|p11 Fig. 2|Early Devonian|Early Devonian|||||||
28537|Errinundra Group|61180|5|Briefly described|p7|Early Devonian|Early Devonian|Shallow marine sediments and volcaniclastics in a synclinal struture in the Mallacoota Gold Province.||||||
28537|Errinundra Group|61181|5|Briefly described|p13|||Thick sequence of marine clastics, volcaniclastics and acid volcanics formed in a rift-like extension basin.||||||
28537|Errinundra Group|61187|5|Briefly described|p5 Fig.3.|Early Devonian|Early Devonian|Mallacoota Zone, Benambra Terrane. Correlative of Snowy River Volcanics, Buchan Zone, Benambra Terrane.||||||
28537|Errinundra Group|66197|5|Briefly described|p634|Early Devonian||Boulder Creek Syncline. Silicic volcanics and marine sediments.||||||14-MAR-12
28537|Errinundra Group|70601|5|Briefly described|p28, p55|Pragian|Pragian|East Gippsland. Post-Benambran Orogeny.|||Bungywarr Formation.||Quartzose and lithic sandstones, felsic volcanics, limestones.|
28537|Errinundra Group|71040|5|Briefly described|p4 Fig.2, p13|Emsian|Emsian|Appears as Erinundra Group on p13.||||Is overlain unconformably by Combyingbar Formation.||
6337|Ettrick Formation|2967|6|Mentioned|p24|||Ludbrook (1957). Renamed Ettrick Marl (see references p14, p15 Fig.2.2, p24) and assigned to the Murray Group by Lawrence (1966).||||||
6337|Ettrick Formation|10010|5|Briefly described|p12 Fig. 3|Late Oligocene|Early Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||13-AUG-07
6337|Ettrick Formation|22587|6|Mentioned|p79 Fig.7|Late Oligocene|Early Oligocene|||||||
6337|Ettrick Formation|22626|6|Mentioned|446 fig 10|Early Miocene|Late Oligocene|Geol province Murray Basin. Overlying unit Lower Mannum Formation||||||
6337|Ettrick Formation|22773|5|Briefly described|p351,Fig24.8p352|Oligocene|Oligocene|||||||
6337|Ettrick Formation|22799|2|Defined|p30|Early Miocene|Oligocene|Murray Group.||||||13-AUG-07
6337|Ettrick Formation|22857|5|Briefly described|p351, p352 Fig.24.8|Early Miocene|Oligocene|Basal conglomerate of the Murray Group. Composed of sand and silt. Equivalent of Compton Conglomerate. Geological Province: Murray Basin. See also p353 Fig. 24.9.||||||
6337|Ettrick Formation|22887|5|Briefly described|Fig.6 p13||Early Oligocene|||||||
6337|Ettrick Formation|22893|5|Briefly described|fig4 p9|||||||||
6337|Ettrick Formation|22938|5|Briefly described|fig5|Oligocene|Oligocene|Eastern Mount Lofty Ranges.||||||
6337|Ettrick Formation|23179|6|Mentioned|Fig.2|Early Miocene|Late Oligocene|Murray Supergroup||||||
6337|Ettrick Formation|23226|6|Mentioned|p889,890,891,894|||Of Murray Supergroup.||||||
6337|Ettrick Formation|23671|6|Mentioned|p3|||Disconformably overlies the Renmark Beds.||||||
6337|Ettrick Formation|23768|5|Briefly described|p28 Fig.5|Miocene|Oligocene|Geological Province: Murray Basin.||||||11-SEP-09
6337|Ettrick Formation|23818|5|Briefly described|p174 Fig.84, p180|Oligocene|Oligocene|Geological Province: Murray Basin. Overlying units: Buccleuch Group and Renmark Beds.[this seems unlikely CEBDec 2013] Contains foraminifer Massilina torquayensis.||||||03-DEC-13
6337|Ettrick Formation|23884|5|Briefly described|p153, p155 Fig.13.2|Early Oligocene|Early Oligocene|Geological Province: Murray Basin||||||
6337|Ettrick Formation|23921|5|Briefly described|p1109|Early Miocene|Early Miocene|Geological Province: Murray Basin.||||||
6337|Ettrick 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 - Ettrick Formation not included.  Geological Province: Murray Basin.||||||
6337|Ettrick Formation|29591|6|Mentioned|Table 20|||||||||
6337|Ettrick Formation|29697|5|Briefly described|Table 1|||||||||
6337|Ettrick Formation|29828|6|Mentioned|p25|||||||||
6337|Ettrick Formation|29898|6|Mentioned|p216|||||||||
6337|Ettrick Formation|30751|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
6337|Ettrick Formation|30753|4|Described|Table 2|||Oligocene age||||||
6337|Ettrick Formation|30754|6|Mentioned|p14|||Stratigraphic table. See also P42 section||||||
6337|Ettrick Formation|30758|6|Mentioned|p66|||Oliogocene. Marine transgression||||||
6337|Ettrick Formation|30918|6|Mentioned|p85|||||||||
6337|Ettrick Formation|31241|6|Mentioned|p99|||Equivalent in age to Gambier Lst.||||||
6337|Ettrick Formation|31625|6|Mentioned|Fig. 5.2|||Oligocene||||||
6337|Ettrick Formation|31746|6|Mentioned|p194|||||||||
6337|Ettrick Formation|31848|5|Briefly described|p15|||Oligocene - Miocene||||||
6337|Ettrick Formation|31850|6|Mentioned|p36|||||||||
6337|Ettrick Formation|31851|4|Described|p12|||Lithostratigraphy.||||||
6337|Ettrick Formation|31922|6|Mentioned|p173|||||||||
6337|Ettrick Formation|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
6337|Ettrick Formation|32432|5|Briefly described|Table 1|||||||||
6337|Ettrick Formation|32653|6|Mentioned|p285|||||||||
6337|Ettrick Formation|32859|4|Described|p69|||Oligocene||||||
6337|Ettrick Formation|32862|6|Mentioned|Fig. 3|||Section from boreholes||||||
6337|Ettrick Formation|32864|6|Mentioned|Fig. 5|||||||||
6337|Ettrick Formation|33224|6|Mentioned|Fig.35|||Photo.||||||
6337|Ettrick Formation|33490|4|Described|p10|||See also p27. Oligocene -Miocene.||||||28-JUL-08
6337|Ettrick Formation|33798|6|Mentioned|p98|||Fig.2||||||
6337|Ettrick Formation|33834|5|Briefly described|p11|||||||||
6337|Ettrick Formation|33982|6|Mentioned|p116|||||||||
6337|Ettrick Formation|34029|5|Briefly described|Table 1|||Oligo-Miocene||||||
6337|Ettrick Formation|34114|6|Mentioned|Fig.2|||||||||
6337|Ettrick Formation|34191|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene - Miocene||||||
6337|Ettrick Formation|34295|5|Briefly described|p36|||Oligocene||||||
6337|Ettrick Formation|34296|4|Described|p97|||Olig.- Miocene. Lithology||||||
6337|Ettrick Formation|34308|5|Briefly described|p180|||Correlation chart. Olig.- L.Miocene||||||
6337|Ettrick Formation|34418|4|Described|p506|||Equivalent||||||
6337|Ettrick Formation|34461|5|Briefly described|p52|||Oligocene||||||
6337|Ettrick Formation|34758|6|Mentioned|Fig.2|||||||||
6337|Ettrick Formation|35071|6|Mentioned|Table 1|||||||||
6337|Ettrick Formation|35200|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
6337|Ettrick Formation|35232|6|Mentioned|p11|||See also Table 3.||||||
6337|Ettrick Formation|35541|6|Mentioned|p13|||||||||
6337|Ettrick Formation|37132|5|Briefly described|p368|||||||||
6337|Ettrick Formation|38068|6|Mentioned|Fig.7|||||||||
6337|Ettrick Formation|38070|6|Mentioned|Fig.12|||Murray Basin||||||
6337|Ettrick Formation|38601|6|Mentioned|p7|||||||||
6337|Ettrick Formation|39329|6|Mentioned|Fig.1|||||||||
6337|Ettrick Formation|39929|6|Mentioned|p268|||||||||
6337|Ettrick Formation|40003|5|Briefly described|p38|||||||||
6337|Ettrick Formation|40033|6|Mentioned|p228|||||||||
6337|Ettrick Formation|41478|5|Briefly described|Table 1|||||||||
6337|Ettrick Formation|41511|5|Briefly described|p18|||||||||
6337|Ettrick Formation|41517|6|Mentioned|p139|||||||||
6337|Ettrick Formation|41520|5|Briefly described|Fig.11|||||||||
6337|Ettrick Formation|42125|5|Briefly described|p135|||See also Fig.5||||||
6337|Ettrick Formation|42126|6|Mentioned|p156|||||||||
6337|Ettrick Formation|42127|5|Briefly described|p219|||See also Fig.3||||||
6337|Ettrick Formation|42129|6|Mentioned|p254|||See also Fig.6||||||
6337|Ettrick Formation|42130|6|Mentioned|Fig.3 P265|||||||||
6337|Ettrick Formation|42132|6|Mentioned|Fig.5 P298|||||||||
6337|Ettrick Formation|42134|6|Mentioned|Fig.3 P335|||||||||
6337|Ettrick Formation|42137|4|Described|p370|||See also Table 1||||||
6337|Ettrick Formation|42138|6|Mentioned|p388|||||||||
6337|Ettrick Formation|42443|5|Briefly described|p6|||||||||
6337|Ettrick Formation|42623|6|Mentioned|p2|||aquitard||||||
6337|Ettrick Formation|42717|5|Briefly described|map legend|Miocene|Oligocene|||||||
6337|Ettrick Formation|42881|4|Described|Fig.3, P84|||||||||
6337|Ettrick Formation|42966|2|Defined|p116|Early Miocene|Oligocene|Of Murray Group.||||||13-AUG-07
6337|Ettrick Formation|43073|4|Described|Table 3|||||||||
6337|Ettrick Formation|43195|5|Briefly described|Map Legend||Oligocene|See also commentary on back of map.||||||
6337|Ettrick Formation|43383|14|Not recorded|p29||Oligocene|||||||
6337|Ettrick Formation|43466|14|Not recorded|p3,fig.2,Pl.1|||Equivalent to SA||||||
6337|Ettrick Formation|43467|14|Not recorded|p3,20,25,31,32|||||||||
6337|Ettrick Formation|43667|6|Mentioned|Fig.3,p12|Miocene|Oligocene|||||||
6337|Ettrick Formation|43686|6|Mentioned|Fig.5,p233|||||||||
6337|Ettrick Formation|43780|6|Mentioned|p5|||||||||
6337|Ettrick Formation|43791|6|Mentioned|p372, Fig1|||||||||
6337|Ettrick Formation|43804|6|Mentioned|Fig.2,p49|||||||||
6337|Ettrick Formation|44133|5|Briefly described|p158, 152 Fig. 10.2|Early Miocene|Early Oligocene|Geological Province: Murray Basin. ||||||
6337|Ettrick Formation|44191|5|Briefly described|Map Legend||Late Oligocene|||||||
6337|Ettrick Formation|46802|6|Mentioned|Table 1|||||||||
6337|Ettrick Formation|46839|6|Mentioned|p82|||||||||
6337|Ettrick Formation|49038|4|Described|Table 2|||Briefly described p26.||||||19-SEP-18
6337|Ettrick Formation|49040|6|Mentioned|p11|||||||||
6337|Ettrick Formation|60785|5|Briefly described|p184 Fig.1, p195. |Chattian|Chattian|South Australia. Has yielded several fossil cetacean heterodont teeth.|||||Glauconitic marl, calcareous clay, and mudstone, with silt and sand.|
6337|Ettrick Formation|61155|5|Briefly described|p18||Early Oligocene|Of the Murray group. Glauconitic marls; diachronous. Overlain by Gambier Limestone; interfingers with Duddo Limestone and Geera Clay in central Murray Basin. Age: 32-14.9Ma. Max. thickness: 50m. Geological Province: Murray Basin. See also p3. p4.||||||03-MAR-10
6337|Ettrick Formation|61314|5|Briefly described|p129|Oligocene|Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||
6337|Ettrick Formation|63066|5|Briefly described|p485|||Revised stratigraphy of Lukasik and James (1999)  incorporates this unit,  the Geera Clay and Winnambool Formation into their new Murray Supergroup. These were not formerly included in the definition of the Murray Group.||||||08-FEB-07
6337|Ettrick Formation|63460|5|Briefly described|p837, p839 Fig. 2b|Erly Miocene|Late Oligocene|Overlain by Mannum Fm. Passes laterally into Winnambool Formation and Geera Clay to the north and east. Max. thickness" 40m. Geological province: Murray Basin. Dark grey-greenish, glauconitic calcareous clay and marl. ||||||
6337|Ettrick Formation|63887|5|Briefly described|p20, p21 Fig. 1|Middle Miocene|Late Oligocene|Of Murray Group. Marl.||||||
6337|Ettrick Formation|64237|4|Described|p17,p18,p18|Oligocene|Oligocene|Formerly part of the now obsolete Glenelg Group together with Compton Conglomerate; now incorporates Compton Conglomerate (obsolete) and is the basal unit of Murray Group ( in South Australia).||||||18-SEP-09
6337|Ettrick Formation|65552|5|Briefly described|p5 Fig. 3, p6|Middle Miocene|Late Oligocene|Deposited during the final stages of an Oligocene-Miocene marine incursion. Contemporaneous with Geera Clay, Murray Group and Winnambool, Olney Formations. Locally underlies Murray Group. Overlies Buccleuch beds.||||||
6337|Ettrick Formation|67462|5|Briefly described|Map legend.|||Murray Basin.||||||
6337|Ettrick Formation|68140|6|Mentioned|p1701|Neogene|Paleogene|Middle Tertiary age.||||||
6337|Ettrick Formation|68715|6|Mentioned|p31 Fig.5|Chattian|Rupelian|Murray Basin.||Murray Group.||||07-APR-17
6337|Ettrick Formation|70718|5|Briefly described|p24|Middle Miocene|Late Oligocene|Murray Basin. Deposited as a marginal-marine muddy facies.||||||
6337|Ettrick Formation|70961|14|Not recorded|p136|||Geological section.||||||
6337|Ettrick Formation|71248|14|Not recorded|p2||Oligocene|||||||
6337|Ettrick Formation|71593|4|Described|p52-p54|Miocene|Oligocene|Murray Basin. Palynology in Stavely 14 linked ot Ettrick Fm.||Murray Group||Interfingered with the Geera Clay, Olney Formation and the Calivil Formation.|Muddy shallow marine marl.|19-SEP-18
6337|Ettrick Formation|72445|5|Briefly described|App.7 p2, p5, p7 Fig.4, p19-20; App.2.|Middle Miocene|Early Oligocene|See also App.1, App.6 p1 Tb.1, p2 Fig.1, p4. Mentioned in text as marls in the far west of the Murray Basin (see Truswell 1987, Macphail & Truswell 1989). Identified in Stavely 08,11,14,16. App.6 sample in Stavely 11 include a high diversity of marine bioclast types including abundant bryozoans. A Middle Miocene M5 zone (16.39-15.73 Ma) determined from foraminifera(p.4, but table 1 gives M6 zone 15.10-14.78 Ma). Early Oligocene spore/pollen zone identified in samples from Stavely 14 (App.7).|16.39 - 14.78 Ma min age.|Murray Group||Shown as underlying Gambier Limestone. Overlies Renmark Group (unconformity), Olney Formation (gradational or sharp contact), Compton Conglomerate. Laterally equivalent with Geera Clay.|Including glauconitic marl, sand and limestone. Includes lesser silt and mud.|
6337|Ettrick Formation|73107|5|Briefly described|Map legend.|||Murray Basin. Equivalent to an un-named Oligocene unit of silicified dolomitic calcilutite, boulders of which are washed up at Cape Hart, Point Reynolds, Cape Linois and Cape Gantheaume.||||||
6337|Ettrick Formation|73118|5|Briefly described|p17, 24, 30, 34, 45, 82|||Murray Basin. Drill core summary logs. <30m thick. Almost entirely concealed. Deposited in shallow-marine, restricted platform to lagoonal environments.||Murray Group.||Overlies Olney Formation. Is overlain by Duddo Limestone and Geera Clay.|Weakly lithified grey, green glauconitic, highly fossiliferous calcareous clay (marl), silt, sandy skeletal clay, thin micritic limestone intercalations. Contains abundant and diverse faunas.|
6337|Ettrick Formation|73188|6|Mentioned|p320|Oligocene|Oligocene|Murray Basin.||||||
6337|Ettrick Formation|73228|4|Described|p50, p52-57, p60|Middle Miocene|Late Paleocene|Murray Basin. From the lower Murray Group. Estuarine and marginal marine depositional environments. Represents a transgressive phase of shallow-marine shelf environment. Identified in Cooltong 1, Berri North 1, Nadda 1, and Loxton 1 drillholes.||Murray Group, lower||Underlain by Renmark Group including Olney Formation. Overlain by Gambier Limestone.|Grey to green glauconitic and fossiliferous marl, calcareous clay and mudstone, and silt and fine quartz sand, as well as skeletal debris.|
6337|Ettrick Formation|73229|5|Briefly described|p66-67, p70-72, p74|Early Miocene|Late Oligocene|Murray Basin. [Analysed using pXRF; see article]. From the lower Murray Group.||Murray Group, lower|||Includes clayey limestone with interbedded clay and calcareous, glauconitic shelly fragments; glauconitic, fossiliferous marl; calcareous clay and mudstone; silt; fine-grained sand.|
6363|Eumeralla Formation|12781|5|Briefly described|p385-387, 391-392|Early Cretaceous|Early Cretaceous|Penola Trough, W Otway Basin. Excellent reservoir sands and shale seals.||Otway Supergroup.|Windermere Sandstone Member.|Overlies Katnook Sandstone (Crayfish Group). Is overlain unconformably by Waarre and Copa Formations (Sherbrook Group).||
6363|Eumeralla Formation|12796|5|Briefly described|p456 Fig. 2|Albian|Albian|Geological Province: Otway Basin.||||||
6363|Eumeralla Formation|22476|6|Mentioned|p952|||||||||
6363|Eumeralla Formation|22674|4|Described|p718, Fig.2 p719|Albian|Aptian|See also Fig.8 p725. Of Otway Supergroup.||||||
6363|Eumeralla Formation|22686|5|Briefly described|Fig3p745,746-47|Aptian|Albian| Geological Province: Otway Basin.||||||17-JAN-06
6363|Eumeralla Formation|22875|3|Fully described|p34|Aptian|Valanginian|Of the Crayfish Group.||||||24-APR-07
6363|Eumeralla Formation|22914|6|Mentioned|17|||||||||
6363|Eumeralla Formation|22930|6|Mentioned|50|||||||||
6363|Eumeralla Formation|23356|5|Briefly described|26 Tab.2|Early Cretaceous|Early Cretaceous|||||||
6363|Eumeralla Formation|23427|5|Briefly described|Table 11.2 p418.|||||||||
6363|Eumeralla Formation|23911|4|Described|p93, p95 Fig. 9B|Albian|Aptian|Geological Province: Otway Basin.  Max. Thickness: >2500m.  Underlain by Crayfish Subgroup. Of the Otway Group.||||||30-JAN-08
6363|Eumeralla Formation|24056|4|Described|p85|Early Cretaceous|Early Cretaceous|Of Otway Group.  Geological Basin: Otway Basin.||||||
6363|Eumeralla Formation|24113|5|Briefly described|p278|Early Cretaceous|Early Cretaceous|Geological Province: Otway Basin.  Of the Otway Supergroup.  Overlain by Crayfish Group.||||||24-APR-07
6363|Eumeralla Formation|24209|5|Briefly described|p154|||Interbedded siltstones, sandstones and coals.  Geological Province: Penola Trough (Otway Basin).||||||
6363|Eumeralla Formation|24284|6|Mentioned|p15 Fig.2|||In the Otway Basin.||||||24-APR-07
6363|Eumeralla Formation|24314|5|Briefly described|p61 Fig.2|Cenomanian|Hauterivian|Geological Province: Otway Basin. Of the Otway Supergroup.||||||30-NOV-04
6363|Eumeralla Formation|24323|5|Briefly described|p135|Albian|Aptian|Unconformably overlies the Crayfish Group and the Casterton Formation. Geological Province: Otway Basin.||||||
6363|Eumeralla Formation|24405|5|Briefly described|p6|||Geological Province: Otway Basin. Equivalent to Strzelecki Formation (Gippsland Basin).||||||
6363|Eumeralla Formation|24453|4|Described|p808, p809 Fig.2|Albian|Aptian|High energy braided river environment. Contains diverse vertebrate and invertebrate fossils. Overlies Windemere Sandstone Member and Crayfish Subgroup. Of Otway Group. Geological Province: Otway Basin.||||||26-JUN-13
6363|Eumeralla Formation|24455|6|Mentioned|p327|||Overlain unconformably in some areas by Dilwyn Formation.||||||
6363|Eumeralla Formation|24507|6|Mentioned|p26|Albian|Aptian|Geological Province: Otway Basin.||||||
6363|Eumeralla Formation|24551|5|Briefly described|p241, 243, 245, 250, 635|Albian|Aptian|Interfingers with the Pretty Hill Sandstone and the Geltwood Beech Formation. Overlain by Waarre Formation.||||||24-APR-07
6363|Eumeralla Formation|24561|5|Briefly described|p27, p41|||Geological Province: Otway Basin. Includes volcanigenic sediments.||||||26-JUN-13
6363|Eumeralla Formation|24562|5|Briefly described|p8 Fig. 2|Aptian|Aptian|Geological Province: Otway Basin.  Of the Otway Supergroup.  Maximum Thickness: 900m.||||||
6363|Eumeralla Formation|29856|6|Mentioned|p37|||||||||
6363|Eumeralla Formation|30576|5|Briefly described|Table 2|||||||||
6363|Eumeralla Formation|30578|6|Mentioned|p5|||See also Tables 1 and 2.||||||
6363|Eumeralla Formation|30905|6|Mentioned|p148|||||||||
6363|Eumeralla Formation|32898|6|Mentioned|Table 2-1|||||||||
6363|Eumeralla Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
6363|Eumeralla Formation|33940|6|Mentioned|p400|||L.Cret.||||||
6363|Eumeralla Formation|35290|6|Mentioned|p23|||||||||
6363|Eumeralla Formation|36499|6|Mentioned|p17|||Refers Reynolds et al 1966.||||||
6363|Eumeralla Formation|36913|6|Mentioned|Fig.2|||||||||
6363|Eumeralla Formation|38625|6|Mentioned|Table 2|||||||||
6363|Eumeralla Formation|39315|6|Mentioned|Fig.7|||||||||
6363|Eumeralla Formation|40560|5|Briefly described|Fig.3|||Mention p4.||||||24-APR-07
6363|Eumeralla Formation|41016|5|Briefly described|p214|||||||||
6363|Eumeralla Formation|41185|5|Briefly described|p177|||See Also Fig.4||||||
6363|Eumeralla Formation|41269|5|Briefly described|p245|||||||||
6363|Eumeralla Formation|41642|6|Mentioned|p218|||||||||
6363|Eumeralla Formation|41704|5|Briefly described|p99|||||||||
6363|Eumeralla Formation|41714|4|Described|p300|||See also p303.||||||24-APR-07
6363|Eumeralla Formation|41726|5|Briefly described|p420|||See also p422, p425.||||||24-APR-07
6363|Eumeralla Formation|41868|4|Described|p532,p533|||||||||
6363|Eumeralla Formation|41936|6|Mentioned|p77|||||||||
6363|Eumeralla Formation|42075|5|Briefly described|Fig.13 P252|||||||||
6363|Eumeralla Formation|42152|4|Described|p10|||See also p38.||||||24-APR-07
6363|Eumeralla Formation|42153|5|Briefly described|p352|||||||||
6363|Eumeralla Formation|42318|5|Briefly described|p6|||||||||
6363|Eumeralla Formation|42361|3|Fully described|p8|Albian|Aptian|||||||
6363|Eumeralla Formation|42415|6|Mentioned|p177|||||||||
6363|Eumeralla Formation|42524|4|Described|p27|||||||||
6363|Eumeralla Formation|42545|5|Briefly described|p18|||In the Otway Basin.||||||24-APR-07
6363|Eumeralla Formation|42555|5|Briefly described|Fig.2 P285|||||||||
6363|Eumeralla Formation|42599|5|Briefly described|Fig.3 P614|||||||||
6363|Eumeralla Formation|42601|6|Mentioned|Fig.2 p15|||||||||
6363|Eumeralla Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
6363|Eumeralla Formation|43171|4|Described|2-8|Albian|Aptian|Of the Otway Supergroup. Age: 100-120Ma.||||||24-APR-07
6363|Eumeralla Formation|43195|5|Briefly described|Map Legend||Early Cretaceous|See also commentary on back of map. Of Crayfish Group.||||||24-APR-07
6363|Eumeralla Formation|43208|5|Briefly described|map legend|Albian|Aptian|Of Otway Group.||||||
6363|Eumeralla Formation|43219|5|Briefly described|Fig.3,p6.|Albian|Aptian|Of the Otway Group.||||||24-APR-07
6363|Eumeralla Formation|43590|3|Fully described|p9|Albian|Aptian|||||||
6363|Eumeralla Formation|43744|6|Mentioned|Fig.3,p3|||||||||
6363|Eumeralla Formation|43783|6|Mentioned|Fig14, p11|||?Albian age||||||
6363|Eumeralla Formation|43784|6|Mentioned|Fig10, p12|||?Albian age||||||
6363|Eumeralla Formation|43814|6|Mentioned|Fig.3,p115|||||||||
6363|Eumeralla Formation|43937|5|Briefly described|Map Legend|Aptian|Kimmeridgian|||||||
6363|Eumeralla Formation|44133|4|Described|p145-146|Albian|Barremian|Of the Otway Supergroup. Geological Province: Otway Basin. Conformably overlies Windermere Sandstone Member. Thickness: 2350m. ||||||
6363|Eumeralla Formation|48911|3|Fully described|p13|Cretaceous|Cretaceous|||||||24-APR-07
6363|Eumeralla Formation|48977|6|Mentioned|Fig.5|||||||||
6363|Eumeralla Formation|49060|5|Briefly described|Fig.33|||||||||
6363|Eumeralla Formation|50043|5|Briefly described|p2, p10, 12|Early Albian|Late Aptian|A ?protoceratopsian ulna was recovered from this unit at Dinosaur Cove East.||Of Otway Group.||||27-MAR-12
6363|Eumeralla Formation|50154|2|Defined|p25, p131-132|Early Cretaceous|Early Cretaceous|Of the Otway Group. Unconformably overlain by Parilla Sand. Geological Province: Otway Basin. Interbedded mudstone and feldspathic sandstone and conglomerate.||||||15-SEP-04
6363|Eumeralla Formation|50155|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Fluvial; sandstone, siltstone, minor conglomerate, coal.||||||
6363|Eumeralla Formation|50156|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Of Otway Group. Overlies Nangeela Formation. Volcanilithic sandstone, siltstone, mudstone, mud-clast conglomerate, with feldspar and quartz grains, and coal: fine to medium grained, consolidated, well-bedded, cross-bedded; braided stream deposits||||||26-JUN-13
6363|Eumeralla Formation|50157|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Of Otway Group. Overlain by Renmark Group and Ettrick Marl. Volcanilithic sandstone, siltstone, mudstone, mud-clast conglomerate, with feldspar and quartz grains, and coal.||||||26-JUN-13
6363|Eumeralla Formation|50158|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Of Otway Group. Volcanilithic sandstone, siltstone, mudstone, mud-clast conglomerate, with feldspar and quartz grains, and coal: fine to medium grained, consolidated, well-bedded, cross-bedded; braided stream deposits||||||26-JUN-13
6363|Eumeralla Formation|50159|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Otway Group. Volcanilithic sandstone, siltstone, mudstone, mud-clast conglomerate, with feldspar and quartz grains, and coal: fine to medium grained, consolidated, well-bedded, cross-bedded; braided stream deposits||||||26-JUN-13
6363|Eumeralla Formation|50160|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Of Otway Group. Volcanilithic sandstone, siltstone, mudstone, mud-clast conglomerate, with feldspar and quartz grains and coal.||||||26-JUN-13
6363|Eumeralla Formation|50161|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Of Otway Group. Volcanilithic sandstone, siltstone, mudstone, mud-clast conglomerate, with feldspar and quartz grains, and coal: fine to medium grained, consolidated, well-bedded, cross-bedded; braided stream deposits||||||26-JUN-13
6363|Eumeralla Formation|50162|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Of Otway Group. Volcanilithic sandstone, siltstone, mudstone, mud-clast conglomerate, with feldspar and quartz grains, and coal: fine to medium grained, consolidated, well-bedded, cross-bedded; braided stream deposits||||||26-JUN-13
6363|Eumeralla Formation|50163|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Of Otway Group. Volcanilithic sandstone, siltstone, mudstone, mud-clast conglomerate, with feldspar and quartz grains, and coal: fine to medium grained, consolidated, well-bedded, cross-bedded; braided stream deposits||||||26-JUN-13
6363|Eumeralla Formation|60563|5|Briefly described|p45, p47|Early Cretaceous|Early Cretaceous|Includes Barwon River Member.||||||16-JUN-05
6363|Eumeralla Formation|61017|5|Briefly described|p5|Albian|Aptian|Of the Otway Group. Lacustrine to flood plain sediments. Unconformably overlies the Crayfish Subgroup. Geological Province: Otway Basin. See also p6 Fig. 3.||||||07-FEB-11
6363|Eumeralla Formation|61182|3|Fully described|p13-14, p83|||Of Otway Group. Together with Pretty Hill Formation, unconformable over Casterton Fm. Thick monotonous sequence of volcanilithic sandstone, siltstone, mudstone, intraformational mudclast conglomerate and minor coal; plant fossils. Geol.Prov: Otway Basin.||||||26-JUN-13
6363|Eumeralla Formation|61470|5|Briefly described|p28 Fig. 5|Albian|Aptian|Of the Otway Group. Geological Province: Otway Basin.||||||
6363|Eumeralla Formation|61528|5|Briefly described|p820|Albian|Hauterivian|Overlies Casterton Formation. Geological Province: Otway Basin. See also p821 Fig.2||||||
6363|Eumeralla Formation|61547|5|Briefly described|pp461-462, pp472-473. |Albian|Barremian|Deposited in a fluvio-lacustrine environment.|||Includes Windermere Sandstone Member.|Is unconformably overlain by the Sherbrook Group.|Consists of interbedded volcanigenic lithic sandstones, siltstones, coals and claystones.|26-JUN-13
6363|Eumeralla Formation|61553|6|Mentioned|p606.|||Chronostratigraphic equivalent of, with strong lithological similarity to, the Otway Megasequence (Bass Basin).||||||
6363|Eumeralla Formation|61622|5|Briefly described|p436, p438, p436 Fig. 2, p438 Fig. 4|Early Cretaceous|Early Cretaceous|Thickness 2500m. Geological Province: Otway Basin. Carbonaceous mudstones with minor sandstones and coal interbeds.||||||26-JUN-13
6363|Eumeralla Formation|61623|5|Briefly described|p447, p449, p450, p451, p449 Fig. 4|Early Cretaceous|Early Cretaceous|Of Otway Group. Includes Heathfield Member. Geological Province: Otway Basin.||||||07-APR-09
6363|Eumeralla Formation|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4, p489|Albian|Aptian|Of Otway Group. Geological Province: Otway Basin. Non-marine.||||||07-APR-09
6363|Eumeralla Formation|61628|5|Briefly described|p509 Fig. 3|Early Cretaceous|Early Cretaceous|Of Otway Group. Geological Province: Otway Basin.||||||07-APR-09
6363|Eumeralla Formation|63122|5|Briefly described|p17 Fig. 4.3, p20, p40|Albian|Barremian|Of the Otway Supergroup.Unconformably overlain by Copa Formation and Waarre Sandstone; overlies Crayfish Group.  Max. thickness: 2350m. Geological Province: Otway Basin.||||||26-JUN-13
6363|Eumeralla Formation|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p70-73|Albian|Barremian|Of Reynolds et al (1966). Includes basal Windermere Sandstone Member. Unconformably overlies Crayfish Gp; underlies Sherbrook Gp. Age:125-97Ma. Max. thickness: >2500m. Geological Province: Otway Basin.||||||
6363|Eumeralla Formation|63125|5|Briefly described|p108|Cretaceous|Cretaceous|Of the Otway Supergroup. Geological Province: Otway Basin. Contains a thick potential oil source sequence in the lower section characterised by thin bituminous coal seams up to 1m thick. ||||||
6363|Eumeralla Formation|63129|5|Briefly described|p127|||Geological Province: Otway Basin. Shales of this unit act as a top seal for the Windermere Sandstone Member.||||||30-JAN-08
6363|Eumeralla Formation|63130|6|Mentioned|p141, p143|||Overlain by Waarre Sandstone. Geological Province: Otway Basin. Primary hydrocarbon source for the Waarre Sandstone.||||||06-FEB-08
6363|Eumeralla Formation|63150|5|Briefly described|p95, p96|||Plant microfossils are abundant in claystone and coal, and only absent in any sandstone sections. Geological province: Otway Basin.||||||
6363|Eumeralla Formation|63267|5|Briefly described|p485 Fig.2, p486 Fig.3, p491, p496|Early Cretaceous|Early Cretaceous|Penola Trough, Otway Basin. Very thick sequence. Significance of faults discussed.||Otway Supergroup.|Windermere Sandstone Member.|Unconformably overlies Katnook Sandstone.||
6363|Eumeralla Formation|63269|5|Briefly described|p603, p605-606, p616, p618, p623-624|Albian|Aptian|Otway Basin. Thick, post-rift, fluvio-deltaic succession. Details of oils and oil stains in named wells tabulated. Oil-source correlation. Biomarker diagram.||Otway Group.||Unconformably overlies Katnook Sandstone. Is overlain unconformably by Waarre Formation (Sherbrook Group).||
6363|Eumeralla Formation|63431|5|Briefly described|p677 Fig. 2|Albian|Hauterivian|Part of the Otway Supergroup. Geological Province: Penola Trough/Otway Basin. See also p680.||||||07-FEB-11
6363|Eumeralla Formation|63445|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Fluvial, braided stream deposits.||Otway Group.|||Volcanolithic sandstone, siltstone, mudstone, with feldspar and quartz grains, fine- to medium-grained.|
6363|Eumeralla Formation|63446|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|||Unit in Otway Group.|||Fluvial: lithic sandstone, siltstone, minor conglomerate, coal.|
6363|Eumeralla Formation|64232|5|Briefly described|p12|Cretaceous|Cretaceous|Geological Province: Otway Basin. Coal measures are present in this unit.||||||24-JUL-08
6363|Eumeralla Formation|64535|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Otway Group. Sandstone, mudstone, mud-clast conglomerate, minor coal; blue-green to grey, arkose to feldsarenite, fine- to medium-grained, mostly medium to thick bedded, cross-bedded; fluvial deposits. ||||||
6363|Eumeralla Formation|64539|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Otway Group. Sandstone, mudstone, mud-clast conglomerate, minor coal; blue-green to grey, arkose to feldsarenite, fine- to medium-grained, mostly medium to thick bedded, cross-bedded; fluvial deposits. ||||||
6363|Eumeralla Formation|64540|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Otway Group. Sandstone, mudstone, mud-clast conglomerate, minor coal; blue-green to grey, arkose to feldsarenite, fine- to medium-grained, mostly medium to thick bedded, cross-bedded; fluvial deposits. ||||||
6363|Eumeralla Formation|64570|5|Briefly described|p858|||Of Otway Group. Age: 102.6+/-1.1Ma (K-Ar). Geological Province: Gippsland Basin.||||||22-DEC-08
6363|Eumeralla Formation|64605|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Otway Group. Sandstone, mudstone, mud-clast conglomerate, minor coal; alluvial deposits. bright red in RGB due to K-feldspar content. Nonmagnetic.||||||
6363|Eumeralla Formation|64616|3|Fully described|p142-143, p298|Early Cretaceous|Early Cretaceous|North of Tyers; at least 200m thick. Unit in Otway Group. Here includes rocks formerly assigned to Exalt Member (Rintoul Creek Formation). Has distinct and characteristic pink colour in RGB radiometric image. Gradationally overlies Locmany Formation. Mainly thick-bedded, medium- to coarse-grained, quartzose to (K-feldspar rich) lithic sandstone; mudstone, mud-clast conglomerate. The relatively rare fossils include coalified logs and charcoal. Geophysical characteristics given.||||||
6363|Eumeralla Formation|65715|4|Described|p9 Tb.6, p10, p15|Cretaceous|Cretaceous|Of Otway Group. Extended by VandenBerg et al (2006) to include Early Cretaceous arkoses of the Gippsland outcrops of Otway Group. Fluvial. Overlies and interfingers with Barwon River Conglomerate. Unconformaby overlain by Murraduc Basalt. Early Cretaceous.||||||
6363|Eumeralla Formation|65973|6|Mentioned|p14, p20|Aptian|Albian|Otway Basin. Strong affinities with the Strzelecki Group of the Gippsland Basin. Proven gas generator.||Otway Group||||
6363|Eumeralla Formation|66002|5|Briefly described|p9 Tb.6, p11, p16|Mesozoic|Mesozoic|Of Otway Group. Overlain by Wangerrip Group.  Defined by Reynolds et al. 1966. See also VandenBerg 2009.||||||16-FEB-17
6363|Eumeralla Formation|66181|5|Briefly described|p310 Fig.5|Albian|Hauterivian|Overlies the Tyers River Subgroup, in the Otway Group.||||||
6363|Eumeralla Formation|66244|5|Briefly described|p5.|||Formerly Wonthaggi Formation; re-named the Eumeralla Formation by VandenBerg et al. (2006) and VandenBerg (2008); it has identical mineralogical and radiometric RGB image characteristics across southern Victoria. Because of its entrenched use in the petroleum industry, the Wonthaggi Formation name is retained for Eumeralla Formation-equivalent rocks in the Gippsland Basin.||||||
6363|Eumeralla Formation|66245|5|Briefly described|p6 Fig.5, p30, p45. |Albian|Aptian|Fining westwards, indicating rift-opening from that direction. Source of Austral 2 petroleum system, after deposition of the thick clastic Sherbrook Group provided the necessary overburden to mature source intervals near the base of the Eumeralla Formation. A thin, often well-bedded sheet facies.||Uppermost unit in Otway Group.|||Dominantly fluvial sand, much of it derived from volcaniclastic sources to the east and northeast. |
6363|Eumeralla Formation|67061|5|Briefly described|p545, p546 Fig.3, pp549-551, p559.|Albian|Barremian|Deposition in fluvial channels. Maximum proven thickness c.3 km. A major stratigraphic break at the top of this Formation records regional uplift and exhumation beginning between 100 and 95 Ma; up to 2-3 km of this unit were eroded from the Otway Ranges.||Unit in Otway Group.|||A thick sequence of volcanigenic sandstones, with finer-grained sandstones, mudstones and shales.|16-MAR-12
6363|Eumeralla Formation|67366|5|Briefly described|p103 Fig.2, p104. |Albian|Aptian|Over 3000 m of fluvial-lacustrine sediments deposited during a quiescent period between two rifting events. Blankets the entire Otway Basin; is the primary source of hydrocarbons in the Port Campbell Embayment (onshore) and Shipwreck Trough (offshore).||Upper unit in Otway Supergroup.|||Volcaniclastic sandstone, shale and coal.|
6363|Eumeralla Formation|67367|5|Briefly described|p131 Fig.2, pp132-133, p155.|Albian|Aptian|Fluvial and coaly facies. Primary hydrocarbon source interval for the gas in Port Campbell Embayment and Shipwreck Trough. Assigned to the Austral 2 petroleum sub-system. The gas is considered to have been derived mainly from two coaly horizons, although organic-rich mudstones and shales have also contributed. Hydrocarbons have probably migrated up critically stressed, mostly NW trending, fault planes until they reached the Waarre Formation reservoir.||Unit in Otway Group.||||
6363|Eumeralla Formation|67541|6|Mentioned|p76 Fig.1|||||||||
6363|Eumeralla Formation|68116|5|Briefly described|Appendix, Maps 29, 38, 49-50, 54-55.|Early Cretaceous|Early Cretaceous||||||Sandstone, mudstone, mud-clast conglomerate, minor coal: blue-green to grey; arkose to feldsarenite; fine to medium grained, mostly medium to thick-bedded, cross-bedded.|
6363|Eumeralla Formation|68189|6|Mentioned|p3, p19 Fig.8, p25|Albian|Aptian|||Of the Otway Group.||||27-JUN-14
6363|Eumeralla Formation|69297|5|Briefly described|p79, p98, p99, p101, p103|Albian|Aptian|Otway Basin. Potential source rock in the Torquay Sub-basin of the Otway Basin. See also p104, p112, p143, p147, p150.||Otway Group|Includes the Windermere Sandstone Member and the Heathfield Sandstone Member. |Unconformably overlies the Katnook Sandstone. Overlain by the Waarre Formation and unconformably overlain by the Copa Formation. Equivalent to the Otway Megasequence.|Siltstone. |
6363|Eumeralla Formation|69651|5|Briefly described|p10, p12-13, p25, p49|Early Cretaceous|Early Cretaceous|Fluvial to lacustrine deposits. A key source rock in the Otway Basin.||Otway Group.||Unconformably overlies Katnook Sandstone (Crayfish Subgroup). Is overlain unconformably by Waarre Formation (Sherbrook Group).|Lithic sandstone with thin interbeds of carbonaceous shale; includes coaly facies towards the top.|
6363|Eumeralla Formation|69879|5|Briefly described|p424, p430-431|Albian|Albian|Otway Basin. Time-equivalent and lithologically similar to the Otway Megasequence. Believed to be source rock for hydrocarbon reservoirs of Thylacine gas-condensate field.|||||Carbonaceous siltstone and coal.|
6363|Eumeralla Formation|69948|6|Mentioned|Fig.4.2|||Otway Basin (a rift basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Eromanga Basin (an intracratonic basin).|||Windermere Sandstone Member.|Overlies Katnook Sandstone.||
6363|Eumeralla Formation|70076|5|Briefly described|Regional: p5|Albian|Aptian|Otway Basin. A proven gas-generating unit.||||Time-equivalent to Strzelecki Group (Gippsland Basin).||
6363|Eumeralla Formation|70077|5|Briefly described|Nelson:Fig.2. Regional: Fig.4, p6, p8-11|Albian|Albian|Otway Basin. The primary source for Austral 2 Petroleum System gas in the Port Campbell and Shipwreck Trough area. Has intraformational seals and provides seal to the Victorian part of the Penola Trough gas reservoirs.||Otway Group.|Heathfield and Windermere, Sandstone Members.|Overlies Katnook Sandstone or Pretty Hill Formation. Is overlain by Copa or Waarre Formations.|Includes coaly units.|
6363|Eumeralla Formation|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Albian|Albian|Gambier Embayment and Voluta Trough.||Otway Group.||Is overlain by Copa Formation.||
6363|Eumeralla Formation|70193|6|Mentioned|p284 Fig 1, 2, p285 fig 3|Albian||Geological province: Otway Basin. Part of the Sherbrook Supersequence.||||||
6363|Eumeralla Formation|70379|5|Briefly described|p723-727, p732|Early Cretaceous|Early Cretaceous|Otway Basin. There is an apparent overall thickening of this unit towards the centre of the Penola Trough, indicating activity on major faults at the time. Up to 1200m of sediments was eroded following late Albian-Cenomanian uplift. Barremian to Albian.||||Unconformably overlies Laira Formation. Is overlain by Sherbrook Group or (locally) Wangerrip Group.|Comparatively high-energy fluvial sediments.|
6363|Eumeralla Formation|70836|6|Mentioned|p473-474, 482|Albian|Aptian|Contains a nearly complete ulna from an indeterminate megaraptoran similar to Australovenator from the Winton Formation in QLD.||||||
6363|Eumeralla Formation|70880|6|Mentioned|p77|Albian|Aptian|Otway Basin.||||||
6363|Eumeralla Formation|71266|6|Mentioned|p614 Fig.3|Early Cretaceous|Early Cretaceous|Otway Basin.||||||
6363|Eumeralla Formation|71342|6|Mentioned|Ch4 p9|||Otway Basin. ||||||
6363|Eumeralla Formation|71419|5|Briefly described|p8 Fig 2, p16 Fig 17|Cretaceous|Cretaceous|Fluvial sediments. ||Of Otway Group.||||
6363|Eumeralla Formation|71601|6|Mentioned|p120, p121|Albian|Hauterivian|Dinosaur Cove, Flat Rocks, both Vic. Ankylosaurian remains have been identified.||||||
6363|Eumeralla Formation|72050|5|Briefly described|p233 Fig.2, 235-238, 240, 241 Fig.11|Albian|Aptian|Blanketed the whole of the Otway Basin. Rapidly deposited to an original thickness exceeding four kms. Believed to be the source rock for Late Cretaceous offshore gas-fields. See also p242.|||Heathfield Sandstone; Windermere Sandstone Member.||Shales, siltstones, coals and argillaceous sandstones.|
6363|Eumeralla Formation|73153|5|Briefly described|p284-290, p292|Albian|Albian|Otway Basin. A nearly complete middle cervical vertebra assigned to elaphrosaurinae was recovered from the unit at Cape Otway. Area was high latitude at the time of deposition. Deposited in a river channel-dominated, fluvial palaeoenvironment including braided river systems. The theropod fauna from this unit includes indeterminate tetanurans, megaraptorans, tyrannosauroids, indeterminate maniraptorans, and unenlagiine dromaeosaurids.||Otway Group|||Volcanogenic sandstones and claystones.|
6363|Eumeralla Formation|73217|5|Briefly described|p1007-1009, 1013, 1016-1017, 1019-1023|Early Cretaceous|Early Cretaceous|Eastern Otway Basin. Hosts extensive NE-oriented folds; the St George Anticline and Artillery Rocks folds and fracture sets are described in detail.|c.113-100 Ma.|||Is overlain by Eastern View Formation.|Volcaniclastic sandstone.|
6363|Eumeralla Formation|73356|6|Mentioned|p2-4, p9, p14-17, p22, p28-29|Albian|Albian|Deposited during a period of regional sag.||Otway Group||||
6363|Eumeralla Formation|73357|6|Mentioned|p17-19|Albian|Barremian|Otway Basin. Lower part correlated with Pilosisporites notensis Spore-Pollen Zone of Morgan et al., (2002a), largely terrestrial palynofloras. Upper part correlated with Crybelosporites striatus Spore-Pollen Zone and Coptospora paradoxa Zone, moderately frequent expression of brackish/marinal marine depositional environments. Uppermost part correlated to late Albian Phimopollenites pannosus Spore-Pollen Zone.||Of Otway Group.||Overlies Pretty Hill Formation.||
6363|Eumeralla Formation|73383|4|Described|p3-4, p7 Tb.3.1, p9, p16-18, p20-22, p25|Cenomanian|Aptian|Otway Basin. Equivalent to chemostratigraphic sequences S2 to S4. Contains high Ti/Cr values and volcanogenic content in Sequence S2, lower Ti/Cr values and a subtle increase in Si/Al values in S3, and is quartz-rich in S4. Winchester and Floyd (1977) classification of sequences to a uniform andesitic-dacitic composition. Non-marine, but higher S concentrations in upper parts may be linked to marine incursions. Lithologies based on geochemistry using the ChemLith classification includes limestone, calcareous mudstone, calcareous and argillaceous sandstones, calcareous limestone and igneous rocks; and using the Herron classification (1988) includes shale, Fe-sand, Fe-shale, lith-arenite, wacke, subarkose and quartz arenite. See also vi, p8 Tb.3.3, p11, p25-27, p35-41, p45-49, p58-62, p68-88, p96-100, p107-110, p119-126, p136-137, p140-153, p165-167, p168-171, p176-179, p190-194, p201-218, p225-229, p236-239, p248-253, p263-264, p267-278, p322-323.||Otway Group|Windermere Sandstone, Heathfield Sandstone|Unconformably overlies Crayfish Subgroup, Laira Formation, unconformably underlies Sherbrook Group, Waarre Formation|Volcaniclastic and subsidiary siliciclastic material. Includes fluvial volcanoclastics, lithicarenites, mudstones, coal, fluvial overbank and floodplain deposits, and more quartzose sandstone subunits.|
6363|Eumeralla Formation|73385|5|Briefly described|p3, p4 Fig.2.1, p5-6, p19-25, p28|Albian|Aptian|Otway Basin, outcrops in the Merino High, Barangarook High and Otway Ranges. Extensive unit deposited across the basin during a period of regional sag, thickens significantly south of the Mussel-Tartwaup Fault Zone.||Otway Group||Overlies Crayfish Subgroup, Laira Formation, Windamere Sandstone, underlies Waarre Formation, Sherbrook Group, interbedded with Heathfield Sandstone, Hawkesdale Volcanics.|Primarily composed of fluvial sands derived from volcanic sources. Contains fluvial volcanoclastics, lithicarenites, mudstones, coal, fluvial overbank and floodplain deposits.|
6363|Eumeralla Formation|73386|4|Described|p2-3, p4, p6-9, p13, Attachment A1|Albian|Barremian|Otway Basin. Late Barremian maximum age. Varies between 1500 m and 3000 m in thickness, thins from east to west and thins northwards due to erosion. Maximum thickness of approx. 7800 m in the Shipwreck Trough and southern edge of Mussel Platform. Fluvial and overbank depositional environments, sediments derived largely from the products of explosive dacitic volcanism. Contains the Cyclosporites hughesii, Crybelosporites striatus, Coptospora paradoxa and Phimopollenites pannosus spore-pollen zones of Partridge (2006). Chemostratigraphy identified three sequences within the formation, Sequence S2, S3 and S4 (Forbes et al., 2020). Overlies Paleozoic basement where the Crayfish Subgroup is absent.||Otway Group|Windermere Sandstone, Heathfield Sandstone, Killara coal measures|Unconformably overlies Crayfish Subgroup, Laira Formation, Katnook Sandstone, unconformably underlies Waarre Formation, Sherbrook Group|Sequence of fine- to medium-grained sandstones with interbedded mudstones, comprising quartz-poor volcanogenic derived sediments. Includes a basal sandstone member and black coals in lower part.|
6363|Eumeralla Formation|73594|4|Described|p3-4, p27-28, p34-44, p48-51, p66-67|Albian|Barremian|Otway Basin. Late Barremian to Albian in age. Fluvial, high latitude environment. Angular unconformity with Sherbrook Group in places of Cenomanian uplift such as the Otway Ranges. Locally over 2500 m thick onshore, estimated to be over 6000m thick offshore. Framework proposed by Kopsen and Schofield (1990) is used in this study, divides formation into upper, middle and lower units based on seismic character. Principal source of gas found in Late Cretaceous reservoirs. See also viii, p8, p14-15, p25, p45 Fig.5.19, p55, p59.||Otway Group|Windermere Member, Killara Coal Measures, Heathfield Member|Unconformably overlies Crayfish Subgroup. Conformably underlies Sherbrook Group, locally underlies Skull Creek Mudstone and unconformably underlies Waarre Formation.|Fine to medium-grained volcanogenic sandstones of predominantly litharenites and feldspathic litharenites with interbedded mudstones and coals, sporadic quartzose sandstones. Locally includes massive lacustrine clays in basal section.|
6363|Eumeralla Formation|75065|6|Mentioned|p157-159|||Constantine (2001). Otway Basin. Appears as Eumeralla Subgroup on p157.||||Correlates with Korumburra Subgroup.||
73285|Eumeralla Supersequence|63134|2|Defined|101|||||||||
73285|Eumeralla Supersequence|63269|5|Briefly described|p605-606, p609, p616, p618, p622-624|Early Cretaceous|Early Cretaceous|Otway Basin. Most oil-prone coals and shales are near the base. Oil-source correlation.|<115 Ma.|||Overlies Crayfish Supersequence. Is overlain by Shipwreck Supersequence.||
73285|Eumeralla Supersequence|69297|6|Mentioned|p77, p80, p81, p83, p96-p101|Lower Cretaceous|Lower Cretaceous|Nelson Sub-basin of the Otway Basin. Deposited in a fluvial or lacustrine environment. Interpreted from seismic data. See also p110, p114, p120, p370.||||||
73285|Eumeralla Supersequence|69651|5|Briefly described|p6, p10, p12-15, p17-19, p23, p25-26,p31|Albian|Early Cretaceous|See also p36-40, p42-44, p47, p49-50. Krassay et al. (2004). Otway Basin. Part of the Otway Supergroup. Potential source rocks. Fluvial to lacustrine deposits. Modelling diagrams.||||Overlies Crayfish Supersequence. Is overlain by Shipwreck Supersequence.|Argillaceous sandstone with interbedded claystone.|17-JUN-20
73285|Eumeralla Supersequence|70077|5|Briefly described|Nelson: p1. Regional: Fig.4; p3-4, p6-7|Early Cretaceous|Early Cretaceous|See also Regional: p9, p11 . Non-marine, fluvio-lacustrine deposits. A thick growth wedge in the ENE-trending Nerita Trough. Good potential source and reservoir rocks. Sealed by Eumeralla Formation shales both laterally and vertically.||||||
73285|Eumeralla Supersequence|70078|5|Briefly described|Regional: Fig.4; p3-4|Early Cretaceous|Early Cretaceous|Hosts part of Austral 2 petroleum system in Otway Basin. Seismic interpretation suggests it is present in the Sandy Cape Sub-basin.||||Is overlain by Shipwreck Supersequence.|Fluvial and lacustrine rocks, including coaly facies.|
73285|Eumeralla Supersequence|70880|5|Briefly described|p76-77, 81-83|Albian|Aptian|Otway Basin. Thins to the W and N. The likely source rock for gas accumulations in eastern Otway Basin. Is ~2.3 km thick in onshore Victoria; thickens slightly to the S until the shelf-edge break where it noticeably thins. Top surface is a major Basin-wide unconformity.||||Unconformably overlies Crayfish Supersequence. Is overlain unconformably by Shipwreck Supersequence.|Dominantly fluvio-lacustrine strata with a volcaniclastic sediment source.|
73285|Eumeralla Supersequence|71266|5|Briefly described|p614 Fig.3, p616-617, p620, p622 Fig.10|Early Cretaceous|Early Cretaceous|Otway Basin. Post-rift, thermal subsidence deposits. May be the source rock for gas accumulations in the eastern Otway Basin. Affected by faults; their growth is discussed in great detail.||||Overlies Crayfish Supersequence. Is overlain unconformably by Shipwreck Supersequence.|Fluvio-lacustrine deposits with evident volcaniclastic influence.|
76925|Euroa Volcanic Group|66244|5|Briefly described|p7.|Cenozoic|Cenozoic|Formerly Euroa Mafic Volcanics (Paul et al. 2005) to encompass all the Cenozoic mafic volcanics in the Euroa area. Upgraded to Group status because of its three constituents.|||Includes Killeen, Seven Creeks and Balmattum Basalts.||Mafic volcanics.|20-JUN-12
23584|Eustace Creek Granodiorite|23309|5|Briefly described|p430 App 1.||Early Devonian|Supersedes Eustace Creek Diorite. G108 I-Type. Age: 406+/-16Ma, 403+/-16 Ma, 433+/-17Ma, 440+/-9 Ma.||||||
23584|Eustace Creek Granodiorite|39221|3|Fully described|p267|||||||||
23584|Eustace Creek Granodiorite|43220|6|Mentioned|p10||Silurian|||||||
23584|Eustace Creek Granodiorite|44184|5|Briefly described|Map Legend||Early Silurian|||||||
23584|Eustace Creek Granodiorite|61160|6|Mentioned|p137|||||||||
23584|Eustace Creek Granodiorite|68116|5|Briefly described|Appendix, Map 27.|Early Devonian|Early Devonian||||||Hornblende granodiorite, quartz diorite: foliated, medium-grained.|
26542|Everard Granite|23309|5|Briefly described|p431 App 1|||Supersedes Everard Adamellite. G11 I-Type.||||||
26542|Everard Granite|42726|5|Briefly described|map legend|Early Devonian||139.  Of the Everard Suite.  Not intended as a formal name.  Variation on Everard Adamellite. I-type; felsic; fractionated.||||||08-FEB-05
26542|Everard Granite|42827|6|Mentioned|p24|||||||||
26542|Everard Granite|68115|6|Mentioned|p6.|||Tamboon area.||||||
26542|Everard Granite|68116|5|Briefly described|Appendix, Maps 37, 46.|Early Devonian|Early Devonian||||||Biotite granite: I-type.|
6408|Everard Suite|24551|6|Mentioned|p235|||||||||
6408|Everard Suite|42726|5|Briefly described|map legend||Early Devonian|Contains the informal Everard Granite.||||||08-FEB-05
6408|Everard Suite|42827|6|Mentioned|p430|||||||||
6427|Eversley Granite|22756|6|Mentioned|P44|||||||||
6427|Eversley Granite|23309|6|Mentioned|p431 App 1|||G375 I-Type.||||||
6427|Eversley Granite|42726|5|Briefly described|map legend|Early Devonian||Reserved as Eversley Granodiorite, in 1993.||||||
6427|Eversley Granite|44186|5|Briefly described|Map Legend||Early Devonian|G375 Unassigned.||||||
6427|Eversley Granite|66002|5|Briefly described|p7 Tb.5|||Of Mount Cole Suite. G375.  Defined by Cayley and McDonald 1995.||||||
6427|Eversley Granite|67978|5|Briefly described|p499 Tb.1|Frasnian|Emsian|Zircon dating of granodiorite from  a tor-topped hill on the northern side Eversley-Coralynn road (Black, unpublished data)|389 +/- 12 Ma, SIMS U-Pb|Of the Mount Cole Suite.||||
6427|Eversley Granite|68116|5|Briefly described|Appendix, Map 31.|Early Devonian|Early Devonian||||||Biotite granodiorite: pale grey; medium grained; felsic; slightly porphyritic; outer biotite-rich parts are highly weathered.|
27771|Everton Granodiorite|22971|5|Briefly described|p 33|||||||||
27771|Everton Granodiorite|23309|6|Mentioned|p431 App1|||G198 I-Type. Supersedes Everton Granodiorite Porphyrite and Everton Granite.||||||
27771|Everton Granodiorite|24551|6|Mentioned|p229, 725 Table 8.8, 448|Early Devonian|Early Devonian|Of the Tabberabbera Province.||||||
27771|Everton Granodiorite|31713|5|Briefly described|p13|||||||||
27771|Everton Granodiorite|31800|6|Mentioned|p204|||Map legend||||||
27771|Everton Granodiorite|35257|6|Mentioned|p154|||||||||
27771|Everton Granodiorite|35278|6|Mentioned|p356|||||||||
27771|Everton Granodiorite|37885|4|Described|p3|||||||||
27771|Everton Granodiorite|68116|5|Briefly described|Appendix, Map 19.|Late Devonian|Late Devonian||||||Hornblende-biotite granodiorite: fine-grained, pink K-feldspar phenocrysts, accessory magnetite, allanite, sphene, apatite, zircon and fluorite.|
27771|Everton Granodiorite|70910|14|Not recorded|p44|||Geological map on opposite page.||||||
34014|Exalt Member|22476|2|Defined|p957,8||Neocomian|||||||
34014|Exalt Member|24453|4|Described|p808, p809 Fig.2|Hauterivian|Valanginian|Trough cross-bedded sandstones of Braided River environment. Of Rintoul Creek Formation. Thickness: 120 m. Geological Province: Gippsland Basin.||||||07-FEB-11
34014|Exalt Member|24551|5|Briefly described|p263|||Of the Rintoul Creek Formation. Overlies: Locmany Member||||||
34014|Exalt Member|64616|5|Briefly described|p142 Tb.5.6, p143|Early Cretaceous|Early Cretaceous|Of Tosolini et al. (1999). Upper Member of Rintoul Creek Formation, overlying Locmany Member. Name proposed to be dropped and the rocks included within Eumeralla Formation.||||||
34014|Exalt Member|70378|5|Briefly described|p695, p702 Fig.7, p707|Early Cretaceous|Early Cretaceous|Tosolini et al. (1999). Over 200m thick. Measured sections.||Rintoul Creek Formation.||Overlies Locmany Member. Is overlain by Wonthaggi Formation.|Siliceous, interbedded sandstones and shales.|
29835|Fainting Range Ignimbrite|22968|5|Briefly described|P66, P134, P132||Early Devonian|Parent is the Mount Elizabeth Caldera Complex.||||||25-SEP-08
29835|Fainting Range Ignimbrite|23021|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is Mount Elizabeth Caldera Complex.||||||25-SEP-08
29835|Fainting Range Ignimbrite|23028|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is Mount Elizabeth Caldera Complex, overlying unit is Tongio Munjie Ignimbrite.||||||25-SEP-08
29835|Fainting Range Ignimbrite|23309|5|Briefly described|p123, 133-134.|||Parent: Mount Elizabeth Cauldron Complex.||||||25-SEP-08
29835|Fainting Range Ignimbrite|23938|6|Mentioned|p70 Tb. 6|||See also p73 Fig. 26.||||||25-SEP-08
29835|Fainting Range Ignimbrite|24551|5|Briefly described|p149|||Part of the Mount Elizabeth Cauldron Complex.||||||
29835|Fainting Range Ignimbrite|43284|5|Briefly described|Map Legend||Early Devonian|Of Tara Range Subgroup.||||||25-SEP-08
29835|Fainting Range Ignimbrite|68115|5|Briefly described|p5.|Devonian|Devonian|Originally included in Tara Range Subgroup of the Snowy River Volcanic Group (Simpson et al. 1996); later placed in the Mount Elizabeth Caldera Complex by Willman et al. (1999).||Unit in Mount Elizabeth Caldera Complex.||||
29835|Fainting Range Ignimbrite|68116|5|Briefly described|Appendix, Maps 35, 44.|Early Devonian|Early Devonian||||||Vitric ignimbrite: black; pumiceous; up to 10% feldspar and rare quartz phenocrysts.|
38063|Fairview Andesite Breccia|23402|3|Fully described|p9, p8 Tb. 1|Late Cambrian|Late Cambrian|Parent: Mount Stavely Volcanic Complex.   Thickness: 2500m.   Overlain by/intertongued with Nanapundah Tuff.   Geological Province: Adelaide Fold Belt||||||
38063|Fairview Andesite Breccia|50371|5|Briefly described|Map Legend|Cambrian|Cambrian|Of Mount Stavely Volcanic Complex. Massive andesitic breccia, minor andesite and basalt lava flow||||||
38063|Fairview Andesite Breccia|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Mount Stavely Volcanic Complex. Includes Glenronald Shale Member. Defined by Buckland 1986.||||||
38063|Fairview Andesite Breccia|70211|6|Mentioned|p3|||Stavely region.||||||
38063|Fairview Andesite Breccia|70877|4|Described|p2, p48-p53, p61, p80, p168, p172, p190|Cambrian|Cambrian|Grampians-Stavely Zone. SHRIMP ages derived from this study and represent the age of magmatic crystallisation. An age of 501 +/- 9 Ma was suggested (Donaghy, 1994); however Stuart-Smith and Black 1999 attributed that age to Towanway Tuff. Petrography, zircon morphology and SHRIMP U-Pb results are discussed in detail for a sample of this unit.|502 +/- 12 Ma (SHRIMP U-Pb)|Mount Stavely Volcanic Complex||Overlain by the Narrapumelap Road Dacite Member and structurally overlain by the Towanway Tuff.|Andesitic breccia consisting of three plagioclase-phyric andesite units.|
38063|Fairview Andesite Breccia|71593|5|Briefly described|p9, p29, p31, p39-p40, p140, p163|||The type locality for this unit occurs in the Stavely Belt segment. Age is complicated by resetting of the Ar/Ar leading to many discordant spectra, the provided age is derived from the most concordant ones.|510 +/- 2 Ma (Ar/Ar, Bucher, 1998)|Mount Stavely Volcanic Complex|||Andesite, dacite and minor basaltic lava in a volcanolithic matrix.|
30548|Fairy Sandstone|23309|4|Described|p108 Table 2.40, 114, 118|||Maximum Thickness: 550m.  Of the Little River Subgroup.||||||22-FEB-10
30548|Fairy Sandstone|23615|3|Fully described|p120|Early Devonian|Early Devonian|Supersedes Fairy Formation (Teichert and Talent, 1958) and Fairy Member of the Timbarra Formation (Fletcher, 1963). Renamed to emphasise the main lithology.  Of Little River Subgroup. Overlain by Frying Pan Cr. Ignimbrite at Gillingall.  Max.thick: 550m.||||||
30548|Fairy Sandstone|23938|5|Briefly described|p55 Tb. 4, p56|Early Devonian|Early Devonian|Probably supersedes the Fairy Formation? Of the Snowy River Volcanics. See also p63-65 Figs. 23-24, p96, 98.||||||
30548|Fairy Sandstone|24551|6|Mentioned|p145 Fig. 5.37, 606, 439|||Probably should be Fairy Formation.||||||
30548|Fairy Sandstone|43206|5|Briefly described|map legend||Lochkovian|Of Little River Subgroup..||||||25-SEP-08
30548|Fairy Sandstone|43312|5|Briefly described|Map Legend||Early Devonian|Of Little River Group.||||||25-SEP-08
30548|Fairy Sandstone|43313|5|Briefly described|Map Legend||Early Devonian|Of Little River Group.||||||25-SEP-08
30548|Fairy Sandstone|60542|3|Fully described|p61, p79|Early Devonian|Early Devonian|Of Little River Subgroup. Supersedes Fairy Mbr of the Timbarra Fm. Breccia-conglomerate with ignimbrite and lava clasts. Conformably overlain by McRaes Ignimbrite; conformably overlies Carson Creek Ignimbrite.||||||
30548|Fairy Sandstone|68116|5|Briefly described|Appendix, Maps 36, 45.|Pragian|Pragian||||||Tuff, ignimbrite, sandstone, siltstone, breccia, conglomerate: generally thin-bedded; pyroclastic and fluvial deposits.|
69410|Faithfuls Leucogranite|61160|4|Described|p61, p33 Tb. 5.2|Early Silurian|Early Silurian|S-type. Contains large (2cm) dark round clots of biotite, muscovite and quartz in a medium-grained groundmass of feldspar and quartz. Surrounded by Cobungra Granite and is assumed to have intruded the granite. See also p58-59 Fig. 6.8.||||||
69410|Faithfuls Leucogranite|61164|5|Briefly described|map legend|Early Silurian|Early Silurian|Garnet-sillimanite-cordierite leucogranite: medium grained; equigranular to porphyritic with large cordierite phenocrysts; S-type intrusion. GSV map code: G157.||||||
69410|Faithfuls Leucogranite|61165|5|Briefly described|map legend|Early Silurian|Early Silurian|Garnet-sillimanite-cordierite leucogranite: medium grained; equigranular to porphyritic with large cordierite phenocrysts; S-type intrusion. GSV map code: G157.||||||
69410|Faithfuls Leucogranite|61166|5|Briefly described|map legend|Early Silurian|Early Silurian|Garnet-sillimanite-cordierite leucogranite: medium grained; equigranular to porphyritic with large cordierite phenocrysts; S-type intrusion. GSV map code: G157.||||||
69410|Faithfuls Leucogranite|61167|5|Briefly described|map legend|Early Silurian|Early Silurian|Garnet-sillimanite-cordierite leucogranite: medium grained; equigranular to porphyritic with large cordierite phenocrysts; S-type intrusion. GSV map code: G157.||||||07-FEB-11
69410|Faithfuls Leucogranite|61168|5|Briefly described|map legend|Early Silurian|Early Silurian|Garnet-sillimanite-cordierite leucogranite: S-type; nonmagnetic (kv = 0-5 10^-6 cgs); no appreciable gravity response (-416 ums^-2); moderate total radioelement, high K, low Th and U. GSV map code: G157.||||||
69698|Falls Creek Suite|61160|4|Described|p54, p70|Devonian|Devonian|Formerly the Falls Creek Series of Fagan (1979). Comprises: East Kiewa and Niggerheads Granodiorites, Dinner Plain, Carruno and High Tops Tonalites. I-type granites. See also p58-59 Fig. 6.8.||||||
69698|Falls Creek Suite|61161|5|Briefly described|p91, p76-77 Fig 6.1|Early Devonian|Early Devonian|Willman et al (1999) separated out several intrusions into Ensay Suite and Polar Star Suite. Falls Creek Suite redefined (Morand et al 2005) retains some I-type granites based on chemical composition. Includes High Tops Tonalite and Dinner Plain Tonalite.||||||
69698|Falls Creek Suite|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes East Kiewa Granodiorite, Niggerheads Granodiorite, Carruno Tonalite, Dinner Plain Tonalite and High Tops Tonalite.||||||
69698|Falls Creek Suite|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes East Kiewa Granodiorite, Niggerheads Granodiorite, Carruno Tonalite, Dinner Plain Tonalite and High Tops Tonalite.||||||
69698|Falls Creek Suite|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes East Kiewa Granodiorite, Niggerheads Granodiorite, Carruno Tonalite, Dinner Plain Tonalite and High Tops Tonalite.||||||
69698|Falls Creek Suite|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes East Kiewa Granodiorite, Niggerheads Granodiorite, Carruno Tonalite, Dinner Plain Tonalite and High Tops Tonalite.||||||07-FEB-11
69698|Falls Creek Suite|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes East Kiewa Granodiorite, Niggerheads Granodiorite, Carruno Tonalite, Dinner Plain Tonalite and High Tops Tonalite.||||||
69698|Falls Creek Suite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Dinner Plain Tonalite and High Tops Tonalite.||||||08-SEP-05
69698|Falls Creek Suite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Dinner Plain Tonalite and High Tops Tonalite.||||||07-FEB-11
69698|Falls Creek Suite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Dinner Plain Tonalite and High Tops Tonalite.||||||
69698|Falls Creek Suite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Dinner Plain Tonalite and High Tops Tonalite.||||||
69698|Falls Creek Suite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Dinner Plain Tonalite and High Tops Tonalite.||||||
6536|Farquhar Limestone Member|23309|5|Briefly described|p86, 95|Early Silurian|Early Silurian|||Towanga Sandstone||||31-OCT-14
6536|Farquhar Limestone Member|23710|5|Briefly described|p70|||||||||
6536|Farquhar Limestone Member|24551|6|Mentioned|p614||Late Llandovery|Of the Towanga Formation||||||
6536|Farquhar Limestone Member|37727|5|Briefly described|p49|||See also P19.||||||
6536|Farquhar Limestone Member|39447|6|Mentioned|p9|||||||||
6536|Farquhar Limestone Member|40328|6|Mentioned|p71|||||||||
39627|Federal Basalt|24087|6|Mentioned|p330 Fig. 4|||Geological Province: Lachlan Fold Belt.||||||
28549|Feltis Farm Tonalite|23309|6|Mentioned|p431 App 1|||G47 I-Type. Age: 369 +/- 4 Ma. Supersedes Feltis Farm Granite.||||||
28549|Feltis Farm Tonalite|23615|3|Fully described|p159, 152, 201|Devonian|Late Silurian|See also p201 App 1. Age: 369+/-4Ma (Henley and Webb, 1990).  Intrudes Pinnak Sandstone. K/Ar age likely to reflect argon loss. Intrusive age more likely to be middle Silurian.||||||04-NOV-14
28549|Feltis Farm Tonalite|23938|6|Mentioned|p70 Tb. 6|||See also p75 Fig. 27.||||||25-SEP-08
28549|Feltis Farm Tonalite|24551|6|Mentioned|p235|||||||||
28549|Feltis Farm Tonalite|42647|6|Mentioned|p38|||Murrindal area. Reserved as Feltis Farm Granite.||||||
28549|Feltis Farm Tonalite|43206|5|Briefly described|map legend||Wenlock|||||||
28549|Feltis Farm Tonalite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|Of Bete Bolong Suite. I-type. Coarse grained, hornblende, bitotie tonalite.||||||25-SEP-08
28549|Feltis Farm Tonalite|43315|5|Briefly described|Map Legend||Wenlock|Of the Bete Bolong Suite. I-type. Coarse-grained, hornblende, biotite tonalite.||||||03-MAY-05
28549|Feltis Farm Tonalite|44185|5|Briefly described|Map legend.|||I-type. Age uncertain: shown as SDg, ie Silurian-Devonian.||||||
28549|Feltis Farm Tonalite|60541|5|Briefly described|p16, p62, p93|Silurian|Silurian|Part of this intrusive pluton is of the Bete Bolong Suite. The magnetics suggest a multiphase intrusive history for this unit. Age is Middle Silurian. Geological Province: Lachlan Fold Belt. See also p18 Tb. 1.||||||
28549|Feltis Farm Tonalite|60542|4|Described|p90, p19 Fig. 3|Late Silurian|Late Silurian|Of Bete Bolong Suite. Similar to other granites of the B.B. Suite. Contains large elongate hornblende crystals (up to 10mm) in some rock, in others hornblendes are smaller. Intruded the Pinnak Sandstone.||||||
28549|Feltis Farm Tonalite|61187|5|Briefly described|p114, p122, p123 Fig.8.|||A large (c.10 by 7 km) pluton. Hosts the sub-economic Sunday Creek Prospect. Early-reported mineralisation (quartz vein) occurs at this unit's contact with a small outlier of Ordovician cherty rocks; ore minerals included chalcopyrite and lesser pyrite, gold and galena.||Unit in Bete Belong Suite.||Is overlain by Pinnak Sandstone.|Mainly hornblende tonalite.|
28549|Feltis Farm Tonalite|68116|5|Briefly described|Appendix, Map 36.|Devonian|Silurian||||||Hornblende-biotite tonalite: grey-green; fine to medium-grained; altered; I-type.|
41193|Fern Hill Microgranite|50154|2|Defined|p114, p117, p244 App.5|Devonian|Devonian|Of the Rocklands Volcanic Group. Nonconformably overlain by the Newer Volcanics. Probably intrudes Nigretta Ignimbrite.||||||25-SEP-09
41193|Fern Hill Microgranite|50155|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Leucocratic granophyric microgranite||||||
41193|Fern Hill Microgranite|50156|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Leucocratic microgranite: granophyric, medium grained; pink; weakly porphyritic in alkali feldspar||||||
41193|Fern Hill Microgranite|50157|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Leucocratic microgranite: granophyric, medium grained; pink; weakly porphyritic in alkali feldspar||||||
41193|Fern Hill Microgranite|50158|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Leucocratic microgranite: granophyric, medium grained; pink; weakly porphyritic in alkali feldspar||||||
41193|Fern Hill Microgranite|50159|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Leucocratic microgranite: granophyric, medium grained; pink; weakly porphyritic in alkali feldspar||||||24-JUN-04
41193|Fern Hill Microgranite|50160|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Leucocratic microgranite||||||
41193|Fern Hill Microgranite|50161|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Leucocratic microgranite: granophyric, medium grained; pink; weakly porphyritic in alkali feldspar||||||24-JUN-04
41193|Fern Hill Microgranite|50162|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Leucocratic microgranite: granophyric, medium grained; pink; weakly porphyritic in alkali feldspar||||||24-JUN-04
41193|Fern Hill Microgranite|50163|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Leucocratic microgranite: granophyric, medium grained; pink; weakly porphyritic in alkali feldspar||||||24-JUN-04
41193|Fern Hill Microgranite|66002|5|Briefly described|p6 Tb.4|Devonian|Devonian|Of Rocklands Volcanic Group. Defined in Morand et al. 2003.||||||
6619|Ferny Creek Rhyodacite|23268|6|Mentioned|Fig14-2.1p388|||||||||
6619|Ferny Creek Rhyodacite|23269|4|Described|p402, Fig14-3.3p405, 406||Late Devonian|||||||
6619|Ferny Creek Rhyodacite|23309|4|Described|p166, 167 Table 2.60/2.62|Middle Devonian|Devonian| Identical composition to Donna Buang Rhyodacite.  Age: Givetian K/Ar Biotite 376+/-6/370+/-13/372+/-13/370+/-13 Ma.||||||
6619|Ferny Creek Rhyodacite|24551|5|Briefly described|p161, 583|Devonian|Devonian|Part of the Dandenong Ranges Igneous Complex.||||||
6619|Ferny Creek Rhyodacite|29652|6|Mentioned|Table 4|||||||||
6619|Ferny Creek Rhyodacite|29653|6|Mentioned|p4|||||||||
6619|Ferny Creek Rhyodacite|30867|6|Mentioned|p15|||Refers Vandenberg (1971)||||||
6619|Ferny Creek Rhyodacite|33157|4|Described|p42|||||||||
6619|Ferny Creek Rhyodacite|33598|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
6619|Ferny Creek Rhyodacite|33599|4|Described|p8|||||||||
6619|Ferny Creek Rhyodacite|33604|6|Mentioned|p19|||||||||
6619|Ferny Creek Rhyodacite|34956|6|Mentioned|p82|||||||||
6619|Ferny Creek Rhyodacite|35012|6|Mentioned|p430|||||||||
6619|Ferny Creek Rhyodacite|35277|4|Described|p95|||||||||
6619|Ferny Creek Rhyodacite|39291|6|Mentioned|Fig.13|||||||||
6619|Ferny Creek Rhyodacite|41641|4|Described|p165|||||||||
6619|Ferny Creek Rhyodacite|42827|4|Described|p165|||of Mount Dandenong Volcanics||||||
6619|Ferny Creek Rhyodacite|44197|5|Briefly described|Map Legend||Late Devonian|||||||
6619|Ferny Creek Rhyodacite|60083|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Mount Dandenong Volcanics Group.  Hypersthene rhyodacite; schistose dacite in metamorphic aureoles.||||||04-JUN-14
6619|Ferny Creek Rhyodacite|68116|5|Briefly described|Appendix, Map 42.|Late Devonian|Late Devonian||||||Biotite-hypersthene rhyodacite ignimbrite: recrystallized; chilled glassy base shows traces of eutaxic foliation parallel to the sediment band below; becomes increasingly crystalline and phenocryst-rich upwards.|
37242|Ferres Creek Tonalite|23309|5|Briefly described|p335, Table 2.14|Silurian|Ordovician|G423. I-Type. Age: 428+/-18Ma. Geological Province: Delamerian Fold Belt||||||12-JUN-15
37242|Ferres Creek Tonalite|24012|3|Fully described|p222 appendix 1|Ordovician|Cambrian|||||||
37242|Ferres Creek Tonalite|50154|2|Defined|p36, p81|Early Ordovician|Middle Cambrian|Of Caupaul Igneous Complex. Intruded by Dergholm Granite. Intrusive age is Middle Cambrian to Earliest Ordovician. Fission track apatite date of 428 +/- 18 (Gleadow & Lovering,1978) indicates a heating or hydrothermal event .||||||16-MAY-13
37242|Ferres Creek Tonalite|50156|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Biotite-hornblende tonalite: foliated, medium to coarse grained, equigranular; accessory quartz, microcline, magnetite and epidote; some samples contain clinopyroxene||||||
37242|Ferres Creek Tonalite|50157|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Caupaul Igneous Complex. Biotite-hornblende tonalite: foliated, grey, medium to coarse grained, equigranular; accessory quartz, microcline, magnetite and epidote; some samples contain clinopyroxene||||||24-JUN-04
37242|Ferres Creek Tonalite|50158|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Caupaul Igneous Complex. Biotite-hornblende tonalite: foliated, medium to coarse grained, equigranular; accessory quartz, microcline, magnetite and epidote; some samples contain clinopyroxene||||||
37242|Ferres Creek Tonalite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Caupaul Igneous Complex. Biotite-hornblende tonalite: foliated, medium to coarse grained, equigranular; accessory quartz, microcline, magnetite and epidote; some samples contain clinopyroxene||||||24-JUN-04
37242|Ferres Creek Tonalite|50160|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Caupaul Igneous Complex. Biotite-hornblende tonalite||||||
37242|Ferres Creek Tonalite|50161|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Caupaul Igneous Complex. Biotite-hornblende tonalite: foliated, medium to coarse grained, equigranular; accessory quartz, microcline, magnetite and epidote; some samples contain clinopyroxene||||||24-JUN-04
37242|Ferres Creek Tonalite|50162|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Caupaul Igneous Complex. Biotite-hornblende tonalite: foliated, medium to coarse grained, equigranular; accessory quartz, microcline, magnetite and epidote; some samples contain clinopyroxene||||||24-JUN-04
37242|Ferres Creek Tonalite|50163|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Caupaul Igneous Complex (Glenelg River Metamorphic Complex). Overlain by Duddo Limestone. Biotite-hornblende tonalite||||||20-AUG-04
37242|Ferres Creek Tonalite|50164|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Caupaul Igneous Complex. Biotite-hornblende tonalite.||||||
37242|Ferres Creek Tonalite|66002|5|Briefly described|p8 Tb.5|||Of Caupaul Igneous Complex. G423. Defined by Kemp et al. 2002||||||
37242|Ferres Creek Tonalite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Biotite-hornblende tonalite: foliated, grey, medium to coarse grained, equigranular; accessory quartz, microcline, magnetite and epidote; some samples contain clinopyroxene; magnetic.|
30510|Fiddlers Green Granodiorite|23309|6|Mentioned|p431 App 1|||||||||
30510|Fiddlers Green Granodiorite|68116|5|Briefly described|Appendix, Map 37.|Early Devonian|Early Devonian||||||Biotite - minor hornblende granite: pale grey to pink, coarse grained, massive to mylonitic; prominent quartz grains; I-type.|
34431|Fiery Creek Granite|22756|6|Mentioned|Table4 p116|||||||||09-JUN-15
6691|Fishermens Bend Silt|23237|5|Briefly described|p103|||||||||
6691|Fishermens Bend Silt|24551|5|Briefly described|p338 Fig. 11.2, 346|Middle Pleistocene|Early Pleistocene|||||||
6691|Fishermens Bend Silt|29982|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
6691|Fishermens Bend Silt|30986|5|Briefly described|p197|||See also P198,201||||||
6691|Fishermens Bend Silt|31009|6|Mentioned|M3|||||||||
6691|Fishermens Bend Silt|33604|5|Briefly described|p25|||||||||
6691|Fishermens Bend Silt|35011|3|Fully described|p311|||||||||
6691|Fishermens Bend Silt|41848|4|Described|p389|||||||||
6691|Fishermens Bend Silt|42827|4|Described|p389|||of Yarra Delta Group||||||
6691|Fishermens Bend Silt|60083|5|Briefly described|Map legend|Recent|Pleistocene|Silty clay, sometimes fossiliferous; sands, minor gravel of the Yarra delta.||||||
6691|Fishermens Bend Silt|71277|5|Briefly described|p304-306, p308|||Appears also as Fishermans Bend Silt (p301-303, p307 Fig.6, p308-309, p316). Eroded by river processes; distribution is quite variable. Up to 10m thick. Non-fossiliferous. Age from interbedded Burnley Basalt in upper parts.|c. 0.93-0.82 Ma.|||Interbedded with the Burnley and Swan Street Basalts.|Yellow, brown and grey stiff clays; some sandy lenses and calcareous nodules.|
6694|Fishing Point Marl|23768|5|Briefly described|p28 Fig.5, p103|Middle Miocene|Early Miocene|In Browns Creek area.||||||29-MAR-05
6694|Fishing Point Marl|24551|6|Mentioned|p305|||Equivalent to lower parts of Gellibrand Marl.||||||10-MAR-09
6694|Fishing Point Marl|30576|5|Briefly described|Table 2|||||||||
6694|Fishing Point Marl|30578|6|Mentioned|Table 1|||See also Table 2.||||||
6694|Fishing Point Marl|31922|6|Mentioned|Fig.2|||||||||
6694|Fishing Point Marl|33155|5|Briefly described|p121|||||||||
6694|Fishing Point Marl|35066|3|Fully described|p226|||||||||
6694|Fishing Point Marl|38070|6|Mentioned|Fig.12|||Otway Basin||||||
6694|Fishing Point Marl|41043|5|Briefly described|p102|||Mention p96.||||||03-SEP-18
6694|Fishing Point Marl|42318|5|Briefly described|p7|||||||||
6694|Fishing Point Marl|42827|4|Described|p300|||see also Fig 8.12||||||
6694|Fishing Point Marl|43590|6|Mentioned|p24|||Included in Gellibrand Marl||||||
6694|Fishing Point Marl|48911|6|Mentioned|Chart 1|||See also correlation P27||||||
6694|Fishing Point Marl|61155|5|Briefly described|p18|Late Miocene|Late Oligocene|Overlies Calder River Limestone. Age: 24.5-5.5Ma.  Max. thickness: 40m. Geological Province: Aire Embayment.||||||03-MAR-10
6694|Fishing Point Marl|61182|6|Mentioned|p28|||Of Thomas (1957) , Carter (1958) and Abele et al (1976). Now included in the Gellibrand Marl together with the informally named "Upper Glen Aire Clay, previously seen as part of Fishing Point Marl. ||||||
6694|Fishing Point Marl|62899|6|Mentioned|p48|||||||||
6694|Fishing Point Marl|63739|5|Briefly described|p48, p50|||Contains ostracod assemblages at Fishing Point.||||||01-JUL-08
6694|Fishing Point Marl|70942|4|Described|p124, 119|||||||||17-FEB-17
74889|Flagstone Creek Sandstone Member|64010|5|Briefly described|p258 Fig.1. |||||Of the Kevington Creek Formation.||||
74889|Flagstone Creek Sandstone Member|64536|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Of Kevington Creek Formation (Delatite Group). Sandstone, lesser siltstone: sandstone is medium- to coarse-grained, thick to very thick bedded, quartzarenite; siltstone is red. Fluvial deposits.||||||07-FEB-11
74889|Flagstone Creek Sandstone Member|64537|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Of Kevington Creek Formation (Delatite Group). Sandstone, lesser siltstone: sandstone is medium- to coarse-grained, thick to very thick bedded, quartzarenite; siltstone is red. Fluvial deposits.||||||07-FEB-11
74889|Flagstone Creek Sandstone Member|64538|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Of Kevington Creek Formation (Delatite Group). Sandstone, lesser siltstone: sandstone is medium- to coarse-grained, thick to very thick bedded, quartzarenite; siltstone is red. Fluvial deposits.||||||07-FEB-11
74889|Flagstone Creek Sandstone Member|64606|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Of Kevington Creek Formation. Sandstone, lesser siltstone: alluvial deposits. Black or dark brown in RGB. Nonmagnetic.||||||12-NOV-08
74889|Flagstone Creek Sandstone Member|64616|4|Described|p134, p189, p301|Givetian|Givetian|New. Sandstone unit at top of Kevington Creek Formation in Jamieson Syncline. A few hundred metres thick. Medium- to coarse-grained, thick-bedded quartz arenite sandstone; lesser red siltstone. Geophysical characteristics given.||||||
6733|Flaxman Formation|12781|6|Mentioned|p386|Late Cretaceous|Late Cretaceous|Otway Basin. Maximum thickness 620m.||Sherbrook Group.||Unconformably overlies Waarre Formation. Abuts Timboon Sandstone and Belfast Mudstone. Is overlain by Paaratte Formation.||
6733|Flaxman Formation|12796|4|Described|p457, p456 Fig. 2|Turonian|Turonian|Of the Sherbrook Group. Formerly "Flaxman Beds" (Bain 1961). Includes the Banoon Member. Overlain by Belfast Mudstone. Geological Province: Otway Basin.||||||30-JAN-08
6733|Flaxman Formation|22470|5|Briefly described|p13 Fig. 17|Turonian|Turonian|Of Sherbrook Group.||||||
6733|Flaxman Formation|22674|5|Briefly described|Fig.2 p719|Coniacian|Cenomanian|||||||
6733|Flaxman Formation|22875|3|Fully described|p38|Cenomanian|Cenomanian|Of the Sherbrook Group.||||||07-MAR-07
6733|Flaxman Formation|22932|6|Mentioned|22|||||||||
6733|Flaxman Formation|23818|5|Briefly described|p164|Late Cretaceous|Late Cretaceous|Overlain by Belfast Formation. Underlain by Waarre Formation. Geological Province: Otway Basin.||||||08-MAY-07
6733|Flaxman Formation|24056|5|Briefly described|p85|Late Cretaceous|Late Cretaceous|Of Sherbrook Group.  Geological Basin: Otway Basin.||||||
6733|Flaxman Formation|24284|6|Mentioned|p15 Fig.2|||Otway Basin.||||||02-DEC-04
6733|Flaxman Formation|24314|5|Briefly described|p61 Fig.2|Turonian||Geological Province: Otway Basin. Of the Sherbrook Group.||||||
6733|Flaxman Formation|24453|5|Briefly described|p809 Fig.2|Santonian|Coniacin|Of Sherbrook Group. Overlain by Belfast Mudstone, overlies Waare Formation. Geological Province: Otway Basin.||||||07-FEB-11
6733|Flaxman Formation|24551|6|Mentioned|p245|||Of the Sherbrook Group||||||
6733|Flaxman Formation|30576|5|Briefly described|Table 2|||||||||
6733|Flaxman Formation|30578|5|Briefly described|p7|||||||||
6733|Flaxman Formation|30580|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|||||||
6733|Flaxman Formation|30675|5|Briefly described|p253|||Lithology and radioactivity.||||||08-MAY-07
6733|Flaxman Formation|30905|6|Mentioned|Table 7.3|||||||||
6733|Flaxman Formation|30932|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|Part of Wangerrip Group.||||||08-MAY-07
6733|Flaxman Formation|31036|1|Redefined|p200|early Tertiary|early Tertiary|See also p200, Table 9-1. Refers Black and Glenie (1965).||||||07-MAR-07
6733|Flaxman Formation|31424|4|Described|p19|||See also p7. Described from core.||||||07-MAR-07
6733|Flaxman Formation|32896|6|Mentioned|Encl.7.1.|||Upper Cretaceous.||||||08-MAY-07
6733|Flaxman Formation|33936|6|Mentioned|Fig.6|||||||||
6733|Flaxman Formation|34611|5|Briefly described|p164|||Upper Cretaceous||||||
6733|Flaxman Formation|34987|4|Described|p170|||||||||
6733|Flaxman Formation|35722|6|Mentioned|p3|||Stratigraphy.||||||
6733|Flaxman Formation|36913|6|Mentioned|p81|||||||||
6733|Flaxman Formation|40947|6|Mentioned|p4|||||||||
6733|Flaxman Formation|41016|5|Briefly described|p214|||||||||
6733|Flaxman Formation|41269|5|Briefly described|p245|||||||||
6733|Flaxman Formation|41642|4|Described|p244|||||||||
6733|Flaxman Formation|41701|6|Mentioned|Map legend|Cretaceous||||||||
6733|Flaxman Formation|41704|6|Mentioned|Fig.3|||||||||
6733|Flaxman Formation|41769|5|Briefly described|p12|||||||||
6733|Flaxman Formation|41868|6|Mentioned|p533|||||||||
6733|Flaxman Formation|42152|6|Mentioned|p13|||||||||
6733|Flaxman Formation|42318|6|Mentioned|Fig.2 P10|||||||||
6733|Flaxman Formation|42361|1|Redefined|p13|Cenomanian|late Albian|New type section proposed in Flaxmans 1, Victoria. Late Cretaceous (Late Albian to Cenomanian) age.||||||31-JAN-08
6733|Flaxman Formation|42524|5|Briefly described|Fig.3 P27|||||||||
6733|Flaxman Formation|42545|6|Mentioned|p19|||In the Otway Basin.||||||08-MAY-07
6733|Flaxman Formation|42555|5|Briefly described|p284|||||||||
6733|Flaxman Formation|42599|5|Briefly described|Fig.3 P614|||||||||
6733|Flaxman Formation|42827|4|Described|p244|||see also Table 7.12||||||
6733|Flaxman Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
6733|Flaxman Formation|43171|5|Briefly described|5-8|||Of Sherbrook Formation. Age: 85-90 Ma.||||||08-MAY-07
6733|Flaxman Formation|43195|5|Briefly described|Map Legend||Late Cretaceous|See also commentary on back of map. Of Sherbrook Group.||||||
6733|Flaxman Formation|43208|5|Briefly described|map legend|Coniacian|Cenomanian|Of Sherbrook Group.||||||
6733|Flaxman Formation|43590|4|Described|p13|Santonian|Cenomanian|||||||
6733|Flaxman Formation|43733|6|Mentioned|Fig.2.11,p65||Late Cretaceous|||||||
6733|Flaxman Formation|43744|6|Mentioned|Fig.3,p3|||||||||
6733|Flaxman Formation|43783|6|Mentioned|Fig14, p11||Late Cretaceous|||||||
6733|Flaxman Formation|43784|6|Mentioned|Fig10, p12||Late Cretaceous|||||||
6733|Flaxman Formation|43814|6|Mentioned|Fig.3,p115|||||||||
6733|Flaxman Formation|43937|5|Briefly described|Map Legend|Santonian|Aptian|||||||
6733|Flaxman Formation|44133|5|Briefly described|p146|Santonian|Turonian|Of the Sherbrook Group. Geological Province: Otway Basin. Thickness: 619m.||||||
6733|Flaxman Formation|49060|5|Briefly described|Fig.33|||||||||
6733|Flaxman Formation|61016|6|Mentioned|p13|||Geological Province: Otway Basin.||||||20-APR-05
6733|Flaxman Formation|61017|5|Briefly described|p5 Fig. 2, p6|Coniacian|Turonian|Of the Sherbrook Group. Geological Province: Otway Basin. See also p6 Fig. 3.||||||07-FEB-11
6733|Flaxman Formation|61182|3|Fully described|p16, p160-161|Santonian|Cenomanian|Supersedes Flaxman Beds. Of Sherbrook Group. Conformably overlies Waarre Formation; conformably overlain by Belfast Mudstone. Geol.Prov: Otway Basin. Mudstone, siltstone, fine- to coarse-grained sandstone; ironstone, siderite, dolerite, thin coal present.||||||04-FEB-08
6733|Flaxman Formation|61230|5|Briefly described|p317, pp325-326, pp329-342.         |Late Turonian|Late Turonian|Of the Otway Delta. Delta front to prodelta conditions. TOC values vary from high to very high.||Unit in Sherbrook Group.||Overlies the Waarre Formation. Is overlain by Belfast Mudstone (Formation).|Dark grey mudstone with a significant (3 - 15%) sand fraction; glauconitic; granule-sized sand grains, mollusc debris and woody material occur occasionally in lower 100 m.|
6733|Flaxman Formation|61470|5|Briefly described|p28 Fig. 5|Coniacian|Turonian|Of the Sherbrook Group. Overlies Waarre Formation; underlies the Belfast Mudstone. Geological Province: Otway Basin.||||||12-OCT-05
6733|Flaxman Formation|61471|6|Mentioned|p34|||Geological Province: Otway Basin.||||||
6733|Flaxman Formation|61547|6|Mentioned|p461 Fig.2, p462. |Turonian|Turonian|||Unit in Sherbrook Group.||Overlies Waarre Sandstone. Is overlain by Belfast Mudstone.||
6733|Flaxman Formation|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
6733|Flaxman Formation|61623|6|Mentioned|p449 Fig. 4|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
6733|Flaxman Formation|61625|5|Briefly described|p476 Fig. 1, p477, p478 Fig. 3|Late Cretaceous|Late Cretaceous|Named Flaxman Fromation by Bock and Glenie (1965). Of Sherbrook Group. Geological Province: Otway Basin. Fine-grained grey-brown sandstone with occasional coarse sandstone interbeds.||||||07-FEB-11
6733|Flaxman Formation|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||31-MAR-09
6733|Flaxman Formation|61627|5|Briefly described|p500 Fig. 2|Late Cretaceous|Late Cretaceous|Of Shipwreck Subgroup. Geological Province: Otway Basin.||||||07-FEB-11
6733|Flaxman Formation|61628|5|Briefly described|p509 Fig. 3|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||31-MAR-09
6733|Flaxman Formation|63122|5|Briefly described|p17 Fig. 4.3|Santonian|Turonian|Of the Sherbrook Group. Max. thickness: 620m. Geological Province: Otway Basin. ||||||
6733|Flaxman Formation|63124|5|Briefly described|p48 Fig. 5.1, p49 Fig. 5.2, p80|||Earlier referred to as Flaxmans Formation (Reynolds et al 1966 and Wopfner et al (1971). Max. thickness: 620m. Geological Province: Otway Basin.||||||
6733|Flaxman Formation|63125|6|Mentioned|p121 Tb. 7.11|||Geological Province: Otway Basin||||||
6733|Flaxman Formation|63129|5|Briefly described|p137|||Geological Province: Otway Basin. Shales within this unit may act as regional seals.||||||30-JAN-08
6733|Flaxman Formation|63130|5|Briefly described|p143|||Geological Province: Otway Basin. Its reservoirs are sealed by Belfast Mudstone, or by intra-Parratte Formation shales. ||||||
6733|Flaxman Formation|63269|5|Briefly described|p605-607, p616, p618|Late Cretaceous|Late Cretaceous|Otway Basin. Details of natural gas, oils and oil stains in named wells tabulated. Oil-source correlation.||Sherbrook Group.||||
6733|Flaxman Formation|63431|5|Briefly described|p677 Fig. 2|Turonian|Turonian|Of the Sherbrook Group. Overlies Waarre Sandstone. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
6733|Flaxman Formation|66245|5|Briefly described|p6 Fig.5, p21 Fig.23, p68 Fig.D4.|Turonian|Turonian|||Unit in Sherbrook Group.||Overlies Waarre Formation.||
6733|Flaxman Formation|67061|6|Mentioned|p546 Fig.3.|Turonian|Turonian|||Unit in Sherbrook Group.||||
6733|Flaxman Formation|67366|5|Briefly described|p103 Fig.2. |Coniacian|Turonian|||Unit in Sherbrook Group.|Includes Banoon Member.|Overlies Waarre Formation. Is overlain by Belfast Formation.|Shelf to open marine shale.|
6733|Flaxman Formation|67367|5|Briefly described|p131 Fig.2. |Late Cretaceous|Late Cretaceous|Has potential as a viable hydrocarbon source rock.||Unit in Sherbrook Group.||||
6733|Flaxman Formation|69297|5|Briefly described|p78, p79, p83, p84, p98, p115|Turonian|Turonian|Otway and Sorell Basins. Deposited in marine, marginal marine or coastal plain environments. Shales may act as intraformational seals. Potential reservoir in the Sorell Basin.   ||Shipwreck Supersequence|Includes the Banoon Member|Overlies the Waarre Formation. Overlain by the Belfast Mudstone. |Siltstone and mudstone. |
6733|Flaxman Formation|69651|5|Briefly described|p10, p15, p31-34|Late Cretaceous|Late Cretaceous|Turonian. Marine, marginal marine and coastal plain sediments. Reservoirs sealed by Belfast Mudstone; shale units may act as intraformational seals.||Sherbrook Group.||Overlies Waarre Formation. Is overlain unconformably by Belfast Mudstone.|Includes shales.|
6733|Flaxman Formation|69879|5|Briefly described|p424|Turonian|Turonian|Otway Basin. Hydrocarbon reservoir in the Thylacine gas-condensate field. More deeply buried sediments are possibly hydrocarbon source.||||Overlies Waarre Formation.|Marine sandstone.|
6733|Flaxman Formation|70077|5|Briefly described|Nelson: Fig.2; p2. Regional: Fig.4; p5|Late Cretaceous|Late Cretaceous|See also Regional: p8, p10. Otway Basin. Distal equivalents in the Nelson Sub-basin may be important petroleum reservoirs, and shales provide intraformational seals.||Sherbrook Group.|Banoon Member.|Overlies Waarre Formation. Is overlain by Mount Salt Formation or Belfast Mudstone.||
6733|Flaxman Formation|70078|5|Briefly described|Northern:Fig.2; p2. Regional:Fig.4; p4-5|Coniacian|Turonian|Otway Basin. Equivalent sandstones in Sorell Basin are potential reservoirs.||Sherbrook Group.||Overlies Waarre Formation. Is overlain by Mount Salt Formation or Belfast Mudstone.||
6733|Flaxman Formation|70193|6|Mentioned|p284 Fig 2, p285 fig 3|Turonian|Turonian|Geological province: Otway Basin. Part of the Sherbrook Supersequence.|||Includes Banoon Member?|||
6733|Flaxman Formation|70880|6|Mentioned|p77|Turonian|Turonian|Otway Basin.||||||
6733|Flaxman Formation|71266|6|Mentioned|p614 Fig.3|Late Cretaceous|Late Cretaceous|Otway Basin.||||||
6733|Flaxman Formation|71437|4|Described|p157|Coniacian|Cenomanian|Previously Flaxman's Beds. Marine littoral to shallow neritic; minor paralic; lagoonal to tidal flat.||Of Wangerrip Group.||Overlies Waarre Sandstone. Sharp or transitional contact with overlying Belfast Mudstone Member. |Glauconitic and limonitic sandstone, minor siderite.|
6733|Flaxman Formation|73357|5|Briefly described|p20, p31, p45, p47|Coniacian|Turonian|Otway Basin. Correlated with Phyllocladidites mawsonii Spore-Pollen Zone, and Palaeohystrichophora infusorioides Dinocyst Zone marking a marine transgression with marginal to shallow marine facies.||Of Sherbrook Group.||Overlies Waarre Formation, underlies Belfast Mudstone.||
6733|Flaxman Formation|73383|5|Briefly described|vi, p3, p11 Tb.3.9, p134-135, p262|Coniacian|Turonian|Otway Basin. Possibly equivalent to the mudstone-dominant chemostratigraphic package S5-P3, only identified in the Penryn-1 well in this study.||Sherbrook Group||Overlies Waarre Formation, underlies Belfast Mudstone.|Shallow marine and nearshore sandstones. Mudstone and shale based on geochemistry.|
6733|Flaxman Formation|73385|5|Briefly described|p5|Coniacian|Turonian|Otway Basin.||Sherbrook Group||Overlies Waare Formation, underlies Belfast Mudstone.|Shallow marine and nearshore sandstones.|
6733|Flaxman Formation|73386|4|Described|p4, p6, p10-11, Attachment A1|Coniacian|Turonian|Otway Basin. Deposited in a lower delta plain environment, considered as the first marine transgressive unit in the Sherbrook Group. Type section defined between 2340 m and 2483 m in Port Campbell-2 (Partridge, 2001). Occurs within Phyllocladidites mawsonii Spore-Pollen Zone. Onshore, predominantly restricted to the Port Campbell and Tyrendarra embayments. Originally termed Flaxman Beds, also termed Waarre Formation unit D.||Sherbrook Group||Conformably overlies Waarre Formation, conformably underlies Belfast Mudstone|Interbedded sand/shale unit containing dark grey silty mudstones and fine grained grey brown sandstones, with distinctive coarse sand to pebble-sized 'floating quartz'.|
6733|Flaxman Formation|73594|5|Briefly described|p4-5, p15-16, p25-28, p31-32|Coniacian|Turonian|Otway Basin. Very heterogeneous. Marks a widespread marine transgression. Intersection of the unit in Port Campbell-2 well designated as the type section (BMR, 1964). Banoon Member (Partridge, 2001) may be present at the top of the unit, reliable marker of boundary with the Belfast Mudstone. Unit is absent at the crest of some elevated fault blocks in the Port Campbell Embayment.||Sherbrook Group||Overlies Waarre Formation, underlies Belfast Mudstone, Nullawarre Greensand. Unconformably underlies Thylacine Member|Upward-fining sequence of interbedded silty mudstones and fine-grained sandstones including pebbly mudstones at base, glauconitic and sideritic shales and siltstones.|
35577|Flinders Island Granite|23266|6|Mentioned|p365|||||||||
35577|Flinders Island Granite|61216|6|Mentioned|Fig.12 p34-35|Devonian|Devonian|||||||10-FEB-11
6758|Flinders Limestone|23768|6|Mentioned|p71|Batesfordian|Batesfordian|||||||
6758|Flinders Limestone|33237|6|Mentioned|p55|||||||||
6758|Flinders Limestone|33458|6|Mentioned|p18|||||||||
6758|Flinders Limestone|33462|6|Mentioned|p10|||Strat.table.||||||
6758|Flinders Limestone|33464|6|Mentioned|p7|||||||||
6758|Flinders Limestone|34421|6|Mentioned|p262|||||||||
6758|Flinders Limestone|41274|6|Mentioned|p9|||||||||
6758|Flinders Limestone|42824|5|Briefly described|p262|||||||||
6758|Flinders Limestone|66244|6|Mentioned|p5.|||||||||
24985|Flounder Formation|13323|5|Briefly described|p393 Fig. 2|Middle Eocene|Early Eocene|Of the Halibut Subgroup (Latrobe Group). Geological Province: Gippsland Basin.||||||26-JUN-06
24985|Flounder Formation|13332|5|Briefly described|p187 Fig.7|||Geological Province: Gippsland Basin.||||||
24985|Flounder Formation|23230|4|Described|Table4-1p40, 44||Eocene|||||||
24985|Flounder Formation|24054|5|Briefly described|p46|Eocene|Eocene|Of Latrobe Group.  Geological Basin: Gippsland Basin.||||||
24985|Flounder Formation|24551|5|Briefly described|p262 Fig. 9.29|Eocene|Eocene|Of the Halibut Subgroup.||||||
24985|Flounder Formation|29355|6|Mentioned|p190|||||||||
24985|Flounder Formation|29721|6|Mentioned|p192|||||||||
24985|Flounder Formation|29736|6|Mentioned|Fig.2|||||||||
24985|Flounder Formation|29974|6|Mentioned|p48|||||||||
24985|Flounder Formation|31480|4|Described|Fig. 3|||Middle Eocene||||||
24985|Flounder Formation|32162|6|Mentioned|p111|||||||||
24985|Flounder Formation|32574|6|Mentioned|p73|||See also P75||||||
24985|Flounder Formation|33320|6|Mentioned|p57|||Eocene||||||
24985|Flounder Formation|33362|6|Mentioned|p111|||||||||
24985|Flounder Formation|35013|6|Mentioned|p396|||||||||
24985|Flounder Formation|35067|6|Mentioned|Fig.3|||||||||
24985|Flounder Formation|35273|4|Described|p268|||||||||
24985|Flounder Formation|35573|6|Mentioned|Fig.3|||Chronostratigraphic section - Gippsland Basin||||||
24985|Flounder Formation|36643|6|Mentioned|Fig.7|||||||||
24985|Flounder Formation|38929|6|Mentioned|p45|||||||||
24985|Flounder Formation|41193|4|Described|p315|||||||||
24985|Flounder Formation|41282|6|Mentioned|Fig.4|||||||||
24985|Flounder Formation|41534|5|Briefly described|p86|||||||||
24985|Flounder Formation|41868|6|Mentioned|p521|||||||||
24985|Flounder Formation|42827|4|Described|p343|||Of Latrobe Valley Group.||||||12-FEB-08
24985|Flounder Formation|43145|5|Briefly described|p10||Eocene|Of Latrobe Group. Age is Early Eocene.||||||
24985|Flounder Formation|60538|5|Briefly described|p475 Fig. 14|Middle Eocene|Early Eocene|Geological Province: Gippsland Basin.||||||
24985|Flounder Formation|61155|5|Briefly described|p2, p18|Middle Eocene|Early Eocene|Locally derived prograding estuarine sediments - fine marine clastics. Thickness: 500m. Geological Province: Gippsland Basin (offshore channel sequences).||||||
24985|Flounder Formation|61212|5|Briefly described|p301 Fig. 2|Middle Eocene|Early Eocene|Geological Province: Gippsland Basin.||||||
24985|Flounder Formation|61323|6|Mentioned|p3 Fig. 3|||Geological Province: Gippsland Basin.||||||
24985|Flounder Formation|61328|5|Briefly described|p112 Fig. 2|Eocene|Eocene|Geological Province: Gippsland Basin.||||||12-FEB-08
24985|Flounder Formation|61336|5|Briefly described|p(iv) Fig. 4|Late Eocene|Early Eocene|Of Cobia Group. Geological Province: Gippsland Basin.||||||07-FEB-11
24985|Flounder Formation|61552|5|Briefly described|p583 Fig.2, p588 Fig.5, p592, p595. |Early Eocene|Early Eocene|Marine sediments partly infilling major channels which were eroded, during the Early Eocene, into the shelf, shoreface and coaly coastal plain successions.||Unit in Halibut Subgroup.||Is overlain by Gurnard Formation.||
24985|Flounder Formation|64876|5|Briefly described|p145 Fig.2|Eocene|Eocene|Gippsland Basin.||Halibut Subgroup.||||
24985|Flounder Formation|65717|6|Mentioned|p9 Fig.2.2, p11|Eocene|Eocene|Marine sediments filling in submarine channels carved during the early Eocene.||Halibut Subgroup||Unconformably overlies Mackerel Formation.||05-SEP-17
24985|Flounder Formation|65973|4|Described|p16, p22, p43, p57, p62, p65|||Gippsland Basin. Deposited in a marine environment. Intersected in Manta-1 , Kipper-1 , Kipper-2, Judith-1, East Pilchard-1 , Shark-1 and many more drillholes (see appendix). Palynology is discussed. Hosts small petroleum accumulation in the P. asperopolus palynological zone. See also p71, p74, p78, p82, p85-87, p90, p106, p108, p118, p123-124, p126-127, p129-131, p133, p135, p138-139, p144, p171.|||||Hosts coal.|
24985|Flounder Formation|67727|5|Briefly described|p58 Fig.2.|Middle Eocene|Lower Eocene|Offshore Gippsland Basin. Marginal marine infill of the Flounder Channel.||||Overlies Latrobe Group.||
24985|Flounder Formation|70028|6|Mentioned|p79|Eocene|Eocene|Offshore Gippsland Basin.||||||
24985|Flounder Formation|70076|5|Briefly described|South-Eastern: Fig.2; Regional: Fig.3|Ypresian|Ypresian|||Halibut Subgroup.||Overlies Mackerel or Kingfish Formation. Is overlain by Turrum, Opah or Gurnard Formation.||
24985|Flounder Formation|73562|6|Mentioned|p303-304, 312|Eocene|Eocene|Hocking (1972). Gippsland Basin; offshore. Filled in the Tuna channel (a submarine canyon) incised into the Latrobe Group.||Latrobe Group.|||Fine-grained marine sediments.|
24985|Flounder Formation|73640|6|Mentioned|p3 Fig.2|Eocene|Eocene|Gippsland Basin; offshore.||Latrobe Group||||
24985|Flounder Formation|75065|5|Briefly described|p151, 168|Eocene|Eocene|Gippsland Basin; offshore. Transgressive sediments filled in submarine canyons (formerly river valleys).||Halibut Subgroup.||Overlies Mackerel Formation. Is overlain unconformably by Gurnard and Turrum Formations (Cobia Subgroup).|Shallow-marine mudstones and glauconitic sandstones.|
6778|Flowerdale Granodiorite|22882|5|Briefly described|p 13|||||||||
6778|Flowerdale Granodiorite|22885|5|Briefly described|map|||||||||
6778|Flowerdale Granodiorite|22886|4|Described|Table.1|||||||||
6778|Flowerdale Granodiorite|23309|6|Mentioned|p431 App 1|||G220. S-Type. Supersedes Flowerdale Granite.||||||06-NOV-08
6778|Flowerdale Granodiorite|24551|6|Mentioned|p222|||||||||
6778|Flowerdale Granodiorite|44197|5|Briefly described|Map Legend||Late Devonian|G220 Unassigned.||||||
6778|Flowerdale Granodiorite|45087|5|Briefly described|p38|||Chemical analyses||||||
6778|Flowerdale Granodiorite|68116|5|Briefly described|Appendix, Map 33.|Late Devonian|Late Devonian||||||Biotite-muscovite granodiorite: fine-grained, grey; consists of quartz, andesine-oligoclase, orthoclase, dark brown biotite, muscovite and ilmenite.|
6779|Flowerdale Member|23229|5|Briefly described|Table3-3p26, 31|Lochkovian|Lochkovian|||||||
6779|Flowerdale Member|24177|5|Briefly described|p50 Fig.22|Early Devonian|Early Devonian|Of the Humevale Siltstone. Geological Province: Darraweit Guim Province.||||||27-OCT-08
6779|Flowerdale Member|33326|6|Mentioned|p440|||Fauna.||||||
6779|Flowerdale Member|33599|6|Mentioned|p4|||Refers Williams (1965).||||||
6779|Flowerdale Member|33732|5|Briefly described|p105|||||||||
6779|Flowerdale Member|35283|6|Mentioned|p51|||||||||
6779|Flowerdale Member|41585|6|Mentioned|p111|||||||||
6779|Flowerdale Member|43547|14|Not recorded|Table p152||Gedinnian|Part of Humevale Formation.||||||27-OCT-08
6779|Flowerdale Member|60599|5|Briefly described|p47 Fig. 19|Lochkovian|Lochkovian|Of Humevale Siltstone. Abbreviated version of Flowerdale Sandstone Member. Geological Province: Darraweit Guim Province, Melbourne Zone, Lachlan Fold Belt.||||||
6779|Flowerdale Member|61185|5|Briefly described|p21 Fig. 6, p24-25 Fig. 7|||Of Williams (1964) then revised to Flowerdale Sandstone Member by Garratt (1986) as part of Humevale Siltstone; now an obsolete name. Geological Province: LFB, Melbourne Zone. See also Flowerdale Sandstone Member.||||||07-FEB-11
6779|Flowerdale Member|66244|5|Briefly described|p3.|||Flowerdale area. Shown on the Kinglake 1:63 360 sheet (Garratt 1977); it is (equivalent to) the Broadford Formation.||||||
6779|Flowerdale Member|70487|6|Mentioned|p10, p12|Lochkovian|Ludlow|Orthids, strophomenids and gastropods predominate, but there are also tabulate corals and calymenid trilobite fragments. Some corals resemble those in Mount Ida Formation.  Mapped in the Broadford Formation.||Broadford Formation|||Includes fossiliferous siltstone. Previously said to include boulder conglomerate.|
37552|Fluke Knob Ignimbrite|23309|4|Described|p111 table 2.40|||Of Tara Range Subgroup.  Maximum Thickness: 650m.||||||22-FEB-10
37552|Fluke Knob Ignimbrite|60542|3|Fully described|p71|Early Devonian|Early Devonian|Of Mount Tara Subgroup. Formerly mapped into Mount Johnson Member. Red quartz ignimbrites, volcaniclastics, interbedded fluvial sediments. Overlies Windarra Formation; underlies Johnson Mudstone. Max. thickness: 650m.||||||
37552|Fluke Knob Ignimbrite|68116|5|Briefly described|Appendix, Map 45.|Pragian|Lochkovian||||||Quartz ignimbrite: crystal-rich, medium to coarse-grained, red, generally densely welded and with well-developed eutaxitic foliation; roundstone conglomerate, pebbly sandstone, sandstone; fluvial and pyroclastic deposits.|
35593|Footscray Basalt|23275|5|Briefly described|p468|||||||||
35593|Footscray Basalt|68576|6|Mentioned|QLD_D1: p10|||Used in St. John's Cathedral, Brisbane.||||||
38695|Forest Creek Ignimbrite|23615|5|Briefly described|p223 App 2|||Coarse grained quartz-feldspar ignimbrite with grey-green fine-grained groundmass set with large crystals of quartz and less abundant feldspar.||||||
6824|Forlorn Hope Granite|22968|4|Described|P50, P174||Silurian|Intruded the Pinnak Sandstone, parent is Bullenbalong Supersuite.||||||04-NOV-14
6824|Forlorn Hope Granite|23021|5|Briefly described|Map legend|Wenlock|Wenlock|Parent is Bullenbalong Suite||||||
6824|Forlorn Hope Granite|23030|5|Briefly described|Map legend|Silurian|Silurian|Parent is the Bullenbalong Supersuite||||||
6824|Forlorn Hope Granite|23309|6|Mentioned|p431 App1|||G122 S-Type.||||||
6824|Forlorn Hope Granite|23615|4|Described|p72-73, p157|||Name used interchangeably with Forlorn Hope Granodiorite in this report.  Possibly part of Bullenbalong Suite but not geochemically confirmed.  Intrudes Towanga Formation.||||||
6824|Forlorn Hope Granite|24275|6|Mentioned|p1696 Fig. 2|||Geological Province: Lachlan Fold Belt.||||||
6824|Forlorn Hope Granite|24551|6|Mentioned|p234|||||||||
6824|Forlorn Hope Granite|39447|4|Described|p18|||||||||
6824|Forlorn Hope Granite|41585|6|Mentioned|p127|||||||||
6824|Forlorn Hope Granite|42726|5|Briefly described|map legend|Silurian||378.Kosciusco Batholith.||||||
6824|Forlorn Hope Granite|42827|6|Mentioned|p127|||||||||
6824|Forlorn Hope Granite|43206|5|Briefly described|map legend||Wenlock|||||||
6824|Forlorn Hope Granite|43220|6|Mentioned|p10||Silurian|||||||
6824|Forlorn Hope Granite|44184|5|Briefly described|Map Legend||Early Silurian|||||||
6824|Forlorn Hope Granite|44185|5|Briefly described|Map legend.|Silurian|Silurian|S-type.||||||
6824|Forlorn Hope Granite|60503|6|Mentioned|p64|||Intrusives in the Limestone Creek Graben.||||||07-SEP-05
6824|Forlorn Hope Granite|68116|5|Briefly described|Appendix, Maps 28, 35-36.|Wenlock|Llandovery||||||Granite: grey, fine to medium-grained; rare diorite. Contains leucogranite zones along northwestem margin and abundant aplite dykes in some places.|
35646|Forty Foot Sandstone|23109|6|Mentioned|p512 Fig.3|||||||||
6895|Freeman Sandstone Member|35283|6|Mentioned|p53|||||||||
6900|French Park Granite|42726|5|Briefly described|map legend|||||||||
6900|French Park Granite|71889|6|Mentioned|p35, p37|||Trigg (2017) suggests this may be a part of the Collingullie Granite. Originally delineated by Chappell et al (1991) in the eastern part of LOCKHEART.||||||
21818|Frying Pan Creek Ignimbrite|23309|4|Described|p108.  Table 2.40|||Maximum Thickness: 200m.  Of the Little River Subgroup.||||||
21818|Frying Pan Creek Ignimbrite|23615|3|Fully described|p28-29, p128|Early Devonian|Early Devonian|Of Little River Subgroup.  Unconformably underlies Buchan Group.||||||
21818|Frying Pan Creek Ignimbrite|24551|5|Briefly described|p145|||Of Little River Subgroup.||||||
21818|Frying Pan Creek Ignimbrite|43206|5|Briefly described|map legend||Lochkovian|of Little River Subgroup.||||||
21818|Frying Pan Creek Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Feldspar ignimbrite with pink vitric matrix, minor quartz phenocrysts.|
76929|Fumina Basalt|66244|4|Described|p6.|Miocene|Miocene|New name. Flow remnants extending from the Tynong Granite through the Fumina area and down to La Trobe Valley near Willow Grove and Tanjil South. Part of the Neerim Province of Wellman (1974). The boundaries with Thorpdale and Neerim Volcanic Groups are arbitrary.|19 Ma (Wellman 1974).||||Olivine tholeiite, alkali olivine basalt, K-hawaiite; minor nepheline basalt, basanite and nepheline hawaiite.|
76929|Fumina Basalt|68116|5|Briefly described|Appendix, Maps 43, 52.|Burdigalian|Burdigalian||||||Basalt flows: olivine tholeiite, alkali olivine basalt, K-hawaiite, minor nepheline basalt, basanite and nepheline hawaiite.|
77119|Furneaux Sequence|61553|5|Briefly described|p605 Fig.4, p608, p609. |Late Maastrichtian|Late Campanian|Deposited in fluvio-deltaic, lacustrine, coastal plain and peat mires environments.||Unit in Bass Megasequence.||Is overlain by Tilana Sequence.|Fluvio-deltaic sandstones interbedded with (a) freshwater lacustrine shales or (b) thin overbank or delta plain shales and coals.|
77119|Furneaux Sequence|69879|4|Described|p431-433|Maastrichtian|Campanian|Extends across entire Bass Basin; is deeply buried in the Basin centre. Fossil controls. Appears also as Furneaux Group on p433.||Bass Megasequence||Overlies Durroon Megasequence unconformably. Underlies Tilana Sequence unconformably. Equivalent to Middle Eastern View Coal Measures.|Non-marine fining-up interbedded sandstone, silstone and shale with minor coal, deposited in a fluvio-deltaic and lacustrine environment.|
6946|Gabo Island Granite|22857|5|Briefly described|p215|||Of the Boyd Volcanic Complex. Age: 363Ma (K/Ar, Thomson 1974a). Geological Province: Lambie Basin.||||||
6946|Gabo Island Granite|22859|5|Briefly described|p215||Late Devonian|Max Age: 363 Ma.||||||
6946|Gabo Island Granite|23275|5|Briefly described|p473||Early Devonian|||||||
6946|Gabo Island Granite|23309|5|Briefly described|p348|Early Carboniferous|Late Devonian|G1 - A-Type. Age: 356 +/- 12 Ma.||||||
6946|Gabo Island Granite|23456|5|Briefly described|p50 Fig.1|Late Devonian|Late Devonian|||||||
6946|Gabo Island Granite|24551|6|Mentioned|p236|||||||||
6946|Gabo Island Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
6946|Gabo Island Granite|29994|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
6946|Gabo Island Granite|30574|5|Briefly described|p11|||||||||
6946|Gabo Island Granite|30938|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
6946|Gabo Island Granite|32127|6|Mentioned|p253|||||||||
6946|Gabo Island Granite|33480|6|Mentioned|p244|||Age dating||||||
6946|Gabo Island Granite|33602|6|Mentioned|p36|||See also Fig.2||||||
6946|Gabo Island Granite|33732|6|Mentioned|p111|||||||||
6946|Gabo Island Granite|34109|6|Mentioned|p156|||||||||
6946|Gabo Island Granite|34400|6|Mentioned|p8|||||||||
6946|Gabo Island Granite|34403|6|Mentioned|p129|||||||||
6946|Gabo Island Granite|34404|6|Mentioned|p88|||||||||
6946|Gabo Island Granite|34406|6|Mentioned|p224|||Intrudes Eden Rhyolite||||||
6946|Gabo Island Granite|34519|6|Mentioned|p45|||||||||
6946|Gabo Island Granite|34893|6|Mentioned|p33|||||||||
6946|Gabo Island Granite|34989|6|Mentioned|p80|||||||||
6946|Gabo Island Granite|35112|6|Mentioned|Fig.8|||See also P288.||||||
6946|Gabo Island Granite|35278|6|Mentioned|p359|||||||||
6946|Gabo Island Granite|35526|5|Briefly described|p92|||One of the facies in the Boyd Volcanic Complex||||||
6946|Gabo Island Granite|37501|6|Mentioned|p414|||||||||
6946|Gabo Island Granite|38899|6|Mentioned|p71|||||||||
6946|Gabo Island Granite|39627|6|Mentioned|Appendix|||||||||
6946|Gabo Island Granite|39665|6|Mentioned|Fig.2|||||||||
6946|Gabo Island Granite|40276|6|Mentioned|p22|||||||||
6946|Gabo Island Granite|40328|4|Described|p205|||||||||
6946|Gabo Island Granite|40646|6|Mentioned|p24|||||||||
6946|Gabo Island Granite|41919|6|Mentioned|Fig.1|||||||||
6946|Gabo Island Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
6946|Gabo Island Granite|42827|6|Mentioned|p150|||Felsic, even-grained, brick-red colour; perthitic alkali feldspar dominated over plagioclase; khaki coloured ferrohastingsite and Fe-rich biotite; accessory magnetite, zoned zircon, allanite, apatite and secondary fluorite.||||||29-NOV-04
6946|Gabo Island Granite|46574|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Bega Batholith.  Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
6946|Gabo Island Granite|46579|14|Not recorded|p.104,106|||(J55-4/Pambula; J55-8/Eden).||||||
6946|Gabo Island Granite|61186|6|Mentioned|p56|||Attractive red building stone used in the city of Melbourne; rich red colour and fine-grained. Two variants occur - one dark red and the other a paler red-pink colour. The dominant feldspar is red and the minor feldspar is green. ||||||
6946|Gabo Island Granite|63605|6|Mentioned|p991|||Located south of Eden (NSW).||||||07-FEB-11
6946|Gabo Island Granite|64769|6|Mentioned|p27|||VIC.||||||06-MAY-09
6946|Gabo Island Granite|68116|5|Briefly described|Appendix, Map 46.|Late Devonian|Late Devonian||||||Biotite-hornblende granite: medium to fine grained; pink; accessory allanite, magnetite, fayalite, stilpnomelane and fluorite; hornblende is hastingsite variety; A-type.|
6946|Gabo Island Granite|68298|5|Briefly described|p233|||Age: 363+/-12 Ma K/Ar (D. Wyborn, pers. comm.), 395+/-4 Ma (95%CI, Williams, in press).SHRIMP? Age is too old to help constrain overlying Boyd Volcanic Complex fish fauna ages. 'Watergum Granite', No. 1 of B.W. Chappell.|395+/-4 Ma (Williams, in press) [U/Pb SHRIMP?]|||Nonconformably overlain by Boyd Volcanic Complex||
6946|Gabo Island Granite|71206|6|Mentioned|p373, 384|||Lachlan Fold Belt. Geochemistry graphs.||Gabo Suite.|||Aluminous A-type granite.|
6947|Gabo Suite|22815|4|Described|p95|Late Devonian|Late Devonian|K/Ar Age: 356+/-12 Ma.||||||
6947|Gabo Suite|23309|5|Briefly described|p317, 348|Early Carboniferous|Late Devonian|Gabo Island and Howe Range Granites.||||||
6947|Gabo Suite|23550|5|Briefly described|p511|||||||||
6947|Gabo Suite|24222|6|Mentioned|p22|||See also Gabo suite.  Geological Province: Lachlan Fold Belt.||||||
6947|Gabo Suite|24551|6|Mentioned|p235, 236|||||||||
6947|Gabo Suite|42726|5|Briefly described|map legend||Middle Devonian|||||||
6947|Gabo Suite|42827|5|Briefly described|p428|||||||||
6947|Gabo Suite|43233|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|||||||
6947|Gabo Suite|44093|5|Briefly described|p222 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
6947|Gabo Suite|63605|5|Briefly described|p992 Fig. 1, p997|||Includes Gabo Island and Watergums Granites. Associated with the Boyd Volcanic Complex - intrusive relationship.||||||07-FEB-11
6947|Gabo Suite|67779|6|Mentioned|p66.|||Lachlan Fold Belt. A-type granites. Has remarkable chemical similarity with Tin Camp Granite, McArthur Basin.||||||
6947|Gabo Suite|67847|5|Briefly described|p60 fig 3.3.4|Middle Devonian|Middle Devonian|A-type intrusive rocks. ||||||
6947|Gabo Suite|70351|6|Mentioned|p55|||||||||
6947|Gabo Suite|70601|5|Briefly described|p31|Late Devonian|Middle Devonian|||||Intrudes Boyd Volcanic Complex.|A-type subvolcanic granites.|
6947|Gabo Suite|71206|6|Mentioned|p373, 375, 377, 379-382|||Presented as Gabo Island Suite. Geochemistry discussed.|||Watergums, Naghi, Nagha, Carlyle, Howe Range, Gabo Island, Granites.||Aluminous A-type granite.|
6947|Gabo Suite|73431|6|Mentioned|p374 Fig.8|||A-type granites.||||||
75950|Gallows Hill Phonolite|68115|5|Briefly described|p8, p9.|Jurassic|Jurassic|Forms a capping on Gallows Hill. Described by McDougall and Wellman (1976) as a possible plug, but its shape is also consistent with a flow or sill. Its age precludes it from being part of the (Paleogene) Older Volcanic Group, as shown on earlier maps.|||||Nepheline phonolite.|
75950|Gallows Hill Phonolite|68116|6|Mentioned|Appendix, Map 26.|Early Cretaceous|Jurassic||||||Phonolite.|
6976|Gambier Limestone|10010|5|Briefly described|p12 Fig. 3|Late Oligocene|Early Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||13-AUG-07
6976|Gambier Limestone|12781|6|Mentioned|p386|Miocene|Eocene|Otway Basin. Maximum thickness 400m.||Heytsbury Group.||Overlies Gellibrand Marl.||
6976|Gambier Limestone|22541|6|Mentioned|Fig 16|||||||||
6976|Gambier Limestone|22587|6|Mentioned|p79 Fig.7|Early Miocene|Late Eocene|||||||
6976|Gambier Limestone|22626|6|Mentioned|446 fig 10|Early Miocene|Late Oligocene|Geol province West Otway Basin. Overlying unit Heytesbury Group||||||
6976|Gambier Limestone|22773|5|Briefly described|Fig24.8p352+24.9p353|||||||||
6976|Gambier Limestone|22799|5|Briefly described|p23 Fig.7|Early Miocene|Oligocene|Glenelg Group||||||
6976|Gambier Limestone|22857|5|Briefly described|p352 Fig.24.8, p353 Fig. 24.9|Early Miocene|Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||
6976|Gambier Limestone|22887|5|Briefly described|Fig.6 p13||Late Oligocene|Of Murray Group, Murray Basin.||||||03-FEB-09
6976|Gambier Limestone|22893|5|Briefly described|fig4 p9|||||||||
6976|Gambier Limestone|22913|6|Mentioned|29|||||||||
6976|Gambier Limestone|22938|5|Briefly described|fig5|Oligocene|Oligocene|Eastern Mount Lofty Ranges.||||||
6976|Gambier Limestone|23249|5|Briefly described|Fig.2|||Informally divided into Upper/Middle and Lower Gambier Limestone.||||||
6976|Gambier Limestone|23322|4|Described|955, 957|Middle Miocene|Middle Eocene|Geological Province: Gambier Basin.||||||07-SEP-09
6976|Gambier Limestone|23671|6|Mentioned|p2|||Overlies the Compton Conglomerate; disconformably overlies the Burrungule Member.||||||16-AUG-04
6976|Gambier Limestone|23731|6|Mentioned|p20, p27|Miocene|Oligocene|||||||
6976|Gambier Limestone|23768|5|Briefly described|p28 Fig.5, p69|Miocene|Oligocene|Geological Province: Gambier Basin. See also p89, p154.||||||29-MAR-05
6976|Gambier Limestone|23818|5|Briefly described|p174 Fig.84, p177|Middle Miocene|Oligocene|Geological Province: Otway Basin. Max. thickness: 500 ft.||||||
6976|Gambier Limestone|23879|5|Briefly described|p19|||||||||
6976|Gambier Limestone|23884|5|Briefly described|p155 Fig. 13.2|Late Oligocene|Late Oligocene|Geological Province: Murray Basin. Of the Murray Group.||||||
6976|Gambier Limestone|24160|6|Mentioned|p18|Middle Miocene|Middle Miocene|Hosts a calcium bentonite deposit below weathered Newer Volcanics.||||Is overlain by Newer Volcanics.||
6976|Gambier Limestone|24202|5|Briefly described|p313 Fig.2|Middle Miocene|Early Oligocene|Geological Province: Gambier Sub-basin.  See also p314.||||||
6976|Gambier Limestone|24314|5|Briefly described|p61 Fig.2|Miocene|Eocene|Geological Province: Otway Basin. Max. Thickness 400m. Of the Heytesbury Group.||||||30-NOV-04
6976|Gambier Limestone|24363|5|Briefly described|p37|Early Miocene|Oligocene|max. thickness: 400 m. Age: 38-15 Ma.||||||
6976|Gambier Limestone|24410|6|Mentioned|p6|Late Oligocene|Early Miocene|||||||
6976|Gambier Limestone|24551|6|Mentioned|p296, 555, 625|||||||||
6976|Gambier Limestone|24562|5|Briefly described|p15 Fig. 4|Tertiary|Late Cretaceous|Geological Province: Otway Basin.||||||
6976|Gambier Limestone|29591|6|Mentioned|p90|||||||||
6976|Gambier Limestone|29654|6|Mentioned|p101|||||||||
6976|Gambier Limestone|29666|6|Mentioned|p22|||||||||
6976|Gambier Limestone|29697|6|Mentioned|p2|||||||||
6976|Gambier Limestone|29828|6|Mentioned|p25|||||||||
6976|Gambier Limestone|29866|6|Mentioned|p84|||||||||
6976|Gambier Limestone|29891|5|Briefly described|p77|||||||||
6976|Gambier Limestone|29892|6|Mentioned|p77|||||||||
6976|Gambier Limestone|29894|6|Mentioned|p27|||||||||
6976|Gambier Limestone|30179|6|Mentioned|p33|||Oligocene - Miocene age||||||
6976|Gambier Limestone|30184|6|Mentioned|p173|||||||||
6976|Gambier Limestone|30514|6|Mentioned|p108|||||||||
6976|Gambier Limestone|30520|6|Mentioned|p41|||Groundwater||||||
6976|Gambier Limestone|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
6976|Gambier Limestone|30751|6|Mentioned|Map legend|Oligocene|Eocene|Miocene-Eocene||||||
6976|Gambier Limestone|30753|4|Described|Table 2|||Middle Miocene to Upper Eocene age.||||||07-SEP-18
6976|Gambier Limestone|30754|5|Briefly described|p13|||Strat.tables p14,22. See also p20,24,28. Map, block diag.,section.||||||07-SEP-18
6976|Gambier Limestone|30807|6|Mentioned|p101|||Suggested map symbol||||||
6976|Gambier Limestone|30828|6|Mentioned|p113|||||||||
6976|Gambier Limestone|30917|6|Mentioned|p26|||||||||
6976|Gambier Limestone|30918|6|Mentioned|p85|||||||||
6976|Gambier Limestone|30932|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene to Miocene||||||
6976|Gambier Limestone|30996|6|Mentioned|Fig. 3|||||||||
6976|Gambier Limestone|31241|4|Described|p99|||See also P101. Equ. in age to Ettrick Fm.||||||
6976|Gambier Limestone|31245|6|Mentioned|p81|||||||||
6976|Gambier Limestone|31372|6|Mentioned|Fig. 2|||||||||
6976|Gambier Limestone|31424|6|Mentioned|Fig.2|||||||||
6976|Gambier Limestone|31515|6|Mentioned|p292|||||||||
6976|Gambier Limestone|31517|6|Mentioned|p1|||Fossil sites of decapods.||||||
6976|Gambier Limestone|31624|2|Defined|p96|Tertiary|Tertiary|||||||
6976|Gambier Limestone|31625|6|Mentioned|Fig. 5.2|||Oligocene- Miocene||||||
6976|Gambier Limestone|31629|6|Mentioned|Fig.5.2|||Miocene-Oligocene||||||
6976|Gambier Limestone|31746|6|Mentioned|p195|||||||||
6976|Gambier Limestone|31848|6|Mentioned|p15|||Refers Ludbrook (1969)||||||
6976|Gambier Limestone|31851|6|Mentioned|p10|||Also P15||||||
6976|Gambier Limestone|31920|4|Described|p59|||Oligocene. Sponge spicule mb. See also Figs 3-2,4.||||||
6976|Gambier Limestone|31922|6|Mentioned|Table 3|||||||||
6976|Gambier Limestone|31923|6|Mentioned|p16|||||||||
6976|Gambier Limestone|32116|4|Described|p45|||Oligocene. See also p46-47.||||||01-NOV-22
6976|Gambier Limestone|32344|6|Mentioned|p121|||||||||
6976|Gambier Limestone|32552|6|Mentioned|p184|||Longfordian||||||
6976|Gambier Limestone|32570|6|Mentioned|p6|||||||||
6976|Gambier Limestone|32601|6|Mentioned|p682|||||||||
6976|Gambier Limestone|32653|6|Mentioned|Table 1|||||||||
6976|Gambier Limestone|32841|6|Mentioned|p6|||||||||
6976|Gambier Limestone|32859|4|Described|p69|||L.Miocene||||||
6976|Gambier Limestone|32860|5|Briefly described|p91|||Lower Pliocene.||||||07-SEP-18
6976|Gambier Limestone|32894|6|Mentioned|p287|||Olig.-Miocene||||||
6976|Gambier Limestone|32895|6|Mentioned|p328|||Tertiary||||||
6976|Gambier Limestone|32897|6|Mentioned|Fig. 7-1|||||||||
6976|Gambier Limestone|32898|6|Mentioned|p27|||See also Table 2-1||||||
6976|Gambier Limestone|33109|6|Mentioned|p84|||Main aquifer system||||||
6976|Gambier Limestone|33236|6|Mentioned|p19|||Olig. - Miocene||||||
6976|Gambier Limestone|33490|4|Described|p10|||See also p27. Oligocene - Miocene.||||||07-SEP-18
6976|Gambier Limestone|33579|6|Mentioned|p52|||||||||
6976|Gambier Limestone|33712|6|Mentioned|p9|||See also Fig.1. Oligo. - Mioc. Refers Ludbrook (1961).||||||
6976|Gambier Limestone|33713|4|Described|p27|||See also p28.||||||07-SEP-18
6976|Gambier Limestone|33716|3|Fully described|p15|||See also pp16 & 20 & Table 2.||||||07-SEP-18
6976|Gambier Limestone|33798|6|Mentioned|p98|||Fig.2||||||
6976|Gambier Limestone|33940|6|Mentioned|p414|||||||||
6976|Gambier Limestone|33943|6|Mentioned|p379|||||||||
6976|Gambier Limestone|34180|6|Mentioned|p212|||Tertiary||||||
6976|Gambier Limestone|34185|6|Mentioned|p131|||Protected from marine erosion in Pliocene.||||||
6976|Gambier Limestone|34191|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene - Miocene||||||
6976|Gambier Limestone|34308|3|Fully described|p177|||Aldingian - Balcombian. Correlation chart||||||
6976|Gambier Limestone|34418|4|Described|p506|||||||||
6976|Gambier Limestone|34421|6|Mentioned|p261|||See also P262||||||
6976|Gambier Limestone|34524|5|Briefly described|p105|||||||||
6976|Gambier Limestone|34615|6|Mentioned|p3|||||||||
6976|Gambier Limestone|34658|5|Briefly described|p98|||||||||
6976|Gambier Limestone|34954|6|Mentioned|Fig.33|||Analysis.||||||
6976|Gambier Limestone|34958|6|Mentioned|p88|||||||||
6976|Gambier Limestone|34988|6|Mentioned|p294|||||||||
6976|Gambier Limestone|35018|5|Briefly described|p29|||||||||
6976|Gambier Limestone|35051|6|Mentioned|p203|||Analysis.||||||
6976|Gambier Limestone|35066|6|Mentioned|p210|||||||||
6976|Gambier Limestone|35097|6|Mentioned|Fig.4|||||||||
6976|Gambier Limestone|35147|6|Mentioned|p127|||||||||
6976|Gambier Limestone|35200|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
6976|Gambier Limestone|35232|6|Mentioned|p11|||||||||
6976|Gambier Limestone|36492|6|Mentioned|Fig.1|||||||||
6976|Gambier Limestone|37500|6|Mentioned|p385|||||||||
6976|Gambier Limestone|37548|6|Mentioned|p131|||||||||
6976|Gambier Limestone|38068|6|Mentioned|Fig.7|||||||||
6976|Gambier Limestone|38070|6|Mentioned|Fig.12|||Otway Basin||||||
6976|Gambier Limestone|38663|6|Mentioned|Fig.1|||||||||
6976|Gambier Limestone|38699|6|Mentioned|p8|||||||||
6976|Gambier Limestone|38826|6|Mentioned|Fig.1|||||||||
6976|Gambier Limestone|38903|5|Briefly described|Table 2|||||||||
6976|Gambier Limestone|38932|5|Briefly described|p98|||See also Fig.4.||||||07-SEP-18
6976|Gambier Limestone|39077|6|Mentioned|Table 2|||||||||
6976|Gambier Limestone|39329|6|Mentioned|Fig.1|||||||||
6976|Gambier Limestone|39408|6|Mentioned|Fig.2|||||||||
6976|Gambier Limestone|39923|6|Mentioned|p354|||||||||
6976|Gambier Limestone|39929|6|Mentioned|Fig.3|||||||||
6976|Gambier Limestone|40003|5|Briefly described|p44|||||||||
6976|Gambier Limestone|40032|6|Mentioned|p225|||||||||
6976|Gambier Limestone|40125|6|Mentioned|p353|||||||||
6976|Gambier Limestone|40230|6|Mentioned|p6|||||||||
6976|Gambier Limestone|40298|6|Mentioned|p432|||||||||
6976|Gambier Limestone|40429|6|Mentioned|Fig.2|||||||||
6976|Gambier Limestone|40521|6|Mentioned|p307|||||||||
6976|Gambier Limestone|40555|6|Mentioned|p51|||||||||
6976|Gambier Limestone|40556|6|Mentioned|p61|||||||||
6976|Gambier Limestone|40557|6|Mentioned|p169|||||||||
6976|Gambier Limestone|40560|6|Mentioned|p6|||||||||
6976|Gambier Limestone|40561|6|Mentioned|p8|||||||||
6976|Gambier Limestone|40829|5|Briefly described|p14|||||||||
6976|Gambier Limestone|40877|5|Briefly described|p55|||||||||
6976|Gambier Limestone|40947|6|Mentioned|p3|||||||||
6976|Gambier Limestone|40980|6|Mentioned|p335|||||||||
6976|Gambier Limestone|41076|6|Mentioned|p63|||||||||
6976|Gambier Limestone|41185|6|Mentioned|Fig.5|||||||||
6976|Gambier Limestone|41517|6|Mentioned|p138|||||||||
6976|Gambier Limestone|41518|6|Mentioned|p146|||||||||
6976|Gambier Limestone|41519|6|Mentioned|p172|||||||||
6976|Gambier Limestone|41520|5|Briefly described|Fig.12|||||||||
6976|Gambier Limestone|41578|6|Mentioned|p7|||||||||
6976|Gambier Limestone|41599|6|Mentioned|p191|||||||||
6976|Gambier Limestone|41626|6|Mentioned|p54|||||||||
6976|Gambier Limestone|42097|6|Mentioned|p40|||||||||
6976|Gambier Limestone|42125|5|Briefly described|p136|||||||||
6976|Gambier Limestone|42127|5|Briefly described|p223|||||||||
6976|Gambier Limestone|42130|6|Mentioned|Fig.3 P265|||||||||
6976|Gambier Limestone|42137|6|Mentioned|p370|||||||||
6976|Gambier Limestone|42335|5|Briefly described|p338|||||||||
6976|Gambier Limestone|42457|6|Mentioned|p170|||||||||
6976|Gambier Limestone|42594|5|Briefly described|p247|||Oligocene-Miocene||||||
6976|Gambier Limestone|42599|5|Briefly described|Fig.3 P614|||Cooper Basin.||||||07-SEP-18
6976|Gambier Limestone|42601|6|Mentioned|Fig.2 p15|||||||||
6976|Gambier Limestone|42717|6|Mentioned|map legend|Miocene|Oligocene|||||||
6976|Gambier Limestone|42827|6|Mentioned|p285|||||||||
6976|Gambier Limestone|42881|4|Described|Fig.3, p84|||||||||01-NOV-22
6976|Gambier Limestone|42966|2|Defined|Table 15, p126|Early Miocene|Late Oligocene|Of Murray Group, Murray Basin & Glenelg Group, Otway Basin.||||||03-FEB-09
6976|Gambier Limestone|43073|5|Briefly described|p11|||||||||
6976|Gambier Limestone|43171|6|Mentioned|5|||Of Heytesbury Group.||||||03-FEB-09
6976|Gambier Limestone|43195|5|Briefly described|Map Legend|Middle Miocene|Late Eocene|see also commentary on back of map. Of Heytesbury Group.||||||
6976|Gambier Limestone|43258|5|Briefly described|Map Legend|Miocene|Eocene|||||||
6976|Gambier Limestone|43298|5|Briefly described|Map Legend|Miocene|Eocene|||||||
6976|Gambier Limestone|43383|14|Not recorded|p29||Early Miocene|||||||
6976|Gambier Limestone|43466|14|Not recorded|p3,Pl.1|||Equivalent to SA||||||
6976|Gambier Limestone|43467|14|Not recorded|p3,20,31,32|||||||||
6976|Gambier Limestone|43660|6|Mentioned|Fig.7,p16|||||||||
6976|Gambier Limestone|43667|6|Mentioned|Fig.3,p12|Early Miocene|Early Oligocene|||||||
6976|Gambier Limestone|43686|6|Mentioned|Fig.5,p233|||||||||
6976|Gambier Limestone|43733|6|Mentioned|p30||Tertiary|||||||
6976|Gambier Limestone|43744|6|Mentioned|Fig.3,p3|||||||||
6976|Gambier Limestone|43791|6|Mentioned|p372, Fig1|||||||||
6976|Gambier Limestone|43797|5|Briefly described|p201|Miocene|Oligocene|||||||
6976|Gambier Limestone|43799|5|Briefly described|p185|||||||||
6976|Gambier Limestone|43804|6|Mentioned|Fig.2,p49|||||||||
6976|Gambier Limestone|43814|6|Mentioned|Fig.3,p115|||||||||
6976|Gambier Limestone|44133|4|Described|p156, 259, 268|Miocene|Miocene|Thickness: 400m. Of the Heytesbury Group. Geological Province: Gambier Basin. Includes: Greenways Member, Camelback Member, Green Point Member, Naracoorte Limestone Member.||||||
6976|Gambier Limestone|46802|6|Mentioned|Table 1|||||||||
6976|Gambier Limestone|46839|6|Mentioned|p81|||||||||
6976|Gambier Limestone|46899|6|Mentioned|p13|||Thermal conductivity||||||
6976|Gambier Limestone|46909|6|Mentioned|p83|||||||||
6976|Gambier Limestone|48624|14|Not recorded|p4,6,Fig.2|||(J54-6/Benara).||||||
6976|Gambier Limestone|48625|14|Not recorded|p4,5|||(J54-6/Kennion). map opp.p.1.||||||
6976|Gambier Limestone|48911|6|Mentioned|Chart 1|||Heytesbury Gp.||||||
6976|Gambier Limestone|49038|5|Briefly described|p26|||||||||
6976|Gambier Limestone|49040|6|Mentioned|p11|||||||||
6976|Gambier Limestone|50133|5|Briefly described|p3, Fig.1|Mid Miocene|Late Eocene|Also called Mount Gambier Limestone (superseded term) in this article (at p6, p8 Tb 1, p11 Tb.2). Major & trace element geochemistry for 2 samples given.|||Includes Camelback Member.||Fossiliferous carbonate|27-MAR-12
6976|Gambier Limestone|60538|5|Briefly described|p471 Fig. 10, 473 Fig. 12|||Of the Nirranda Group.||||||
6976|Gambier Limestone|60785|6|Mentioned|p184 Fig.1. |Chattian|Chattian|South Australia.|||Includes the Camelback Member.|||
6976|Gambier Limestone|60953|5|Briefly described|Map Legend|Miocene|Eocene|Marine fossiliferous limestone. Geological Province: Gambier Basin.||||||
6976|Gambier Limestone|61108|5|Briefly described|map legend|Miocene|Eocene|Marine fossiliferous limestone. Geological Province: Gambier Basin.||||||
6976|Gambier Limestone|61155|5|Briefly described|p18|Middle Miocene|Early Oligocene|Murray Group. Overlies Ettrick Formation; overlain by Mannum Formation. Age: 27.5-~24Ma to ~33-15Ma. Interfingered with Naracoorte Limestone. Thickness: 100m. Geological Province: Murray and Otway Basin.||||||03-MAR-10
6976|Gambier Limestone|61547|6|Mentioned|p461 Fig.2. |Miocene|Eocene|||Unit in Heytesbury Group.||Overlies Gellibrand Marl.||
6976|Gambier Limestone|61622|5|Briefly described|p436 Fig. 2|Miocene|Eocene|Of Heytsbury Group. Geological Province: Otway Basin.||||||07-FEB-11
6976|Gambier Limestone|61627|5|Briefly described|p500 Fig. 2|Miocene|Late Eocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-FEB-11
6976|Gambier Limestone|62640|6|Mentioned|p76.|||Tertiary. Restricted cave development is due to substantial intergranular porosity and permeability; hence considerable groundwater flow through the limestone matrix and less flow through karst conduits.||||||
6976|Gambier Limestone|63122|5|Briefly described|p17 Fig. 4.3|Early Miocene|Late Eocene|Of the Heytesbury Group. Max. thickness: 400m. Geological Province: Otway Basin. ||||||
6976|Gambier Limestone|63124|4|Described|p49 Fig. 5.2, p87 Fig. 5.29, p91|Miocene|Late Eocene|Of the Heytesbury Group. Supersedes "Mount Gambier Limestone". Comprises Greenways, Gellibrand, Camelback, and Green Point Members, and Naracoorte Limestone Member. Max. thickness: 400m. Geological Province: Otway Basin.||||||
6976|Gambier Limestone|63129|6|Mentioned|p139|||Geological Province: Otway Basin. Surface aquifer.||||||30-JAN-08
6976|Gambier Limestone|63222|5|Briefly described|p40, p41|||Dimension stone from the South East, S.A.||||||01-MAR-10
6976|Gambier Limestone|63431|5|Briefly described|p677 Fig. 2|Miocene|Eocene|Of the Heytesbury Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
6976|Gambier Limestone|63887|5|Briefly described|p21 Fig. 1|||||||||
6976|Gambier Limestone|64769|6|Mentioned|p28|Miocene|Miocene|Material mined is named the Gambier Stone. SA.||||||06-MAY-09
6976|Gambier Limestone|64966|5|Briefly described|p137, p144|Middle Miocene|Late Oligocene|Of the Heytesbury Group. Max. thickness: 400m. Major fossiliferous unit with strong erosional unconformity at the top. Geol.province: Gambier Basin. Equivalent to Mannum Limestone in Murray Basin. Forms bedrock platform beneath most of Lacepede Shelf.||||||07-FEB-11
6976|Gambier Limestone|65374|6|Mentioned|p35|||||||||
6976|Gambier Limestone|65552|6|Mentioned|p5 Fig. 3|Miocene|Oligocene|Of Murray Group (western Murray Basin).||||||
6976|Gambier Limestone|65891|5|Briefly described|p221 Fig.5, p229.|Paleogene|Paleogene|Western Otway Basin. Rupelian age. Pure and temporally persistent neritic carbonate unit. Same suite of planktonic foraminifera as Aldinga Member, but with higher numbers plus Globoturborotalita brevis. ||||||
6976|Gambier Limestone|68211|5|Briefly described|p28, p28 Fig.1, p29|Langhian|Bartonian|Occurs extensively in the Gambier Basin and southwestern Murray Basin. Produced as  a dimension stone and sold under the trade name: Compton Sandstone.|c. 40 - 15 Ma, (White 1996)||||Dolomitic rock.|
6976|Gambier Limestone|68811|6|Mentioned|p110, p130, p156 app 1, p192 tbl 46|Tertiary|Tertiary|Hosts an unconfined aquifer. Also referred to informally as the Gambier limestone on p156 app 1.  ||||Overlies the Dilwyn Formation.||
6976|Gambier Limestone|69297|5|Briefly described|p79|Langhian|Rupelian|Otway Basin.||Heytesbury Group|Includes the Greenways Member, Camelback Member, Green Point Member and the Narracoorle Limestone Member. |Overlies the Narrawaturk Marl. Unconformably overlain by the Bridgewater Formation or the Coomandook Formation. |Limestones. |
6976|Gambier Limestone|70029|5|Briefly described|p151-153,165|Miocene|Oligocene|Affected by localised regional uplift related to volcanism (Mount Burr volcanics), and defines a broad dome near volcanic centres, rising from sea level to 60m APSL east of mount Gambier. Subaerially exposed, karstified marine abrasion surface in which dolines and depressions are common.||||Overlain unconformably by Bridgewater Formation.||04-SEP-19
6976|Gambier Limestone|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Miocene|Oligocene|Otway Basin: Gambier Embayment and Voluta Trough, and Robe-Penola Trough.||Heytesbury Group.|Naracoorte Limestone, Green Point, Camelback and Greenways Members.|Overlies Narrawaturk Marl. Is overlain by Coomandook Formation.||
6976|Gambier Limestone|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Miocene|Miocene|Gambier Embayment and Voluta Trough.||Heytesbury Group.|Greenways, Camelback, Green Point and Naracoorte Members.|Overlies Narrawaturk Marl. Is overlain by Coomandook Formation.||
6976|Gambier Limestone|72445|6|Mentioned|App.7 p7 Fig.4.|Oligocene|Oligocene|See also Gambier Limestone Member in text.||Murray Group||||
6976|Gambier Limestone|73118|6|Mentioned|p17|||||||||
6976|Gambier Limestone|73228|4|Described|p50, p52, p56|Middle Miocene|Late Early Oligocene|Murray Basin. Open shelf environment. Identified in Cooltong 1 drillhole.||||Underlain by Ettrick Formation. Overlain by Mannum Formation, Murray Group.|Includes grey, cream bryozoal limestone, dolomitic in part, with minor glauconite.|
6976|Gambier Limestone|73229|5|Briefly described|p66-67, p70-71, p74|Middle Miocene|Early Miocene|Murray Basin. [Analysed using pXRF; see article]. Incuded in group of early Oligocene to Middle Miocene units p67.|||||Includes limestone, bryzoal, grey-cream, dolomitic in part, minor glauconite.|01-NOV-22
6976|Gambier Limestone|73383|6|Mentioned|p82, p213|||Limestone and sub-litharenite lithologies based on geochemistry using the ChemLith classification and the Herron classification (1988).||||||
28564|Garden Cove Formation|33319|6|Mentioned|p170|||Fauna||||||
75778|Garden Creek Igneous Complex|68115|5|Briefly described|p5, p7.|Devonian|Devonian|New name. Replaces the Besford Caldera (VandenBerg et al. 1998a). The Sloan Knob Microgranite forms its ring dyke.|||Includes Besford Ignimbrite.|||
34782|Gariwerd Sandstone|23309|5|Briefly described|p78|||Maximum Thickness: 300m.  Of the Red Man Bluff Subgroup.||||||
34782|Gariwerd Sandstone|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Man Bluff Sub-Group (Grampians Group). Sandstone and siltstone, quartzo-micaceous-feldspathic.||||||14-JUN-06
34782|Gariwerd Sandstone|44932|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Red Man Bluff Sub-Group (Grampians Group). Sandstone and siltstone, quartzo-micaceous-feldspathic.||||||14-JUN-06
34782|Gariwerd Sandstone|60451|4|Described|p76, 79|Early Devonian|Ordovician|Of the Red Man Bluff Subgroup (Grampians Group). Quartzo-feldspathic sandstone with small amounts of mica. Type section in text. Maximum Thickness: ~300m.||||||
34782|Gariwerd Sandstone|60456|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Man Bluff Sub-Group. Sandstone and siltstone: reddish yellow, quartzo-micaceous and feldspathic; planar and cross laminated, thin to thickly bedded.||||||30-SEP-04
34782|Gariwerd Sandstone|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Man Bluff Subgroup. Unit does not appear on this map.||||||
34782|Gariwerd Sandstone|61183|4|Described|p30 Tb. 2, p36|||Of the Red Man Bluff Subgroup (Grampians Group). Micaceous quartzo-feldspathic sandstone to the east of Mount William and more coarse-grained and pebbly to the north. Overlies Thermopylae Conglomerate; underlies Watgania Gap Sandstone. Thickness: ~300m. ||||||
34782|Gariwerd Sandstone|64541|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Red Man Bluff Sub-group. Sandstone and siltstone: reddish-yellow, quartzo-micaceous-feldspathic; laminated and cross-laminated, thin to thickly bedded; coarser and more pebbly in north.||||||07-FEB-11
34782|Gariwerd Sandstone|64610|5|Briefly described|Map legend|Ordovician|Ordovician|Of Red Man Bluff Subgroup (Grampians Gp). Sandstone and siltstone; reddish-yellow, quartz-micaceous-feldspathic; laminated and cross-laminated, thin to thickly bedded; coarser and more pebbly to the north.||||||
34782|Gariwerd Sandstone|65313|6|Mentioned|p581 Fig. 9,p582 Fig. 10|Ordovician|Ordovician|Grampians National Park sections.||Of Red Man Bluff Subgroup.||Overlies Thermopylae Conglomerate, underlies Watgania Gap Sandstone.||26-MAR-12
34782|Gariwerd Sandstone|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Red Man Bluff Subgroup. Defined by Cayley & Taylor, 1997.||||||
34782|Gariwerd Sandstone|68116|5|Briefly described|Appendix, Maps 22, 30.|Ludlow|Late Ordovician|Early Ludlow minimum age.|||||Sandstone and siltstone: sandstone reddish yellow; quartzo-feldspathic, micaceous; planar and crosslaminated, thin to thick-bedded; pebbly and coarser grained in north.|
7041|Garvey Gully Formation|23229|4|Described|Table3-1p16, 17|Late Cambrian|Middle Cambrian|||||||
7041|Garvey Gully Formation|23309|6|Mentioned|p43, 46||Late Cambrian|||||||
7041|Garvey Gully Formation|24004|5|Briefly described|p275 Fig.2|Cambrian|Cambrian|||||||
7041|Garvey Gully Formation|24551|5|Briefly described|p91|||Includes the Dolodrook Limestone Member.||||||
7041|Garvey Gully Formation|24575|5|Briefly described|p709, p713 Fig. 2|Late Cambrian|Middle Cambrian|Mafic-ultramafic-derived sedimentary rocks and limestone. Geological Province: Lachlan Fold Belt.  See CORRIGENDUM for this paper AJES 50(6) - reference to I.R.Duddy's Hons.thesis and his interpretation of this unit.||||||14-MAR-05
7041|Garvey Gully Formation|33602|6|Mentioned|Fig.2|||P23||||||
7041|Garvey Gully Formation|35073|5|Briefly described|p2|||||||||
7041|Garvey Gully Formation|40761|5|Briefly described|Table 1|||||||||
7041|Garvey Gully Formation|41868|6|Mentioned|p572|||||||||
7041|Garvey Gully Formation|44187|5|Briefly described|Map Legend||Cambrian|||||||
7041|Garvey Gully Formation|60905|5|Briefly described|p919|||Volcanogenic sediments. Interpretation by I.A Duddy (1974) which should have been included in the AJES 50(5) article by Spaggiari,Gray and Foster "Formation and emplacement...Dolodrook serpentinite body, Lachlan Orogen, Victoria".||||||
7041|Garvey Gully Formation|62742|5|Briefly described|p697|Cambrian|Cambrian|Includes the Dolodrook Limestone Member.||||||
7041|Garvey Gully Formation|62791|4|Described|p225, p226|Ordovician|Ordovician|Discovery of mid-Ordovician (Darriwilian) graptolites changes age of this unit and Member status of Cambrian Dolodrook limestones.~200 m thick.||||Unconformably overlies Mount Wellington Greenstone Belt serpentinised ultramafics.|Volcanigenic sandstone and mudstone. Includes blocks of Dolodrook River limestones.|28-MAR-12
7041|Garvey Gully Formation|68116|5|Briefly described|Appendix, Map 43.|Cambrian|Cambrian||||||Chert, volcaniclastic sandstone, mudstone, limestone. Base is a conglomerate with clasts of andesite, serpentinite, metadolerite, metagabbro, and minor rhyolite and shale.|
7041|Garvey Gully Formation|68822|6|Mentioned|p332|Ordovician|Ordovician|Contains preserved blocks of allochthonous limestone. Brock and Talent (1999) inferred an Ordovician age from recovered Middle Ordovician graptolites recovered from sandstone a few meters along strike from one of these bodies.||||||
7041|Garvey Gully Formation|70026|6|Mentioned|p49|||Contains upper middle to lowermost upper Cambrian limestone olistoliths, associated with ultramafic rocks (Crawford et al., 2003a; Engelbretsen 2006), consistent with development of a possible oceanic transform fault segment within the oceanic setting (Spaggiari  et al. 2003, 2004).||||||
7041|Garvey Gully Formation|70601|5|Briefly described|p44|Idamean|Mindyallan|Howqua West area.||||Unconformably overlies Lickhole Volcanics and Thiele Complex.||
7046|Gattamurh Granite|23309|6|Mentioned|p431 Appendix 1|||G73, I-Type. Supersedes Willis Granite.||||||22-FEB-13
7046|Gattamurh Granite|42726|5|Briefly described|map legend|||||||||
7046|Gattamurh Granite|68115|5|Briefly described|pp6-7.|||Deddick Zone. White and Chappell (1988); changed to Willis (?Granite) in Chappell et al. (1991) as the locality of Willis is within the pluton's outcrop. The name reverted to Gattamurh Granite in VandenBerg et al. (2000) as it had precedence, even though the pluton does not lie on Gattamurh Creek (presumably the source of the name).||||||
7046|Gattamurh Granite|68116|5|Briefly described|Appendix, Map 28.|Early Devonian|Wenlock||||||Granite: mafic I-type; magnetic.|
30449|Gatum Ignimbrite|23309|5|Briefly described|p82. Table 2.28|||Maximum Thickness: 30m.||||||
30449|Gatum Ignimbrite|24551|6|Mentioned|p122 Fig. 5.6|||||||||
30449|Gatum Ignimbrite|44929|5|Briefly described|Map Legend||Early Devonian|Of Rocklands Volcanics.  Quartz-feldspar ignimbrite, pinkish grey with abundant crystals up to 3mm.||||||14-JUN-06
30449|Gatum Ignimbrite|44930|5|Briefly described|Map Legend||Early Devonian|Of Rocklands Volcanics.  Quartz-feldspar ignimbrite, pinkish grey with abundant crystals up to 3mm.||||||14-JUN-06
30449|Gatum Ignimbrite|44931|6|Mentioned|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanics.||||||14-JUN-06
30449|Gatum Ignimbrite|44932|5|Briefly described|Map Legend||Early Devonian|Of Rocklands Volcanics.  Quartz-feldspar ignimbrite, pinkish grey with abundant crystals up to 3mm.||||||14-JUN-06
30449|Gatum Ignimbrite|44933|5|Briefly described|Map Legend||Early Devonian|Of Rocklands Volcanics.  Quartz-feldspar ignimbrite, pinkish grey with abundant crystals up to 3mm.||||||14-JUN-06
30449|Gatum Ignimbrite|50154|2|Defined|p117, p245 App.5|Devonian|Devonian|Of the Rocklands Volcanic Group. Overlies the Nigretta Ignimbrite. Thickness: 10-30m||||||15-SEP-04
30449|Gatum Ignimbrite|50155|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Quartz-feldspar ignimbrite. Overlies the Glenelg River Metamorphic Complex.||||||25-JUN-04
30449|Gatum Ignimbrite|50156|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pinkish grey with abundant crystals upto 3mm; eutaxitic texture with pink fiamme foliation||||||
30449|Gatum Ignimbrite|50157|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pinkish grey with abundant crystals upto 3mm; eutaxitic texture with pink fiamme foliation||||||
30449|Gatum Ignimbrite|50158|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pinkish-grey||||||24-AUG-04
30449|Gatum Ignimbrite|50159|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pinkish grey with abundant crystals upto 3mm; eutaxitic texture with pink fiamme foliation||||||24-JUN-04
30449|Gatum Ignimbrite|50160|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz-feldspar ignimbrite||||||
30449|Gatum Ignimbrite|50161|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pinkish grey with abundant crystals upto 3mm; eutaxitic texture with pink fiamme foliation||||||24-JUN-04
30449|Gatum Ignimbrite|50162|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pinkish grey with abundant crystals upto 3mm; eutaxitic texture with pink fiamme foliation||||||24-JUN-04
30449|Gatum Ignimbrite|50163|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pinkish grey with abundant crystals upto 3mm; eutaxitic texture with pink fiamme foliation||||||24-JUN-04
30449|Gatum Ignimbrite|61183|4|Described|p62|Early Devonian|Early Devonian|Of Rocklands Volcanics Group. Texturally similar to Nigretta Ignimbrite but finer grained with less crystals. A conspicuous pink fiamme foliation characterises the rock - lithic fragments are absent. Overlies Nigretta Ignimbrite. Max. thickness: 30m. ||||||
30449|Gatum Ignimbrite|64541|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanics. Quartz-feldspar ignimbrite.||||||07-FEB-11
30449|Gatum Ignimbrite|64610|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Rocklands Volcanics. Quartz feldspar ignimbrite: pinkish-grey with abundant crystals up to 3mm; eutaxitic texture with pink fiamme foliation.||||||11-NOV-08
30449|Gatum Ignimbrite|66002|5|Briefly described|p6 Tb.4|Devonian|Devonian|Of Rocklands Volcanic Group. Defined in Simpson 1997, p62.||||||
7086|Geehi Granite|29953|6|Mentioned|p3|||||||||
7086|Geehi Granite|40328|4|Described|p206|||||||||
7086|Geehi Granite|40498|6|Mentioned|p392|||||||||
7086|Geehi Granite|45087|5|Briefly described|p36|||Chemical analyses.||||||
7090|Geera Clay|2967|5|Briefly described|p14, p15 Fig.2.2, p24, 29, 50, 158|Miocene|Oligocene|Lawrence (1966). Murray Basin. 170m thick. A significant aquiclude. See also p178-179, 231, 285, 300, 304, 315, 318, 320.||Murray Group.||Overlies Renmark Group. Is overlain by Winnambool Formation. Is separated from the overlying Parilla Sand by the Mologa Surface. Grades westwards into the Ettrick Marl.|Sparingly fossiliferous, dark grey to black clay.|
7090|Geera Clay|10010|5|Briefly described|p12 Fig. 3|Middle Miocene|Late Oligocene|Of the Murray Group. Overlain by Renmark beds. Geological Province: Murray Basin.||||||13-AUG-07
7090|Geera Clay|22587|6|Mentioned|p79 Fig.7|Middle Miocene|Late Oligocene|||||||
7090|Geera Clay|22773|5|Briefly described|p351,Fig24.8p352|||||||||
7090|Geera Clay|22799|2|Defined|p31|Middle Miocene|Late Oligocene|Of the Murray Group.||||||29-JUL-08
7090|Geera Clay|22857|5|Briefly described|p351, p353 Fig. 24.9|Miocene|Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||
7090|Geera Clay|22887|5|Briefly described|Fig.6 p13|Miocene|Oligocene|||||||
7090|Geera Clay|22893|3|Fully described|p28 fig8a,9 table3|Miocene|Miocene|||||||
7090|Geera Clay|23179|6|Mentioned|Fig.2|Middle Miocene|Late Oligocene|Murray Supergroup||||||
7090|Geera Clay|23226|6|Mentioned|p889,890,891|||Of Murray Supergroup.||||||
7090|Geera Clay|23884|5|Briefly described|p153, p155 Fig.13.2|Miocene|Oligocene|Geological Province: Murray Basin.||||||
7090|Geera Clay|23909|6|Mentioned|p298|||||||||
7090|Geera Clay|23921|5|Briefly described|p1109|Early Miocene|Early Miocene|Geological Province: Murray Basin.||||||
7090|Geera Clay|24100|6|Mentioned|p99|||Geological Province: Murray Basin.||||||19-APR-05
7090|Geera Clay|24177|5|Briefly described|p69|Middle Miocene|Late Oligocene|Renmark Group grades westward into this deposit (Lawrence, 1975). Geological Province: Murray Basin.||||||
7090|Geera Clay|24551|6|Mentioned|p322 Fig. 10.29|||Of the Murray Group.||||||
7090|Geera Clay|24563|5|Briefly described|p485|||Included in the Murray Supergroup by Lukasik and James (1998).  However, Murray Supergroup now abandoned and Murray Group reinstated - Geera Clay not included.  Geological Province: Murray Basin.||||||
7090|Geera Clay|29591|6|Mentioned|Table 20|||||||||
7090|Geera Clay|29898|6|Mentioned|Table 20|||||||||
7090|Geera Clay|30581|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7090|Geera Clay|30934|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
7090|Geera Clay|30935|6|Mentioned|Map legend|Tertiary|Tertiary|Subsurface||||||
7090|Geera Clay|30936|6|Mentioned|Map legend|Eocene|Eocene|||||||
7090|Geera Clay|31741|6|Mentioned|p6|||||||||
7090|Geera Clay|31746|3|Fully described|p195|||||||||
7090|Geera Clay|31747|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
7090|Geera Clay|34735|4|Described|p32|||Also mention P31.||||||
7090|Geera Clay|34813|6|Mentioned|p62|||||||||
7090|Geera Clay|37796|6|Mentioned|p164|||||||||
7090|Geera Clay|37809|6|Mentioned|p7|||||||||
7090|Geera Clay|38601|4|Described|p7|||||||||
7090|Geera Clay|39329|6|Mentioned|Fig.1|||||||||
7090|Geera Clay|39929|4|Described|p267|||||||||
7090|Geera Clay|40820|6|Mentioned|Fig.4|||||||||
7090|Geera Clay|41423|6|Mentioned|p284|||||||||
7090|Geera Clay|41511|6|Mentioned|p20|||||||||
7090|Geera Clay|41868|6|Mentioned|p551|||||||||
7090|Geera Clay|42125|5|Briefly described|p134|||See also Fig.5||||||
7090|Geera Clay|42126|6|Mentioned|p149|||||||||
7090|Geera Clay|42130|6|Mentioned|p271|||||||||
7090|Geera Clay|42132|6|Mentioned|p295|||||||||
7090|Geera Clay|42133|6|Mentioned|p301|||||||||
7090|Geera Clay|42134|4|Described|p339|||||||||
7090|Geera Clay|42137|4|Described|p372,p376|||See also Table 3||||||
7090|Geera Clay|42138|6|Mentioned|p388|||||||||
7090|Geera Clay|42375|5|Briefly described|p26|early Miocene|late Oligocene|Murray Basin||||||
7090|Geera Clay|42509|5|Briefly described|p2|||||||||
7090|Geera Clay|42510|5|Briefly described|p35|||||||||
7090|Geera Clay|42511|6|Mentioned|Fig.2 P55|||||||||
7090|Geera Clay|42512|6|Mentioned|p68|||||||||
7090|Geera Clay|42514|6|Mentioned|p116|||||||||
7090|Geera Clay|42515|6|Mentioned|p134|||||||||
7090|Geera Clay|42517|5|Briefly described|p169|||||||||
7090|Geera Clay|42518|5|Briefly described|p185|||||||||
7090|Geera Clay|42519|6|Mentioned|p205|||||||||
7090|Geera Clay|42720|5|Briefly described|map legend|Miocene|Oligocene|||||||
7090|Geera Clay|42813|5|Briefly described|p24|||||||||
7090|Geera Clay|42827|3|Fully described|p269|||Of Murray Group.||||||03-FEB-09
7090|Geera Clay|42881|4|Described|Fig.3, P84|||||||||
7090|Geera Clay|42966|2|Defined|p139|Middle Miocene|Late Oligocene|Of the Murray Group.||||||03-FEB-09
7090|Geera Clay|43655|5|Briefly described|p40-846|||||||||
7090|Geera Clay|43669|4|Described|p22|Middle Miocene|Early Miocene|||||||
7090|Geera Clay|43780|6|Mentioned|p5|Middle Miocene|Late Oligocene|||||||
7090|Geera Clay|43790|5|Briefly described|p383|||||||||
7090|Geera Clay|43791|5|Briefly described|p371|||||||||
7090|Geera Clay|43804|5|Briefly described|p47|Miocene|Oligocene|||||||
7090|Geera Clay|44133|5|Briefly described|p159|Middle Miocene|Early Miocene|Of the Muray Group. Geological Province: Murray Basin. ||||||
7090|Geera Clay|44188|5|Briefly described|Map Legend|Late Miocene|Late Oligocene|Geological province: Murray Basin. Poorly consolidated, plastic to friable, black, grey dark green clay, silt, minor sand; commonly glauconitic, fossiliferous, calcareous, carbonaceous; local sandy dolomitic intercalations.||||||15-MAY-08
7090|Geera Clay|44191|5|Briefly described|Map Legend|Middle Miocene|Late Oligocene|||||||
7090|Geera Clay|47060|6|Mentioned|p183|||||||||
7090|Geera Clay|49038|4|Described|Table 2|||||||||
7090|Geera Clay|49040|5|Briefly described|p12|||See also P11||||||
7090|Geera Clay|50154|5|Briefly described|p135|||Of the Murray Group.||||||
7090|Geera Clay|60452|5|Briefly described|p33|Middle Miocene|Late Oligocene|Marine Deposits.||||||
7090|Geera Clay|60491|4|Described|p21|||Of the Murray Group. Conformably overlies the Olney Formation. Geological Province: Murray Basin.||||||
7090|Geera Clay|60538|5|Briefly described|p480 Fig. 19|||Geological Province: Murray Basin.||||||
7090|Geera Clay|61155|5|Briefly described|p4, p18|Middle Miocene|Late Oligocene|Of the Murray group. Carbonaceous silts and minor carbonates. Interfingers with Olney Formationand ettrick Formation. Max. thickness: 150m.  Geological Province: Murray Basin.||||||03-MAR-10
7090|Geera Clay|61181|5|Briefly described|p153 Fig. 47|||Carbonaceous clay. ||||||
7090|Geera Clay|61314|5|Briefly described|p129|Miocene|Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||
7090|Geera Clay|63066|5|Briefly described|p485|||Revised stratigraphy of Lukasik and James (1999)  incorporates this unit and the Ettrick and Winnambool Formations into their new Murray Supergroup.  These were not formerly included in the definition of the Murray Group.||||||08-FEB-07
7090|Geera Clay|63460|5|Briefly described|p838, p839 Fig. 2b|Middle Miocene|Late Oligocene|Geological province: Murray Basin. Bioturbated, dark grey to black, slightly calcareous and poorly fossiliferous clay. Equivalent to Winnambool and Ettrick Formations. ||||||
7090|Geera Clay|63777|6|Mentioned|p1104 Fig. 1, p1105|||Geological Province: Murray Basin.||||||18-MAR-09
7090|Geera Clay|63887|5|Briefly described|p20, p21 Fig. 1|Middle Miocene|Late Oligocene|Of Murray Group. Lagoonal and marginal marine muddy facies.||||||
7090|Geera Clay|64237|5|Briefly described|p17, p18|Late Oligocene|Late Oligocene|Included in the Murray Group stratigraphic scheme by Lawrence (1966), retained through the various revisions of the Murray Group up to Murray Supergroup; and is now included in the reinstated Murray Group in South Australia.||||||
7090|Geera Clay|64823|5|Briefly described|p1011|Late Miocene|Paleocene|Clays and marls. Geological province: Murray Basin||||||
7090|Geera Clay|65552|5|Briefly described|p5 Fig. 3, p6|Middle Miocene|Early Oligocene|Clay/claystone with occasional dolomite. Deposited during a marine incursion. Unconformably underlies Loxton-Parilla Sands and Bookpurnong beds. Contemporaneous with Murray Group and Winnambool, Ettrick and Olney Formations.||||||
7090|Geera Clay|65719|5|Briefly described|p7|Miocene|Oligocene|In Murray Basin. Lateral equivalent of Mystic Park Formation. Marginal marine or paralic.||||||10-MAY-12
7090|Geera Clay|66573|6|Mentioned|p873|Miocene|Miocene|Murray Basin. Marine.||||||
7090|Geera Clay|67127|6|Mentioned|p73|||||||Overlies the Renmark Group. Underlies the Parilla Sand.||
7090|Geera Clay|67179|6|Mentioned|p579|||||||||
7090|Geera Clay|67462|5|Briefly described|Map legend.|Miocene|Miocene|Murray Basin.||Unit in Murray Group.||||
7090|Geera Clay|68140|5|Briefly described|p1700 Fig.1, p1701, p1704 Fig.5|Neogene|Paleogene|Up to 75m thick. Acts as an effective aquitard. Middle Tertiary age.|||||Comprises massive clays with minor sand and silt layers.|09-FEB-18
7090|Geera Clay|68189|5|Briefly described|p27 Tb.3.2, p29|Miocene|Oligocene|Depositional environment: marginal marine, lagoonal, tidal flats. The Geera Clay is the only part of the Murray Group previously recorded in ST ARNAUD. It is an important barrier which separates water flows between the Parilla Sand and Renmark Groups.||Of the Murray Group.||Underlain by the Olney Formation. Overlain by the Parilla Sand.|Comprises plastic black-green mud and sand; glauconitic.|
7090|Geera Clay|68194|5|Briefly described|p23|Miocene|Oligocene|Lawrence (1966). Murray Basin. Over 50m thick.||Unit in Murray Group.||Lateral facies equivalent of Calivil Formation.|Glauconitic claystone and interbedded dolomitic siltstone.|
7090|Geera Clay|68715|6|Mentioned|p31 Fig.5|Miocene|Miocene|Murray Basin. Early to Middle Miocene age.||Murray Group.||||07-APR-17
7090|Geera Clay|70718|4|Described|p24-p25, p103|Middle Miocene|Late Oligocene|Murray Basin. Deposited as a marginal-marine muddy facies. Improperly concatenated as Geera Formation on p24. Approximately 150m thick. Silt and sand are primarily terriginous in origin.||Murray Group|||Black, olive grey, dark-grey or dark-green silty mud, silt and clay with minor dark sand.|
7090|Geera Clay|71593|6|Mentioned|p52-p54|||||||||
7090|Geera Clay|72445|5|Briefly described|.App.1, App.2; App.6 p1, p3-4, p6; App.7|Miocene|Oligocene|Shown in App 7 Fig 4 (from Brown & Stephenson 1991). See also App. 7 p2, p4, p16-18. Identified in Stavely 12,16. App.6, App.7 propose Early Miocene Geera Clay at 65m in Stavely 11, but this is identified as Olney Formation, Renmark Group in well logs.||Murray Group||Underlies Port Campbell Limestone,conformity; Calivil Formation, sharp contact; Loxton Sand. Overlies Carrolls Amphibolite,sharp contact; Winnambool Formation, gradational; Renmark Group, unconformity|Includes carbonaceous fine sand and (black) clays, grey and mottled silty mud.|
7090|Geera Clay|73118|5|Briefly described|p17, 37, 45, 48, 61, 82|||Glenelg Zone, Western Victoria. Drill core summary logs. 170m thick; mainly <50m. Entirely concealed. Deposited in shallow and marginal marine, interdistributary bay, lagoonal and tidal flat environments.||Murray Group.||Overlies Ettrick, Olney Formations and Saint Arnaud Group. Is overlain by Bookpurnong Beds and Loxton-Parilla Sands.|Poorly consolidated, black to dark green silt, clay, minor sand; commonly glauconitic, fossiliferous, calcareous, carbonaceous; locally includes sandy dolomitic intercalations. Abundant low-diversity faunas.|
7090|Geera Clay|73188|6|Mentioned|p320|Miocene|Miocene|Murray Basin.|||||Clay.|
7090|Geera Clay|73228|4|Described|p50, p55-57, p60|Middle Miocene|Late Early Oligocene|Murray Basin. Muddy lagoonal and marginal marine / tidal environments [although Fabris 2003 provided a different interpretation]. Represents marine incursions within the Murray Group.||Murray Group|||Black to grey-green, carbonaceous, pyritic clay and silt with minor sand and glauconite and sparse marine fossils.|
7090|Geera Clay|73229|6|Mentioned|p67|Middle Miocene|Late Early Oligocene|Murray Basin.||Murray Group||||
7090|Geera Clay|73496|6|Mentioned|Map legend|Miocene|Oligocene|||||||
7090|Geera Clay|73505|4|Described|p2, p11, p13-14, p36|Miocene|Late Eocene|Murray Basin. Mostly deposited in a marginal marine environment, includes intertital and estuarine deposits. Interfingers with lateral equivalents of the Calivil Formation. No detectable magnetic response.||Murray Group||Overlies Norval Regolith, offshore equivalent to Calivil Formation, underlies Bookpurnong beds|Marginal marine, marine to nonmarine clay, 100 m thick.|
7097|Gelantipy Ignimbrite|23309|4|Described|p109, Table 2.40|||Of the Little River Subgroup.  Maximum Thickness: 1300m.||||||
7097|Gelantipy Ignimbrite|23615|3|Fully described|p113|Early Devonian|Early Devonian|Base of Little River Subgroup.  See also p225 App 2.  Orginally mapped as Gelantipy Rhyodacite (Ringwood, 1955a,b). Composed of numerous flows of pumiceous ignimbrite with minor breccia and sediment lenses.  Age: Early Devonian ~410-395Ma.  Max. thickness: 1300m.||||||16-AUG-18
7097|Gelantipy Ignimbrite|24551|5|Briefly described|p144|||Of Little River Subgroup.||||||
7097|Gelantipy Ignimbrite|41585|4|Described|p136|||||||||
7097|Gelantipy Ignimbrite|43206|5|Briefly described|map legend||Lochkovian|of Little River Subgroup.||||||
7097|Gelantipy Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Quartz-feldspar ignimbrite: grey, green; pumice-rich.|
7107|Gellibrand Marl|12781|6|Mentioned|p386|Miocene|Eocene|Otway Basin. Maximum thickness 26m.||Heytsbury Group.||Overlies Compton Conglomerate conformably and Narrawaturk Marl unconformably. Is overlain by Gambier Limestone.||
7107|Gellibrand Marl|22875|5|Briefly described|p68|Middle Miocene|Early Oligocene|Of the Heytesbury Group.||||||09-MAY-07
7107|Gellibrand Marl|22944|5|Briefly described|Fig3|||||||||
7107|Gellibrand Marl|23230|5|Briefly described|Table4-1p40, Fig4-3p46|||||||||
7107|Gellibrand Marl|23307|5|Briefly described|Map Legend|Miocene|Miocene|Of Heytesbury Group||||||
7107|Gellibrand Marl|23322|5|Briefly described|957 Fig.2|Miocene|Oligocene|Of the Heytesbury Group.  Geological Province: Otway Basin.||||||07-SEP-09
7107|Gellibrand Marl|23909|5|Briefly described|p291|Miocene|Miocene|Geological Province: Otway Basin.||||||
7107|Gellibrand Marl|24056|5|Briefly described|p84 Fig. 2|Miocene|Oligocene|Of Heytesbury Group.  Geological Basin: Otway Basin.||||||
7107|Gellibrand Marl|24314|5|Briefly described|p61 Fig.2|Miocene|Eocene|Geological Province: Otway Basin. Max. Thickness 28m. Of the Heytesbury Group.||||||30-NOV-04
7107|Gellibrand Marl|24551|5|Briefly described|p246, 584, p732 Table 17.2|Miocene|Oligocene|Of the Heytesbury Group.  Max thickness: 450m.||||||
7107|Gellibrand Marl|24562|5|Briefly described|p8 Fig. 2|Miocene|Oligocene|Of the Heytesbury Group.  Geological Province: Otway Basin.||||||
7107|Gellibrand Marl|29823|5|Briefly described|p14|||||||||
7107|Gellibrand Marl|29856|6|Mentioned|p36|||||||||
7107|Gellibrand Marl|30576|6|Mentioned|Table 1|||||||||
7107|Gellibrand Marl|30578|5|Briefly described|p12|||||||||
7107|Gellibrand Marl|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7107|Gellibrand Marl|30675|5|Briefly described|p253|||Lithology & radioactivity||||||
7107|Gellibrand Marl|30865|6|Mentioned|p315|||Middle Miocene||||||
7107|Gellibrand Marl|30932|6|Mentioned|Map legend|Miocene|Oligocene|Equivalent in part to Gambier Lst. Oligocene-Miocene||||||
7107|Gellibrand Marl|31036|1|Redefined|p212|Tertiary|Tertiary|Unit of Heytesbury Gp. See also p199, Table 19-1.||||||09-MAY-07
7107|Gellibrand Marl|31583|6|Mentioned|p18|||Section||||||
7107|Gellibrand Marl|31625|6|Mentioned|Fig. 5.2|||Oligocene- Miocene||||||
7107|Gellibrand Marl|31922|6|Mentioned|Fig.2|||||||||
7107|Gellibrand Marl|32499|6|Mentioned|p111|||||||||
7107|Gellibrand Marl|33940|6|Mentioned|p414|||||||||
7107|Gellibrand Marl|34954|6|Mentioned|Fig.35|||||||||
7107|Gellibrand Marl|35066|3|Fully described|p211|||p223.||||||09-MAY-07
7107|Gellibrand Marl|35262|6|Mentioned|p4|||||||||
7107|Gellibrand Marl|35274|6|Mentioned|p422|||||||||
7107|Gellibrand Marl|35290|6|Mentioned|p38|||||||||
7107|Gellibrand Marl|36499|6|Mentioned|p43|||||||||
7107|Gellibrand Marl|36913|6|Mentioned|p81|||||||||
7107|Gellibrand Marl|37385|6|Mentioned|p9|||||||||
7107|Gellibrand Marl|38625|6|Mentioned|Table 2|||||||||
7107|Gellibrand Marl|39967|4|Described|p43|||||||||
7107|Gellibrand Marl|40947|6|Mentioned|p3|||||||||
7107|Gellibrand Marl|41016|5|Briefly described|p214|||||||||
7107|Gellibrand Marl|41185|6|Mentioned|Fig.4|||||||||
7107|Gellibrand Marl|41269|6|Mentioned|Fig.2|||||||||
7107|Gellibrand Marl|41398|6|Mentioned|p1|||||||||
7107|Gellibrand Marl|41642|6|Mentioned|Fig.8.6|||||||||
7107|Gellibrand Marl|41701|6|Mentioned|Map legend|Miocene||||||||
7107|Gellibrand Marl|41704|6|Mentioned|Fig.3|||||||||
7107|Gellibrand Marl|41714|6|Mentioned|Fig.2|||||||||
7107|Gellibrand Marl|41726|6|Mentioned|Fig.5|||||||||
7107|Gellibrand Marl|41769|4|Described|p33|||||||||
7107|Gellibrand Marl|42079|6|Mentioned|Fig.2 P264|||See also Fig.10, p272||||||
7107|Gellibrand Marl|42371|6|Mentioned|p42|Janjukian||||||||
7107|Gellibrand Marl|42452|5|Briefly described|Map legend|middle Miocene|late Oligocene|||||||
7107|Gellibrand Marl|42453|4|Described|p17|||||||||
7107|Gellibrand Marl|42524|5|Briefly described|Fig.3 P27|||||||||
7107|Gellibrand Marl|42635|6|Mentioned|p89|||(Fyansford Formation)||||||
7107|Gellibrand Marl|42827|3|Fully described|p285|||Of the Heytesbury Group.||||||09-MAY-07
7107|Gellibrand Marl|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
7107|Gellibrand Marl|43195|6|Mentioned|Map Legend|Middle Miocene|Late Eocene|of Heytesbury Group.||||||
7107|Gellibrand Marl|43208|5|Briefly described|map legend|Middle Miocene|Oligocene|Of Middle Oligocene - Middle Miocene age. Of Heytesbury Group.||||||09-MAY-07
7107|Gellibrand Marl|43219|5|Briefly described|Fig.3,p6.|Miocene|Oligocene|Of Heytesbury Group.||||||09-MAY-07
7107|Gellibrand Marl|43590|4|Described|p24|Middle Miocene|Early Oligocene|||||||
7107|Gellibrand Marl|43604|5|Briefly described|p145,Fig.2|||||||||
7107|Gellibrand Marl|43660|6|Mentioned|Fig.6,p15||Oligocene|||||||
7107|Gellibrand Marl|43667|6|Mentioned|Fig.3,p12|Middle Miocene|Early Miocene|||||||
7107|Gellibrand Marl|43733|6|Mentioned|Fig.2.11,p65||Oligocene|||||||
7107|Gellibrand Marl|43937|5|Briefly described|Map Legend|Early Oligocene|Middle Eocene|||||||
7107|Gellibrand Marl|44133|4|Described|p156|Early Oligocene|Early Oligocene|Of the Heytesbury Group. Geological Province: Gambier Basin. Underlies Camelback Member of the Gambier Limestone. Thickness: 7m.||||||
7107|Gellibrand Marl|44186|5|Briefly described|Map Legend||Miocene|||||||
7107|Gellibrand Marl|48911|6|Mentioned|Chart 1|||||||||
7107|Gellibrand Marl|48977|6|Mentioned|Fig.5|||||||||
7107|Gellibrand Marl|50154|5|Briefly described|p135|||Of the Heytesbury Group.||||||25-AUG-04
7107|Gellibrand Marl|60421|5|Briefly described|p417|Middle Miocene|Oligocene|Of the Heytesbury Group.||||||
7107|Gellibrand Marl|60452|6|Mentioned|p15|||Used as an age indicator in the phrase 'post Gellibrand Marl (late Miocene)'.||||||26-JUN-13
7107|Gellibrand Marl|60563|5|Briefly described|p46|||Of the Heytesbury Group. Overlain by the Port Campbell Limestone.||||||16-JUN-05
7107|Gellibrand Marl|60581|5|Briefly described|Map Legend|Miocene|Miocene|Of the Heytesbury Group. Marine shelf deposits: clay, marl and worm-burrowed calcarenite, fine to medium grained quartz and detrital calcareous fossil fragments in clay matrix, moderately sorted, massive to well bedded.||||||
7107|Gellibrand Marl|60582|5|Briefly described|Map Legend|Miocene|Miocene|Of the Heytesbury Group. Marine shelf deposits: clay, marl and worm-burrowed calcarenite, fine to medium grained quartz and detrital calcareous fossil fragments in clay matrix, moderately sorted, massive to well bedded.||||||23-NOV-04
7107|Gellibrand Marl|60583|5|Briefly described|Map Legend|Miocene|Miocene|Of the Heytesbury Group. Marine shelf deposits: clay, marl and worm-burrowed calcarenite, fine to medium grained quartz and detrital calcareous fossil fragments in clay matrix, moderately sorted, massive to well bedded.||||||23-NOV-04
7107|Gellibrand Marl|60584|5|Briefly described|Map Legend|Miocene|Miocene|Of the Heytesbury Group. Marine shelf deposits: clay, marl and worm-burrowed calcarenite, fine to medium grained quartz and detrital calcareous fossil fragments in clay matrix, moderately sorted, massive to well bedded.||||||
7107|Gellibrand Marl|60585|4|Described|p30|Early Miocene|Late Oligocene|Disconformably overlain by the Newer Volcanics and Hanson Plain Sand. Overlies the Clifton Formation. Consists of massive, calcareous clay and marl; and thin to medium beds of calcarenite.||||||
7107|Gellibrand Marl|60785|5|Briefly described|p184 Fig.1, p188.  |Burdigalian|Aquitanian|Of the Otway Basin. The middle section has yielded one well-preserved isolated fossil cetacean tooth.|||||Marl, calcareous silt, clay, and sand with minor calcarenite layers.|
7107|Gellibrand Marl|61136|6|Mentioned|p27|||||||||
7107|Gellibrand Marl|61155|5|Briefly described|p18|Late Miocene|Early Miocene|Of the Heytesbury Group. Overlies the Clifton Formation. Max. thickness: 1300m. Geological Province: Otway Basin (Tyrendarra and Port Campbell Embayments).||||||03-MAR-10
7107|Gellibrand Marl|61181|6|Mentioned|p133|||Overlies Maude Formation; overlain by Port Campbell Limestone. ||||||
7107|Gellibrand Marl|61182|3|Fully described|p26-p27, p28, p177|Middle Miocene|Early Miocene|Of Heytesbury Gp. Formerly Gellibrand Clays and Gellibrand Clay. Incorporates Fishing Point Marl and "Upper Glen Aire Clay". Overlies Demons Bluff Fm and Clifton Fm. and disconformable on Dilwyn Fm also; underlies Port Campbell Lst. Max. thickness: 406m. ||||||
7107|Gellibrand Marl|61185|6|Mentioned|p58|||Unnamed sediments described as post-Gellibrand Marl sediments.||||||07-FEB-11
7107|Gellibrand Marl|61547|6|Mentioned|p461 Fig.2. |Miocene|Eocene|||Unit in Heytesbury Group.||Overlies Narrawaturk Marl. Is overlain by Gambier Limestone.||
7107|Gellibrand Marl|61622|5|Briefly described|p436 Fig. 2|Miocene|Eocene|Of Heytsbury Group. Geological Province: Otway Basin.||||||07-FEB-11
7107|Gellibrand Marl|61623|6|Mentioned|p449 Fig. 4|Miocene|Oligocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-APR-09
7107|Gellibrand Marl|61624|5|Briefly described|p465, p466 Fig. 2, p471|Early Miocene|Early Miocene|Of Haytesbury Group. Underlain by Clifton Formation. Geological Province: Otway Basin.||||||07-APR-09
7107|Gellibrand Marl|61626|5|Briefly described|p487, p486 Fig. 2, p488 Fig. 4|Miocene|Oligocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-APR-09
7107|Gellibrand Marl|61627|5|Briefly described|p500 Fig. 2|Miocene|Late Eocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-FEB-11
7107|Gellibrand Marl|61628|5|Briefly described|p509 Fig. 3|Late Miocene|Early Oligocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-APR-09
7107|Gellibrand Marl|62068|5|Briefly described|p135, Fig.2,|Early Miocene|Early Miocene|||||Unconformably overlain by the Hanson Plain Sands||
7107|Gellibrand Marl|62899|6|Mentioned|p46|Miocene|Miocene|On the Leigh River, SA.||||||
7107|Gellibrand Marl|63122|5|Briefly described|p17 Fig. 4.3|Early Miocene|Late Eocene|Of the Heytesbury Group. Max. thickness: 28m. Geological Province: Otway Basin. ||||||
7107|Gellibrand Marl|63124|3|Fully described|p49 Fig. 5.2, p93|Miocene|Late Eocene|Of the Heytesbury Group. Initially called "Gellibrand beds". Unconformably overlies Dilwyn Formation; conformably overlain by Camelback Member of Gambier Limestone. Age: ~32Ma. Max. thickness: 18m. Geological Province: Otway Basin.||||||
7107|Gellibrand Marl|63269|5|Briefly described|p605|Miocene|Oligocene|Otway Basin.||Heytesbury Group.||||
7107|Gellibrand Marl|63431|5|Briefly described|p677 Fig. 2|Miocene|Eocene|Of the Heytesbury Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
7107|Gellibrand Marl|63739|5|Briefly described|p46, p48|Middle Miocene|Middle Miocene|Contains ostracod assemblages on the Leigh River.||||||01-JUL-08
7107|Gellibrand Marl|64314|5|Briefly described|p500 , p502 Fig. 7|Early Miocene|Early Miocene|Marine sediments. Coded as GM in figure.||||||21-OCT-08
7107|Gellibrand Marl|65715|4|Described|p14 Tb.8, p16|Miocene|Oligocene|First used by Tate and Dennant (1893) p126 as Gellibrand beds. Of Torquay Group and Heytesbury Groups? Overlies Batesford Limestone, Clifton Springs Tuff. Underlies Black Rock Sandstone. Offshore quiet water facies. Senior synonym of Fyansford Clay and Puebla Formation.||||||
7107|Gellibrand Marl|66002|4|Described|p12, p13 Tb.9, p16, p26 Fig.7|Miocene|Miocene|Of Heytesbury Group. Called Gellibrand Clay by Baker (1953). Defined by Glenie 1971. Underlies Black Rock Sandstone. Calcareous silty clay and clayey silt, minor fine- to coarse-grained shelly calcarenite beds. Massive to moderately well bedded. Contains fossils||||||
7107|Gellibrand Marl|66012|4|Described|p18|Miocene|Oligocene|Of Heytesbury Group. Overlies Clifton Formation. Overlain by Port Campbell Limestone. Oligocene to middle Miocene| | | | | |13-JUN-13
7107|Gellibrand Marl|66245|5|Briefly described|p6 Fig.5. |Tortonian|Rupelian|||Unit in Heytesbury Group.||Overlies Clifton Formation. Is overlain by Port Campbell Limestone.||
7107|Gellibrand Marl|67061|6|Mentioned|p546 Fig.3.|Miocene|Oligocene|||Unit in Heytesbury Group.||||
7107|Gellibrand Marl|67366|5|Briefly described|p103 Fig.2. |Miocene|Miocene|||Unit in Heytesbury Group.||Overlies Clifton Formation. Is overlain by Port Campbell Limestone.|Open marine marl and calcareous mudstone.|
7107|Gellibrand Marl|67367|5|Briefly described|p131 Fig.2. |Late Miocene|Middle Miocene|||Unit in Heytesbury Group.||||
7107|Gellibrand Marl|68116|5|Briefly described|Appendix, Maps 40-41, 48-51, 54-55.|Miocene|Chattian||||||Marl, mudstone, sandstone, calcarenite, minor lignite, ligneous clay: marl blue-green and yellow; abundant carbonate nodules; contains shelly fossils and microfossils; lignite dark brown; contains spores and pollen.|
7107|Gellibrand Marl|68991|5|Briefly described|p465, p465 Fig.2|Miocene|Oligocene|Cliff-forming unit with a middle Miocene minimum age. Maximum thickness: 406 m thick.||||Conformably overlain by the Port Campbell Limestone.|Consists mainly of marine, grey calcareoous silty clay to clayey silt, with glauconite pellets and some calcarenite interbeds.|
7107|Gellibrand Marl|69297|5|Briefly described|p79, p98|Serravallian|Chattian|Otway Basin. ||Heytesbury Group||Overlies the Clifton Formation. Overlain by the Port Campbell Limestone. |Marl. |
7107|Gellibrand Marl|69651|5|Briefly described|p10|Miocene|Oligocene|||Heytesbury Group.||Overlies Clifton Formation. Is overlain by Port Campbell Limestone and unconformably by Hanson Plain Sand.||
7107|Gellibrand Marl|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Miocene|Miocene|Otway Basin: Port Campbell Embayment.||Heytesbury Group.||Overlies Clifton Formation. Is overlain by Port Campbell Limestone.||
7107|Gellibrand Marl|70880|6|Mentioned|p77|Miocene|Oligocene|Otway Basin.||||||
7107|Gellibrand Marl|70909|14|Not recorded|p62|||Distribution.||||||
7107|Gellibrand Marl|71266|6|Mentioned|p614 Fig.3|Miocene|Oligocene|Otway Basin.||||||
7107|Gellibrand Marl|71419|4|Described|p8 Fig 2, p16-17, p21-22|Miocene|Miocene|Originally 'Gellibrand-beds' of Tate and Dennant (1893). Described by them as 'Blue clay from 80 to 90 feet thick, highly fossiliferous; yellowish clay 20 to 30 feet' in cliffs west of the Gellibrand River mouth. This section designated as the type section by Baker (1953).||||Overlain by Sandringham Sandstone, Bridgewater Formation.||02-FEB-18
7107|Gellibrand Marl|71437|4|Described|Fig. 1 opp 154, p155,p160-162|Miocene|Miocene|Marine, widespread. ||Of Heytesbury Group.|Includes Rutledge Marl Member.|Transitional to overlying Port Campbell Limestone.|Marl.|
7107|Gellibrand Marl|71593|6|Mentioned|p51|||||||||
7107|Gellibrand Marl|72445|5|Briefly described|App 2; App.6 p1 Tb.1, p3.|Early Miocene|Early Miocene|App.2 is a .csv format file. Identified in Stavely 01. sample from 73m gives Early Miocene M4 zonal age (17.54 - 16.39 Ma GTS2012 timescale) deeper sample also Early Miocene based on foraminifera.||Heytesbury Group|||Includes bioturbated silty to sandy marl with lesser mud and shell fragments. Some intervals of cleaner sand in Stavely 01.|
7107|Gellibrand Marl|73357|5|Briefly described|p30, p44, p46, p48|Langhian|Chattian|Otway Basin. Correlated with Proteacidites tuberculatus Spore-Pollen Zone and Operculodinium Dinocyst Superzone, nearshore to offshore marine depositional environments. Upper part correlated to Triporopollenites bellus Spore-Pollen Zone.||Of Heytesbury Group.||Overlies Clifton Formation, underlies Port Campbell Limestone.||
7107|Gellibrand Marl|73383|5|Briefly described|p3, p10 Tb.3.8, p25, p28, p164, p236|Miocene|Oligocene|Otway Basin. Approximately equivalent to chemostratigraphic package S6-P3 which has high Ti/Cr and low Cr/Nb values. Lithologies based on geochemistry using the ChemLith classification includes limestone and calcareous limestone, and using the Herron classification (1988) includes Fe-shale, shale, Fe-sand and wacke. See also vi, p11 Tb.3.9, p34, p107, p130-131, p137, p257, p264.||Heytesbury Group||Overlies Nirranda Group, Narrawaturk Marl, Clifton Formation, underlies Port Campbell Limestone|Marls and calcareous mudstones.|
7107|Gellibrand Marl|73385|5|Briefly described|p5|Miocene|Oligocene|Otway Basin.||Heytesbury Group||Overlies Narrawaturk Marl, Clifton Formation, underlies Port Campbell Limestone.|Open marine marls and calcareous mudstones.|
7107|Gellibrand Marl|73386|4|Described|p4, p6, p14, Attachment A1|Miocene|Oligocene|Otway Basin. Abundant planktonic foraminifera. Low-energy inner shelf depositional environment where there was clastic input, outer shelf environment in the Portland area. Belongs to the Middle Proteacidites tuberculatus to Lower Triporopollenites bellus spore-pollen subzones, late Oligocene to middle Miocene.||Heytesbury Group||Overlies Clifton Formation, Narrawaturk Marl, Nirranda Group, underlies Port Campbell Limestone|Dominated by marl with sporadic horizons of calcarenite, chalks and calcsiltites.|
7107|Gellibrand Marl|73486|4|Described|p509, p511-512, p516-517, p519, p526-530|Tortonian|Chattian|Otway Basin. Gradationally transitions into Port Campbell Limestone. Common to abundant foraminifera of outer shelf depositional conditions, top lies in the middle Miocene M6/N9/E1 zones at Brumbys 1 drillhole. See also p534-535.|ca 14-15 Ma|Heytesbury Group||Overlies Clifton Formation, underlies Port Campbell Limestone|Compact fossiliferous dark greenish grey marl in upper part, with well-preserved bryozoans, scaphopods, bivalves, foraminifera, ostracods and echinoids. Made up of carbonate, quartz silt, muscovite, kaolinite, anatase.|
7107|Gellibrand Marl|73594|5|Briefly described|p4|Miocene|Oligocene|Otway Basin.||Heytesbury Group||Overlies Clifton Formation, underlies Port Campbell Limestone|Marine marls and calcareous mudstones.|
7115|Gembrook Granite|35283|6|Mentioned|p48|||||||||
7121|Genoa Peak Granite|23309|5|Briefly described|p346||Early Devonian|G7 - I-Type. Age:  395+/-8 Ma.||||||
7121|Genoa Peak Granite|30574|5|Briefly described|p10|||||||||
7121|Genoa Peak Granite|30938|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
7121|Genoa Peak Granite|33602|6|Mentioned|p37|||||||||
7121|Genoa Peak Granite|35278|6|Mentioned|p359|||||||||
7121|Genoa Peak Granite|37800|6|Mentioned|p91|||||||||
7121|Genoa Peak Granite|41572|6|Mentioned|p24|||||||||
7121|Genoa Peak Granite|41868|6|Mentioned|p590|||||||||
7121|Genoa Peak Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
7121|Genoa Peak Granite|42827|6|Mentioned|p590|||||||||
7121|Genoa Peak Granite|68116|5|Briefly described|Appendix, Map 46.|Early Devonian|Early Devonian||||||Biotite granite: pink; porphyritic with phenocrysts of orthoclase, plagioclase and quartz; accessory magnetite.|
37719|Gentle Annie Porphyry|23309|6|Mentioned|p431, Appendix 1|||G581||||||
37719|Gentle Annie Porphyry|24133|3|Fully described|p82||Early Devonian|Intrudes Pinnak Sandstone.  Geological Province: Lachlan Fold Belt.||||||
37719|Gentle Annie Porphyry|24142|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37719|Gentle Annie Porphyry|24143|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37719|Gentle Annie Porphyry|24144|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37719|Gentle Annie Porphyry|24145|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Geological Province: Lachlan Fold Belt||||||
37719|Gentle Annie Porphyry|24146|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
36865|Gibbo River Formation|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
36865|Gibbo River Formation|23309|4|Described|p90, 97, table 2.32|Late Silurian|Late Silurian|Of Wombat Creek Group. Underlying unit: Toaks Creek Conglomerate.  Maximum Thickness: 400m.||||||04-JUN-14
36865|Gibbo River Formation|60503|6|Mentioned|p30|||Same unit as Gibbo River Siltstone? probably used informally in this study, or misspelt?||||||06-SEP-05
36865|Gibbo River Formation|68116|5|Briefly described|Appendix, Map 27.|Pridoli|Ludlow||||||Siltstone, olive green-brown, laminated; calcareous siltstone; minor lenses of conglomerate, fine grained quartzitic sandstone and limestone.|
27289|Gibsons Folly Formation|22968|4|Described|P31, P111, P114||Late Silurian|Parent is Enano Group, maximum thickness is 500m, conformably underlain by Cowombat Siltstone||||||
27289|Gibsons Folly Formation|23021|5|Briefly described|Map legend|Pridoli|Pridoli|Parent is Enano Group, overlies Cowombat Siltstone||||||
27289|Gibsons Folly Formation|23030|5|Briefly described|Map legend|Late Silurian|Late Silurian|Parent is the Enano Group||||||
27289|Gibsons Folly Formation|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
27289|Gibsons Folly Formation|23309|5|Briefly described|p89-99.||Late Silurian|||||||
27289|Gibsons Folly Formation|23615|6|Mentioned|p78|Late Silurian|Silurian|Of Enano Group.||||||
27289|Gibsons Folly Formation|23938|5|Briefly described|p14 Tb. 1, p139 Tb.1 App.|Late Silurian|Middle Silurian|Of Enano Gp. Highly deformed unit but in places it conformably overlies Cowombat Siltstone. In the Limestone Creek Graben. See also p38-39 Tb. 2, p77.||||||
27289|Gibsons Folly Formation|24275|4|Described|p1695, p1698 Tb. 1|Late Silurian|Silurian|Of the Enano Group.  Mafic to felsic, subaqueous volcanic, shallow intrusive, hylaoclastic, volcaniclastic and epiclastic rocks hosted by fine-grained trubidites. Conformably overlies Cowombat Siltstone. Thickness: >500m. Geol.Prov: Lachlan Fold B.||||||24-JAN-06
27289|Gibsons Folly Formation|24551|4|Described|p135|Late Silurian|Late Silurian|Of Enano Group.||||||
27289|Gibsons Folly Formation|38145|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
27289|Gibsons Folly Formation|38151|6|Mentioned|Table 1|||||||||
27289|Gibsons Folly Formation|38367|6|Mentioned|Fig.1|||See also Fig.9||||||
27289|Gibsons Folly Formation|39447|2|Defined|p7|Silurian|Silurian|See also P25||||||
27289|Gibsons Folly Formation|39860|6|Mentioned|p10|||See also P41||||||
27289|Gibsons Folly Formation|40761|6|Mentioned|p227|||||||||
27289|Gibsons Folly Formation|41585|4|Described|p128|||||||||
27289|Gibsons Folly Formation|42791|5|Briefly described|p215|||see also Fig.10 P215||||||
27289|Gibsons Folly Formation|42827|4|Described|p128|||Of Enano Group.||||||25-SEP-08
27289|Gibsons Folly Formation|43128|5|Briefly described|Fig.6,p476||Late Silurian|||||||
27289|Gibsons Folly Formation|43770|5|Briefly described|p831|||||||||
27289|Gibsons Folly Formation|44092|5|Briefly described|map legend|Late Silurian|Late Silurian|Ss5||||||
27289|Gibsons Folly Formation|44184|5|Briefly described|Map Legend||Late Silurian|||||||
27289|Gibsons Folly Formation|44185|5|Briefly described|Map legend.|Late Silurian|Late Silurian|||Unit in Enano Group.|||Marine, extrusive, intrusive: siltstone, andesite.|
27289|Gibsons Folly Formation|60503|3|Fully described|p110, p30, p43 Tb. 2|Late Silurian|Late Silurian|Of the Enano Group. Comprises strongly foliated volcanics ranging from rhyolite to basalt and interbedded siltstone. Contains the Wilga deposit, and Currawong deposit. Conformably overlies Cowombat Siltstone. Max. thickness: 500m.||||||16-NOV-09
27289|Gibsons Folly Formation|60504|5|Briefly described|Map Legend|Pridoli|Pridoli|Of the Enano Group.||||||
27289|Gibsons Folly Formation|60505|5|Briefly described|Map legend|Pridoli|Pridoli|Of the Enano Group.||||||25-SEP-08
27289|Gibsons Folly Formation|60506|5|Briefly described|Map legend|Pridoli|Pridoli|Of the Enano Group.||||||
27289|Gibsons Folly Formation|60507|5|Briefly described|Map Legend|Pridoli|Pridoli|Of the Enano Group.||||||
27289|Gibsons Folly Formation|60508|5|Briefly described|Map legend|Late Silurian|Late Silurian|Of the Enano Group. Andesite, dacite, basalt, rhyolite, siltstone: weakly magnetic (20 nT) over dacite; low total count, K, Th, U, northwest trending moderate K bands.||||||
27289|Gibsons Folly Formation|61187|5|Briefly described|p24, p26 Fig.2, p28, p29 Fig.4. |Silurian|Silurian|NE-trending belt, minimum 500 m thick. Hosts Wilga and Currawong mineralisation. Radiometric response varies considerably along strike.||Unit in Enano Group.|||Interbedded siltstone and strongly foliated volcanics (rhyolite to basalt); local massive porphyritic rhyolite bodies.|
27289|Gibsons Folly Formation|66197|5|Briefly described|p635 Fig.5c|Late Silurian||Buchan Basin. Mixed mafic/silicic volcanics and clastics. Overlies the Cowombat Siltstone. Age: Pridoli?||||||14-MAR-12
27289|Gibsons Folly Formation|67802|5|Briefly described|p29||Late Silurian|Of the Limestone Creek Graben. Hosts the Wilga and Currawong seafloor volcanic-associated deposits.||||||
27289|Gibsons Folly Formation|68116|5|Briefly described|Appendix, Maps 27-28, 35.|Pridoli|Pridoli||||||Siltstone, minor sandstone, lavas: sandstone of mixed volcanic and non-volcanic provenance; lavas from stratiform lenses of andesite to dacite.|
7191|Giffard Sandstone Member|35273|4|Described|p258|||||||||
7191|Giffard Sandstone Member|42827|4|Described|p332|||of Lakes Entrance Formation||||||
7191|Giffard Sandstone Member|65717|6|Mentioned|p11|Oligocene|Oligocene|Onshore.||Lakes Entrance Formation||||05-SEP-17
7191|Giffard Sandstone Member|65718|6|Mentioned|p10 Fig 3.2, p12, p18, p43|Oligocene|Oligocene|See also Giffard Sandstone.||||Basal unit of the Lakes Entrance Formation.||10-JAN-17
7191|Giffard Sandstone Member|70076|5|Briefly described|Regional: Fig.3|Rupelian|Rupelian|||Lakes Entrance Formation.||Overlies Burong Formation. Is overlain by Seacombe Marl Member.||
7191|Giffard Sandstone Member|73289|5|Briefly described|p767, 770, 776|Oligocene|Oligocene|Lake Wellington, Seaspray Depressions, onshore Gippsland Basin. See also references to Giffard Sandstone (p765, 773, 775).||Lakes Entrance Formation.||||
7191|Giffard Sandstone Member|73488|6|Mentioned|p632 Fig.2|Rupelian|Rupelian|Gippsland Basin. See also Gifford Sandstone Member, Giffard Sandstone.||||||
30550|Gillingall Ignimbrite|23309|4|Described|p109.  Table 2.40|||Maximum Thickness: 150m.  Of the Little River Subgroup.||||||22-FEB-10
30550|Gillingall Ignimbrite|23615|3|Fully described|p119|Early Devonian|Early Devonian|Not related to "Gillingall Limestone" (Talent 1956).  Of Little River Subgroup.  Vitric-rich feldspar ignimbrite with minor quartz.  Unconformably overlies Windarra Formation.||||||
30550|Gillingall Ignimbrite|24551|5|Briefly described|p144|||Of Little River Subgroup.||||||
30550|Gillingall Ignimbrite|43206|5|Briefly described|map legend||Lochkovian|of Little River Subgroup.||||||
30550|Gillingall Ignimbrite|68116|5|Briefly described|Appendix.|Pragian|Lochkovian||||||Feldspar ignimbrite: green or pink matrix with feldspar (up to 6 mm) and wispy pumice.|
7269|Gippsland Limestone|13324|5|Briefly described|p94 Fig. 4|Miocene|Oligocene|Gippsland Basin.||Of Seaspray Group||||
7269|Gippsland Limestone|13332|5|Briefly described|p184 Fig.2|Pleistocene|Oligocene|Geological Province: Gippsland Basin.||||||
7269|Gippsland Limestone|13350|5|Briefly described|p94, p96 Fig.3|Pleistocene|Oligocene|Of the Seaspray Group. Geological Province: Gippsland Basin. See also p100 Fig.7||||||
7269|Gippsland Limestone|22663|5|Briefly described|V97 - G1 to G4 Fig.2|Miocene|Miocene|||||||01-MAR-10
7269|Gippsland Limestone|23230|5|Briefly described|Table4-1p40|||||||||
7269|Gippsland Limestone|23238|5|Briefly described|Fig10-3.3p108|Tertiary|Tertiary|||||||
7269|Gippsland Limestone|23264|6|Mentioned|Fig13-3.5p330|||||||||
7269|Gippsland Limestone|23372|4|Described|p251 Fig.3|Miocene|Oligocene|Equivalent to Torquay Group. Of Gippsland Basin.||||||12-FEB-08
7269|Gippsland Limestone|23768|5|Briefly described|p28 Fig.5|Early Miocene|Oligocene|Geological Province: Gippsland Basin.  See also p71, p82.||||||30-MAR-05
7269|Gippsland Limestone|23885|5|Briefly described|p163|Middle Miocene|Middle Miocene|Geological Province: Gippsland Basin.||||||
7269|Gippsland Limestone|23909|5|Briefly described|p290 Fig.3|Miocene|Miocene|Of Seaspray Group.  Geological Province: Gippsland Basin.||||||
7269|Gippsland Limestone|24038|5|Briefly described|p439 Fig.2|Miocene|Miocene|Geological Province: Gippsland Basin||||||
7269|Gippsland Limestone|24053|4|Described|p38|Miocene|Miocene|Of Seaspray Group.  Max. thickness: 781m.  Geological Basin: Gippsland Basin.||||||
7269|Gippsland Limestone|24054|4|Described|p46|||Geological Basin: Gippsland Basin.||||||
7269|Gippsland Limestone|24164|5|Briefly described|p13, p20 Fig.12, p29, p35, p43|Pleistocene|Oligocene|See also misspelt Gippsland Limestone Formation (p22 Fig.14).||Seaspray Group||||
7269|Gippsland Limestone|24211|5|Briefly described|p86 Fig. 3|Pleistocene|Oligocene|Geological Province: Gippsland Basin.  See also p85 Fig. 2 and p87 Fig. 4.||||||
7269|Gippsland Limestone|24403|6|Mentioned|p3|||Geological Province: Gippsland Basin.||||||
7269|Gippsland Limestone|24468|5|Briefly described|p405 Fig.2|Miocene|Miocene|Geological Province: Gippsland Basin. Of the Angler Subgroup||||||
7269|Gippsland Limestone|24551|5|Briefly described|p262 Fig. 9.29, p733 Table 17.3|Quaternary|Oligocene|Of the Seaspray Group.  Max thickness: 500m.||||||
7269|Gippsland Limestone|29591|5|Briefly described|p98|||||||||
7269|Gippsland Limestone|29650|6|Mentioned|p111|||||||||
7269|Gippsland Limestone|29721|6|Mentioned|p192|||||||||
7269|Gippsland Limestone|29736|6|Mentioned|Fig.2|||||||||
7269|Gippsland Limestone|30574|5|Briefly described|p14|||||||||
7269|Gippsland Limestone|30930|6|Mentioned|Map legend|Miocene|Miocene|||||||
7269|Gippsland Limestone|30933|6|Mentioned|Map legend|Miocene|Miocene|||||||
7269|Gippsland Limestone|30938|6|Mentioned|Map legend|Miocene|Miocene|||||||
7269|Gippsland Limestone|31159|6|Mentioned|p85|||See also P86, 87.||||||
7269|Gippsland Limestone|31351|6|Mentioned|p85|||Miocene||||||
7269|Gippsland Limestone|31480|4|Described|Fig. 3|||Oligocene - Miocene.||||||
7269|Gippsland Limestone|31508|6|Mentioned|Table 1|||Miocene||||||
7269|Gippsland Limestone|31627|6|Mentioned|p12|||||||||
7269|Gippsland Limestone|31646|6|Mentioned|Fig. 2|||||||||
7269|Gippsland Limestone|31922|6|Mentioned|Fig.2|||||||||
7269|Gippsland Limestone|32228|6|Mentioned|p28|||||||||
7269|Gippsland Limestone|32232|6|Mentioned|p20|||||||||
7269|Gippsland Limestone|32370|5|Briefly described|p9|||||||||
7269|Gippsland Limestone|32374|6|Mentioned|p16|||||||||
7269|Gippsland Limestone|32375|6|Mentioned|Table 1|||See also P7||||||
7269|Gippsland Limestone|32574|6|Mentioned|p78|||||||||
7269|Gippsland Limestone|32679|6|Mentioned|p94|||||||||
7269|Gippsland Limestone|33320|6|Mentioned|p57|||Miocene||||||
7269|Gippsland Limestone|33362|6|Mentioned|p112|||||||||
7269|Gippsland Limestone|33459|6|Mentioned|p14|||Refers ground water.||||||
7269|Gippsland Limestone|33460|6|Mentioned|p13|||Refers aquifers.||||||
7269|Gippsland Limestone|33929|6|Mentioned|p70|||See also P71 & 72.||||||
7269|Gippsland Limestone|34421|6|Mentioned|p259|||See also P261||||||
7269|Gippsland Limestone|34519|6|Mentioned|p46|||||||||
7269|Gippsland Limestone|34815|6|Mentioned|p20|||||||||
7269|Gippsland Limestone|34842|4|Described|p23|||||||||
7269|Gippsland Limestone|34843|4|Described|p10|||||||||
7269|Gippsland Limestone|34954|6|Mentioned|Fig.34|||Analysis Fig.33. See also Fig.35.||||||
7269|Gippsland Limestone|35067|6|Mentioned|Fig.3|||||||||
7269|Gippsland Limestone|35271|6|Mentioned|Fig.2|||||||||
7269|Gippsland Limestone|35273|3|Fully described|p259|||||||||
7269|Gippsland Limestone|35274|4|Described|p422|||||||||
7269|Gippsland Limestone|35285|5|Briefly described|p415|||||||||
7269|Gippsland Limestone|35573|6|Mentioned|Fig.3|||Chronostratigraphic section - Gippsland Basin||||||
7269|Gippsland Limestone|36331|6|Mentioned|Fig.1|||||||||
7269|Gippsland Limestone|36643|6|Mentioned|Fig.7|||||||||
7269|Gippsland Limestone|37127|6|Mentioned|p349|||||||||
7269|Gippsland Limestone|37330|6|Mentioned|p45|||See also Table 4.||||||
7269|Gippsland Limestone|37530|3|Fully described|p10|||||||||
7269|Gippsland Limestone|37783|6|Mentioned|Fig.12|||||||||
7269|Gippsland Limestone|38070|6|Mentioned|Fig.12|||Gippsland Basin||||||
7269|Gippsland Limestone|38313|6|Mentioned|Fig.2|||||||||
7269|Gippsland Limestone|38930|6|Mentioned|p59|||Also mentioned Fig.1||||||
7269|Gippsland Limestone|38973|6|Mentioned|Fig.2|||||||||
7269|Gippsland Limestone|40117|6|Mentioned|p53|||||||||
7269|Gippsland Limestone|40716|6|Mentioned|p67|||||||||
7269|Gippsland Limestone|41043|5|Briefly described|p97|||||||||
7269|Gippsland Limestone|41124|6|Mentioned|p255|||||||||
7269|Gippsland Limestone|41193|6|Mentioned|p315|||||||||
7269|Gippsland Limestone|41213|5|Briefly described|Fig.2|||||||||
7269|Gippsland Limestone|41227|6|Mentioned|p1|||||||||
7269|Gippsland Limestone|41231|6|Mentioned|p109|||||||||
7269|Gippsland Limestone|41282|6|Mentioned|p34|||||||||
7269|Gippsland Limestone|41534|5|Briefly described|p221|||||||||
7269|Gippsland Limestone|41537|6|Mentioned|Fig.2|||||||||
7269|Gippsland Limestone|41727|5|Briefly described|p433|||||||||
7269|Gippsland Limestone|41868|5|Briefly described|p576|||See also P550 and Fig.12.8a||||||
7269|Gippsland Limestone|42075|6|Mentioned|p252|||||||||
7269|Gippsland Limestone|42083|4|Described|Fig.9 P346|||||||||
7269|Gippsland Limestone|42184|6|Mentioned|Fig.2 P348|||||||||
7269|Gippsland Limestone|42311|5|Briefly described|Fig.2 P526|||||||||
7269|Gippsland Limestone|42371|6|Mentioned|p36|||||||||
7269|Gippsland Limestone|42635|5|Briefly described|p89|||||||||
7269|Gippsland Limestone|42648|6|Mentioned|p45|||||||||
7269|Gippsland Limestone|42649|6|Mentioned|p193|||||||||
7269|Gippsland Limestone|42827|4|Described|p343|||Of Seaspray Group||||||01-JUL-08
7269|Gippsland Limestone|43145|4|Described|p11||Miocene|Of Seaspray Group.||||||01-JUL-08
7269|Gippsland Limestone|43667|6|Mentioned|Fig.3,p12||Miocene|||||||
7269|Gippsland Limestone|44185|5|Briefly described|Map legend.|Miocene|Miocene||||||Marine: calcarenite, marl.|
7269|Gippsland Limestone|45128|6|Mentioned|Fig.42|||Correlation table of sediments containing Dromornithidae in Australia.||||||
7269|Gippsland Limestone|48631|5|Briefly described|p4,5,Pl.1 sh1||Miocene|(J55-11).||||||
7269|Gippsland Limestone|48636|14|Not recorded|p.1,14,17,18,19,60|||(J55-11/Sale).||||||
7269|Gippsland Limestone|60538|5|Briefly described|p473 Fig.12, 480, 483 Fig. 22|Oligocene|Eocene|Of the Seaspray Group. Geological Province: Gippsland Basin.||||||
7269|Gippsland Limestone|60542|5|Briefly described|p84|Tertiary|Tertiary|Of the Seaspray Group. Overlain by "Haunted Hill Gravel" (conformably to disconformably). ||||||
7269|Gippsland Limestone|60666|5|Briefly described|p15 (Fig.)|||Geological Province: Gippsland Basin.||||||
7269|Gippsland Limestone|61155|5|Briefly described|p4, p18|Late Miocene|Early Miocene|Of the Seaspray Group. Marls and limestones. Overlain by Tambo River Formation (onshore). Age: probably as young as Pliocene/Pleistocene? Thickness: 1500m. Geological Province: Gippsland Basin (SE onshore and offshore).||||||03-MAR-10
7269|Gippsland Limestone|61181|5|Briefly described|p133|Middle Miocene|Early Miocene|Includes the Wuk Wuk Marl and Bairnsdale Limestone Member. Thick sheet of bryozoal marl and limestone. Max. thickness: 500m.||||||20-DEC-07
7269|Gippsland Limestone|61212|5|Briefly described|p301 Fig. 2|Pleistocene|Miocene|Geological Province: Gippsland Basin.||||||
7269|Gippsland Limestone|61302|5|Briefly described|p12, p11 Fig.4|Miocene|Oligocene|Of the Seaspray Group. Consists of marls and calcarenite. Overlies the Lakes Entrance Formation. Max. thickness: 800m (offshore). Geological Province: Gippsland Basin.||||||02-JUN-06
7269|Gippsland Limestone|61323|5|Briefly described|p3 Fig. 3|Pleistocene|Oligocene|Geological Province: Gippsland Basin.||||||
7269|Gippsland Limestone|61336|5|Briefly described|p(iv) Fig. 4|Miocene|Miocene|Geological Province: Gippsland Basin. See also p(xi) Fig. 11.||||||07-FEB-11
7269|Gippsland Limestone|61469|5|Briefly described|p33|||Overlies Lakes Entrance Formation. Geological Province: Gippsland Basin.||||||
7269|Gippsland Limestone|62899|5|Briefly described|p37 Fig. 2|||Includes the Lindenow Sand Member. Geological province: Lakes Entrance Platform.||||||12-DEC-06
7269|Gippsland Limestone|63173|5|Briefly described|p342 Fig. 9.2|Recent|Early Miocene|Geological Province: Gippsland Basin, offshore.||||||07-FEB-11
7269|Gippsland Limestone|63739|5|Briefly described|p37 Fig. 2|||Overlies Lakes Entrance Formation. Geological province: Gippsland Basin.||||||01-JUL-08
7269|Gippsland Limestone|65717|5|Briefly described|p12, p17, p19-23, p34, p38; Appendix 3.|Miocene|Miocene|Thickness ranges from 500m (onshore) to over 1500m (offshore). MICP anlaysis results.||||Overlies Lakes Entrance Formation. Is overlain unconformably by Wuk Wuk Marl.|A thick sequence of marine carbonates: fossiliferous limestones, marly limestones and marls.|05-SEP-17
7269|Gippsland Limestone|65718|5|Briefly described|p10 Fig 3.2, p12, p19, pp22-25|Miocene|Miocene|Early to middle Miocene age.||Of the Seaspray Group.||Underlain by the Lakes Entrance Formation.||
7269|Gippsland Limestone|65973|5|Briefly described|p17, p57, p62, p65, p71, p74|Miocene|Miocene|Gippsland Basin. Geophysical response is discussed briefly. Intersected in Kipper-1,  Judith-1, Hammerhead-1, East Pilchard-1, Longtom-1, Longtom-1/ST-1, Northright-1, Sole-1, Sweep-1 and many more drillholes (see appendix). See also p76-78, p80, p82, p85, p104, p108, p112, p116, p118.||Seaspray Group||Overlies the Lakes Entrance Formation.|Limestone.|
7269|Gippsland Limestone|68116|5|Briefly described|Appendix, Maps 52-53.|Miocene|Miocene||||||Calcarenite, marl.|
7269|Gippsland Limestone|69016|5|Briefly described|p88-89|||Of the Gippsland Basin. Marls act as aquitards, while fracture limestone acts as aquifers.||Unit of Seaspray Group.||Laterally grades into upper unit of Balook Formation.|Marine marl and carbonate units.|
7269|Gippsland Limestone|70028|6|Mentioned|p79-80, 82|Miocene|Oligocene|||||Overlies Lakes Entrance Formation.|A thick sequence of prograding marly limestones.|
7269|Gippsland Limestone|70076|5|Briefly described|Regional: Fig.3; p3|Pliocene|Miocene|Provided the critical loading for source rocks in Latrobe and Strzelecki Groups.||Seaspray Group.|Glencoe Limestone Member.|Overlies Lakes Entrance Formation.|Thick limestone.|
7269|Gippsland Limestone|73471|5|Briefly described|p86|||Gippsland Basin. Overlies Latrobe Unconformity. See also Gippsland Limestone Subgroup p87.||Seaspray Group||Overlies Gurnard Formation, Burong Formation, Lakes Entrance Formation|Marls and marine carbonates.|
7269|Gippsland Limestone|73488|5|Briefly described|p631-632, p633 Fig.3, p634 Fig.4, p636|Miocene|Miocene|See also Gippsland Limestone Formation.||Seaspray Group||Overlies Lakes Entrance Formation||
7269|Gippsland Limestone|73562|5|Briefly described|p303-304|Pleistocene|Miocene|Gippsland Basin; onshore.||Seaspray Group.||Overlies Lakes Entrance Formation. Onshore equivalents include Morwell and Yallourn Formations, upper part of Balook Formation, Wuk Wuk Marl Member, and Bairnsdale Limestone.|Fossiliferous limestone and marl.|
7269|Gippsland Limestone|75065|5|Briefly described|p151, 154, 170|Quaternary|Oligocene|Gippsland Basin; offshore.||Seaspray Group.||Overlies Lakes Entrance Formation.|Shallow-marine carbonates.|
28574|Girringurrup basalt|34988|5|Briefly described|p293|||||||||
28574|Girringurrup basalt|41848|6|Mentioned|p368|||Probably Pleistocene to Holocene age||||||
7299|Gisborne basalt|33153|6|Mentioned|p96|||||||||
7299|Gisborne basalt|70999|6|Mentioned|p169|||Mineralogy, affinities.Shown as Gisborne Basalt p166 Fig1.||||||03-MAY-17
24287|Glen Creek Lithic Sandstone|24096|6|Mentioned|p6|Devonian|Devonian|||||||
24287|Glen Creek Lithic Sandstone|36389|2|Defined|p41|Devonian|Devonian|Prob. Devonian||||||
24287|Glen Creek Lithic Sandstone|75072|6|Mentioned|p232|Early Devonian|Early Devonian|||||||
30436|Glen Hills Sandstone Member|23309|5|Briefly described|p78|||Maximum Thickness: 350m.  Of the Silverband Formation.||||||
30436|Glen Hills Sandstone Member|44929|5|Briefly described|Map Legend|Silurian|Ordovician|Of Silverband Formation. Purplish, fine- to medium-grained quartzo-micaceous sandstone.||||||14-JUN-06
30436|Glen Hills Sandstone Member|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Silverband Formation (Grampians Group). Sandstone, purplish, fine- to medium-grained, quartzo-micaceous.||||||13-JUN-06
30436|Glen Hills Sandstone Member|44932|5|Briefly described|Map Legend|Silurian|Ordovician|Of Silverband Formation. Purplish, fine- to medium-grained quartzo-micaceous sandstone.||||||14-JUN-06
30436|Glen Hills Sandstone Member|44933|5|Briefly described|Map Legend|Silurian|Ordovician|Of Silverband Formation. Purplish, fine- to medium-grained quartzo-micaceous sandstone.||||||14-JUN-06
30436|Glen Hills Sandstone Member|60451|4|Described|p77 Fig. 47, 81, 137|Early Devonian|Ordovician|Of the Silverband Formation (Grampians Group). Type section in text. Maximum Thickness: ~350m.||||||
30436|Glen Hills Sandstone Member|60456|5|Briefly described|Map Legend|Silurian|Ordovician|Sandstone: purplish, fine to medium grained, quartzo-micaceous; with planar, cross and trough cross lamination, thin to thickly bedded.||||||
30436|Glen Hills Sandstone Member|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Sandstone, purplish, fine to medium grained, quartzo-micaceous; with planar, cross and trough cross lamination, thin to thickly bedded.||||||
30436|Glen Hills Sandstone Member|61183|4|Described|p42-43, p55|||Of Silverband Formation. Multiply stacked, upward-fining and -thinning sandstone packages, each capped with red bed mudstone. Quartz sandstone: abundant mica, minor feldspar. Thickness: ~350m. See also Glen Hills sandstone member and Glen Hills Sandstone.||||||
30436|Glen Hills Sandstone Member|64541|5|Briefly described|Map Legend|Silurian|Ordovician|Sandstone: purplish, fine to medium grained, quartzo-micaceous; laminated, cross-laminated and trough cross-laminated, thin to thickly bedded; minor interbeds of red micaceous mudstone.||||||07-FEB-11
30436|Glen Hills Sandstone Member|64610|5|Briefly described|Map legend|Ordovician|Ordovician|Of Silverband Formation (Grampians Gp). Sandstone: purplish, fine- to medium-gr., quartzo-micaceous; laminated, x-laminated and trough x-laminated; thin to thickly bedded; minor interbeds of red micaceous mudst. capping stacked packages, etc. More details||||||
30436|Glen Hills Sandstone Member|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Silverband Formation. Defined by Cayley & Taylor, 1997. ||||||
21860|Glen Shiel Ignimbrite|23309|4|Described|p110 Table 2.40|||Maximum Thickness: 200m.  Of the Marroo Subgroup.||||||
21860|Glen Shiel Ignimbrite|23615|4|Described|p23, p100|Early Devonian|Early Devonian|Of Marroo Subgroup.  Overlies Statham Ignimbrite.  Maximum thickness: 200m.  Grey-green ignimbrite with a bimodal quartz phenocryst population.  Age:410-395Ma.||||||
21860|Glen Shiel Ignimbrite|24551|6|Mentioned|p144|||||||||
21860|Glen Shiel Ignimbrite|43206|5|Briefly described|map legend||Ludlow|Of Marroo Subgroup||||||
21860|Glen Shiel Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Quartz-feldspar ignimbrite with bimodal quartz and small feldspar phenocrysts.|
32492|Glenaroua Microgranite|22885|5|Briefly described|map|||||||||
32492|Glenaroua Microgranite|23309|6|Mentioned|p431 App1|||G287 S-Type.||||||
32492|Glenaroua Microgranite|44197|5|Briefly described|Map Legend||Late Devonian|G287 S-Type.||||||
32492|Glenaroua Microgranite|68116|5|Briefly described|Appendix, Map 32.|Late Devonian|Late Devonian||||||Porphyritic biotite microgranite with phenocrysts of quartz, orthoclase, oligoclase and biotite in a fine grained groundmass of the same minerals; S-type.|
27781|Glenaulin Clay Member|24551|6|Mentioned|p582|||||||||
27781|Glenaulin Clay Member|30184|6|Mentioned|p173|||||||||
27781|Glenaulin Clay Member|31624|4|Described|p112|||See also P119||||||
27781|Glenaulin Clay Member|31625|6|Mentioned|Fig. 5.2|||Oligocene||||||
27781|Glenaulin Clay Member|35066|5|Briefly described|p211|||||||||
27781|Glenaulin Clay Member|42827|5|Briefly described|p285|||||||||
7361|Glenbog Suite|22606|6|Mentioned|P831|||||||||
7361|Glenbog Suite|22719|6|Mentioned|p486|||||||||
7361|Glenbog Suite|22778|4|Described|p 163|||||||||
7361|Glenbog Suite|22815|5|Briefly described|p75, fig 25|||||||||
7361|Glenbog Suite|22876|4|Described|p25|||||||||
7361|Glenbog Suite|22878|6|Mentioned|p57 Table 7|||||||||
7361|Glenbog Suite|23309|5|Briefly described|p345|||||||||
7361|Glenbog Suite|23439|5|Briefly described|p124 fig.1|||||||||
7361|Glenbog Suite|23549|4|Described|p520-521|||Of Glenbog Supersuite. Comprises 12 putons. Mineral assemblage is: quartz, plagioclase, K-feldspar, sepia-brown biotite, hornblende and minor magnetite, ilmenite and allanite; titanite is absent. Geological Province: Bega Batholith.  See also Fig 4 p518.||||||04-DEC-15
7361|Glenbog Suite|23551|5|Briefly described|p495|||I-Type Granite. of Bega Batholith.||||||
7361|Glenbog Suite|24222|5|Briefly described|p9, p17|||Chemistry of samples reported. Comrpises 12 separate plutons. See also Glenbog Supersuite.  Geological Province: Bega Batholith, Lachlan Fold Belt.||||||
7361|Glenbog Suite|24514|5|Briefly described|p33|||I-type granites. Geological Province: Lachlan Fold Belt.||||||
7361|Glenbog Suite|24551|6|Mentioned|p235|||||||||
7361|Glenbog Suite|38822|6|Mentioned|p198|||||||||
7361|Glenbog Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
7361|Glenbog Suite|42827|6|Mentioned|p428|||||||||
7361|Glenbog Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
7361|Glenbog Suite|44093|5|Briefly described|p218 App. 1|Early Devonian|Early Devonian|Orogenic granite. Geological Province: Lachlan Fold Belt.||||||
7361|Glenbog Suite|60423|6|Mentioned|p374|||Geological Province: Lachlan Fold Belt. Of the Bega Batholith||||||
7361|Glenbog Suite|64571|6|Mentioned|p834|||||||||
7361|Glenbog Suite|66300|6|Mentioned|p41, 46.||||||Includes Boro Granite.|||29-OCT-13
7361|Glenbog Suite|68592|3|Fully described|p74 Tb.5, p1674-81|Early Devonian|Early Devonian|Glenbog Granodiorite (Chappell et al. 1987) is the type pluton: E of Nimmitabel. Named after nearby Glenbog State Forest. Called Lake Bathurst Suite by Chappell et al. (1991). Low Sr values. Goulburn structural zone: deformation described.||Unit in Glenbog Supersuite.|Includes Bundong, Ballallaba, Boro Granites; Glenbog, Yalgatta, Towamba, Frogs Hollow, Anembo Granodiorites; Nimmitabel, Towneys Creek and Cannabul Adamellites.|Intrudes Abercrombie Formation, Bendoc and Margules Groups, Covan Creek Formation and Long Flat Volcanics.|Granite, granodiorite, monzogranite.|
7361|Glenbog Suite|69159|5|Briefly described|Map legend|Pragian|Pragian||||Includes Bundong, Mullens, Boro and Ballallaba Granites.|||07-SEP-15
7361|Glenbog Suite|69270|5|Briefly described|p1, p15-16, p20, p23, p30, p34|Early Devonian|Early Devonian|Chappell et al. (1991) assigned Anembo Granodiorite to Glenbog Suite, an interpretation supported by the fact that this new magmatic crystallisation age is indistinguishable from that of the only other dated unit within the suite: ~412 Ma Boro Granite (Bodorkos and Simpson, 2008).||Glenbog Supersuite|Anembo Granodiorite, Towneys Creek Monzogranite, Glenbog Granite and Boro Granite|||
7361|Glenbog Suite|69876|5|Briefly described|p316|||Australian mainland. Discussed in relation to mafic enclaves and restite model.|||||I-type granite.|
7361|Glenbog Suite|70192|5|Briefly described|Map Legend|Pragian|Pragian|On Goulburn 1:100 000 mapsheet portion of Time-Space Plot.|||Includes Bundong Granite.|||
7361|Glenbog Suite|70542|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Bundong Granite|||
7361|Glenbog Suite|71069|5|Briefly described|p9, p26 fig 9, p28, p29, p40 fig 17, p42|Early Devonian|Early Devonian||||Includes the Anembo Granodiorite, Boro Granite and the Bundong Granite|Overlain by the Hoskinstown Group.|Granites.|
7361|Glenbog Suite|71699|5|Briefly described|Map legend.|Devonian|Devonian||||Boro, Ballallaba, Mullens, Bundong Granites.|||
7361|Glenbog Suite|71700|2|Defined|viii, ix, p7, p26, p28, CD|Early Devonian|Early Devonian|Named for the Glenbog Granodiorite which is also the type pluton for this suite. Chappell et al. (1991) used the invalid name"Lake Bathurst Suite" which included a single pluton, the"Lake Bathurst Granite". This pluton is now regarded as Bundong Granite (Dgo) and is included in the Glenbog Suite (Thomas & Pogson 2012). the Glenbog Suite also includes the Glenbog Granodiorite, Yalgatta Granodiorite, Towamba Granodiorite, Frogs Hollow Granodiorite, Anembo Granodiorite, Nimmitabel Adamellite, Towneys Creek Adamellite and Cannabul Adamellite. See also p36-p38, p41, p44, p50, p57, p65-p66, p76, p80-p81, p85. Distribution, geomorphic expression, outcrop,  structure, metamorphism, geochemistry, geophysical characteristics, distinguishing features and economic geology are discussed.||Glenbog Supersuite|Includes the Ballallaba Granite, Boro Granite, Bundong Granite and the Mullens Granite.|Faulted against the Thurralilly Suite and Braidwood Suite.|Granitoids containing quartz, plagioclase, K-feldspar, biotite, hornblende and minor magnetite, ilmenite and allanite.|
7362|Glenbog Supersuite|22876|6|Mentioned|p23 Table 4|||||||||
7362|Glenbog Supersuite|22877|5|Briefly described|map|Silurian|Silurian|||||||
7362|Glenbog Supersuite|22878|4|Described|p57|||||||||
7362|Glenbog Supersuite|22879|5|Briefly described|map|Early Devonian|Early Devonian|||||||
7362|Glenbog Supersuite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Blue Gum Tonalite, Buldah Gap Granodiorite, Weeragua Granodiorite, Cann Mountain Granite, Whitegum Tonalite, Fiddlers Green Granite, Archie Granodiorite, Coopracambra Tonalite||||||01-OCT-04
7362|Glenbog Supersuite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||06-OCT-04
7362|Glenbog Supersuite|23549|4|Described|p520|||Occurs along the western side of the Bega Batholith. Includes the Blue Gum and Glenbog Suites.||||||05-APR-05
7362|Glenbog Supersuite|24222|6|Mentioned|p14|||See also Glenbog Suite.  Geological Province: Lachlan Fold Belt.||||||
7362|Glenbog Supersuite|24551|5|Briefly described|p235|||Includes the Blue Gum and Glenbog suites.||||||
7362|Glenbog Supersuite|42627|5|Briefly described|Map legend|Wenlock|Wenlock|Variation on Glenbog Suite?||||||
7362|Glenbog Supersuite|42726|5|Briefly described|map legend|||||||||
7362|Glenbog Supersuite|42827|5|Briefly described|p429|||||||||
7362|Glenbog Supersuite|60541|6|Mentioned|p64|||Includes Blue Gums Tonalite. Watchmaker Granodiorite may be associated with this supersuite because of its similarity to the Blue Gums Tonalite. Geological Province: Lachlan Fold Belt.||||||20-JUN-05
7362|Glenbog Supersuite|68592|5|Briefly described|p24, p1674-81|Early Devonian|Early Devonian|First mapped and described by Beams (1980), and decribed by Douglas and Ferguson (1988). Named after Glenbog Granodiorite (Chappell et al. 1987). A north-trending belt 300 x 15 km forming the westernmost part of the Bega Batholith. Unfractionated I-type.|||Includes Badja, Blue Gum, Cathcart, Glenbog and Myocum Suites (NSW); and Archie Granodiorite with Blue Gums, Coopracambra and Whitegum Tonalites (Vic).|||
7362|Glenbog Supersuite|69270|6|Mentioned|p15||||||Glenbog Suite|||
7362|Glenbog Supersuite|71700|2|Defined|vi, CD|||Named for the Glenbog Granodiorite which is also the type pluton for this supersuite. See Glenbog Suite for further information regarding distribution, geomorphic expression, outcrop, depositional environment, lithology, structure, metamorphism, geochemistry, geophysical characteristics, unit relationships, age, distinguishing features and economic geology.|||Includes the Glenbog Suite, Badja Suite, Cathcart Suite, Myocum Suite, Archie Granodiorite, Blue Gum Suite, Blue Gums Tonalite, Coopracambra Tonalite and Whitegum Tonalite.|||
7370|Glencoe Limestone Member|24551|5|Briefly described|p327 Fig. 10.33|Miocene|Miocene|||||||
7370|Glencoe Limestone Member|31351|6|Mentioned|p85|||Rock unit of local significance only. New name Glencoe Limestone Tongue.||||||09-MAY-07
7370|Glencoe Limestone Member|35273|5|Briefly described|p260|||||||||
7370|Glencoe Limestone Member|42635|5|Briefly described|p89|||Of the Gippsland Limestone.||||||09-MAY-07
7370|Glencoe Limestone Member|42827|5|Briefly described|p334|||||||||
7370|Glencoe Limestone Member|65718|6|Mentioned|p10 Fig 3.2|Miocene|Miocene|Early to middle Miocene age.||||||
7370|Glencoe Limestone Member|70076|5|Briefly described|Regional: Fig.3|Langhian|Burdigalian|||Gippsland Limestone.||Overlies Longford Limestone. Is overlain by Wuk Wuk Marl.||
41186|Glendara Granite|50154|2|Defined|p88-89, p247 App.5|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex. Intruded by Barrama Microgranite.||||||25-SEP-09
41186|Glendara Granite|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Muscovite-biotite granite||||||
41186|Glendara Granite|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite||||||25-AUG-04
41186|Glendara Granite|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite||||||25-AUG-04
41186|Glendara Granite|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite||||||25-AUG-04
41186|Glendara Granite|50159|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite||||||25-AUG-04
41186|Glendara Granite|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Overlain by Lowan Sand. Muscovite-biotite granite.||||||25-AUG-04
41186|Glendara Granite|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite||||||25-AUG-04
41186|Glendara Granite|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite||||||25-AUG-04
41186|Glendara Granite|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite||||||25-AUG-04
41186|Glendara Granite|50164|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Muscovite-biotite granite.||||||
41186|Glendara Granite|66002|5|Briefly described|p9 Tb.5|||G448. Called Glendara Adamellite by Kemp et al. (2002)||||||
41186|Glendara Granite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Muscovite-biotite granite: massive, cream coloured, coarse grained, porphyritic with phenocrysts of alkali feldspar; accessory magnetite; rare mafic biotite-rich microgranitoid enclaves; magnetic to non-magnetic.|
7378|Glendart Granite|23309|6|Mentioned|p448 App1|||Obsolete granite name.||||||
7378|Glendart Granite|39860|6|Mentioned|p18|||||||||
7378|Glendart Granite|42726|5|Briefly described|map legend|||||||||
7378|Glendart Granite|44184|5|Briefly described|Map Legend||Early Silurian|Shown as Glendart Unassigned.||||||
30451|Glendinning Ignimbrite|23309|5|Briefly described|p83. Table 2.28|||||||||
30451|Glendinning Ignimbrite|44929|5|Briefly described|Map Legend||Early Devonian|Of Rocklands Volcanics.  Quartz-feldspar ignimbrite, dark brown with sparse crystals up to 2mm.||||||14-JUN-06
30451|Glendinning Ignimbrite|44930|5|Briefly described|Map Legend||Early Devonian|Of Rocklands Volcanics.  Quartz-feldspar ignimbrite, dark brown with sparse crystals up to 2mm.||||||14-JUN-06
30451|Glendinning Ignimbrite|44931|6|Mentioned|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanics.||||||14-JUN-06
30451|Glendinning Ignimbrite|44932|5|Briefly described|Map Legend||Early Devonian|Of Rocklands Volcanics.  Quartz-feldspar ignimbrite, dark brown with sparse crystals up to 2mm.||||||14-JUN-06
30451|Glendinning Ignimbrite|44933|5|Briefly described|Map Legend||Early Devonian|Of Rocklands Volcanics.  Quartz-feldspar ignimbrite, dark brown with sparse crystals up to 2mm.||||||25-JUL-06
30451|Glendinning Ignimbrite|50154|2|Defined|p118, p245 App.5|Devonian|Devonian|Of the Rocklands Volcanic Group. Contains clasts of Mooralla Ignimbrite. Max. thickness: 35-40m.||||||15-SEP-04
30451|Glendinning Ignimbrite|50155|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Quartz-feldspar ignimbrite||||||
30451|Glendinning Ignimbrite|50156|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: dark brown with sparse crystals up to 2mm; abundant lithics of Rocklands Volcanics up to 25cm at base; pumice rich at top; eutaxitic texture; fiamme; localised haematite-sericite alteration||||||17-MAY-13
30451|Glendinning Ignimbrite|50157|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: dark brown with sparse crystals up to 2mm; abundant lithics of Rocklands Volcanics up to 25cm at base; pumice rich at top; eutaxitic texture; fiamme; localised haematite-sericite alteration||||||17-MAY-13
30451|Glendinning Ignimbrite|50158|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: dark brown with sparse crystals up to 2mm; abundant lithics of Rocklands Volcanics up to 25cm at base; pumice rich at top; eutaxitic texture; fiamme; localised haematite-sericite alteration||||||17-MAY-13
30451|Glendinning Ignimbrite|50159|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: dark brown with sparse crystals upto 2mm; abundant lithics of Rocklands Volcanics upto 25cm at base; pumice rich at top; eutaxitic texture; fiamme; localised haematite-sericite alteration||||||24-JUN-04
30451|Glendinning Ignimbrite|50160|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz-feldspar ignimbrite||||||
30451|Glendinning Ignimbrite|50161|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: dark brown with sparse crystals upto 2mm; abundant lithics of Rocklands Volcanics upto 25cm at base; pumice rich at top; eutaxitic texture; fiamme; localised haematite-sericite alteration||||||24-JUN-04
30451|Glendinning Ignimbrite|50162|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: dark brown with sparse crystals upto 2mm; abundant lithics of Rocklands Volcanics upto 25cm at base; pumice rich at top; eutaxitic texture; fiamme; localised haematite-sericite alteration||||||24-JUN-04
30451|Glendinning Ignimbrite|50163|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: dark brown with sparse crystals upto 2mm; abundant lithics of Rocklands Volcanics upto 25cm at base; pumice rich at top; eutaxitic texture; fiamme; localised haematite-sericite alteration||||||24-JUN-04
30451|Glendinning Ignimbrite|61183|3|Fully described|p64-65, p124|Early Devonian|Early Devonian|Of Rocklands Volcanics Group. Two flow units, densely welded, an upper and a lower unit. Dark brown pumice- and vitric-rich rock containing up to 5% phenocrysts of quartz, and altered feldspar. Contains clasts of Mooralla Ignimbrite. Max. thickness: 40m. ||||||
30451|Glendinning Ignimbrite|64541|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanics. Quartz-feldspar ignimbrite.||||||07-FEB-11
30451|Glendinning Ignimbrite|64610|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Rocklands Volcanics. Quartz feldspar ignimbrite: dk brown+sparse crystals up to 2mm; abundant lithics of Rocklands Volcs. up to 25cm at base, pumice-rich at top; eutaxitic texture partly  devitrified, fiamme often attentuated to rheomorphic flow, etc.||||||
30451|Glendinning Ignimbrite|66002|5|Briefly described|p6 Tb.4|Devonian|Devonian|Of Rocklands Volcanic Group. Defined in Simpson 1997, p64.||||||
7400|Glenelg River Metamorphic Complex|22628|6|Mentioned|p109,p112|||||||||
7400|Glenelg River Metamorphic Complex|22708|6|Mentioned|p207|||||||||
7400|Glenelg River Metamorphic Complex|23309|5|Briefly described|p45-51, 335-337|||||||||
7400|Glenelg River Metamorphic Complex|23417|6|Mentioned|p6 Fig.4||Late Cambrian|||||||
7400|Glenelg River Metamorphic Complex|24551|6|Mentioned|p52 Fig. 2.66|||||||||
7400|Glenelg River Metamorphic Complex|33602|6|Mentioned|Table 1|||||||||
7400|Glenelg River Metamorphic Complex|35112|6|Mentioned|Table.1|||||||||
7400|Glenelg River Metamorphic Complex|35281|6|Mentioned|p18|||||||||
7400|Glenelg River Metamorphic Complex|37501|6|Mentioned|p397|||||||||
7400|Glenelg River Metamorphic Complex|41571|5|Briefly described|p37|||see also Fig 2.1||||||
7400|Glenelg River Metamorphic Complex|43218|5|Briefly described|p21|Cambrian|Precambrian|Metamorphosed Glenelg River beds.||||||
7400|Glenelg River Metamorphic Complex|50154|2|Defined|p17, p66|Late Cambrian|Late Cambrian|Geological Province: Delamerian Fold Belt. Supersedes the Glenelg River Complex.||||||15-SEP-04
7400|Glenelg River Metamorphic Complex|50155|5|Briefly described|Map Legend|Late Cambrian|Early Cambrian|Overlain by Nigretta and Gatum Ignimbrites. Metamorphic: Biotite phyllite and schist, gneiss and migmatite grading into various granite and pegmatite phases, quartzofeldspathic schist with pegmatite pods, calc-silicate||||||25-JUN-04
7400|Glenelg River Metamorphic Complex|50156|5|Briefly described|Map Legend|Late Cambrian|Early Cambrian|||||||
7400|Glenelg River Metamorphic Complex|50157|5|Briefly described|Map Legend|Late Cambrian|Early Cambrian|||||||
7400|Glenelg River Metamorphic Complex|50158|5|Briefly described|Map Legend|Late Cambrian|Early Cambrian|Of Moralana Supergroup||||||
7400|Glenelg River Metamorphic Complex|50159|5|Briefly described|Map Legend|Late Cambrian|Early Cambrian|Of Moralana Supergroup||||||
7400|Glenelg River Metamorphic Complex|50160|5|Briefly described|Map Legend|Late Cambrian|Early Cambrian|Of Moralana Supergroup. Overlain by Hypatia Formation, Bacchus Marsh Formation, Duddo Limestone and Parilla Sand.||||||25-JUN-04
7400|Glenelg River Metamorphic Complex|50161|5|Briefly described|Map Legend|Late Cambrian|Early Cambrian|Of Moralana Supergroup. Overlain by Bacchus Marsh Formation and  Den Hills Formation||||||25-JUN-04
7400|Glenelg River Metamorphic Complex|50162|5|Briefly described|Map Legend|Late Cambrian|Early Cambrian|Of Moralana Supergroup||||||22-JUN-04
7400|Glenelg River Metamorphic Complex|50163|5|Briefly described|Map Legend|Late Cambrian|Early Cambrian|Of Moralana Supergroup. Overlain by Duddo Limestone||||||25-JUN-04
7400|Glenelg River Metamorphic Complex|50164|5|Briefly described|Map Legend|||Of Moralana Supergroup.||||||16-JUN-04
7400|Glenelg River Metamorphic Complex|60421|5|Briefly described|p415|||Overlain by the Loxton-Parilla Sands.||||||
7400|Glenelg River Metamorphic Complex|60451|6|Mentioned|p20|||Geological Province: Delarmerian Fold Belt.||||||
7400|Glenelg River Metamorphic Complex|61163|6|Mentioned|p126|||||||||
7400|Glenelg River Metamorphic Complex|61181|5|Briefly described|p189, p196|||Includes biotite schist and almandine biotite schist which locally contain staurolite and andalusite. ||||||
7400|Glenelg River Metamorphic Complex|62742|5|Briefly described|p700|||Ranges from biotite to sillimanite grade. In western Victoria.||||||
7400|Glenelg River Metamorphic Complex|64571|6|Mentioned|p824|||||||||
7400|Glenelg River Metamorphic Complex|65716|5|Briefly described|p4|Cambrian|Cambrian|In Glenelg Zone. Have a 500-600 ma detrital zircon peak age similar to Moralana Supergroup rocks enclosing Truro Volcanics.||||||
7400|Glenelg River Metamorphic Complex|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Moralana Supergroup. Called Glenelg River Complex by Wells (1956)||||||
7400|Glenelg River Metamorphic Complex|66286|6|Mentioned|p189.|||Source material in Dundas Tableland for fluvial sediments of Loddon River Group.||||||
7400|Glenelg River Metamorphic Complex|67104|6|Mentioned|p633, p636, p637 Fig.4|||Region of high Cambrian heat flow.||||||
7400|Glenelg River Metamorphic Complex|68116|5|Briefly described|Appendix, Maps 29, 38.|Early Ordovician|Middle Cambrian|Informally subdivided into biotite granite, leucogranite, and migmatite phases. Migmatite grades into various granite and pegmatite phases. Biotite granite: non-magnetic.|||||Biotite granite: massive to foliated, medium to coarse grained, equigranular, muscovite-bearing. Leucogranite: garnet-bearing varieties and pegmatite. Migmatite: layered to nebulitic gneiss with dark biotite-rich layers and pale granitic layers. |
7400|Glenelg River Metamorphic Complex|70493|5|Briefly described|p63|Cambrian|Cambrian|Western Victoria, Lachlan Orogen. A possible source of some sediment in the Adaminaby Group. See also references to Glenelg River Complex (p54, p55 Fig.2, p63).||||Juxtaposed (?faulted) against the Mount Stavely Volcanic Complex.|Low grade, deformed and metamorphosed rocks.|
7400|Glenelg River Metamorphic Complex|70967|6|Mentioned|p17-18|||Glenelg Zone. High-grade metamorphic rocks.||||||
7400|Glenelg River Metamorphic Complex|71593|4|Described|p8, p12, p19-p20, p22-p23|||Glenelg Zone extending northwest beneath the Murray Basin before emerging in Palmer-Springton region of South Australia. See also  p64, p72-p73, p102, p133, p178.||||Faulted against the Nargoon Group, Glenthompson Sandstone and the Mount Stavely Volcanic Complex.|Pelitic, quartzo-feldspathic and psammitic schist, calc-silicate, amphibolite, talc schist and migmatite and diatexite.|
7400|Glenelg River Metamorphic Complex|72445|6|Mentioned|p17.||||||||High-grade metamorphic rocks.|
7400|Glenelg River Metamorphic Complex|73118|5|Briefly described|p15|||Glenelg Zone, Western Victoria.|||||Multiply deformed amphibolite facies schist and gneiss; openly folded greenschist facies greywacke, slate and dolomitic limestone.|
41962|Glenelg Suite|60544|6|Mentioned|Map legend|||Age: 520-500Ma (U/Pb zircon) and 500-480Ma (K/Ar).||||||
41189|Glengoyne Granite|50154|2|Defined|p97, p247 App.5|Cambrian|Cambrian|Of the Glenelg Metamorphic Complex.||||||25-SEP-09
41189|Glengoyne Granite|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Muscovite-garnet leucogranite; S-type||||||
41189|Glengoyne Granite|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite-garnet leucogranodiorite||||||20-AUG-04
41189|Glengoyne Granite|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite-garnet leucogranodiorite||||||20-AUG-04
41189|Glengoyne Granite|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite-garnet leucogranodiorite||||||20-AUG-04
41189|Glengoyne Granite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite-garnet leucogranodiorite||||||20-AUG-04
41189|Glengoyne Granite|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite-garnet leucogranodiorite||||||20-AUG-04
41189|Glengoyne Granite|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite-garnet leucogranodiorite||||||20-AUG-04
41189|Glengoyne Granite|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite-garnet leucogranodiorite||||||20-AUG-04
41189|Glengoyne Granite|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite-garnet leucogranodiorite||||||20-AUG-04
41189|Glengoyne Granite|66002|5|Briefly described|p9 Tb.5|||G446. Called Glengoyne Adamellite by Kemp et al. (2002)||||||
41189|Glengoyne Granite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Muscovite-garnet leucogranite: massive, white, fine to medium grained, porphyritic with microcline megacrysts and rare biotite; pegmatite, aplite and microgranite phases occur; non-magnetic.|
25014|Glenlogie Granodiorite|22756|5|Briefly described|P40, P46, Table2||Early Devonian|||||||
25014|Glenlogie Granodiorite|23309|5|Briefly described|p431 App1|Middle Devonian|Early Devonian|G372 I-Type. Age: 393 +/- 14Ma, 394 +/- 5 Ma,  397 +/- 6 Ma.  Supersedes Glenlogie Granite.||||||
25014|Glenlogie Granodiorite|41850|6|Mentioned|p437|||||||||
25014|Glenlogie Granodiorite|43260|5|Briefly described|Map Legend||Early Devonian|Of the Glenlogie Suite. Hornblende-biotite granodiorite: mafic; speckled grey; medium to coarse grained. Strongly kaolinised in places, with limonite and goethite staining.||||||27-OCT-04
25014|Glenlogie Granodiorite|44186|5|Briefly described|Map Legend||Early Devonian|G372 I-type.||||||
25014|Glenlogie Granodiorite|66002|5|Briefly described|p7 Tb.5|||Of Glenlogie Suite. G372.  Defined by Cayley and McDonald 1995.||||||
25014|Glenlogie Granodiorite|67978|6|Mentioned|p496 Fig.1, p499 Tb.1||||399 +/- 8 Ma (SIMS U-Pb; Black, unpub.).|||||19-SEP-14
25014|Glenlogie Granodiorite|68116|5|Briefly described|Appendix, Map 31.|Early Devonian|Early Devonian||||||Hornblende-biotite granodiorite: mafic; speckled grey; medium to coarse grained; strongly kaolinised in places, with limonite and goethite staining.|
7426|Glenlogie Suite|22756|5|Briefly described|P45|||||||||
7426|Glenlogie Suite|24551|5|Briefly described|p226|||Of the Stawell Province.||||||
7426|Glenlogie Suite|41563|6|Mentioned|p516|||||||||
7426|Glenlogie Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
7426|Glenlogie Suite|42827|5|Briefly described|p437|||||||||
7426|Glenlogie Suite|43260|5|Briefly described|Map Legend||Early Devonian|||||||
7426|Glenlogie Suite|66002|5|Briefly described|p7 Tb.5|||Includes Tailor Creek Tonalite, Powncebys Tonalite, Ben Major Granite, Lexton Granodiorite, Mount Lonarch Granite and Glenlogie Granodiorite. Defined in White and Chappell 1988.||||||
37620|Glenloth Suite|23309|6|Mentioned|p339|||Superseded by Hemsley Suite.||||||
37620|Glenloth Suite|60452|4|Described|p54|||See also Glenloth suite. Component buried plutons: Barraport, Tunstalls. See also p49.||||||
37620|Glenloth Suite|60461|5|Briefly described|Map legend|Early Devonian|Early Devonian|Consists of the Barraport and Tunstalls plutons.||||||
37620|Glenloth Suite|60462|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||15-SEP-04
37620|Glenloth Suite|60491|6|Mentioned|p31|||Includes the north-northeast trending granites.||||||22-NOV-04
37620|Glenloth Suite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Wycheproof Granite, Jeffcott Granite, Teddywaddy Granite, Wescotts Granite, Glenloth Granite.||||||
37620|Glenloth Suite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Includes: Wescotts Granite, Wychproof Granite, Jeffcott Granite, Teddywaddy Granite, Glenloth Granite.||||||
37620|Glenloth Suite|66002|5|Briefly described|p6 Tb.5|||Includes Wycheproof Granite, Hemleys Granite, Jeffcott Granite, Teddywaddy Granite and Wescotts Granite. Defined in Bibby and Moore 1998.||||||
37620|Glenloth Suite|68189|6|Mentioned|p15 Fig.6||||||||granites|
37620|Glenloth Suite|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian||||Includes Hemsleys Granite and 11 geophysically identified plutons.|||
76930|Glenmaggie Basalt|66244|4|Described|p6.|Miocene|Miocene|New name. Includes flows just west of Lake Glenmaggie and in the Macalister River valley, and the upstream remnants around Connors Plain. Magnetic imaging shows it continues under cover into the La Trobe Valley to Heyfield. One K-Ar date gives early Miocene age (McKenzie et al., 1984)|||||Mainly alkali olivine basalt, with olivine tholeiite and hawaiite. |
76930|Glenmaggie Basalt|68116|5|Briefly described|Appendix, Map 43.|Aquitanian|Aquitanian||||||Basalt flows; alkali olivine basalt, olivine tholeiite and hawaiite, with alkali olivine basalt being the most abundant.|
26582|Glennie Granite|23266|5|Briefly described|p356|||||||||
26582|Glennie Granite|23309|6|Mentioned|p431 App1|||G253 S-Type.||||||
26582|Glennie Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
26582|Glennie Granite|68116|5|Briefly described|Appendix.|Middle Devonian|Middle Devonian||||||Cordierite-biotite granite: coarse grained, subequigranular; S-type.|
37062|Glenore Granite|23603|6|Mentioned|p11|Permian|Permian|||||||
25015|Glenronald Shale Member|23309|5|Briefly described|p35|||Of the Fairview Andesitic Breccia.||||||
25015|Glenronald Shale Member|23402|4|Described|p10, p8 Tb. 1|Late Cambrian|Late Cambrian|Also referred to as Glenronald Chert Member (Buckland & Ramsay, 1982).   Parent: Fairview Andesite Breccia. Geological Province: Adelaide Fold Belt||||||
25015|Glenronald Shale Member|40172|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
25015|Glenronald Shale Member|40887|2|Defined|p13|Cambrian|Cambrian|Prob. Cambrian. Supersedes Glenronald Chert Member.||||||
25015|Glenronald Shale Member|41571|5|Briefly described|p39|||||||||
25015|Glenronald Shale Member|42827|5|Briefly described|p39|||||||||
25015|Glenronald Shale Member|50371|5|Briefly described|Map Legend|Cambrian|Cambrian|Of Fairview Andesite Breccia (Mount Stavely Volcanic Complex). Laminated black pyritic shale, volcanic siltstone, minor chert||||||11-JUN-04
25015|Glenronald Shale Member|61187|6|Mentioned|p69 Fig.2.|Early Cambrian|Early Cambrian|||Unit in Fairview Andesitic Breccia.||||
25015|Glenronald Shale Member|62742|5|Briefly described|p698, p700, 702|Middle Cambrian|Middle Cambrian|Of the Stavely Volcanics. Deformed and relatively weakly altered unit containing acritarchs and minor other fossil fragments in a chert section.  Age: ca 505Ma.||||||06-SEP-18
25015|Glenronald Shale Member|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Fairview Andesite Breccia. Defined by Buckland 1986.||||||
25015|Glenronald Shale Member|68466|5|Briefly described|p70|||Stawell Zone, W VIC. Contains acritarchs associated with a probable paraconodont; assigned a probable Middle Cambrian age.||Stavely Volcanics.|||Includes chert.|
25015|Glenronald Shale Member|71593|6|Mentioned|p29|||||Mount Stavely Volcanic Complex||||
7443|Glenrowan Granite|22971|5|Briefly described|p 34|||||||||
7443|Glenrowan Granite|23309|6|Mentioned|p432 App1|||G202.||||||
7443|Glenrowan Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
7443|Glenrowan Granite|68116|5|Briefly described|Appendix, Map 19.|Late Devonian|Late Devonian||||||Biotite granite: fine grained, sugary, grey-brown; extensive hydrothermal alteration; I-type.|
24290|Glenthompson Sandstone|22628|5|Briefly described|fig1p108|Middle Cambrian|Middle Cambrian|||||||
24290|Glenthompson Sandstone|22708|6|Mentioned|p209|||||||||
24290|Glenthompson Sandstone|22756|6|Mentioned|P9|||||||||
24290|Glenthompson Sandstone|23229|5|Briefly described|Table3-1p16, 16-7|Cambrian|Cambrian|||||||
24290|Glenthompson Sandstone|23309|5|Briefly described|p41  Table 2.11||Middle Cambrian|Intruded by Bushy Creek Granodiorite.  Overlies: Mount Stavely Complex (Conformably).||||||
24290|Glenthompson Sandstone|23402|3|Fully described|p19, p8 Tb. 1|Late Cambrian|Late Cambrian|Variation on the Glenthompson beds of Vandenberg and Wilkinson (1982).  Overlies Mount Stavely Volcanic Complex.   Intruded by Bushy Creek Granodiorite and Wickliffe Rhyolite.   Geological Province: Adelaide Fold Belt.||||||21-OCT-08
24290|Glenthompson Sandstone|24087|6|Mentioned|p327 Fig.2|||Geological Province: Lachlan Fold Belt.||||||
24290|Glenthompson Sandstone|24221|5|Briefly described|p893 Fig. 2|||Geological Province:  Delamerian Fold Belt.||||||
24290|Glenthompson Sandstone|24311|5|Briefly described|p1058|Cambrian|Cambrian|||||||
24290|Glenthompson Sandstone|24323|5|Briefly described|p145|Cambrian|Cambrian|Geological Province: Otway Basin||||||
24290|Glenthompson Sandstone|24551|5|Briefly described|p80|Late Cambrian|Late Cambrian|Of Nargoon Group.||||||
24290|Glenthompson Sandstone|40172|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
24290|Glenthompson Sandstone|40761|5|Briefly described|Table 1|||||||||
24290|Glenthompson Sandstone|40887|2|Defined|p22|Cambrian|Cambrian|Prob. Cambrian||||||
24290|Glenthompson Sandstone|41571|6|Mentioned|Table 2.2|||||||||
24290|Glenthompson Sandstone|42827|5|Briefly described|p38|||||||||
24290|Glenthompson Sandstone|43627|5|Briefly described|p13, p15|Cambrian|Cambrian|||||||28-OCT-04
24290|Glenthompson Sandstone|43753|6|Mentioned|p622||Cambrian|||||||
24290|Glenthompson Sandstone|44186|5|Briefly described|Map Legend||Cambrian|||||||
24290|Glenthompson Sandstone|44931|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Turbiditic quartzo-micaceous sandstone and mudstone.||||||01-JUN-12
24290|Glenthompson Sandstone|50154|5|Briefly described|p72, p159|Cambrian|Neoproterozoic III|Age: 500-600 Ma (detrital zircons; Fanning and Morand, 2002). Intruded by Bushy Creek Granodiorite. Overlies Mount Stavely Volcanic Complex. Geological Province: Grampians-Stavely Zone, Delamerian Fold Belt.||||||
24290|Glenthompson Sandstone|50371|5|Briefly described|Map Legend|Cambrian|Cambrian|Fine to medium-grained graded metaquartz sandstone, minor siltstone; flysch deposits.||||||
24290|Glenthompson Sandstone|60451|3|Fully described|p22, 25, 47, 107, 125-126|Late Cambrian|Late Cambrian|Originally named Glenthompson Beds. Includes sediments previously referred to informally as Moyston sandstone. Minimum Thickness: ~900m. Overlain by Grampians Group. Consists of turbiditic sandstone, greywacke and mudstone. Age: Zircon 520-550Ma.||||||05-JUN-14
24290|Glenthompson Sandstone|60454|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt. Of the Nargoon Group. Turbiditic sandstone, greywacke, and mudstone: fine to coarse grained.||||||10-MAR-09
24290|Glenthompson Sandstone|60456|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt. Of the Nargoon Group. Turbiditic sandstone, greywacke and mudstone: fine to coarse grained.||||||10-MAR-09
24290|Glenthompson Sandstone|60457|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Nargoon Group. Unit does not appear on map. Geological Province: Delamerian Fold Belt.||||||10-MAR-09
24290|Glenthompson Sandstone|60458|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt. Of the Nargoon Group. Turbiditic sandstone, greywacke and mudstone.||||||10-MAR-09
24290|Glenthompson Sandstone|60459|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt. Of the Nargoon Group. Turbiditic quartz-rich sandstone, greywacke, mudstone. Prehnite-pumpellyite grade.||||||01-JUN-12
24290|Glenthompson Sandstone|60544|5|Briefly described|Map legend|Cambrian|Cambrian|Quartz sandstone with minor lithic units.||||||23-DEC-09
24290|Glenthompson Sandstone|61183|6|Mentioned|p23|Cambrian|Cambrian|Part of the Mount Stavely Volcanic Complex. Pale turbiditic sandstone and mudstone, characteristically micaceous.||||||
24290|Glenthompson Sandstone|61187|5|Briefly described|p5 Fig.3, p69, pp74-76, p80, p83 Fig.1.|Late Cambrian|Middle Cambrian|Glenelg Zone, Melbourne Terrane. Nonmagnetic to weakly magnetic; moderate to high K and Th responses. Magnetic susceptibility and S.G. are given. North Ltd. regard the boundary with Towanway Tuff as the prospective copper VHMS horizon.||||Conformably overlies Towanway Tuff. Is intruded by Buckeran Diorite and Bushy Creek Granodiorite.||
24290|Glenthompson Sandstone|61410|6|Mentioned|p7 Fig.2|Cambrian|Cambrian|||||||
24290|Glenthompson Sandstone|61726|5|Briefly described|p924 Fig.3|Late Cambrian|Late Cambrian|Geological Province: Lachlan Fold Belt/Grampians-Stavely Zone. Sandstone written as s/s in figure. See also p926 Fig.4, p936.||||||
24290|Glenthompson Sandstone|61749|6|Mentioned|p13|||Micaceous marine rocks. See also Glenthompson Beds.||||||01-JUN-12
24290|Glenthompson Sandstone|61752|5|Briefly described|p3 Fig. 1|Cambrian|Cambrian|Comprises poorly exposed sequence of low-grade, weakly deformed micaceous turbidites. Includes a major population of detrital zircons of age: 500Ma. Geological Province: Adelaide Fold Belt.||||||07-FEB-11
24290|Glenthompson Sandstone|62755|5|Briefly described|p876 Fig.1|Cambrian|Cambrian|Of the Nargoon Group. Sandstone, siltstone. See also p885 Fig. 8.||||||
24290|Glenthompson Sandstone|63599|5|Briefly described|p977|Cambrian|Cambrian|Intruded by Bushy Creek Igneous Complex. See also Glenthompson granodiorite.||||||02-OCT-09
24290|Glenthompson Sandstone|64314|6|Mentioned|p502|||||||||
24290|Glenthompson Sandstone|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Nargoon Group. Defined by Buckland 1986. Name replaces informal Glenthompson Beds and Glenthompson-Chatsworth sediments of VandenBerg and Wilkinson (1982)||||||
24290|Glenthompson Sandstone|66769|5|Briefly described|116|Late Cambrian|Late Cambrian|Grampians-Stavely Zone. Underlies Carrolls Amphibolite which is thrust over it. Overlies Mount Stavely Volcanic Complex. Marine terrigenous sediments, possibly sourced from the eroding Adelaide Rift System.||||||
24290|Glenthompson Sandstone|68116|5|Briefly described|Appendix, Maps 22, 30, 39.|Late Cambrian|Early Cambrian|Weathered.|||||Sandstone, mudstone, phyllite: fine to coarse-grained; detrital quartz, muscovite, biotite, lithic fragments, K-feldspar and plagioclase in fine-grained matrix (greywacke and sublitharenite); graded turbidites; anchizone to biotite zone metamorphism.|
24290|Glenthompson Sandstone|68189|6|Mentioned|p3, p19|||See also Glentompson Sandstone.||||||
24290|Glenthompson Sandstone|68194|5|Briefly described|p20-21, p31, p75, p77-78, p95|Cambrian|Cambrian|Buckland (1987). Grampians-Stavely zone. In situ regolith described. Basement to Department of Natural Resources and Environment boreholes, details of which are given.||Unit in Nargoon Group.|||Marine turbidites: sandstone, greywacke and mudstone beds. Locally contact metamorphosed to hornfels.|
24290|Glenthompson Sandstone|70211|5|Briefly described|p1-3, p6, p35-46, p60|||Marine terrigenous sediments. Deposition post-dated c.510-500 Ma (superposition) and pre-dated intrusion (500 Ma). Some sediments are interpreted to have protolith source rocks from Antarctica and/or parts of Pan-Gondwana.|569.0 +/- 3.6 Ma (maximum depositional age).|Nargoon Group.||Overlies the Mount Stavely Volcanic Complex. Is intruded by the Bushy Creek Igneous Complex.|Folded turbiditic sandstone; medium-grained, sub-angular to rounded, with disseminated and veined pyrite throughout.|
24290|Glenthompson Sandstone|70877|4|Described|p2, p10-p12, p14-p15,  p23-p40, p61, |Cambrian|Ediacaran|See also p70, p91, p109, p114, p135, p143, p167-p168, p170, p196, p202. Grampians-Stavely Zone. Ballarat 1:250k and Willaura 1:100k map sheets. SHRIMP ages derived from this study and represent a maximum age of deposition. Deposited in a deep marine environment as turbidites. Previously the only constituent of the Nargoon Group; in this volume it was seperated on the basis of being older than the Nargoon Group. Petrography, zircon morphology and SHRIMP U-Pb results are discussed in detail for several samples of this unit.  Intruded by the Bushy Creek Granodiorite and Buckeran Diorite. Equivalent to the Kanmantoo Group.|538 +/- 23 Ma and 560.9 +/- 4.2 Ma (SHRIMP U-Pb)|||Overlain by the Mount Stavely Volcanic Complex. Structurally overlies and is faulted against the Towanway Tuff.|Low-grade metasedimentary rocks; sandstone and siltstone dominated by mica.|
24290|Glenthompson Sandstone|70967|5|Briefly described|p9, 14, 20, 28|||Stavely Belt.||Nargoon Group.||Overlies Mount Stavely Volcanic Complex. Is intruded by Bushy Creek Igneous Complex.|Deep marine turbiditic rocks; includes volcaniclastics.|
24290|Glenthompson Sandstone|71593|4|Described|p1, p8-p9, p12, p14, p19, p24-p28, p32|Late Cambrian|Cambrian|Delamerian Orogen, Grampians-Stavely Zone. Sandstones of this unit have previously been included in the Nargoon Group but are now regarded as older and thus a separate unit. Non-magnetic. Age derived from dating of related units. Petrography briefly discussed. Faulted against the Glenelg River Metamorphic Complex. Together with the Towanway Tuff hosts the Thursdays Gossan Prospect. Hosts the Fairview North and South prospects. See also  p35, p37, p40, p43, p57-p58, p70, p72, p74-p77, p84, p95, p98, p102, p120, p124, p133, p135, p137, p139, p144, p150, p161, p163, p171, p188, p193, p198.|c. 520-502 Ma|||Conformably (gradationally) overlies the Mount Stavely Volcanic Complex. Intruded by the Bushy Creek Granodiorite, Buckeran Diorite and Chatsworth Basalt. Equivalent to the Kanmantoo Group.|Turbiditic, deep marine sediments including terrigenous thinly- to thickly-bedded micaceous quartz arenite, quartz lithic sandstone and siltstone, with minor interbeds of shale and pelitic mudstone.|
24290|Glenthompson Sandstone|72445|5|Briefly described|p8, p9, p13, p19; App.1, App.2; App.5.|Cambrian|Cambrian|Shown as part of the target basement. Terrigenous deep marine turbiditic low-grade sedimentary rocks. App.2 is a .csv format file. Identified in Stavely 11, 17. Described as Paleozoic but minimum age from intrusive relationship of Bushy Creek Igenous Complex. Overlies the Mount Stavely Volcanic Complex. Underlies the Grampians Group.||Nargoon Group.||Intruded by unassigned porphyry in Stavely17. Shown as underlying Olney Formation, Renmark Group. Intruded by Bushy Creek Igneous Complex.|Fine- to medium- to coarse-grained sandstone with 0.8-7.3 m subordinate siltstone intervals; Altered fine-grained sandstone with subordinate siltstone intervals. Local soft-sediment deformation. Minor sedimentary breccias.|15-OCT-20
24290|Glenthompson Sandstone|73118|5|Briefly described|p6-7, 14, 53, 72, 74|Cambrian|Cambrian|Glenelg Zone, Lachlan Fold Belt, Western Victoria. Mis-spelt in p7 as Glenthomson Sandstone. A syntectonic unit formed by erosion during the Delamerian Orogeny.|500-485 Ma; deposition.|||Is overlain by Olney Formation. Is intruded by Bushy Creeh Tonalite.|Micaceous sandstone and mudstone, grey-blue siltstone and less common greywacke.|
24290|Glenthompson Sandstone|73264|5|Briefly described|p1388, p1389 Fig.11|Late Cambrian|Late Cambrian|Grampians-Stavely Zone. Panafrican 550-700 Ma zircon population and ~1050-1300 Ma Grenvillian zircon population.|500-490 Ma||||Quartz-rich sandstone.|
34823|Glenvale Granodiorite|22885|5|Briefly described|map|||||||||
34823|Glenvale Granodiorite|22886|5|Briefly described|Table.1|||||||||
34823|Glenvale Granodiorite|23309|6|Mentioned|p432 App1|||G222. Supersedes Glenvale Granite.||||||
69404|Goat Rocks Conglomerate|64619|5|Briefly described|Map legend|Early Devonian|Silurian|Of Kerrie Group.  Age: Silurian or Lower Devonian. Conglomerate, sandstone - pebble to boulder conglom., massive to crudely bedded, mod'ly sorted, generally well-rounded; clasts of quartzite, sandstone, chert, gritstone, minor vein qtz; sst rare, etc.||||||
69404|Goat Rocks Conglomerate|65715|4|Described|p5, p5 Tb.3, p29 Fig.2|Devonian|Silurian|Newly defined. Basal Member of Kerrie Group. Interfingers Kirribilly Sandstone. Type locality at Conglomerate Gully on the Goat Rocks property (MGA ref given). Mostly massive pebble to boulder conglomerate with a closed framework of sandstone, quartzite, chert and gritstone clasts derived from Ordovician rocks. Clasts are generally well rounded. Bedding defined by rare beds of thin lenticular sandstone. Nearly 900 m thick in the Black Range, but less elsewhere.||||||02-FEB-15
69404|Goat Rocks Conglomerate|68116|5|Briefly described|Appendix, Map 32.|Devonian|Silurian||||||Conglomerate, sandstone: pebble to boulder conglomerate massive to crudely bedded; sorting moderate; well rounded; clasts of quartzite, sandstone, chert, gritstone, minor vein quartz; sandstone rare: well sorted with planar and cross-lamination.|
26585|Golden Ball Granite|22971|5|Briefly described|p 33|||||||||
26585|Golden Ball Granite|23309|6|Mentioned|p432 App1|||G196 I-Type. Supersedes Golden Ball Adamellite.||||||
26585|Golden Ball Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|Variation on Golden Ball Adamellite.||||||
26585|Golden Ball Granite|68116|5|Briefly described|Appendix, Map 19.|Late Devonian|Late Devonian||||||Leucocratic biotite granite: medium grained; accessory muscovite, fluorite, topaz, ilmenite and zircon; I-type.|05-JUN-14
32307|Golden Beach Subgroup|13323|4|Described|p395-6, p393 Fig. 2|Late Campanian|Santonian|Of the Latrobe Group. Comprises Chimaera and Anenome Formations. Non-marine to paralic clastics; marine clastics. Geological Province: Gippsland Basin. See also p394 Fig. 3.||||||
32307|Golden Beach Subgroup|13324|4|Described|p94 Fig.4, Fig.5, p98|Campanian|Santonian|Gippsland Basin. Formerly included in Golden Beach Group of Lowry and Longley (1991). Non-marine to open marine environments. Termination of sedimentation associated with volcanism in Campanian.||Of Latrobe Group|Includes Chimaera Formation?|Unconformably overlies Emperor Subgroup. Overlain unconformably by Latrobe Siliciclastics.|Sandstones and shales.|
32307|Golden Beach Subgroup|24090|5|Briefly described|p8 Fig.3|Late Cretaceous|Late Cretaceous|Of the Latrobe Group. See also page 17. Geological Province: Gippsland Basin.||||||06-APR-05
32307|Golden Beach Subgroup|24164|5|Briefly described|p3,11,18,20,22,24-25,27-28,30 and more|Campanian|Santonian|Horizon top of this unit was mapped from seismic data. A volcanic episode at top of Golden Beach Subgroup is a little younger than 80 Ma (Bernecker and Partridge 2001). Seabed dredging yielded Santonian microplankton, typical of this unit. Gippsland Basin. Also included on p32, 34, 37, p39-42 and in Figs.10,12,14,15,19,22,26, Tb.2.||Latrobe Group||Overlies Strzelecki Group; is overlain by Latrobe Group||
32307|Golden Beach Subgroup|24404|5|Briefly described|p5|||Unconformably overlain by Latrobe Siliclastics.||||||
32307|Golden Beach Subgroup|24407|5|Briefly described|p13 Fig.2, p14|Campanian|Santonian|Parent: Latrobe Group. Geological Province: Gippsland Basin||||||
32307|Golden Beach Subgroup|24495|5|Briefly described|p10, p12|Late Cretaceous|Late Cretaceous|Of  Latrobe Group.  Geological Province: Gippsland Basin.||||||
32307|Golden Beach Subgroup|24551|5|Briefly described|p267|Campanian|Santonian|Of the Latrobe Group. Overlies the Emeror Subgroup.||||||
32307|Golden Beach Subgroup|60666|5|Briefly described|p15 (Fig.)|||Of the Latrobe Group.  Geological Province: Gippsland Basin.||||||23-DEC-04
32307|Golden Beach Subgroup|61212|5|Briefly described|p300, p301 Fig. 2|Campanian|Santonian|Mostly non-marine sediments.||||||
32307|Golden Beach Subgroup|61552|5|Briefly described|p583 Fig.2. |Late Cretaceous|Late Cretaceous|Deposited during a margin sag-phase, involving rapid subsidence in response to sea floor spreading in the adjacent Tasman Sea.||Unit in Latrobe Group.|Includes Chimaera and Anemone Formations and Campanian Volcanics.|||
32307|Golden Beach Subgroup|64876|5|Briefly described|p145 Fig.2|Campanian|Santonian|Gippsland Basin.||Latrobe Group.|Chimaera, Anemone Formations.|Overlies Emperor Subgroup (Longtom Unconformity). Is overlain by Halibut Subgroup (Seahorse Unconformity).||
32307|Golden Beach Subgroup|65717|5|Briefly described|p9 Fig.2.2, p10-13, p37|Campanian|Santonian|Formerly known as Golden Beach Group (Lowry and Longley, 1991). Reflects tectonic movement and fluvial systems. Includes intraformational seals.||Latrobe Group|Includes Chimaera Formation, Anemone Formation|Unconformably overlies Emperor Subgroup, unconformably overlain by Halibut Subgroup|Conglomerates and finer sediments.|05-SEP-17
32307|Golden Beach Subgroup|65718|5|Briefly described|p5, pp10-12, p32 Fig 4.3, pp38-41|Cretaceous|Cretaceous|Gippsland Basin. Written as Golden Beach subgroup on p39. Identified as a potential hydrocarbon or geological carbon storage reservoir. Upper Cretaceous age.||Of the Latrobe Group.|Includes the Chimaera Formation.|||
32307|Golden Beach Subgroup|65973|5|Briefly described|p14-15, p19, p22-23, p29, p31, p33, p38|||Gippsland Basin. Parts of this group were intersected in Archer-1, Anemone-1, Angler-1, Chimaera-1, Kipper-2, Judith-1, East Pilchard-1, Northright-1, Shark-1 and Pisces-1 and many more drillholes (see appendix). Generally confined to the Central Deep area of the basin. Hosts the offshore Kipper field hydrocarbon discovery. Dominated by upper coastal plains facies. See also p42, p57, p59, p62, p66, p70-72, p74-75, p78, p82-84, p86, p90, p104, p106-109, p123-124, p126-127, p129-131, p135, p138-139, p171, p180, p182, p184.||Latrobe Group|Includes the Anemone Formation and the Chimaera Formation.|Unconformably overlies the Emperor Subgroup. Unconformably overlain by the Halibut Subgroup.|Quartzose, commonly lithic, fine- to medium-grained, angular to subrounded, poor to moderately sorted, sandstones.|
32307|Golden Beach Subgroup|66181|5|Briefly described|p310 Fig.5|Campanian|Santonian|Unconformably underlies the Halibut Subgroup, unconformably overlies the Emperor Subgroup. Non marine to paralic clastics, in the Latrobe Group.||||||
32307|Golden Beach Subgroup|69297|5|Briefly described|p400, p415, p431, p434|||Gippsland Basin.|||||Mudstone and marine shales. |
32307|Golden Beach Subgroup|69879|6|Mentioned|p428|Campanian|Santonian|Gippsland Basin. Synrift deposits; faulted and folded.||||||
32307|Golden Beach Subgroup|70028|5|Briefly described|p79-80, 82|Campanian|Santonian|Gippsland Basin.|85-75 Ma.|Latrobe Group.||Unconformably overlies Emperor Subgroup. Is overlain unconformably by Latrobe Group.|Coarse-grained alluvial-fluvial sediments and fine-grained floodplain deposits.|
32307|Golden Beach Subgroup|70076|5|Briefly described|South-Eastern: Fig.2; p1, p3|Campanian|Santonian|See also Regional: Fig.3; p2, p4-5, p7-8. Fluvial and marine sediments. Hosts the Kipper gas field.||Latrobe Group.|Chimaera and Anemone Formations; Campanian Volcanics.|Overlies Emperor Subgroup. Is overlain by Halibut Subgroup.||
32307|Golden Beach Subgroup|70331|5|Briefly described|p69-70|Late Cretaceous|Late Cretaceous|Gippsland Basin (western).||Latrobe Group.||Unconformably overlies Emperor Subgroup. Is overlain unconformably by Halibut Subgroup.|Onshore: fluvial to paralic sandstone, siltstone, shale, coal. Offshore: marine siltstone, shale.|
32307|Golden Beach Subgroup|73471|5|Briefly described|p85-90, p93 Fig.5, p100, p103-105, p108|Campanian|Coniacian|Gippsland Basin. Incorporated into the post-rift mega-sequence. Overlies Longtom Unconformity, underlies Seahorse Unconformity. Intercalated with subaerial basaltic flows. Contains hydrocarbon source rocks. See also Golden Beach Formation p104.|90-78 Ma|Latrobe Group|Chimaera Formation, Anemone Formation|Unconformably overlies Emperor Subgroup, unconformably underlies Halibut Subgroup, intercalated with Campanian Volcanics||
32307|Golden Beach Subgroup|75065|5|Briefly described|p149, 151, 154-155, 162-164, 172|Campanian|Santonian|Bernecker and Partridge (2001). Gippsland Basin; offshore. Contains reservoirs and potential petroleum source rocks. Also appears as Golden Beach Formation on p163.||Latrobe Group.|Chimaera, Anemone Formations; Campanian Volcanics.|Unconformably overlies Emperor Subgroup. Is overlain unconformably by Halibut Subgroup.|Characterised by quartz clastics. A series of basaltic volcanics occurs in the upper part.|
7511|Goldie Chert|22857|5|Briefly described|p89 Fig. 14.7A, p124|Late Cambrian|Middle Cambrian|Geological Province: Mathinna Terrace. ||||||
7511|Goldie Chert|22858|6|Mentioned|Fig14.7ap88-9|Late Cambrian|Middle Cambrian|||||||
7511|Goldie Chert|22885|5|Briefly described|map|Late Cambrian|Middle Cambrian|||||||
7511|Goldie Chert|22886|4|Described|p10|Early Ordovician|Late Cambrian|||||||
7511|Goldie Chert|22971|5|Briefly described|p 20||Late Cambrian|||||||
7511|Goldie Chert|23229|4|Described|Table3-1p16, 17|Ordovician|Middle Cambrian|||||||
7511|Goldie Chert|23245|5|Briefly described|p124|Datsonian|Payntonian|||||||
7511|Goldie Chert|23309|5|Briefly described|p38, 42-46.||Cambrian|||||||
7511|Goldie Chert|24002|5|Briefly described|p228 Fig.2|Cambrian|Cambrian|||||||
7511|Goldie Chert|24003|5|Briefly described|p258 Fig.3b|Middle Cambrian|Middle Cambrian|||||||
7511|Goldie Chert|24098|5|Briefly described|p27 Fig. 2|Late Cambrian|Late Cambrian|Geological Province: Bendigo Zone, Lachlan Fold Belt.||||||
7511|Goldie Chert|24177|4|Described|p43, p39 Fig.15|Late Cambrian|Late Cambrian|Overlies the Knowsley East Shale. Part of the formation may be equivalent to at least the top part of the Knowsley East Formation. Previously known as the Goldie Chert.||||||
7511|Goldie Chert|24328|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|||||||
7511|Goldie Chert|24329|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|||||||
7511|Goldie Chert|24551|4|Described|p86|Early Ordovician|Late Cambrian|Overlies Knowsley East Shale (85).||||||27-OCT-08
7511|Goldie Chert|40761|5|Briefly described|Table 1|||||||||
7511|Goldie Chert|41570|6|Mentioned|p81|||||||||
7511|Goldie Chert|41571|4|Described|p46|||||||||
7511|Goldie Chert|42628|5|Briefly described|Map legend|Late Cambrian||||||||
7511|Goldie Chert|42790|5|Briefly described|Fig.14 P189|||||||||
7511|Goldie Chert|42826|3|Fully described|p24|||Late Cambrian to Early Ordovician.||||||27-OCT-08
7511|Goldie Chert|42827|4|Described|p46|||||||||
7511|Goldie Chert|44197|5|Briefly described|Map Legend||Cambrian|||||||
7511|Goldie Chert|60591|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Deep water hemipelagic deposit: siliceous shale, chert; white, dark grey, black, thinly bedded.||||||25-NOV-04
7511|Goldie Chert|60592|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Deep water hemipelagic deposit: siliceous shale, chert; white, dark grey, black, thinly bedded.||||||25-NOV-04
7511|Goldie Chert|60593|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Deep water hemipelagic deposit: siliceous shale, chert; white, dark grey, black, thinly bedded.||||||
7511|Goldie Chert|60595|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Deep water hemipelagic deposit: siliceous shale, chert; white, dark grey, black, thinly bedded.||||||26-NOV-04
7511|Goldie Chert|60596|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Deep water hemipelagic deposit: siliceous shale, chert; white, dark grey, black, thinly bedded.||||||
7511|Goldie Chert|60597|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Weakly magnetic; low K, Th and U||||||
7511|Goldie Chert|60599|3|Fully described|p19, p42|Cambrian|Cambrian|Supersedes Goldie beds (upper half) and Goldie Shale, and now includes only the true cherts and siliceous siltstones. Non-magnetic unit. Overlies Heathcote Volcanics units. Interfingers with Knowsley East Shale.  See also p24 Tb. 4.||||||
7511|Goldie Chert|62099|5|Briefly described|p332|Cambrian|Cambrian|In the Bendigo Zone of the Lachlan Orogen. ||||||
7511|Goldie Chert|62742|5|Briefly described|p697|Late Cambrian|Late Cambrian|Siliceous siltstone (chert); contains abundant phyllocarid crustacean remains and a single Datsonian (Late Cambrian) conodont. In the Heathcote Greenstone Belt. ||||||
7511|Goldie Chert|62744|5|Briefly described|p708|Late Cambrian|Late Cambrian|Geological Province: Heathcote Greenstone Belt.||||||
7511|Goldie Chert|64611|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian|Chert, shale and siltstone: dark grey to black, thinly bedded chert, siliceous black shale, siliceous siltstone and rare chert breccia: deep marine hemipelagic deposits.||||||16-DEC-08
7511|Goldie Chert|64612|2|Defined|p26, p33-34, p53, p57, p65|Datsonian|Middle Cambrian|Conformably overlies Knowsley East Shale with gradational contact, overlain by Romsey Subgroup (Stauro Gully Shale), sharp and conformable. Thickness: 600m. Thin-bedded chert, with lesser interbedded siliceous black shale and siliceous siltstone.||||||07-FEB-11
7511|Goldie Chert|64619|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Chert, siliceous siltstone, shale: black to pale coloured, thin-bedded; pyritic in places, with rough stylolitic bedding planes; deep marine hemipelagic deposits.||||||
7511|Goldie Chert|65715|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Formation rank.||||||
7511|Goldie Chert|65969|5|Briefly described|p3, p11|Cambrian|Cambrian|Overlies Knowsley East Shale. Deep marine chert. Overlain by Castlemaine Group.||||||
7511|Goldie Chert|66182|6|Mentioned|p320|Late Cambrian|Late Cambrian|Deep sea chert.||||||11-MAY-12
7511|Goldie Chert|66196|5|Briefly described|p617, p621, 623|||Heathcote Greenstone Belt. Overlies Heathcote Volcanics, overlies Knowsley East Formation, underlies Castlemaine Supergroup. Includes latest Cambrian (Datsonian) conodonts in topmost bed. Pelagic deep-sea environment. Light-grey to white argillaceous chert.||||||16-NOV-12
7511|Goldie Chert|66769|6|Mentioned|118-119|Cambrian|Cambrian|Conformably overlies the Knowsley East Shale. Thin, deep-ocean sedimentary rock.||||||
7511|Goldie Chert|67322|6|Mentioned|p15|Datsonian|Datsonian|Late Cambrian age based on the presence of Cordylodus conodonts (Stewart and Fergusson 1988, Kakuwa and Webb 2010). ||||||
7511|Goldie Chert|68116|5|Briefly described|Appendix, Maps 24, 32.|Late Cambrian|Late Cambrian||||||Chert, siliceous siltstone, shale: black to pale-coloured; thin-bedded; pyritic in places; with rough stylolitic bedding planes.|
7511|Goldie Chert|68314|5|Briefly described|p750, p754, p756|Late Cambrian|Late Cambrian|Heathcote Greenstone Belt. Contains Datsonian conodonts.|||||Fine-grained siliceous siltstones; abundantly fossiliferous.|
7511|Goldie Chert|70601|5|Briefly described|p44|Warendan|Idamean|Kilmore/Heathcote area.||||Underlies Castlemaine Group. Overlies Knowsley East Shale.||
7511|Goldie Chert|73497|5|Briefly described|Map legend|Cambrian|Cambrian|Marine.||||Overlies Knowsley East Shale, underlies Saint Arnaud Group|Chert, siliceous siltstone: weakly magnetic; low K, Th and U.|
37557|Good Morning Bill Schist|23309|5|Briefly described|p227, Table 2.23|||Of Moornambool Metamorphic Complex.||||||
37557|Good Morning Bill Schist|60451|4|Described|p57, 73, 114, 167|||Of the Moornambool Metamorphic Complex. Warrak Formation probably protolith of this unit. Type section in text. Metamorphosed to amphibolite grade.||||||
37557|Good Morning Bill Schist|60454|5|Briefly described|Map Legned|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-muscovite-biotite (+/-garnet+/-K-feldspar+/-staurolite) schist: coarsely schistose.||||||
37557|Good Morning Bill Schist|60456|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-muscovite-biotite (+/-garnet+/-K-feldspar+/-staurolite) schist: coarsely schistose.||||||
37557|Good Morning Bill Schist|60457|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-muscovite-boitite (+/-garnet+/-K-feldspar+/-staurolite) schist: coarsely schistose; transposition and mylonitic fabrics and folds.||||||24-SEP-04
37557|Good Morning Bill Schist|60458|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-muscovite-biotite (+/-garnet+/-K-feldspar+/-staurolite) schist; coarsely schistose.||||||
37557|Good Morning Bill Schist|60459|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-muscovite-biotite (+/-garnet+/-K-feldspar+/-staurolite) pelitic schist. Amphibolite grade.||||||
37557|Good Morning Bill Schist|65716|4|Described|p17-24|Cambrian|Ediacaran|Of Moornambool Metamorphic Complex. Pelitic schist. Dated sample composed of quartz, muscovite and biotite, with accessory apatite, opaques and feldspar. Lower amphibolite metamorphic grade. Depositional age between 570-500 Ma.||||||
37557|Good Morning Bill Schist|66002|5|Briefly described|p5 Tb.2|Cambrian|Cambrian|Of Moornambool Metamorphic Complex. Defined by Cayley and Taylor 2001.||||||
37557|Good Morning Bill Schist|68116|5|Briefly described|Appendix, Map 30.|Late Cambrian|Middle Cambrian|Psammitic layers from Warrak Formation precursor? |||||Quartz-muscovite-biotite (+/- garnet +/- K-feldspar +/- staurolite) schist: coarsely schistose; transposition and mylonitic fabrics and folds ubiquitous; coarsely layered with quartz and mica domains; occasional thicker psammitic layers; nonmagnetic.|
37557|Good Morning Bill Schist|71593|6|Mentioned|p36-p37|||||Moornambool Metamorphic Complex||||
23628|Goongerah Granodiorite|22876|4|Described|p25|||Currawong Suite||||||
23628|Goongerah Granodiorite|22877|5|Briefly described|map|Silurian|Silurian|Currowong Suite. G50. Hornblende-biotite granodiorite, I-Type.||||||26-OCT-04
23628|Goongerah Granodiorite|23309|6|Mentioned|p432 App1|||G50 - I-Type.||||||
23628|Goongerah Granodiorite|41850|6|Mentioned|p431|||||||||
23628|Goongerah Granodiorite|42627|5|Briefly described|Map legend|Wenlock||||||||
23628|Goongerah Granodiorite|42647|4|Described|p41|||||||||
23628|Goongerah Granodiorite|42827|5|Briefly described|p431|||||||||
23628|Goongerah Granodiorite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Hornblende-biotite granodiorite: medium to coarse grained, bluish grey; contains abundant dark enclaves; I-type.|
31497|Goongerah Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Currowong Supersuite.  Includes the Goongerah Granite (informal name).||||||09-FEB-05
7571|Goonmirk Rocks Granodiorite|23309|6|Mentioned|p432 App1|Early Devonian|Late Silurian|G34 A-Type.  Supersedes Goonmirk Rocks Granitoid.||||||16-MAY-05
7571|Goonmirk Rocks Granodiorite|24551|6|Mentioned|p235|||||||||
7571|Goonmirk Rocks Granodiorite|42627|5|Briefly described|Map legend|Wenlock|Wenlock|Reserved as Goonmirk Granodiorite.||||||
7571|Goonmirk Rocks Granodiorite|68116|5|Briefly described|Appendix, Map 36.|Early Devonian|Early Devonian||||||Hornblende granodiorite: medium grained, moderately foliated; I-type.|
21889|Gordon Creek Ignimbrite|23309|4|Described|p112. Table 2.40|Early Silurian|Early Silurian|Of the Timbarra Subgroup.  Maximum Thickness: >100m.||||||
21889|Gordon Creek Ignimbrite|23615|3|Fully described|p92|Early Devonian|Early Devonian|Of Timbarra Subgroup. Overlies Scorpion Creek Ignimbrite.||||||
21889|Gordon Creek Ignimbrite|24551|5|Briefly described|p142|||Of the Timbarra Subgroup.||||||
21889|Gordon Creek Ignimbrite|43206|5|Briefly described|map legend||Ludlow|Timbarra Subgroup||||||
21889|Gordon Creek Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Quartz ignimbrite: red to purple with large quartz, small feldspar phenocrysts.|
7635|Gough trachyte|35215|6|Mentioned|p190|||||||||
69400|Goughs Bay Sandstone Member|64536|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Montys Hut Fm (Walhalla Grp). Sandstone, siltstone:sst thin to thick bedded, quartzite-lithic;Ta-c, Tbc + Tc turbidites; interbedded siltstone thin bedded, shaly, generally weathered to pale colours. Deep-marine turbidite fans + hemipelagic deposits.||||||07-FEB-11
69400|Goughs Bay Sandstone Member|64537|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Montys Hut Fm (Walhalla Grp). Sandstone, siltstone:sst thin to thick bedded, quartzite-lithic;Ta-c, Tbc + Tc turbidites; interbedded siltstone thin bedded, shaly, generally weathered to pale colours. Deep-marine turbidite fans + hemipelagic deposits.||||||07-FEB-11
69400|Goughs Bay Sandstone Member|64538|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Montys Hut Fm (Walhalla Grp). Sandstone, siltstone:sst thin to thick bedded, quartzite-lithic;Ta-c, Tbc + Tc turbidites; interbedded siltstone thin bedded, shaly, generally weathered to pale colours. Deep-marine turbidite fans + hemipelagic deposits.||||||07-FEB-11
69400|Goughs Bay Sandstone Member|64606|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of Montys Hut Formation. Sandstone, siltstone: deep-marine deposits. Dark blue to light blue-pink in RGB. Generally low magnetic response.||||||
69400|Goughs Bay Sandstone Member|64616|4|Described|p117, p280, p302|Emsian|Emsian|New name. Within Montys Hut Formation. 50-250m thick. Thick-bedded sandstone, quartzitic to lithic; interbedded thin-bedded, shaly siltstone; some shelly fossils. Age not discussed. Geophysical characteristics given.||||||
7672|Grampians Group|22531|4|Described|p19|Silurian|Ordovician|||||||
7672|Grampians Group|22532|5|Briefly described|map legend|Silurian|Ordovician|||||||
7672|Grampians Group|22628|5|Briefly described|p115, fig3p111|||||||||
7672|Grampians Group|22708|6|Mentioned|p212|||||||||
7672|Grampians Group|22768|5|Briefly described|p141,146,184|Early Devonian|Late Silurian|||||||
7672|Grampians Group|22773|5|Briefly described|Fig24.5p350|Early Devonian|Silurian|||||||
7672|Grampians Group|22857|5|Briefly described|p141, p166, p183|Early Devonian|Late Silurian|Equivalents mentioned on p350 Fig. 24.5. Geological Province: Kanmantoo Fold Belt, Grampians Basin. ||||||
7672|Grampians Group|22887|5|Briefly described|Fig.5 p12|Middle Devonian|Silurian|||||||
7672|Grampians Group|22893|6|Mentioned|fig4 p9|||Describing an equivalent to this unit.||||||
7672|Grampians Group|23061|6|Mentioned|293 fig 1|||Underlying unit Saint Arnaud Beds||||||
7672|Grampians Group|23110|5|Briefly described|p502|||||||||
7672|Grampians Group|23229|4|Described|p24-5|||||||||
7672|Grampians Group|23231|6|Mentioned|Fig5-4p51|||||||||
7672|Grampians Group|23232|5|Briefly described|p62|||||||||
7672|Grampians Group|23234|5|Briefly described|p85|Mesozoic|Late Devonian|||||||
7672|Grampians Group|23235|5|Briefly described|p68|Devonian|Silurian|||||||
7672|Grampians Group|23236|6|Mentioned|Fig10-1.2p99|||||||||
7672|Grampians Group|23247|4|Described|Fig12-1.1p182, 183-4|Early Devonian|Late Silurian|||||||
7672|Grampians Group|23306|6|Mentioned|Map legend|||||||||
7672|Grampians Group|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
7672|Grampians Group|23309|4|Described|p76-83, 203-208, 349|||||||||
7672|Grampians Group|23402|3|Fully described|p25, p7 Tb. 1|Silurian|Silurian|Previously mapped on WILLAURA as 'Willaura Sandstones' (Spencer-Jones, 1965), later modified to 'Willaura Sandstone' (Buckland, 1987).   Age: 412.6+/-3.5Ma (U-Pb zircon).   Unconformably overlies Wickliffe Rhyolite and Glenthompson Sandstone.||||||
7672|Grampians Group|23417|6|Mentioned|p6 Fig.4||Silurian|||||||
7672|Grampians Group|23522|5|Briefly described|p246|Middle Devonian|Early Devonian|||||||
7672|Grampians Group|23857|5|Briefly described|p907|Silurian|Silurian|||||||
7672|Grampians Group|23918|6|Mentioned|p1327|||Geological Province: Lachlan Fold Belt.||||||
7672|Grampians Group|23991|5|Briefly described|p188 Fig.1|Silurian|Silurian|||||||
7672|Grampians Group|24002|5|Briefly described|p227 fig. 1|Ordovician|Ordovician|Age: 425Ma.||||||21-OCT-08
7672|Grampians Group|24100|6|Mentioned|p98 Fig. 4|||Geological Province: Stawell Zone.||||||19-APR-05
7672|Grampians Group|24311|5|Briefly described|p1061, p1059 Fig. 2|Silurian|Silurian|||||||
7672|Grampians Group|24323|5|Briefly described|p138|Silurian|Silurian|||||||
7672|Grampians Group|24383|6|Mentioned|p56 Tb.6|||||||||
7672|Grampians Group|24581|5|Briefly described|p811|Ludlovian|Late Ordovician|Geological Province: Kanmantoo Fold Belt.||||||
7672|Grampians Group|24588|5|Briefly described|p31 Fig.15|Emsian|Emsian|Geological Province: Lachlan Fold Belt.||||||
7672|Grampians Group|29889|6|Mentioned|p141|||||||||
7672|Grampians Group|30329|6|Mentioned|p30|||On table P30||||||
7672|Grampians Group|30522|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Lower Carboniferous to Upper Devonian||||||
7672|Grampians Group|30579|6|Mentioned|Map legend|Silurian|Silurian|||||||
7672|Grampians Group|30928|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
7672|Grampians Group|30934|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
7672|Grampians Group|31161|5|Briefly described|PA11|||||||||
7672|Grampians Group|32001|6|Mentioned|p77|||||||||
7672|Grampians Group|32865|6|Mentioned|p486|||||||||
7672|Grampians Group|33232|3|Fully described|p71|||||||||
7672|Grampians Group|33236|6|Mentioned|p24|||U.Dev. _ L.Carb.||||||
7672|Grampians Group|33238|5|Briefly described|p640|||||||||
7672|Grampians Group|33394|6|Mentioned|p78|||||||||
7672|Grampians Group|33602|6|Mentioned|Table 1|||||||||
7672|Grampians Group|33608|6|Mentioned|p45|||||||||
7672|Grampians Group|33940|6|Mentioned|p416|||||||||
7672|Grampians Group|34990|6|Mentioned|p435|||||||||
7672|Grampians Group|35013|6|Mentioned|p390|||||||||
7672|Grampians Group|35099|6|Mentioned|p325|||||||||
7672|Grampians Group|35112|6|Mentioned|Table.1|||||||||
7672|Grampians Group|35278|6|Mentioned|p349|||||||||
7672|Grampians Group|35281|6|Mentioned|p19|||||||||
7672|Grampians Group|36534|6|Mentioned|p221|||||||||
7672|Grampians Group|36732|6|Mentioned|p300|||||||||
7672|Grampians Group|37501|5|Briefly described|p407|||||||||
7672|Grampians Group|38070|5|Briefly described|p97|||||||||
7672|Grampians Group|38367|6|Mentioned|p158|||See also Fig.1||||||
7672|Grampians Group|38436|6|Mentioned|p420|||||||||
7672|Grampians Group|39291|6|Mentioned|p214|||||||||
7672|Grampians Group|39331|6|Mentioned|Fig.0-3|||See Fig.0-3||||||
7672|Grampians Group|39446|6|Mentioned|p11|||See also P65||||||
7672|Grampians Group|39967|4|Described|p33|||||||||
7672|Grampians Group|40172|6|Mentioned|Map legend|Silurian|Silurian|||||||
7672|Grampians Group|40761|6|Mentioned|p215|||See also p225.||||||07-SEP-18
7672|Grampians Group|40887|6|Mentioned|p25|||||||||
7672|Grampians Group|40947|6|Mentioned|p4|||||||||
7672|Grampians Group|41002|5|Briefly described|p183|||||||||
7672|Grampians Group|41563|6|Mentioned|p516|||||||||
7672|Grampians Group|41571|4|Described|p38|||||||||
7672|Grampians Group|41572|6|Mentioned|p3|||||||||
7672|Grampians Group|41585|4|Described|p141|||||||||
7672|Grampians Group|41637|6|Mentioned|p210|||||||||
7672|Grampians Group|41641|6|Mentioned|p191|||||||||
7672|Grampians Group|42119|5|Briefly described|p524|||||||||
7672|Grampians Group|42745|5|Briefly described|p3, p6|||Also P9.||||||
7672|Grampians Group|42827|6|Mentioned|p141|||see also Table 4.3||||||
7672|Grampians Group|42966|5|Briefly described|Fig. 25 p47|||||||||
7672|Grampians Group|42971|5|Briefly described|p142|||||||||
7672|Grampians Group|43027|5|Briefly described|p601|||||||||
7672|Grampians Group|43193|5|Briefly described|p71,78.|||Minimum age: Late Silurian-earliest Devonian.||||||
7672|Grampians Group|43218|4|Described|Fig.3 p22, p25|Early Devonian|Late Silurian|||||||
7672|Grampians Group|43461|14|Not recorded|table p625|Early Carboniferous|Late Devonian|||||||
7672|Grampians Group|43547|14|Not recorded|Table p153,154|Famennian|Frasnian|||||||
7672|Grampians Group|43627|5|Briefly described|p2, p6|||Age: 410 Ma.||||||21-OCT-08
7672|Grampians Group|43753|5|Briefly described|p621-624|Early Carboniferous|Late Silurian|||||||
7672|Grampians Group|43846|4|Described|9, 11|Early Devonian|Late Silurian|Intrusives into group aged around 400Ma.||||||21-OCT-08
7672|Grampians Group|44093|5|Briefly described|p47, p91|Early Devonian|Late Silurian|See also p102 Fig 10.3. Geological Province: Kanmantoo Fold Belt.||||||08-MAR-05
7672|Grampians Group|44186|5|Briefly described|Map Legend||Silurian|||||||
7672|Grampians Group|44929|5|Briefly described|Map Legend|Silurian|Ordovician|Includes Mount Difficulty and Red Man Bluff Sub-Groups.||||||14-JUN-06
7672|Grampians Group|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Includes Mount Difficult and Red Man Bluff Sub-Groups.||||||13-JUN-06
7672|Grampians Group|44931|5|Briefly described|Map Legend|Silurian|Ordovician|Sandstone, minor conglomerate and mudstone. Undifferentiated for this interpretation.||||||14-JUN-06
7672|Grampians Group|44932|5|Briefly described|Map Legend|Silurian|Ordovician|Includes Mount Difficulty and Red Man Bluff Sub-Groups.||||||14-JUN-06
7672|Grampians Group|44933|5|Briefly described|Map Legend|Silurian|Ordovician|Includes Mount Difficulty and Red Man Bluff Sub-Groups.||||||14-JUN-06
7672|Grampians Group|48911|6|Mentioned|p7|||Lithology||||||
7672|Grampians Group|49038|6|Mentioned|p22|||||||||
7672|Grampians Group|49040|6|Mentioned|p6|||||||||
7672|Grampians Group|50154|2|Defined|p17, p18 Fig3.1, p110-113|Ludlow|Early Silurian|Max. thickness: 3700m. Overlies the Gringegalgona Granite and unconformably overlies the Nargoon Group. Unconformably overlain by the Rocklands Volcanic Group. Geological Province: Lachlan Fold Belt.||||||15-SEP-04
7672|Grampians Group|50155|5|Briefly described|Map Legend|Silurian|Silurian|Sandstone||||||
7672|Grampians Group|50156|5|Briefly described|Map Legend|Silurian|Silurian|Sandstone: quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded||||||
7672|Grampians Group|50157|5|Briefly described|Map Legend|Silurian|Silurian|Sandstone: quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded||||||
7672|Grampians Group|50158|5|Briefly described|Map Legend|Silurian||Unconformably overlies Nargoon Group. Overlain by Barangaroo Ignimbrite. Sandstone: quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded||||||25-JUN-04
7672|Grampians Group|50159|5|Briefly described|Map Legend|Silurian||Overlies Nargoon Group. Overlain by Barangaroo Ignimbrite, Parilla Sand and Shepparton Formation. Sandstone: quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded.||||||21-OCT-08
7672|Grampians Group|50160|5|Briefly described|Map Legend|Silurian||||||||16-JUN-04
7672|Grampians Group|50161|5|Briefly described|Map Legend|Silurian||Sandstone: quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded.||||||21-OCT-08
7672|Grampians Group|50162|5|Briefly described|Map Legend|Silurian||Quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded sandstone.||||||21-OCT-08
7672|Grampians Group|50163|5|Briefly described|Map Legend|Silurian||Quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded sandstone||||||
7672|Grampians Group|50371|5|Briefly described|Map Legend|Silurian|Silurian|Includes the Willaura Sandstone.||||||21-JUN-04
7672|Grampians Group|50546|6|Mentioned|p1232 Fig.1a|||||||||
7672|Grampians Group|60412|6|Mentioned|p237||||499 +/- 2 Ma (40Ar-39Ar biotite).||||Sandstones.|
7672|Grampians Group|60421|5|Briefly described|p408 Fig. 1, 416, 418 Fig. 5|Silurian|Silurian|||||||
7672|Grampians Group|60451|4|Described|p20, 24, 75, 142-143|Silurian|Silurian|Age: ~425-415Ma Maximum Thickness: ~3700m. Includes Red Man Bluff Subgroup, Silverband Formation.||||||
7672|Grampians Group|60454|5|Briefly described|Map Legend|Silurian|Ordovician|Units do not appear on this map.||||||
7672|Grampians Group|60456|5|Briefly described|Map Legend|Silurian|Ordovician|Sandstone: quartz-rich to micaceous or feldspathic; occasional scattered or lag horizons of vein quartz pebbles; with planar, cross and trough cross lamination, thin to thickly bedded.||||||
7672|Grampians Group|60457|5|Briefly described|Map Legend|Silurian|Ordovician|Units do not appear on this map.||||||24-SEP-04
7672|Grampians Group|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Sandstone: quartz rich to micaceous or feldspathic; occasional scattered or lag horizons of vein quartz pebbles; with planar, trough or trough cross lamination, thin to thickly bedded.||||||
7672|Grampians Group|60459|5|Briefly described|Map Legend|Silurian|Ordovician|Includes: Mount Difficult Sub-Group, Red Man Bluff Sub-Group, Silverband Formation.||||||
7672|Grampians Group|60491|6|Mentioned|p13 Fig.5|||||||||
7672|Grampians Group|60543|5|Briefly described|Map legend|Devonian|Silurian|Terrestrial to marine sandstone with lesser conglomerate and siltstone.||||||23-DEC-09
7672|Grampians Group|61180|5|Briefly described|p5|Early Devonian|Silurian|Overlies Saint Arnaud Beds.||||||
7672|Grampians Group|61181|5|Briefly described|p153 Fig. 47|Devonian|Devonian|Sandstone and shale. ||||||
7672|Grampians Group|61183|3|Fully described|p7, p23-24, p28-33|Early Silurian|Ordovician|Incl: Red Man Bluff Subgp(lower), Silverband Fm(middle) and Difficult Subgp(upper). Fluvial/shallow marine lower quartzo-feldspathic to micaceous sst; intervening micaceous mudst. and upper quartzose sst package. Overlain by Rocklands Volcs. Thick:~3700m.||||||
7672|Grampians Group|61186|6|Mentioned|p76|||Source of the Grampians Sandstone dimension stone in Victoria quarried in the Heatherlie quarry which lies within the Serra Sandstone Formation of the Grampians Group. ||||||
7672|Grampians Group|61187|5|Briefly described|p4, p5 Fig.3, p6, p9, p69. |Silurian||Glenelg Zone, Melbourne Terrane. Marginal marine to terrestrial deposition on the Delamerian Craton. Folded during Benambran Orogeny. Early Devonian A-type volcanics were deposited over this deformed and eroded Group.|||Includes Willaura Sandstone.|||
7672|Grampians Group|61410|5|Briefly described|p7 Fig.2, p8-9|Silurian|Ordovician|Overlies the Glenelg Zone. Crops out as a series of spectacular rugged strike ranges. Hosts only scattered small amounts of gold mineralisation.||||Intruded by the Mafeking Granodiorite|Includes conglomerate hosting minor auriferous quartz veins.|
7672|Grampians Group|61726|5|Briefly described|p924 Fig.3|Silurian|Silurian|||||||
7672|Grampians Group|61749|6|Mentioned|p11, p14|Silurian|Silurian|Includes Red Man Bluff and Mount Difficulty Subgroup seperated by Silverband Formation. Fluvial to shallow marine sequence.||||||21-JAN-10
7672|Grampians Group|61752|4|Described|p10|Silurian|Ordovician|Fluvial to marginal marine sequence. Geological Province: Lachlan Fold Belt.||||||07-FEB-11
7672|Grampians Group|61841|5|Briefly described|p242, p244|Silurian|Silurian|Sediments on the Dundas Tablelands. Overlain by Rocklands Volcanic Group.||||||
7672|Grampians Group|62741|5|Briefly described|p678 Fig. 1, p682|Silurian|Silurian|Predominantly sandstone. A cover sequence overlying a Cambrian basement possibly deposited in Late Ordovician?||||||
7672|Grampians Group|62755|5|Briefly described|p876 Fig. 1|Silurian|Silurian|Sandstone, siltstone. See also p885 Fig. 8. See also misspelt Grampian Group.||||||
7672|Grampians Group|63124|5|Briefly described|p52|Early Devonian|Late Silurian|Thick sequence of quartzose sandstone, red siltstone and shale with minor conglomerate. ||||||
7672|Grampians Group|63446|5|Briefly described|Map legend|Silurian|Silurian||||||Marine, fluvial: sandstone, minor conglomerate, siltstone.|
7672|Grampians Group|63457|5|Briefly described|p123, p125.|||>3.5 km thickness of fluviatile and shallow marine sequences, sourced from Delamerian Highlands to the W (in the Adelaide Fold Belt). Forms two major strike ridges: the Serra and Victoria Ranges.|||||More than 3.5 km thick, including fluviatile and shallow-marine sedimentary sequences.|
7672|Grampians Group|63599|5|Briefly described|p976|Silurian|Silurian|||||||
7672|Grampians Group|64314|5|Briefly described|p495 Fig. 2a, p502|Silurian|Silurian|||||||
7672|Grampians Group|64541|5|Briefly described|Map Legend|Silurian|Silurian|Sandstone: quartz-rich to micaceous or feldspathic, occasional scattered or lag horizions of vein quartz pebbles; laminated, cross-laminated and trough cross-laminated; thin to thickly bedded; shallow marine trace fossils.||||||07-FEB-11
7672|Grampians Group|64597|6|Mentioned|p760 Fig.1. |||||||||
7672|Grampians Group|64610|5|Briefly described|Map legend|Silurian|Ordovician|Includes Red Man Bluff and Mount Difficult Subgroups.  Predominantly sandstones, and conglomerates.||||||12-NOV-08
7672|Grampians Group|64616|6|Mentioned|p343 Fig.23|||||||||
7672|Grampians Group|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Grampians. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
7672|Grampians Group|65313|5|Briefly described|p580, p576|Silurian|Silurian|Quartzites are poorly fossiliferous, riverine and minor intertidal facies. Silurian paleosols studied.||||||26-MAR-12
7672|Grampians Group|65665|6|Mentioned|p1144 Fig.1|Silurian|Silurian|||||||
7672|Grampians Group|66002|5|Briefly described|p5, p5 Tb.3|Silurian|Silurian|Includes Mount Difficult Subgroup, Silverband Formation and Red Man Bluff Subgroup. Defined by Spencer-Jones, 1965. Revised Cayley & Taylor, 1997. Formerly called Grampians sandstone series (Selwyn, 1862) and Grampian sandstone group (Selwyn and Ulrich, 1866)||||||
7672|Grampians Group|66769|5|Briefly described|117, 148|Silurian|Silurian|Grampians-Stavely Zone. Fluvial to shallow marine siliciclastics. Deformed in the Late Silurian-early Devonian. Restricted to Moyston Fault footwall; deposited in a shallow-marine foreland-basin depocentre.||||||
7672|Grampians Group|67104|5|Briefly described|p631 Fig.2, p635, p646, |Early Silurian|Late Ordovician|Confined to the area immediately west of the Moyston Fault. Younger than the Leap Year Group.|ca. 425 Ma|||||
7672|Grampians Group|67127|6|Mentioned|p73|Devonian|Devonian|Forms basement below the WIM 150 heavy mineral deposit.||||Underlies the Renmark Group.||
7672|Grampians Group|67847|6|Mentioned|p10 fig 2.3, p81|Silurian|Silurian|||||||
7672|Grampians Group|68116|5|Briefly described|Appendix, Maps 21, 22, 29, 30, 38.|Early Devonian|Late Ordovician||||||Sandstone, quartz-rich to micaceous or feldspathic; mudstone; minor polymict conglomerate.|05-JUN-14
7672|Grampians Group|68298|5|Briefly described|p220-222|Pragian|Pragian|Includes Early Devonian possible tetrapod trackways. Pragian age based on isotopic evidence. ||||||
7672|Grampians Group|70211|5|Briefly described|p3|Silurian|Late Ordovician|Fluvial to shallow-marine siliciclastic rocks.||||Unconformably overlies Nargoon Group.||
7672|Grampians Group|70493|6|Mentioned|p56||Late Ordovician|Grampians-Stavely Zone, Lachlan Orogen.||||Unconformably overlies Nargoon Group.||
7672|Grampians Group|70877|4|Described|p10, p12-p13, p170-p171|Silurian|Late Ordovician|Grampians-Stavely Zone. Deposited in fluvial to shallow marine environments. Thickest and most structurally complex close to the eastern edge of the Grampians-Stavely Zone.||||Overlies the Nargoon Group and the Rocklands Volcanics. Intruded by the Dwyer Granite, Mirranatwa Granite, Bullawin Porphyry, Mafeking Suite and Duchembegarra Granite.|Sandstone and siltstone.|
7672|Grampians Group|70904|14|Not recorded|p 38|||Stratigraphy.||||||
7672|Grampians Group|70967|6|Mentioned|p3-4, 10-11, 13|Silurian|Late Ordovician|Cayley and Taylor (1997). Fluvial to shallow-marine siliciclastic rocks. Structurally complex.|||||Sandstones and conglomerate.|
7672|Grampians Group|71040|5|Briefly described|p3, p6, p22|||W of the Moyston Fault, but has characteristics of the Lachlan Orogen, including Silurian to Early Devonian sedimentation and deformation. Age given as probably Silurian.||||Is overlain unconformably by Rocklands Volcanics.|Fluvial to shallow-marine deposits.|
7672|Grampians Group|71419|6|Mentioned|p16 Fig 17|Silurian|Silurian|Fluvial and paralic sediments.||||||
7672|Grampians Group|71593|4|Described|p8-p9, p12, p24, p44-p48|Silurian|Ordovician|Silurian. See also p57, p59, p62, p68-p70, p73-p75, p77-p78, p80-p85, p92, p95, p98-p100, p102, p133, p138-p139, p166, p169, p179, p195, p202-p203.|ca. 440 Ma|||Overlain by the Rocklands Volcanic Group. Unconformably overlies the Nargoon Group.|Fluvial to shallow marine red bed sandstone and mudstone.|
7672|Grampians Group|72445|5|Briefly described|p2-3, p9-10, p12, p16, App.1, App.7.|Silurian|Late Ordovician|See also App.2; App.5, App.7 p6 Fig.3. Contains significant structural complexity. Identified in STAVELY02. App.2 is a .csv format file. Also overlies the Nargoon Group.||||Overlies Mount Stavely Volcanic Complex, also in faulted or sheared contact. Intruded by Dwyer Granite, Mirranatwa Granite, Bullawin Porphyry, Mafeking Suite and Duchembegarra Granite.|Dominantly sandstone to conglomeratic sandstone with 0.7-2.3 m lenses of conglomerate. Includes fluvial to shallow marine siliciclastic rocks; sandstone and conglomerate.|15-OCT-20
7672|Grampians Group|73059|6|Mentioned|p1059|Late Ordovician|Late Ordovician|Grampians-Stavely Zone.||||||
7672|Grampians Group|73118|5|Briefly described|p6-8, 14, 19, 42, 48, 53, 64-72, 74|Silurian|Silurian|Glenelg Zone, Western Victoria. A terrestrial to marginal marine sequence. Features basal subhorizontal cataclastic zones; underwent repeated thrusting and extensional faulting.|||Wartook Sandstone.|Is overlain by Rocklands Rhyolite, Shepparton Formation or Loxton-Parilla Sands. Is intruded by Victoria Valley Granite. Is metamorphosed locally by Duchembegarra Granite.|Includes massive to banded quartz sandstones, and intraclast conglomerate.|
7672|Grampians Group|73576|6|Mentioned|p818|Devonian|Devonian|||||||
7672|Grampians Group|74367|6|Mentioned|p16|Early Cambrian|Early Cambrian|||||||
30954|Grand View Syenite|22968|5|Briefly described|P221||Triassic|Highly magnetic||||||
30954|Grand View Syenite|23029|5|Briefly described|Map legend|Triassic|Triassic|Parent is the Mount Leinster Igneous Complex||||||
30954|Grand View Syenite|23030|5|Briefly described|Map legend|Triassic|Triassic|Parent is the Mount Leinster Igneous Complex||||||
30954|Grand View Syenite|60503|6|Mentioned|p65, p66|Triassic|Triassic|Same as Grandview Syenite.||||||
30954|Grand View Syenite|60504|5|Briefly described|Map Legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Biotite-hornblende syenite: A-type; grey to dark grey, coarse grained, porphyritic in orthoclase.||||||
30954|Grand View Syenite|60505|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Biotite-hornblende syenite: A-type; grey to dark grey, coarse grained, porphyritic in orthoclase.||||||
30954|Grand View Syenite|60506|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Biotite-hornblende syenite: A-type; grey to dark grey, coarse grained, porphyritic in orthoclase.||||||
30954|Grand View Syenite|60507|5|Briefly described|Map Legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Biotite-hornblende syenite: A-type; grey to dark grey, coarse grained, porphyritic in orthoclase.||||||07-OCT-04
30954|Grand View Syenite|68116|5|Briefly described|Appendix, Maps 27, 35.|Triassic|Triassic||||||Biotite-hornblende syenite; mid to dark grey, coarse-grained, with orthoclase phenocrysts.|05-JUN-14
7680|Grange Burn Formation|23768|5|Briefly described|p30 Fig.6, p27|Early Pliocene|Late Miocene|Geological Province: Otway Basin.  See also p33, p162.||||||30-MAR-05
7680|Grange Burn Formation|23909|5|Briefly described|p291|Pliocene|Pliocene|||||||
7680|Grange Burn Formation|24551|5|Briefly described|p306, 581||Early Pliocene|||||||
7680|Grange Burn Formation|30393|6|Mentioned|p309|||||||||
7680|Grange Burn Formation|31516|6|Mentioned|p49|||||||||
7680|Grange Burn Formation|33160|6|Mentioned|p300|||See also P303||||||
7680|Grange Burn Formation|34988|6|Mentioned|Table 9.4|||||||||
7680|Grange Burn Formation|35066|3|Fully described|p215|||||||||
7680|Grange Burn Formation|35271|6|Mentioned|Fig.2|||||||||
7680|Grange Burn Formation|38070|6|Mentioned|Fig.12|||Otway Basin||||||
7680|Grange Burn Formation|40756|6|Mentioned|Fig.1.2|||Entered as SA unit. Probably should be VIC.||||||
7680|Grange Burn Formation|40759|5|Briefly described|p70|||||||||
7680|Grange Burn Formation|41043|6|Mentioned|p98|||||||||
7680|Grange Burn Formation|41075|6|Mentioned|p22|||||||||
7680|Grange Burn Formation|41398|6|Mentioned|p3|||||||||
7680|Grange Burn Formation|41537|6|Mentioned|p350|||||||||
7680|Grange Burn Formation|42827|3|Fully described|p289||Tertiary|see also Fig 8.9||||||
7680|Grange Burn Formation|44238|14|Not recorded|Fig.3||Pliocene|||||||
7680|Grange Burn Formation|45128|6|Mentioned|p55|||Originally wrongly entered as a NT unit.||||||
7680|Grange Burn Formation|48911|6|Mentioned|Chart 1|||||||||
7680|Grange Burn Formation|60421|5|Briefly described|p409, 418 Fig. 5|Pliocene|Upper Miocene|||||||
7680|Grange Burn Formation|60785|5|Briefly described|p184 Fig.1, pp186-187.  |Zanclean|Messinian|Of the Otway Basin. Foraminifera dates indicate N17 age (Mallett, 1977). The overlying basalt is dated to 4.35 Ma with K-Ar (Turnbull et al., 1965)Sr/Sr dates from the base indicate 4.0-5.0 Ma max. age (Dickinson et al., 2002). Isolated, rolled, polished and broken fossil cetacean elements.||||Disconformably overlies the Muddy Creek Marl Member.|The base is marked by a phosphatic nodule bed horizon. Shelly marl and sandy to pebbly limestone.|
7680|Grange Burn Formation|61207|5|Briefly described|p280 Fig. 2|Early Pliocene|Early Pliocene|Marls (rich in molluscs) and sands. Underlie the Newer Volcanics, and/or Dorodong Sands. Age: 5.5-4.7Ma; generally considered to be Kalimnan. Geological Province: onshore Otway Basin. See also p283 Fig. 3, p286-287.||||||12-JAN-06
7680|Grange Burn Formation|61841|5|Briefly described|p242|||Marine sediments.  Age: is post-Eocene. Geological Province: Otway Basin.||||||03-JUL-06
7680|Grange Burn Formation|63446|5|Briefly described|Map legend|Pliocene|Miocene||||||Marine: shell beds, sandy limestone, calcareous sand.|
7680|Grange Burn Formation|67061|6|Mentioned|p554 Fig.10.|Pliocene|Pliocene|Otway Basin.||||||
7680|Grange Burn Formation|68116|5|Briefly described|Appendix, Map 38.|Zanclean|Messinian||||||Shell beds, shelly marl, sandy limestone, calcareous sand.|05-JUN-14
78062|Granite Hill Granodiorite|67978|5|Briefly described|p496 Fig.1, p499 Tb.1|||See also Granite Hill granodiorite.|399 +/- 6 Ma (U-Pb; Black, unpub.).|||||19-SEP-14
7705|Grantville Gravels|24551|6|Mentioned|p320|||||||||
7705|Grantville Gravels|30083|6|Mentioned|Map 1|||Quaternary age.||||||
7705|Grantville Gravels|31510|6|Mentioned|p22|||See also Table 1.||||||
7705|Grantville Gravels|33237|6|Mentioned|p57|||||||||
7705|Grantville Gravels|33358|5|Briefly described|Table 1|||Tert.||||||
7705|Grantville Gravels|33462|6|Mentioned|p17|||Refers Jenkin (1962).||||||
7707|Granya Granite|22508|5|Briefly described|p2||Silurian|Keotong Supersuite, Lachlan Fold Belt||||||
7707|Granya Granite|23309|6|Mentioned|p432 App1|||Supersedes Granya Adamellite G103 S-Type.||||||
7707|Granya Granite|29953|5|Briefly described|p13|||||||||
7707|Granya Granite|32684|6|Mentioned|Fig.2|||||||||
7707|Granya Granite|39860|4|Described|p18|||Contains quartz, K-feldspar, plagioclase, biotite and muscovite; abundant xenoliths.||||||30-NOV-04
7707|Granya Granite|41868|6|Mentioned|p478|||||||||
7707|Granya Granite|42726|5|Briefly described|map legend|Silurian||||||||
7707|Granya Granite|44184|5|Briefly described|Map Legend||Early Silurian|Shown as Granya Unassigned.||||||
7707|Granya Granite|64571|6|Mentioned|p825|Early Silurian|Early Silurian|||||||
7707|Granya Granite|68116|5|Briefly described|Appendix, Map 20.|Wenlock|Llandovery||||||Granite: coarse grained, leucocratic; contains quartz, K-feldspar, plagioclase, biotite, muscovite and accessory apatite, zircon, tourmaline and sillimanite; abundant enclaves; S-type.|
7707|Granya Granite|68310|6|Mentioned|p241-242|||Wagga Batholith. Geochemical plots of schistose enclaves.||||||
7707|Granya Granite|69801|5|Briefly described|p2, p4-p5, p122-p127, p135-137|Middle Silurian|Middle Silurian|Central Lachlan Orogen. Occurs on the NSW-Victoria border east of Albury. This unit is the same age as granites near Holbrook but younger than the Granya Granite sampled 10km further south. Sample locality, petrography, zircon characteristics, SHRIMP analyses and interpretation are detailed.|428.2 +/- 2.7 Ma|Koetong Suite||Intruded by the Holbrook Granite.|S-type granite.|
7707|Granya Granite|73457|5|Briefly described|p10-13|Silurian|Silurian|Boundary with the Budginigi Ignimbrite is either a fault or a nonconformity.||||Nonconformably underlies Yambla Formation, faulted against Adaminaby Group|Strongly sheared, contains a well-developed subvertical shear fabric.|
35341|Great Western Formation|24383|6|Mentioned|p57|||||||||
7746|Green Gully Limestone Member|33605|6|Mentioned|Map legend|Miocene|Miocene|||||||
7753|Green Hills Granodiorite|37529|5|Briefly described|p4|||See also P5||||||
7753|Green Hills Granodiorite|42313|3|Fully described|p41|Middle Silurian|Early Silurian|||||||
7753|Green Hills Granodiorite|42314|5|Briefly described|Map|Early Silurian||||||||
7753|Green Hills Granodiorite|42828|5|Briefly described|Fig.2 P128|||||||||
7753|Green Hills Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb9.||||||
7753|Green Hills Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
7753|Green Hills Granodiorite|63290|6|Mentioned|p403 Fig. 6(c)|Silurian|Silurian|Granodiorite.||||||
7753|Green Hills Granodiorite|68115|5|Briefly described|p7.|||Omeo Zone. Most of the supposed Tom Groggin Granite shown by Chappell et al. (1991) continuing well into NSW from Victoria is now shown as Green Hills Granodiorite in the NSW 1:250 000 data. A small outcrop on the SE corner of Corryong, interpreted as Tom Groggin Granite, is now considered to be Green Hills Granodiorite.||||||
7753|Green Hills Granodiorite|68116|5|Briefly described|Appendix, Map 28.|Pridoli|Llandovery||||||Biotite granodiorite and granite: grey, medium to coarse grained, commonly containing cordierite; common metasedimentary xenoliths.|
7753|Green Hills Granodiorite|69801|5|Briefly described|p2, p4-p5, p110-115, p135, p137|Middle Silurian|Middle Silurian|Central Lachlan Orogen. Occurs on the NSW-Victoria border east of Albury. This unit is the same age as granites near Holbrook but younger than the Granya Granite sampled 10km further south.|428.3 +/- 2.1 Ma (SHRIMP U-Pb)|Tom Groggin Suite||Intrudes the Wagga Group.|Medium to coarse-grained, biotite monzogranite and S-type granodiorite.|
7753|Green Hills Granodiorite|73082|6|Mentioned|p17|||Underlies, but is not the source of gold in, the Laurel Hill-Tumbarumba deep lead.||||||
7771|Greensborough Basalt|33604|6|Mentioned|p21|||Strat. diagram.||||||
7771|Greensborough Basalt|66244|5|Briefly described|p7.|Miocene|Miocene|Includes the erosional remnants of basalt flows around the northern suburbs of Melbourne, the Kangaroo Ground area, and an outlier near Lilydale. Was included in the Melbourne Province of Wellman (1974) and the Melbourne Subprovince of Price et al. (2003). Kenley (1967) introduced the term 'Greensborough Phase' as part of the Newer Volcanics; Garratt (1972) included the 'Greensborough Phase' in the Older Volcanics without delineating the area on the map; VandenBerg (1973) mentioned the Greensborough Basalt but also did not show its distribution on a map. May be the same unit as the nearby Monbulk Volcanic Group of very similar age.|17.5 Ma (Wellman 1974); 22 Ma (Bowen 1975).||||Alkali olivine basalt.|14-SEP-12
7771|Greensborough Basalt|68116|5|Briefly described|Appendix, Map 42.|Aquitanian|Aquitanian||||||Basalt: blue-grey; phenocrysts of olivine in groundmass of titanaugite, labradorite laths, pyroxene, iron oxide, interstitial glass; olivine partly altered to serpentine.|
7778|Greenwald-Cobboboonee Basalt|42827|5|Briefly described|Table 9.3, p366|||Variation on Cobboboonee-Greenwald basalt, p367.||||||
37723|Greggs Granodiorite|23309|6|Mentioned|p432, Appendix 1|||G86.Supersedes: Mount Misery Granodiorite.||||||
37723|Greggs Granodiorite|68116|5|Briefly described|Appendix, Map 27.|Wenlock|Llandovery||||||Muscovite-biotite granite: grey; medium to coarse grained; with tourmaline, cordierite, garnet, sillimanite; foliated.|
83434|Gretgrix pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G613.||Of Glenloth Suite|||Strongly magnetically zoned, with magnetic core (to 75 nT) and rim (to 100 nT) separated by a largely nonmagnetic phase; gravity response in south to 200 micrometres/second/second lower than adjacent metasediments but with little difference in north.|
37725|Grieves Granite|23309|6|Mentioned|p432, Appendix 1|||G339, I-type. Supersedes: Nardoo Granite.||||||
37725|Grieves Granite|60452|4|Described|p51|||Supersedes Nardoo Granite. Medium-grained biotite-hornblende granite. Cut by the Buckrabanyule Granite. Mostly in CHARLTON area. See also p17, p47.||||||
37725|Grieves Granite|60461|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Coonooer Suite.  Biotite-hornblende granite, medium-grained.||||||
37725|Grieves Granite|60462|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Coonooer Suite. Granite: I-type, reduced; nonmagnetic; gravity response variable; K, Th and U responses all high.||||||15-SEP-04
37725|Grieves Granite|66002|5|Briefly described|p6 Tb.5|||Of Coonooer Suite.G339. Replaces Nardoo Granite  of Bibby and Moore (1998)||||||
37725|Grieves Granite|68116|5|Briefly described|Appendix, Map 16.|Early Devonian|Early Devonian||||||Biotite hornblende granite: medium grained; I-type; nonmagnetic.|
41190|Gringegalgona Granite|50154|2|Defined|p87, p99, p110, p225 App.1|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex. Nonconformably overlain by the Grampians Group.||||||25-SEP-09
41190|Gringegalgona Granite|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Muscovite granite; S-type||||||
41190|Gringegalgona Granite|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite granite||||||20-AUG-04
41190|Gringegalgona Granite|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite granite||||||20-AUG-04
41190|Gringegalgona Granite|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite granite||||||20-AUG-04
41190|Gringegalgona Granite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite granite||||||20-AUG-04
41190|Gringegalgona Granite|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite granite||||||20-AUG-04
41190|Gringegalgona Granite|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite granite||||||20-AUG-04
41190|Gringegalgona Granite|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite granite||||||20-AUG-04
41190|Gringegalgona Granite|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite granite||||||20-AUG-04
41190|Gringegalgona Granite|66002|6|Mentioned|p9 Tb.5|||G447. Defined by Morand et al. 2003.||||||
41190|Gringegalgona Granite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Massive to foliated muscovite granite; white, medium to coarse grained, porphyritic with phenocrysts of microcline and muscovite; schist and migmatite enclaves abundant; foliation is schlieric with aligned microcline phenocrysts; non-magnetic.|
32299|Grunter Member|13323|5|Briefly described|p393 Fig. 2|Early Paleocene|Early Paleocene|Of the Kingfish Formation (Halibut Subgroup, Latrobe Group). Geological Province: Gippsland Basin.||||||
32299|Grunter Member|24090|5|Briefly described|p8 Fig. 3|Early Paleocene|Early Paleocene|Of the Kingfish Formation (Halibut Subgroup, Latrobe Group). Geological Province: Gippsland Basin.||||||
32299|Grunter Member|24551|6|Mentioned|p478 Fig 15.8||Paleocene|Of the Halibut Subgroup.||||||
32299|Grunter Member|61552|6|Mentioned|p583 Fig.2. |Early Paleocene|Early Paleocene|||Unit in Kingfish Formation.||||
32299|Grunter Member|65717|5|Briefly described|p9 Fig.2.2|Paleocene|Paleocene|||Kingfish Formation||Overlies Kate Shale.|Interbedded sandstone, siltstone and coal.|05-SEP-17
32299|Grunter Member|70076|5|Briefly described|Regional: Fig.3|Danian|Danian|||Kingfish Formation.||Overlies Roundhead Member (Volador Formation) or Kate Shale.||
37741|Gubbins Bridge Granite|23309|6|Mentioned|p432, Appendix 1|||G392, I-Type.||||||
7883|Gunbower Limestone|41868|6|Mentioned|p601|||||||||
37742|Gundowring Granite|23309|6|Mentioned|p432, Appendix 1|||G171.||||||
37742|Gundowring Granite|24551|6|Mentioned|p717 Table 2.4|Wenlock|Llandovery |Age: 429 +/- 1.4Ma.||||||
41774|Gunns pluton|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: inferred from low response in the gravity data; nonmagnetic. GSV map code: G473.||||||
41774|Gunns pluton|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: inferred from low response in the gravity data; nonmagnetic. GSV map code: G473.||||||07-FEB-11
41774|Gunns pluton|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: inferred from low response in the gravity data; nonmagnetic. GSV map code: G473.||||||
41774|Gunns pluton|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: inferred from low response in the gravity data; nonmagnetic. GSV map code: G473.||||||
41774|Gunns pluton|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: low gravity response (-480 to -400 ums^-2); nonmagnetic, background is weakly magnetic (30 nT). GSV map code: G473.||||||
25939|Gurnard Formation|13323|5|Briefly described|p393 Fig. 2|Early Oligocene|Middle Eocene|Of the Cobia Subgroup (Latrobe Group). Marine clastics. Geological Province: Gippsland Basin.||||||
25939|Gurnard Formation|13324|5|Briefly described|p94 Fig. 4, Fig.5|Eocene|Eocene|Gippsland Basin.||Of Latrobe Group||||
25939|Gurnard Formation|13332|5|Briefly described|p184 Fig.2|Oligocene|Eocene|Geological Province: Gippsland Basin.||||||
25939|Gurnard Formation|22663|5|Briefly described|V97 - G1 to G4 Fig.2|Eocene|Eocene|||||||01-MAR-10
25939|Gurnard Formation|23230|4|Described|Table4-1p40, 44|Oligocene||||||||
25939|Gurnard Formation|24038|5|Briefly described|p439 Fig.2|Oligocene|Eocene|Geological Province: Gippsland Basin.||||||12-FEB-08
25939|Gurnard Formation|24054|5|Briefly described|p46|Eocene|Eocene|Of Latrobe Group.  Geological Basin: Gippsland Basin.||||||
25939|Gurnard Formation|24090|5|Briefly described|p8 Fig.3|Oligocene|Eocene|Geological Province: Gippsland Basin.||||||
25939|Gurnard Formation|24164|6|Mentioned|p20 Fig.12, p28|Oligocene|Eocene|||Latrobe Group||Is unconformably overlain by Lakes Entrance Formation|Mafic volcanic rocks|
25939|Gurnard Formation|24211|5|Briefly described|p84, p85 Fig. 2|Eocene|Eocene|Of the Latrobe Group. Geological Province: Gippsland Basin.  See also p87 Fig. 4.||||||12-FEB-08
25939|Gurnard Formation|24407|5|Briefly described|p13 Fig.2|Early Oligocene|Middle Eocene|Geological Province: Gippsland Basin||||||
25939|Gurnard Formation|24495|5|Briefly described|p9, p10|||Of Cobia Subgroup.  Shallow to open marine deposits.  Geological Province: Gippsland Basin.||||||
25939|Gurnard Formation|24551|5|Briefly described|p262 Fig. 9.29, 477, 607|Oligocene|Eocene|Of the Cobia Subgroup.||||||
25939|Gurnard Formation|29355|6|Mentioned|p190|||||||||
25939|Gurnard Formation|29721|6|Mentioned|p192|||||||||
25939|Gurnard Formation|29736|6|Mentioned|Fig.2|||||||||
25939|Gurnard Formation|29974|6|Mentioned|Fig.1|||||||||
25939|Gurnard Formation|31352|6|Mentioned|p134|||Late Eocene||||||
25939|Gurnard Formation|31480|2|Defined|p71|late Eocene|late Eocene|See also P72, 73||||||
25939|Gurnard Formation|32162|6|Mentioned|Fig.3|||Correlation chart||||||
25939|Gurnard Formation|32574|6|Mentioned|p73|||See also P75||||||
25939|Gurnard Formation|33320|6|Mentioned|p57|||Eocene||||||
25939|Gurnard Formation|33362|6|Mentioned|p112|||||||||
25939|Gurnard Formation|35013|6|Mentioned|p397|||||||||
25939|Gurnard Formation|35067|6|Mentioned|Fig.3|||||||||
25939|Gurnard Formation|35273|4|Described|p269|||||||||
25939|Gurnard Formation|35573|6|Mentioned|Fig.3|||Chronostratigraphic section - Gippsland Basin||||||
25939|Gurnard Formation|36643|6|Mentioned|Fig.7|||||||||
25939|Gurnard Formation|37809|6|Mentioned|p7|||||||||
25939|Gurnard Formation|38929|6|Mentioned|p45|||||||||
25939|Gurnard Formation|40715|6|Mentioned|Fig.16|||||||||
25939|Gurnard Formation|41213|5|Briefly described|Fig.2|||||||||
25939|Gurnard Formation|41259|5|Briefly described|p448|||||||||
25939|Gurnard Formation|41282|6|Mentioned|p33|||||||||
25939|Gurnard Formation|41534|5|Briefly described|p53|||||||||
25939|Gurnard Formation|41727|5|Briefly described|p433|||||||||
25939|Gurnard Formation|41868|6|Mentioned|p521|||||||||
25939|Gurnard Formation|42083|4|Described|p347|||See also Fig.9||||||
25939|Gurnard Formation|42311|5|Briefly described|Fig.2 P526|||||||||
25939|Gurnard Formation|42827|4|Described|p343|||see also Fig 12.17, Of Latrobe Valley Group.||||||12-FEB-08
25939|Gurnard Formation|43145|5|Briefly described|p10|Oligocene|Late Eocene|Of Latrobe Group.||||||12-FEB-08
25939|Gurnard Formation|60538|5|Briefly described|p475 Fig. 14|Early Oligocene|Middle Eocene|Geological Province: Gippsland Basin.||||||
25939|Gurnard Formation|61155|5|Briefly described|p3, p18|Late Eocene|Middle Eocene|Of the Latrobe Group. Shallow-marine glauconitic clastics. Underlies Lakes Entrance Formation. Thickness: 120m. Geological Province: Gippsland Basin (offshore).||||||
25939|Gurnard Formation|61323|5|Briefly described|p3 Fig. 3|Oligocene|Eocene|Geological Province: Gippsland Basin.||||||
25939|Gurnard Formation|61328|5|Briefly described|p112 Fig. 3|Oligocene|Eocene|Geological Province: Gippsland Basin.||||||
25939|Gurnard Formation|61336|5|Briefly described|p(iv) Fig. 4|Early Oligocene|Early Oligocene|Of Cobia Group. See also Gurnard formation. Geological Province: Gippsland Basin. See also p(v) Fig. 5.||||||07-FEB-11
25939|Gurnard Formation|61469|5|Briefly described|p33|||Overlies Strzelecki Group rocks, and in places, Halibut Subgroup; underlies Lakes Entrance Formation. Geological Province: Gippsland Basin.||||||12-FEB-08
25939|Gurnard Formation|61552|5|Briefly described|p583 Fig.2, p586, p590. |Early Oligocene|Middle Eocene|||Unit in Cobia Subgroup.||Locally overlies Halibut Group. Is overlain by Seaspray Group.|A thin section, typically non-calcareous glauconitic facies.|
25939|Gurnard Formation|64876|5|Briefly described|p145 Fig.2|Oligocene|Eocene|Gippsland Basin.||Cobia Subgroup.||||
25939|Gurnard Formation|65717|5|Briefly described|p6, p9 Fig.2.2, p11-14, p17, p19-23, p25|Oligocene|Eocene|See also p28; Appendix 3. James and Evans (1971). Shallow- to open-marine facies deposit: a condensed section. Highly variable seal capacity. Thickness is highly variable may be as thin as 7m and thicker than 78m. MICP anlaysis results.||Cobia Subgroup||Unconformably overlies Kingfish, Opah and Flounder Formations. Unconformably overlain by Swordfish, Lakes Entrance Formations.|Interbedded sandstone, siltstone and fine- to medium-grained glauconitic siliciclastics.|05-SEP-17
25939|Gurnard Formation|65718|5|Briefly described|p12, p38|Eocene|Eocene|James and Evans (1971). Shallow to open marine depositional setting. Acts as a giant seal for some of the hydrocarbon fields offshore - considered a potential sealing facies for coal seam gas in some areas. Middle to Late Eocene age.||Of the Cobia Subgroup.||Overlain by the Latrobe Group.|A condensed section composed of fine- to medium-grained glauconitic siliciclastics.|10-JAN-17
25939|Gurnard Formation|65973|4|Described|p16, p22, p57, p78, p82, p85-87|Oligocene|Oligocene|Gippsland Basin. Deposited in a shallow to open marine environment. Intersected in Kipper-1, Kipper-2, Judith-1, East Pilchard-1, Longtom-1, Longtom-1/ST-1, Longtom-2/ST-1, Sweep-1 and many more drillholes (see appendix). See also p90, p97, p100, p102, p112, p114, p123, p126, p129-134, p136, p142-143, p149, p151, p171.||Cobia Subgroup||||
25939|Gurnard Formation|67727|5|Briefly described|p58 Fig.2, p60 Fig.3, p74 Fig.9, p79.|Late Eocene|Late Eocene|Offshore Gippsland Basin. Marine deposits.||Unit in Traralgon Formation.||Overlies Dutson Sand Member. Is overlain by Lakes Entrance Formation.|Biogenic carbonate limestones and marls.|
25939|Gurnard Formation|70028|6|Mentioned|p79|Oligocene|Eocene|||||||
25939|Gurnard Formation|70076|5|Briefly described|South-Eastern:Fig.2;Regional:Fig.3;p3,p7|Rupelian|Lutetian|Transgressive shallow to open marine sediments. Acts as a seal as well as a reservoir unit; hosts the Patricia-Baleen gas accumulation.||Cobia Subgroup||Overlies Burong or Flounder Formation.|A condensed section characterised by fine- to medium-grained glauconitic siliciclastic sediments.|
25939|Gurnard Formation|73289|6|Mentioned|p764, 768, 776|||Latrobe Valley, Gippsland Basin.||||Lateral facies variation of Traralgon 0 and 1 Seams. Transitions laterally into the Dutson Sand Member. Equivalent to Burong Formation.|Offshore (marine) basin sediments; thin, condensed marine clays.|
25939|Gurnard Formation|73471|5|Briefly described|p86|||Gippsland Basin.||Cobia Subgrop||Overlies Burong Formation, underlies Lakes Entrance Formation, Gippsland Limestone|Marine clastics.|
25939|Gurnard Formation|73488|5|Briefly described|p632|||Correlated with Traralgon Formation coal measures, and interpreted as the offshore equivalent of the Traralgon Formation coastal plains facies.|||||Condensed clastic marine unit. Contains glauconitic fine sandstones and siltstones.|
25939|Gurnard Formation|73562|5|Briefly described|p303, 312|Eocene|Eocene|Gippsland Basin; offshore. Strongly diachronous. Appears as Gurnard Greensand on p312.||Topmost Latrobe Group.|||Thin, glauconitic sandstone.|
25939|Gurnard Formation|73640|6|Mentioned|p2-3|Eocene|Paleocene|A condensed marine section of the Latrobe Group.||Latrobe Group||||
25939|Gurnard Formation|75065|5|Briefly described|p151, 168|Eocene|Eocene|Gippsland Basin; offshore. Widespread shallow marine and deltaic sands.||Cobia Subgroup.||Adjacent to and locally overlies Burong Formation. Is overlain locally by Lakes Entrance Formation.|Siltstone,  glauconitic sandstones.|
37743|Guys Forest Granodiorite|23309|5|Briefly described|p432 Appendix 1|Silurian|Silurian|G572, I-Type. Age: 413+/3Ma.||||||
37743|Guys Forest Granodiorite|24133|3|Fully described|p69|Silurian|Silurian|I-type granodiorite.  Parent: Boggy Plain Supersuite.  Intrudes the Corryong Granite and the Allwood Granodiorite.  Geological Province: Lachlan Fold Belt. Age: 413 +/- 3 Ma (K/Ar)||||||13-SEP-04
37743|Guys Forest Granodiorite|24142|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||
37743|Guys Forest Granodiorite|24143|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||
37743|Guys Forest Granodiorite|24144|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||
37743|Guys Forest Granodiorite|24145|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||13-SEP-04
37743|Guys Forest Granodiorite|24146|5|Briefly described|Map Legend|Devonian|Devonian|Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||
37743|Guys Forest Granodiorite|68116|5|Briefly described|Appendix, Map 20.|Pragian|Lochkovian|Informally subdivided into hornblende and biotite granodiorite phases.|||||Hornblende granodiorite: pale grey, medium grained; few enclaves; I-type; intensely magnetic. Biotite granodiorite: grey, medium grained, mostly foliated; I-type; non-magnetic.|
32294|Halibut Subgroup|13323|5|Briefly described|p393 Fig. 2|Middle Eocene|Maastrictian|Of the Latrobe Group. Non-marine to paralic clastics; marine clastics. Geological Province: Gippsland Basin. See also p394 Fig. 3.||||||
32294|Halibut Subgroup|24090|5|Briefly described|p8 Fig.3|Eocene|Late Cretaceous|Of Latrobe Group. Geological Province: Gippsland Basin.||||||
32294|Halibut Subgroup|24164|6|Mentioned|p3,26 Fig.16,27 Fig.17,28-29,41 Tb.2,44|||Gippsland Basin||||||
32294|Halibut Subgroup|24495|5|Briefly described|p10|||Includes Kingfish Formation.  Geological Province: Gippsland Basin.||||||
32294|Halibut Subgroup|24551|5|Briefly described|p260, 262 Fig. 9.29, 269, 477|Eocene|Late Cretaceous|Of the Latrobe Group.||||||
32294|Halibut Subgroup|61469|6|Mentioned|p33|||Geological Province: Gippsland Basin.||||||
32294|Halibut Subgroup|61552|4|Described|p581, pp583-585, p595 Fig.14. |Early Eocene|Maastrichtian|Deposited during a margin sag-phase, involving rapid subsidence in response to sea floor spreading in the adjacent Tasman Sea. Contains the principal reservoir intervals intersected in the major oil fields in the Gippsland Basin.||Unit in Latrobe Group.|Includes Barracouta, Volador, Mackerel, Flounder and Kingfish Formations and Kate Shale.||Most sediments occur in two coal-bearing successions, separated to the east by marine shale.|
32294|Halibut Subgroup|64876|5|Briefly described|p145 Fig.2|Eocene|Maastrichtian|Gippsland Basin.||Latrobe Group.|Barracouta, Volador, Kingfish, Mackerel, Flounder Formations; Kate Shale.|Overlies Golden Beach Subgroup (Seahorse Unconformity). Is overlain by Cobia Subgroup (Marlin Unconformity).||
32294|Halibut Subgroup|65717|5|Briefly described|p9 Fig.2.2, p11-13, p28|Paleocene|Maastrichtian|Hosts the bulk of the hydrocarbons in the Gippsland Basin. Documents the changes from non-marine to marine environments. Includes intraformational seals.||Latrobe Group|Kingfish, Barracouta, Mackerel, Flounder, Volador Formations; Kate Shale; Currajung, Bream Volcanics.|Unconformably overlies Golden Beach Subgroup, Unconformably overlain by Cobia Subgroup||05-SEP-17
32294|Halibut Subgroup|65718|5|Briefly described|p5, p14 Fig 3.2, p12, p41, p43 Fig 5.4|Eocene|Late Cretaceous|Hosts the bulk of the hydrocarbons in the Gippsland Basin and comprises five formations that are distinguished according to their dominant depositional facies. Equivalent in age to the Yarram Formation.||Of the Latrobe Group.|||Includes coarse to pebbly sandstone.|
32294|Halibut Subgroup|65973|5|Briefly described|p14-16, p19, p22-23, p29, p42, p57, p62|||Gippsland Basin. Hosts the bulk of hydrocarbons in the Gippsland Basin. Sandstones were deposited in fluvial, coastal barrier and marine environments. Intersected in the Kipper-1 drillhole, Leatherjacket-1, Judith-1, Hammerhead-1, East Pilchard-1, Longtom-1, Longtom-1/ST-1, Longtom-2/ST-1, Northright-1, Sweep-1 and many more drillholes (see appendix). See also p70-72, p74, p76, p78, p80, p82, p84-86, p88, p90, p93, p97, p100, p102, p104, p106, p108-110, p112, p114, p116, p118, p123-140, p142-144, p171.||Latrobe Group|Includes the Barracouta Formation, Voldor Formation, Kingfish Formation, Kate Shale and the Mackerel Formation.||Sandstones.|
32294|Halibut Subgroup|66181|5|Briefly described|p310 Fig.5|Eocene|Maastricht|Unconformably underlies the Cobia Subgroup, unconformably overlies the Golden Beach Subgroup. Non marine to paralic clastics, in the Latrobe Group.||||||
32294|Halibut Subgroup|69879|5|Briefly described|p428|Eocene|Maastrichtian|Post-rift Gippsland Basin. ~500m thick.||Latrobe Group||Overlies Strzelecki Group.|Gently folded siliciclastics.|
32294|Halibut Subgroup|70028|6|Mentioned|p79|Eocene|Maastrichtian|Gippsland Basin.||Latrobe Group.||Unconformably overlies Golden Beach Subgroup. Is overlain unconformably by Cobia Subgroup.||
32294|Halibut Subgroup|70076|5|Briefly described|South-Eastern: Fig.2; p2-3|Ypresian|Campanian|See also Regional: Fig.3; p3-5, p7. Hydrocarbon source rocks and a major reservoir unit. A succession of fluvial, deltaic and marine sediments deposited across the Basin.||Latrobe Group.|Volador, Mackerel, Flounder, Kingfish, Barracouta Formations; Kate Shale.|Overlies Golden Beach Subgroup. Is overlain by Cobia Subgroup.|Includes coals and carbonaceous shales (source rocks) and marine near-shore barrier and shoreface sandstones (reservoirs).|
32294|Halibut Subgroup|70331|5|Briefly described|p69|Eocene|Late Cretaceous|Gippsland Basin (western).||Latrobe Group.||Unconformably overlies Golden Beach Subgroup. Is overlain unconformably by Cobia Subgroup.|Onshore: fluvial to paralic sandstone, siltstone, shale, coal. Offshore: marine sandstone, siltstone.|
32294|Halibut Subgroup|73471|5|Briefly described|p86-89, p91 Fig.4, p93 Fig.5, p103, p108|Ypresian|Campanian|Gippsland Basin. Coastal-plain-dominated siliciclastic sag-phase deposits. Overlies the Seahorse Unconformity, underlies the Marlin Unconformity. Contains hydrocarbon source rocks.|78-46.5 Ma|Latrobe Group|Volador Formation, Kate Shale, Mackerel Formation, Kingfish Formation, Barracouta Formation|Unconformably overlies Golden Beach Subgroup, unconformably underlies Cobia Subgroup||
32294|Halibut Subgroup|75065|5|Briefly described|p149, 151, 154-155, 164, 166|Eocene|Maastrichtian|Gippsland Basin; mostly offshore. Non-marine to shallow marine sediments. Contains reservoirs and potential petroleum source rocks.||Latrobe Group.|Barracouta, Volador, Mackerel, Kingfish, Flounder, Yarram Formations; Kate Shale; Currajung, Bream Volcanics.|Unconformably overlies Golden Beach Subgroup. Is overlain unconformably by Cobia Subgroup.||
34854|Hallets Road Tonalite|22968|5|Briefly described|P71, P199||Late Silurian|New name, parent is Polar Star Suite||||||
34854|Hallets Road Tonalite|23029|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is the Polar Star Suite||||||
34854|Hallets Road Tonalite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Polar Star Suite||||||
34854|Hallets Road Tonalite|23309|6|Mentioned|p432 App1|||G148 I-Type.||||||
34854|Hallets Road Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Biotite tonalite: grey; medium-grained equigranular; massive to weakly foliated; rare small microgranitoid enclaves; local intense chlorite-hematite alteration.|
37744|Halls Paddock Diorite|23309|6|Mentioned|p432, Appendix 1|||G 583.||||||
37744|Halls Paddock Diorite|24142|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
37744|Halls Paddock Diorite|24143|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
37744|Halls Paddock Diorite|24144|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
37744|Halls Paddock Diorite|24145|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt||||||
37744|Halls Paddock Diorite|24146|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37744|Halls Paddock Diorite|68116|5|Briefly described|Appendix.|Early Devonian|Early Devonian||||||Hornblende diorite: dark grey to green, coarse, equigranular to strongly porphyritic; intensely magnetic.|
8011|Hamilton Basalt|34988|6|Mentioned|Table 9.4|||||||||
21939|Handford Creek Formation|23309|5|Briefly described|p36, Table 2.7||Cambrian|Of the Jamieson Volcanics.||||||
21939|Handford Creek Formation|24551|5|Briefly described|p87|||Of Jamieson Volcanics (fig.3.15)||||||
21939|Handford Creek Formation|24576|6|Mentioned|p731|||Geological Province: Lachlan Fold Belt||||||
21939|Handford Creek Formation|61187|6|Mentioned|p51 Fig.2. |Early Cambrian|Early Cambrian|||Unit in Jamieson Volcanics.||||
21939|Handford Creek Formation|68116|5|Briefly described|Appendix, Map 34.|Cambrian|Cambrian||||||Sandstone, shale, conglomerate: volcanigenic; marine.|
38326|Hapuku Subgroup|13323|5|Briefly described|p394 Fig. 3|Pleistocene|Middle Miocene|Of the Seaspray Group. Geological Province: Gippsland Basin.||||||
38326|Hapuku Subgroup|23625|5|Briefly described|p61|Miocene|Miocene|Parent: Seaspray Group.  Geological Province: Gippsland Basin||||||
38326|Hapuku Subgroup|24468|5|Briefly described|p405 Fig.2|||Geological Province: Gippsland Basin. Of the Seaspray Group. Underlying Unit: Albacore Subgroup||||||
38326|Hapuku Subgroup|24551|5|Briefly described|p355|Quaternary|Neogene|Geological Province: Gippsland Basin.  Of the Seaspray Group.||||||
38326|Hapuku Subgroup|60538|5|Briefly described|p483 Fig. 22|||Geological Province: Gippsland Basin.||||||
38326|Hapuku Subgroup|66181|5|Briefly described|p310 Fig.5|Pleistocene|Late Miocene|Marine clastics and carbonates, in the Seaspray Group.||||||10-SEP-14
38326|Hapuku Subgroup|70076|5|Briefly described|South-Eastern: Fig.2; Regional: Fig.3|Pliocene|Miocene|||Seaspray Group.|Whiting Formation.|Overlies Albacore Subgroup.||
8069|Harcourt Granodiorite|22502|6|Mentioned|P251|||||||||
8069|Harcourt Granodiorite|22885|5|Briefly described|map|||||||||
8069|Harcourt Granodiorite|22886|4|Described|Table.1|||Age: Rb/Sr 375;368 Ma.||||||
8069|Harcourt Granodiorite|23106|5|Briefly described|p528|||||||||
8069|Harcourt Granodiorite|23107|5|Briefly described|p522||Devonian|||||||
8069|Harcourt Granodiorite|23109|5|Briefly described|p512|||||||||
8069|Harcourt Granodiorite|23232|6|Mentioned|p62|||||||||
8069|Harcourt Granodiorite|23234|6|Mentioned|p91|||||||||
8069|Harcourt Granodiorite|23261|5|Briefly described|p274, 286-7||Late Devonian|Max Age: 358 (+/-) 15 Ma.||||||
8069|Harcourt Granodiorite|23269|6|Mentioned|Fig14-3.1p403|||||||||
8069|Harcourt Granodiorite|23300|5|Briefly described|Map Legend|Devonian|Devonian|Of Harcourt Suite.||||||21-OCT-08
8069|Harcourt Granodiorite|23301|5|Briefly described|Map Legend|Devonian|Devonian|Of Harcourt Suite.||||||21-OCT-08
8069|Harcourt Granodiorite|23302|5|Briefly described|Map Legend|Devonian|Devonian|Of Harcourt Suite.||||||21-OCT-08
8069|Harcourt Granodiorite|23303|5|Briefly described|Map Legend|Devonian|Devonian|Of Harcourt Suite.||||||21-OCT-08
8069|Harcourt Granodiorite|23304|5|Briefly described|Map Legend|Devonian|Devonian|Of Harcourt Suite.||||||21-OCT-08
8069|Harcourt Granodiorite|23305|4|Described|p44 Table 6, 7||Late Devonian|of Cherry and Wilkinson (1994). Age: 361+/-7, 367+/-2 and 375+/-7 Ma K/Ar. Of Harcourt Suite. Central Victorian Magmatic Province.||||||
8069|Harcourt Granodiorite|23308|6|Mentioned|Map Legend|||Mine name?||||||
8069|Harcourt Granodiorite|23309|5|Briefly described|p254, 256, 348, 350||Late Devonian|G290 - I Type.  Age: 361+/-7Ma, 367+/-2Ma, 375+/-7 Ma.||||||
8069|Harcourt Granodiorite|23603|5|Briefly described|p11|Late Devonian|Late Devonian|||||||
8069|Harcourt Granodiorite|24134|4|Described|p9|||||||||
8069|Harcourt Granodiorite|24177|3|Fully described|p62|Late Devonian|Late Devonian|Previously mapped as Harcourt Batholith (King & Wilkinson, 1975; Wilkinson et al., 1995). Intruded by the Baringhup Granodiorite. Intrudes the Castlemaine Group. Age: 368 Ma (K/Ar, 1989)||||||11-MAY-04
8069|Harcourt Granodiorite|24180|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Granodiorite, medium-grained, equigranular to slightly porphyritic, with plagioclase (albite, andesine and labradorite), orthoclase, quartz and biotite, accessory apatite, ilmenite, sphene and zircon.||||||21-OCT-08
8069|Harcourt Granodiorite|24312|5|Briefly described|p1081, p1080 Fig.3|Devonian|Devonian|||||||
8069|Harcourt Granodiorite|24328|5|Briefly described|Map legend|Devonian|Devonian|||||||
8069|Harcourt Granodiorite|24329|5|Briefly described|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
8069|Harcourt Granodiorite|24383|5|Briefly described|p9 Fig.1|||Parent: Harcourt Suite. Geological Province: Lachlan Fold Belt.||||||21-OCT-08
8069|Harcourt Granodiorite|24384|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Harcourt Suite.||||||
8069|Harcourt Granodiorite|24385|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Harcourt Suite.||||||
8069|Harcourt Granodiorite|24386|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Harcourt Suite.  Biotite granodiorite: medium-grained; equigranular to weakly porphyritic in plagioclase, quartz and feldspar.||||||
8069|Harcourt Granodiorite|24387|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Harcourt Suite. Biotite granodiorite; medium-grained; equigranular to weakly porphyritic in plagioclase, quartz and K-feldspar||||||
8069|Harcourt Granodiorite|24388|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Harcourt Suite. Age: 368+/-5Ma (K/Ar). Biotite granodiorite; reduced I-type; nonmagnetic, high K, moderate-high Th and U, high total radioelements, areas of deeper weathering have low K; areas with high Th may be related to monazite occurrence.||||||
8069|Harcourt Granodiorite|24439|6|Mentioned|p56 App. 2|||Geological Province: Lachlan Fold Belt.||||||
8069|Harcourt Granodiorite|24440|5|Briefly described|Map legend|||||||||
8069|Harcourt Granodiorite|24551|6|Mentioned|p717, 718 Table 2.4, 8.1.|Late Devonian|Middle Devonian|Age: 385 +/- 6Ma, 368 +/- 2Ma.||||||
8069|Harcourt Granodiorite|29712|6|Mentioned|p83|||||||||
8069|Harcourt Granodiorite|30936|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
8069|Harcourt Granodiorite|31654|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
8069|Harcourt Granodiorite|32001|6|Mentioned|p78|||||||||
8069|Harcourt Granodiorite|33394|6|Mentioned|p70|||||||||
8069|Harcourt Granodiorite|34735|6|Mentioned|p22|||||||||
8069|Harcourt Granodiorite|34986|6|Mentioned|p333|||||||||
8069|Harcourt Granodiorite|34990|6|Mentioned|p442|||||||||
8069|Harcourt Granodiorite|35277|6|Mentioned|p98|||||||||
8069|Harcourt Granodiorite|35278|5|Briefly described|p354|||||||||
8069|Harcourt Granodiorite|37501|6|Mentioned|p405|||||||||
8069|Harcourt Granodiorite|40522|6|Mentioned|p230|||||||||
8069|Harcourt Granodiorite|41641|6|Mentioned|p168|||||||||
8069|Harcourt Granodiorite|41849|6|Mentioned|p405|||||||||
8069|Harcourt Granodiorite|41868|6|Mentioned|p464|||See also P595||||||
8069|Harcourt Granodiorite|42154|6|Mentioned|Table 1 P334|||||||||
8069|Harcourt Granodiorite|42682|6|Mentioned|p20|||||||||
8069|Harcourt Granodiorite|42827|5|Briefly described|p168|||see also Fig 5.1||||||
8069|Harcourt Granodiorite|43199|5|Briefly described|Map Legend||Late Devonian|||||||
8069|Harcourt Granodiorite|43211|2|Defined|p4,24,Fig.5 p15,23||Devonian|2 ages of 367+/-7Ma (Ka-Ar) Previously been described as adamellite (McInerny 1929)||||||
8069|Harcourt Granodiorite|43261|5|Briefly described|Map Legend||Late Devonian|||||||
8069|Harcourt Granodiorite|43282|6|Mentioned|p80|||||||||
8069|Harcourt Granodiorite|43493|4|Described|22-67||Late Devonian|Ages: 375Ma, 368Ma. Medium grained, equigranular leucocratic adamellite also includes granodiorite, granite, aplite, pegmatite and porphyry dykes.||||||03-SEP-04
8069|Harcourt Granodiorite|43787|5|Briefly described|p800, Fig1||Late Devonian|||||||
8069|Harcourt Granodiorite|44186|5|Briefly described|Map Legend||Late Devonian|G290 I-type.||||||21-OCT-08
8069|Harcourt Granodiorite|44197|5|Briefly described|Map Legend||Late Devonian|G290 I-Type.||||||
8069|Harcourt Granodiorite|61179|6|Mentioned|p20|||Intruded by lamprophyre dykes dated to 149+/-5Ma and 159+/-6Ma. (Byrne 1985a) indicating Late Jurassic age.||||||
8069|Harcourt Granodiorite|64312|6|Mentioned|p439 Tb. 2|||Chemical analysis information.||||||
8069|Harcourt Granodiorite|65665|6|Mentioned|p1145 Fig. 2, p1152-p1153, p1158, p1161|Late Devonian|Late Devonian|||||||
8069|Harcourt Granodiorite|65715|5|Briefly described|p8 Tb.4|||G290. Of Harcourt Batholith.||||||
8069|Harcourt Granodiorite|65969|5|Briefly described|p19, p25 Tb.3.1, p26 Fig.13|Tournaisian|Frasnian|Extensively mobilised the mineralisation at nearby Maldon. Ages range from 361+/-7 Ma (K/Ar biotite) to 375+/-7 Ma (K/Ar biotite). U-Pb zircon date of 369 +/- 2 Ma (Bierlein et al., 2001). Magnetic. Called Harcourt Granite on p19 and 25.||||||
8069|Harcourt Granodiorite|68116|5|Briefly described|Appendix, Maps 23-24, 31-32.|Late Devonian|Late Devonian||||||Biotite granodiorite: medium grained, pale grey; equigranular to weakly porphyritic in plagioclase, quartz and K-feldspar; numerous enclaves; nonmagnetic; reduced; I-type.|
8069|Harcourt Granodiorite|68189|6|Mentioned|p21|||||||||
8069|Harcourt Granodiorite|68576|6|Mentioned|QLD_D1: p10|||Used in St. John's Cathedral, Brisbane.||||||
8069|Harcourt Granodiorite|69089|5|Briefly described|Map legend|Late Devonian|Late Devonian|I-type.||||||
8069|Harcourt Granodiorite|70904|14|Not recorded|p 30|||Refers to Thomas 1934, Beavis 1963.||||||
8069|Harcourt Granodiorite|71020|14|Not recorded|p175|||Narrow metamorphic aureole.||||||
8069|Harcourt Granodiorite|73497|5|Briefly described|Map legend|Late Devonian|Late Devonian|G290.||Harcourt Suite|||Granodiorite: I-type; nonmagnetic, weakly magnetic dykes (less than 5 nT); moderately magnetic aureole (up to 35 nT); high K, Th and U; gravity low of 120 micrometres/second/second.|
8070|Harcourt Suite|23300|5|Briefly described|Map Legend|Devonian|Devonian|||||||
8070|Harcourt Suite|23301|5|Briefly described|Map Legend|Devonian|Devonian|||||||
8070|Harcourt Suite|23302|5|Briefly described|Map Legend|Devonian|Devonian|||||||
8070|Harcourt Suite|23303|5|Briefly described|Map Legend|Devonian|Devonian|||||||
8070|Harcourt Suite|23304|5|Briefly described|Map Legend|Devonian|Devonian|||||||
8070|Harcourt Suite|23305|4|Described|p44||Late Devonian|Central Victorian Magmatic Province||||||
8070|Harcourt Suite|23309|5|Briefly described|p347|||||||||
8070|Harcourt Suite|24383|5|Briefly described|p9 Fig.1|||Geological Province: Lachlan Fold Belt||||||
8070|Harcourt Suite|24384|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes the Harcourt Granodiorite, Metcalfe Granite and Baringhup Granodiorite.||||||
8070|Harcourt Suite|24385|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes the Harcourt Granodiorite, Metcalfe Granite and the Baringhup Granodiorite.||||||
8070|Harcourt Suite|24386|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes the Harcourt Granodiorite, Metcalfe Granite and the Baringhup Granodiorite.||||||
8070|Harcourt Suite|24387|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes the Harcourt Granodiorite, Metcalfe Granite and the Baringhup Granodiorite.||||||
8070|Harcourt Suite|24388|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes the Harcourt Granodiorite, Metcalfe Granite and the Baringhup Granodiorite.||||||
8070|Harcourt Suite|24551|6|Mentioned|p221|||||||||
8070|Harcourt Suite|42726|5|Briefly described|map legend|||||||||
8070|Harcourt Suite|42827|6|Mentioned|p435|||||||||
8070|Harcourt Suite|65715|5|Briefly described|p8 Tb.4|||Includes Harcourt Batholith and Tullaroop Granodiorite.||||||
8070|Harcourt Suite|73497|5|Briefly described|Map legend|Late Devonian|Late Devonian||||Harcourt Granodiorite, Baringhup Granodiorite|||
31528|Harcourt Supersuite|42726|5|Briefly described|map legend|||||||||
73158|Hardie Hill Complex|61896|5|Briefly described|p59|||Member of a prominent NNE-trending belt of volcanoes which includes Mount Mercer, Mount Buninyong, Mount Warrenheip and Clarkes Hill.||||||24-FEB-14
21945|Hardwicke Creek Rhyolite|23309|5|Briefly described|p36, Table 2.7||Cambrian|Of the Jamieson Volcanics.||||||
21945|Hardwicke Creek Rhyolite|24551|5|Briefly described|p87|||Of Jamieson Volcanics (fig.3.15)||||||
21945|Hardwicke Creek Rhyolite|24576|6|Mentioned|p731|||Geological Province: Lachlan Fold Belt||||||
21945|Hardwicke Creek Rhyolite|61187|6|Mentioned|p51 Fig.2. |Early Cambrian|Early Cambrian|||Unit in Jamieson Volcanics.||||
21945|Hardwicke Creek Rhyolite|68116|5|Briefly described|Appendix, Map 34.|Cambrian|Cambrian||||||Rhyolite lava, breccia, volcaniclastic sediments; marine.|
37745|Harringtons Tonalite|23309|6|Mentioned|p432, Appendix 1|||G578, I-Type.||||||
37745|Harringtons Tonalite|24133|3|Fully described|p71|Silurian|Silurian|Parent: Surveyors Creek Suite.  Geological Province: Lachlan Fold Belt.||||||
37745|Harringtons Tonalite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Of Surveyors Creek Suite. Geological Province: Lachlan Fold Belt.||||||
37745|Harringtons Tonalite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Of Surveyors Creek Suite. Geological Province: Lachlan Fold Belt.||||||
37745|Harringtons Tonalite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Of Surveyors Creek Suite. Geological Province: Lachlan Fold Belt.||||||
37745|Harringtons Tonalite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Of Surveyors Creek Suite.  Geological Province: Lachlan Fold Belt||||||
37745|Harringtons Tonalite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Of Surveyors Creek Suite. Geological Province: Lachlan Fold Belt.||||||
37745|Harringtons Tonalite|68116|5|Briefly described|Appendix.|Pridoli|Wenlock||||||Hornblende tonalite: mid to dark grey, medium grained; strongly foliated; contains several large hornfels rafts; I-type; nonmagnetic.|
8103|Harrow Granodiorite|23309|5|Briefly described|p335|||G407  S-Type||||||
8103|Harrow Granodiorite|23319|4|Described|p408 Fig. 1,  p411, p415|Ordovician|Cambrian|Known as 'Harrow Granodiorite' by Turner et al (1993). Muscovite-bearing granitic rock in homogeneous tors; medium-grained with phenocrysts of poikilitic microcline and abundant biotite with lesser primary muscovite||||||20-MAY-13
8103|Harrow Granodiorite|24012|5|Briefly described|p217|||||||||
8103|Harrow Granodiorite|24551|5|Briefly described|p77, p717 Table 2.4|Early Ordovician|Early Ordovician|Of the Glenelg River Complex.  Age: 487 +/- 6Ma, 481 +/- 2Ma.||||||
8103|Harrow Granodiorite|30928|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian - Ordovician||||||
8103|Harrow Granodiorite|33602|6|Mentioned|p10|||||||||
8103|Harrow Granodiorite|42275|5|Briefly described|p473|||||||||
8103|Harrow Granodiorite|42889|4|Described|p282|||age of 466 +/- 6 Ma||||||
8103|Harrow Granodiorite|42971|5|Briefly described|p153|||||||||
8103|Harrow Granodiorite|50154|2|Defined|p91, p96-97, p247 App.5|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex. Applied by Turner et al. (1993) to all granitic rocks in the Harrow area, but defined by Kemp & Gray (1999) as one of many individual granite bodies. Intrudes Kout Norien Granodiorite.||||||15-SEP-04
8103|Harrow Granodiorite|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Biotite-muscovite granite; S-type||||||
8103|Harrow Granodiorite|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granite||||||20-AUG-04
8103|Harrow Granodiorite|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granite||||||20-AUG-04
8103|Harrow Granodiorite|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granite||||||20-AUG-04
8103|Harrow Granodiorite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granite||||||20-AUG-04
8103|Harrow Granodiorite|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granite||||||20-AUG-04
8103|Harrow Granodiorite|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granite||||||20-AUG-04
8103|Harrow Granodiorite|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granite||||||20-AUG-04
8103|Harrow Granodiorite|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granite||||||20-AUG-04
8103|Harrow Granodiorite|66002|6|Mentioned|p8 Tb.5|||G407. Defined by Kemp and Gray 1999.||||||
8103|Harrow Granodiorite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Biotite-muscovite granite: foliated to massive, grey, medium grained, porphyritic with phenocrysts of plagioclase; accessory sillimanite; rare schlieren; nonmagnetic.|
38464|Harts Paddock Diorite|24133|3|Fully described|p76|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
37236|Hassall Creek Granodiorite|23991|6|Mentioned|p188 Fig.2|||||||||
37236|Hassall Creek Granodiorite|24012|5|Briefly described|p219|||||||||
37236|Hassall Creek Granodiorite|50154|2|Defined|p31, p105-107|Early Ordovician|Late Cambrian|Intruded by the Rocklands Volcanic Group and Coleraine Volcanic Group. Overlain by the Coleraine Group. Age: 410 +/- 4 Ma, 401 +/- 5 Ma (K/Ar), ~465 Ma (Ar/Ar). The granodiorite is older than Middle Ordovician, probably Late Cambrian to Early Ordovician.||||||15-SEP-04
37236|Hassall Creek Granodiorite|65716|4|Described|p11-15|Tremadocian|Furongian|From Nareen and part of Coleraine 1:50k sheets. High-level, coarse grained, equigranular granodiorite. Quartz, plagioclase, orthoclase, biotite, hornblende, magnetite, sphene, allanite, apatite and zircon. SHRIMP zircon U-Pb magmatic age of 487.3 +/- 2.9 Ma.||||||
37236|Hassall Creek Granodiorite|68116|5|Briefly described|Appendix, Maps 29, 38.|Floian|Tremadocian|Age written as Lancefieldian in text. Includes minor quartz diorite: fine to medium grained, equigranular dominated by hornblende, plagioclase and biotite, with minor quartz, clinopyroxene, alkali feldspar and chalcopyrite; magnetic.|||||Biotite-hornblende granodiorite: massive, grey, medium to coarse grained, equigranular; accessory magnetite and sphene; rare mafic microgranitoid enclaves. |
8153|Haunted Hills Formation|23885|6|Mentioned|p163 Fig. 14.3|||Geological Province: Gippsland Basin.||||||
8153|Haunted Hills Formation|23909|5|Briefly described|p295|Pliocene|Pliocene|Geological Province: Gippsland Basin.||||||
8153|Haunted Hills Formation|33689|6|Mentioned|Table 3|||||||||
8153|Haunted Hills Formation|34558|5|Briefly described|p19|||Pliocene.||||||18-SEP-18
8153|Haunted Hills Formation|61181|5|Briefly described|p109, p112|Pliocene|Pliocene|Fluvial deposits - succession of cross-bedded and lenticular gravels, sands and clays - in which kaolinitic clays have been identified in the Boisdale area. Also a useful quartz sand resource in west central Gippsland. ||||||
8153|Haunted Hills Formation|65718|6|Mentioned|p10 Fig 3.2|Pleistocene|Pliocene|See also Haunted Hill Formation.||||||
8153|Haunted Hills Formation|66181|6|Mentioned|p295|Pliocene||Fluvial gravel deposits. See also Haunted Hills Gravel (p294 Fig.2, p295 Fig.3).||||||10-SEP-14
8153|Haunted Hills Formation|66244|5|Briefly described|p5, p6.|||||||Locally overlies the Aberfeldy Basalt and the Neerim Volcanic Group.||
8153|Haunted Hills Formation|67061|6|Mentioned|p554 Fig.10.|Pleistocene|Pliocene|Latrobe Valley, Gippsland Basin.||||||
8153|Haunted Hills Formation|68116|5|Briefly described|Appendix, Maps 36, 43-44, 51-53, 56-57.|Pleistocene|Pliocene||||||Sand, silt, gravel: various shades of brown, yellow, red, white; variably sorted; variably rounded; crudely to well-bedded; commonly strongly oxidised with ironstone near the top and also within the formation.|
8153|Haunted Hills Formation|69750|6|Mentioned|p68|Pliocene|Pliocene|On-shore Gippsland Basin.||||Unconformably overlies Yallourn Formation.||
8153|Haunted Hills Formation|70076|5|Briefly described|Regional: Fig.3|Holocene|Pleistocene|||Sale Subgroup.||Overlies Coongulmerang Formation.||
8153|Haunted Hills Formation|73562|5|Briefly described|p303-304|Pleistocene|Pliocene|Gippsland Basin; onshore.||||Lateral equivalent to Jemmys Point Formation.|Fluvial gravels.|
8189|Hawksview Granite|23309|6|Mentioned|p448 App1|||This publication lists it as an obsolete granite name, but later GSV publications have used the name.||||||06-SEP-07
8189|Hawksview Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
8189|Hawksview Granite|32684|6|Mentioned|p250|||See also Fig.2. Petrology P252||||||
8189|Hawksview Granite|37029|6|Mentioned|p48|||||||||
8189|Hawksview Granite|39331|6|Mentioned|p27|||||||||
8189|Hawksview Granite|40328|4|Described|p207|||||||||
8189|Hawksview Granite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
8189|Hawksview Granite|40498|6|Mentioned|p392|||||||||
8189|Hawksview Granite|42726|5|Briefly described|map legend|Silurian||||||||
8189|Hawksview Granite|60085|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
8189|Hawksview Granite|70777|5|Briefly described|p2, p63, p81|Pridoli|Pridoli|Lachlan Orogen.|422.0 +/- 3.0 Ma (Keay et al., 1999)|||||
31589|Hawksview Suite|42726|5|Briefly described|map legend||Silurian|||||||
25049|Hazelwood Formation|23909|6|Mentioned|p298|||||||||
25049|Hazelwood Formation|24551|5|Briefly described|p327 Fig. 10.33|Miocene|Miocene|||||||
25049|Hazelwood Formation|35273|6|Mentioned|p266|||||||||
25049|Hazelwood Formation|38928|6|Mentioned|Fig.14|||||||||
25049|Hazelwood Formation|41868|4|Described|p520|||||||||
25049|Hazelwood Formation|42827|4|Described|p340|||||||||
25049|Hazelwood Formation|60538|5|Briefly described|p488 Fig. 27|||Geological province: Gippland Basin or Latrobe Valley.||||||
25049|Hazelwood Formation|63217|4|Described|p97, p102, p105, p109, p110, p112.   |Late Miocene|Middle Miocene|Traralgon Syncline. >150m thick. Palynologically dated. Lateral equivalent to Boisdale Formation. Less carbonaceous than usual; meandering river deposits.||||Overlies the Yallourn Seam. Is overlain by Haunted Hill Formation.|Clay to sandy clay.|
25049|Hazelwood Formation|65718|6|Mentioned|p10 Fig 3.2|Pliocene|Miocene|Late Miocene minimum age.||||||
25049|Hazelwood Formation|73289|6|Mentioned|p766 Fig.3|||||||Overlies Yallourn Coal Seam. Is overlain by Haunted Hill Formation.||
74894|Hearns Mudstone Member|64010|5|Briefly described|p258 Fig.1. |Tournaisian|Tournaisian|||Of the Snowy Plains Formation.||||
74894|Hearns Mudstone Member|64536|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation (Mansfield Group). Mudstone, minor sandstone: mudstone is grey and red, thin bedded, laminated: sandstone is thin bedded. Recessive; fluvial deposits.||||||07-FEB-11
74894|Hearns Mudstone Member|64537|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation (Mansfield Group). Mudstone, minor sandstone: mudstone is grey and red, thin bedded, laminated: sandstone is thin bedded. Recessive; fluvial deposits.||||||07-FEB-11
74894|Hearns Mudstone Member|64538|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation (Mansfield Group). Mudstone, minor sandstone: mudstone is grey and red, thin bedded, laminated: sandstone is thin bedded. Recessive; fluvial deposits.||||||07-FEB-11
74894|Hearns Mudstone Member|64606|5|Briefly described|Map Legend|Neogene|Neogene|Of Snowy Plains Formation. Mudstone, minor sandstone: alluvial deposits. Blue to pink in RGB with large areas of green probably due to Th enrichment in regolith. Nonmagnetic.||||||
74894|Hearns Mudstone Member|64616|4|Described|p140, p299|Early Carboniferous|Early Carboniferous|New member of Snowy Plains Formation. Conformably overlies Lanky Creek Sandstone Member with gradational contact. Is overlain conformably by Devils Plain Siltstone Member. ~100m thick. Dominantly red and grey mudstone, minor thin-bedded sandstone. Geophysical characteristics given.||||||
32300|Heart Member|70076|6|Mentioned|Regional: Fig.3|Paleocene|Paleocene|||Kingfish Formation.||||
8207|Heath Hill Silt|29679|6|Mentioned|p140|||||||||
8207|Heath Hill Silt|32002|6|Mentioned|p115|||||||||
8207|Heath Hill Silt|33237|6|Mentioned|p61|||||||||
8207|Heath Hill Silt|33458|6|Mentioned|p23|||||||||
8207|Heath Hill Silt|33462|4|Described|p17|||Hydrogeology P33.||||||
8207|Heath Hill Silt|35276|6|Mentioned|p245|||||||||
8207|Heath Hill Silt|42827|5|Briefly described|p319|||||||||
68647|Heathcote Volcanic Group|24551|6|Mentioned|p609|||||||||
68647|Heathcote Volcanic Group|64611|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Includes Lazy Bar Andesite, Mount William Metabasalt and undifferentiated Heathcote Volcanic Group.||||||15-DEC-08
68647|Heathcote Volcanic Group|64612|2|Defined|p26, p29-30, p42, p57, p65|Cambrian|Early Cambrian|Named by Edwards et al. (1998) as Heathcote Volcanics. Of Dja Dja Wrung Supergroup. Confomably overlain by Knowsley East Shale (sharp contact). Thickness: 1600m. Igneous and sedimentary rocks in a deep marine setting.||||||30-JAN-15
68647|Heathcote Volcanic Group|64619|5|Briefly described|Map legend|Cambrian|Cambrian|Includes Mount William Metabasalt.||||||03-NOV-08
68647|Heathcote Volcanic Group|65715|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Dja Dja Wrung Supergroup. Includes Sheoak Gully Boninite, Lazy Bar Andesite, Mount William Metabasalt and unnamed diorite dykes.||||||
68647|Heathcote Volcanic Group|65719|5|Briefly described|p7-8|Cambrian|Cambrian|||||Overlain by Castlemaine Group.|Ocean floor basalts with some boninites and black shales.|10-MAY-12
68647|Heathcote Volcanic Group|65969|5|Briefly described|p3,p11,p15, p17 Fig.7,p19,p31,p36-37|Cambrian|Cambrian|Basement to Castlemaine Group, Knowsley East Shale and Goldie Chert. Includes Mount William Metabasalt, Sheoak Gully Boninite and Lazy Bar Andesite. Basaltic and boninitic volcanics. Repeatedly thrust over itself in the Rochester Antiformal Stack, in Bendigo Zone.||||||
68647|Heathcote Volcanic Group|66769|6|Mentioned|119, 132, 145|Cambrian|Cambrian|Laterally continuous packages of coherent massive and pillowed metabasalt; low-grade, greenschist facies. Underlies Knowsley East Shale and Goldie Chert.||||||
68647|Heathcote Volcanic Group|67104|6|Mentioned|p640|||||||||
68647|Heathcote Volcanic Group|68116|5|Briefly described|Appendix, Map 24.|Cambrian|Early Cambrian||||||Mafic to minor felsic igneous rocks, sandstone, mudstone, chert.|
68647|Heathcote Volcanic Group|71593|4|Described|p35|Lower Cambrian||Basalts in this group are compositionally similar to the Magdala Basalt. Age derived from trilobite fossils (VandenBerg et al, 2000).||||||
68647|Heathcote Volcanic Group|73497|5|Briefly described|Map legend|Cambrian|Cambrian|||Dja Dja Wrung Supergroup|Sheoak Gully Boninite, Lazy Bar Andesite, Mount William Metabasalt|||
68647|Heathcote Volcanic Group|73505|6|Mentioned|p8|||||||||
8219|Heathfield Sandstone Member|22674|5|Briefly described|Fig.2 p719|Albian|Albian|||||||
8219|Heathfield Sandstone Member|24551|5|Briefly described|p251||Albian|||||||
8219|Heathfield Sandstone Member|24562|5|Briefly described|p6|||Geological Province: Otway Basin.||||||
8219|Heathfield Sandstone Member|41269|5|Briefly described|p245|||||||||
8219|Heathfield Sandstone Member|41642|6|Mentioned|Table 7.4|||||||||
8219|Heathfield Sandstone Member|41726|6|Mentioned|p422|||||||||
8219|Heathfield Sandstone Member|42152|6|Mentioned|Fig.2 P4|||||||||
8219|Heathfield Sandstone Member|42827|5|Briefly described|Table 7.4|||||||||
8219|Heathfield Sandstone Member|61329|6|Mentioned|p121|||||||||
8219|Heathfield Sandstone Member|63124|5|Briefly described|p70|||Of the Eumeralla Formation and in wide usage, but not yet formally defined. No designated type section. Geological Province: Otway Basin.||||||
8219|Heathfield Sandstone Member|70077|5|Briefly described|Regional: Fig.4|Albian|Aptian|Otway Basin: Robe-Penola Trough.||Eumeralla Formation.||||
8219|Heathfield Sandstone Member|72050|6|Mentioned|p243|||Is described as ""a member of the Eumeralla Formation"" but is given the formal rank only on p243. A possible reservoir target in the Tantanoola Trough. See references to Heathfield Sandstone on p233 Fig.2, 235-236, 238.||||||
41920|Hemleys Granite|60452|6|Mentioned|p54|||Formerly known as Glenloth Granite. Appears to have been intruded by the Barraport pluton in CHARLTON, and the Tunstalls pluton.||||||
41920|Hemleys Granite|66002|5|Briefly described|p6 Tb.5|||Of Glenloth Suite. G333. See VandenBerg et al 2000. Replaces the superseded Glenloth Granite of Bibby and Moore (1998)||||||
41920|Hemleys Granite|68116|5|Briefly described|Appendix, Map 16.|Middle Devonian|Early Devonian||||||Biotite-muscovite granite: coarse grained; I-type.|
41920|Hemleys Granite|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G333.||Of Glenloth Suite|||Magnetic responses to 150 nT above surrounds; gravity response mostly less than 5 micrometres/second/second.|
37560|Hemsley Suite|23309|5|Briefly described|p339|||Supersedes Glenloth Suite.||||||
8294|Hermit Granite|23309|6|Mentioned|p433, App1|||G580 I-Type||||||
8294|Hermit Granite|24133|3|Fully described|p74|Late Silurian|Late Silurian|Intrudes the Omeo Metamorphic Complex.  Geological Province: Lachlan Fold Belt.||||||
8294|Hermit Granite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
8294|Hermit Granite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Of Surveyors Creek Suite. Geological Province: Lachlan Fold Belt.||||||
8294|Hermit Granite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
8294|Hermit Granite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Biotite granite:grey, medium to coarse grained, foliated quartz-phyric; strong to moderate porphyritic texture, slightly stretched quartz phenocrysts to 10mm; I-type; nonmagnetic; weathered||||||09-SEP-04
8294|Hermit Granite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Biotite granite: I-type; nonmagnetic; weathered; low K, Th, U. G580a is weakly magnetic, G580b is highly magnetic||||||09-SEP-04
8294|Hermit Granite|31800|6|Mentioned|p204|||||||||
8294|Hermit Granite|68116|5|Briefly described|Appendix.|Pridoli|Wenlock|Informally subdivided into weakly and highly magnetic phases.|||||Biotite granite: grey, medium to coarse grained, foliated quartz-phyric; strong to moderate porphyritic texture, slightly stretched quartz phenocrysts to 10 mm; I-type; weakly to highly magnetic.|
8294|Hermit Granite|70910|14|Not recorded|p44|||Cassiterite p44, map opposite. ||||||
21957|Hesket Ignimbrite|22886|5|Briefly described|p15|||||||||
21957|Hesket Ignimbrite|23309|5|Briefly described|p170|||||||||
21957|Hesket Ignimbrite|44197|5|Briefly described|Map Legend||Late Devonian|||||||
21957|Hesket Ignimbrite|64619|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Macedon Volcanics Group. Rhyolite ignimbrite; red to dark grey, fine-grained, vitric-rich with garnet phenocrysts; densely welded, pyroclastic deposits.||||||03-NOV-08
21957|Hesket Ignimbrite|65715|3|Fully described|p3, p5-6, p7 Tb.4|Devonian|Devonian|Newly defined. Basal formation of Macedon Igneous Complex. Underlies Willimigongong Ignimbrite (conformably?). Only a small area exposed at the foot of the Macedon range near Hesket. Number of different ignimbrite flows. Inferred faulted contact or angular unconformity with Castlemaine Group. Variable thickness, but at least 50 m. Dark grey, fine-grained (glassy) and porphyritic. Phenocryst-poor. Contains plagioclase, K-feldspar, minor biotite and/or enstatite, quartz, garnet and opaques. Intruded by unnamed porphyry.||||||
21957|Hesket Ignimbrite|68116|5|Briefly described|Appendix, Map 32.|Late Devonian|Late Devonian||||||Rhyolite ignimbrite: red to dark grey; fine-grained; vitric-rich; with garnet phenocrysts; densely welded to rheomorphic.|
8304|Hesse Clay|37583|6|Mentioned|Fig.2|||||||||
8304|Hesse Clay|62068|5|Briefly described|p134|||Informal name||||Also called 'Post Miocene Clay'. Southern correlate of the Timboon Surface Laterite.|Laterite|
8304|Hesse Clay|68991|5|Briefly described|p465, p465 Fig.2, p466, p468|Miocene|Miocene|Late Miocene age. (Gill 1965; Shoemaker and Uhlherr 1999).||||Disconformably underlain by the Port Campbell Limestone. Disconformably overlain by the Bridgewater Formation.|Comprises a pale to dark brown pedogenic unit.|
8304|Hesse Clay|73486|5|Briefly described|p509, p511-513, p516-517, p519-522, p534|Pleistocene|Pleistocene|Considered possibly coeval with or younger than Newer Volcanics, post-dates the Timboon/Hanson Plain surface. Appears to be a derivative of Newer Volcanics. See also p526.||||Overlies Port Campbell Limestone|Thin surface interval of a dense clayey mud, made up of quartz silt, kaolinite, microcline feldspar silt, and anatase. Dark soil and claystone.|
8311|Heytesbury Group|22587|6|Mentioned|p79 Fig.7|Middle Miocene|Late Eocene|||||||
8311|Heytesbury Group|22626|6|Mentioned|446 fig 10|Early Miocene|Early Miocene|Geol province West Otway Basin. Overlying unit Naracoorte Limestone Member, underlying unit Gambier Limestone||||||
8311|Heytesbury Group|22674|5|Briefly described|p718, Fig.2 p719|Late Miocene|Early Oligocene|||||||
8311|Heytesbury Group|22875|4|Described|p65-72, p26-27, p59, 135, 149-151|Late Miocene|Early Oligocene|Age: ~7-29 Ma. Apatite fission track ages: 7.9+/-1.3 Ma, 6.2+/-2.3 Ma||||||19-SEP-18
8311|Heytesbury Group|22938|6|Mentioned|p233|||||||||
8311|Heytesbury Group|22944|5|Briefly described|Fig3|Miocene|Oligocene|||||||
8311|Heytesbury Group|23226|5|Briefly described|p889|||Separated from Murray basin by Padthaway Ridge Paleozoic Basement. of Gambier Basin.||||||26-JUN-13
8311|Heytesbury Group|23230|4|Described|Table4-1p40, 42, 44|Miocene|Eocene|||||||
8311|Heytesbury Group|23249|5|Briefly described|p143 Fig.2||Miocene|Of Otway Basin.||||||24-JUL-08
8311|Heytesbury Group|23307|5|Briefly described|Map Legend|Miocene|Miocene|||||||
8311|Heytesbury Group|23322|5|Briefly described|957 Fig.2|Miocene|Oligocene|Geological Province: Gambier Basin (SA) and Otway Basin (VIC).||||||07-SEP-09
8311|Heytesbury Group|23417|6|Mentioned|p6|||||||||
8311|Heytesbury Group|23778|5|Briefly described|p660|||Geological Province: Otway Basin.||||||
8311|Heytesbury Group|23792|5|Briefly described|p26|Recent|Eocene|Carbonates and siliciclastics. Geological Province: Otway Basin||||||26-JUN-13
8311|Heytesbury Group|23939|6|Mentioned|Fig.5|||May be Late Oligocene to Middle Miocene in age.||||||
8311|Heytesbury Group|24056|5|Briefly described|p84, p87|||Geological Basin: Otway Basin.||||||
8311|Heytesbury Group|24200|5|Briefly described|p423 Fig. 15, 16.|||Heytesbury Group Equivalents discussed throughout text.||||||
8311|Heytesbury Group|24314|5|Briefly described|p60, p61 Fig.2|Miocene|Eocene|Geological Province: Otway Basin.||||||
8311|Heytesbury Group|24323|5|Briefly described|p136 Fig. 3|Miocene|Oligocene|Unconformably overlies the Nirranda Group. Geological Province: Otway Basin.||||||
8311|Heytesbury Group|24344|5|Briefly described|p69|Miocene|Oligocene|||||||
8311|Heytesbury Group|24551|5|Briefly described|p246|Miocene|Oligocene|Consists of: Clifton Formation, Gellibrand Marl, Port Campbell Limestone.||||||
8311|Heytesbury Group|24562|5|Briefly described|p8, 35 Fig. 2|Miocene|Oligocene|Geological Province: Otway Basin.||||||
8311|Heytesbury Group|24563|6|Mentioned|p485|Tertiary|Tertiary|||||||
8311|Heytesbury Group|29355|6|Mentioned|p179|||||||||
8311|Heytesbury Group|29823|5|Briefly described|p14|||||||||
8311|Heytesbury Group|29856|6|Mentioned|p41|||||||||
8311|Heytesbury Group|30522|6|Mentioned|Map legend|Miocene|Oligocene|Oligo-Miocene||||||
8311|Heytesbury Group|30576|5|Briefly described|Table 2|||||||||
8311|Heytesbury Group|30578|6|Mentioned|p9|||||||||
8311|Heytesbury Group|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
8311|Heytesbury Group|30928|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
8311|Heytesbury Group|30932|6|Mentioned|Map legend|Tertiary|Tertiary|Equivalent Glenelg Group and Nirranda Group in part.||||||
8311|Heytesbury Group|31036|1|Redefined|p210|late Tertiary|middle Tertiary|Middle to Late Tertiary. See also Table 19-1.||||||
8311|Heytesbury Group|31424|6|Mentioned|Table 2|||Lithostratigraphy||||||
8311|Heytesbury Group|31534|6|Mentioned|p369|||See also Table 19-3||||||
8311|Heytesbury Group|31625|6|Mentioned|Fig. 5.2|||Oligocene-Miocene||||||
8311|Heytesbury Group|31746|6|Mentioned|p194|||||||||
8311|Heytesbury Group|32162|6|Mentioned|p58|||See also Fig. 5||||||
8311|Heytesbury Group|32499|6|Mentioned|p107|||Miocene||||||
8311|Heytesbury Group|33135|5|Briefly described|p17|||||||||
8311|Heytesbury Group|33230|6|Mentioned|Encl.12.1|||Olig. - Miocene||||||
8311|Heytesbury Group|33807|6|Mentioned|p97|||||||||
8311|Heytesbury Group|33940|6|Mentioned|p414|||||||||
8311|Heytesbury Group|34063|6|Mentioned|p2|||Olig.-Mioc. Table||||||
8311|Heytesbury Group|34954|6|Mentioned|Fig.35|||||||||
8311|Heytesbury Group|35013|6|Mentioned|p393|||||||||
8311|Heytesbury Group|35066|4|Described|p208|||p221.||||||31-JAN-07
8311|Heytesbury Group|35262|6|Mentioned|p4|||||||||
8311|Heytesbury Group|35271|6|Mentioned|p66|||||||||
8311|Heytesbury Group|35274|6|Mentioned|p423|||||||||
8311|Heytesbury Group|35285|6|Mentioned|p414|||||||||
8311|Heytesbury Group|35290|6|Mentioned|p38|||||||||
8311|Heytesbury Group|35722|6|Mentioned|p4|||Stratigraphy.||||||
8311|Heytesbury Group|36499|6|Mentioned|p43|||||||||
8311|Heytesbury Group|36913|6|Mentioned|p79|||||||||
8311|Heytesbury Group|37385|6|Mentioned|p9|||||||||
8311|Heytesbury Group|37548|6|Mentioned|p131|||||||||
8311|Heytesbury Group|38221|6|Mentioned|Fig.4|||Otway Basin||||||
8311|Heytesbury Group|38625|6|Mentioned|p272|||||||||
8311|Heytesbury Group|38717|5|Briefly described|p20|||||||||
8311|Heytesbury Group|39315|6|Mentioned|Fig.7|||||||||
8311|Heytesbury Group|39967|6|Mentioned|p44|||||||||
8311|Heytesbury Group|41016|5|Briefly described|Mention|||||||||
8311|Heytesbury Group|41043|6|Mentioned|p97|||||||||
8311|Heytesbury Group|41185|5|Briefly described|p175|||||||||
8311|Heytesbury Group|41269|5|Briefly described|p246|||||||||
8311|Heytesbury Group|41487|5|Briefly described|p625|||||||||
8311|Heytesbury Group|41701|6|Mentioned|Map legend|early Miocene||||||||
8311|Heytesbury Group|41704|6|Mentioned|p100|||||||||
8311|Heytesbury Group|41714|6|Mentioned|p301|||||||||
8311|Heytesbury Group|41726|6|Mentioned|p421|||||||||
8311|Heytesbury Group|41769|5|Briefly described|p30|||||||||
8311|Heytesbury Group|41868|5|Briefly described|p535|||||||||
8311|Heytesbury Group|42075|5|Briefly described|Fig.13 P252|||||||||
8311|Heytesbury Group|42152|6|Mentioned|Fig.2 P4|||||||||
8311|Heytesbury Group|42184|6|Mentioned|Fig.2 P348|||||||||
8311|Heytesbury Group|42318|6|Mentioned|p8|||||||||
8311|Heytesbury Group|42453|6|Mentioned|p20|||||||||
8311|Heytesbury Group|42524|5|Briefly described|Fig.3 P27|||||||||
8311|Heytesbury Group|42827|4|Described|p282|||see also Fig 8.10||||||
8311|Heytesbury Group|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
8311|Heytesbury Group|43171|6|Mentioned|2-8|Middle Miocene|Late Oligocene|Age 10-30 Ma||||||
8311|Heytesbury Group|43195|5|Briefly described|Map Legend|Middle Miocene|Late Eocene|see also commentary on back of map.||||||
8311|Heytesbury Group|43208|5|Briefly described|map legend|Late Miocene|Oligocene|Of Middle Oligocene to Late Miocene age.||||||24-JUL-08
8311|Heytesbury Group|43219|5|Briefly described|Fig.3,p6.|Miocene|Oligocene|||||||
8311|Heytesbury Group|43590|4|Described|p23|||||||||
8311|Heytesbury Group|43604|6|Mentioned|p144,Fig.1|Miocene|Oligocene|||||||
8311|Heytesbury Group|43667|6|Mentioned|Fig.3,p12|Miocene|Oligocene|||||||
8311|Heytesbury Group|43686|5|Briefly described|p233|||||||||
8311|Heytesbury Group|43733|6|Mentioned|Fig.2.11,p65|Pliocene|Miocene|||||||
8311|Heytesbury Group|43744|6|Mentioned|Fig.3,p3|||||||||
8311|Heytesbury Group|43783|6|Mentioned|Fig14, p11|Neogene|Late Oligocene|||||||
8311|Heytesbury Group|43784|6|Mentioned|Fig10, p12|Neogene|Late Oligocene|||||||
8311|Heytesbury Group|43937|5|Briefly described|Map Legend|Early Oligocene|Middle Eocene|||||||
8311|Heytesbury Group|44133|5|Briefly described|p156|Middle Miocene|Late Eocene|Geological Province: Gambier Basin. Includes: Gambier Limestone, Gellibrand Marl.||||||04-FEB-08
8311|Heytesbury Group|44135|6|Mentioned|p49|Miocene|Late Oligocene|Mentioned in the context of correlates.||||||07-DEC-09
8311|Heytesbury Group|44186|5|Briefly described|Map Legend||Miocene|||||||
8311|Heytesbury Group|46802|6|Mentioned|Table 1|||||||||
8311|Heytesbury Group|48581|4|Described|p37|||See also p12,13,28,39. Fig.4,6,7,Pl.1,2. (J54-12/Port Campbell).||||||
8311|Heytesbury Group|48911|3|Fully described|p26|Late Eocene|Miocene|||||||03-JUL-06
8311|Heytesbury Group|48977|6|Mentioned|p1,p2|||See also P59, Table 3||||||
8311|Heytesbury Group|49060|5|Briefly described|Fig.33|||||||||
8311|Heytesbury Group|50154|5|Briefly described|p26, p135|||Geological Province: Otway Basin. Includes: Clifton Formation, Gellibrand Marl and Port Campbell Limestone.||||||
8311|Heytesbury Group|60421|5|Briefly described|p408 Fig. 1, 409|Oligocene|Upper Eocene|Overlies: Wangerrip Group. Includes: Gellibrand Marl, Clifton Formation, Port Campbell Formation.||||||31-JAN-07
8311|Heytesbury Group|60451|5|Briefly described|p95 Fig. 61|||||||||
8311|Heytesbury Group|60538|5|Briefly described|p470, 473 Fig. 12, 474 Fig. 13|Miocene|Late Oligocene|Limestone, marl, littoral deposits. Geological Province: Otway Basin.||||||
8311|Heytesbury Group|60563|5|Briefly described|p45|Miocene|Oligocene|Mostly carbonates. Includes Port Campbell Limestone. Geological Province: Otway Basin.||||||
8311|Heytesbury Group|60581|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Clifton Formation, Gellibrand Marl.||||||
8311|Heytesbury Group|60582|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Clifton Formation, Gellibrand Marl.||||||
8311|Heytesbury Group|60583|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Clifton Formation, Gellibrand Marl.||||||23-NOV-04
8311|Heytesbury Group|60584|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Clifton Formation, Gellibrand Marl.||||||23-NOV-04
8311|Heytesbury Group|60585|5|Briefly described|p29|Middle Miocene|Late Oligocene|Includes: Clifton Formation, Gellibrand Marl, Port Campbell Limestone.||||||
8311|Heytesbury Group|61155|5|Briefly described|p4, p18|Middle Miocene|Late Oligocene|Includes: Clifton Formation, Gellibrand Marl, and Port Campbell Limestone.  Consists of littoral to deep marine bryozoan carbonates and clastics. Geological Province: Otway Basin.||||||03-MAR-10
8311|Heytesbury Group|61182|4|Described|p24, p27-28, p36|Late Miocene|Late Oligocene|Comprises Clifton Fm, Gellibrand Marl and Port Campbell Lst; Hanson Plain Sand has been included by some authors; excluded here. Mostly shelf carbonates and only minor terrigenous sediments. Max. thick: 698m. Disconformable over Nirranda Gp. Age: 29-5Ma. ||||||
8311|Heytesbury Group|61185|5|Briefly described|p58|||Marine sediments. Geological Province: Otway Basin.||||||07-FEB-11
8311|Heytesbury Group|61528|6|Mentioned|p827|||||||||
8311|Heytesbury Group|61547|6|Mentioned|pp461-462. |Miocene|Eocene|||||Overlies Nirranda Group.||
8311|Heytesbury Group|61607|6|Mentioned|p5 Fig. 2|Cenozoic|Oligocene|Geological Province: Otway Basin.||||||12-MAR-09
8311|Heytesbury Group|61608|6|Mentioned|p41 Fig. 5|||Refers to equivalent unit.||||||
8311|Heytesbury Group|61622|4|Described|p436, p437, p436 Fig. 2|Miocene|Eocene|Includes Gellibrand Marl and Gambier Limestone. Geological Province: Otway Basin. Thin marls and carbonates deposited in mid to inner shelf environment.||||||07-FEB-11
8311|Heytesbury Group|61623|5|Briefly described|p447, p449 Fig. 4|Tertiary|Tertiary|Includes; Clifton Formation, Gellibrand Marl and Port Campbell Limestone. Geological Province: Otway Basin.||||||
8311|Heytesbury Group|61624|5|Briefly described|p465, p466, p466 Fig. 2, p467, p469|Miocene|Oligocene|Includes Clifton Formation, Gellibrand Marl and Port Campbell Limestone. Geological Province: Otway Basin.||||||
8311|Heytesbury Group|61626|5|Briefly described|p487, p486 Fig. 2, p489 Fig. 6, p493|Miocene|Oligocene|Includes; Clifton Formation, Gellibrand Marl and Port Campbell Limestone. Geological Province: Otway Basin.||||||
8311|Heytesbury Group|61627|5|Briefly described|p500 Fig. 2|Miocene|Late Eocene|Includes Compton Conglomerate, Gellibrand Marl and Gambier Limestone. Geological Province: Otway Basin.||||||07-FEB-11
8311|Heytesbury Group|61628|5|Briefly described|p509 Fig. 3|Late Miocene|Early Oligocene|Includes; Clifton Formation, Gellibrand Marl, Port Campbell Limestone. Geological Province: Otway Basin.||||||
8311|Heytesbury Group|61841|5|Briefly described|p242|Eocene|Paleocene|Dominantly marine limestone and marl.  Geological Province: Otway Basin.||||||03-JUL-06
8311|Heytesbury Group|62370|6|Mentioned|p464 Fig.12|||Marine carbonates.||||||
8311|Heytesbury Group|62896|6|Mentioned|p88|Tertiary|Tertiary|||||||07-FEB-11
8311|Heytesbury Group|63066|5|Briefly described|p485|Tertiary|Tertiary|Geological Province: Murray Basin.||||||08-FEB-07
8311|Heytesbury Group|63122|5|Briefly described|p17 Fig. 4.3, p21|Early Miocene|Late Eocene|Includes Gambier Limestone, Compton Conglomerate and Gellibrand Marl. Geological Province: Otway Basin. ||||||
8311|Heytesbury Group|63124|4|Described|p49 Fig. 5.2, p87 Fig. 5.29|Miocene+|Late Eocene|Incl: Gambier Limestone, Compton Conglomerate and Gellibrand Marl. In Otway Basin/ Gambier Basin. Group name - previously used for the Victorian Clifton Formation, Gellibrand Marl and Port Campbell Limestone, of which only G.Marl occurs in South Australia||||||
8311|Heytesbury Group|63125|6|Mentioned|p103|||Geological Province: Otway Basin||||||
8311|Heytesbury Group|63173|5|Briefly described|p342 Fig. 9.2|Recent|Late Oligocene|Geological Province: Otway Basin, offshore.||||||07-FEB-11
8311|Heytesbury Group|63269|5|Briefly described|p604-605|Miocene|Oligocene|Otway Basin.|||Clifton Formation, Gellibrand Marl, Port Campbell Limestone.|Unconformably overlies Nirranda Group. Is overlain unconformably by Hanson Plain Sand.||
8311|Heytesbury Group|63431|5|Briefly described|p677 Fig. 2|Miocene|Eocene|Includes Gambier Limestone and Gellibrand Marl.||||||07-FEB-11
8311|Heytesbury Group|63446|5|Briefly described|Map legend|Miocene|Miocene||||||Marine: calcarenite, marl, silt.|
8311|Heytesbury Group|65316|6|Mentioned|p598|||In the Otway Basin.|||Includes the Clifton Formation.|||23-APR-12
8311|Heytesbury Group|65715|4|Described|p14 Tb.8, p16|Miocene|Oligocene|Includes Gellibrand Marl and Clifton Formation. Called Heytesbury Formation by Baker (1950). In Port Campbell Embayment. Marine.||||||
8311|Heytesbury Group|66002|5|Briefly described|p10 Tb.7, p12, p13 Tb.9, p16, p26 Fig.7|Neogene|Neogene|Includes Port Campbell Limestone, Gellibrand Marl and Clifton Formation. Defined by Glenie 1971. Modified from Heytesbury Formation of Baker (1950)||||||
8311|Heytesbury Group|66012|4|Described|p4, p6, p10 Tb.1, p17-18, p27, p30 Tb.3|Neogene|Paleogene|Intersected in boreholes. Includes Clifton Formation, Gellibrand Marl & Port Campbell Limestone. Overlies Dilwyn Formation. Underlies Moorabool Viaduct Sand & Newer Volcanic Group. Calcareous quartz sand, sandy limestone, limestone, marl, & calcareous clay. Up to 55m thick| | | | | |16-FEB-15
8311|Heytesbury Group|66245|5|Briefly described|p6 Fig.5, p8. |Messinian|Rupelian|Coastal and shallow marine, progradational sequence of carbonates. Helped in building out the present day shelf.|||Includes Clifton Formation, Gellibrand Marl and Port Campbell Limestone.|||
8311|Heytesbury Group|67061|6|Mentioned|p546 Fig.3, p557.|Miocene|Oligocene||||Includes Clifton Formation, Gellibrand Marl and Port Campbell Limestone.|||
8311|Heytesbury Group|67366|6|Mentioned|p103 Fig.2. |Miocene|Oligocene||||Includes Clifton Formation, Gellibrand Marl and Port Campbell Limestone.|Unconformably overlies Nirranda Group.||
8311|Heytesbury Group|67367|5|Briefly described|p130, p131 Fig.2. |Oligocene|Oligocene|Carbonates. The unit is relatively thin across most of the inner shelf of the Otway Basin, hence little or no hydrocarbon was generated during the Late Tertiary. Its rapid thickening across the outer shelf has rapidly matured the Austral 2 source rocks (Eumeralla Formation).|||Includes Clifton Formation, Gellibrand Marl and Port Campbell Limestone.|||
8311|Heytesbury Group|68116|5|Briefly described|Appendix, Maps 38-39, 47-48.|Miocene|Oligocene||||||Calcarenite, marl, silt.|
8311|Heytesbury Group|68189|6|Mentioned|p26|||||||||
8311|Heytesbury Group|69297|4|Described|p78, p79, p81, p98, p112, p115, p116|Tortonian|Rupelian|Otway Basin. Coastal plain to open marine siliciclastic and carbonate sediments. Potential seal of the Nirranda and Wangerrip Group reservoirs. |||Includes the Gambier Limestone, Clifton Formation, Gellibrand Marl and the Port Campbell Limestone. |Overlies the Nirranda Group. Unconformably overlain by the Hanson Plain Sand, Coomnandook Formation and the Bridgewater Formation. |Marls and fine-grained limestones. |
8311|Heytesbury Group|69651|5|Briefly described|p6, p10, p12, p33, p38|Miocene|Eocene|Otway Basin. Mixed carbonate/siliciclastic rocks. Carbonates are potential seals. Modelling diagrams.|||Clifton Formation, Gellibrand Marl, Port Campbell Limestone.|Unconformably overlies Nirranda Group. Is overlain unconformably by Hanson Plain Sand.|Marls and fine-grained limestone.|
8311|Heytesbury Group|69879|5|Briefly described|p418, p424|Miocene|Oligocene|Strahan Sub-basin, Sorell Basin. Shown as Heytesbury Group equivalent. Offshore exploration well Cape Sorell 1.||||Overlies Nirranda Group.|Nannofossil ooze/chalk carbonates with quartzitic sand sub-unit. Outer shelf carbonate, including fossiliferous reefal limestone.|
8311|Heytesbury Group|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Miocene|Oligocene|Otway Basin: Gambier Embayment and Voluta Trough.|||Gambier, Port Campbell Limestones; Gellibrand Marl; Clifton Formation.|Overlies Nirranda Group.||
8311|Heytesbury Group|70078|5|Briefly described|Northern: Fig.2; p2. Regional: Fig.4; p5|Miocene|Oligocene|Otway Basin. Sandstones equivalent to this unit in the Sorell Basin are potential hydrocarbon sources. Similarly, equivalent marls and fine-grained limestones are potential regional seals, eg to Nirranda and Wangerrip Groups reservoirs.|||Gambier Limestone.|Overlies Nirranda Group. Is overlain by Coomandook Formation.||
8311|Heytesbury Group|70379|6|Mentioned|p724-727|||Otway Basin.||||Overlies Nirranda Group.||
8311|Heytesbury Group|70909|14|Not recorded|p62||Miocene|||||||
8311|Heytesbury Group|71419|6|Mentioned|p22|||Stated in this article to be upgraded from Heytesbury Formation to Group by Glenie (1971). [The Heytesbury Group appears in Baker (1953) Fig.1 p126].||||||02-FEB-18
8311|Heytesbury Group|71437|5|Briefly described|Fig. 1 opp 154, p155, p159|Pliocene|Oligocene||||Includes Clifton Formation, Gellibrand Marl, Port Campbell Limestone, Moorarbool Viaduct Formation.||Limestone-marl-sandy limestone suite.|
8311|Heytesbury Group|71593|5|Briefly described|p51|Miocene|Oligocene|||||||
8311|Heytesbury Group|72445|5|Briefly described|App 1; App.2; App.5; App.6 p1, p3.|Miocene|Oligiocene|Murray and Otway basins. App.2 is a .csv format file. Identified in Stavely 01. A diverse inner to middle shelf benthic foraminiferal assemblage is present. Samples include planktic and benthic foraminifera.|||Includes Port Campbell Limestone and Gellibrand Marl.|Shown as overlying Moornambool Metamorphic Complex with sharp contact, and conformably underlying Wunghnu Group.|Bioturbated silty to sandy marl with lesser mud and shell fragments. Some intervals of cleaner sand.  Sandy to muddy calcareous marl with some muddier sections and abundant shell fragments.|15-OCT-20
8311|Heytesbury Group|73356|6|Mentioned|p3, p16|Miocene|Oligocene|||||Unconformably underlain by Nirranda Group. Unconformably overlain by Bridgewater Formation.|Marine marls and limestones.|
8311|Heytesbury Group|73357|6|Mentioned|p44, p46, p48|Tortonian|Chattian|Otway Basin.|||Includes Clifton Formaiton, Gellibrand Marl, Port Campbell Limestone.|Overlies Nirranda Group, underlies Whalers Bluff Group.||
8311|Heytesbury Group|73383|4|Described|p3, p7 Tb.3.1, p10, p137, p264|Miocene|Oligocene|Otway Basin. Equivalent to chemostratigraphic Sequence S6, primarily defined by high Ca values. Lithologies based on geochemistry using the ChemLith classification includes limestone and calcareous limestone, and using the Herron classification (1988) includes shale and Fe-shale.|||Clifton Formation, Gellibrand Marl, Port Campbell Limestone|Overlies Nirranda Group, underlies Bridgewater Formation|Carbonate units including limestones, marls and calcareous mudstones.|
8311|Heytesbury Group|73385|5|Briefly described|p3-5|Miocene|Oligocene|Otway Basin. Overlies regional intra-Oligocene unconformity, underlies late-Miocene unconformity.|||Clifton Formation, Gellibrand Marl, Port Campbell Limestone|Unconformably overlies Nirranda Group, unconformably underlies Bridgewater Formation.|Marine marls and limestones.|
8311|Heytesbury Group|73386|4|Described|p1-2, p4-7, p14, iii, Attachment A1|Tortonian|Chattian|Otway Basin. Covers basin west of the Otway Ranges, thins towards basin margins. Deposited in setting of post-rift subsidence, inversion. Top of Heytesbury Group is an unconformity, marked by uplift, folding and erosion at the end of the Miocene. Overlain by units of Pliocene to Pleistocene age. Contains Middle Proteacidites tuberculatus to Upper Triporopollenites bellus spore-pollen zones, chemostratigraphic sequence S6 of Forbes et al. (2020). Appears as Heystesbury Group p6.|||Port Campbell Limestone, Gellibrand Marl, Clifton Formation|Unconformably overlies Nirranda Group, underlies Bridgewater Formation|Marine marls and limestones.|
8311|Heytesbury Group|73486|5|Briefly described|p510, p511 Fig.2, p528|Miocene|Oligocene|Otway Basin. Represents final megacycle of sediment accumulation in basin.|||Clifton Formation, Gellibrand Marl, Port Campbell Limestone|Overlies Nirranda Group, underlies Hanson Plain Sand, Hesse Clay||
8311|Heytesbury Group|73594|5|Briefly described|p4-6|Miocene|Oligocene|Otway Basin. Onshore thickness of 200-400m, up to 1750m thick at the seaward end of the Shipwreck Trough. Erosion of the uppermost part in the late Miocene.|||Clifton Formation, Gellibrand Marl, Port Campbell Limestone|Overlies Nirranda Group|Marine marls and limestones.|
73300|Heytesbury Supersequence|63134|2|Defined|112|||||||||
73300|Heytesbury Supersequence|63269|5|Briefly described|p605|Miocene|Oligocene|Otway Basin.||||Overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.||
73300|Heytesbury Supersequence|69297|6|Mentioned|p80, p110, p111|||||||||
73300|Heytesbury Supersequence|69651|5|Briefly described|p10, p12-15, p17-19, p22-23, p29, p39|Miocene|Oligocene|See also p44-47, p49-50. Open marine deposits. Possible seals. Modelling diagrams.||||Overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.|Calcareous claystone overlain by marls, calcarenite and calcilutite; shaly limestone overlain by calcarenite and calcilutite; quartz sandstone overlain by silty mudstone, and limestone.|
73300|Heytesbury Supersequence|70077|5|Briefly described|Regional: Fig.4; p4-5|Miocene|Oligocene|Otway Basin.||||Overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.||
73300|Heytesbury Supersequence|70078|5|Briefly described|Regional: Fig.4; p3|Miocene|Oligocene|||||Unconformably overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.|Shelfal marls and limestones.|
73300|Heytesbury Supersequence|70880|5|Briefly described|p77|Miocene|Oligocene|Otway Basin. Open marine environment.||||Overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.|Mixed carbonate/siliciclastic sediments.|
73300|Heytesbury Supersequence|71266|5|Briefly described|p614 Fig.3, p615|Miocene|Oligocene|Otway Basin.||||Overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.||
8316|Heywood Marl|24551|6|Mentioned|p300|||Of the Heytesbury Group.||||||
8316|Heywood Marl|31372|6|Mentioned|Fig. 2|||||||||
8316|Heywood Marl|31424|4|Described|p14|||See also p7. Described from core||||||21-OCT-15
8316|Heywood Marl|31624|6|Mentioned|p101|||U.Palaeocene. Unit of Dartmoor Fm.||||||
8316|Heywood Marl|48911|6|Mentioned|p27|||Chart 1. Correlation||||||
21958|Hickman Creek Granite|23309|6|Mentioned|p433 App1|||G384 I-Type.||||||
21958|Hickman Creek Granite|23810|5|Briefly described|p888||Devonian|Of Mount Cole Suite. Lachlan Fold Belt.||||||
21958|Hickman Creek Granite|44186|5|Briefly described|Map Legend||Early Devonian|G384 Unassigned.||||||
21958|Hickman Creek Granite|66002|5|Briefly described|p7 Tb.5|||Of Mount Cole Suite. G384. Called Hickman Creek Adamellite by Cayley and McDonald (1995)||||||
21958|Hickman Creek Granite|68116|5|Briefly described|Appendix, Map 31.|Early Devonian|Early Devonian||||||Biotite granite: felsic; pink to pale grey; coarse and even grained; small pegmatitic patches.|
69416|High Tops Tonalite|61160|3|Fully described|p75-76, p30 Tb. 5.2|Early Devonian|Early Devonian|Of Falls Creek Suite. Enclosed within Cobungra Granite which it intruded. Pale cream, medium-grained and equigranular, comprising quartz, plagioclase and biotite, roughly aligned into a penetrative foliation. See also p58-59 Fig. 6.8.||||||16-NOV-05
69416|High Tops Tonalite|61161|5|Briefly described|p91-92, p76-77 Fig 6.1 |Early Devonian|Early Devonian|Of Falls Creek Suite. Highly magnetic, pale cream, medium-grained, equigranular tonalite; quartz, plagioclase, biotite. Intrudes surrounding Cobungra Granite, migmatite and gneiss. Type locality p91. Age: inferred Early Devonian. GSV map code: G189.||||||
69416|High Tops Tonalite|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Falls Creek Suite. Biotite tonalite: pale cream; medium grained, equigranular; weak magmatic alignment of biotite; magnetic; I-type intrusion. GSV map code: G189.||||||
69416|High Tops Tonalite|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Falls Creek Suite. Biotite tonalite: pale cream; medium grained, equigranular; weak magmatic alignment of biotite; magnetic; I-type intrusion. GSV map code: G189.||||||
69416|High Tops Tonalite|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Falls Creek Suite. Biotite tonalite: pale cream; medium grained, equigranular; weak magmatic alignment of biotite; magnetic; I-type intrusion. GSV map code: G189.||||||
69416|High Tops Tonalite|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Falls Creek Suite. Biotite tonalite: pale cream; medium grained, equigranular; weak magmatic alignment of biotite; magnetic; I-type intrusion. GSV map code: G189.||||||07-FEB-11
69416|High Tops Tonalite|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Falls Creek Suite. Biotite tonalite: I-type; moderate to highly magnetic (20 - 75 nT; kv = 70-700 x10^-6 cgs); low to moderate gravity (-420 ums ^-2); moderate total radioelement and K, low Th and U. GSV map code: G189.||||||
69416|High Tops Tonalite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Falls Creek Suite. Biotite tonalite: pale cream; medium-grained, equigranular; weak magmatic alignment of biotite; magnetic; I-type intrusion. GSV map code: G189.||||||
69416|High Tops Tonalite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Falls Creek Suite. Biotite tonalite: pale cream; medium-grained, equigranular; weak magmatic alignment of biotite; magnetic; I-type intrusion. GSV map code: G189.||||||07-FEB-11
69416|High Tops Tonalite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Falls Creek Suite. Biotite tonalite: pale cream; medium-grained, equigranular; weak magmatic alignment of biotite; magnetic; I-type intrusion. GSV map code: G189.||||||
69416|High Tops Tonalite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Falls Creek Suite. Biotite tonalite: pale cream; medium-grained, equigranular; weak magmatic alignment of biotite; magnetic; I-type intrusion. GSV map code: G189.||||||
69416|High Tops Tonalite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Falls Creek Suite. Biotite tonalite: low gravity response (-420 ums^-2); highly magnetic (200 to 290 nT, k = 5 to 710 x 10^-6 cgs); moderate K and Th, low to moderate U, moderate total radioelements. GSV map code: G189.||||||
69416|High Tops Tonalite|68116|5|Briefly described|Appendix, Maps 27, 35.|Early Devonian|Early Devonian||||||Biotite tonalite: pale cream; medium-grained, equigranular; weak magmatic alignment of biotite; magnetic.|
21960|Highton Volcanics|23309|5|Briefly described|p169, 175, 176, 181, 185. Table 2.67|||Supersedes the Blue Range Volcanics.  Of the Wellington Volcanic Group||||||30-NOV-11
21960|Highton Volcanics|24551|4|Described|p169, Fig. 6.9|||Overlies the Kevington Creek Formation (u).  Of the Delatite Group.  Consists of informal units, Quarry Rhyodacite Unit, Gun Club Andesite Unit, Volcanic Conglomerate Unit.||||||05-JUN-14
21960|Highton Volcanics|64010|5|Briefly described|p258 Fig.1. |||||Of the Wellington Volcanic Group.|||Includes unnamed conglomerate, andesite, and rhyodacite members.|
21960|Highton Volcanics|64536|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of Wellington Volcanic Group. Comprise 3 unnamed members of conglomerate, andesite and rhyodacite. More lithological detail included in map legend.||||||07-FEB-11
21960|Highton Volcanics|64537|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of Wellington Volcanic Group. Comprise 3 unnamed members of conglomerate, andesite and rhyodacite. More lithological detail included in map legend.||||||07-FEB-11
21960|Highton Volcanics|64538|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of Wellington Volcanic Group. Comprise 3 unnamed members of conglomerate, andesite and rhyodacite. More lithological detail included in map legend.||||||07-FEB-11
21960|Highton Volcanics|64606|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Wellington Volcanic Group. Rhyodacite ignimbrite, andesite and conglomerate, minor sandstone and pebble breccia.||||||11-NOV-08
21960|Highton Volcanics|64616|3|Fully described|p136, p155, p279, p300|Late Devonian|Late Devonian|Of Wellington Volcanic Group. Three lenticular patches in Jamieson Syncline. Disconformable on Kevington Creek Formation and unconformably overlies Delatite Group. Unconformably overlain by Mansfield Group. Subdivided informally into rhyodacitic ignimbrite, andesite lava flows and volcaniclastic deposits. Geophysical characteristics given.||||||
21960|Highton Volcanics|68116|5|Briefly described|Appendix, Map 34.|Late Devonian|Late Devonian|Contains three informal subdivisions.|||||Lava unit: lenticular unit of andesite lava, flow breccia and andesitic volcaniclastics. Clastic unit: <20 m of volcanolithic conglomerate and sandstone. Ignimbrite unit: <120 m welded garnet-bearing rhyolitic ignimbrite with prominent fiamme.|
37747|Hinno Munjie Granite|23309|6|Mentioned|Table 4.1|||See also Hinno-Munjie Granite.||||||
37747|Hinno Munjie Granite|60503|4|Described|p150|Silurian|Silurian|Fine-grained rock, generally altered with few fresh mafic minerals; main mafic mineral is biotite, altered to chlorite or epidote. Probably intruded by Anglers Rest Granite. ||||||
37747|Hinno Munjie Granite|60504|5|Briefly described|Map Legend|Wenlock|Wenlock|Biotite granite: S-type, foliated granite with high compositional variability; numerous metasedimentary enclaves; grey to pink, medium grained.||||||
37747|Hinno Munjie Granite|60505|5|Briefly described|Map legend|Wenlock|Wenlock|Biotite granite: S-type, foliated granite with high compositional variability; numerous metasedimentary enclaves; grey to pink, medium grained.||||||
37747|Hinno Munjie Granite|60506|5|Briefly described|Map legend|Wenlock|Wenlock|Biotite granite: S-type, foliated granite with high compositional variability; numerous metasedimentary enclaves; grey to pink, medium grained.||||||
37747|Hinno Munjie Granite|60507|5|Briefly described|Map Legend|Wenlock|Wenlock|Biotite granite: S-type, foliated granite with high compositional variability; numerous metasedimentary enclaves; grey to pink, medium grained.||||||
37747|Hinno Munjie Granite|68116|5|Briefly described|Appendix, Map 27.|Wenlock|Llandovery||||||Biotite granite: grey to pink, medium-grained; foliated; composition variable; numerous metasedimentary enclaves.|
26615|Hobbs Granite|23309|6|Mentioned|p433 App1|||G69 I-Type. Supersedes Hobbs Adamellite.||||||
26615|Hobbs Granite|24551|6|Mentioned|p234|||||||||
26615|Hobbs Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Hobbs Adamellite.||||||
26615|Hobbs Granite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Hornblende granite: fine to medium grained; grey; I-type.|
31586|Hobbs Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
8424|Holey Plains Marl|24551|5|Briefly described|p327 Fig. 10.33|Miocene|Miocene|||||||
8424|Holey Plains Marl|31351|6|Mentioned|p27|||See also P89.||||||
8424|Holey Plains Marl|34954|6|Mentioned|Fig.35|||||||||
8424|Holey Plains Marl|65718|6|Mentioned|p10 Fig 3.2|Miocene|Miocene|Early Miocene age.||||||
35114|Hollands Creek Ignimbrite|22971|4|Described|p 18|Devonian|Devonian|||||||
35114|Hollands Creek Ignimbrite|23309|5|Briefly described|p169, Tables 2.63, 2.64, 2.65|||Of the Tolmie Igneous Complex. Maximum thickness: 300m.  Geological Province: Wabonga Cauldron.||||||
35114|Hollands Creek Ignimbrite|24551|6|Mentioned|p157|||||||||
35114|Hollands Creek Ignimbrite|61163|5|Briefly described|p89 Tb. 8.1|||Grouped within Mount Warrick Rhyolite subdivision of Tolmie Igneous Complex. Rhyolitic to rhyodacitic quartz ignimbrite, rich in large phenocrysts and moderatley to densely welded. Thickness: >300m.||||||
35114|Hollands Creek Ignimbrite|64312|6|Mentioned|p440|||Of the Wabonga Volcanic Complex. Contains barium. ||||||
35114|Hollands Creek Ignimbrite|75072|5|Briefly described|p230, 251|Frasnian|Givetian|Eastern margin of the Melbourne Zone.||Tolmie Igneous Complex.|||S-type.|
37561|Holloways Formation|23309|4|Described|p108 Table 2.40|||Of Little River Subgroup (Snowy River Volcanics). See also Holloways formation.||||||22-FEB-10
37561|Holloways Formation|24551|5|Briefly described|p144|||Of Little River Subgroup.||||||
37561|Holloways Formation|60542|4|Described|p14|Early Devonian|Early Devonian|Probably misspelt - see Holloway Formation. This name is applied to the upper part of "Mount Johnson Member". Volcaniclastic sediments and mudstone - sandstones, microbreccia, sandy turbidites. Overlies Stonehenge Ignimbrite. ||||||
37561|Holloways Formation|68116|5|Briefly described|Appendix, Map 45.|Pragian|Pragian||||||Volcaniclastic sandstone, mudstone, conglomerate: thin to thick bedded, pumiceous, commonly with open framework; marine mass-flow deposits.|
34855|Holstons Tonalite|22968|5|Briefly described|P71, P206|Early Devonian|Late Silurian|Parent is the Ensay Suite||||||
34855|Holstons Tonalite|23028|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Ensay Suite||||||
34855|Holstons Tonalite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Ensay Suite||||||
34855|Holstons Tonalite|23309|5|Briefly described|p296|||G518 I-Type. Formerly part of the Bald Hills Creek Tonalite.||||||
34855|Holstons Tonalite|68116|5|Briefly described|Appendix, Maps 35-36.|Early Devonian|Early Devonian||||||Biotite-hornblende tonalite; grey, medium to coarse-grained, massive to moderately foliated.|
74175|Home Station Sandstone Member|63738|5|Briefly described|p3|Early Carboniferous||Of the Snowy Plains Formation (Mansfield Group). Geological Province: Mansfield Basin. Contained an in situ actinopterygian near Bridge Creek and Broken River intersection.||||||13-MAY-08
74175|Home Station Sandstone Member|64010|5|Briefly described|p257-273.   |Tournaisian|Tournaisian|250-500 m thick. Includes a unit referred to as Fish Hill which contains abundant and diverse trace fossils, including a new trace-fossil ichnospecies of Fuersichnus and a new ichnotaxon Platicytes lioparadus. Lithofacies and systematic ichnology described in detail.||Of the Snowy Plains Formation.|||Includes 28 m interval of fossiliferous beds consisting of alternating laminated mudstone and siltstone, laminated and massive sandstones.|
74175|Home Station Sandstone Member|64536|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation (Mansfield Group). Sandstone, minor mudstone: medium-grained, medium to very thick bedded; quartz-lithic, micaceous. Forms prominent outcrops and strike ridges. Fluvial deposits.||||||07-FEB-11
74175|Home Station Sandstone Member|64537|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation (Mansfield Group). Sandstone, minor mudstone: medium-grained, medium to very thick bedded; quartz-lithic, micaceous. Forms prominent outcrops and strike ridges. Fluvial deposits.||||||07-FEB-11
74175|Home Station Sandstone Member|64538|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation (Mansfield Group). Sandstone, minor mudstone: medium-grained, medium to very thick bedded; quartz-lithic, micaceous. Forms prominent outcrops and strike ridges. Fluvial deposits.||||||07-FEB-11
74175|Home Station Sandstone Member|64606|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation. Sandstone, minor mudstone: alluvial deposits. Dark red to pink in RGB. Nonmagnetic.||||||
74175|Home Station Sandstone Member|64616|4|Described|p139, p299|Early Carboniferous|Early Carboniferous|New member of Snowy Plains Formation. Conformable between underlying Ashwin Siltstone Member and overlying Buttercup Mudstone Member or Lanky Creek Sandstone Member. 200-500m thick. Medium-grained, thick-bedded, quartz-lithic sandstone; minor mudstone. Geophysical characteristics given.||||||
74175|Home Station Sandstone Member|66498|6|Mentioned|p46|||||Snowy Plains Formation.||||
8460|Honeysuckle Hill Gravels|24551|5|Briefly described|p498 Fig. 16.8|Eocene|Eocene|||||||
8460|Honeysuckle Hill Gravels|37127|6|Mentioned|p349|||||||||
8460|Honeysuckle Hill Gravels|41227|4|Described|p4|||||||||
8460|Honeysuckle Hill Gravels|42827|5|Briefly described|Fig 8.21|||||||||
8460|Honeysuckle Hill Gravels|61336|5|Briefly described|p(xi)|||Of Traralgon Formation?? Thick gravel sequences up to 200m thick.||||||07-FEB-11
8460|Honeysuckle Hill Gravels|67727|5|Briefly described|p58 Fig.2, pp59-60, pp72-75.|Eocene|Eocene|Onshore Gippsland Basin. Fluvial deposits to 200 m thick, equivalent to the upper part of the paralic Latrobe Group in the offshore Gippsland Basin.|||||Thick conglomerate sequences.|
8460|Honeysuckle Hill Gravels|70076|5|Briefly described|Regional: Fig.3|Lutetian|Lutetian|||Latrobe Group.||Is overlain by Traralgon Formation.||
8483|Hope Hill Granite|41868|6|Mentioned|p494|||||||||
8486|Hopkins River Granite|23309|6|Mentioned|p448 App1|||Obsolete granite name.||||||
8486|Hopkins River Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
8486|Hopkins River Granite|44186|5|Briefly described|Map Legend||Early Devonian|G382 I-type. Shown as Hopkins River.||||||
8486|Hopkins River Granite|60451|6|Mentioned|p88|||||||||
69419|Horsehair Creek Tonalite|61161|5|Briefly described|p94, p76-77 Fig 6.1|Early Devonian|Early Devonian|Of Rileys Creek Suite. Underlies Older Volcanic Group. Moderately to highly magnetic, green to grey speckled, fine to medium-grained tonalite; weak magmatic foliation. I-type. Type locality p94. GSV map code: G462.||||||
69419|Horsehair Creek Tonalite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende tonalite: fine to medium-grained, foliated; contains quartz, plagioclase, biotite, hornblende; weak magmatic foliation due to aligned biotite, hornblende and plagioclase; I-type intrusion. GSV map code: G462.||||||
69419|Horsehair Creek Tonalite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende tonalite: fine to medium-grained, foliated; contains quartz, plagioclase, biotite, hornblende; weak magmatic foliation due to aligned biotite, hornblende and plagioclase; I-type intrusion. GSV map code: G462.||||||07-FEB-11
69419|Horsehair Creek Tonalite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende tonalite: fine to medium-grained, foliated; contains quartz, plagioclase, biotite, hornblende; weak magmatic foliation due to aligned biotite, hornblende and plagioclase; I-type intrusion. GSV map code: G462.||||||
69419|Horsehair Creek Tonalite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende tonalite: fine to medium-grained, foliated; contains quartz, plagioclase, biotite, hornblende; weak magmatic foliation due to aligned biotite, hornblende and plagioclase; I-type intrusion. GSV map code: G462.||||||
69419|Horsehair Creek Tonalite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende tonalite: no gravity data; moderately to highly magnetic (100 to 190 nT, k = 35 to 410 x10^-6 cgs); low K, low to moderate Th, U and total radioelements. GSV map code: G462.||||||
69419|Horsehair Creek Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Silurian||||||Biotite-hornblende tonalite: fine to medium-grained, foliated; contains quartz, plagioclase, biotite, hornblende; weak magmatic foliation due to aligned biotite, hornblende and plagioclase.|
29698|Hospital Creek Sandstone|23309|4|Described|p111. Table 2.40|||Of the Tara Range Subgroup.||||||22-FEB-10
29698|Hospital Creek Sandstone|24551|5|Briefly described|p143|||Of Tara Range Subgroup.||||||
29698|Hospital Creek Sandstone|43312|5|Briefly described|Map Legend||Early Devonian|of Tara Range Subgroup||||||
29698|Hospital Creek Sandstone|43313|5|Briefly described|Map Legend||Early Devonian|of Tara Range Subgroup||||||
29698|Hospital Creek Sandstone|60542|3|Fully described|p71, p14|Early Devonian|Early Devonian|Mass flow sediments with minor pyroclastics - thick-bedded, coarse-grained volcanolithic sandstone consisting of predominantly quartz and feldspar crystal. Probably overlies Kanni Ignimbrite.||||||
29698|Hospital Creek Sandstone|68116|5|Briefly described|Appendix, Map 45.|Pragian|Pragian||||||Sandstone: crystal rich, thick-bedded and graded, mudstone, pebbly mudstone; volcanolithic conglomerate; marine turbidite deposits.|
28611|Hotspur High Level Alluvials|34988|6|Mentioned|Table 9.4|||||||||
8531|House Creek Granite|23309|6|Mentioned|p448 App1|||Obsolete granite name.||||||
8531|House Creek Granite|42726|5|Briefly described|map legend|||Of the Bethanga Suite (Cooma Supersuite).  Formal name not intended.||||||09-FEB-05
26622|Howe Range Granite|22815|6|Mentioned|p95|||||||||
26622|Howe Range Granite|23309|6|Mentioned|p433 App1|||G2 A-Type.||||||
26622|Howe Range Granite|42726|5|Briefly described|map legend|Middle Devonian||No 88. Of Gabo Suite. Reserved as Howe Range.||||||29-AUG-12
26622|Howe Range Granite|68116|5|Briefly described|Appendix, Maps 37, 46.|Late Devonian|Late Devonian||||||Biotite-hornblende granite: medium to fine grained; accessory allanite, magnetite, fayalite, stilpnomelane and fluorite; hornblende is hastingsite; A-type.|
26622|Howe Range Granite|71206|6|Mentioned|p373|||Lachlan Fold Belt.||Gabo Suite.|||Aluminous A-type granite.|
37563|Howitt Spur Formation|23309|4|Described|p171-185. Tbl 2.67.|||Of Wellington Volcanics.  Underlying unit: Bindaree Formation.  Maximum thickness: 500m.||||||22-FEB-10
37563|Howitt Spur Formation|24551|4|Described|p175|||Of the Wellington Volcanic Group.  Maximum Thickness: 500m.  ||||||
37563|Howitt Spur Formation|66244|6|Mentioned|p6.|||||||||
37563|Howitt Spur Formation|66252|2|Defined|p209, p211-216 Figs.31-6.|Frasnian|Frasnian|See also p222 Fig.8, p224-226, p228-229, p231. New name. Definition data given. Unit in Avon River Group. In this study, replaces "Unit 4" to "Unit 6" of Marsden (1976). Type area in upper Howqua Valley. Comprises (informal) Pebble Sandstone Unit (conglomerate, sandstone); (informal) Brown Siltstone Unit (khaki and green siltstone, mudstone, minor sandstone); minor rhyodacite unit. About 500m thick. Conformably overlies Bindaree Formation, Rose River Volcanics and Refrigerator Gap Dacite. Is overlain by Mount Kent Conglomerate. Detailed stratigraphic section and petrography.||||||
37563|Howitt Spur Formation|68116|5|Briefly described|Appendix, Map 34.|Late Devonian|Late Devonian||||||Sandstone and siltstone: sandstone unit: <150 m of upward fining pebble/cobble conglomerate, sandstone, minor mudstone; siltstone unit: ~400 m of brown siltstone and thin sandstone; rhyodacite unit <50m thick near top.|
8538|Howqua Chert|22628|6|Mentioned|fig1p108|||||||||
8538|Howqua Chert|22832|5|Briefly described|p635|Ordovician|Cambrian|||||||
8538|Howqua Chert|23229|5|Briefly described|Table3-1p16, 19||Cambrian|||||||
8538|Howqua Chert|23307|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
8538|Howqua Chert|23309|5|Briefly described|p43|||||||||
8538|Howqua Chert|23860|5|Briefly described|p944|Ordovician|Cambrian|Overlying unit Pinnak Sandstone.||||||
8538|Howqua Chert|24002|5|Briefly described|p228 Fig.2|Cambrian|Cambrian|||||||
8538|Howqua Chert|24003|5|Briefly described|p258|||||||||
8538|Howqua Chert|24004|5|Briefly described|p275 Fig.2|Ordovician|Ordovician|||||||
8538|Howqua Chert|24037|6|Mentioned|p425 Fig.2|Early Ordovician|Cambrian|Geological Province: Lachlan Fold Belt.||||||
8538|Howqua Chert|24098|5|Briefly described|p27 Fig. 2|Late Cambrian|Late Cambrian|Geological Province: Lachlan Fold Belt.||||||
8538|Howqua Chert|24551|4|Described|p90|Early Ordovician|Early Ordovician|||||||
8538|Howqua Chert|24576|6|Mentioned|p737|||Geological Province: Lachlan Fold Belt||||||
8538|Howqua Chert|29709|5|Briefly described|p33|||||||||
8538|Howqua Chert|30329|6|Mentioned|p30|||On table P30||||||
8538|Howqua Chert|31161|5|Briefly described|PA9|||||||||
8538|Howqua Chert|32074|6|Mentioned|p18|||||||||
8538|Howqua Chert|33602|6|Mentioned|p18|||||||||
8538|Howqua Chert|33607|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
8538|Howqua Chert|35073|4|Described|p4|||||||||
8538|Howqua Chert|35112|6|Mentioned|p276|||||||||
8538|Howqua Chert|35281|6|Mentioned|p23|||||||||
8538|Howqua Chert|36534|6|Mentioned|p222|||||||||
8538|Howqua Chert|39331|6|Mentioned|Fig.0-3|||||||||
8538|Howqua Chert|41571|6|Mentioned|Table 2.6|||||||||
8538|Howqua Chert|42827|5|Briefly described|Fig 2.6|||||||||
8538|Howqua Chert|61160|5|Briefly described|p46|||Conformably overlain by Pinnak Sandstone. ||||||
8538|Howqua Chert|61161|5|Briefly described|p78, p14|||Underlies Pinnak Sandstone.||||||
8538|Howqua Chert|62742|5|Briefly described|p699 Fig. 2|Late Cambrian|Late Cambrian|Siliceous siltstone (chert). In the Mount Wellington Greenstone Belt.||||||
8538|Howqua Chert|62744|5|Briefly described|p708|Late Cambrian|Late Cambrian|Geological Province: Mount Wellington Greenstone Belt.||||||
8538|Howqua Chert|66196|4|Described|p616, p617, p622, 623|Early Ordovician|Early Cambrian|Conformably overlies Lickhole Volcanics, underlies Adaminaby Group. To 480m thick. Dated from conodonts and graptolites. Deep-sea environment. Lower chert is blue/dark-grey and vitreous; middle and upper is pale-grey to white with thin shale interbeds.||||||
8538|Howqua Chert|67322|6|Mentioned|p15|Datsonian|Datsonian|Late Cambrian age based on the presence of Cordylodus conodonts (Stewart and Fergusson 1988, Kakuwa and Webb 2010).||||||
8538|Howqua Chert|68116|5|Briefly described|Appendix, Maps 26, 34, 52.|Floian|Late Cambrian|Minimum age written as Lancefieldian in text.|||||Black chert, siliceous shale, mafic sandstone, pebbly sandstone and chert conglomerate.|
8538|Howqua Chert|68314|5|Briefly described|p750, p754, p756|Late Cambrian|Late Cambrian|Mount Wellington Greenstone Belt. Contains Datsonian conodonts.|||||Fine-grained siliceous siltstones; abundantly fossiliferous.|
8538|Howqua Chert|68466|6|Mentioned|p70|Ordovician|Cambrian|Lachlan Orogen. Very low degree of bioturbation implying low oxygen in Early Ordovician deep ocean waters.||||||
8538|Howqua Chert|68592|5|Briefly described|p279, p287|Early Ordovician|Early Ordovician|||||Overlies Lickhole Volcanics. Is overlain conformably by Pinnak Sandstone.||
8538|Howqua Chert|68822|6|Mentioned|p346|||||||Underlain by the Mount Read Volcanics.||
8538|Howqua Chert|70493|6|Mentioned|p56|Late Cambrian|Middle Cambrian|Tabberabbera Zone, Lachlan Orogen.||||Overlies Lickhole Volcanics. Is overlain by Adaminaby Group.||
8538|Howqua Chert|70601|4|Described|p43-48, p52|Lancefieldian|Middle Cambrian|Howqua East area. Jamieson Volcanics could be source of felsic tuff bands in chert. Estimated thickness 480m. Contains 480 Ma graptolites in carbonaceous shale at top. Howqua Chert fragments and blocks found in melange within Cobannah Group. |c.485 Ma: zone fossil conodont Cordylodus proavus.|||Underlies Pinnak Sandstone (Adaminaby Group). Conformably overlies Eagles Peak Basalt and Dookie Igneous Complex. Equivalent to "Melville Chert".|Carbonaceous shale, graptolites and conodont Cordylodus proavus in upper horizon of chert. At Dookie, the chert contains felsic tuff bands, minor sandstone and conglomerate with gabbroic detritus.|
8538|Howqua Chert|70661|6|Mentioned|p14|Lancefieldian|Lancefieldian|||||Conformably overlain by Adaminaby Group, overlies Lickhole Volcanics.||
8538|Howqua Chert|71069|6|Mentioned|p52|Lancefieldian|Lancefieldian|||||Overlies the Lickhole Volcanics. Overlain by the Pinnak Sandstone.||
8538|Howqua Chert|71700|6|Mentioned|CD|Lancefieldian|Lancefieldian|||||||
8538|Howqua Chert|73059|6|Mentioned|p1053 Fig.2, 1059|Ordovician|Cambrian|||||Overlies Lickhole Volcanics. Is overlain by Adaminaby Group.||
28613|Humevale Siltstone|22570|6|Mentioned|p189|Pragian|Lochkovian|||||||
28613|Humevale Siltstone|22628|6|Mentioned|fig1p108|Devonian|Devonian|||||||
28613|Humevale Siltstone|22882|4|Described|p 11- 12|Devonian|Devonian|||||||
28613|Humevale Siltstone|22885|5|Briefly described|map|Early Devonian|Early Devonian|||||||
28613|Humevale Siltstone|22886|4|Described|p14|Pragian|Lochkovian|||||||
28613|Humevale Siltstone|23229|4|Described|Table3-3p26, 29-31|Pragian|Ludlow|||||||
28613|Humevale Siltstone|23268|6|Mentioned|p397|||||||||
28613|Humevale Siltstone|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
28613|Humevale Siltstone|23309|4|Described|p139-153. Tb 2.52||Devonian|||||||
28613|Humevale Siltstone|24177|4|Described|p54, p50 Fig.22|Pragian|Pridolian|Overlain by the Wilson Creek Shale. Correlates with McIvor Sandstone and Mount Ida Formations.||||||
28613|Humevale Siltstone|24328|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
28613|Humevale Siltstone|24329|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
28613|Humevale Siltstone|24551|5|Briefly described|p123|Late Devonian|Late Devonian|Included in the Murrindindi Supergroup.||||||
28613|Humevale Siltstone|24588|5|Briefly described|p20, p12 Fig.3|Pragian|Ludlow|Geological Province: Darraweit Guim Province.||||||29-NOV-13
28613|Humevale Siltstone|32077|5|Briefly described|p33|||||||||
28613|Humevale Siltstone|33238|6|Mentioned|p642|||||||||
28613|Humevale Siltstone|33601|6|Mentioned|Fig.6|||||||||
28613|Humevale Siltstone|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
28613|Humevale Siltstone|37727|6|Mentioned|p53|||||||||
28613|Humevale Siltstone|39331|6|Mentioned|Table 2-1|||||||||
28613|Humevale Siltstone|41585|4|Described|p110|||see also Table 4.1||||||
28613|Humevale Siltstone|42938|5|Briefly described|p576 Fig.3|||||||||
28613|Humevale Siltstone|44187|5|Briefly described|Map Legend||Early Devonian|||||||
28613|Humevale Siltstone|44197|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
28613|Humevale Siltstone|60529|5|Briefly described|Map Legend|Pragian|Ludlow|Distal shelf and hemipelagic sediment: mudstone; brown, laminated; minor very fine to fine grained sandstone and laminae and thin beds towards the top of the formation.||||||
28613|Humevale Siltstone|60591|5|Briefly described|Map Legend|Pragian|Ludlow|Distal shelf and hemipelagic sediment: mudstone; brown, laminated; minor very fine- to fine-grained sandstone laminae and thin beds towards the top of the formation.||||||
28613|Humevale Siltstone|60592|5|Briefly described|Map Legend|Pragian|Ludlow|Distal shelf and hemipelagic sediment: mudstone; brown, laminated; minor very fine- to fine-grained sandstone laminae and thin beds towards the top of the formation.||||||
28613|Humevale Siltstone|60593|5|Briefly described|Map Legend|Pragian|Ludlow|Distal shelf and hemipelagic sediment: mudstone; brown, laminated; minor very fine- to fine-grained sandstone laminae and thin beds towards the top of the formation.||||||
28613|Humevale Siltstone|60595|5|Briefly described|Map Legend|Pragian|Ludlow|Distal shelf and hemipelagic sediment: mudstone; brown, laminated; minor very fine- to fine-grained sandstone laminae and thin beds towards the top of the formation.||||||
28613|Humevale Siltstone|60596|5|Briefly described|Map Legend|Pragian|Ludlow|Distal shelf and hemipelagic sediment: mudstone; brown, laminated; minor very fine- to fine-grained sandstone laminae and thin beds towards the top of the formation.||||||
28613|Humevale Siltstone|60597|5|Briefly described|Map Legend|Pragian|Ludlow|Weakly magnetic, masked by a magnetic intrusion at depth; high K, Th and U||||||
28613|Humevale Siltstone|60599|3|Fully described|p31 Fig. 9, p66-67, p105, p107|Early Devonian|Late Silurian|Supersedes Humevale Fm of Williams (1963). Sequence of thick, monotonous siltstones. Overlain by Wilson Creek Shale; conformable on Melbourne Fm(Melbourne Zone), and Yan Yean Fm; in the south overlies Broadford Formation.||||||27-OCT-08
28613|Humevale Siltstone|61120|6|Mentioned|p2 Fig.1.|||Vandenberg 1970,1971; Garratt 1972||||||22-SEP-14
28613|Humevale Siltstone|61138|5|Briefly described|p207-210, p218|Early Devonian|Late Silurian|Lilydale area. 3800m thick. Contains abundant trilobites (29 species) and brachiopods (75 species). Poorly constrained age of fauna is discussed.||||||
28613|Humevale Siltstone|61185|2|Defined|p22-23, p26, p21 Fig. 6|Pragian|Ludlow|Retained name for portion from Humevale Fm (Williams 1964). Conformable under Wilson Creek Shale; under Lilydale Limestone; covered in part by Hilldene Basalt; conformable over Melbourne Fm and Yan Yean Fm. Geol.Prov: LFB, Melbourne Zone.||||||07-FEB-11
28613|Humevale Siltstone|61701|5|Briefly described|Map Legend|Pragian|Ludlow|Distal shelf and hemipelagic sediment: mudstone; brown, laminated; minor very fine to fine grained sandstone and laminae and thin beds towards the top of the formation.||||||
28613|Humevale Siltstone|61702|5|Briefly described|Map Legend|Pragian|Ludlow|Distal shelf and hemipelagic sediment: mudstone; brown, laminated; minor very fine to fine grained sandstone and laminae and thin beds towards the top of the formation.||||||
28613|Humevale Siltstone|61703|5|Briefly described|Map Legend|Pragian|Ludlow|Distal shelf and hemipelagic sediment: mudstone; brown, laminated; minor very fine to fine grained sandstone and laminae and thin beds towards the top of the formation.||||||
28613|Humevale Siltstone|61704|6|Mentioned|Map legend|Silurian|Silurian|Low K, variable Th.||||||14-JUN-06
28613|Humevale Siltstone|62099|5|Briefly described|p331|Early Devonian|Silurian|In eastern Melbourne Zone of the Lachlan Orogen. ||||||
28613|Humevale Siltstone|62469|5|Briefly described|p7, p20, p38, p60|Lochkovian|Pridoli|At Lilydale, central Victoria. Geological Province: Darraweit Guim Province.  See also p59 Fig. 23.||||||12-FEB-15
28613|Humevale Siltstone|63083|6|Mentioned|p252|Early Devonian|Early Devonian|Acastid fossils recorded in this siltstone.||||||07-FEB-11
28613|Humevale Siltstone|64616|6|Mentioned|p386|||At Lilydale, contains trilobite fossil Sthenarocalymene angustior, which also occurs in the Boola Formation at Tyers. Appears as Humevale Formation in the same paragraph.||||||
28613|Humevale Siltstone|66244|5|Briefly described|pp2-3.|||Equivalent to Kilmore Siltstone (VandenBerg 1992), which it now replaces, having precedence. Also replaces Yan Yean Formation in the Merriang-Wandong area, continuing all the way to Kilmore. |||Includes Clonbinane and Mount Phillipa Members.|Interfingers with, and locally is overlain conformably by, Broadford Formation.||
28613|Humevale Siltstone|68116|5|Briefly described|Appendix, Maps 24-25, 32-33, 41-42.|Early Devonian|Llandovery||||||Siltstone: brown, laminated; minor very fine- to fine-grained sandstone laminae and thin beds towards the top of the formation; distal shelf and hemipelagic deposits.|
28613|Humevale Siltstone|69089|5|Briefly described|Map legend|Early Devonian|Early Devonian||||||Marine: black shale, black siltstone.|
28613|Humevale Siltstone|70487|6|Mentioned|p 8-11, p11 Fig.5, p13|Lochkovian|Llandovery|Fossils occur in a thin diamictite bed within a sequence which is otherwise thin-bedded (even shaly) siltstone. Include trilobite fragments and vascular plant fragments. Graptolites enabled early Llandovery date estimate.||||Interfingers with and overlies Broadford Formation. Possible lateral equivalence by palaentological evidence with Lochkovian part of Broadford Formation (Sandford 2002).|Fossiliferous siltstone, thin diamictite bed.|
28613|Humevale Siltstone|73497|5|Briefly described|Map legend|Devonian|Devonian|Marine.||Murrindindi Supergroup|||Mudstone, siltstone, minor sandstone: weakly magnetic, masked by a magnetic body at depth; high K, Th and U.|
28613|Humevale Siltstone|75072|6|Mentioned|p232, 240|Late Silurian|Late Silurian|Melbourne Zone. Zircon age distribution.|||||Quartz-rich metagreywacke.|
8585|Hummocks Serpentinite|23309|5|Briefly described|p24, p25 Table 2.1, p26 Table 2.2|Cambrian|Neoproterozoic|Age:  700 Ma +/- 200 Ma||||||03-SEP-18
8585|Hummocks Serpentinite|24551|5|Briefly described|p75 Fig. 3.3|||||||||
8585|Hummocks Serpentinite|42275|6|Mentioned|p468|||||||||
8585|Hummocks Serpentinite|43218|5|Briefly described|p21|Cambrian|Precambrian|||||||
8585|Hummocks Serpentinite|43846|4|Described|9|Middle Cambrian|Early Cambrian|Informal name||||||
8585|Hummocks Serpentinite|50154|2|Defined|p14, p47, p216, p249 App.5|Cambrian|Neoproterozoic|Of the Glenelg River Metamorphic Complex. Age: 700 Ma (Nd/Sm model age), however a Cambrian age is likely. Geological Province: Hummocks Fault Zone, Delamerian Fold Belt.||||||15-SEP-04
8585|Hummocks Serpentinite|50156|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Serpentinite: massive, dark green; talc schist; massive chlorite-magnetite rock.||||||20-MAY-13
8585|Hummocks Serpentinite|50157|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Serpentinite: massive, dark green; talc schist; massive chlorite-magnetite rock.||||||20-MAY-13
8585|Hummocks Serpentinite|50158|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Serpentinite: massive, dark green; talc schist; massive chlorite-magnetite rock.||||||20-MAY-13
8585|Hummocks Serpentinite|50159|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Serpentinite: massive, dark green; talc schist; massive chlorite-magnetite rock.||||||20-MAY-13
8585|Hummocks Serpentinite|50160|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|||||||
8585|Hummocks Serpentinite|50161|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Serpentinite: massive, dark green; talc schist; massive chlorite-magnetite rock.||||||20-MAY-13
8585|Hummocks Serpentinite|50162|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Serpentinite: massive, dark green; talc schist; massive chlorite-magnetite rock.||||||20-MAY-13
8585|Hummocks Serpentinite|50163|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Serpentinite: massive, dark green; talc schist; massive chlorite-magnetite rock.||||||20-MAY-13
8585|Hummocks Serpentinite|50164|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Glenelg River Metamorphic Complex (Moralana Supergroup).||||||
8585|Hummocks Serpentinite|60451|6|Mentioned|p22|||||||||
8585|Hummocks Serpentinite|62742|6|Mentioned|p698|||Ultramafic rocks.||||||
8585|Hummocks Serpentinite|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Defined by Wells 1956 p96; Morand et al 2003.||||||
8585|Hummocks Serpentinite|68116|5|Briefly described|Appendix, Map 29.|Middle Cambrian||Precambrian maximum age.|||||Serpentinite: massive, dark green, cumulate texture locally preserved; talc schist; massive chlorite-magnetite rock. Relic pyroxene indicated by exsolution lamellae defined by magnetite granules.|10-JUN-14
8585|Hummocks Serpentinite|71593|6|Mentioned|p12, p19-p20, p123, p133|||Glenelg Zone. Petrography discussed. See also p150, p166, p169-p170, p172, p180, p195, p199.||||||
8585|Hummocks Serpentinite|72445|6|Mentioned|App 7 p6 Fig.3.|Cambrian|Cambrian|Shown only on the geological map covering the Stavely Project area (from Geology of Victoria 2003: 21).||||||
35154|Hunken Granite|22971|5|Briefly described|p 34|||||||||
30592|Hylands Member|23309|5|Briefly described|p138. Table 2.49|||||||||
30592|Hylands Member|24177|5|Briefly described|p52, p50 Fig.22|Lochkovian|Ludlovian|Lowermost unit in McIvor Sandstone. Geological Province: Darraweit Guim Province.||||||11-MAY-04
30592|Hylands Member|24328|5|Briefly described|Map legend|Late Silurian|Late Silurian|Parent: McIvor Sandstone.||||||27-OCT-08
30592|Hylands Member|24329|5|Briefly described|Map legend|Late Silurian|Late Silurian|Parent: McIvor Sandstone.||||||27-OCT-08
30592|Hylands Member|60591|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the McIvor Sandstone. Overlies the Dargile Formation. Consists of a sequence of thin-bedded turbiditites and interbedded bioturbated siltstones; abundant shelly fossils.||||||
30592|Hylands Member|60592|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the McIvor Sandstone. Overlies the Dargile Formation. Consists of a sequence of thin-bedded turbiditites and interbedded bioturbated siltstones; abundant shelly fossils.||||||25-NOV-04
30592|Hylands Member|60593|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the McIvor Sandstone. Overlies the Dargile Formation. Consists of a sequence of thin-bedded turbiditites and interbedded bioturbated siltstones; abundant shelly fossils.||||||
30592|Hylands Member|60595|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the McIvor Sandstone. Overlies the Dargile Formation. Consists of a sequence of thin-bedded turbiditites and interbedded bioturbated siltstones; abundant shelly fossils.||||||26-NOV-04
30592|Hylands Member|60596|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the McIvor Sandstone. Overlies the Dargile Formation. Consists of a sequence of thin-bedded turbiditites and interbedded bioturbated siltstones; abundant shelly fossils.||||||
30592|Hylands Member|60597|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the McIvor Sandstone. Low magnetic response, with weak linear features; distinct high K band, higher K response than the rest of the McIvor Sandstone, moderate Th, variable U.||||||29-NOV-04
30592|Hylands Member|60599|2|Defined|p24 Tb. 4, p58|Ludlow|Ludlow|Of McIvor Sandstone. Comprises former units 3 and 4 of the Dargile Beds. Monotonous sequence of thinly bedded turbidites with variable interbedded bioturbated siltstone. Thickness: ~320m.||||||08-OCT-08
30592|Hylands Member|61185|5|Briefly described|p21 Fig. 6|Ludlow|Ludlow|Of McIvor Sandstone. Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
30592|Hylands Member|64611|5|Briefly described|Map legend|Ludlow|Ludlow|Of McIvor Sandstone (Murrindindi Supergroup). Sandstone, siltstone and mudstone: monotonous sequence of thin bedded turbidites and interbedded bioturbated siltstone; large nested channels, abundant shelly fossils. Moderately shallow-marine deposits.||||||15-DEC-08
30592|Hylands Member|64612|2|Defined|p41-42|Late Ludlow|Late Ludlow|Basal portion of McIvor Sandstone. Conformably overlies Dargile Formation, contact is gradational. Underlies McIvor Sandstone. Thick: 300m. Monotonous sequence of thin-bedded turbiditic quartz sandstone and interbedded bioturbated mudstone.||||||07-FEB-11
30592|Hylands Member|66244|5|Briefly described|p2.|||Defined by Edwards et al. (1998) to include the Dargile Sandstone and the Chonetes-Encrinurus Mudstone of Thomas (1937).||Unit in McIvor Sandstone.||||
41195|Hypatia Formation|50154|2|Defined|p124-126, p129, p130|Late Jurassic|Early Jurassic|Overlies the Moralana Supergroup, Glenelg River Metamorphic Complex, Dergholm Granite and Bacchus Marsh Formation. Locally interbedded with Den Hills formation. Max. thickness at type locality: 80m. Age: 191 +/- 10 Ma, 153 +/- 5 Ma (K/Ar).||||||25-SEP-09
41195|Hypatia Formation|50155|5|Briefly described|Map Legend|Jurassic|Jurassic|Plugs and Flows; olivine basalt, nephelenite, hawaiite, basanite, mugearite, ankaramite, picrobasalt||||||
41195|Hypatia Formation|50156|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Flows and plugs of olivine basalt, nephelenite, hawaiite, basanite, mugearite, ankaramite, picrobasalt.||||||24-JUN-04
41195|Hypatia Formation|50157|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Flows and plugs of olivine basalt, nephelenite, hawaiite, basanite, mugearite, ankaramite, picrobasalt.||||||
41195|Hypatia Formation|50158|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Flows and plugs of olivine basalt, nephelenite, hawaiite, basanite, mugearite, ankaramite, picrobasalt.||||||
41195|Hypatia Formation|50159|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Flows and plugs of olivine basalt, nephelenite, hawaiite, basanite, mugearite, ankaramite, picrobasalt.||||||
41195|Hypatia Formation|50160|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Overlain by Lowan Sand, Parilla Sand and Duddo Limestone. Flows and plugs of olivine basalt, nephelenite, hawaiite, basanite, mugearite, ankaramite, picrobasalt.||||||25-JUN-04
41195|Hypatia Formation|50161|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Flows and plugs of olivine basalt, nephelenite, hawaiite, basanite, mugearite, ankaramite, picrobasalt.||||||
41195|Hypatia Formation|50162|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Flows and plugs of olivine basalt, nephelenite, hawaiite, basanite, mugearite, ankaramite, picrobasalt.||||||
41195|Hypatia Formation|50163|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Flows and plugs of olivine basalt, nephelenite, hawaiite, basanite, mugearite, ankaramite, picrobasalt.||||||
41195|Hypatia Formation|50164|5|Briefly described|Map Legend|Jurassic|Jurassic|Of Coleraine Volcanic Group. Flows and plugs of olivine basalt, nephelenite, hawaiite, basanite, mugearite, ankaramite, picrobasalt.||||||
41195|Hypatia Formation|66002|5|Briefly described|p9 Tb.6|Mesozoic|Mesozoic|Of Coleraine Volcanic Group.  Defined by Morand et al. 2003.||||||
41195|Hypatia Formation|68116|5|Briefly described|Appendix, Maps 29, 38.|Jurassic|Jurassic||||||Flows and plugs of olivine basalt, nephelinite, hawaiite, basanite, mugearite, ankaramite, picrobasalt. Flows are black, vesicular, fine-grained with small phenocrysts of olivine and pyroxene. Plugs are strongly porphyritic in olivine and pyroxene.|10-JUN-14
74775|Illaenus Band|60599|5|Briefly described|p47 Fig. 19|Llandovery|Llandovery|Variation of "Illaenus Band" - both informal names. Part of Costerfield Siltstone. See also p49-50.||||||
74775|Illaenus Band|61185|5|Briefly described|p21 Fig. 6|Llandovery|Llandovery|At top of Costerfield Siltstone. Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
37748|Illoura Granodiorite|23309|5|Briefly described|p433, Appendix 1|Late Devonian|Middle Devonian|G 305, I-Type.  Supersedes Lismore Granite.  Age: 369+/-18Ma.||||||
37748|Illoura Granodiorite|64314|6|Mentioned|p494, p495 Fig. 2|||I-type.||||||21-OCT-08
37748|Illoura Granodiorite|66002|5|Briefly described|p6 Tb.5|||Of Beckworth Suite. G305. Defined in VandenBerg et al. 2000. Incorporates superseded Wallinduc Granodiorite and part of the Tiac Granite of White & Chappell 1988.||||||
37748|Illoura Granodiorite|68116|5|Briefly described|Appendix, Map 40.|Late Devonian|Late Devonian||||||Coarse grained equigranular hornblende biotite granodiorite and porphyritic biotite granite with phenocrysts of K-feldspar, plagioclase and quartz; pale pinkish grey; mafic clots and enclaves abundant in the granodiorite.|
27436|Ingliston Granite|22885|5|Briefly described|map|||||||||
27436|Ingliston Granite|22886|4|Described|Table.1|||||||||
27436|Ingliston Granite|23258|5|Briefly described|Fig12-3.1p214, 215||Devonian|||||||
27436|Ingliston Granite|23309|6|Mentioned|p433 App1|||G279 I-Type. Supersedes Ingliston Granodiorite.||||||
27436|Ingliston Granite|24551|6|Mentioned|p218|||||||||
27436|Ingliston Granite|39865|4|Described|p15|||||||||
27436|Ingliston Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
27436|Ingliston Granite|44197|5|Briefly described|Map Legend||Late Devonian|G279 I-type.||||||
27436|Ingliston Granite|62897|6|Mentioned|p118|Devonian|Devonian|||||||18-MAR-08
27436|Ingliston Granite|63741|6|Mentioned|p118|Devonian|Devonian|||||||
27436|Ingliston Granite|65715|6|Mentioned|p7 Tb.4|||Defined in Roberts (1984) p15-16. G279.||||||
27436|Ingliston Granite|65974|6|Mentioned|p55|||Modelled with a larger lateral extent than mapped at the surface, indicating granite at shallow depths proximal to the known contact.||||||
27436|Ingliston Granite|68116|5|Briefly described|Appendix, Map 41.|Late Devonian|Late Devonian||||||Biotite granite: grey; medium to coarse-grained; dykes of quartz porphyry and feldspar porphyry.|
34711|Ino Creek Granodiorite|22878|4|Described|p89|||Highly magnetic along northwestern boundary, lower (180-250 nT) over eastern part.||||||06-OCT-04
34711|Ino Creek Granodiorite|22879|5|Briefly described|map|Silurian|Silurian|Of the Kuark Metamorphic Complex. Biotite-muscovite granodiorite: brownish grey, coarse grained, massive; prominent quartz; includes pods of fine-grained leucocratic muscovite granite and pegmatite.||||||10-JUN-14
34711|Ino Creek Granodiorite|22880|5|Briefly described|Map Legend|Silurian|Silurian|Of the Kuark Metamorphic Complex. Biotite-muscovite granodiorite: brownish grey, coarse grained, massive; prominent quartz; includes pods of fine-grained leucocratic muscovite granite and pegmatite.||||||10-JUN-14
34711|Ino Creek Granodiorite|23309|5|Briefly described| p313||Silurian|Supersedes Ino Creek Granite. G27 -  I-Type||||||
34711|Ino Creek Granodiorite|24551|6|Mentioned|p49|Middle Silurian|Middle Silurian|||||||
34711|Ino Creek Granodiorite|68116|5|Briefly described|Appendix, Map 37.|Wenlock|Llandovery||||||Biotite-muscovite granodiorite: brownish grey, coarse grained, massive; prominent quartz; includes pods of fine-grained leucocratic muscovite granite and pegmatite.|
8753|Iona Tonalite|22815|4|Described|p56|Silurian|Silurian|Formerly known as Iona Granodiorite.||||||
8753|Iona Tonalite|22876|4|Described|p24|||Currawong Suite||||||
8753|Iona Tonalite|22877|5|Briefly described|map|Silurian|Silurian|Currowong Suite. G54. Tonalite. I-Type.||||||26-OCT-04
8753|Iona Tonalite|23309|5|Briefly described|p68, 338, 344, 350|Silurian|Silurian|G54 - I-Type. Age: 422 +/- 3 Ma.||||||
8753|Iona Tonalite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
8753|Iona Tonalite|41572|6|Mentioned|Fig.1.10|||||||||
8753|Iona Tonalite|41905|2|Defined|p61|Silurian||||||||
8753|Iona Tonalite|41933|5|Briefly described|Map legend|Late Silurian||||||||
8753|Iona Tonalite|42627|5|Briefly described|Map legend|Wenlock||||||||
8753|Iona Tonalite|42647|4|Described|p39|||Currowong Suite||||||
8753|Iona Tonalite|42827|6|Mentioned|Fig 1.10|||||||||
8753|Iona Tonalite|43233|5|Briefly described|Map Legend|Late Silurian||of Currowong Suite.||||||
8753|Iona Tonalite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh23||||||
8753|Iona Tonalite|60078|6|Mentioned|Map Legend|Devonian|Late Silurian|||||||
8753|Iona Tonalite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Tonalite: medium to fine grained, pale green to pink; moderately foliated.|
8785|Irondoon Granodiorite|22876|5|Briefly described|p18 Table 3|Late Silurian|Late Silurian|||||||
8785|Irondoon Granodiorite|22877|5|Briefly described|map|Silurian|Silurian|Kuark Metamorphic Complex Supersuite. G32. Biotite granodiorite.||||||26-OCT-04
8785|Irondoon Granodiorite|22878|4|Described|p87|||||||||
8785|Irondoon Granodiorite|22879|5|Briefly described|map|Silurian|Silurian|Of the Kuark Metamorphic Complex. Biotite granodiorite: dark grey, medium grained, strongly foliated; dyke like bodies; abundant elongate mafic inclusions.||||||01-OCT-04
8785|Irondoon Granodiorite|22880|5|Briefly described|Map Legend|Silurian|Silurian|Of the Kuark Metamorphic Complex. Biotite granodiorite: dark grey, medium grained, strongly foliated; dyke like bodies; abundant elongate mafic inclusions.||||||01-OCT-04
8785|Irondoon Granodiorite|22881|5|Briefly described|Map legend|Silurian|Silurian|Of the Kuark Metamorphic Complex Supersuite. Biotite granodiorite: Moderately magnetic (40-60 nT). High K, Th and U.||||||06-OCT-04
8785|Irondoon Granodiorite|23309|6|Mentioned|p433 App 1|||G32 I-Type.||||||
8785|Irondoon Granodiorite|30574|6|Mentioned|p9|||||||||
8785|Irondoon Granodiorite|30938|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
8785|Irondoon Granodiorite|40328|4|Described|p207|||||||||
8785|Irondoon Granodiorite|46574|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Berridale Batholith. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
8794|Irymple Member|24551|5|Briefly described|p338 Fig. 11.2, 340|Middle Pleistocene|Late Pliocene|||||||
8794|Irymple Member|30935|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
8794|Irymple Member|31745|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
8794|Irymple Member|35272|4|Described|p284|||||||||
8794|Irymple Member|37873|6|Mentioned|p9|||||||||
8794|Irymple Member|41537|6|Mentioned|p350|||||||||
8794|Irymple Member|41848|5|Briefly described|p359|||Lower part of Blanchetown Clay.||||||21-APR-09
8794|Irymple Member|42827|5|Briefly described|p359|||see also Table 9.1, of Blanchetown Clay.||||||21-APR-09
8794|Irymple Member|42966|2|Defined|Table 33 p200|Late Pleistocene|Late Pliocene|Of Blanchetown Clay.||||||21-APR-09
8794|Irymple Member|44133|6|Mentioned|p252|||Equivalent to Chowilla Sand.||||||
8794|Irymple Member|64961|5|Briefly described|p260|||Brown and Stephenson (1991) equated this unit of  Lawrence (1975) to Gill's (1973)Chowilla Sand,||||||25-FEB-13
83701|Jacaranda Ridge Sandstone|73594|5|Briefly described|p45, p50-51|||Otway Basin. Informal subdivision of the upper Sawpit Shale introduced by Camac and Boult (2008). Appears to be restricted to the Penola Trough.||Upper Sawpit Shale|||Thin, laterally extensive unit interpreted as a sheet sand.|
8824|Jack River Formation|38930|5|Briefly described|p64|||||||||
8841|Jahanna River Formation|41626|6|Mentioned|p52|||||||||
35145|Jallukar Volcanics|23061|6|Mentioned|293 fig 1|||||||||
73609|Jamieson Volcanic Group|66244|5|Briefly described|p2.|Cambrian|Cambrian|Has been extended to include all the Cambrian calcalkaline volcanic and related rocks in the eastern Melbourne Zone, including those in the (now redundant) Licola Volcanic Group and those in the Glen Creek Window. All are potentially continuous under the overlying Ordovician to Devonian strata.|||Includes Cobbs Spur Andesite Breccia, Tobacco Creek Andesite and Whisky Knob Rhyolite.||Andesite, rhyolite, volcanic breccia, minor volcaniclastic sandstone and limestone.|
73609|Jamieson Volcanic Group|66769|5|Briefly described|121, 136-138, 156 Fig 8, 13, 15|Cambrian|Cambrian|Selwyn Block. Calcalkaline volcanics. Formerly the Licola Volcanic Group. Correlated with Mount Read Volcanics in Tas.||||||
73609|Jamieson Volcanic Group|67104|6|Mentioned|p635, p634, p638 |||Selwayn Block. Formerly Licola Volcanic Group. Similar age, petrography and composition to the Mount Stavely Volcanics of western Victoria.||||||
73609|Jamieson Volcanic Group|68116|5|Briefly described|Appendix, Map 25.|Cambrian|Cambrian||||||Andesite and dacite: green; highly silicified; includes porphyritic andesite with plagioclase, hornblende and rare quartz, clinopyroxene and K-feldspar; flow-banded in places.|
73609|Jamieson Volcanic Group|71593|6|Mentioned|p156, p182-p184|||Melbourne Zone. Hosts the Hill 800 Prospect.||||||
8858|Jan Juc Marl|22626|6|Mentioned|446 fig 10, 447|Late Oligocene|Late Oligocene|Geol province East Otway Basin. Overlying unit Puebla Clay, underlying unit Angahook Formation||||||
8858|Jan Juc Marl|23778|6|Mentioned|p674|||||||||
8858|Jan Juc Marl|24038|5|Briefly described|p439 Fig.2|Oligocene|Oligocene|Geological Province: Torquay Basin||||||
8858|Jan Juc Marl|24551|5|Briefly described|p313, 310 Fig. 10.18|||Of the Torquay Group.||||||
8858|Jan Juc Marl|33155|4|Described|p118|||||||||
8858|Jan Juc Marl|37602|4|Described|p645|||||||||
8858|Jan Juc Marl|43702|6|Mentioned|Fig.2,p398|Miocene|Late Oligocene|||||||
8858|Jan Juc Marl|60785|5|Briefly described|p184 Fig.1, pp190-191, pp199-200.   |Chattian|Chattian|Of the Torquay/Port Phillip Basins. Foraminifera zone P21-P22 (Holdgate and Gallagher,2003) Sr/Sr age of 23.9-27.4 Ma (Dickinson, 2002). The most important unit for fossil cetaceans in Australia to date; has yielded a variety of elements including eight skulls/skeletons.|||||Grey-yellow glauconitic and pyritic carbonate-cemented calcarenite. Silty glauconitic marl and clayey sandy glauconitic calcarenite.|
8858|Jan Juc Marl|65316|4|Described|p595, p598, p597 Fig 2, 601-603|Aquitanian|Rupelian|Torquay Basin. Equivalent to lower Point Addis Limestone;  thought correlative of Clifton Formation; subsurface age may be 30-32.6Ma.|28.4 - 23.03 Ma.|Of Torquay Group.||Overlies Demons Bluff Group; conformably overlain by Puebla Clay.|Fine-grained silty glauconitic marl with sandy calcarenite interbeds; coarsens upwards.|23-APR-12
8858|Jan Juc Marl|67061|5|Briefly described|p546.|Oligocene|Oligocene|See also Jan Juc Formation p546, p555 Fig.12, p557.|27.9 - 24.2 Ma.|Unit in Torquay Group.||||16-MAR-12
8858|Jan Juc Marl|70942|5|Briefly described|p121, 119|||||||||17-FEB-17
30295|Japan Creek Gravel|60503|5|Briefly described|p139, p21 Fig. 4|Tertiary|Tertiary|Fine gravel and medium/coarse sand and minor pebbly sand, with good sorting and well-rounded pebbles, consisting of quartzite,vein quartz and sandstone. Forms a thin cover on Morass Creek Basalt. Inferred to be Pleistocene. ||||||
30295|Japan Creek Gravel|60504|5|Briefly described|Map Legend|Pliocene|Pliocene|Alluvium: gravel, sand; moderately to well sorted and poorly to moderately consolidated||||||20-OCT-04
30295|Japan Creek Gravel|60505|5|Briefly described|Map legend|Pliocene|Pliocene|Alluvium: gravel, sand; moderately to well sorted and poorly to moderately consolidated||||||
30295|Japan Creek Gravel|60506|5|Briefly described|Map legend|Pliocene|Pliocene|Alluvium: gravel, sand; moderately to well sorted and poorly to moderately consolidated||||||
30295|Japan Creek Gravel|60507|5|Briefly described|Map Legend|Pliocene|Pliocene|Alluvium: gravel, sand; moderately to well sorted and poorly to moderately consolidated||||||
30295|Japan Creek Gravel|60508|5|Briefly described|Map legend|Quaternary|Tertiary|Alluvium: magnetic response masked by Morass Creek Basalt; moderate Th, low total count, K, U.||||||
30295|Japan Creek Gravel|68116|5|Briefly described|Appendix, Map 27.|Pleistocene|Pliocene||||||Gravel, sand: moderately to well sorted and poorly to moderately consolidated.|
8881|Jarrahmond Granite|23309|6|Mentioned|p433 App 1|||G45 I-Type.||||||
8881|Jarrahmond Granite|42726|5|Briefly described|map legend|Early Devonian||NOT variation on Jarrahmond Formation.||||||
8881|Jarrahmond Granite|43312|5|Briefly described|Map Legend||Wenlock|G45. Hornblende-biotite granodiorite, grey-green, medium grained with some elongate mafic enclaves, altered, I-Type.||||||26-OCT-04
8881|Jarrahmond Granite|43313|5|Briefly described|Map Legend||Wenlock|||||||
8881|Jarrahmond Granite|60542|4|Described|p93-94, p88 Tb. 4|||See also Jarrahmond Granodiorite; and p23 Tb. 2 - presented as Jarrahmond only. Med- to coarse-gr.granite; characterised by lg. perfectly-shaped crystals of hornblende; mafic xenoliths, qtz-poor and rich in opaque oxides, hornblende, biotite, plagioclase.||||||19-DEC-07
8881|Jarrahmond Granite|68116|5|Briefly described|Appendix.|Devonian|Silurian||||||Hornblende-biotite granodiorite: grey-green, medium-grained with some elongate mafic enclaves; I-type.|
28623|Jeffcott Granite|23309|5|Briefly described|p339|||G334 - S-Type. Age: 392 +/- 6 Ma, 375 +/- 6Ma, 389 +/- 6Ma, 411 +/- 4Ma.||||||
28623|Jeffcott Granite|24551|6|Mentioned|p717 Table 2.4|Early Devonian|Early Devonian|Age: 402 +/- 2Ma.||||||
28623|Jeffcott Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
28623|Jeffcott Granite|60491|4|Described|p31, p38|Devonian|Late Silurian|Of the Glenloth Suite. Age: 411+/- 4 Ma to 389 +/- 6 Ma (K/Ar muscovite), 392 +/- 6 Ma to 375 +/- 6 Ma (K/Ar Biotite). Intrudes the Wycheproof Granite. Intruded by the Whitimaria Granite and Chirrup pluton.||||||22-NOV-04
28623|Jeffcott Granite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Glenloth Suite. Leucocratic granite: medium to coarse grained, pale grey; contains biotite and garnet; weathered in part to quartz grains in a kaolinite matrix.||||||
28623|Jeffcott Granite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of the Glenloth Suite. Age: 392+/-6 Ma, 411+/-4 Ma (K/Ar). Granite; reduced S-type; essentially nonmagnetic, most responses < 5 nT; gravity response less than host metasediments; over outcrops K is higher, Th and U similar to nearby alluvium.||||||
28623|Jeffcott Granite|66002|5|Briefly described|p6 Tb.5|||Of Glenloth Suite. G334. Defined in Bibby and Moore 1998.||||||
28623|Jeffcott Granite|68116|5|Briefly described|Appendix, Map 16.|Middle Devonian|Early Devonian||||||Leucocratic garnet-muscovite granite: medium to coarse grained.|
28623|Jeffcott Granite|68189|6|Mentioned|p42 App.2|||K-Ar ages from McKenzie et al. (1984) and Richards & Singleton (1981) respectively.|411 +/- 4 Ma to 375 +/- 6 Ma.|||||30-JUN-14
22023|Jellung Ignimbrite|23309|4|Described|p108. Tb 2.40||Early Devonian|Age: 400 +/- 8 Ma [this appears to be the Rb/Sr age of the Jemba Ignimbrite, shown on p126, NOT the Jellung Ignimbrite - CEB16-AUG-2018]. Of the Little River Subgroup.  Maximum Thickness: 250m.||||||16-AUG-18
22023|Jellung Ignimbrite|23615|3|Fully described|p129|Early Devonian|Early Devonian|Of Little River Subgroup.  80m thick at type section.  Feldspathic ignimbrite with purple matrix, weathering to pink, grey and yellow, containging phenocrysts, lithic clasts and pumice fragments.||||||
22023|Jellung Ignimbrite|23938|6|Mentioned|p55 Tb. 4|||Of the Snowy River Volcanics.||||||25-SEP-08
22023|Jellung Ignimbrite|24551|5|Briefly described|p145|||Of Little River Subgroup.||||||
22023|Jellung Ignimbrite|43206|5|Briefly described|map legend||Lochkovian|of Little River Subgroup.||||||
22023|Jellung Ignimbrite|43312|5|Briefly described|Map Legend||Early Devonian|Of Little River Group.||||||25-SEP-08
22023|Jellung Ignimbrite|43313|5|Briefly described|Map Legend||Early Devonian|Of Little River Group.||||||25-SEP-08
22023|Jellung Ignimbrite|60542|3|Fully described|p62, p115 Fig. 47|Early Devonian|Early Devonian|Of Little River Subgroup. Formerly "Upper Feldspathic Lenticle Tuff". Conformably overlies Buchan Caves Lst; overlies McRaes Ignimbrite, Rankin Road Ignimbrite, Balley Hooley Ignimbrite; overlain by Spring Creek Mbr, Moores Ford Andesite.||||||
22023|Jellung Ignimbrite|63594|5|Briefly described|p1032 Fig. 1|||Of the Snowy River Volcanics.||||||04-OCT-07
22023|Jellung Ignimbrite|68116|5|Briefly described|Appendix, Maps 36, 45.|Early Devonian|Early Devonian||||||Feldspar ignimbrite: sparse small quartz phenocrysts, commonly with well developed eutaxitic foliation, variably welded; pyroclastic deposits.|
37869|Jemba Ignimbrite|23309|5|Briefly described|p121, p126|||Maximum Thickness: 650m. Rb/Sr age 400 +/-8 Ma (Richards & Singleton, 1981) recalculated from 409+/-8 Ma (Brooks & Leggo, 1972)||||||16-AUG-18
37869|Jemba Ignimbrite|24133|3|Fully described|p43|Devonian|Devonian|Parent: Mount Burrowa Group.  Geological Province: Lachlan Fold Belt.||||||
37869|Jemba Ignimbrite|24142|5|Briefly described|Map Legend|Devonian|Devonian|Of Mount Burrowa Volcanic Group. Geological Province: Lachlan Fold Belt.||||||
37869|Jemba Ignimbrite|24143|5|Briefly described|Map Legend|Devonian|Devonian|Of Mount Burrowa Volcanic Group. Geological Province: Lachlan Fold Belt.||||||
37869|Jemba Ignimbrite|24144|5|Briefly described|Map Legend|Devonian|Devonian|Of Mount Burrowa Volcanic Group. Geological Province: Lachlan Fold Belt.||||||
37869|Jemba Ignimbrite|24145|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of Mount Burrowa Volcanic Group. Geological Province: Lachlan Fold Belt||||||
37869|Jemba Ignimbrite|24551|5|Briefly described|p148|Devonian|Devonian|Included as part of the Mount Burrowa Cauldron Complex.||||||
37869|Jemba Ignimbrite|68116|5|Briefly described|Appendix, Map 20.|Middle Devonian|Early Devonian||||||Ignimbrite: dark bluish grey to pinkish grey, crystal rich, mostly recrystallised; sparse small lithic fragments; highly magnetic.|
8906|Jemmys Point Formation|23230|5|Briefly described|Table4-1p40||Pliocene|||||||
8906|Jemmys Point Formation|23768|5|Briefly described|p30 Fig.6|Early Pliocene|Late Miocene|Overlies Tambo River Formation. Geological Province: Gippsland Basin.  See also p27, p171, p173.||||||29-MAR-05
8906|Jemmys Point Formation|23909|5|Briefly described|p295|Pliocene|Pliocene|Geological Province: Gippsland Basin.||||||
8906|Jemmys Point Formation|24038|5|Briefly described|p439 Fig.2|Pliocene|Miocene|Geological Province: Gippsland Basin||||||
8906|Jemmys Point Formation|24468|5|Briefly described|p405 Fig.2|Pliocene|Pliocene|Geological Province: Gippsland Basin. Of the Hapuku Subgroup. Point is spelt Pt. in text||||||
8906|Jemmys Point Formation|24551|5|Briefly described|p327 Fig. 10.33, 608|Early Pliocene|Late Miocene|||||||
8906|Jemmys Point Formation|29355|6|Mentioned|p185|||||||||
8906|Jemmys Point Formation|29591|6|Mentioned|p54|||||||||
8906|Jemmys Point Formation|29673|6|Mentioned|p311|||||||||
8906|Jemmys Point Formation|30582|6|Mentioned|p9|||Kangaroo remains||||||
8906|Jemmys Point Formation|30836|4|Described|p1264|||Early Pliocene||||||
8906|Jemmys Point Formation|30865|6|Mentioned|p310|||Upper Miocene-Lower Pliocene age||||||
8906|Jemmys Point Formation|30933|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
8906|Jemmys Point Formation|31351|6|Mentioned|Fig. 5|||||||||
8906|Jemmys Point Formation|31352|4|Described|p134|||See also Fig. 3. Pliocene.||||||
8906|Jemmys Point Formation|31509|6|Mentioned|p155|||||||||
8906|Jemmys Point Formation|31516|6|Mentioned|Fig. 6|||Ammatocarcinus distribution||||||
8906|Jemmys Point Formation|31627|6|Mentioned|p12|||||||||
8906|Jemmys Point Formation|32636|5|Briefly described|p33|||L.Pliocene||||||
8906|Jemmys Point Formation|32679|6|Mentioned|p94|||||||||
8906|Jemmys Point Formation|33160|6|Mentioned|p303|||||||||
8906|Jemmys Point Formation|33358|6|Mentioned|Table 1|||Plio.||||||
8906|Jemmys Point Formation|33362|6|Mentioned|p112|||Strat.diag.||||||
8906|Jemmys Point Formation|33413|6|Mentioned|p236|||L.Pliocene||||||
8906|Jemmys Point Formation|33459|6|Mentioned|p10|||Stratigraphy.||||||
8906|Jemmys Point Formation|33689|5|Briefly described|p13|||||||||
8906|Jemmys Point Formation|33929|6|Mentioned|p71|||||||||
8906|Jemmys Point Formation|34519|6|Mentioned|p47|||||||||
8906|Jemmys Point Formation|34558|5|Briefly described|p19|||Pliocene||||||
8906|Jemmys Point Formation|34832|6|Mentioned|p23|||||||||
8906|Jemmys Point Formation|34842|6|Mentioned|Table 3|||||||||
8906|Jemmys Point Formation|34843|6|Mentioned|p10|||||||||
8906|Jemmys Point Formation|34892|4|Described|p370|||||||||
8906|Jemmys Point Formation|35097|6|Mentioned|p36|||||||||
8906|Jemmys Point Formation|35271|6|Mentioned|p67|||||||||
8906|Jemmys Point Formation|35273|3|Fully described|p261|||||||||
8906|Jemmys Point Formation|35720|6|Mentioned|p131|||See also Fig.2, stratigraphic column.||||||
8906|Jemmys Point Formation|36386|6|Mentioned|p156|||||||||
8906|Jemmys Point Formation|37330|5|Briefly described|Table 4|||||||||
8906|Jemmys Point Formation|37809|6|Mentioned|p5|||||||||
8906|Jemmys Point Formation|38070|6|Mentioned|Fig.12|||Gippsland Basin||||||
8906|Jemmys Point Formation|38929|4|Described|p52|||See also Fig.6||||||
8906|Jemmys Point Formation|40703|5|Briefly described|p89|||||||||
8906|Jemmys Point Formation|41043|5|Briefly described|p97|||||||||
8906|Jemmys Point Formation|41075|6|Mentioned|p22|||||||||
8906|Jemmys Point Formation|41511|4|Described|p14|||||||||
8906|Jemmys Point Formation|41868|6|Mentioned|Fig.12.14|||||||||
8906|Jemmys Point Formation|42184|6|Mentioned|Fig.2 P348|||||||||
8906|Jemmys Point Formation|42824|6|Mentioned|p262|||||||||
8906|Jemmys Point Formation|42827|3|Fully described|p335|||Of Seaspray Group.||||||01-JUL-08
8906|Jemmys Point Formation|43667|6|Mentioned|Fig.3,p12||Pliocene|||||||
8906|Jemmys Point Formation|45128|6|Mentioned|p56|||||||||
8906|Jemmys Point Formation|60538|5|Briefly described|p483 Fig. 22, 488 Fig. 27|||Geological Province: Gippsland Basin.||||||
8906|Jemmys Point Formation|60542|5|Briefly described|p84|Tertiary|Tertiary|Of the Seaspray Group. ||||||
8906|Jemmys Point Formation|60785|5|Briefly described|p184 Fig.1, pp193-194.  |Zanclean|Messinian|Of the Gippsland Basin. planktonic foraminifera zone N18-N19 (Holdgate and Gallagher, 2003). Has yielded fossil cetacean elements including one incomplete skeleton.|||||Sandy clay with shell beds. Also, phosphorite concretions.|
8906|Jemmys Point Formation|61155|6|Mentioned|2|||||||||
8906|Jemmys Point Formation|61207|5|Briefly described|p280 Fig. 2, p288-289.|Late Pliocene|Early Pliocene|Strandlines: basal, shelly offshore marine marls underlie sparsely fossiliferous shoreface sands. Underlies Nyerimilang Formation; overlies Tambo River Formation. Age: 4.5-3.1Ma foraminifera; 3.5-2.5Ma Sr isotope. Geol. Prov: onshore Gippsland Basin.||||||11-JAN-06
8906|Jemmys Point Formation|61302|5|Briefly described|p12, p11 Fig.4|Early Pliocene|Miocene|Of the Seapray Group. Consists of marls and marly limestone overlain by shoreline beach sands, marls and claystone. Geological Province: Gippsland Basin.||||||
8906|Jemmys Point Formation|61336|5|Briefly described|p(iv) Fig. 4|Recent|Pliocene|Of the Sale Group. Geological Province: Gippsland Basin. See also p(v) Fig. 5.||||||07-FEB-11
8906|Jemmys Point Formation|62899|5|Briefly described|p37 Fig. 2|||Geological province: Lakes Entrance Platform.||||||12-DEC-06
8906|Jemmys Point Formation|63217|6|Mentioned|p102 Fig.6.|||Gippsland Basin.||||Unconformably overlies Tambo River Formation.||
8906|Jemmys Point Formation|63739|5|Briefly described|p37 Fig. 2|||Geological province: Gippsland Basin.||||||01-JUL-08
8906|Jemmys Point Formation|65717|6|Mentioned|p12|Pliocene|Miocene|Part of unnamed marine sequence (p12)||||||
8906|Jemmys Point Formation|67061|6|Mentioned|p554 Fig.10.|Pliocene|Pliocene|Gippsland Basin, onshore.||||||
8906|Jemmys Point Formation|70076|5|Briefly described|Regional: Fig.3|Pliocene|Pliocene|||Seaspray Group.||Overlies Tambo River Formation. Is overlain by Coongulmerang Formation.||
8906|Jemmys Point Formation|73289|6|Mentioned|p765 Fig.2|Recent|Pliocene|||||Overlies Tambo River Formation and Bairnsdale Limestone Formation. Unconformably overlies Yallourn Formation.||
8906|Jemmys Point Formation|73488|6|Mentioned|p634 Fig.4|||||||||
8906|Jemmys Point Formation|73562|5|Briefly described|p303-304|Pleistocene|Pliocene|Gippsland Basin; onshore. Appears as Jemmy's Point Formation on p304.||||Lateral equivalent to Haunted Hills Formation.|Sandy marl, calcareous sandstone and shell beds.|
8926|Jerilderie Formation|22773|5|Briefly described|Fig24.5p350|Middle Triassic|Middle Triassic|||||||
8926|Jerilderie Formation|22857|5|Briefly described|p277, p540 App.1 Tb.A1.10|Middle Triassic|Middle Triassic|Conglomerate, sandstone, mudstone. Max. thickness: 220m. Geological Province: Oaklands Basin, Tasman Epicratonic Province. See also p350 Fig. 24.5. ||||||
8926|Jerilderie Formation|22860|5|Briefly described|p277||Middle Triassic|||||||
8926|Jerilderie Formation|22887|5|Briefly described|Fig.5 p12|Middle Triassic|Middle Triassic|||||||
8926|Jerilderie Formation|22893|6|Mentioned|fig4 p9|||||||||
8926|Jerilderie Formation|35498|2|Defined|p145|Triassic|Triassic|||||||
8926|Jerilderie Formation|35503|6|Mentioned|p202|||Defined in Standing Committee Coalfield Geology NSW (1978)||||||
8926|Jerilderie Formation|38293|4|Described|p22|||||||||
8926|Jerilderie Formation|40520|6|Mentioned|Fig.5|||||||||
8926|Jerilderie Formation|42966|3|Fully described|p64|||||||||
8926|Jerilderie Formation|43841|4|Described|8||Triassic|Unconformably overlies Coorabin Coal Measures||||||
8926|Jerilderie Formation|44093|5|Briefly described|p245 App. 1|Middle Triassic|Middle Triassic|||||||
8926|Jerilderie Formation|49038|6|Mentioned|p23|||||||||
8926|Jerilderie Formation|49040|6|Mentioned|p8|||||||||
8926|Jerilderie Formation|61314|5|Briefly described|p129|Middle Triassic|Early Triassic|Fluvial sandstone, conglomerate and mudstone. Overlies the Coorabin Coal Measures. Geological Province: Oaklands Basin, Murray Basin.||||||
8926|Jerilderie Formation|69798|5|Briefly described|p4, p9, p11, p13-16|Triassic|Triassic|Oaklands Basin. Seismic profiles. Very low-amplitude high-frequency reflections.||||Disconformably overlies Coorabin Coal Measures.||
8926|Jerilderie Formation|70125|5|Briefly described|p391, p396-397|Middle Triassic|Middle Triassic|Oaklands Basin. 220m of dominantly fluvial sand deposits.|242 Ma.|||Overlies Coorabin Coal Measures. Coeval with Hawkesbury Sandstone (same palynozone).||
34917|Jim and Jack Tonalite|22968|5|Briefly described|P217|Early Devonian|Late Silurian|New name, type locality location given on P217||||||
34917|Jim and Jack Tonalite|23029|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
34917|Jim and Jack Tonalite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
34917|Jim and Jack Tonalite|23309|6|Mentioned|p434 App1|||G548 I-Type.||||||
34917|Jim and Jack Tonalite|61161|5|Briefly described|p99-101, p76-77 Fig 6.1|Early Devonian|Early Devonian|Two phases: coarse-grained, equigranular, highly magnetic biotite tonalite grading into quartz diorite with I-type character; and, fine to medium-grained, equigranular, nonmagnetic tonalite. Intruded Omeo Metamorphic Complex. GSV map code: G548.||||||
34917|Jim and Jack Tonalite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite tonalite and minor leucogranite: grey; equigranular; weakly to moderately foliated; magnetic phase: I-type; non-magnetic phase: S-type; leucogranitic porphyry and aplite dykes: I- and S-type intrusions. GSV map code: G548.||||||
34917|Jim and Jack Tonalite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite tonalite and minor leucogranite: grey; equigranular; weakly to moderately foliated; magnetic phase: I-type; non-magnetic phase: S-type; leucogranitic porphyry and aplite dykes: I- and S-type intrusions. GSV map code: G548.||||||07-FEB-11
34917|Jim and Jack Tonalite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite tonalite and minor leucogranite: grey; equigranular; weakly to moderately foliated; magnetic phase: I-type; non-magnetic phase: S-type; leucogranitic porphyry and aplite dykes: I- and S-type intrusions. GSV map code: G548.||||||
34917|Jim and Jack Tonalite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite tonalite and minor leucogranite: grey; equigranular; weakly to moderately foliated; magnetic phase: I-type; non-magnetic phase: S-type; leucogranitic porphyry and aplite dykes: I- and S-type intrusions. GSV map code: G548.||||||
34917|Jim and Jack Tonalite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite tonalite and minor leucogranite: low to moderate gravity response; nonmagnetic and highly magnetic; low to moderate K and U, moderate to high Th and total radioelements. GSV map code: G548.||||||
34917|Jim and Jack Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian|Intruded by leucogranitic porphyry and aplite dykes.|||||Biotite tonalite and minor leucogranite: grey; equigranular; weakly to moderately foliated; magnetic phase coarse-grained with fine to medium-grained microgranitoid enclaves; non-magnetic phase medium-grained; I-type. |
8980|Jindera Granite|30906|6|Mentioned|Map legend|Devonian|Devonian|||||||
8980|Jindera Granite|30909|6|Mentioned|Map legend|Early Devonian|Early Devonian|Prob.Lower Devonian||||||
8980|Jindera Granite|33553|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
8980|Jindera Granite|37029|6|Mentioned|p48|||||||||
8980|Jindera Granite|40328|4|Described|p207|||||||||
8980|Jindera Granite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
8980|Jindera Granite|40498|6|Mentioned|p376|||||||||
8980|Jindera Granite|42726|5|Briefly described|map legend|Silurian||||||||
8980|Jindera Granite|43344|14|Not recorded|p132|||||||||
8980|Jindera Granite|44340|14|Not recorded|p.9,Table.1,p.5|||||||||
8980|Jindera Granite|44341|14|Not recorded|map legend||Devonian|||||||
8980|Jindera Granite|69801|5|Briefly described|p2, p4-p5, p116-120, p137|Devonian|Devonian|Central Lachlan Orogen. Occurs north of Albury. Sole occupant of the Jindera Suite. Classified by Chappell et al (1991) as an I-type felsic fractionated pluton of Silurian age and the sole member of the Jindera Suite. Chappell et al (1999) noted that this unit features significant geochemical variation and is likely mapped as a composite body. Sample locality, sample description, petrography, SHRIMP analyses and interpretation are detailed.|403.4 +/- 2.5 Ma (SHRIMP)|Jindera Suite|||Medium- to coarse-grained, seriate-textured biotite granite.|
8980|Jindera Granite|70777|5|Briefly described|p2, p64, p81|Emsian|Emsian|Lachlan Orogen.|403.4 +/- 2.5 Ma (Bodorkos et al., 2015)|||||
8980|Jindera Granite|71206|6|Mentioned|p384|||Lachlan Fold Belt.||||||
8980|Jindera Granite|72528|5|Briefly described|p1, p49, p109.|Emsian|Emsian|Name assigned in company reports to granite dated herein as Mount Royal Granite from Hickory Hill. Date given for Jindera Granite is from Bodorkos et al (2015), from 40km to S. Geochemical variation in the Jindera Granite as described by Chappell (1999) indicate the Jindera Granite is most likely a composite of multiple intrusions, which has been supported by recent mapping.|403+/-2.5 Ma U-Pb SHRIMP||||A composite I-type biotite granite.|
31594|Jindera Suite|42726|5|Briefly described|map legend||Silurian|||||||
31594|Jindera Suite|44093|5|Briefly described|p170 App. 1|Late Silurian|Silurian|Max Age: Middle Silurian. In the Wagga-Omeo Zone. Geological Province: Lachlan Fold Belt.||||||
31594|Jindera Suite|69801|6|Mentioned|p116|||Central Lachlan Orogen.|||Includes the Jindera Granite.|||
31594|Jindera Suite|72528|5|Briefly described|p49.|Emsian|Emsian|Affiliated with the Mount Royal Granite.|403.4+/-2.6 Ma||Includes Mount Royal Granite, Jindera Granite.|||
37749|Jingellic Tonalite|23309|5|Briefly described|p434, Appendix 1|Ordovician|Ordovician|G97, I-Type. Age: 460+/-4Ma.||||||
37749|Jingellic Tonalite|24133|3|Fully described|p55|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
37749|Jingellic Tonalite|24142|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
37749|Jingellic Tonalite|24143|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
37749|Jingellic Tonalite|24144|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
37749|Jingellic Tonalite|24145|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt||||||
37749|Jingellic Tonalite|24146|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
37749|Jingellic Tonalite|68116|5|Briefly described|Appendix, Map 20.|Middle Ordovician|Middle Ordovician||||||Hornblende tonalite: medium to dark grey, medium grained; equigranular; foliated; S-type; nonmagnetic; occurs as small pods within Corryong Granite.|
69424|Jirnkee Granite|61161|5|Briefly described|p98-99, p76-77 Fig 6.1, |Early Devonian|Early Devonian|Nonmagnetic, pale grey to cream, homogeneous, coarse-grained, massive leucogranite; qtz, plag (albite), microcline perthite, musc, zircon; basin-like topography. Intrudes Pinnak Sandstone. Age: inferred Early Devonian or younger. GSV map code: G461.||||||
69424|Jirnkee Granite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Muscovite leucogranite: coarse-grained; pale grey; homogeneous; consists of perthitic microcline, quartz, plagioclase, muscovite; S-type intrusion. GSV map code: G461.||||||
69424|Jirnkee Granite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Muscovite leucogranite: coarse-grained; pale grey; homogeneous; consists of perthitic microcline, quartz, plagioclase, muscovite; S-type intrusion. GSV map code: G461.||||||07-FEB-11
69424|Jirnkee Granite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Muscovite leucogranite: coarse-grained; pale grey; homogeneous; consists of perthitic microcline, quartz, plagioclase, muscovite; S-type intrusion. GSV map code: G461.||||||
69424|Jirnkee Granite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Muscovite leucogranite: coarse-grained; pale grey; homogeneous; consists of perthitic microcline, quartz, plagioclase, muscovite; S-type intrusion. GSV map code: G461.||||||
69424|Jirnkee Granite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Muscovite leucogranite: no gravity data; nonmagnetic (k < 1 x10^-6 cgs); moderate to high K, low Th, moderate U, low to moderate total radioelements. GSV map code: G461.||||||
69424|Jirnkee Granite|68116|5|Briefly described|Appendix, Map 35.|Devonian|Silurian||||||Muscovite leucogranite: coarse-grained; pale grey; homogeneous; consists of perthitic microcline, quartz, plagioclase, muscovite.|
9003|Johanna River Sand|23010|6|Mentioned|p333-341|||||||||
9003|Johanna River Sand|24551|6|Mentioned|p305, 630|Middle Eocene|Middle Eocene|||||||
9003|Johanna River Sand|30185|6|Mentioned|p108|||Refers Taylor(1965)||||||
9003|Johanna River Sand|30576|5|Briefly described|Table 2|||||||||
9003|Johanna River Sand|30578|6|Mentioned|p9|||||||||
9003|Johanna River Sand|31245|4|Described|p81|||See also P82, 83||||||
9003|Johanna River Sand|31922|6|Mentioned|p166|||||||||
9003|Johanna River Sand|33155|5|Briefly described|p119|||||||||
9003|Johanna River Sand|33319|6|Mentioned|p167|||Fauna||||||
9003|Johanna River Sand|33412|6|Mentioned|p224|||M.Palaeocene||||||
9003|Johanna River Sand|35066|3|Fully described|p224|||||||||
9003|Johanna River Sand|38070|6|Mentioned|Fig.12|||Otway Basin||||||
9003|Johanna River Sand|38903|6|Mentioned|p2|||||||||
9003|Johanna River Sand|39923|6|Mentioned|p354|||||||||
9003|Johanna River Sand|40429|6|Mentioned|Fig.2|||||||||
9003|Johanna River Sand|41043|6|Mentioned|p95|||||||||
9003|Johanna River Sand|42318|5|Briefly described|p7|||||||||
9003|Johanna River Sand|42827|3|Fully described|p298|||see also Fig 8.12||||||
9003|Johanna River Sand|43590|6|Mentioned|p15|||Mapped in Dilwyn Formation||||||
9003|Johanna River Sand|43675|6|Mentioned|p334|||||||||
9003|Johanna River Sand|47054|5|Briefly described|Fig.3 P481|||||||||
9003|Johanna River Sand|48911|6|Mentioned|Chart 1|||||||||
9003|Johanna River Sand|61155|5|Briefly described|p18|Middle Eocene|Early Paleocene|Overlies Rotten Point Sand; underlies Browns Creek Clay. Age: 65.5-46.5Ma. Thickness: 40m. Geological Province: Aire Embayment.||||||
9003|Johanna River Sand|61182|5|Briefly described|p19|||Of Wangerrip Group. Isolated outcrop mapped as part of Dilwyn Formation together with Rotten Point Sand. Geological Province: Otway Basin. Lower part is coeval with Pebble Point Formation. ||||||
9010|Johnson Hill Sandstone|32074|6|Mentioned|Table 1|||Section. See also p180||||||31-MAR-17
9010|Johnson Hill Sandstone|33601|6|Mentioned|p28|||||||||
9010|Johnson Hill Sandstone|43547|14|Not recorded|Table p153||Emsian|||||||
30558|Johnson Mudstone|23309|4|Described|p112. Tb 2.40|||Of the Timbarra Subgroup.  Maximum Thickness: ~500m.||||||22-FEB-10
30558|Johnson Mudstone|23615|3|Fully described|p23, p89|Early Devonian|Early Devonian|Of Timbarra Subgroup.  Supersedes Johnson Member and Mount Johnson Member.  Characterised by turbiditic mudstone and sandstone.  Age: 410-395Ma.||||||
30558|Johnson Mudstone|24551|4|Described|p142|||Of the Timbarra Subgroup.||||||
30558|Johnson Mudstone|43206|5|Briefly described|map legend||Ludlow|Timbarra Subgroup||||||
30558|Johnson Mudstone|43312|5|Briefly described|Map Legend||Early Devonian|of Timbarra Subgroup||||||
30558|Johnson Mudstone|43313|5|Briefly described|Map Legend||Early Devonian|of Timbarra Subgroup.||||||
30558|Johnson Mudstone|60542|4|Described|p51, p13|Early Devonian|Early Devonian|Formerly Johnson Member, Mount Johnson Member, Johnson Mudstone Formation. Overlies Windarra Fm, and Fluke Knob Ignimbrite; overlain by Davidsons Lane Fm, and Stonehenge Ignimbrite. Max.thickness: ~500m.||||||19-DEC-07
30558|Johnson Mudstone|68116|5|Briefly described|Appendix, Maps 36, 45.|Pragian|Lochkovian||||||Volcanigenic mudstone, sandstone, conglomerate, pumiceous vitric sandstone: includes various styles of Bouma sequences; basalt lava; marine turbidites with rare lava pods.|
9014|Jolimont Clay|24551|5|Briefly described|p338 Fig. 11.2, 350|Middle Pleistocene|Middle Pleistocene|||||||
9014|Jolimont Clay|29982|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
9014|Jolimont Clay|35011|4|Described|p313|||||||||
9014|Jolimont Clay|41848|5|Briefly described|p389|||||||||
9014|Jolimont Clay|42827|4|Described|p391|||of Yarra Delta Group||||||
9014|Jolimont Clay|71277|5|Briefly described|p301-305|Quaternary|Quaternary|Kenley (1967). Restricted to the area north of the present Yarra River, between Spencer Street and Punt Road.||Yarra Delta Group.||Overlies the Burnley Basalt.|Red, orange, yellow or grey mottled stiff clay with minor sand and silt.|
9028|Jordan River Group|22628|6|Mentioned|fig1p108|Silurian|Silurian|||||||
9028|Jordan River Group|22708|5|Briefly described|p210|Late Ordovician|Late Ordovician|||||||
9028|Jordan River Group|22885|5|Briefly described|map|Early Devonian|Early Devonian|||||||
9028|Jordan River Group|22971|4|Described|p 18|Devonian|Devonian|Mudstone and fine-grained quartzose sandstone. Overlain by Walhalla Group. Thickness: ~300m.?||||||19-JAN-06
9028|Jordan River Group|23229|5|Briefly described|p25, 31-3|||||||||
9028|Jordan River Group|23307|5|Briefly described|Map Legend|Devonian|Silurian|||||||
9028|Jordan River Group|23309|4|Described|p87, 141-146, 148. Tb 2.53/2.54|Devonian|Silurian|||||||
9028|Jordan River Group|24177|5|Briefly described|p59|Devonian|Silurian|Includes the Wilson Creek Shale which is Devonian in age.||||||
9028|Jordan River Group|24328|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes Wilson Creek Shale.||||||
9028|Jordan River Group|24329|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes Wilson Creek Shale.||||||22-DEC-08
9028|Jordan River Group|24551|5|Briefly described|p88 Fig. 3.15|Silurian|Silurian|Of the Murrindindi Supergroup.||||||
9028|Jordan River Group|24576|5|Briefly described|p727|Early Devonian|Silurian|Overlies the Mount Easton Shale. Geological Province: Lachlan Fold Belt.||||||22-DEC-08
9028|Jordan River Group|24588|5|Briefly described|p12 Fig.3|Early Devonian|Early Silurian|Geological Province: Mount Easton Province.||||||29-NOV-13
9028|Jordan River Group|30906|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
9028|Jordan River Group|33601|2|Defined|p4|Early Devonian|Early Silurian|Early Silurian - Early Devonian.||||||22-DEC-08
9028|Jordan River Group|33602|6|Mentioned|Fig.2|||||||||
9028|Jordan River Group|33604|6|Mentioned|p17|||Silurian to L.Dev. Correlation chart.||||||
9028|Jordan River Group|33607|6|Mentioned|Map legend|Devonian|Silurian|Silurian-Devonian||||||
9028|Jordan River Group|34843|6|Mentioned|p6|||||||||
9028|Jordan River Group|35073|6|Mentioned|p6|||||||||
9028|Jordan River Group|37727|4|Described|p65|||||||||
9028|Jordan River Group|38070|6|Mentioned|Fig.8|||P96||||||
9028|Jordan River Group|40126|6|Mentioned|p14|||||||||
9028|Jordan River Group|41585|5|Briefly described|p112|||Mention p118 and Fig.4.1||||||21-OCT-22
9028|Jordan River Group|42827|4|Described|p112|||||||||
9028|Jordan River Group|44187|5|Briefly described|Map Legend||Early Silurian|||||||
9028|Jordan River Group|44197|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
9028|Jordan River Group|61185|4|Described|p34, p37|Devonian|Silurian|Includes McAdam Sst, Bullung Sltst, Sinclair Valley Sst, Whitelaw Sltst, Boola Fm, Coopers Creek Lst, Eildon Sst and Wilson Creek Shale. Only Wilson Creek Shale (youngest unit) is represented on NAGAMBIE. Geol.Prov: Mount Easton Province, Melbourne Zone.||||||07-FEB-11
9028|Jordan River Group|61187|5|Briefly described|p5 Fig.3, p50.|Silurian|Silurian|Melbourne Zone, Melbourne Terrane.|||||Marine siltstone and sandstone.|
9028|Jordan River Group|61329|5|Briefly described|p121|Middle Devonian|Ordovician|Geological Province: Gippsland Basin.||||||12-FEB-08
9028|Jordan River Group|64535|5|Briefly described|Map legend|Early Devonian|Silurian|Contains 12 named units, mainly siltstone formations; and sandstone, limestone and shale.||||||
9028|Jordan River Group|64536|5|Briefly described|Map legend|Early Devonian|Silurian|Contains 10 named units, mainly siltstone formations; and sandstone, limestone and shale.||||||07-FEB-11
9028|Jordan River Group|64537|5|Briefly described|Map legend|Early Devonian|Silurian|Contains 10 named units, mainly siltstone formations; and sandstone, limestone and shale.||||||07-FEB-11
9028|Jordan River Group|64538|5|Briefly described|Map legend|Early Devonian|Silurian|Contains 10 named units, mainly siltstone formations; and sandstone, limestone and shale.||||||07-FEB-11
9028|Jordan River Group|64539|5|Briefly described|Map legend|Early Devonian|Silurian|Contains 12 named units, mainly siltstone formations; and sandstone, limestone and shale.||||||
9028|Jordan River Group|64540|5|Briefly described|Map legend|Early Devonian|Silurian|Contains 12 named units, mainly siltstone formations; and sandstone, limestone and shale.||||||
9028|Jordan River Group|64605|5|Briefly described|Map legend|Early Devonian|Silurian|Comprises 12 named formations of sandstone, siltstone, and some limestone. All components are nonmagnetic.||||||17-NOV-08
9028|Jordan River Group|64606|5|Briefly described|Map Legend|Early Devonian|Ordovician|Incl: Wilson Ck Shale, Eildon Sst., Whitelaw Sitlst., Sinclair Valley Sst., Murderers Hill Siltst., Snake-Edwards Sst. Mbr., Bullung Siltst., McAdam Sst., Serpenitine Ck Sst., Donnellys Ck Siltst., Cherrytree Gap Sst. Mbr., Lazarini Siltst.||||||22-DEC-08
9028|Jordan River Group|64616|2|Defined|p73, p144, p147, p156 Fig.6.5, p158-161 |Early Devonian|Silurian|See also p163-164, p166, p175, p179-181, p184-185, p190-191, p200 Fig.7.1, p202-204, p207, p250, p281, p283-284, p287-288, p290, p293, p304-306. Of Murrindindi Supergroup. 13 constituents: Coopers Creek Limestone; Wilson Creek Shale; Wurutwun, Boola Formations; Eildon, Sinclair Valley, McAdam, Serpentine Creek Sandstones; Whitelaw, Bullung, Donnelly Creek, Murderers Hill, Lazarini Siltstones. Sandstones generally less lithic,shelly fossils rare and bioturbation common in siltstones, when compared with overlying Walhalla Group. Overlies Mount Easton Shale; is overlain by Walhalla Group. Mis-spelled as Jordon on p207.||||||
9028|Jordan River Group|65900|5|Briefly described|p156 Fig. 2, p158, 161, p167|Early Devonian|Silurian|Melbourne Zone.||Of Murrindindi Supergroup.|||Dominated by siltstone, with thin sandstone formations.|10-MAY-12
9028|Jordan River Group|67804|5|Briefly described|p64|Early Devonian|Early Devonian|||||Intruded by Woods Point dyke swarm. Is conformably overlain by Cathedral Group.|Folded marine siliciclastic sediments.|
9028|Jordan River Group|67847|5|Briefly described|p44 fig 3.2.2.|||See also reference to the misspelt Jordon River Group (p44 fig 3.2.2.)||||||
9028|Jordan River Group|68116|5|Briefly described|Maps 18, 25-26, 34, 43, 52, 56.|Devonian|Silurian|Also occurs in the Appendix.|||||Siltstone, shale, sandstone, rare conglomerate and limestone; sandstone typically quartz-rich, siltstone commonly bioturbated; marine.|
9028|Jordan River Group|70742|5|Briefly described|p163|Early Devonian|Early Devonian|Cerberean Cauldron, S of Lake Eildon.||Murrindindi Supergroup.|Wilson Creek Shale.|Is overlain by Walhalla Group.||
9028|Jordan River Group|73497|5|Briefly described|Map legend|Devonian|Devonian||||Wilson Creek Shale|||
69417|Junction Plain Tonalite|61161|5|Briefly described|p93, p76-77 Fig. 6.1|Early Devonian|Early Devonian|Of Rileys Creek Suite. Small pluton; nonmagnetic, medium-grained, dark grey-green speckled appearance; quartz, plagioclase, chocolate-brown biotite, hornblende, and accessory zircon, allanite and apatite. I-type. Type locality p93. GSV map code: G464.||||||
69417|Junction Plain Tonalite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Hornblende-biotite tonalite: medium-grained, with magmatic foliation; contains quartz, plagioclase (some with calcic cores), biotite, hornblende; I-type intrusion. GSV map code: G464.||||||
69417|Junction Plain Tonalite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Hornblende-biotite tonalite: medium-grained, with magmatic foliation; contains quartz, plagioclase (some with calcic cores), biotite, hornblende; I-type intrusion. GSV map code: G464.||||||07-FEB-11
69417|Junction Plain Tonalite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Hornblende-biotite tonalite: medium-grained, with magmatic foliation; contains quartz, plagioclase (some with calcic cores), biotite, hornblende; I-type intrusion. GSV map code: G464.||||||
69417|Junction Plain Tonalite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Hornblende-biotite tonalite: medium-grained, with magmatic foliation; contains quartz, plagioclase (some with calcic cores), biotite, hornblende; I-type intrusion. GSV map code: G464.||||||
69417|Junction Plain Tonalite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Hornblende-biotite tonalite: no gravity data; nonmagnetic to weakly magnetic (10 nT, k = 5 to 15 x10^-6 cgs); moderate to high K, high Th and total radioelements, low to moderate U. GSV map code: G464.||||||
69417|Junction Plain Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Silurian||||||Hornblende-biotite tonalite: medium-grained, with magmatic foliation; contains quartz, plagioclase (somewith calcic cores), biotite, hornblende.|
23676|Jungle Creek Granodiorite|22876|4|Described|p25|||Currawong Suite||||||
23676|Jungle Creek Granodiorite|22877|5|Briefly described|map|Silurian|Silurian|Currowong Suite. G51. Biotite granodiorite. I-Type.||||||26-OCT-04
23676|Jungle Creek Granodiorite|23309|5|Briefly described| p350|||G51 I-Type||||||
23676|Jungle Creek Granodiorite|24551|6|Mentioned|p235, 729 Table 8.12|||||||||
23676|Jungle Creek Granodiorite|41850|6|Mentioned|p431|||||||||
23676|Jungle Creek Granodiorite|42627|5|Briefly described|Map legend|Wenlock||||||||
23676|Jungle Creek Granodiorite|42647|4|Described|p41|||||||||
23676|Jungle Creek Granodiorite|42827|5|Briefly described|p431|||||||||
23676|Jungle Creek Granodiorite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Biotite granodiorite: coarse grained, pale to greenish grey; I-type.|
31498|Jungle Creek Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Currowong Supersuite.  Includes the Jungle Creek Granite (informal name).||||||09-FEB-05
41185|Kadnook Creek Granodiorite|50154|2|Defined|p36, p87, p247 App.5|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex.||||||09-SEP-04
41185|Kadnook Creek Granodiorite|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite granodiorite||||||20-MAY-13
41185|Kadnook Creek Granodiorite|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite granodiorite||||||20-MAY-13
41185|Kadnook Creek Granodiorite|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite granodiorite||||||20-MAY-13
41185|Kadnook Creek Granodiorite|50159|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite granodiorite||||||20-MAY-13
41185|Kadnook Creek Granodiorite|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Overlain by Eumeralla Formation. Biotite-muscovite granodiorite.||||||20-AUG-04
41185|Kadnook Creek Granodiorite|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite granodiorite||||||20-MAY-13
41185|Kadnook Creek Granodiorite|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite granodiorite||||||20-MAY-13
41185|Kadnook Creek Granodiorite|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite granodiorite||||||20-MAY-13
41185|Kadnook Creek Granodiorite|50164|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Biotite-muscovite granodiorite.||||||
41185|Kadnook Creek Granodiorite|66002|6|Mentioned|p9 Tb.5|||G449. Defined by Morand et al. 2003.||||||
41185|Kadnook Creek Granodiorite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Biotite-muscovite granodiorite: massive, medium grained; accessory magnetite; strongly weathered; magnetic.|
37564|Kaerwut Tonalite|23309|5|Briefly described|p345|||G516, I-type.  Supersedes Kaermut Trondhjemite.||||||
37564|Kaerwut Tonalite|23938|5|Briefly described|p70 Tb. 6|Early Devonian|Early Devonian|I-type. See also Kaerwut Trondhjemite. See also p71 Fig. 25, p100.||||||
37564|Kaerwut Tonalite|24551|6|Mentioned|p439|||||||||
37564|Kaerwut Tonalite|68116|5|Briefly described|Appendix, Map 45.|Wenlock|Wenlock||||||Biotite tonalite: medium-grained equigranular with porphyritic marginal phase; I-type.|
9126|Kalimnan beds|32686|6|Mentioned|p235|||Fauna collection||||||
37565|Kalingur Tonalite|23309|5|Briefly described|p47, 336, Table 2.14|Cambrian|Cambrian|G441, I-type. Age: 504+/-8Ma.||||||
37565|Kalingur Tonalite|50154|5|Briefly described|p24|Cambrian|Cambrian|Age: 504 +/- 8 Ma (U/Pb).||||||
9144|Kalkallo Formation|33020|6|Mentioned|p241|||Potential energy of source area||||||
27441|Kalorama Rhyodacite|23268|6|Mentioned|Fig14-2.1p388||Devonian|||||||
27441|Kalorama Rhyodacite|23269|4|Described|p402, 404-6, Fig14-3.3p405||Late Devonian|||||||
27441|Kalorama Rhyodacite|23309|5|Briefly described|p167, 166. Tb 2.62|||||||||
27441|Kalorama Rhyodacite|24551|5|Briefly described|p162|Devonian|Devonian|Part of the Dandenong Ranges Igneous Complex.||||||
27441|Kalorama Rhyodacite|29652|6|Mentioned|Table 4|||||||||
27441|Kalorama Rhyodacite|29653|6|Mentioned|p4|||||||||
27441|Kalorama Rhyodacite|33157|4|Described|p42|||||||||
27441|Kalorama Rhyodacite|33598|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27441|Kalorama Rhyodacite|33599|4|Described|p8|||Dev.||||||
27441|Kalorama Rhyodacite|34956|6|Mentioned|p82|||||||||
27441|Kalorama Rhyodacite|35012|6|Mentioned|p430|||||||||
27441|Kalorama Rhyodacite|35277|4|Described|p93|||||||||
27441|Kalorama Rhyodacite|39291|6|Mentioned|Fig.13|||||||||
27441|Kalorama Rhyodacite|41641|4|Described|p163|||||||||
27441|Kalorama Rhyodacite|42827|4|Described|p163|||of Mount Dandenong Volcanics||||||
27441|Kalorama Rhyodacite|44197|5|Briefly described|Map Legend||Late Devonian|||||||
27441|Kalorama Rhyodacite|60083|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Mount Dandenong Volcanics Group.  Rhyodacite, porphyritic.||||||
27441|Kalorama Rhyodacite|68116|5|Briefly described|Appendix, Map 42.|Late Devonian|Late Devonian|Lacustrine.|||||Garnet-bearing rhyodacite ignimbrite, recrystallized; siltstone, lenticular, under recrystallised dark vitric-rich ignimbrite with phenocrysts of quartz, feldspar, occasional almandine garnet, under a thin band of volcanigenic lacustrine sediments.|
30434|Kalymna Falls Sandstone|23309|5|Briefly described|p205, 78|||Maximum Thickness: 450m.  Of the Red Man Bluff Subgroup.||||||
30434|Kalymna Falls Sandstone|44929|5|Briefly described|Map Legend|Silurian|Ordovician|Of Red Man Bluff Sub-Group. Reddish yellow sandstone, quartzose to quartzo-feldspathic, fine- to medium-grained.||||||14-JUN-06
30434|Kalymna Falls Sandstone|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Man Bluff Sub-Group (Grampians Group). Quartz sandstone, reddish-yellow, quartzose to quartzo-feldspathic, fine- to medium-grained sandstone with occasional pebbly lag horizons of sub-rounded vein quartz.||||||13-JUN-06
30434|Kalymna Falls Sandstone|44932|5|Briefly described|Map Legend|Silurian|Ordovician|Of Red Man Bluff Sub-Group. Reddish yellow sandstone, quartzose to quartzo-feldspathic, fine- to medium-grained.||||||14-JUN-06
30434|Kalymna Falls Sandstone|44933|5|Briefly described|Map Legend|Silurian|Ordovician|Of Red Man Bluff Sub-Group. Reddish yellow sandstone, quartzose to quartzo-feldspathic, fine- to medium-grained.||||||14-JUN-06
30434|Kalymna Falls Sandstone|60451|4|Described|p76, 80|Early Devonian|Ordovician|Of the Red Man Bluff Subgroup (Grampians Group). Type section in text. Maximum thickness: ~450m. Fine to medium grained laminated sandstone and siltstone.||||||02-MAY-13
30434|Kalymna Falls Sandstone|60456|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Man Bluff Sub-Group. Sandstone: reddish yellow, quartzose to quartzo-feldspathic; fine to medium grained sandstone with occasionally pebbly lag horizons of subrounded vein quartz.||||||30-SEP-04
30434|Kalymna Falls Sandstone|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Mans Bluff Subgroup. Sandstone; reddish yellow, quartzose to quartzo-feldspathic; fine to medium grained sandstone with occasionally pebbly lag horizons of subrounded vein quartz.||||||
30434|Kalymna Falls Sandstone|61183|4|Described|p30 Tb. 2, p39-40, p82|||Of Red Man Bluff Subgroup (Grampians Gp). Mostly thin to medium bedded, fine- to medium-grained quartz sandstone; abundant thin interbeds of laminated micaceous siltstone. Overlies Murray Hill Sst; underlies Major Mitchell Sst. Thickness: ~450m.||||||
30434|Kalymna Falls Sandstone|64541|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Red Man Bluff Sub-group. Sandstone: reddish-yellow, quartzose to quartzo-feldspathic; fine to medium grained sandstone with occasional pebbly lag horizons of sub-rounded vein quartz.||||||07-FEB-11
30434|Kalymna Falls Sandstone|64610|5|Briefly described|Map legend|Ordovician|Ordovician|Of Red Man Bluff Subgroup (Grampians Gp). Sandstone: reddish-yellow, quartzose to quartzo-feldspathic, fine- to med.gr. sst, with occasional pebbly lag horizons of sub-rounded vein quartz; laminated, x-laminated+x-trough-laminated. med-thickly bedded, etc||||||11-NOV-08
30434|Kalymna Falls Sandstone|65313|6|Mentioned|p581 Fig. 9,p582 Fig. 10|Llandovery|Llandovery|Grampians National Park sections. Age from adjacent units.||Of Red Man Bluff Subgroup.||Overlies Murray Hill Sandstone and is overlain by Major Mitchell Sandstone.||26-MAR-12
30434|Kalymna Falls Sandstone|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Red Man Bluff Subgroup. Defined by Cayley & Taylor, 1997.||||||
30434|Kalymna Falls Sandstone|68116|5|Briefly described|Appendix, Maps 22, 30.|Ludlow|Late Ordovician|Abundant thin beds of laminated purple siltstone occur in the south.|||||Sandstone: reddish yellow, quartzose to quartzo-feldspathic; fine to medium-grained with occasional pebble lags of subrounded vein quartz; variably laminated; medium to thick-bedded; coarser in the north.|
9185|Kameruka Suite|22778|5|Briefly described|p 161|||||||||
9185|Kameruka Suite|22815|6|Mentioned|p69|||||||||
9185|Kameruka Suite|24517|6|Mentioned|p48|||Informal name. Of the Bega Batholith. Name used interchangeably with Kameruka pluton.||||||25-MAY-05
9185|Kameruka Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
9185|Kameruka Suite|42827|5|Briefly described|p430|||of Kameruka Supersuite||||||
9185|Kameruka Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
9187|Kameruka Supersuite|22878|5|Briefly described|p83|||||||||
9187|Kameruka Supersuite|22879|5|Briefly described|map|Early Devonian|Early Devonian|||||||
9187|Kameruka Supersuite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Yambula Granodiorite||||||01-OCT-04
9187|Kameruka Supersuite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||06-OCT-04
9187|Kameruka Supersuite|23309|5|Briefly described|p339|||G5, G7, G8, G9, G10, G31, G521||||||
9187|Kameruka Supersuite|24551|5|Briefly described|p235|||Consists of: Wallagaraugh Suite, Betka Suite.||||||
9187|Kameruka Supersuite|42726|5|Briefly described|map legend||Early Devonian|||||||
9187|Kameruka Supersuite|42827|5|Briefly described|p430|||||||||
9187|Kameruka Supersuite|68592|6|Mentioned|p24|Early Devonian|Early Devonian|||||||
9187|Kameruka Supersuite|69801|5|Briefly described|p3, p129, p138|Devonian|Devonian|Eastern Lachlan Orogen.|||Includes the Wallagaraugh Suite, Pericoe Monzogranite and the Yambulla Granodiorite.|||
9187|Kameruka Supersuite|72528|5|Briefly described|p108.|Emsian|Emsian|Age from dating of Mount Poole Monzogranite.|||Includes Mount Poole Monzogranite.|||
9214|Kangaroo Gully Volcanic Breccia|24177|4|Described|p68, p17 Tb.1|Jurassic|Jurassic|Overlies the Castlemaine Group.||||||
9214|Kangaroo Gully Volcanic Breccia|24328|5|Briefly described|Map legend|Jurassic|Jurassic|||||||
9214|Kangaroo Gully Volcanic Breccia|24329|5|Briefly described|Map legend|Jurassic|Jurassic|||||||
9214|Kangaroo Gully Volcanic Breccia|24440|5|Briefly described|Map legend|||||||||
9214|Kangaroo Gully Volcanic Breccia|42682|4|Described|p20|||Name appears only in heading. Vic convenor advises that it is intended as a formal name.||||||
9214|Kangaroo Gully Volcanic Breccia|42683|5|Briefly described|map legend|||||||||
9214|Kangaroo Gully Volcanic Breccia|43261|5|Briefly described|Map Legend||Jurassic|||||||
9214|Kangaroo Gully Volcanic Breccia|43493|4|Described|9-67||Jurassic|See p28 for unit description.||||||04-FEB-15
9214|Kangaroo Gully Volcanic Breccia|65715|5|Briefly described|p9 Tb.6|Mesozoic|Mesozoic|Formation rank. Map symbol implies probable Jurassic age. Defined in Cherry and Wilkinson (1994) p28.||||||
9229|Kangerong Formation|23274|5|Briefly described|p445, 458|||||||||
9229|Kangerong Formation|24551|5|Briefly described|p99 Fig. 4.4|Early Ordovician|Early Ordovician|Of the Castlemaine Group||||||
9229|Kangerong Formation|31508|6|Mentioned|p20|||L. Ordovician||||||
9229|Kangerong Formation|31510|6|Mentioned|Table 1|||See also P6.||||||
9229|Kangerong Formation|35290|6|Mentioned|p19|||||||||
9229|Kangerong Formation|41570|4|Described|p87|||||||||
9229|Kangerong Formation|42827|6|Mentioned|p87|||||||||
28634|Kanmantoo Group|7992|6|Mentioned|165|Ordovician|Cambrian|||||||
28634|Kanmantoo Group|9124|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|12781|6|Mentioned|p386|Paleozoic|Paleozoic|Basement to Otway Basin.||||Is overlain unconformably by Casterton Formation.||
28634|Kanmantoo Group|22458|5|Briefly described|p523||Cambrian|||||||
28634|Kanmantoo Group|22492|5|Briefly described|31|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|22531|6|Mentioned|p2|||||||||
28634|Kanmantoo Group|22573|4|Described|p 47, Fig 1||Cambrian|Minimum thickness: >8km.||||||04-MAY-10
28634|Kanmantoo Group|22580|6|Mentioned|p89|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|22581|5|Briefly described|Fig.2,p37||Cambrian|In the Kanmantoo Basin.||||||17-JAN-07
28634|Kanmantoo Group|22603|5|Briefly described|p99||Early Cambrian|Age: 540 Ma (?)||||||17-JAN-07
28634|Kanmantoo Group|22628|6|Mentioned|p109,p112|||||||||
28634|Kanmantoo Group|22634|5|Briefly described|p506|Cambrian|Neoproterozoic|||||||
28634|Kanmantoo Group|22643|4|Described|p186, fig3,6,7|Early Cambrian|Early Cambrian|||||||
28634|Kanmantoo Group|22671|5|Briefly described|p848-49|||Overlies Heatherdale Shale. Geological Province: Kanmantoo Fold Belt.||||||18-JAN-06
28634|Kanmantoo Group|22708|6|Mentioned|p207|||||||||
28634|Kanmantoo Group|22719|6|Mentioned|p487|||||||||
28634|Kanmantoo Group|22726|6|Mentioned|p233,235||Early Cambrian|||||||
28634|Kanmantoo Group|22755|4|Described|p547, Fig.1 p548||Early Cambrian|In the Stansbury Basin. See also p548.||||||17-JAN-07
28634|Kanmantoo Group|22766|4|Described|Fig.2 p561, p562|Early Cambrian|Early Cambrian|||||||
28634|Kanmantoo Group|22772|5|Briefly described|Table 13.1|Middle Cambrian|Early Cambrian|||||||
28634|Kanmantoo Group|22840|5|Briefly described|P37||Cambrian|||||||
28634|Kanmantoo Group|22848|5|Briefly described|36|||||||||
28634|Kanmantoo Group|22857|5|Briefly described|Tb 13.1 (insert p70-71), p75, p94, p96|Middle Cambrian|Early Cambrian|Of the Moralana Supergroup. Correlate with Teltawongee beds. Max. thickness: 9km. Geological Province: Kanmantoo Trough. See also p99 and p405 App.1 Tb.A1.4.||||||04-MAY-10
28634|Kanmantoo Group|22858|6|Mentioned|p75,Fig14.8p96,96||Early Cambrian|Max Age: 526 (+/-) 6 Ma.||||||
28634|Kanmantoo Group|22869|6|Mentioned|P40|||||||||
28634|Kanmantoo Group|22875|6|Mentioned|p25|||||||||
28634|Kanmantoo Group|22933|6|Mentioned|p10|||||||||
28634|Kanmantoo Group|22938|6|Mentioned|p235||Cambrian|||||||
28634|Kanmantoo Group|22944|5|Briefly described|Fig3|Tithonian||||||||
28634|Kanmantoo Group|22945|5|Briefly described|p8|Cambrian|Cambrian|Mentioned under - Area C geology.||||||
28634|Kanmantoo Group|22951|6|Mentioned|p55|||||||||
28634|Kanmantoo Group|23019|6|Mentioned|p617|||||||||
28634|Kanmantoo Group|23022|6|Mentioned|p1803|||||||||
28634|Kanmantoo Group|23023|6|Mentioned|p1797,1799-1800|||||||||
28634|Kanmantoo Group|23226|6|Mentioned|p895|||Transgressive to Mannum Formation.||||||
28634|Kanmantoo Group|23309|5|Briefly described|p19, 26, 40, 46, 195.|||||||||
28634|Kanmantoo Group|23317|5|Briefly described|377|Early Cambrian|Early Cambrian|Includes clastic turbidites. Geological Province: Adelaide Fold Belt.||||||04-MAY-10
28634|Kanmantoo Group|23319|5|Briefly described|p407|Early Cambrian|Early Cambrian|||||||07-FEB-07
28634|Kanmantoo Group|23539|4|Described|p 466- 467|||||||||
28634|Kanmantoo Group|23564|6|Mentioned|p1444|||||||||
28634|Kanmantoo Group|23731|6|Mentioned|p43|||||||||
28634|Kanmantoo Group|23818|4|Described|p51 Fig.16, p99|Cambrian|Cambrian|Underlain by Barossa Complex, Adelaidean Group and Hawker Group (unconformable). Max. thickness: 60 000 ft.||||||17-JAN-07
28634|Kanmantoo Group|23824|5|Briefly described|p100 Fig 2|Early Devonian|Cambrian|Geological Province: Great Australian Bight Basin.||||||
28634|Kanmantoo Group|23827|5|Briefly described|p260|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|23854|5|Briefly described|p863|Middle Cambrian|Early Cambrian|||||||
28634|Kanmantoo Group|23869|5|Briefly described|p15 Fig. 3|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|23932|5|Briefly described|p667|Early Cambrian|Early Cambrian|Geological Province: Adelaide Fold Belt.||||||
28634|Kanmantoo Group|23981|5|Briefly described|p8-9 Fig. 4|Early Cambrian|Early Cambrian|Thick sequence of siliciclastics. Disconformably overlies Normanville group. Thickness>8000m. Geological Province: Stansbury Basin (Fleurieu Peninsula).||||||12-FEB-07
28634|Kanmantoo Group|23991|5|Briefly described|p188 Fig.1|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|23996|5|Briefly described|p352 Fig.1|Cambrian|Cambrian|Geological Province: Adelaid Fold Belt.||||||07-MAR-05
28634|Kanmantoo Group|24102|5|Briefly described|p131, p132 Fig.2|Cambrian|Cambrian|Age: ~520 Ma.||||||30-NOV-04
28634|Kanmantoo Group|24263|4|Described|p1384||Cambrian|Geological Province: Wonominta Block.||||||17-JAN-07
28634|Kanmantoo Group|24314|5|Briefly described|p61 Fig.2||Paleozoic|Geological Province: Otway Basin.||||||07-NOV-08
28634|Kanmantoo Group|24361|6|Mentioned|p50|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|24362|6|Mentioned|p42|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|24381|6|Mentioned|p58|||||||||
28634|Kanmantoo Group|24425|6|Mentioned|p16|||Fractured rock aquifer.||||||
28634|Kanmantoo Group|24465|4|Described|p343|Middle Cambrian|Early Cambrian|Overlies Normanville Group.  Geological Province: Stansbury Basin.||||||19-JAN-05
28634|Kanmantoo Group|24509|5|Briefly described|p39, p41 Fig. 2b|Cambrian|Cambrian|Metasedimentary rock. Interbedded with Teal Flat Volcanics.||||||
28634|Kanmantoo Group|24551|5|Briefly described|p74|Cambrian|Cambrian|Of the Moralana Supergroup in SA.||||||
28634|Kanmantoo Group|24566|5|Briefly described|p110, p111|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|24599|5|Briefly described|p494|||Geological Province: Adelaide Fold Belt.||||||
28634|Kanmantoo Group|24604|5|Briefly described|p907 Fig. 4|Cambrian|Cambrian|Group is Gp in text.||||||
28634|Kanmantoo Group|29395|6|Mentioned|p1|||||||||
28634|Kanmantoo Group|29406|6|Mentioned|p51|||||||||
28634|Kanmantoo Group|29474|6|Mentioned|p7|||[Originally entered for NT. CEBMar95]||||||
28634|Kanmantoo Group|29591|6|Mentioned|p103|||||||||
28634|Kanmantoo Group|29665|6|Mentioned|p77|||||||||
28634|Kanmantoo Group|29697|6|Mentioned|p7|||||||||
28634|Kanmantoo Group|29836|4|Described|p89|||||||||
28634|Kanmantoo Group|29872|6|Mentioned|p77|||||||||
28634|Kanmantoo Group|30051|6|Mentioned|Fig.1|||Middle Cambrian age.||||||
28634|Kanmantoo Group|30052|5|Briefly described|p91|||Middle Cambrian age.||||||
28634|Kanmantoo Group|30085|6|Mentioned|p132|||Geological Plan on P132. Cambrian age.||||||
28634|Kanmantoo Group|30329|6|Mentioned|p30|||On table P30||||||
28634|Kanmantoo Group|30377|4|Described|p203|||See also p204-207.||||||17-JAN-07
28634|Kanmantoo Group|30378|6|Mentioned|p431|||Lower Cambrian age.||||||
28634|Kanmantoo Group|30379|5|Briefly described|p90|||Cambrian age||||||
28634|Kanmantoo Group|30380|6|Mentioned|Table 1|||Correlation||||||
28634|Kanmantoo Group|30381|4|Described|p213|||See also p214-251.||||||17-JAN-07
28634|Kanmantoo Group|30382|6|Mentioned|p388|||||||||
28634|Kanmantoo Group|30398|5|Briefly described|p259|||||||||
28634|Kanmantoo Group|30753|6|Mentioned|Table 2|||Lower Permian age||||||
28634|Kanmantoo Group|30754|6|Mentioned|p12|||Stratigraphic table||||||
28634|Kanmantoo Group|30758|5|Briefly described|p65|||Schist as source of aggregate P66. Favourable foundation conditions P70||||||
28634|Kanmantoo Group|30783|5|Briefly described|p12|||Sediments discussed||||||
28634|Kanmantoo Group|30801|6|Mentioned|p5|||Table P5-6||||||
28634|Kanmantoo Group|30805|6|Mentioned|p4|||||||||
28634|Kanmantoo Group|30807|6|Mentioned|p102|||Suggested map symbol||||||
28634|Kanmantoo Group|31292|6|Mentioned|p1|||Cambrian||||||
28634|Kanmantoo Group|31314|6|Mentioned|p102|||||||||
28634|Kanmantoo Group|31321|5|Briefly described|p15|||See also P16. Map. Mineral deposits||||||
28634|Kanmantoo Group|31322|6|Mentioned|p23|||M. Cambrian. Stratigraphy||||||
28634|Kanmantoo Group|31577|5|Briefly described|p76|||Cambrian||||||
28634|Kanmantoo Group|31851|6|Mentioned|Fig. 2|||||||||
28634|Kanmantoo Group|31923|6|Mentioned|p11|||||||||
28634|Kanmantoo Group|31999|6|Mentioned|p127|||||||||
28634|Kanmantoo Group|32146|6|Mentioned|p369|||||||||
28634|Kanmantoo Group|32161|6|Mentioned|p55|||Basement||||||
28634|Kanmantoo Group|32194|6|Mentioned|p311|||||||||
28634|Kanmantoo Group|32196|4|Described|p149|||||||||
28634|Kanmantoo Group|32321|6|Mentioned|p82|||||||||
28634|Kanmantoo Group|32323|5|Briefly described|p9|||Petrology||||||
28634|Kanmantoo Group|32401|6|Mentioned|p103|||||||||
28634|Kanmantoo Group|32404|6|Mentioned|p18|||||||||
28634|Kanmantoo Group|32432|6|Mentioned|Fig.2|||See also Table 1||||||
28634|Kanmantoo Group|32433|6|Mentioned|p80|||See also Table 2||||||
28634|Kanmantoo Group|32439|6|Mentioned|p99|||||||||
28634|Kanmantoo Group|32457|6|Mentioned|p88|||||||||
28634|Kanmantoo Group|32547|4|Described|p60|||L.-M. Camb.||||||
28634|Kanmantoo Group|32791|6|Mentioned|p11|||||||||
28634|Kanmantoo Group|33224|6|Mentioned|p48|||Photo Fig.35||||||
28634|Kanmantoo Group|33236|6|Mentioned|p24|||L. - M.Camb.||||||
28634|Kanmantoo Group|33311|6|Mentioned|p50|||||||||
28634|Kanmantoo Group|33332|3|Fully described|p11|||Lower Cambrian. See also Figs. 3 and 4.||||||05-MAR-08
28634|Kanmantoo Group|33468|6|Mentioned|p217|||||||||
28634|Kanmantoo Group|33471|4|Described|p555|||||||||
28634|Kanmantoo Group|33472|6|Mentioned|p470|||||||||
28634|Kanmantoo Group|33474|6|Mentioned|Fig.1|||||||||
28634|Kanmantoo Group|33488|6|Mentioned|p8|||||||||
28634|Kanmantoo Group|33490|4|Described|p10|||Cambrian?||||||
28634|Kanmantoo Group|33625|6|Mentioned|p198|||||||||
28634|Kanmantoo Group|33634|6|Mentioned|p561|||||||||
28634|Kanmantoo Group|33798|6|Mentioned|p98|||||||||
28634|Kanmantoo Group|33834|5|Briefly described|p7|||||||||
28634|Kanmantoo Group|33936|6|Mentioned|Fig.1a|||||||||
28634|Kanmantoo Group|33998|6|Mentioned|p25|||Cambrian||||||
28634|Kanmantoo Group|34029|5|Briefly described|Table 1|||?Cambrian||||||
28634|Kanmantoo Group|34185|6|Mentioned|p129|||||||||
28634|Kanmantoo Group|34195|6|Mentioned|p1|||Cambrian ?||||||
28634|Kanmantoo Group|34248|5|Briefly described|p113|||Palaeozoic||||||
28634|Kanmantoo Group|34265|6|Mentioned|p242|||Camb.||||||
28634|Kanmantoo Group|34287|6|Mentioned|p59|||||||||
28634|Kanmantoo Group|34296|4|Described|p97|||||||||
28634|Kanmantoo Group|34308|6|Mentioned|p181|||||||||
28634|Kanmantoo Group|34497|6|Mentioned|p60|||Cambrian. See P61||||||
28634|Kanmantoo Group|34535|6|Mentioned|Fig.16|||Camb.||||||
28634|Kanmantoo Group|34536|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|Lower to Middle Cambrian||||||
28634|Kanmantoo Group|34598|6|Mentioned|p20|||Cambrian||||||
28634|Kanmantoo Group|34612|3|Fully described|p102|||See also Fig.32.||||||05-MAR-08
28634|Kanmantoo Group|34617|6|Mentioned|p2|||||||||
28634|Kanmantoo Group|34719|6|Mentioned|p374|||||||||
28634|Kanmantoo Group|34760|6|Mentioned|Fig.1|||||||||
28634|Kanmantoo Group|34812|6|Mentioned|Table 9|||||||||
28634|Kanmantoo Group|34933|6|Mentioned|p60|||||||||
28634|Kanmantoo Group|34941|6|Mentioned|p234|||||||||
28634|Kanmantoo Group|35027|6|Mentioned|p385|||||||||
28634|Kanmantoo Group|35089|4|Described|p203|||Discussed throughout.||||||
28634|Kanmantoo Group|35092|6|Mentioned|p108|||||||||
28634|Kanmantoo Group|35099|6|Mentioned|p332|||||||||
28634|Kanmantoo Group|35175|6|Mentioned|p1166|||||||||
28634|Kanmantoo Group|35200|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
28634|Kanmantoo Group|35232|6|Mentioned|p5|||See also Table.1||||||
28634|Kanmantoo Group|35255|6|Mentioned|Fig.8|||||||||
28634|Kanmantoo Group|35358|5|Briefly described|p8|||||||||
28634|Kanmantoo Group|35565|6|Mentioned|p15|||Geochemistry program||||||
28634|Kanmantoo Group|35744|6|Mentioned|p3|||||||||
28634|Kanmantoo Group|36198|6|Mentioned|p280|||||||||
28634|Kanmantoo Group|36534|6|Mentioned|p221|||||||||
28634|Kanmantoo Group|36731|4|Described|p125|||||||||
28634|Kanmantoo Group|36816|5|Briefly described|Table 1|||See also Fig.2||||||
28634|Kanmantoo Group|36833|6|Mentioned|p21|||||||||
28634|Kanmantoo Group|36836|6|Mentioned|p39|||||||||
28634|Kanmantoo Group|37132|6|Mentioned|p368|||||||||
28634|Kanmantoo Group|37264|6|Mentioned|p91|||||||||
28634|Kanmantoo Group|37461|6|Mentioned|p346|||||||||
28634|Kanmantoo Group|37501|6|Mentioned|p416|||||||||
28634|Kanmantoo Group|37873|6|Mentioned|p1|||||||||
28634|Kanmantoo Group|38004|6|Mentioned|Table 1|||||||||
28634|Kanmantoo Group|38008|6|Mentioned|p3|||||||||
28634|Kanmantoo Group|38068|5|Briefly described|p69|||See also Fig.4.||||||
28634|Kanmantoo Group|38290|4|Described|p20|||||||||
28634|Kanmantoo Group|38660|6|Mentioned|p89|||||||||
28634|Kanmantoo Group|38699|6|Mentioned|p16|||||||||
28634|Kanmantoo Group|38703|6|Mentioned|p131|||||||||
28634|Kanmantoo Group|38704|6|Mentioned|p133|||||||||
28634|Kanmantoo Group|38873|4|Described|Table 2|||||||||
28634|Kanmantoo Group|38927|4|Described|p45|||||||||
28634|Kanmantoo Group|38932|5|Briefly described|p97|||||||||
28634|Kanmantoo Group|39132|6|Mentioned|p189|||||||||
28634|Kanmantoo Group|39331|6|Mentioned|Fig.0-3|||||||||
28634|Kanmantoo Group|39344|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|39350|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|39352|6|Mentioned|Map legend|Late Cambrian|Early Cambrian|Early to Late Cambrian||||||
28634|Kanmantoo Group|39489|6|Mentioned|Fig.1|||||||||
28634|Kanmantoo Group|39524|6|Mentioned|Fig.1|||||||||
28634|Kanmantoo Group|39806|6|Mentioned|p207|||||||||
28634|Kanmantoo Group|39842|6|Mentioned|p5|||||||||
28634|Kanmantoo Group|39880|6|Mentioned|p352|||||||||
28634|Kanmantoo Group|39885|6|Mentioned|p434|||||||||
28634|Kanmantoo Group|39909|6|Mentioned|p5|||||||||
28634|Kanmantoo Group|40003|6|Mentioned|p40|||||||||
28634|Kanmantoo Group|40196|4|Described|p1826|||||||||
28634|Kanmantoo Group|40228|6|Mentioned|p38|||||||||
28634|Kanmantoo Group|40442|4|Described|p16|||||||||
28634|Kanmantoo Group|40454|4|Described|p43|||||||||
28634|Kanmantoo Group|40455|5|Briefly described|p67|||||||||
28634|Kanmantoo Group|40500|6|Mentioned|p139|||||||||
28634|Kanmantoo Group|40501|6|Mentioned|p118|||||||||
28634|Kanmantoo Group|40503|4|Described|p107|||||||||
28634|Kanmantoo Group|40695|6|Mentioned|p3|||||||||
28634|Kanmantoo Group|40761|6|Mentioned|p215|||||||||
28634|Kanmantoo Group|40763|4|Described|p206|||||||||
28634|Kanmantoo Group|40852|6|Mentioned|p32|||||||||
28634|Kanmantoo Group|40856|5|Briefly described|p312|||||||||
28634|Kanmantoo Group|41103|6|Mentioned|p261|||||||||
28634|Kanmantoo Group|41253|5|Briefly described|p57|||||||||
28634|Kanmantoo Group|41400|6|Mentioned|p26|||||||||
28634|Kanmantoo Group|41401|6|Mentioned|p32|||||||||
28634|Kanmantoo Group|41478|5|Briefly described|Table 1|||||||||
28634|Kanmantoo Group|41494|6|Mentioned|p31|||||||||
28634|Kanmantoo Group|41526|6|Mentioned|p10|||||||||
28634|Kanmantoo Group|41570|6|Mentioned|p102|||||||||
28634|Kanmantoo Group|41572|6|Mentioned|p5|||||||||
28634|Kanmantoo Group|41594|5|Briefly described|p48|||||||||
28634|Kanmantoo Group|41853|6|Mentioned|Fig.1|||[Originally entered for NT. CEBMar95]||||||
28634|Kanmantoo Group|41947|5|Briefly described|p16|||||||||
28634|Kanmantoo Group|42115|6|Mentioned|p6|||||||||
28634|Kanmantoo Group|42119|5|Briefly described|p523|||||||||
28634|Kanmantoo Group|42129|6|Mentioned|Table 1 P253|||||||||
28634|Kanmantoo Group|42138|6|Mentioned|p388|||||||||
28634|Kanmantoo Group|42154|5|Briefly described|p336|||||||||
28634|Kanmantoo Group|42167|6|Mentioned|Fig.2 P115|||||||||
28634|Kanmantoo Group|42192|6|Mentioned|p4|||||||||
28634|Kanmantoo Group|42222|5|Briefly described|p11|||||||||
28634|Kanmantoo Group|42225|6|Mentioned|Fig.4 P224|||||||||
28634|Kanmantoo Group|42232|6|Mentioned|Fig.1 P269|||||||||
28634|Kanmantoo Group|42242|6|Mentioned|p200|||||||||
28634|Kanmantoo Group|42243|4|Described|p211|||||||||
28634|Kanmantoo Group|42245|6|Mentioned|p37|||[Originally entered for NT. CEBMar95]||||||
28634|Kanmantoo Group|42246|6|Mentioned|p10|||||||||
28634|Kanmantoo Group|42266|5|Briefly described|p291|||||||||
28634|Kanmantoo Group|42268|5|Briefly described|p327|||||||||
28634|Kanmantoo Group|42270|4|Described|p353|||||||||
28634|Kanmantoo Group|42271|6|Mentioned|p369|||||||||
28634|Kanmantoo Group|42272|6|Mentioned|p398|||||||||
28634|Kanmantoo Group|42273|5|Briefly described|p422|||||||||
28634|Kanmantoo Group|42275|6|Mentioned|p465|||||||||
28634|Kanmantoo Group|42276|5|Briefly described|p482|||||||||
28634|Kanmantoo Group|42357|5|Briefly described|p10|||||||||
28634|Kanmantoo Group|42439|6|Mentioned|p351|||||||||
28634|Kanmantoo Group|42487|5|Briefly described|p122|||||||||
28634|Kanmantoo Group|42488|5|Briefly described|Fig.1C P186|||||||||
28634|Kanmantoo Group|42499|5|Briefly described|Map legend|Cambrian||||||||
28634|Kanmantoo Group|42505|5|Briefly described|Map legend|Cambrian||||||||
28634|Kanmantoo Group|42599|5|Briefly described|Fig.3 P614|||||||||
28634|Kanmantoo Group|42601|6|Mentioned|Fig.2 p15|||||||||
28634|Kanmantoo Group|42717|5|Briefly described|map legend|Cambrian||||||||
28634|Kanmantoo Group|42761|5|Briefly described|Fig.1 P6|||||||||
28634|Kanmantoo Group|42788|5|Briefly described|p139, p147|||||||||
28634|Kanmantoo Group|42884|5|Briefly described|p10|||see also Fig.1 p11.||||||17-JAN-07
28634|Kanmantoo Group|42903|5|Briefly described|p424|||see also Fig.1 p423.||||||17-JAN-07
28634|Kanmantoo Group|42966|5|Briefly described|p407|||||||||
28634|Kanmantoo Group|42982|6|Mentioned|Table 1,p333|||||||||
28634|Kanmantoo Group|43027|6|Mentioned|p599|||||||||
28634|Kanmantoo Group|43052|5|Briefly described|p105|||||||||
28634|Kanmantoo Group|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Marine metasandstone, phyllite, schist, gneiss, minor calcsilicate and marble; pyritic metasiltstone.||||||25-MAY-05
28634|Kanmantoo Group|43073|5|Briefly described|Table 1|||||||||
28634|Kanmantoo Group|43190|5|Briefly described|Fig.1,p28.||Cambrian|see also Fig.2,p29.Age early to ?middle Cambrian.||||||
28634|Kanmantoo Group|43192|6|Mentioned|p58||Cambrian|||||||
28634|Kanmantoo Group|43193|6|Mentioned|p71,78.|||||||||
28634|Kanmantoo Group|43195|5|Briefly described|Map Legend||Cambrian|||||||
28634|Kanmantoo Group|43200|6|Mentioned|p4|||||||||
28634|Kanmantoo Group|43218|4|Described|Fig.3,p22||Cambrian|||||||
28634|Kanmantoo Group|43258|5|Briefly described|Map Legend||Cambrian|||||||
28634|Kanmantoo Group|43298|5|Briefly described|Map Legend||Cambrian|||||||
28634|Kanmantoo Group|43560|6|Mentioned|p234||Cambrian|||||||
28634|Kanmantoo Group|43595|6|Mentioned|p545||Cambrian|||||||
28634|Kanmantoo Group|43627|6|Mentioned|p7|||||||||28-OCT-04
28634|Kanmantoo Group|43660|6|Mentioned|Fig.6,p15||Cambrian|||||||
28634|Kanmantoo Group|43686|5|Briefly described|p235||Cambrian|||||||
28634|Kanmantoo Group|43703|4|Described|p75|||||||||
28634|Kanmantoo Group|43759|4|Described|p445|Middle Cambrian|Early Cambrian|||||||
28634|Kanmantoo Group|43800|5|Briefly described|p169-170|||||||||
28634|Kanmantoo Group|43814|6|Mentioned|Fig.3,p115|||||||||
28634|Kanmantoo Group|44093|6|Mentioned|p47, p108|||Age: Cambrian? Geological Provinve: Kanmantoo Fold Belt.||||||
28634|Kanmantoo Group|44133|5|Briefly described|p6, 14, 17|Cambrian|Cambrian|Metasediments and volcanics.||||||
28634|Kanmantoo Group|44191|6|Mentioned|Map Legend|Middle Cambrian|Early Cambrian|||||||
28634|Kanmantoo Group|48911|6|Mentioned|p7|||Cambrian. Lithology||||||
28634|Kanmantoo Group|48977|6|Mentioned|p19|||Underlies Duntroon Embayment. Under Otway Basin P24. See P56||||||
28634|Kanmantoo Group|49040|6|Mentioned|Plate 1|||||||||
28634|Kanmantoo Group|49060|6|Mentioned|p67|||||||||
28634|Kanmantoo Group|50154|5|Briefly described|p22, p65|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Overlies Normanville Group. Age: 500-600 Ma (detrital zircons). Includes the Karinya Shale. See also the Kanmantoo group.||||||25-AUG-04
28634|Kanmantoo Group|60544|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|60567|5|Briefly described|p37, p39|||Undifferentiated greywackes of the group now classified as Teal Flat and Marne River Volcanics.||||||
28634|Kanmantoo Group|60712|5|Briefly described|p27, p30 Fig. 3|Early Cambrian|Early Cambrian|Thick succession of metamorphosed mudstone and lithic sandstone. Overlies Normanville Group.  Geological Province: Kanmantoo Trough (Adelaide Geosyncline).  See also p28 Fig. 1.||||||
28634|Kanmantoo Group|60889|6|Mentioned|p249|||Correlation with Billy Creek Formation (Arrowie Basin) and alternative views are presented in text (p249). Stansbury Basin.|||||Clastic dominated, rapidly deposited.|
28634|Kanmantoo Group|60904|5|Briefly described|p803, p804 24a|Early Cambrian|Early Cambrian|Age: ca.532-526Ma.  Of the Lachlan Orogen.||||||17-JAN-07
28634|Kanmantoo Group|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Marine metasandstone, phyllite, schist, gneiss, minor calcsilicate and marble.||||||
28634|Kanmantoo Group|60958|6|Mentioned|Map Legend|Cambrian|Cambrian|Erratics of this unit in Cape Jervis Formation.||||||
28634|Kanmantoo Group|61046|5|Briefly described|p7|Early Cambrian|Early Cambrian|Includes Tapanappa Formation.||||||
28634|Kanmantoo Group|61108|5|Briefly described|map legend|Cambrian|Cambrian|Marine metasandstone, phyllite, schist, gneiss, minor calcsilicate rock and marble.||||||
28634|Kanmantoo Group|61180|6|Mentioned|p5|||In South Australia.||||||
28634|Kanmantoo Group|61182|6|Mentioned|p49|||Includes metamorphics.||||||
28634|Kanmantoo Group|61307|5|Briefly described|p6 Fig. 3, p7|Middle Cambrian|Early Cambrian|This group has a complex history of stratigraphic nomenclature (details on p7). Geological Province: Adelaide Fold Belt. See also p3-4 Figs. 1 and 2.||||||
28634|Kanmantoo Group|61314|5|Briefly described|p128|Cambrian|Cambrian|Metamorphosed deep water clastic sediments that underlie the Murray Basin. Consist of phyllite, slate and metagreywacke. ||||||
28634|Kanmantoo Group|61411|6|Mentioned|p4 Fig.1.||Cambrian|||||||
28634|Kanmantoo Group|61412|6|Mentioned|p4 Fig.1. ||Cambrian|||||||
28634|Kanmantoo Group|61547|6|Mentioned|p461 Fig.2.|Paleozoic|Paleozoic|Equivalent units underlie the Jurassic and younger rocks of the Penola Trough, Otway Basin.||||||
28634|Kanmantoo Group|61622|6|Mentioned|p436, p440, p436 Fig. 2|Paleozoic|Paleozoic|Geological Province: Otway Basin.||||||07-FEB-11
28634|Kanmantoo Group|61726|5|Briefly described|p925||Early Cambrian|Includes turbidities. Geological Province: Adelaide Fold Belt.||||||
28634|Kanmantoo Group|61752|6|Mentioned|p5|||||||||07-FEB-11
28634|Kanmantoo Group|61762|6|Mentioned|p17|Cambrian|Cambrian|||||||
28634|Kanmantoo Group|61838|5|Briefly described|p221|Cambrian|Cambrian|Includes the Nairne Pyrite Member.||||||
28634|Kanmantoo Group|62742|5|Briefly described|p699 Fig. 2|Early Cambrian|Early Cambrian|||||||
28634|Kanmantoo Group|62744|5|Briefly described|p709 Fig. 2|Early Cambrian|Early Cambrian|||||||
28634|Kanmantoo Group|63020|5|Briefly described|p972 Fig. 1b, p973|Early Cambrian|Early Cambrian|See also p974 Fig. 2. ||||||
28634|Kanmantoo Group|63122|5|Briefly described|p16, p17 Fig. 4.3|Cambrian|Cambrian|Geological Province: Otway Basin. Metasediments and volcanics.||||||
28634|Kanmantoo Group|63124|6|Mentioned|p49, p77|Cambrian|Cambrian|Geological Province: Otway Basin. Mentioned only in terms of equivalents in Figure 5.1.||||||
28634|Kanmantoo Group|63431|5|Briefly described|p677 Fig. 2|Paleozoic|Paleozoic|mentioned in terms of equivalents only.||||||07-FEB-11
28634|Kanmantoo Group|63433|6|Mentioned|p768, p769|||In South Australia. ||||||
28634|Kanmantoo Group|63562|6|Mentioned|p353 Fig.11.||||||Includes Balquhidder Formation.|||
28634|Kanmantoo Group|63599|6|Mentioned|p986|||Geological Province: Adelaide Fold Belt.||||||10-DEC-07
28634|Kanmantoo Group|63793|6|Mentioned|p22.|||Eastern Mount Lofty Ranges. Equivalent to Teltawongee beds in NSW.||||||
28634|Kanmantoo Group|63848|5|Briefly described|p531, p532, p534 Fig.4, p538.|||About 8 km thick, yet deposited within about 12 million years. Fossils are rare, but include trace fossils of Helminthoidichnites and Psammichnites gigas.|||Includes Carrickalinga Head, Talisker, Tapanappa and Tunkalilla  Formations. |||
28634|Kanmantoo Group|64233|5|Briefly described|p22 Fig. 2|Cambrian|Cambrian|Part of a sediments and metasediments group.||||||
28634|Kanmantoo Group|64281|5|Briefly described|p28|Cambrian|Cambrian|Geological Province: Stansbury Basin - where the basinal sequence is locally folded against the Gawler Craton, and against Kangaroo Island Group rocks. . Deep marine terrigenous sediments.||||||23-DEC-09
28634|Kanmantoo Group|64282|6|Mentioned|Map legend|Cambrian|Cambrian|Mentioned in the context of forming pebbles, boulders and residual erratics within the diamictite section of Cape Jervis Formation.||||||
28634|Kanmantoo Group|64334|6|Mentioned|p46|Cambrian|Cambrian|"SE South Australia. Marks the first appearance of the ""Gondwana pattern"" of Late Cambrian to Middle Ordovician zircon age spectrum. Probability density plots."|||||Predominantly turbiditic.|
28634|Kanmantoo Group|64571|6|Mentioned|p835, p836|Early Cambrian|Early Cambrian|Thickness: ~8000m.||||||15-DEC-08
28634|Kanmantoo Group|64647|5|Briefly described|p38, p38 Fig. 1, p39, p44|Cambrian|Cambrian|Overlies Burra Group. Intruded by Rathjen Gneiss. Marnie sediments.||||||
28634|Kanmantoo Group|64705|5|Briefly described|p80 Fig. 7e (photo)|Cambrian|Cambrian|Age: ~520Ma. Metamorphics.||||||04-DEC-08
28634|Kanmantoo Group|64746|6|Mentioned|p394. |||Contains detrital zircons aged 950-900 Ma.|||Includes Carrickalinga Head Formation.|||
28634|Kanmantoo Group|65375|5|Briefly described|p33.|Cambrian|Cambrian||||Includes Carrickalinga Head, Backstairs Passage, Tapanappa, Tunkalilla, Balquhidder and Petrel Cove Formations; Talisker Calc-siltstone; Middleton Sandstone.|Overlies Normanville Group.||
28634|Kanmantoo Group|65376|6|Mentioned|p92 Fig. 2.82. |Cambrian|Cambrian|||||||
28634|Kanmantoo Group|65624|5|Briefly described|map legend|Ordovician|Cambrian|Quartzites, argillaceous schistose quartzites and schistose slates; coarse glaciofluvial conglomerate bands at Penneshaw; ubiquitous slump bedding of Kangaroo Island||||||12-JAN-10
28634|Kanmantoo Group|65664|3|Fully described|pp1095-1108|Early Cambrian|Early Cambrian|Age constrained between underlying Heatherdale Shale and magmatism. 7-8 km thick. Probably laterally equivalent with the Glenelg River Complex.|522 +/- 2 Ma to 514 +/- 3 Ma.||Includes Keynes and Bollaparudda Subgroups.|Overlies Heatherdale Shale (Normanville Group).||09-MAY-12
28634|Kanmantoo Group|65686|5|Briefly described|p408||Cambrian|Stansbury Basin. Includes trilobites.||||Overlies the Heatherdale Shale unconformably.||07-MAY-12
28634|Kanmantoo Group|65892|5|Briefly described|p9 Fig.4, p10, p16, p19.|Middle Cambrian|Early Cambrian|Fleurieu Peninsula. Largely unfossiliferous. Total thickness about 10 km includes two successions separated by an unconformity.|||Includes Carrickalinga Head, Backstairs Passage, Talisker, Tapanappa, Tunkalilla, Balquhidder and Petrel Cove Formations; and Middleton Sandstone.|Overlies Normanton Group.|Two successions of turbidites passing upwards into shallow-water sandstones.|
28634|Kanmantoo Group|65921|5|Briefly described|p1, p2 (map legend).|Cambrian|Cambrian|Deposited in outer shelf, continental slope, and ocean basin environments. Intense deformation and metamorphism, complex fold patterns and melting and granite inclusions are observable. Occurs as inclusions in the Cape Willoughby Granite.|||Carrickalinga Head Formation, Backstairs Passage Formation, Talisker Calcsiltstone, Tapanappa Formation, Tunkalilla Formation, Balquhidder Formation, Petrel Cove Formation, Middleton Sandstone.||Silts and sandstones.|10-JAN-17
28634|Kanmantoo Group|66623|6|Mentioned|p425.|||Correlated in age and facies with Teltawongee Group, Koonenberry Belt.|||Includes basal Carrickalinga Head Formation.|||
28634|Kanmantoo Group|66761|5|Briefly described|p245 Fig.2, p254|Cambrian|Cambrian|Fleurieu Peninsula. Correlated with Minlaton Formation, Yorke Peninsula, and Kangaroo Island Group, in part.||||||
28634|Kanmantoo Group|67103|6|Mentioned|p612, 614-615, 621|||Deposition of these sediments was likely syn-orogenic. The source of zircons in the Rathjen Gneiss. Detrital zircon age spectra.||||||
28634|Kanmantoo Group|67104|6|Mentioned|p629|||||||||
28634|Kanmantoo Group|67536|5|Briefly described|Map Legend|||Kanmantoo Province; basement to Murray Basin.||||Intercalated with Teal Flat Volcanics, Marne River Volcanics, and/or Truro Volcanics|Metasandstone, phyllite, schist, gneiss.|
28634|Kanmantoo Group|68314|5|Briefly described|p749-750, p754-755, p757|Early Cambrian|Early Cambrian|Major influx of foreland siliciclastic detritus in the Delamerian Orogen from c.526 Ma. Similar detrital compositions and depositional characteristics to Leviathan Formation. Has an inferred mid- to late-Early Cambrian age.|||||Quartz-rich turbidites.|
28634|Kanmantoo Group|68315|6|Mentioned|p772-773|Middle Cambrian|Middle Cambrian|Crops out in the southern Delamerian Orogen.||||||
28634|Kanmantoo Group|68731|6|Mentioned|p216, p217|||||||||
28634|Kanmantoo Group|68735|5|Briefly described|p231, p233, p233 Fig.2, p235 Fig.3, p239|Middle Cambrian|Early Cambrian|Stansbury Basin. > 8 km thick. Deposited predominantly below wave base as turbidites, with some shallow water facies. The base of this Group correlates with the bases of both the Billy Creek and Minlaton formations.|||Includes Middleton Sandstone; Petrel Cove, Balquhidder. Tunkalilla, Tapanappa, Talisker, Backstairs Passage, and Carrickalinga Head Formations. |||10-APR-17
28634|Kanmantoo Group|68822|6|Mentioned|p324, p331, p333|Stage 5||Intruded by ca 506 to 490 Ma syntectonic granites.||||||
28634|Kanmantoo Group|68993|5|Briefly described|p544 Fig.1|Middle Cambrian|Early Cambrian||||Middleton Sandstone; Petrel Cove, Balquhidder, Tunkalilla, Tapanappa, Talisker, Backstairs Passage and Carrickalinga Head Formations.|||28-JUL-15
28634|Kanmantoo Group|69213|5|Briefly described|p37, p38, Fig. 14, p24|Early Cambrian||Includes migmatites of Delamerian [Orogeny] age (~500 Ma)|||Includes Carrickalinga Head Formation|Underlain by Neoproterozoic sediments.|Shallow and deep water mainly clastic sediments. |
28634|Kanmantoo Group|69255|5|Briefly described|p770 Fig.1, p771|Cambrian|Cambrian||Between 522-515 Ma.||||Sedimentary rocks and metasediments.|
28634|Kanmantoo Group|69372|6|Mentioned|p27 fig. 5, p30|Cambrian|Cambrian|Forms bedrock in some regions.||||Underlies Cape Jervis Formation|Shows glaciation striations and textures.|
28634|Kanmantoo Group|69562|6|Mentioned|p684|||||||||
28634|Kanmantoo Group|69876|6|Mentioned|p313|||87Sr/86Sr ratios.||||||
28634|Kanmantoo Group|70025|6|Mentioned|p17|||||||||
28634|Kanmantoo Group|70125|5|Briefly described|p399-401, p403 Fig.15|Early Cambrian|Early Cambrian|Haines et al. (2009) rule out Australia as the source of sediments in this unit in favour of a source beneath the East Antarctic ice sheet.||||||
28634|Kanmantoo Group|70382|5|Briefly described|p32-34|Early Cambrian|Early Cambrian|Deformed and metamorphosed during Cambrian Delamarian Orogeny. Over 8km thick turbiditic sequence.|||Includes Carrickalinga Head Formation.|||
28634|Kanmantoo Group|70407|6|Mentioned|p112||Cambrian||||Includes Milendella Limestone.|||
28634|Kanmantoo Group|70493|6|Mentioned|p56, 63|Early Cambrian|Early Cambrian|Delamerian Orogen, SA. East of the Gawler Craton. Considered unlikely as a sediment source for the Adaminaby Group.||||Overlies Normanville Group.||
28634|Kanmantoo Group|70744|5|Briefly described|p935 Fig.2,p936-937,p943-945,p946 Fig.14|Cambrian|Cambrian|SE Delamerian Orogen. Consists of tectonised, mainly deep-marine sedimentary rocks. Up to 8000m thick. Equivalent to NE Thomson Orogen basement. Detrital zircons are of the Pacific-Gondwana (600-510 Ma) signature; age distribution graph.|524-514 Ma (Haines and Flottmann, 1998).||||Siliciclastic turbidites and local shallow-marine sedimentary rocks.|
28634|Kanmantoo Group|70803|5|Briefly described|p5-p7, p11, p42|Early Cambrian|Early Cambrian|Kanmantoo Trough. Deposited in a subsiding basin or marginal shelf setting.|||||Poorly sorted silts including turbidites.|
28634|Kanmantoo Group|70833|5|Briefly described|p200|Cambrian|Cambrian|Of Eastern Stansbury Basin.||||Underlain unconformably by Heatherdale Shale.||
28634|Kanmantoo Group|70838|6|Mentioned|p267 Fig.1, p271, p277|||Possible tectonic settings discussed.||||||
28634|Kanmantoo Group|70840|6|Mentioned|p444|Cambrian|Cambrian|Geological province: Delamerian Orogen. Comparable detrital zircon age spectra to the northern Victoria Land Neoproterozoic-early paleozoic metasedimentary rocks.||||||
28634|Kanmantoo Group|70865|6|Mentioned|p2|||Adelaide Hills area.|||Nairne Pyrite Member.||Fine-grained greywackes, quartzites and siltstones.|
28634|Kanmantoo Group|70877|6|Mentioned|p168|||||||Equivalent to the Glenthompson Sandstone.||
28634|Kanmantoo Group|71139|6|Mentioned|p152-159, 161|||Adelaide Geosyncline. Pb, Th, U concentrations and Pb isotope data tabulated. Often referred to in the article as Kanmantoo sediment.|>526 Ma (Cooper et al., 1992).|||Overlies Normanville Group. Interbedded with Truro Volcanics.||
28634|Kanmantoo Group|71322|5|Briefly described|p52 Fig.1, p73|Cambrian|Cambrian|||||Intrercalated with Truro Volcanics.|Sandstone; siltstone, occasionally sulfidic; metamorphosed.|
28634|Kanmantoo Group|71348|6|Mentioned|p217|||Affected by Delamerian Orogeny. Rift complex that developed at the southern margin of Gondwanan supercontinent.||||||
28634|Kanmantoo Group|71593|4|Described|p19-p22, p26, p121-p123|Early Cambrian|Early Cambrian|MORB-like rocks. See also p126, p150, p166, p169-p171, p180, p195, p198.|c. 510 Ma|Moralana Supergroup|Includes the Tapanappa Formation.|Disconformably overlies the Normanville Group. Overlies the Truro Volcanics and Heatherdale Shale. Equivalent (in part) to the Nangeela Formation.|Basaltic rocks and MORB-like mafic rocks.|
28634|Kanmantoo Group|73059|5|Briefly described|p1059, 1061-1062, 1064|Early Cambrian|Early Cambrian|Delamerian Fold Belt, South Australia. Contains a substantial 700-500 Ma peak of detrital zircons. Formed in a synorogenic basinal setting, not in an extensional basin setting.||||Overlies Normanville Group.||
28634|Kanmantoo Group|73092|6|Mentioned|p2|Cambrian|Neoproterozoic|||||||
28634|Kanmantoo Group|73093|5|Briefly described|map legend|Cambrian|Cambrian|Shown as 3 distinct units. One sedimentary, the others dominantly igneous. Ek and EK?: Marine metasandstone, phyllite, schist, gneiss, minor calcsilicate rock and marble. Ek3?:dolerite/basalt and minor siltstone. Ek4? Basalt-dolerite, minor siltstone, schist; intruded by granite.|||||Marine metasandstone, phyllite, schist, gneiss, minor calcsilicate rock and marble. Dolerite/basalt and siltstone.|12-DEC-21
28634|Kanmantoo Group|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Kanmantoo Trough. Several facies are mapped separately.|||Carrickalinga Head, Backstairs Passage, Tapanappa, Tunkalilla, Balquhidder, Petrel Cove Formations; Talisker Calc-Siltstone; Middleton Sandstone.||Undifferentiated: grey metasandstone; migmatised, granitised, mylonitised metasediments. Lithologies detailed in the map legend.|
28634|Kanmantoo Group|73118|6|Mentioned|p8, 15, 21|||||||Correlated with Glenelg Zone in western Victoria.|Metasediments.|
28634|Kanmantoo Group|73129|6|Mentioned|p45|||||||||
28634|Kanmantoo Group|73188|5|Briefly described|p: 310-311, 315-317, 339-344, 349-354|Early Cambrian|Early Cambrian|Mount Lofty Ranges, Kanmantoo Trough. Thrust over Pleistocene alluvial fanglomerate at Saunders Creek by the Cenozoic Milendella Fault. Extremely thick succession; deposited rapidly. Better developed in the eastern and southern Mount Lofty Ranges. Deposition was followed by the Delamerian Orogeny. Type section along the south coast of Fleurieu Peninsula.|||Bollaparudda Subgroup, Keynes Subgroup and units therein|Disconformably underlain by Heatherdale Shale (Normanville Group).|Turbidites and shallow-marine sandstones; variously metamorphosed.|
28634|Kanmantoo Group|73228|6|Mentioned|p50-53|Cambrian|Cambrian|Basement.||||Unconformably overlain by Urana Formation.||
28634|Kanmantoo Group|73229|6|Mentioned|p67|early Paleozoic|Neoproterozoic|Basement.||||||
28634|Kanmantoo Group|73236|6|Mentioned|p47|Cambrian|Cambrian|Fleurieu Peninsula; eroded from the Hallett Cove area.|c. 530-510 Ma||||Turbidite-dominated.|
28634|Kanmantoo Group|73247|6|Mentioned|p205, p210|Cambrian (Stage 4)|Cambrian (Stage 4)|Fleurieu Peninsula.||||Unconformably underlain by Heatherdale Shale. Equivalent to Boxing Bay Formation, Emu Bay Shale, Marsden Sandstone, and White Point Conglomerate.|Includes turbidites.|
28634|Kanmantoo Group|73253|6|Mentioned|p15-16|||Adelaide Fold Belt. Characterised by a main zircon population between 700-500 Ma, with a subordinate population between 1200-900 Ma and scattered older zircon ages of 3500-2000 Ma.|||||Includes metasandstones.|
28634|Kanmantoo Group|73264|6|Mentioned|p1386 Fig.9, p1387 Fig.10, p1388|||Adelaide Rift Complex. Marked by introduction of a Panafrican zircon population (~500-650 Ma) and a smaller Grenvillian population (~900-1200 Ma), probably derived from Antarctica. Correlatives of Kanmantoo Group shown p1386 Fig.9 as Cambrian deep water sediments, Delamerian Supercycle.|||Balquidder Formation, Carrickalinga Head Formation|||
28634|Kanmantoo Group|73430|5|Briefly described|p490-493, p495, p497, p507, p512, p518|Early Cambrian|Early Cambrian|Delamerian Orogen. Rapidly deposited in a deep basin and includes a prominent 550-560 Ma source. Sedimentation terminated by an early D1 fold-thrust phase of deformation, possibly as early as 515 Ma. Ar-Ar muscovite ages of 504.7+/-5.5 Ma, 501+/-4.9 Ma and 501.3+/-18 Ma interpreted as cooling ages, from NW Kangaroo Island. Hosts mafic sills or dykes of tholeiitic composition including the Cape Hart dykes, Woodside dykes. Hosts late syn-tectonic 495+/-1.2 Ma granite intrusions of adakite affinity at Kinchina quarry. Equated with Harvester's Creek greywacke (Gibson et al., 2015). Extends from western Kangaroo Island to the western Victorian Glenelg Terrane (Harvester's Creek greywacke). [See also Kanmantoo group p516-517, Kanmantoo complex and Kanmantoo migmatite complexes p513, Kanmantoo Migmatite p505.]||||Overlies Normanville Group, unconformably underlies Mount Monster rhyolite|Thick-bedded siliciclastic-rich turbidites at base. Includes folded metamorphic complexes; deformed amphibolite facies metasedimentary rocks of interbedded sandstone and mudstone recrystallised to black and white pelite-psamite layers.|
28634|Kanmantoo Group|73594|6|Mentioned|p45 Fig.5.19||||||||Volcanics and metasediments.|
28634|Kanmantoo Group|73635|6|Mentioned|p1, p3, p9|Early Cambrian|Early Cambrian|~9000 m thick in the Kanmantoo Trough. Deformed in the Delamerian Orogeny. Intruded by Cambrian granites.|532-514 Ma||||Sedimentary.|
28634|Kanmantoo Group|74367|5|Briefly described|p6-7, p22|||||||Overlies Normanville Group. Intruded by Rathjen Gneiss|Marine metasandstone, phyllite, schist, gneiss, minor calcsilicat and marble.|
37566|Kanni Ignimbrite|23309|4|Described|p110, Table 2.40|||Of the Ninnie Subgroup.  Maximum Thickness: 200m.||||||
37566|Kanni Ignimbrite|24551|4|Described|p143 |||Of Ninnie Subgroup.||||||
37566|Kanni Ignimbrite|60542|3|Fully described|p54, p50|Early Devonian|Early Devonian|Of Ninnie Subgp. Feldspar ingimbrite, low quartz content; lithic fragments. Conformable on Windarra Fm; conformably overlain by Fluke Knob Ignimbrite and Tomato Creek Ignimbrite. Max.thick. in Fluke Knob area: 200m.||||||
37566|Kanni Ignimbrite|68116|5|Briefly described|Appendix, Map 45.|Pragian|Pragian||||||Feldspar ignimbrite: crystal rich, small pumice fragments, not welded, green-grey; pyroclastic deposits.|
9246|Kanowna Island Granite|23309|6|Mentioned|p434 App 1|||G252 S-Type||||||
9246|Kanowna Island Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
9246|Kanowna Island Granite|68116|5|Briefly described|Appendix.|Middle Devonian|Middle Devonian||||||Granite, S-type.|
27046|Kanuka Granodiorite|22876|4|Described|p26|||||||||
27046|Kanuka Granodiorite|22877|5|Briefly described|map|Silurian|Silurian|G36. Biotite Granodiorite.||||||26-OCT-04
27046|Kanuka Granodiorite|22878|4|Described|p88|||||||||
27046|Kanuka Granodiorite|22879|5|Briefly described|map|Silurian|Silurian|Of the Kuark Metamorphic Complex. Biotite granodiorite: grey, fine to medium grained, foliated with compositional banding: dyke like body||||||01-OCT-04
27046|Kanuka Granodiorite|22880|5|Briefly described|Map Legend|Silurian|Silurian|Of the Kuark Metamorphic Complex. Biotite granodiorite: grey, fine to medium grained, foliated with compositional banding: dyke like body||||||01-OCT-04
27046|Kanuka Granodiorite|22881|5|Briefly described|Map legend|Silurian|Silurian|Of the Kuark Metamorphic Complex Supersuite. Biotite granodiorite: Highly magnetic, decreasing towards the periphery.||||||17-JAN-07
27046|Kanuka Granodiorite|23309|5|Briefly described|p350.|Devonian|Devonian|G36 I-Type. Supersedes Kanuka Adamellite and Kanuka Granite. Age: 388 +/- 8 Ma.||||||
27046|Kanuka Granodiorite|41572|6|Mentioned|Fig.1.10|||||||||
27046|Kanuka Granodiorite|42627|5|Briefly described|Map legend|Wenlock||||||||
27046|Kanuka Granodiorite|42647|4|Described|p44|||||||||
27046|Kanuka Granodiorite|42827|6|Mentioned|Fig 1.10|||||||||
27046|Kanuka Granodiorite|68116|5|Briefly described|Appendix.|Wenlock|Llandovery||||||Biotite granodiorite and granite: medium-grained; foliated to strongly rodded with compositional banding; I-type.|
9265|Kapuni Group|40715|6|Mentioned|p59|||||||||
75956|Karoonda Park Volcanic Group|68115|5|Briefly described|p10.|Eocene|Eocene|New name, after Karoonda Park homestead. Replaces Older Volcanic Group for basalt flows on the Wulgulmerang Plateau and outliers to the east. Included in the Gelantipy Subprovince of Price et al. (2003). Further work may divide these extensive rocks into Formations.|||||Olivine tholeiitic basalt and quartz tholeiitic basalt containing olivine phenocrysts.|
75956|Karoonda Park Volcanic Group|68116|5|Briefly described|Appendix, Maps 28, 36.|Rupelian|Lutetian||||||Basalt flows with minor plugs, sills and dykes: olivine tholeiitic basalt and quartz tholeiitic basalt, with olivine phenocrysts.|
37258|Kassingbrook Granodiorite|24012|3|Fully described|p224 appendix 1|||||||||
37258|Kassingbrook Granodiorite|50154|2|Defined|p90, p98, p247 App.5|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex.||||||09-SEP-04
37258|Kassingbrook Granodiorite|50155|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Muscovite-biotite granodiorite; S-type||||||25-JUN-04
37258|Kassingbrook Granodiorite|50156|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granodiorite.||||||20-AUG-04
37258|Kassingbrook Granodiorite|50157|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granodiorite.||||||20-AUG-04
37258|Kassingbrook Granodiorite|50158|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granodiorite.||||||20-AUG-04
37258|Kassingbrook Granodiorite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granodiorite.||||||20-AUG-04
37258|Kassingbrook Granodiorite|50160|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granodiorite.||||||20-AUG-04
37258|Kassingbrook Granodiorite|50161|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granodiorite.||||||20-AUG-04
37258|Kassingbrook Granodiorite|50162|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granodiorite.||||||20-AUG-04
37258|Kassingbrook Granodiorite|50163|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granodiorite.||||||20-AUG-04
37258|Kassingbrook Granodiorite|66002|6|Mentioned|p8 Tb.5|||G417. Defined by Kemp et al. 2002||||||
37258|Kassingbrook Granodiorite|68116|5|Briefly described|Appendix, Maps 29, 38.|Early Ordovician|Middle Cambrian||||||Muscovite-biotite granodiorite: massive, light grey-buff, medium to coarse grained, porphyritic with microcline phenocrysts; common mafic biotite-rich microgranitoid enclaves; local migmatite enclaves and schlieric layering; non-magnetic.|
9306|Katandra Member|29898|5|Briefly described|p213|||||||||
9306|Katandra Member|34735|5|Briefly described|p40|||||||||
9306|Katandra Member|35272|5|Briefly described|p279|||||||||
9306|Katandra Member|41848|5|Briefly described|p355|||Part of Shepparton Formation.||||||27-OCT-08
9306|Katandra Member|42827|5|Briefly described|p355|||see also Table 9.1, of Shepparton Formation.||||||27-OCT-08
9306|Katandra Member|42966|2|Defined|Table 30 p196|Pleistocene||Of Shepparton Formation.||||||27-OCT-08
9306|Katandra Member|60599|5|Briefly described|p92|Quaternary|Quaternary|Of Shepparton Formation.||||||
9306|Katandra Member|70961|4|Described|p133|||Refers to Lawrence (1966). Alluvial.||||||
32297|Kate Shale|12796|6|Mentioned|p460|||Geological Province: Gippsland Basin. Equivalent to Massacre Shale in Otway Basin.||||||
32297|Kate Shale|13323|5|Briefly described|p393 Fig. 2|Early Paleocene|Early Paleocene|Of the Halibut Subgroup (Latrobe Group). Geological Province: Gippsland Basin. See also p395 Fig. 5||||||
32297|Kate Shale|24090|5|Briefly described|p8 Fig.3|Paleocene|Maastrichtian|Geological Province: Gippsland Basin.||||||
32297|Kate Shale|24407|5|Briefly described|p13 Fig.2|||Geological Province: Gippsland Basin||||||
32297|Kate Shale|24551|5|Briefly described|p262 Fig. 9.29, 269|Paleocene|Late Cretaceous|Of the Halibut Subgroup.  Overlies the Volador Formation.||||||
32297|Kate Shale|60538|5|Briefly described|p475 Fig. 14|Early Paleocene|Early Paleocene|Geological Province: Gippsland Basin.||||||
32297|Kate Shale|61552|4|Described|p583-585, pp588-592, p595.  |Early Paleocene|Late Maastrichtian|A mappable stratigraphic marker unit. Type section is in the Flounder-6A Sidetrack hole. Up to 120m thick. This unit separates the Volador and Kingfish Formations in the east of the Gippsland Basin. It is the sealing unit to the intra-Latrobe reservoirs of the Flounder oil field. Log correlation of this unit is aided by its straddling the F. longus and L. balmei spore-pollen zones.||Unit in Halibut Subgroup.||Overlies Volador Formation. Is overlain by Kingfish Formation.|Dark grey mudstones with minor intercalated glauconitic and quartz-bearing sandstones.|
32297|Kate Shale|64876|5|Briefly described|p145 Fig.2|Paleocene|Maastrichtian|Gippsland Basin.||Halibut Subgroup.||||
32297|Kate Shale|65717|5|Briefly described|p9 Fig.2.2, p11-12, p14, p18, p38|Paleocene|Maastrichtian|Partridge (1999). Marine shelf interval, regarded as good sealing lithology. Up to 120m thick.||Halibut Subgroup||Overlain by Grunter Member (Kingfish Formation), Mackerel Formation. Overlies Roundhead Member (Volador Formation).|Siltstone and glauconite.|05-SEP-17
32297|Kate Shale|65973|4|Described|p16, p29, p57, p62, p65|Tertiary|Cretaceous|Gippsland Basin. Deposited in a marine environment. 10m thick in the Sole-1 drillhole. Intersected in Leatherjacket-1,  Kipper-2, Kipper-1, Judith-1, Hammerhead-1, East Pilchard-1, Longtom-1, Longtom-1/ST-1, Longtom-2/ST-1, Sole-1 and many more drillholes (see appendix). See also p71, p74, p76, p78, p80, p82, p86, p90, p97, p100, p106, p110, p123-135, p138, p140, p171.||Halibut Subgroup||Overlies the Volador Formation. Overlain by the Kingfish Formation.||
32297|Kate Shale|70028|6|Mentioned|p79|Paleocene|Paleocene|Offshore Gippsland Basin.||||||
32297|Kate Shale|70076|5|Briefly described|South-Eastern:Fig.2;p2.Regional:Fig.3;p3|Danian|Danian|Marine. Potentially a significant intraformational (Latrobe Group) seal.||Halibut Subgroup.||Overlies Volador Formation. Is overlain by Mackerel or Kingfish Formation.||
32297|Kate Shale|73471|5|Briefly described|p86|||Gippsland Basin.||Halibut Subgroup||Overlies Volador Formation, underlies Mackerel Formation, Kingfish Formation|Marine clastics.|
32297|Kate Shale|75065|5|Briefly described|p151, 154, 166|Paleocene|Maastrichtian|Gippsland Basin; offshore.||Halibut Subgroup.||Overlies Volador Formation. Is overlain by Kingfish Formation.|Dark grey marine mudstones; siltstone, shale.|
9330|Katnook Sandstone|12781|6|Mentioned|p386|Early Cretaceous|Early Cretaceous|Otway Basin. Maximum thickness 690m.||Crayfish Group.||Overlies Laira Formation. Is overlain unconformably by Eumeralla Formation.||
9330|Katnook Sandstone|22674|4|Described|p718, Fig.2 p719|Early Cretaceous|Barremian|||||||
9330|Katnook Sandstone|22686|5|Briefly described|Fig3p745|Aptian|Barremian|Of the upper Crayfish Group.  Geological Province: Otway Basin.||||||17-JAN-06
9330|Katnook Sandstone|24314|5|Briefly described|p61 Fig.2||Hauterivian|Geological Province: Otway Basin. Max. Thickness 690m. Of the Otway Supergroup.||||||30-NOV-04
9330|Katnook Sandstone|24453|5|Briefly described|p809 Fig.2|Hauterivian|Hauterivian|Of Crayfish Subgroup. Geological Province: Otway Basin.||||||07-FEB-11
9330|Katnook Sandstone|24551|6|Mentioned|p245, 249|||Of the Crayfish Subgroup. Overlies: Laira Formation.||||||
9330|Katnook Sandstone|24562|5|Briefly described|p8 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Crayfish Group.  Geological Province: Otway Basin.||||||
9330|Katnook Sandstone|42361|2|Defined|p8|Barremian|Barremian|||||||
9330|Katnook Sandstone|42545|5|Briefly described|Fig.4 P15|||||||||
9330|Katnook Sandstone|42599|5|Briefly described|Fig.3 P614|||||||||
9330|Katnook Sandstone|43171|6|Mentioned|5-6|||||||||
9330|Katnook Sandstone|43195|5|Briefly described|Map Legend||Early Cretaceous|See also commentary on back of map. Of Crayfish Group.||||||
9330|Katnook Sandstone|43660|5|Briefly described|p14|||||||||
9330|Katnook Sandstone|43733|6|Mentioned|Fig.2.11,p65||Early Cretaceous|||||||
9330|Katnook Sandstone|43744|6|Mentioned|Fig.3,p3|||||||||
9330|Katnook Sandstone|43747|5|Briefly described|p5||Early Cretaceous|||||||
9330|Katnook Sandstone|43814|6|Mentioned|Fig.3,p115|||||||||
9330|Katnook Sandstone|44133|5|Briefly described|p145|Hauterivian|Hauterivian|Geological Province: Otway Basin. Previously also known as 'Crayfish Group, Unit D'. Maximum Thickness: 530m. ||||||
9330|Katnook Sandstone|61017|5|Briefly described|p5 Fig. 2|Barremian|Barremian|Of the Crayfish Sungroup (Otway Group). Geological Province: Otway Basin.||||||07-FEB-11
9330|Katnook Sandstone|61470|5|Briefly described|p28 Fig. 5|Barremian|Barremian|Of the Crayfish Subgroup (Otway Group). Overlies and interfingers with Laira Formation. Geological Province: Otway Basin.||||||
9330|Katnook Sandstone|61547|5|Briefly described|p459, p465, pp471-473.|Hauterivian|Hauterivian|On the hangingwall of the Pyrus Fault; juxtaposed against the Pretty Hill Sandstone in the footwall, allowing leaking of hydrocarbons. Consists of reworked Laira Formation.||Unit in the Crayfish Group||Overlies Laira Formation. Is overlain unconformably by the Windermere Sandstone Member.|Predominantly sandstone units with typical shale volumes of 5%, with frequent thin interbeds of shale rich units.|
9330|Katnook Sandstone|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-FEB-11
9330|Katnook Sandstone|61626|5|Briefly described|p486 Fig. 2|Early Cretaceous|Early Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-APR-09
9330|Katnook Sandstone|61627|5|Briefly described|p500 Fig. 2|Early Cretaceous|Early Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-FEB-11
9330|Katnook Sandstone|61628|5|Briefly described|p509 Fig. 3|Early Cretaceous|Early Cretaceous|Of Crayfish Subgroup. Geological Province: Otway Basin.||||||07-APR-09
9330|Katnook Sandstone|63122|5|Briefly described|p17 Fig. 4.3|Barremian|Hauterivian|Of the Crayfish Group. Max. thickness: 690m. Geological Province: Otway Basin. ||||||
9330|Katnook Sandstone|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p63-64|Hauterivian|Valanginian|Of Morton (1990). Formerly unnamed in Pretty Hill Sst (Wopfner et al (1971); also known as Geltwood Beach Mbr and G.B. Fm. Of Crayfish Gp.Overlies Laira Fm; unconformably overlain by Windermere Sst Mbr. Age:133-125Ma. Max. thickness: 690m. In Otway Basin.||||||
9330|Katnook Sandstone|63125|6|Mentioned|p116 Tb.7.6|||Geological Province: Otway Basin||||||
9330|Katnook Sandstone|63129|6|Mentioned|p131|||Geological Province: Otway Basin.||||||30-JAN-08
9330|Katnook Sandstone|63130|5|Briefly described|p143|||Geological Province: Otway Basin.||||||06-FEB-08
9330|Katnook Sandstone|63150|5|Briefly described|p96|||Geological province: Otway Basin. Availability of palynological criteria is vital for identification of this unit.||||||
9330|Katnook Sandstone|63267|5|Briefly described|p485 Fig.2|Early Cretaceous|Early Cretaceous|Penola Trough, Otway Basin.||Crayfish Group.||Overlies Laira Formation. Is overlain unconformably by Windermere Sandstone Member (Eumeralla Formation).||
9330|Katnook Sandstone|63269|5|Briefly described|p605|Early Cretaceous|Early Cretaceous|Otway Basin.||Crayfish Subgroup.||||
9330|Katnook Sandstone|63431|5|Briefly described|p676, p677 Fig. 2|Hauterivian|Hauterivian|Topmost unit of Crayfish Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
9330|Katnook Sandstone|66245|5|Briefly described|p6 Fig.5. |Barremian|Barremian|||Unit in Crayfish Subgroup.||Overlies Laira Formation.||
9330|Katnook Sandstone|67367|5|Briefly described|p131 Fig.2. |Barremian|Barremian|||Unit in Crayfish Subgroup.||||
9330|Katnook Sandstone|69297|5|Briefly described|p79|Barremian|Barremian|Otway Basin. ||Crayfish Subgroup||Overlies the Laira Formation. Unconformably Overlain by the Eumeralla Formation. |Sandstone. |
9330|Katnook Sandstone|69651|5|Briefly described|p10|Early Cretaceous|Early Cretaceous|||Crayfish Subgroup.||Overlies Laira Formation. Is overlain unconformably by Eumeralla Formation.||
9330|Katnook Sandstone|69948|6|Mentioned|Fig.4.2|||Otway Basin (a rift basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Eromanga Basin (an intracratonic basin).||||Overlies Laira Formation. Is overlain by Windermere Sandstone Member (Eumeralla Formation).||
9330|Katnook Sandstone|70077|5|Briefly described|Regional: Fig.4; p4|Barremian|Barremian|Otway Basin: Robe-Penola Trough. Higher energy fluvial sediments.||Crayfish Subgroup.||Overlies Laira Formation. Is overlain by Windermere Sandstone Member (Eumeralla Formation).||
9330|Katnook Sandstone|70880|6|Mentioned|p77|Barremian|Barremian|Otway Basin.||||||
9330|Katnook Sandstone|71266|6|Mentioned|p614 Fig.3|Early Cretaceous|Early Cretaceous|Otway Basin.||||||
9330|Katnook Sandstone|71342|6|Mentioned|Ch4 p9|||Otway Basin. ||||||
9330|Katnook Sandstone|72050|5|Briefly described|p233 Fig.2, 234-235|Barremian|Barremian|Has variable reservoir quality and patchy distribution.||Crayfish Group.|||A thin, discontinuous sandy unit.|
9330|Katnook Sandstone|73356|6|Mentioned|p1, p4, p29|Barremian|Barremian|||Crayfish Subgroup, Otway Group||Underlain by Laira Formation. Unconformably overlain by Windermere Sandstone.||
9330|Katnook Sandstone|73383|5|Briefly described|p3|Barremian|Barremian|Otway Basin.||Crayfish Subgroup|||Fluvial channel sandstones.|
9330|Katnook Sandstone|73385|5|Briefly described|p5|Barremian|Barremian|Otway Basin.||Crayfish Subgroup|||Fluvial channel sandstones.|
9330|Katnook Sandstone|73386|4|Described|p4, p8-9|Barremian|Barremian|Otway Basin. Associated with meandering fluvial to distal braided fluvial palaeoenvironments. Gradational and diachronous relationship with the underlying Laira Formation. Associated with the Upper Foraminisporis wonthaggiensis Spore-Pollen Subzone. Limited to the Penola Trough in South Australia, has not been intersected in Victoria. Type section defined between 1892 m and 1979 m in Katnook-2.||Crayfish Subgroup||Overlies Laira Formation, unconformably underlies Eumeralla Formation, Windermere Sandstone|Dominant lithology is fine- to medium-grained sandstone with interbedded siltstone.|
9330|Katnook Sandstone|73594|5|Briefly described|p3-4, p16, p41-44, p47, p67|Barremian|Barremian|Otway Basin. Diachronous unit. Passes laterally into the Laira Formation. Type section defined in Katnook-1 well by Morton (1990). Defined by the upper F. wonthaggiensis spore-pollen zone. Becomes thicker and sandier westwards towards the St Claire Trough. High-sinuosity fluvial sandstone. Characterised by an apparent fluvial flow reversal when compared to the Pretty Hill and Eumeralla formations.||Crayfish Subgroup, uppermost unit||Overlies Laira Formation, Pretty Hill Formation. Unconformably underlies Windermere Member, Eumeralla Formation|Fine to medium grained cross bedded sandstone with reworked siltstone intraclasts and carbonaceous partings.|
9346|Kawarren Formation|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
9346|Kawarren Formation|42827|6|Mentioned|p296|||refers to informal use by Mines Department (1966)||||||
37752|Keelangie Creek Granodiorite|23309|5|Briefly described|p434, Appendix 1|Silurian|Silurian|G570, I-Type.  Age: 424+/-3Ma.||||||
37752|Keelangie Creek Granodiorite|24133|3|Fully described|p65|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Age: 424 +/- 3 Ma (K/Ar). Hornblende granodiorite: I-type; nonmagnetic; moderate to low K, low Th, variable U.||||||09-SEP-04
37752|Keelangie Creek Granodiorite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37752|Keelangie Creek Granodiorite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37752|Keelangie Creek Granodiorite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37752|Keelangie Creek Granodiorite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Hornblende granodiorite: pale grey, medium to coarse grained equigranular; I-type; nonmagnetic; weathered||||||09-SEP-04
37752|Keelangie Creek Granodiorite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37752|Keelangie Creek Granodiorite|68116|5|Briefly described|Appendix, Map 20.|Ludlow|Ludlow||||||Hornblende granodiorite: pale grey, medium to coarse grained equigranular; I-type; nonmagnetic; weathered; minor pale green amphibole, chlorite, sphene and opaques.|
35172|Kelfeera Granite|22971|5|Briefly described|p 35|||||||||
35172|Kelfeera Granite|68116|5|Briefly described|Appendix, Map 26.|Late Devonian|Late Devonian||||||Biotite granite: medium grained slightly porphyritic.|
26657|Kelly Gap Granite|22971|5|Briefly described|p 34|||||||||
26657|Kelly Gap Granite|23309|5|Briefly described|p434 App1|||G201 S-Type.||||||27-AUG-04
26657|Kelly Gap Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
26657|Kelly Gap Granite|68116|5|Briefly described|Appendix, Map 19.|Late Devonian|Late Devonian||||||Biotite granite: fine to medium grained, mid grey; fractionated; porphyritic; contains miarolitic cavities and areas of granophyre; S-type.|
37753|Kenny Creek Diorite|23309|6|Mentioned|p434 Appendix 1|||G129, I-Type.  Supersedes Kenny Creek Granodiorite.||||||
37753|Kenny Creek Diorite|23938|5|Briefly described|p71 Fig. 25|Silurian|Silurian|Creek is Ck. In text of figure.||||||25-SEP-08
37753|Kenny Creek Diorite|43312|5|Briefly described|Map Legend|Wenlock|Wenlock|G129. Hornblende diorite, medium grained, leucocratic fine-grained granodiorite in southern portion, I-Type.||||||
37753|Kenny Creek Diorite|44185|5|Briefly described|Map legend.|Silurian|Silurian|I-type.||||||
37753|Kenny Creek Diorite|60542|4|Described|p96, p19 Fig. 3|Late Silurian|Late Silurian|Hornblende-rich diorite, medium-grained; well-zoned, euhedral plagioclase crystals (up to 2.5mm long) and hornblende crystals (up to 10mm long) form an aggregate infilled with interstitial quartz and minor K-feldspar. ||||||
37753|Kenny Creek Diorite|68116|5|Briefly described|Appendix, Map 45.|Wenlock|Llandovery||||||Hornblende diorite: medium-grained, leucocratic fine-grained granodiorite in southern portion; I-type intrusive.|
41932|Kent Road Granite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|Of the Ocean View Suite. G507. S-type. Foliated, medium grained biotite, muscovite granodiorite.||||||
41932|Kent Road Granite|43315|5|Briefly described|Map Legend|Wenlock|Wenlock|G507. Of Ocean View Suite, S-type. Foliated, medium grained biotite, muscovite granodiorite.||||||03-MAY-05
41932|Kent Road Granite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Biotite-muscovite granodiorite: medium-grained; foliated; S-type.|
32460|Keppel Creek Granodiorite|23309|5|Briefly described|p162 Fig 2.111.|||G225 S-Type||||||
32460|Keppel Creek Granodiorite|44187|5|Briefly described|Map Legend||Late Devonian|G225 Unassigned.||||||
32460|Keppel Creek Granodiorite|68116|5|Briefly described|Appendix, Map 33.|Late Devonian|Late Devonian||||||Microgranodiorite: medium to fine grained; saccharoidal, porphyritic.|
9458|Kerang Sand Member|2967|4|Described|p35, 46|||One line after the first appearance in the text, it appears as Kerang Sand; this [presumed] abbreviation continues in the text; see references (p35, p36 Fig.2.19, p46-47, 80-81, 148).||Parilla Sand.||Locally overlies, and partly intertongues with, the Calivil Formation.||
9458|Kerang Sand Member|10010|5|Briefly described|p12 Fig. 3|Early Pliocene|Late Miocene|Of Loxton-Parilla Sand. Geological Province: Murray Basin.||||||13-AUG-07
9458|Kerang Sand Member|22773|5|Briefly described|Fig24.8p352||Late Miocene|||||||
9458|Kerang Sand Member|22782|6|Mentioned|p15|||||||||
9458|Kerang Sand Member|22799|5|Briefly described|p24 Fig.10|Early Pliocene|Late Miocene|||||||
9458|Kerang Sand Member|22857|5|Briefly described|p352 Fig.24.8|Early Pliocene|Late Miocene|Of the Loxton-Parilla Sand? (relationship not clear in figure). Geological Province: Murray Basin.||||||
9458|Kerang Sand Member|22887|5|Briefly described|Fig.6 p13||Late Miocene|||||||
9458|Kerang Sand Member|22893|5|Briefly described|fig4 p9|||||||||
9458|Kerang Sand Member|23884|5|Briefly described|p155 Fig.13.2|Early Pliocene|Late Miocene|Geological Province: Murray Basin.||||||
9458|Kerang Sand Member|34757|6|Mentioned|p50|||||||||
9458|Kerang Sand Member|39329|6|Mentioned|p483|||||||||
9458|Kerang Sand Member|40820|6|Mentioned|Fig.4|||||||||
9458|Kerang Sand Member|42130|6|Mentioned|Fig.3 P265|||||||||
9458|Kerang Sand Member|42134|6|Mentioned|Fig.3 P335|||||||||
9458|Kerang Sand Member|42966|2|Defined|Table 27, p172|Early Pliocene|Late Miocene|of Loxton-Parilla Sands||||||
9458|Kerang Sand Member|43791|6|Mentioned|p372, Fig1|||||||||
9458|Kerang Sand Member|43804|6|Mentioned|Fig.2,p49|||||||||
9458|Kerang Sand Member|49040|6|Mentioned|Fig.6|||||||||
9458|Kerang Sand Member|60452|5|Briefly described|p37|Cenozoic|Cenozoic|Basal unit of the Parilla Sand. Medium to coarse-grained marine quartz sand. Overlain by the Tragowel Member. Maximum Thickness: 30m.||||||19-NOV-08
9458|Kerang Sand Member|65552|5|Briefly described|p5 Fig. 3|Early Pliocene|Late Miocene|Of Loxton-Parilla Sands. Unconformably overlies Geera Clay and Olney Formation. Underlies Tragowel and Wandella Sandstone Members.||||||
9458|Kerang Sand Member|66286|6|Mentioned|p179, 188|||Southern Murray Basin. Transgressive beach facies.||Unit in Loxton-Parilla sands.||Is overlain by Tragowel Member.||
9458|Kerang Sand Member|67179|4|Described|p581|Pliocene|Miocene|Transgressive. Also described as Kerang Sand.||Of Loxton Sand||Underlies by the Tragowel Member.|Coarse-grained quartz sand, swash zone.|
9458|Kerang Sand 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 underlying and partially equivalent to  Tragowel Member and Bookpurnong beds.|Includes sand.|
27663|Kergunyah Granite|22971|5|Briefly described|p 33|||||||||
27663|Kergunyah Granite|23309|5|Briefly described|p434 App 1|||G180. Supersedes Kergunyah Adamellite. Age: 392 +/- 4 Ma.||||||
27663|Kergunyah Granite|38879|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Middle to Lower Devonian||||||
27663|Kergunyah Granite|39446|5|Briefly described|p27|||||||||
27663|Kergunyah Granite|44184|5|Briefly described|Map Legend||Early Devonian|||||||
27663|Kergunyah Granite|68116|5|Briefly described|Appendix, Maps 19, 20.|Early Devonian|Early Devonian||||||Leucocratic two-mica granite: coarse grained; S-type.|
9471|Kerrie Group|41585|6|Mentioned|Fig.4.1|||||||||
9471|Kerrie Group|64619|5|Briefly described|Map legend|Early Devonian|Silurian|Includes Kirribilly Siltstone and Goat Rocks Conglomerate. Age is either Silurian or Lower Devonian.||||||
9471|Kerrie Group|65715|2|Defined|p5-6, p5 Tb.3, p29|Early Devonian|Silurian|Newly defined here. Of Skeats and Summers (1912). Includes Goat Rocks Conglomerate and Kirribilly Formation. Possibly unconformable contact with Willimigongong Ignimbrite. Limited distribution of ~50 sq. km on E and SE flanks of Macedon Range. Intruded by Barringo Granodiorite. ~900 m thick. In Lancefield 1:50 000 sheet. Silurian or Lower Devonian.||||||
9475|Kerrs Road Basalt|39865|4|Described|p34|||||||||
9475|Kerrs Road Basalt|65715|5|Briefly described|p14 Tb.8|Neogene|Neogene|Of Roberts (1984) p34.||||||
32291|Kersop Arkose|13323|5|Briefly described|p393 Fig. 2|Turonian|Turonian|Oldest unit of Emperor Subgroup. Alluvial fan/fluvial deposits - coarse feldspathic sandstones and conglomerates. Overlain by Kipper Shale; also overlain by Admiral Formation which is partly laterally equivalent. Geol. Prov: Gippsland Basin. ||||||
32291|Kersop Arkose|24090|5|Briefly described|p8 Fig.3|Cretaceous|Cretaceous|Geological Province: Gippsland Basin.||||||
32291|Kersop Arkose|24407|5|Briefly described|p13 Fig.2|||Geological Province: Gippsland Basin||||||
32291|Kersop Arkose|24551|5|Briefly described|p267|||Of the Emperor Subgroup.  Underlies: Admiral Formation.||||||
32291|Kersop Arkose|61552|6|Mentioned|p583 Fig.2. |Late Cretaceous|Late Cretaceous|||Unit in Emperor Subgroup.||||
32291|Kersop Arkose|64876|5|Briefly described|p145 Fig.2|Turonian|Turonian|Gippsland Basin.||Emperor Subgroup.||||
32291|Kersop Arkose|65717|5|Briefly described|p9 Fig.2.2, p10|Turonian|Cenomanian|Bernecker and Partridge (2001). Gippsland Basin. Derived from erosion of uplifted granites.||Emperor Subgroup||Overlain by, and may be laterally equivalent to, Admiral Formation.|Coarse grained to conglomeratic quartz and feldspathic sandstone.|05-SEP-17
32291|Kersop Arkose|65973|5|Briefly described|p14, p57, p123, p171|||Gippsland Basin. Defined in Moray-1 (the type section). Intersected in Admiral-1 borehole.||Emperor Subgroup.|||Coarse-grained, feldspathic sandstone.|
32291|Kersop Arkose|70076|5|Briefly described|South-Eastern: Fig.2. Regional: p2|Turonian|Turonian|Represents the earliest erosion of uplifted granites at the southern Basin margin.||Emperor Subgroup||Locally overlies Wonthaggi Formation. Is overlain by Kipper Shale or Chimaera Formation.||
32291|Kersop Arkose|75065|5|Briefly described|p151, 161|Turonian|Albian|Gippsland Basin; offshore.||Emperor Subgroup.||Unconformably overlies Korumburra Subgroup. Is overlain by Curlip Formation. Is adjacent to Kersop Arkose.||
9481|Kevington Creek Formation|22729|4|Described|p583,84,87,590,92|Frasnian|Givetian|Subunit of Delatite Group.||||||27-OCT-08
9481|Kevington Creek Formation|23309|5|Briefly described|p173-184 Tb 2.65|||||||||
9481|Kevington Creek Formation|24177|5|Briefly described|p50 Fig.22|Late Devonian|Late Devonian|Geological Province: Mount Easton Province.||||||
9481|Kevington Creek Formation|24551|5|Briefly described|p88 Fig. 3.15, 168|Late Devonian|Late Devonian|Of Delatite Group.  Overlies: Callemondah Conglomerate (c).  ||||||
9481|Kevington Creek Formation|42827|5|Briefly described|Table 4.1|||||||||
9481|Kevington Creek Formation|60599|5|Briefly described|p47 Fig. 19|Late Devonian|Late Devonian|Geological Province: Mount Easton Province, Melbourne Zone, Lachlan Fold Belt.||||||
9481|Kevington Creek Formation|61161|5|Briefly described|p125|||Of Delatite Group. Mansfield Basin. Overlies Callemondah Conglomerate.||||||
9481|Kevington Creek Formation|61185|5|Briefly described|p21 Fig. 6|Late Devonian|Late Devonian|Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
9481|Kevington Creek Formation|64010|5|Briefly described|p258 Fig.1. |||||Of the Delatite Group. |Includes Monkey Gully Sandstone Member, Flagstone Creek Sandstone Member and Callemondah Conglomerate.|||
9481|Kevington Creek Formation|64536|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Of Delatite Group. Mudstone, minor sandstone, occasional conglomerate:mudstone is red; sandstone thick bedded, through- and tabular-cross-bedded, quartz lithic, micaceous; conglomerates form bases of upward-fining sequences. Fluvial.||||||07-FEB-11
9481|Kevington Creek Formation|64537|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Of Delatite Group. Mudstone, minor sandstone, occasional conglomerate:mudstone is red; sandstone thick bedded, through- and tabular-cross-bedded, quartz lithic, micaceous; conglomerates form bases of upward-fining sequences. Fluvial.||||||07-FEB-11
9481|Kevington Creek Formation|64538|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Of Delatite Group. Mudstone, minor sandstone, occasional conglomerate:mudstone is red; sandstone thick bedded, through- and tabular-cross-bedded, quartz lithic, micaceous; conglomerates form bases of upward-fining sequences. Fluvial.||||||07-FEB-11
9481|Kevington Creek Formation|64606|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Of Delatite Group. Includes Monkey Gully Sandstone Member and Flagstone Creek Sandstone Member. Mudstone, minor sandstone, occasional conglomerate: alluvial deposits. Red-pink to yellow-pink in RGB. Nonmagnetic.||||||11-NOV-08
9481|Kevington Creek Formation|64616|4|Described|p133, 132, p155, p188-189, p279, p301|Givetian|Givetian|Of Delatite Group. Includes Flagstone Creek Sandstone Member and Monkey Gully Sandstone Member. Unconformably overlies Murrindindi Supergroup. Conformably overlies Callemondah Conglomerate. Unconformably overlain by Highton Volcanics and Mansfield Group. 1000-1500m thick. Red siltstone; minor interbedded gritty sandstone, thick-bedded; occasional conglomerate. Mid-Givetian fish fauna p132. Geophysical characteristics given.||||||
9481|Kevington Creek Formation|68116|5|Briefly described|Appendix, Map 34.|Late Devonian|Late Devonian||||||Mudstone, minor sandstone, occasional conglomerate: mudstone red; sandstone thick-bedded, trough- and tabular cross-bedded; quartz-lithic, micaceous; conglomerates form bases of upward-fining sequences.|
9507|Kialla Member|29898|6|Mentioned|p213|||||||||
9507|Kialla Member|35272|5|Briefly described|p280|||||||||
9507|Kialla Member|41848|5|Briefly described|p355|||Part of Shepparton Formation.||||||27-OCT-08
9507|Kialla Member|42827|5|Briefly described|p355|||Of Shepparton Formation.||||||04-OCT-06
9507|Kialla Member|42966|2|Defined|Table 30 p196|Pleistocene||Of Shepparton Formation.||||||04-OCT-06
9507|Kialla Member|60599|5|Briefly described|p92|Quaternary|Quaternary|Of Shepparton Formation.||||||
9507|Kialla Member|61185|5|Briefly described|p63|||Of Lawrence (1966,1975) and Jenkin (1988). Of Shepparton Formation. Disconformably underlies Katandra Member.||||||07-FEB-11
9507|Kialla Member|70961|14|Not recorded|p133|||Refers to Lawrence (1966). Alluvial.||||||
27446|Kiandra Group|22857|5|Briefly described|p126, p420 App. 1 Tb. A1.5|Late Ordovician|Darriwilian|Volcanics.||||||14-MAR-07
27446|Kiandra Group|22968|5|Briefly described|P30, P103||Ordovician|||||||
27446|Kiandra Group|23020|5|Briefly described|Map legend|Late Ordovician|Late Ordovician|||||||
27446|Kiandra Group|23021|5|Briefly described|Map legend|Late Ordovician|Late Ordovician|Overlies the Adaminaby Group.||||||25-SEP-08
27446|Kiandra Group|23028|5|Briefly described|Map legend|Late Ordovician|Late Ordovician|Underlying unit is Adaminaby Group.||||||25-SEP-08
27446|Kiandra Group|23029|5|Briefly described|Map legend|Eastonian|Gisbornian|||||||
27446|Kiandra Group|23030|5|Briefly described|Map legend|Ordovician|Ordovician|||||||
27446|Kiandra Group|23245|6|Mentioned|p126-7|||||||||
27446|Kiandra Group|23307|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
27446|Kiandra Group|23309|5|Briefly described|p15, 59, 60, 61. Tb 2.20||Late Ordovician|||||||
27446|Kiandra Group|23938|5|Briefly described|p31-32 Fig. 12|Middle ordovician|Early Ordovician|See also p139 Tb. 1 Appendix.||||||20-MAY-08
27446|Kiandra Group|24004|5|Briefly described|p275 Fig.2|Ordovician|Ordovician|||||||
27446|Kiandra Group|24133|3|Fully described|p55|||Geological Province: Lachlan Fold Belt.||||||
27446|Kiandra Group|24164|5|Briefly described|p15 Fig.8|Ordovician|Ordovician|Min age: Ordovician/Silurian boundary?|||||Turbidite, shale, chert|
27446|Kiandra Group|24551|4|Described|p106|Gisbornian|Gisbornian|||||||14-MAR-07
27446|Kiandra Group|36443|5|Briefly described|map legend|Late Ordovician|Early Ordovician|Includes Temperance Formation and Nine Mile Volcanics. Geol. Prov: Molong Volcanic Arc.||||||
27446|Kiandra Group|36512|6|Mentioned|p21|||||||||
27446|Kiandra Group|40136|6|Mentioned|p18|||||||||
27446|Kiandra Group|41905|6|Mentioned|p27|||||||||
27446|Kiandra Group|42820|5|Briefly described|p78|||||||||
27446|Kiandra Group|43220|6|Mentioned|p9||Ordovician|||||||
27446|Kiandra Group|44092|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Ovk1||||||
27446|Kiandra Group|44093|5|Briefly described|p189 App. 1|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
27446|Kiandra Group|44184|5|Briefly described|Map Legend||Early Ordovician|||||||
27446|Kiandra Group|45147|3|Fully described|M20|||||||||
27446|Kiandra Group|60078|6|Mentioned|Map Legend|Late Ordovician|Middle Ordovician|||||||
27446|Kiandra Group|61187|6|Mentioned|p26 Fig.2, p29 Fig.4. |||||||||
27446|Kiandra Group|63278|5|Briefly described|p157|Gisbornian|Darriwilian |Includes; Blueys Creek Formation, Temperance Formation, Nine Mile Volcanics. Geological Province: Kiandra Volcanic Belt, LFB.||||||07-FEB-11
27446|Kiandra Group|63290|6|Mentioned|p403 Fig. 6(c)|Early Silurian|Middle Ordovician|Geological Province: Tantangara Block.||||||
27446|Kiandra Group|67322|5|Briefly described|p4 Fig.2, p26; Fig.5|Katian|Darriwilian|Macquarie Arc. Defined by Owen and Wyborn (1979). New, unpublished mapping by Quinn suggests a significant reassessment is warranted. Occurs in the Kiandra Volcanic Belt.|||Temperance Formation, Nine Mile Volcanics, Gooandra Volcanics.|||22-FEB-18
27446|Kiandra Group|67847|6|Mentioned|p77|||Molong Volcanic Arc. ||||||
27446|Kiandra Group|68116|5|Briefly described|Appendix, Map 28.|Sandbian|Sandbian|Gisbornian age.|||||Basalt lava, agglomerate, sandstone, chert, black cherty slate.|
27446|Kiandra Group|68592|5|Briefly described|p30|Ordovician|Ordovician|Snowy Mountains area. Displaced at least 50km with left lateral strike-slip movement by the Long Plain Fault.||||Is faulted against Adaminaby Group. Is overlain unconformably by Tantangara Formation.||
27446|Kiandra Group|70718|5|Briefly described|p44|Gisbornian|Darriwilian|Wagga-Omeo Zone, Murray Basin. The source of the ages is not provided. Deposited in a submarine volcanic chain.|468.1-460.5 Ma||||Agglomerate, sandstone, basaltic lavas, mudstone and chert.|
27446|Kiandra Group|73581|6|Mentioned|p25|Ordovician|Ordovician|||||||
9536|Kiewa Granodiorite|31800|5|Briefly described|p210|||||||||
9536|Kiewa Granodiorite|39860|4|Described|p15|||||||||
9536|Kiewa Granodiorite|70910|4|Described|p49|||||||||
9552|Kilgower Member|23229|6|Mentioned|p35||Early Devonian|||||||
9552|Kilgower Member|23309|5|Briefly described|p104, 133. Tb 2.38||Early Devonian|||||||
9552|Kilgower Member|23710|14|Not recorded|p84|||Excursion.||||||
9552|Kilgower Member|24551|5|Briefly described|p138, 620||Late Pragian|Of the Tabberabbera Formation.||||||
9552|Kilgower Member|30790|6|Mentioned|p3|||Member Tabberabbera Formation. Early Emsian? age||||||
9552|Kilgower Member|32399|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
9552|Kilgower Member|32583|6|Mentioned|p374|||||||||
9552|Kilgower Member|33326|6|Mentioned|p433|||Fauna.||||||
9552|Kilgower Member|33393|6|Mentioned|p163|||||||||
9552|Kilgower Member|33408|6|Mentioned|p234|||||||||
9552|Kilgower Member|33481|6|Mentioned|p16|||||||||
9552|Kilgower Member|33606|6|Mentioned|p68|||||||||
9552|Kilgower Member|33732|5|Briefly described|Table III|||||||||
9552|Kilgower Member|34250|6|Mentioned|p19|||L.Dev.||||||
9552|Kilgower Member|34251|6|Mentioned|p540|||L.Dev. See also PP545, 547||||||
9552|Kilgower Member|34403|6|Mentioned|p149|||||||||
9552|Kilgower Member|34954|6|Mentioned|Fig.34|||||||||
9552|Kilgower Member|35193|6|Mentioned|p21|||||||||
9552|Kilgower Member|36587|6|Mentioned|p8|||||||||
9552|Kilgower Member|37330|5|Briefly described|p17|||||||||
9552|Kilgower Member|41000|6|Mentioned|p279|||||||||
9552|Kilgower Member|41585|6|Mentioned|Fig.4.9|||||||||
9552|Kilgower Member|42015|6|Mentioned|p316|||||||||
9552|Kilgower Member|42033|6|Mentioned|p653|||||||||
9552|Kilgower Member|42577|5|Briefly described|Fig.3, P28|||||||||
9552|Kilgower Member|43461|14|Not recorded|p628|||Part of Tabberabbera Formation||||||
9552|Kilgower Member|43530|14|Not recorded|p1030|||Part of Wentworth Group||||||
9552|Kilgower Member|43541|14|Not recorded|p263|||||||||
9552|Kilgower Member|43547|14|Not recorded|p150,154||Emsian|Part of Tabberabbera Formation||||||
9552|Kilgower Member|43871|14|Not recorded|p12-55||Early Devonian|||||||
9552|Kilgower Member|47037|6|Mentioned|p114|||||||||
9552|Kilgower Member|48971|6|Mentioned|p10|||See also P40, P24.||||||
9552|Kilgower Member|61161|5|Briefly described|p118|||Of Tabberabbera Formation. Overlies Dead Bull Member. Underlies Roaring Mag Member. Interbedded mudstone and sandstone.||||||
9552|Kilgower Member|70742|6|Mentioned|p173|||Tabberabbera area. Age approximately early Emsian. Contains possible Taungurungetes taggertyensis brachiopods.||||||
83257|Killara coal measures|73386|5|Briefly described|p5, p9|||Otway Basin. Not a formal lithostratigraphic unit. Coal beds occur at the base of the Eumeralla Formation and elsewhere in the formation. The coals are not laterally extensive and are difficult to correlate. Appears as 'Killara coal measures' p9.||Eumeralla Formation|||Black coals at the base of the Eumeralla Formation.|
26662|Killawarra Granite|22971|5|Briefly described|p 34|||||||||
26662|Killawarra Granite|23309|5|Briefly described|p434 App1|||G206 S-Type.||||||27-AUG-04
26662|Killawarra Granite|24551|6|Mentioned|p223|||Of the Strathbogie Province.||||||
26662|Killawarra Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
26662|Killawarra Granite|68116|5|Briefly described|Appendix, Map 19.|Late Devonian|Late Devonian||||||Biotite granite: medium grained, pale grey; S-type.|
40916|Killeen Basalt|24177|4|Described|p74|Cenozoic|Cenozoic|Of the Newer Volcanics. Erupted through the Strathbogie Granite which it unconformably overlies. Maximum Thickness: <4m||||||19-NOV-08
40916|Killeen Basalt|60529|5|Briefly described|Map Legend|Pliocene|Pliocene|Of the Newer Volcanics. Lava flow: basanite, iddingsitised olivine phenocrysts in matrix of clinopyroxene, plagioclase, olivine and opaque minerals; nodular weathered texture; irregular jointing.||||||14-JUN-06
40916|Killeen Basalt|61185|2|Defined|p63, p62|Tertiary|Tertiary|Of Newer Volcanics.  Volcanic vent and small lava flow erupted through Strathbogie Granite and overlies it nonconformably; and does not extend beyond it. Max. thickness: remains of flow <4m. Massive basalt.||||||07-FEB-11
40916|Killeen Basalt|61701|5|Briefly described|Map Legend|Pliocene|Pliocene|Of the Newer Volcanics. Lava flow: basanite, iddingsitised olivine phenocrysts in matrix of clinopyroxene, plagioclase, olivine and opaque minerals; nodular weathered texture; irregular jointing.||||||25-JUL-06
40916|Killeen Basalt|61702|5|Briefly described|Map Legend|Pliocene|Pliocene|Of the Newer Volcanics. Lava flow: basanite, iddingsitised olivine phenocrysts in matrix of clinopyroxene, plagioclase, olivine and opaque minerals; nodular weathered texture; irregular jointing.||||||25-JUL-06
40916|Killeen Basalt|61703|5|Briefly described|Map Legend|Pliocene|Pliocene|Of the Newer Volcanics. Lava flow: basanite, iddingsitised olivine phenocrysts in matrix of clinopyroxene, plagioclase, olivine and opaque minerals; nodular weathered texture; irregular jointing.||||||25-JUL-06
40916|Killeen Basalt|61704|6|Mentioned|Map legend|Quaternary|Quaternary|Indistinct radiometric  and magnetic responses.||||||12-FEB-15
40916|Killeen Basalt|66244|5|Briefly described|p7-8|||Euroa area. Description and analysis in Paul et al. (2005). Grouped with the Newer Volcanic Group by Edwards et al. (1997). A small flow about 8 km SE of Longwood.||Unit in Euroa Volcanic Group.|||Alkali basalt.|
40916|Killeen Basalt|68116|5|Briefly described|Appendix, Map 25.|Miocene|Miocene||||||Mottled grey basanite with partially altered olivine crystals to 3 mm in a very fine-grained groundmass consisting of clinopyroxene, plagioclase, olivine and opaque minerals.|
23698|Killingworth Formation|23229|5|Briefly described|Table3-3p26, 31|Pragian|Pragian|||||||
23698|Killingworth Formation|23309|5|Briefly described|p146|||||||||
23698|Killingworth Formation|24177|5|Briefly described|p50 Fig.22|Early Devonian|Early Devonian|Of the Humevale Siltstone. Geological Province: Darraweit Guim Province.||||||27-OCT-08
23698|Killingworth Formation|38787|6|Mentioned|p125|||||||||
23698|Killingworth Formation|41585|4|Described|p111|||||||||
23698|Killingworth Formation|41909|6|Mentioned|p111|||||||||
23698|Killingworth Formation|42827|5|Briefly described|p111|||see also Table 4.1||||||
23698|Killingworth Formation|60599|5|Briefly described|p47, p56|Pragian|Lochkovian|Geological Province: Darraweit Guim Province, Melbourne Zone, Lachlan Fold Belt.||||||
23698|Killingworth Formation|61185|5|Briefly described|p21 Fig. 6, p45|Pragian|Pridolian|Formerly of Humevale Siltstone. Of Garratt (1986). Now considered to belong to Norton Gully Sandstone. Geological Province: Lachlan Fold Belt, Melbourne Zone. See Killingsworth Formation.||||||07-FEB-11
23698|Killingworth Formation|66244|5|Briefly described|p3.|||Flowerdale area. Shown on the Kinglake 1:63 360 sheet (Garratt 1977); it is (equivalent to) the Broadford Formation.||||||
9565|Kiln Member|23309|5|Briefly described|p149. Tb 2.57||Devonian|||||||
9565|Kiln Member|24551|5|Briefly described|p130|||Of Waratah Limestone||||||
9565|Kiln Member|30570|6|Mentioned|p4|||||||||
9565|Kiln Member|34954|5|Briefly described|p194|||||||||
9565|Kiln Member|35274|5|Briefly described|p421|||||||||
9565|Kiln Member|41868|5|Briefly described|p575|||||||||
9565|Kiln Member|42577|6|Mentioned|p31|||Synonymous with "Mushroom Rock Member"?||||||
9565|Kiln Member|42635|5|Briefly described|p26|||||||||
9565|Kiln Member|42827|5|Briefly described|p575|||of Waratah Limestone||||||
9565|Kiln Member|43530|14|Not recorded|p1029|||Part of Bell Point Limestone||||||
9565|Kiln Member|43537|14|Not recorded|p7||Siegenian|Member of Waratah Limestone||||||
9565|Kiln Member|61181|5|Briefly described|p127|Early Devonian|Early Devonian|Together with the Kiln Member forms the uppermost section of the Waratah Limestone. Light grey, generally poorly fossiliferous limestone. Thickness: 110m. See also the informal Kiln member.||||||
34839|Kimberly Park Granite|22968|5|Briefly described|P54, P178||Early Silurian|New name, nonmagnetic, intrudes the Omeo Metamorphics||||||
34839|Kimberly Park Granite|23021|5|Briefly described|Map legend|Wenlock|Wenlock|||||||
34839|Kimberly Park Granite|23309|6|Mentioned|p434 App1|||G79 S-Type.||||||
34839|Kimberly Park Granite|60508|5|Briefly described|Map legend|Early Silurian|Early Silurian|Biotite granite: S-type; nonmagnetic (0-5 nT); moderate K, low total count, Th, U||||||
34839|Kimberly Park Granite|68116|5|Briefly described|Appendix, Maps 27, 35.|Wenlock|Llandovery||||||Granodiorite: medium-grained, grey, foliated; contains large metasedimentary enclaves.|
30359|Kindalyn Granite|23165|5|Briefly described|Map legend||Devonian|||||||
32494|King Parrot Creek Granodiorite|22882|4|Described|p 13|||||||||11-FEB-15
32494|King Parrot Creek Granodiorite|22885|5|Briefly described|map|||||||||
32494|King Parrot Creek Granodiorite|22886|5|Briefly described|Table.1|||Age: Rb/Sr 370 Ma. of Strathbogie Batholith.||||||
32494|King Parrot Creek Granodiorite|23309|5|Briefly described|p435 App1|Devonian|Devonian|G219 S-Type. Age: 362 +/- 6Ma.||||||
32494|King Parrot Creek Granodiorite|24551|6|Mentioned|p717 Table 2.4|Late Devonian|Late Devonian|Age: 369 +/- 3Ma.||||||
32494|King Parrot Creek Granodiorite|44197|5|Briefly described|Map Legend||Late Devonian|G219 S-type.||||||
32494|King Parrot Creek Granodiorite|66244|3|Fully described|p4.|||Originally the Kerrisdale Cordierite Microadamellite (Phillips et al. 1981); subsequently the King Parrot Creek intrusion, with no lithology specified (Gray 1990); later the King Parrot Creek Granodiorite (McDonald 1997). Named after King Parrot Creek, which flows along the aureole of the pluton. Type locality MGA 343430-5883840. A circular, non-magnetic, very low-K/Th/U pluton on SW edge of the Strathbogie Granite.|||||Medium-grained, biotite-cordierite granodiorite, mostly porphyritic with scattered phenocrysts of K-feldspar 5 - 20 mm across; local equigranular outcrops; accessory apatite, zircon and ilmenite: the last two within biotite grains.|11-FEB-15
32494|King Parrot Creek Granodiorite|68116|5|Briefly described|Appendix, Map 33.|Late Devonian|Late Devonian||||||Biotite granodiorite: grey, medium grained, equigranular to porphyritic with K-feldspar phenocrysts 5 - 20 mm across; rare small biotite-rich enclaves; S-type.|
32298|Kingfish Formation|13323|5|Briefly described|p393 Fig. 2|Early Eocene|Early Paleocene|Of the Halibut Subgroup (Latrobe Group). Includes the Stonefish and Grunter Members. Fluvial-deltaic and paralic deposits. Geological Province: Gippsland Basin.||||||
32298|Kingfish Formation|24090|5|Briefly described|p8 Fig.3|Eocene|Paleocene|Includes the Stonefish Sandstone and Grunter Members.  Geological Province: Gippsland Basin.||||||19-JAN-05
32298|Kingfish Formation|24407|5|Briefly described|p13 Fig.2|||Geological Province: Gippsland Basin||||||
32298|Kingfish Formation|24495|5|Briefly described|p10|||Of Halibut Subgroup.  Geological Province: Gippsland Basin.||||||
32298|Kingfish Formation|24551|5|Briefly described|p262 Fig. 9.29|Eocene|Paleocene|Of the Halibut Subgroup.||||||
32298|Kingfish Formation|61469|5|Briefly described|p33|||Of the Latrobe Group.  Its sandstones are the main producing oil and gas reservoir in the basin. Geological Province: Gippsland Basin.||||||27-MAY-06
32298|Kingfish Formation|61552|4|Described|p581, p583 Fig.2, p585, pp589-592.  |Early Eocene|Paleocene|Deposited in lower coastal plain environments. This unit is the lateral, seaward equivalent of the Barracouta Formation. More shaly and coal facies to the west; sandier in the east where it grades into the Mackerel Formation.||Of the Halibut Subgroup. |Includes Grunter Member.|Overlies Volador Formation and Kate Shale. Interfingers with the Barracouta Formation to the west.|Includes coal.|
32298|Kingfish Formation|64876|5|Briefly described|p145 Fig.2|Eocene|Paleocene|Gippsland Basin.||Halibut Subgroup.||||
32298|Kingfish Formation|65717|5|Briefly described|p9 Fig.2.2, p11, p13, p28|Eocene|Paleocene|Comprises typical lower coastal plain coal-rich sediments.||Halibut Subgroup|Grunter Member.|Overlies Kate Shale and Volador Formation. Interbedded with Stonefish Sandstone Member (Barracouta Formation). Is overlain unconformably by Burong, Gurnard and Opah Formations.|Interbedded sandstone, siltstone and coal.|05-SEP-17
32298|Kingfish Formation|65718|6|Mentioned|p10 Fig 3.2, p12|Eocene|Maastrichtian|Early Eocene minimum age.||||||
32298|Kingfish Formation|65973|4|Described|p16, p22, p25, p29-30, p38, p57|Paleocene|Paleocene|Gippsland Basin. Comprises typical lower coastal plain coal-rich sediments. Forms a good quality reservoir at the top Latrobe Group level. At least 27m thick in Northright 1 well. Intersected in Leatherjacket-1, Kipper-2, Kipper-1, Judith-1, Hammerhead-1, East Pilchard-1, Longtom-1, Longtom-1/ST-1, Longtom-2/ST-1, Northright-1, Sole-1, Sweep-1 and many more drillholes (see appendix). See also p62, p65, p71, p74, p76, p78, p80-82, p86, p90, p97, p100, p104, p106, p110-112, p114, p116, p123-135, p137-138, p140-141, p143.||Halibut Subgroup||Overlies the Kate Shale.||
32298|Kingfish Formation|70028|6|Mentioned|p79|Eocene|Paleocene|Offshore Gippsland Basin.||||||
32298|Kingfish Formation|70076|5|Briefly described|South-Eastern: Fig.2; Regional: Fig.3;p3|Ypresian|Danian|Lower coastal plain, coal-rich sediments.||Halibut Subgroup.|Heart and Grunter Members.|Overlies Kate Shale, Volador or Barracouta Formation. Is overlain by Burong, Gurnard or Flounder Formation.||
32298|Kingfish Formation|73471|5|Briefly described|p86|||Gippsland Basin.||Halibut Subgroup||Overlies Kate Shale|Fluvial-deltaic and paralic sandstones and siltstones with interbedded coal layers.|
32298|Kingfish Formation|75065|5|Briefly described|p151, 154|Eocene|Paleocene|Gippsland Basin; offshore. Fluvial-deltaic and paralic sediments.||Halibut Subgroup.||Overlies Kate Shale and Volador Formation. Abuts Barracouta and Mackerel Formations. Is overlain unconformably by Burong Formation (Cobia Subgroup).|Sandstone, siltstone, coal.|
39633|Kingsley's Formation|24088|5|Briefly described|p355 Fig. 4|||Geological Province: Lachlan Fold Belt.||||||
32308|Kipper Shale|13323|5|Briefly described|p391, p393 Fig. 2|Turonian|Turonian|Of Emperor Subgroup. Thick succession of shallow to deep-water lacustrine sediments - shales and siltstones sands. Interfingers with and overlain by Curlip Formation. Thickness: <596m. Geological Province: Gippsland Basin.||||||
32308|Kipper Shale|13324|5|Briefly described|p94|||Mud-dominated lacustrine sediments in the basin centre.||?Of Emperor Subgroup||||
32308|Kipper Shale|22663|6|Mentioned|V97 - G1 to G4 p7|||||||||
32308|Kipper Shale|24090|5|Briefly described|p8 Fig.3|Cretaceous|Cretaceous|Geological Province: Gippsland Basin.||||||
32308|Kipper Shale|24407|5|Briefly described|p13 Fig.2|||Geological Province: Gippsland Basin||||||
32308|Kipper Shale|24495|5|Briefly described|p9|||Lacustrine deposits.  Geological Province: Gippsland Basin.||||||
32308|Kipper Shale|61552|6|Mentioned|p583 Fig.2. |Late Cretaceous|Late Cretaceous|||Unit in Emperor Subgroup.||||
32308|Kipper Shale|61553|6|Mentioned|p607.|||Chronostratigraphic equivalent of Durroon Formation (Bass Basin).||||||
32308|Kipper Shale|64876|5|Briefly described|p145 Fig.2|Turonian|Turonian|Gippsland Basin.||Emperor Subgroup.||||
32308|Kipper Shale|65717|5|Briefly described|p9 Fig.2.2, p10, p14|Turonian|Cenomanian|Lowry and Longley (1991). Gippsland Basin. Over 500m thick.  Represents shallow to deep water lacustrine deposition with lakes receiving detrital sediments from basin margins. Widespread distribution. An excellent intra-formational seal.||Emperor Subgroup||Conformably overlain by, and interfingers with, Curlip Formation|Dominated by mudstones intercalated with fine- to medium-grained sandstones.|05-SEP-17
32308|Kipper Shale|65718|5|Briefly described|p10 Fig 3.2, p11|Turonian|Turonian|Lowry and Longley (1991).||Of the Emperor Subgroup.||Overlain by and interfingered with the Curlip Formation.|Dominated by mudstones and intercalated fine- to medium-grained sandstones.|
32308|Kipper Shale|65973|4|Described|p14-15, p21, p28, p38, p44, p46, p57|Santonian|Turonian|Gippsland Basin. Interpreted to have been deposited in a lacustrine environment. Has excellent oil and gas seal potential. Exceeds thicknesses of 500m. Palynological zones are provided. Intersected in numerous drillholes including Kipper-1,  Hammerhead-1, Longtom-1, Longtom-1/ST-1, Longtom-2/ST-1, Shark-1. See also p80, p82-83, p86, p97-98, p100, p108, p123, p128-130, p133-134, p139, p171.||Emperor Subgroup.||Overlain by and interfingers with the Curlip Formation. Overlies the Admiral Formation.|Mudstones intercalated with fine- to medium-grained sandstones.|
32308|Kipper Shale|70028|6|Mentioned|p79|Turonian|Turonian|Offshore Gippsland Basin.||||||
32308|Kipper Shale|70076|5|Briefly described|South-Eastern: Fig.2; p2-3|Coniacian|Turonian|See also Regional: Fig.3; p2, p6-7. Lacustrine; hydrocarbon source rocks and an excellent seal. Generation is a critical risk due to thermal immaturity. Over 500m, up to 1000m, thick. Also appears as Kipper Formation on South-Eastern p2.||Emperor Subgroup.||Locally overlies Kersop Arkose. Is overlain by Chimaera Formation, as well as the Curlip Formation with which it also interfingers.|Includes carbonaceous shales (unproven in release area).|
32308|Kipper Shale|73471|5|Briefly described|p86-87, p90, p100, p102-104|||Gippsland Basin. Underlies Longtom Unconformity.||Emperor Subgroup, lower part|||Lacustrine shales.|
32308|Kipper Shale|75065|5|Briefly described|p151, 154, 161-162|Turonian|Albian|Gippsland Basin; offshore. The Kipper Volcanics mentioned on p164 refers to the Campanian Volcanics, another unit in the Golden Beach Subgroup.||Emperor Subgroup.||Overlies Admiral Formation conformably and Korumburra Subgroup (Strzelecki Group) unconformably. Is overlain by Curlip Formation. Is adjacent to Kipper Shale.|Non-marine / lacustrine shale.|
77295|Kirribilly Sandstone|65715|4|Described|p5, p30 Figs.3-4|Devonian|Silurian|Newly defined. Of Kerrie Group. Interfingers Goat Rocks Conglomerate. Incorrectly(?) called Kirribilly Formation in Tb.3. Type locality: series of cuttings on Kirribilly Road, Barringo (MGA ref given). Desc at type locality is thin-bedded siltstone and sandstone (now hornfels) with occasional soft-sediment deformation structures and low-angle small-scale bedding truncations. Sedimentary structures suggest reworking by storm waves, probably in a lacustrine setting||||||02-FEB-15
32495|Knowsley East Shale|22885|5|Briefly described|map|Late Cambrian|Middle Cambrian|||||||
32495|Knowsley East Shale|23309|5|Briefly described|p38, 42-46. Tb 2.13||Cambrian|||||||
32495|Knowsley East Shale|24177|4|Described|p42, p61|Middle Cambrian|Middle Cambrian|Overlain by Castlemaine Group where Goldie Chert is missing. Overlies the Mount William Metabasalt.||||||26-JUN-13
32495|Knowsley East Shale|24328|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|||||||
32495|Knowsley East Shale|24551|4|Described|p86|Middle Cambrian|Middle Cambrian|Formerly called Monegeetta Shale. Confomably overlain by Goldie Chert. Overlies Mount William Metabasalt. Includes the former Knowsley East beds, part of Goldie Beds and Goldie Shale. Doesn't included Goldie Chert at Lancefield.  ||||||
32495|Knowsley East Shale|44197|5|Briefly described|Map Legend||Cambrian|||||||
32495|Knowsley East Shale|60591|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Overlain by the Castlemaine Supergroup. Overlies the Mount William Metabasalt. Deep water hemipelagic sediments: shale, mudstone, minor interbedded mafic volcanic sandstone; slump deposits: monomictic chert breccia and polymictic conglomerate.||||||
32495|Knowsley East Shale|60592|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Overlain by the Castlemaine Supergroup. Overlies the Mount William Metabasalt. Deep water hemipelagic sediments: shale, mudstone, minor interbedded mafic volcanic sandstone; slump deposits: monomictic chert breccia and polymictic conglomerate.||||||25-NOV-04
32495|Knowsley East Shale|60593|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Overlain by the Castlemaine Supergroup. Overlies the Mount William Metabasalt. Deep water hemipelagic sediments: shale, mudstone, minor interbedded mafic volcanic sandstone; slump deposits: monomictic chert breccia and polymictic conglomerate.||||||
32495|Knowsley East Shale|60595|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Overlain by the Castlemaine Supergroup. Overlies the Mount William Metabasalt. Deep water hemipelagic sediments: shale, mudstone, minor interbedded mafic volcanic sandstone; slump deposits: monomictic chert breccia and polymictic conglomerate.||||||
32495|Knowsley East Shale|60596|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Overlain by the Castlemaine Supergroup. Overlies the Mount William Metabasalt. Deep water hemipelagic sediments: shale, mudstone, minor interbedded mafic volcanic sandstone; slump deposits: monomictic chert breccia and polymictic conglomerate.||||||
32495|Knowsley East Shale|60597|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Shale, mudstone, minor mafic volcanic sandstone: weakly magnetic; low K, Th and U.||||||
32495|Knowsley East Shale|60599|3|Fully described|p19, p24 Tb. 4, p40-41, p83|Middle Cambrian|Middle Cambrian|Supersedes Knowsley East beds/ "Dinesus-Hydroid Beds" and Goldie beds of Thomas (1956).NOTE:Goldie Chert at KILMORE is NOT included - instead it overlies/interfingers with Knowsley East Shale. Black shale, chert+ volcaniclastic units. Detailed litholog. ||||||
32495|Knowsley East Shale|62742|5|Briefly described|p697|Cambrian|Cambrian|Contains rare Botoman (ca 518-513Ma) trilobites. Conformably overlies Magdala Basalt. In the Heathcote Greenstone Belt.||||||
32495|Knowsley East Shale|62744|5|Briefly described|p709 Fig. 2|Cambrian|Cambrian|Geological Province: Heathcote Greenstone Belt.||||||
32495|Knowsley East Shale|64611|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Shale, mudstone, sandstone and minor chert: thinly bedded black shale and mudstone predominate, minor chert and laminated to thick bedded mafic volcanic sandstone; slump deposits common, sparsely fossiliferous; deep marine hemipelagic and turbidite deposit||||||26-JUN-13
32495|Knowsley East Shale|64612|2|Defined|p26, p33, p53, p57, p65, p73|Late Cambrian|Middle Cambrian|Underlain conformably by Mount William Metabasalt, conformably overlain by Goldie Chert, Heathcote Volcanic Group. Thickness: 100m. Finely laminated silicified black shale, commonly bleached to pale grey colours. Deep marine setting.||||||26-JUN-13
32495|Knowsley East Shale|65715|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Contains an unnamed conglomerate member. Formation rank.||||||
32495|Knowsley East Shale|65969|5|Briefly described|p3, p11, p13, p17 Fig.7|Cambrian|Cambrian|Mapped as conformably overlying Mount William Metabasalt, but contact may be faulted instead. Overlain by Goldie Chert. Correlated with Albion Formation by Squire and Wilson (2005). Thin unit of mafic volcaniclastic and hemipelagic sediments.||||||
32495|Knowsley East Shale|66196|6|Mentioned|p617||Early Cambrian|Overlies the Heathcote Volcanics. Contains trilobite fauna of late Early Cambrian age. See also Knowsley East Formation.||||||
32495|Knowsley East Shale|66769|6|Mentioned|118-119, 132, 141|||Conformably underlies the Goldie Chert. Thin, deep-ocean sedimentary rock. Overlies Heathcote Volcanic Group. Mechanically weak; candidate for a regional-scale detachment horizon.||||||
32495|Knowsley East Shale|68116|5|Briefly described|Appendix, Maps 17, 23, 32.|Late Cambrian|Middle Cambrian|Shale sparsely fossiliferous with trilobites, phosphatic brachiopods and hydroids. Chert derived from mafic igneous rocks. Chert laminated to thickly bedded|||||Shale, mudstone, sandstone, conglomerate, slump deposits: black shale and mudstone predominant, thinly bedded; minor chert; sandstone thin to thick-bedded, turbiditic; conglomerates monomictic with chert breccia or polymictic.|
32495|Knowsley East Shale|68314|5|Briefly described|p754-755|Early Cambrian|Early Cambrian|Heathcote Greenstone Belt. Age from Botoman trilobites. Shows remarkably similar sedimentary facies, age and stratigraphic relationships to the Albion Formation.|c.418-413 Ma.|||Conformably overlies Mount William Metabasalt.|Black mudstones.|
32495|Knowsley East Shale|69089|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian||||||Marine: shale, volcaniclastic sandstone.|
32495|Knowsley East Shale|69573|6|Mentioned|p656-657, 659, 670|||Features Cambrian Stage 5 fossil sites.||||||
32495|Knowsley East Shale|70601|5|Briefly described|p44, p47|Early Ordovician|Cambrian|Contains Ordian to basal Templetonian (ca 508 Ma) and Undillian (ca 503-501 Ma) trilobites (Jell, 2014). Overlies Heathcote Volcanics which are older than Eagles Peak Basalt.|503 +/- 8 Ma.|||Underlies Goldie Chert. Overlies Mount William Metabasalt.|Shale with trilobites.|
32495|Knowsley East Shale|73497|5|Briefly described|Map legend|Cambrian|Cambrian|Marine.||||Underlies Goldie Chert|Shale, siltstone, chert, conglomerate, volcanic sandstone: generally weakly magnetic, but some highly magnetic features either in the sandstone or from andesite at depth; low K, Th and U.|
32495|Knowsley East Shale|73505|5|Briefly described|p5|Middle Cambrian|Middle Cambrian|||||Conformably overlies Dja Dja Wrung Supergroup along the Mount William Fault||
35515|Koala Creek Formation|23309|5|Briefly described|p147-149. Tb 2.56|||||||||
35515|Koala Creek Formation|24551|4|Described|p123, p125|||Of the Cathedral Group.||||||
35515|Koala Creek Formation|24588|5|Briefly described|p12 Fig.3|Eifelian|Eifelian|Geological Province: Mount Easton Province. Creek is Ck in text. Of the Cathedral Group.||||||29-NOV-13
9701|Koetong Granite|22508|5|Briefly described|p2||Silurian|Keotong Supersuite, Lachlan Fold Belt||||||
9701|Koetong Granite|22968|6|Mentioned|P19|||||||||
9701|Koetong Granite|23309|5|Briefly described|p296, 298, 343, 346, 350.||Late Silurian|G101 S-Type. Age: 421 Ma, 418+/-4 Ma, 419+/- 6 Ma. Supersedes Koetong Granodiorite.||||||
9701|Koetong Granite|23547|5|Briefly described|p554|||||||||
9701|Koetong Granite|24133|3|Fully described|p62|Silurian|Silurian|Age: 419+/-6Ma (U-Pb); 418+/-4Ma (Rb-Sr).   Geological Province: Lachlan Fold Belt.||||||
9701|Koetong Granite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
9701|Koetong Granite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
9701|Koetong Granite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
9701|Koetong Granite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Two mica cordierite granite: bluish grey, coarse grained biotite muscovite granite; mostly equigranular but centre is porphyritic & parts of margins are fine grained; locally abundant enclaves; S-type; nonmagnetic||||||09-SEP-04
9701|Koetong Granite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Age: 419 +/- 6 Ma (U/Pb), 418 +/- 4 Ma (Rb/Sr). Biotite-muscovite-cordierite-granite: S-type; nonmagnetic; variable K, moderate-low Th, variable U||||||09-SEP-04
9701|Koetong Granite|24438|6|Mentioned|p14|||Radiometric response false anomaly is probably due to pine tree plantations.||||||10-JUN-14
9701|Koetong Granite|24551|6|Mentioned|p232 Fig. 8.17|||||||||
9701|Koetong Granite|29953|4|Described|p3|||||||||
9701|Koetong Granite|31800|6|Mentioned|p203|||||||||
9701|Koetong Granite|32684|6|Mentioned|p250|||See also Fig.2||||||
9701|Koetong Granite|35257|6|Mentioned|p11|||See also P154.||||||
9701|Koetong Granite|35278|4|Described|p358|||||||||
9701|Koetong Granite|37871|4|Described|p8|||||||||
9701|Koetong Granite|38335|6|Mentioned|p1728|||||||||
9701|Koetong Granite|39858|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
9701|Koetong Granite|39860|6|Mentioned|p17|||See also P42||||||
9701|Koetong Granite|40328|6|Mentioned|p204|||||||||
9701|Koetong Granite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
9701|Koetong Granite|40498|6|Mentioned|p392|||||||||
9701|Koetong Granite|40761|6|Mentioned|p242|||||||||
9701|Koetong Granite|41433|6|Mentioned|Fig.3|||||||||
9701|Koetong Granite|41572|6|Mentioned|p19|||||||||
9701|Koetong Granite|41868|6|Mentioned|p586|||||||||
9701|Koetong Granite|42089|6|Mentioned|p16|||||||||
9701|Koetong Granite|42726|5|Briefly described|map legend|Silurian||||||||
9701|Koetong Granite|42827|5|Briefly described|p586|||||||||
9701|Koetong Granite|64571|6|Mentioned|p825|Early Silurian|Early Silurian|||||||
9701|Koetong Granite|68116|5|Briefly described|Appendix, Map 20.|Lochkovian|Ludlow||||||Two-mica cordierite granite: bluish grey, coarse grained biotite muscovite granite; mostly equigranular but centre is porphyritic and parts of margins are fine grained; locally abundant metasedimentary enclaves; S-type; nonmagnetic.|
9701|Koetong Granite|68310|6|Mentioned|p241-242|||Wagga Batholith. Geochemical plots of schistose enclaves.|||||S-type granite.|
9701|Koetong Granite|70910|14|Not recorded|p43|||Gneissic granite.||||||
9701|Koetong Granite|73264|6|Mentioned|p1392|||S-type granite.||||||
9703|Koetong Suite|22778|5|Briefly described|p 159|||||||||
9703|Koetong Suite|23439|5|Briefly described|p124 fig.1|||||||||
9703|Koetong Suite|23549|5|Briefly described|p523.|||The major component of the Koetong Supersuite. S-type granite. Geological Province:  Wagga Batholith in the Lachlan Fold Belt.||||||05-APR-05
9703|Koetong Suite|23550|5|Briefly described|p502|||S-type granite. Lachlan Fold Belt.||||||
9703|Koetong Suite|23551|6|Mentioned|p491|||||||||
9703|Koetong Suite|24514|5|Briefly described|p29|||Felsic S-type granites.||||||
9703|Koetong Suite|24551|6|Mentioned|p233|||||||||
9703|Koetong Suite|41898|6|Mentioned|p1182|||||||||
9703|Koetong Suite|42726|5|Briefly described|map legend||Silurian|||||||
9703|Koetong Suite|42827|6|Mentioned|p432|||||||||
9703|Koetong Suite|44093|5|Briefly described|p170 App. 1|Late Silurian|Silurian|Max age: Middle Silurian. In the Wagga-Omeo Zone. Geological Province: Lachlan Fold Belt.||||||
9703|Koetong Suite|61964|3|Fully described|p14 Fig. 4, p37|Middle Silurian|Early Silurian|Of Koetong Supersuite.Incorporates former "Ungarie Suite (mafic) + felsic "Kikoira Suite" (Chappell et al 1991). Now includes; Erigolia, Eura Bonny, Weethalle, Kikoira, Yalgongrin + Ungarie Granites + Cookaburragong Granodiorite. Lith.details included||||||
9703|Koetong Suite|62405|5|Briefly described|Map legend|Silurian|Silurian|Includes: Ugalong Dacite, Cookaburragong Granodiorite, Erigolia, Eura Bonny, Weethalle, Yalgogrin, Ungarie (and its Derrida Phase) and Kikoira Granites.||||||26-MAR-08
9703|Koetong Suite|63290|6|Mentioned|p399|Early Silurian|Early Silurian|Age: ca 432Ma (Colquhoun et al. 2005). Granites.||||||
9703|Koetong Suite|64568|5|Briefly described|Map legend|Silurian|Silurian|Includes Ungarie Granite, Cookaburragong Granodiorite, Kinoira Granite and Ugalong Dacite.||||||
9703|Koetong Suite|65469|5|Briefly described|p15, p18|Middle Silurian|Early Silurian|Lachlan Orogen.|432 Ma (Colquhoun et al., 2005)||Includes the Thule Granite, Ungarie Granite, Ugalong Dacite, Cookaburragong Granodiorite and Kikoira Granite. |Intrudes the Wagga Group. ||
9703|Koetong Suite|67060|5|Briefly described|p503, p505 Table 1.|||Of the Wagga Batholith. S-type.  Includes Wantabagdery/Wantabadgery,  Mount Flakney, Granya plutons.|435.8 +/- 4.4 to 432.3 +/- 4.3 Ma.||||Ranges from granodiorite rich in mafic minerals to highly-fractionated Sn-mineralised leucogranites.|13-JUN-13
9703|Koetong Suite|69160|5|Briefly described|Map legend|Early Silurian|Early Silurian||||Includes Ugalong, Eura Bonny, Weethalle, Yalgogrin, Ungarie and Kikoira Granites.|||
9703|Koetong Suite|69161|5|Briefly described|Map legend|Silurian|Silurian||||Includes Erigolia and Kikoira Granites.|||
9703|Koetong Suite|69801|6|Mentioned|p32, p85, p91, p122, p135|||Central Lachlan Orogen. Incorporates the Grong Grong Granite of the former Grong Grong Suite.||Koetong Supersuite|Includes the Woomargama Granite, the Grong Grong Granite and the Granya Granite.|||
9703|Koetong Suite|70777|6|Mentioned|p39, p52-p53, p79|||||Koetong Supersuite||||
9703|Koetong Suite|71039|6|Mentioned|p6|Silurian|Silurian|||||||
9703|Koetong Suite|71069|6|Mentioned|p75|||||||||
9704|Koetong Supersuite|22508|5|Briefly described|p2||Silurian|Lachlan Fold Belt||||||
9704|Koetong Supersuite|22606|6|Mentioned|P830|||||||||
9704|Koetong Supersuite|23309|5|Briefly described|p346|||Comprises of Corryong Granite (G92) and Mount Willis Granite (G111).||||||
9704|Koetong Supersuite|23547|5|Briefly described|p554|||||||||
9704|Koetong Supersuite|23549|4|Described|Fig 2 p517, p523|||S-Type granites within the Wagga Batholith. The major component is the Koetong Suite.  Geological Province: Lachlan Fold Belt.||||||05-APR-05
9704|Koetong Supersuite|24133|6|Mentioned|p57|||Geological Province: Lachlan Fold Belt.||||||
9704|Koetong Supersuite|24222|5|Briefly described|p4|||S-type.  See also Koetong supersuite.   Geological Province: Lachlan Fold Belt.||||||24-JAN-06
9704|Koetong Supersuite|24263|6|Mentioned|p1394|||Geological Province: Wagga Belt||||||
9704|Koetong Supersuite|24270|6|Mentioned|p1608|||Geological Province: Wagga tin belt.||||||
9704|Koetong Supersuite|24271|6|Mentioned|p1621|||Geological Province: Lachlan Fold Belt.||||||
9704|Koetong Supersuite|24512|6|Mentioned|p5|||Geological Province: Lachlan Orogen.||||||
9704|Koetong Supersuite|41563|6|Mentioned|p514|||||||||
9704|Koetong Supersuite|42726|5|Briefly described|map legend|||||||||
9704|Koetong Supersuite|61964|4|Described|p14 Fig. 4, p37|Middle Silurian|Early Silurian| Well-defined group of high-K, peraluminous, S-type granites extending from northern Victoria to Cargelligo area.  Age: c.432Ma.  For geophysics of suite - see p222||||||
9704|Koetong Supersuite|62367|5|Briefly described|p10|Early Silurian|Early Silurian|Includes the Ungarie Granite. Fractionated S-type granites.||||||31-MAY-06
9704|Koetong Supersuite|65469|6|Mentioned|p16, p17|||Lachlan Orogen.||||||
9704|Koetong Supersuite|69043|5|Briefly described|p1, p24, p28, p30, p34, p44|Silurian|Silurian|Indistinguishable age from that of the Mine Granite (this study) of 428.1 +/- 2.8 Ma.|c.433-c.427 Ma (Black,2005; Colquhoun et al.,2005)||Kyeamba Suite; Mine Granite.||S-type.|
9704|Koetong Supersuite|69511|6|Mentioned|p1-2|Silurian|Silurian||c.427 Ma.|||||
9704|Koetong Supersuite|69798|6|Mentioned|p6|||||||||
9704|Koetong Supersuite|69801|6|Mentioned|p1-p2, p18, p39, p85, p91, p135-137|||Central Lachlan Orogen.|||Includes the Koetong Suite and the Tom Groggin Suite.|Intruded by the Holbrook Granite.||
9704|Koetong Supersuite|70296|6|Mentioned|p1, p10|Llandovery|Llandovery||||Includes the Kikoira Granite, Yalgogrin Granite and the Erigolia Granite.|||
9704|Koetong Supersuite|70777|5|Briefly described|p1, p39, p52, p79-p80|||Lachlan Orogen.|||Includes the Koetong Suite, Yalgogrin Granite, Wargin Granite, Ungarie Granite and the Buddigower Granite.|||
9704|Koetong Supersuite|71039|6|Mentioned|p6|Silurian|Silurian|||||||
9704|Koetong Supersuite|71345|6|Mentioned|p26|||Occurs to the south of the Wilgaroon Granite.|||||S-type granitic rocks.|
9704|Koetong Supersuite|71693|5|Briefly described|Map legend.|Silurian|Silurian||||Ungarie, Currah, Yalgogrin, Weethalle, Eura Bonny, Nyora, Erigolia, Kikoira Granites; Ugalong Dacite. ||Coarse- to medium-grained equigranular to porphyritic biotite +/- cordierite and muscovite granite and granodiorite with locally abundant metasedimentary xenoliths. Felsic fractionated members usually tourmaline-bearing.|
9747|Konagaderra shaley flysch|33020|5|Briefly described|p241|||Early Llandovery. Lith. & palaeocurrent direction anal.||||||
9761|Konkon Sandstone|41715|4|Described|p318|||||||||
37755|Konong Wootong Granodiorite|23309|6|Mentioned|p435, Appendix 1|||G420, I-Type.||||||
37755|Konong Wootong Granodiorite|63446|5|Briefly described|Map legend|Early Devonian|Early Devonian|No lithology given: is listed as Konong Wootong. G420.|||||I-type granite.|12-JUN-15
37254|Koolomurt Granodiorite|23309|5|Briefly described|p337|||G426, I-Type.||||||
37254|Koolomurt Granodiorite|24012|3|Fully described|p223 appendix 1|Ordovician|Cambrian|Intrudes Glendara Adamellite||||||
37254|Koolomurt Granodiorite|24551|5|Briefly described|p77|||Of the Glenelg River Complex||||||
37254|Koolomurt Granodiorite|50154|2|Defined|p104-105|Ordovician|Ordovician|||||||15-SEP-04
37254|Koolomurt Granodiorite|50155|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite granodiorite; I-type||||||
37254|Koolomurt Granodiorite|50156|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite granodiorite: massive, greenish-grey, medium to coarse grained, equigranular; accessory magnetite, sphene and allanite; sporadic mafic biotite-hornblende-rich mafic microgranitoid enclaves.||||||
37254|Koolomurt Granodiorite|50157|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite granodiorite: massive, greenish-grey, medium to coarse grained, equigranular; accessory magnetite, sphene and allanite; sporadic mafic biotite-hornblende-rich mafic microgranitoid enclaves.||||||
37254|Koolomurt Granodiorite|50158|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite granodiorite: massive, greenish-grey, medium to coarse grained, equigranular; accessory magnetite, sphene and allanite; sporadic mafic biotite-hornblende-rich mafic microgranitoid enclaves.||||||
37254|Koolomurt Granodiorite|50159|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite granodiorite: massive, greenish-grey, medium to coarse grained, equigranular; accessory magnetite, sphene and allanite; sporadic mafic biotite-hornblende-rich mafic microgranitoid enclaves.||||||24-JUN-04
37254|Koolomurt Granodiorite|50160|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite granodiorite||||||
37254|Koolomurt Granodiorite|50161|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite granodiorite: massive, greenish-grey, medium to coarse grained, equigranular; accessory magnetite, sphene and allanite; sporadic mafic biotite-hornblende-rich mafic microgranitoid enclaves.||||||24-JUN-04
37254|Koolomurt Granodiorite|50162|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite granodiorite: massive, greenish-grey, medium to coarse grained, equigranular; accessory magnetite, sphene and allanite; sporadic mafic biotite-hornblende-rich mafic microgranitoid enclaves.||||||24-JUN-04
37254|Koolomurt Granodiorite|50163|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite granodiorite: massive, greenish-grey, medium to coarse grained, equigranular; accessory magnetite, sphene and allanite; sporadic mafic biotite-hornblende-rich mafic microgranitoid enclaves.||||||24-JUN-04
37254|Koolomurt Granodiorite|50164|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Biotite granodiorite; I-type||||||
37254|Koolomurt Granodiorite|66002|6|Mentioned|p8 Tb.5|||G426.Defined by Kemp et al. 2002||||||
37254|Koolomurt Granodiorite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Late Cambrian||||||Biotite granodiorite: massive, greenish-grey, medium to coarse grained, equigranular; accessory magnetite, sphene and allanite; sporadic mafic biotite-hornblende-rich mafic microgranitoid enclaves; magnetic.|
32560|Koomberar Formation|22968|3|Fully described|P31, Fig32, P116|Silurian|Silurian|Type section location given on P117, parent is Barmouth Group||||||
32560|Koomberar Formation|23020|5|Briefly described|Map legend|Pridoli|Pridoli|Parent is Barmouth Group||||||
32560|Koomberar Formation|23309|5|Briefly described|p90, 92, 96. Tb 2.33|||||||||
32560|Koomberar Formation|24551|4|Described|p137|Silurian|Silurian|Of Barmouth Group||||||
32560|Koomberar Formation|68116|5|Briefly described|Appendix, Map 35.|Silurian|Silurian||||||Sandstone, conglomerate: sandstone thick to thin-bedded, sandstone and conglomerate both volcanilithic with mafic and lesser rhyolitic rock fragments; minor mudstone; possible rhyolite lava.|
9790|Koonalunda Lens|35066|5|Briefly described|p211|||||||||
9790|Koonalunda Lens|42827|5|Briefly described|p285|||||||||
9798|Koonwarra Fossil Bed|24453|5|Briefly described|p811|Albian|Barremian|Lower "Wonthaggi Formation". Contains significant macrofossils. Geological Province: Gippsland Basin.||||||07-FEB-11
9798|Koonwarra Fossil Bed|41426|6|Mentioned|p1|||||||||
9798|Koonwarra Fossil Bed|41427|5|Briefly described|p79|||||||||
9798|Koonwarra Fossil Bed|42673|6|Mentioned|p194|||||||||
9798|Koonwarra Fossil Bed|60726|5|Briefly described|p1-4, p8, throughout text.|Aptian|Aptian|Tarwin area, South Gippsland. Contains fish, insect, bird, plant fossils.|116+/-5 Ma (fission track: Drinnan and Chambers).|Korumburra Group (=Strzelecki Group).|||Varved lake deposits.|
9798|Koonwarra Fossil Bed|63124|5|Briefly described|p72|||Of the Korumburra Group. Contains fossil remnants of birds (feathers), tortoises, fish, crustaceans, insects, worms, bivalves and plants. Geological Province: Gippsland Basin.||||||
77724|Kooreelah Diorite|66002|5|Briefly described|p8 Tb.5|||Of Caupaul Igneous Complex. G428. Defined by Morand et al. 2003.||||||
41184|Kooreelah Gabbro-Diorite|50154|2|Defined|p81-82, p248 App.5|Cambrian|Cambrian|Of the Caupaul Igneous Complex. Includes two small intrusions of diorite-gabbro referred to by Ferguson (1993) as the Caupaul Monzonite and gabbro-pyroxenite intrusions were referred to as Kooreelah Gabbro by Ferguson (1993).||||||15-SEP-04
41184|Kooreelah Gabbro-Diorite|50156|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Caupaul Igneous Complex (Glenelg River Metamorphic Complex). Quartz diorite to quartz monzodiorite and gabbro-pyroxenite||||||20-AUG-04
41184|Kooreelah Gabbro-Diorite|50157|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Caupaul Igneous Complex (Glenelg River Metamorphic Complex). Quartz diorite to quartz monzodiorite and gabbro-pyroxenite||||||20-AUG-04
41184|Kooreelah Gabbro-Diorite|50158|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Caupaul Igneous Complex (Glenelg River Metamorphic Complex). Quartz diorite to quartz monzodiorite and gabbro-pyroxenite||||||20-AUG-04
41184|Kooreelah Gabbro-Diorite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Caupaul Igneous Complex (Glenelg River Metamorphic Complex). Quartz diorite to quartz monzodiorite and gabbro-pyroxenite||||||20-AUG-04
41184|Kooreelah Gabbro-Diorite|50160|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Caupaul Igneous Complex (Glenelg River Metamorphic Complex). Quartz diorite to quartz monzodiorite and gabbro-pyroxenite||||||20-AUG-04
41184|Kooreelah Gabbro-Diorite|50161|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Caupaul Igneous Complex (Glenelg River Metamorphic Complex). Quartz diorite to quartz monzodiorite and gabbro-pyroxenite||||||20-AUG-04
41184|Kooreelah Gabbro-Diorite|50162|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Caupaul Igneous Complex (Glenelg River Metamorphic Complex). Quartz diorite to quartz monzodiorite and gabbro-pyroxenite||||||20-AUG-04
41184|Kooreelah Gabbro-Diorite|50163|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Caupaul Igneous Complex (Glenelg River Metamorphic Complex). Quartz diorite to quartz monzodiorite and gabbro-pyroxenite||||||20-AUG-04
41184|Kooreelah Gabbro-Diorite|50164|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Of Caupaul Igneous Complex. G428 Quartz diorite to quartz monzodiorite: highly magnetic; gravity high; high K, moderate Th, low U. G428a gabbro-pyroxenite: weakly to moderately magnetic; low to moderate K, low Th, U||||||13-SEP-04
41184|Kooreelah Gabbro-Diorite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Quartz diorite to quartz monzodiorite: massive, dark grey-brown, medium-grained, equigranular containing plagioclase, biotite, clinopyroxene, orthopyroxene and magnetite; magnetic.|
28137|Kooreh Granite|23165|5|Briefly described|Map legend||Devonian|||||||
28137|Kooreh Granite|23166|5|Briefly described|Map legend||Devonian|of Mount Cole Suite.||||||
28137|Kooreh Granite|23167|5|Briefly described|Map legend||Devonian|of Mount Cole Suite. G357. Deeply weathered, non magnetic pluton.||||||27-OCT-04
28137|Kooreh Granite|23168|5|Briefly described|Map legend||Devonian|of Mount Cole Suite.||||||
28137|Kooreh Granite|23169|5|Briefly described|Map legend||Devonian|of Mount Cole Suite.||||||
28137|Kooreh Granite|23309|6|Mentioned|p435 App1|||G357 I-Type.||||||
28137|Kooreh Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
28137|Kooreh Granite|66002|5|Briefly described|p7 Tb.5|||Of Mount Cole Suite. G357. Defined by Krokowski de Vickerod et al 1997.||||||
28137|Kooreh Granite|68116|5|Briefly described|Appendix, Map 23.|Early Devonian|Early Devonian||||||Granite: non-magnetic; deeply weathered.|
9807|Kooyoora Granite|23260|6|Mentioned|p270|||||||||
9807|Kooyoora Granite|23309|6|Mentioned|p435 App 1|||G347 I-Type. Supersedes Kooyoora Adamellite.||||||
9807|Kooyoora Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
9807|Kooyoora Granite|65715|5|Briefly described|p8 Tb.4, p25 Fig.1a|||Of Mount Cole Suite. G347. Called Kooyara Adamellite by Marlow and Bushell (1995). Fig. 1a includes an aplitic phase of Kooyoora Granite.||||||
9807|Kooyoora Granite|68116|5|Briefly described|Appendix, Map 23.|Early Devonian|Early Devonian|Informally subdivided into an aplitic phase.|||||Biotite-hornblende-muscovite granite: mostly evenly coarse grained, locally porphyritic; mafic enclaves; pegmatite and aplite dykes; nonmagnetic. Contains an aplitic phase.|
9807|Kooyoora Granite|68189|6|Mentioned|p21, p23 Fig.11, p42 App.2|||Non-magnetic. K-Ar age from Bowen (1975) and McKenzie et al. (1984).|401 +/- 8 Ma.|||||30-JUN-14
9807|Kooyoora Granite|73576|6|Mentioned|p803 Fig.1|Devonian|Devonian|||||||
37756|Korong Creek Tonalite|23309|5|Briefly described|p435, Appendix 1|Devonian|Devonian|G322, I-Type.  Age: 394+/-6Ma,  389+/-6Ma.||||||
37756|Korong Creek Tonalite|60452|4|Described|p55-56|||Previously included with the Wedderburn Granodiorite. Porphyritic hornblende tonalite. Intrudes the Saint Arnaud Group.||||||
37756|Korong Creek Tonalite|60461|5|Briefly described|Map legend|Early Devonian|Early Devonian|Hornblende tonalite: porphyritic in plagioclase.||||||
37756|Korong Creek Tonalite|60462|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Tonalite: oxidised; magnetic response to 160 nT||||||
37756|Korong Creek Tonalite|65715|6|Mentioned|p8 Tb.4|||G322. Of Edwards et al (2001) p55.||||||
37756|Korong Creek Tonalite|68116|5|Briefly described|Appendix, Map 16.|Early Devonian|Early Devonian||||||Hornblende tonalite: porphyritic in plagioclase; magnetic.|
37756|Korong Creek Tonalite|68189|6|Mentioned|p42 App.2|||K-Ar ages from Richards & Singleton (1981).|394 +/- 6 and 389 +/- 6 Ma.|||||30-JUN-14
39833|Korumburra Subgroup|13323|5|Briefly described|p393 Fig. 2|Albian|Albian|Of th Strzelecki Group. Non-marine arkose and volcanoclastics. Overlies Tyers River Subgroup (Strzelecki Group). Geological Province: Gippsland Basin. See also p393 Fig. 3.||||||26-JUN-06
39833|Korumburra Subgroup|24407|5|Briefly described|p13 Fig.2|||Geological Province: Gippsland Basin||||||
39833|Korumburra Subgroup|24551|6|Mentioned|p478 Fig 15.8|||Of the Strzelecki Group.||||||
39833|Korumburra Subgroup|61552|6|Mentioned|p583 Fig.2. |Albian||||Unit in Strzelecki Group.||||
39833|Korumburra Subgroup|64876|5|Briefly described|p145 Fig.2|Albian||Gippsland Basin.||Strzelecki Group.||||
39833|Korumburra Subgroup|65717|5|Briefly described|p9 Fig.2.2|Albian|Albian|||Strzelecki Group|||Interbedded sandstone, siltstone and shale.|05-SEP-17
39833|Korumburra Subgroup|65973|6|Mentioned|p171|||Gippsland Basin.||||||
39833|Korumburra Subgroup|70076|5|Briefly described|South-Eastern: Fig.4|Albian|Barremian|||Strzelecki Group.|Wonthaggi Formation.|Is overlain by Emperor Subgroup (Latrobe Group).||
39833|Korumburra Subgroup|75065|5|Briefly described|p151, 156-159, 172|Albian|Barremian|Bernecker and Partridge (2001). Gippsland Basin. Good hydrocarbon potential reservoir.||Strzelecki Group.|San Remo Member.|Overlies Tyers River Subgroup unconformably (onshore) and conformably (offshore). Is overlain unconformably by Emperor Subgroup. Correlates with Eumeralla Subgroup. Equivalent to Wonthaggi Formation?.|Sandstone, non-marine arkose and volcaniclastics, some coal.|
9831|Kosciusko Granite|29860|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
9831|Kosciusko Granite|29953|6|Mentioned|p3|||||||||
9831|Kosciusko Granite|31800|6|Mentioned|p203|||||||||
9831|Kosciusko Granite|33606|5|Briefly described|p70|||||||||
9831|Kosciusko Granite|34367|6|Mentioned|p570|||Pebbles in moraine||||||
9831|Kosciusko Granite|34400|6|Mentioned|p7|||Associated with Bowning Orogeny.||||||
9831|Kosciusko Granite|36602|6|Mentioned|p115|||||||||
9831|Kosciusko Granite|38064|6|Mentioned|p39|||||||||
9831|Kosciusko Granite|43344|14|Not recorded|p8|||Associated with Bowning Orogeny||||||
9831|Kosciusko Granite|45087|6|Mentioned|p31|||Chemical analyses||||||
9831|Kosciusko Granite|60007|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Included in undifferentiated granites of the Kosciusko Batholith.||||||
9831|Kosciusko Granite|60085|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
9831|Kosciusko Granite|70910|14|Not recorded|p44|||Stratigraphic confirmation of K-Ar ages.||||||
25133|Kotupna Sands|35474|6|Mentioned|Table 3.2|||||||||
33131|Kout Norien Granodiorite|23309|5|Briefly described|p335.|Ordovician|Ordovician|G410 - S-Type. Age: 466+/-6 Ma, 487+/-6 Ma.||||||
33131|Kout Norien Granodiorite|23319|4|Described|p408 Fig. 1,  p411|Ordovician|Cambrian|Intruded by Tuloona Granodiorite. referred to as "Harrow Granodiorite" by Turner et al (1993).||||||07-FEB-07
33131|Kout Norien Granodiorite|50154|2|Defined|p91-92|Ordovician|Cambrian|Of the Glenelg River Metamorphic Complex. Intruded by Harrow Granodiorite, Schofield Granite and Tuloona Granodiorite. Intrusive age of 490-500 Ma.||||||15-SEP-04
33131|Kout Norien Granodiorite|50155|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Biotite-muscovite granodiorite; S-type||||||
33131|Kout Norien Granodiorite|50156|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granodiorite.||||||20-AUG-04
33131|Kout Norien Granodiorite|50157|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granodiorite.||||||20-AUG-04
33131|Kout Norien Granodiorite|50158|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granodiorite.||||||20-AUG-04
33131|Kout Norien Granodiorite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granodiorite.||||||20-AUG-04
33131|Kout Norien Granodiorite|50160|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granodiorite.||||||20-AUG-04
33131|Kout Norien Granodiorite|50161|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granodiorite.||||||20-AUG-04
33131|Kout Norien Granodiorite|50162|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granodiorite.||||||20-AUG-04
33131|Kout Norien Granodiorite|50163|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granodiorite.||||||20-AUG-04
33131|Kout Norien Granodiorite|66002|6|Mentioned|p8 Tb.5|||G410. Defined by Kemp and Gray 1999.||||||
33131|Kout Norien Granodiorite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Biotite-muscovite granodiorite: foliated, medium grained, porphyritic with phenocrysts of plagioclase and microcline; accessory sillimanite; common enclaves of schist and migmatite; foliation is defined by biotite-rich schlieren; non-magnetic.|
9844|Kow Sand|2967|5|Briefly described|p67-68|||Thorne and Macumber (1969). Kow Swamp, northern Victoria,|||||Wind-blown sand forming a low dune on the SE shoreline of Kow Swamp.|
9844|Kow Sand|31385|6|Mentioned|Table 5|||||||||
9844|Kow Sand|31954|4|Described|p10|||||||||
9844|Kow Sand|31957|4|Described|p312|||Mention P309||||||
9844|Kow Sand|32232|6|Mentioned|p19|||||||||
9844|Kow Sand|33486|6|Mentioned|p316|||||||||
9844|Kow Sand|42966|5|Briefly described|p407|||||||||
9854|Kuark Metamorphic Complex|22708|6|Mentioned|p210|||||||||
9854|Kuark Metamorphic Complex|22721|6|Mentioned|Fig.1 p502|||||||||
9854|Kuark Metamorphic Complex|22794|5|Briefly described|p65|||||||||
9854|Kuark Metamorphic Complex|22876|5|Briefly described|p14|||||||||
9854|Kuark Metamorphic Complex|22878|6|Mentioned|p8|||||||||
9854|Kuark Metamorphic Complex|22879|5|Briefly described|map|Silurian|Silurian|||||||
9854|Kuark Metamorphic Complex|22880|5|Briefly described|Map Legend|Silurian|Silurian|Includes: Ino Creek Granodiorite, Kanuka Granodiorite, Irondoon Granodiorite||||||01-OCT-04
9854|Kuark Metamorphic Complex|23309|5|Briefly described|p67-69, 312-313|||||||||
9854|Kuark Metamorphic Complex|23938|5|Briefly described|p31-32 Fig. 12|Middle Ordovician|Early Ordovician|See also p139 Tb. 1 Appendix.||||||09-DEC-08
9854|Kuark Metamorphic Complex|24004|6|Mentioned|p285 Fig.6|||||||||
9854|Kuark Metamorphic Complex|24310|5|Briefly described|p1044|||Geological Province: Lachlan Fold Belt||||||
9854|Kuark Metamorphic Complex|24551|6|Mentioned|p47 Fig. 2.58|Lower Silurian|Lower Silurian|||||||
9854|Kuark Metamorphic Complex|42627|5|Briefly described|Map legend|Silurian|Silurian|Variation on Kuark Metamorphics.||||||
9854|Kuark Metamorphic Complex|42647|3|Fully described|p50|||Supersedes Kuark Metamorphics. Derived from Pinnak Sandstone.||||||
9854|Kuark Metamorphic Complex|43314|5|Briefly described|Map Legend|||||||||
9854|Kuark Metamorphic Complex|43315|5|Briefly described|Map Legend|||See also Rock Relationship Diagram and Main Structural Features map.||||||03-MAY-05
9854|Kuark Metamorphic Complex|60541|4|Described|p31, p85, p10|||Comprises an elliptical-shaped region of regionally metamorphosed Pinnak Sst and possibly some Bendoc Gp sediments. The Kuark Met. Belt is in middle of MURRUNGOWAR. Considered to be continuous with Cambalong Met. Complex near Bombala. See also Kuark Mets.||||||20-JUN-05
9854|Kuark Metamorphic Complex|60542|6|Mentioned|p13|||||||||
9854|Kuark Metamorphic Complex|60904|5|Briefly described|p784 Fig. 10|||Of the Lachlan Orogen.||||||
9854|Kuark Metamorphic Complex|61187|5|Briefly described|p6, p5 Fig.3.|Early Silurian|Early Silurian|Kuark Zone. Generated during Benambran Orogeny. Name shortened to Kuark Metamorphics on p.5.||||||
9854|Kuark Metamorphic Complex|61413|6|Mentioned|p2 Fig.1.|||||||||
9854|Kuark Metamorphic Complex|67847|6|Mentioned|p78|||Kuark Zone, Lachlan Orogen. ||||||
9854|Kuark Metamorphic Complex|68116|5|Briefly described|Appendix, Maps 36-37, 45.|Wenlock|Llandovery|Informally subdivided into K-feldspar-silimanite and cordierite-andalusite zones. Most cordierite is replaced by fine aggregates of muscovite, biotite and chlorite.|||||Cordierite-andalusite schist and phyllite with porphyroblasts of andalusite and/or cordierite in a mica/quartz matrix. K-feldspar-sillimanite schist, gneiss and minor migmatite with biotite, sillimanite, K-feldspar, quartz, cordierite, plagioclase.|
34704|Kuark Metamorphic Complex Supersuite|22876|5|Briefly described|p18 Table 3|Late Silurian|Late Silurian|||||||
34704|Kuark Metamorphic Complex Supersuite|22877|5|Briefly described|map|Silurian|Silurian|||||||
34704|Kuark Metamorphic Complex Supersuite|22881|5|Briefly described|Map legend|Silurian|Silurian|||||||06-OCT-04
9964|Kyalite Member|24551|6|Mentioned|p341|||||||||
9964|Kyalite Member|29898|6|Mentioned|p218|||||||||
9964|Kyalite Member|35272|6|Mentioned|p286|||||||||
9964|Kyalite Member|41848|5|Briefly described|p361|||Member of Woorinen Formation. Age 15550 +- 230 yrs||||||
9964|Kyalite Member|42264|6|Mentioned|Fig.5 P12|||||||||
9964|Kyalite Member|42827|5|Briefly described|Table 9.1|||of Woorinen Formation||||||
9964|Kyalite Member|42966|2|Defined|Table35 p236|Holocene|Late Pleistocene|of Woorinen Formation||||||
9964|Kyalite Member|44133|6|Mentioned|p253|Holocene|Middle Pleistocene|Of the Woorinen Formation. Geological Province: Murray Basin.||||||
9964|Kyalite Member|70961|14|Not recorded|p138|||Stratigraphic sequence.||||||
9986|Laceby Gravel Member|35091|4|Described|p17|||||||||
9986|Laceby Gravel Member|42966|5|Briefly described|p407, p201|||of Shepparton Formation.||||||
9990|Lacepede Formation|22541|6|Mentioned|Fig 16|||Otway Formation||||||
9990|Lacepede Formation|23010|6|Mentioned|p340|||||||||
9990|Lacepede Formation|23249|6|Mentioned|Fig.2||Late Eocene|||||||
9990|Lacepede Formation|23322|5|Briefly described|962|Late Eocene|Middle Eocene|of McGowran (1973). Geological Province: Gambier Basin.||||||07-SEP-09
9990|Lacepede Formation|23818|5|Briefly described|p174 Fig.84, p177|Late Eocene|Middle Eocene|Geological Province: Otway Basin. Underlain by Kongorong Sand. Overlain by Gambier Limestone. Max. thickness: 37 ft.||||||09-DEC-08
9990|Lacepede Formation|24562|5|Briefly described|p15 Fig. 4|Late Cretaceous|Early Cretaceous|Geological Province: Otway Basin.||||||
9990|Lacepede Formation|29355|6|Mentioned|p188|||||||||
9990|Lacepede Formation|29591|6|Mentioned|p92|||||||||
9990|Lacepede Formation|29697|6|Mentioned|Fig.11|||||||||
9990|Lacepede Formation|30754|6|Mentioned|p13|||See also p14. Stratigraphic table.||||||09-DEC-08
9990|Lacepede Formation|31245|5|Briefly described|p82|||||||||
9990|Lacepede Formation|31247|6|Mentioned|p162|||Microplankton. Refers Traverse (1955)||||||
9990|Lacepede Formation|31624|6|Mentioned|p111|||M.-U.Eocene||||||
9990|Lacepede Formation|31625|6|Mentioned|Fig. 5.2|||Eocene||||||
9990|Lacepede Formation|31850|6|Mentioned|p34|||||||||
9990|Lacepede Formation|31920|3|Fully described|p58|||Eocene. See also Fig.3-2,4,5.||||||
9990|Lacepede Formation|31922|6|Mentioned|p169|||||||||
9990|Lacepede Formation|32116|4|Described|p47|||||||||
9990|Lacepede Formation|32117|6|Mentioned|Fig.2|||||||||
9990|Lacepede Formation|32120|6|Mentioned|p276|||Eocene fauna||||||
9990|Lacepede Formation|32894|5|Briefly described|p287|||Eocene||||||
9990|Lacepede Formation|32895|6|Mentioned|p328|||Tertiary||||||
9990|Lacepede Formation|32897|6|Mentioned|p180|||U.Eocene||||||
9990|Lacepede Formation|32898|6|Mentioned|Table 2-1|||||||||
9990|Lacepede Formation|33109|6|Mentioned|p84|||Separates aquifers||||||
9990|Lacepede Formation|33224|6|Mentioned|p69|||Palynology||||||
9990|Lacepede Formation|33716|5|Briefly described|Table 2|||||||||
9990|Lacepede Formation|33798|6|Mentioned|Fig.2|||||||||
9990|Lacepede Formation|33938|6|Mentioned|p48|||Refs McGowran et al (1971) & Harris (1971).||||||
9990|Lacepede Formation|34308|4|Described|p177|||Johannian - Aldingan||||||
9990|Lacepede Formation|34658|5|Briefly described|p98|||||||||
9990|Lacepede Formation|35018|5|Briefly described|p29|||||||||
9990|Lacepede Formation|35066|6|Mentioned|p209|||||||||
9990|Lacepede Formation|35147|6|Mentioned|Table.1|||||||||
9990|Lacepede Formation|38068|6|Mentioned|Fig.7|||||||||
9990|Lacepede Formation|38903|5|Briefly described|Table 2|||||||||
9990|Lacepede Formation|39077|6|Mentioned|Table 2|||||||||
9990|Lacepede Formation|39408|6|Mentioned|Fig.5|||||||||
9990|Lacepede Formation|39923|6|Mentioned|p354|||||||||
9990|Lacepede Formation|40429|6|Mentioned|p28|||||||||
9990|Lacepede Formation|40557|6|Mentioned|p169|||||||||
9990|Lacepede Formation|41520|5|Briefly described|Fig.12|||||||||
9990|Lacepede Formation|41626|6|Mentioned|p54|||||||||
9990|Lacepede Formation|41627|5|Briefly described|p69|||||||||
9990|Lacepede Formation|42827|6|Mentioned|p283|||||||||
9990|Lacepede Formation|42966|5|Briefly described|p110, Fig.57|||Otway Basin||||||
9990|Lacepede Formation|43675|6|Mentioned|340|||||||||
9990|Lacepede Formation|43700|6|Mentioned|p24||Late Eocene|||||||
9990|Lacepede Formation|43813|6|Mentioned|p133|||||||||
9990|Lacepede Formation|46839|6|Mentioned|Fig.3|||||||||
9990|Lacepede Formation|47054|5|Briefly described|Fig.3 P481|||||||||
9990|Lacepede Formation|61155|5|Briefly described|p19|Early Oligocene|Middle Eocene|Overlies Kangarong Sand. Thickness: 200m. Geological Province: Otway Basin (Gambier Embayment). ||||||
9990|Lacepede Formation|65891|6|Mentioned|p221 Fig.5.|Rupelian|Bartonian|W Otway Basin.||||||
39638|Lady Fiona Sandstone|24088|6|Mentioned|p355 Fig. 4||| Geological Province: Lachlan Fold Belt.||||||
10030|Laira Formation|12781|6|Mentioned|p386|Early Cretaceous|Early Cretaceous|Otway Basin. Maximum thickness 880m.||Crayfish Group.||Overlies Pretty Hill Formation. Is overlain by Katnook Sandstone.||
10030|Laira Formation|22686|5|Briefly described|Fig3p745,Table1p746|Barremian|Valanginian|Consists predominantly of shale, siltstone with minor fine-grained sandstone. Max Age: 134 Ma; Min Age: 123 Ma.  Geological Province: Otway Basin.||||||17-JAN-06
10030|Laira Formation|24208|5|Briefly described|p169|Early Cretaceous|Early Cretaceous|Of the Crayfish Group.  Geological Province: Penola Trough (Otway Basin).||||||
10030|Laira Formation|24209|5|Briefly described|p151|||Geological Province: Penola Trough (Otway Basin)||||||
10030|Laira Formation|24314|5|Briefly described|p61 Fig.2|Hauterivian|Valanginian|Geological Province: Otway Basin. Max. Thickness 890m. Of the Otway Supergroup.||||||30-NOV-04
10030|Laira Formation|24453|5|Briefly described|p809 Fig.2|Hauterivian|Valanginian|Of Crayfish Subgroup. Geological Province: Otway Basin.||||||07-FEB-11
10030|Laira Formation|24551|6|Mentioned|p245, 249|||Of the Crayfish Subgroup. Underlies: Katnook Sandstone.||||||
10030|Laira Formation|24562|5|Briefly described|p8 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Crayfish Group.  Geological Province: Otway Basin.||||||
10030|Laira Formation|42361|2|Defined|p6|Barremian|Valanginian|||||||
10030|Laira Formation|42545|5|Briefly described|p18|||Otway Basin.||||||14-APR-08
10030|Laira Formation|42599|5|Briefly described|Fig.3 P614|||||||||
10030|Laira Formation|43171|6|Mentioned|5-8|||Age: 125-130 Ma||||||
10030|Laira Formation|43195|5|Briefly described|Map Legend||Early Cretaceous|See also commentary on back of map. Of Crayfish Group.||||||
10030|Laira Formation|43660|5|Briefly described|p14|||||||||
10030|Laira Formation|43733|6|Mentioned|Fig.2.11,p65||Early Cretaceous|||||||
10030|Laira Formation|43744|6|Mentioned|Fig.3,p3|||||||||
10030|Laira Formation|43747|5|Briefly described|p5||Early Cretaceous|||||||
10030|Laira Formation|43814|6|Mentioned|Fig.3,p115|||||||||
10030|Laira Formation|44133|5|Briefly described|p144|Hauterivian|Valanginian|Previously also known as 'Crayfish Group, Unit C'. Thickness: 863m. ||||||
10030|Laira Formation|61017|5|Briefly described|p5 Fig. 2|Barremian|Hauterivian|Of the Crayfish Sungroup (Otway Group). Geological Province: Otway Basin.||||||07-FEB-11
10030|Laira Formation|61182|6|Mentioned|p12|||Of Morton (1990). Name assigned to fine-grained strata below Eumeralla Formation in South Australia only - equiv. of Geltwood Beach Formation in Victoria where it is not recognised. ||||||
10030|Laira Formation|61470|5|Briefly described|p28 Fig. 5|Barremian|Hauterivian|Of the Crayfish Subgroup (Otway Group). Overlies Pretty Hill Formation; interfingers with Katnook Sandstone. Geological Province: Otway Basin.||||||12-OCT-05
10030|Laira Formation|61547|5|Briefly described|p459, p461, pp465-466, pp471-472. |Hauterivian|Valanginian|Forms the regional seal to the Pretty Hill Sandstone reservoir. Overbank to lacustrine deposits. Eroded and reworked material from this unit provided sediment for the Katnook Sandstone.||||Overlies the Pretty Hill Formation.|Consists of frequent, fine shale units: interbedded siltstones, shales and occasional sands.|
10030|Laira Formation|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-FEB-11
10030|Laira Formation|61623|6|Mentioned|p449 Fig. 4|Early Cretaceous|Early Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-APR-09
10030|Laira Formation|61626|5|Briefly described|p486 Fig. 2|Early Cretaceous|Early Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-APR-09
10030|Laira Formation|61627|5|Briefly described|p500 Fig. 2|Early Cretaceous|Early Cretaceous|Of Crayfish Group. Underlain by Pretty Hill Formation. Geological Province: Otway Basin.||||||07-FEB-11
10030|Laira Formation|61628|5|Briefly described|p509 Fig. 3|Early Cretaceous|Early Cretaceous|Of Crayfish Subgroup. Geological Province: Otway Basin.||||||07-APR-09
10030|Laira Formation|63122|5|Briefly described|p17 Fig. 4.3||Hauterivian|Of the Crayfish Group. Max. thickness: 880m. Geological Province: Otway Basin. ||||||
10030|Laira Formation|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p63|Hauterivian|Valanginian|Of Morton (1990). Formerly unnamed in Pretty Hill Sandstone; also known as Geltwood Beach Member and Geltwood Beach Fm. Of Crayfish Gp. Overlies Pretty Hill Fm. Age: 136-125Ma. Max.thickness: 890m. Geological Province: Otway Basin. Shale/siltstone suite.||||||30-JAN-08
10030|Laira Formation|63125|5|Briefly described|p107, p116 Tb. 7.6|||Geological Province: Otway Basin. Mature for oil generation. Referred to as upper and lower Laira Formations. ||||||
10030|Laira Formation|63129|5|Briefly described|p127|||Geological Province: Otway Basin.||||||30-JAN-08
10030|Laira Formation|63130|6|Mentioned|p141, p143|||Geological Province: Otway Basin. Its seal for the Pretty Hill Formation reservoirs is regionally thick - up to 900m.||||||31-JAN-08
10030|Laira Formation|63150|5|Briefly described|p96|||Geological province: Otway Basin. Microfasta evansii (non-marine algae) present in upper Foraminisporis wonthaggiensis Zone of this formation - probably representing maximum lake development.||||||
10030|Laira Formation|63267|5|Briefly described|p483, p485 Fig.2, p486, p490-491, p496|Early Cretaceous|Early Cretaceous|Main seal in the Penola Trough, Otway Basin. Floodplain to lacustrine deposits. Poor hydrocarbon source potential. Wireline log. Significance of faults discussed.||Crayfish Group.||Conformably and transitionally overlies Pretty Hill Formation. Is overlain by Katnook Sandstone.|Predominantly dark grey siltstone and shale, with thin, very fine-grained to granular sandstone and wispy shale interbeds.|
10030|Laira Formation|63269|5|Briefly described|p605|Early Cretaceous|Early Cretaceous|Otway Basin.||Crayfish Subgroup.||||
10030|Laira Formation|63431|5|Briefly described|p676, p677 Fig. 2|Hauterivian|Valanginian|Of Crayfish Group. Geological Province: Penola Trough/Otway Basin. See also p680.||||||07-FEB-11
10030|Laira Formation|66245|5|Briefly described|p6 Fig.5. |Barremian|Hauterivian|||Unit in Crayfish Subgroup.||Overlies Pretty Hill Formation. Is overlain by Katnook Sandstone.||
10030|Laira Formation|67367|5|Briefly described|p131 Fig.2, p132. |Barremian|Hauterivian|Is potentially generative for both oil and gas where it is thermally mature.||Unit in Crayfish Subgroup.||Conformably overlies the Pretty Hill Formation.||
10030|Laira Formation|67541|6|Mentioned|p76 Fig.1|||||||||
10030|Laira Formation|69297|5|Briefly described|p79, 104|Barremian|Hauterivian|Otway Basin. ||Crayfish Subgroup||Overlies the Pretty Hill Formation. Overlain by the Katnook Sandstone. |Mudstone and shale. |06-SEP-18
10030|Laira Formation|69651|5|Briefly described|p10|Early Cretaceous|Early Cretaceous|||Crayfish Subgroup.||Overlies Pretty Hill Formation. Is overlain by Katnook Sandstone.||
10030|Laira Formation|69948|6|Mentioned|Fig.4.2|||Otway Basin (a rift basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Eromanga Basin (an intracratonic basin).||||Overlies Pretty Hill Formation. Is overlain by Katnook Sandstone.||
10030|Laira Formation|70077|5|Briefly described|Regional: Fig.4; p4, p8|Barremian|Hauterivian|Otway Basin: Robe-Penola Trough. Lower energy fluvial and lacustrine sediments. In SA, provides vertical and cross-fault sealing of Penola Trough gas reservoirs.||Crayfish Subgroup.||Overlies Pretty Hill Formation. Is overlain by Katnook Sandstone.||
10030|Laira Formation|70379|5|Briefly described|p717, p719, p723-729, p732|Early Cretaceous|Early Cretaceous|Otway Basin. Isopach map. 350-400m of sediments were subsequently eroded prior to deposition of Eumeralla Formation. Relationship of tectonic activity to sediment accumulation discussed in detail. Hauterivian to late Barremian.||Crayfish Group.||Overlies Pretty Hill Formation but is replaced by it in the E of the Basin. Is overlain unconformably by Eumeralla Formation.|Lacustrine and floodplain sediments.|
10030|Laira Formation|70880|6|Mentioned|p77|Barremian|Hauterivian|Otway Basin.||||||
10030|Laira Formation|71266|6|Mentioned|p614 Fig.3|Early Cretaceous|Early Cretaceous|Otway Basin.||||||
10030|Laira Formation|71342|6|Mentioned|Ch4 p9|||Otway Basin. ||||||
10030|Laira Formation|72050|5|Briefly described|p233 Fig.2, 234-235, 238|Barremian|Hauterivian|Shales in this unit are well-developed seals.||Crayfish Group.|||Mainly lacustrine shales. Local interbedded sands and shales on basement highs.|
10030|Laira Formation|73356|6|Mentioned|p. v-1, p4, p10, p13-16, p20-21, p26-29|Barremian|Hauterivian|Otway Basin. Basal boundary with Pretty Hill Formation is gradational and may be diachronous.||Crayfish Subgroup, Otway Group||Underlain by Pretty Hill Formation. Overlain by and equivalent to Katnook Sandstone. Unconformably overlain by Windermere Sandstone.||
10030|Laira Formation|73357|6|Mentioned|p17|Barremian|Valangian|Otway Basin. Correlated to the Foraminisporis wonthaggiensis Zone, mid Valangian to mid Barremian age and with possible brackish influences.||||||
10030|Laira Formation|73383|5|Briefly described|p3, p7 Tb.3.1, p11, p15, p41-42, p62-64|Aptian|Valangian|Otway Basin. Equivalent to chemostratigraphic packages S1-P7 to S1-P9. Lithologies based on geochemistry using the ChemLith classification includes mudstone, limestone, argillaceous and calcareous sandstones, igneous rock, calcareous limestone and siltstone; and using the Herron classification (1988) includes shale, wacke, lith-arenite and Fe-shale. See also vi, p88-94, p100-102, p171, p194-195, p218-224, p229-231, p282, p285, p288-289, p292, p331, p333-334, p336, p339.||Crayfish Subgroup||Overlies Pretty Hill Formation, unconformably underlies Eumeralla Formation|Lacustrine mudstones and alluvial sandstones.|
10030|Laira Formation|73385|5|Briefly described|p5|Barremian|Valanginian|Otway Basin.||Crayfish Subgroup||Overlies Pretty Hill Formation, underlies Eumeralla Formation.|Lacustrine mudstones and alluvial sandstones.|
10030|Laira Formation|73386|4|Described|p4, p6, p8-9, Attachment A1|Barremian|Hauterivian|Otway Basin. Deposited in fluvial floodplain to shallow lacustrine environments. The formation is a thick shale unit in the Penola Trough, thins and becomes increasingly sandstone dominant along the northern basin margin towards the east. Primarily associated with the Upper Foraminisporis wonthaggiensis Spore-Pollen Subzone, corresponds to the S1-P7 to S1-P9 chemostratigraphic packages (Eid et al., 2021b). The interval from 1979 m to 2842 m in Katnook-2 is the designated type section.||Crayfish Subgroup||Overlies Pretty Hill Formation, unconformably underlies Eumeralla Formation, Windermere Sandstone, conformably underlies Katnook Sandstone in the west|Consists of light grey to green siltstone and claystone interbedded with fine grained sandstone.|
10030|Laira Formation|73594|5|Briefly described|p3-4, p42, p45 Fig.5.19, p47-48|Barremian|Valanginian|Otway Basin. Fluvial-lacustrine, deposited in alluvial floodplain and shallow lacustrine environments. Typically over 300 m thick, over 850 m thick in the type section at Katnook-2 well. Passes laterally into the Katnook Sandstone in the western part of the basin.||Crayfish Subgroup||Overlies Pretty Hill Formation, Pretty Hill Sandstone. Underlies Katnook Sandstone, Eumeralla Formation, Windemere Sandstone|Claystones, siltstones and minor sandstones. Includes massive, dissagregated shale with interbedded thin, quartzose sandstones at base.|
10035|Lake Boga Granite|23309|5|Briefly described|p209, 348|Late Devonian|Late Devonian|G321. Age: 356+/-5, 349+/-6, 358+/-6Ma, 357+/-6, 363+/-6, 362+/-6, 360+/-7, 366+/-7 Ma. (K/Ar)||||||23-MAY-05
10035|Lake Boga Granite|24551|6|Mentioned|p229, 657|||Of the Charlton Province.||||||
10035|Lake Boga Granite|31747|6|Mentioned|Map legend|Devonian|Devonian|||||||
10035|Lake Boga Granite|35278|6|Mentioned|p352|||||||||
10035|Lake Boga Granite|41543|6|Mentioned|p126|||||||||
10035|Lake Boga Granite|41868|6|Mentioned|p483|||||||||
10035|Lake Boga Granite|42827|6|Mentioned|p483|||||||||
10035|Lake Boga Granite|60452|5|Briefly described|p69|Late Devonian|Late Devonian|Age: 358 +/- 5Ma (K/Ar, Richards and Singleton, 1981).||||||
10035|Lake Boga Granite|60491|6|Mentioned|p68|||||||||
10035|Lake Boga Granite|64096|5|Briefly described|p281-283|Early Carboniferous|Late Devonian|Non-magnetic, fractionated S-type. Accessory minerals include: primary U and REE-bearing phosphates and oxides, primary Cu sulfides. Unconformable under Parilla Sand. Age: 366 and 349 Ma (K-Ar biotite and muscovite). Geol Prov: western Lachlan Fold Belt.||||||26-JUN-13
10035|Lake Boga Granite|65715|6|Mentioned|p8 Tb.4|||G321. Described by Hills (1941), named by Lawrence and Macumber (1974).||||||
10035|Lake Boga Granite|66934|6|Mentioned|Map legend|||Similar to the informally-named Baldon granite.||||||
10035|Lake Boga Granite|67347|5|Briefly described|p835, p836-7, p838, p839, p842, p844|Devonian|Devonian|Lachlan Fold Belt. Largely buried by up to several hundred metres of Cenozoic sedimentary rocks of the Murray Basin, but exposed in a quarry SW of Lake Boga town. Age of uranium phosphate minerals produced by weathering is discussed.|||||Highly fractionated S-type intrusion. Heterogeneous near top but grading downward to medium-grained, strongly (orthoclase) porphyritic granite.|11-MAY-12
10035|Lake Boga Granite|68116|5|Briefly described|Appendix, Map 11.|Late Devonian|Early Devonian|Accessory minerals include apatite, zircon, monazite-series minerals, primary uranium+REE-bearing phosphates and oxides and primary copper sulfides.|||||Alkali-feldspar muscovite-biotite granite, aplite and pegmatite; non-magnetic; fractionated; porphyritic, S-type; abundant miarolitic cavities and muscovite and tourmaline segregations. Miarolitic cavities lined with quartz, microcline and albite.|
10035|Lake Boga Granite|70718|4|Described|p38, p80, p128|Devonian|Devonian|Has similar geophysical characteristics as the Cunninyeuk granite suite. Based on U-Th-Pb dating the emplacement age may be closer to 377 Ma.|365 +/- 3 Ma|||Intrudes the Sunbury Group.|Non-magnetic, peraluminous, highly fractionated S-type granite.|
10035|Lake Boga Granite|73496|5|Briefly described|Map legend|Late Devonian|Late Devonian|G321.|||||Muscovite-biotite granite; nonmagnetic but with magnetic contact aureole to 80 nT; gravity low to 150 micrometres/second/second below the regional; K, U high.|
10035|Lake Boga Granite|73505|5|Briefly described|p2, p5, p8 Tb.3.2, p9, p14, p35|Early Carboniferous|Late Devonian|(G321). Contains traces of uranium. Numerous K/Ar ages on biotite and muscovite are provided, preferred age of 358+/-5 Ma. Highly fractionated where outcropping. Nonmagnetic.|349+/-6 Ma K/Ar, 366+/-7 Ma|||||
10036|Lake Bonney Sand|37661|6|Mentioned|p8.2.5|||||||||
10062|Lake Mountain Rhyodacite|23229|6|Mentioned|p37|||||||||
10062|Lake Mountain Rhyodacite|23309|5|Briefly described|p164-166.|Late Devonian|Late Devonian|Age: 353 Ma.  See also Lake Mountain Ignimbrite.||||||
10062|Lake Mountain Rhyodacite|24551|4|Described|p165, 223|Devonian|Devonian|Of Cerberean Volcanics, Marysville Igneous Complex||||||10-JUN-14
10062|Lake Mountain Rhyodacite|29786|6|Mentioned|Fig.1|||||||||
10062|Lake Mountain Rhyodacite|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
10062|Lake Mountain Rhyodacite|35073|6|Mentioned|p9|||See also Table 2.||||||
10062|Lake Mountain Rhyodacite|35186|4|Described|p6|||||||||
10062|Lake Mountain Rhyodacite|35277|6|Mentioned|p90|||||||||
10062|Lake Mountain Rhyodacite|35278|6|Mentioned|p361|||||||||
10062|Lake Mountain Rhyodacite|39291|6|Mentioned|p214|||See also Table 1||||||
10062|Lake Mountain Rhyodacite|40178|5|Briefly described|p6|||||||||
10062|Lake Mountain Rhyodacite|41641|4|Described|p160|||||||||
10062|Lake Mountain Rhyodacite|42154|6|Mentioned|Table 1 P334|||||||||
10062|Lake Mountain Rhyodacite|42827|5|Briefly described|Fig 5.4|||same as Lake Mountain Biotite Rhyodacite||||||
10062|Lake Mountain Rhyodacite|44187|5|Briefly described|Map Legend||Late Devonian|||||||
10062|Lake Mountain Rhyodacite|68116|5|Briefly described|Appendix, Maps 33, 42.|Late Devonian|Late Devonian|Very rare cordierite in fine groundmass. Lithic fragments of underlying rock are common.|||||Rhyolite to rhyodacite: uniform, porphyritic with abundant phenocrysts of quartz, plagioclase and biotite, minor enstatite, almandine, rare orthoclase, very rare cordierite; rare pumiceous ignimbrite (base). |
10062|Lake Mountain Rhyodacite|75072|5|Briefly described|p230 Fig.2, 233, 243, 245, 249-250|Late Devonian|Late Devonian|Melbourne Zone. Zircons crystals discussed; probability density distribution graph.|375.0 +/- 2.0 Ma (Compston, 2004).|Marysville Igneous Complex.|||Ignimbrite. S-type.|
10068|Lake Reeve Sand Member|24551|6|Mentioned|p332|||||||||
10068|Lake Reeve Sand Member|35273|5|Briefly described|p261|||||||||
10068|Lake Reeve Sand Member|42827|4|Described|p335|||of Jemmys Point Formation||||||
10076|Lake Wellington Formation|24468|5|Briefly described|p405 Fig.2|Miocene|Miocene|Geological Province: Gippsland Basin.||||||25-SEP-08
10076|Lake Wellington Formation|24551|5|Briefly described|p327 Fig. 10.33|Miocene|Miocene|||||||
10076|Lake Wellington Formation|38929|4|Described|p51|||See also Fig.6||||||
10076|Lake Wellington Formation|38973|6|Mentioned|Fig.2|||||||||
10076|Lake Wellington Formation|39446|5|Briefly described|p56|||||||||
10076|Lake Wellington Formation|41868|6|Mentioned|Fig.12.14|||||||||
10076|Lake Wellington Formation|42649|5|Briefly described|Fig.3 P197-198|||||||||
10076|Lake Wellington Formation|61336|5|Briefly described|p(v) Fig. 5|Middle Miocene|Early Miocene|Geological Province: Gippsland Basin.||||||07-FEB-11
10076|Lake Wellington Formation|65718|6|Mentioned|p10 Fig 3.2, p17 Fig 3.6|Miocene|Miocene|Lake Wellington and Seaspray Depressions, onshore Gippsland Basin. Middle to late Miocene age. Overlies Jemmy's Point Formation in North Seaspray-1.||||Unconformably overlies Latrobe Valley Group and Balook Formation. is overlain conformably by Boisdale Formation. Is adjacent to (?interfingers with) Tambo River Formation and Bairnsdale Limestone.||10-JAN-17
22162|Lakelands Flat Andesite Breccia|23309|5|Briefly described|p36 Table 2.7|||Of the Jamieson Volcanics.||||||
22162|Lakelands Flat Andesite Breccia|24551|5|Briefly described|p87|||Of Jamieson Volcanics (fig.3.15)||||||
22162|Lakelands Flat Andesite Breccia|24576|6|Mentioned|p731|||Geological Province: Lachlan Fold Belt||||||
22162|Lakelands Flat Andesite Breccia|61187|6|Mentioned|p51 Fig.2. |Early Cambrian|Early Cambrian|||Unit in Jamieson Volcanics.||||
22162|Lakelands Flat Andesite Breccia|68116|5|Briefly described|Appendix, Map 34.|Cambrian|Cambrian||||||Andesite breccia, polymictic; minor clinopyroxene-phyric andesite lava; marine.|
10081|Lakes Entrance Formation|13323|5|Briefly described|p393 Fig. 2|Late Oligocene|Early Oligocene|Of the Latrobe Valley Subgroup (Seaspray Group). Marine carbonates. Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|13324|5|Briefly described|p94 Fig. 4, Fig. 10|Miocene|Oligocene|Gippsland Basin.||Of Seaspray Group||||
10081|Lakes Entrance Formation|13332|5|Briefly described|p184 Fig.2|Miocene|Oligocene|Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|13350|5|Briefly described|p94, p96 Fig.3|Miocene|Oligocene|Of the Seaspray Group. Geological Province: Gippsland Basin.  See also p100 Fig. 7.||||||30-JUN-06
10081|Lakes Entrance Formation|22663|5|Briefly described|V97 - G1 to G4 Fig.2|Miocene|Miocene|||||||01-MAR-10
10081|Lakes Entrance Formation|23230|5|Briefly described|Table4-1p40||Oligocene|||||||
10081|Lakes Entrance Formation|23372|4|Described|p250,251 Fig.3|Oligocene|Eocene|Of Gippsland Basin.||||||01-JUL-08
10081|Lakes Entrance Formation|23768|5|Briefly described|p28 Fig.5|Early Miocene|Oligocene|Geological Province: Gippsland Basin.  See also p125 Fig. 42.||||||29-MAR-05
10081|Lakes Entrance Formation|23885|6|Mentioned|p163 Fig 14.3|||Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|23909|5|Briefly described|p290 Fig.3|Miocene|Miocene|Of Seaspray Group.  Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|24038|5|Briefly described|p439 Fig.2|Oligocene|Oligocene|Geological Province: Gippsland Basin||||||
10081|Lakes Entrance Formation|24053|4|Described|p37|Oligocene|Oligocene|Of Seaspray Group.  Max. thickness: 91m.  Geological Basin: Gippsland Basin.||||||
10081|Lakes Entrance Formation|24054|4|Described|p46|||Geological Province: Gippsland Basin.||||||30-AUG-06
10081|Lakes Entrance Formation|24090|5|Briefly described|p8 Fig.3|Oligocene|Oligocene|Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|24164|5|Briefly described|p11,18,20,22,29,30,32,37,40 and more|Miocene|Oligocene|Horizon top of this unit was mapped from seismic data. Presented as Lakes Entr. Formation in Fig.12. Included in Figs.10,12,14,19,22,26.||Seaspray Group||Is overlain by Gippsland Limestone Formation; overlies Latrobe Group||
10081|Lakes Entrance Formation|24211|5|Briefly described|p86 Fig. 3|Miocene|Oligocene|Marine marls, claystones and carbonates.  Geological Province: Gippsland Basin.  See also p85 Fig. 2 and p87 Fig. 4.||||||
10081|Lakes Entrance Formation|24403|5|Briefly described|p3|||Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|24405|6|Mentioned|p5|||Geological Province: Gippsland Basin.||||||12-AUG-04
10081|Lakes Entrance Formation|24407|5|Briefly described|p13 Fig.2|Oligocene|Oligocene|Geological Province: Gippsland Basin.||||||01-JUL-08
10081|Lakes Entrance Formation|24495|6|Mentioned|p9, p10|||Marls.  Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|24551|5|Briefly described|p262 Fig. 9.29, p327 Fig. 10.33|Miocene|Oligocene|Of the Seaspray Group.||||||
10081|Lakes Entrance Formation|24561|5|Briefly described|p44|Oligocene|Oligocene|Geological Province: Gippsland Basin. Basal unit of the basin. Predominantly marl.||||||04-FEB-08
10081|Lakes Entrance Formation|29500|6|Mentioned|p11|||||||||
10081|Lakes Entrance Formation|29591|5|Briefly described|p98|||||||||
10081|Lakes Entrance Formation|29650|6|Mentioned|p111|||||||||
10081|Lakes Entrance Formation|29678|6|Mentioned|p191|||||||||
10081|Lakes Entrance Formation|29721|6|Mentioned|p192|||||||||
10081|Lakes Entrance Formation|29736|6|Mentioned|Fig.2|||||||||
10081|Lakes Entrance Formation|29974|6|Mentioned|p47|||||||||
10081|Lakes Entrance Formation|30836|4|Described|p1264|||Oligcene||||||
10081|Lakes Entrance Formation|30933|6|Mentioned|Map legend|Oligocene|Eocene|Eocene-Miocene||||||
10081|Lakes Entrance Formation|31159|6|Mentioned|p85|||See also P86, 87, 88.||||||
10081|Lakes Entrance Formation|31351|5|Briefly described|Fig. 5|||See also P85, 87||||||
10081|Lakes Entrance Formation|31352|4|Described|p133|||See also P137, Fig. 3. Oligocene.||||||
10081|Lakes Entrance Formation|31480|4|Described|p74|||Oligocene - Miocene||||||
10081|Lakes Entrance Formation|31508|6|Mentioned|Table 1|||Oligocene||||||
10081|Lakes Entrance Formation|31627|6|Mentioned|p12|||||||||
10081|Lakes Entrance Formation|31646|6|Mentioned|Fig. 2|||||||||29-SEP-04
10081|Lakes Entrance Formation|31850|6|Mentioned|p36|||Refers Carter (1964)||||||
10081|Lakes Entrance Formation|31922|6|Mentioned|p166|||||||||
10081|Lakes Entrance Formation|32574|6|Mentioned|p77|||||||||
10081|Lakes Entrance Formation|32679|6|Mentioned|p94|||||||||
10081|Lakes Entrance Formation|33130|6|Mentioned|p60|||||||||
10081|Lakes Entrance Formation|33267|6|Mentioned|p70|||See also Fig.8||||||
10081|Lakes Entrance Formation|33320|6|Mentioned|p57|||Olig. Mioc.||||||
10081|Lakes Entrance Formation|33362|6|Mentioned|p112|||||||||
10081|Lakes Entrance Formation|33459|6|Mentioned|Table 1|||||||||
10081|Lakes Entrance Formation|33929|6|Mentioned|p70|||See also PP71 - 73.||||||
10081|Lakes Entrance Formation|34519|5|Briefly described|p46|||||||||
10081|Lakes Entrance Formation|34558|4|Described|p19|||See also Fig.2||||||
10081|Lakes Entrance Formation|34842|4|Described|p21|||||||||
10081|Lakes Entrance Formation|34843|6|Mentioned|p10|||||||||
10081|Lakes Entrance Formation|34954|6|Mentioned|Fig.35|||||||||
10081|Lakes Entrance Formation|35013|5|Briefly described|p397|||||||||
10081|Lakes Entrance Formation|35067|6|Mentioned|Fig.3|||||||||
10081|Lakes Entrance Formation|35273|3|Fully described|p257|||||||||
10081|Lakes Entrance Formation|35285|6|Mentioned|p415|||||||||
10081|Lakes Entrance Formation|35573|6|Mentioned|Fig.3|||Chronostratigraphic section - Gippsland Basin||||||
10081|Lakes Entrance Formation|36107|6|Mentioned|p101|||||||||
10081|Lakes Entrance Formation|36310|6|Mentioned|p149|||||||||
10081|Lakes Entrance Formation|36331|6|Mentioned|Fig.1|||See also P24||||||
10081|Lakes Entrance Formation|36643|6|Mentioned|Fig.7|||||||||
10081|Lakes Entrance Formation|36916|6|Mentioned|p107|||||||||
10081|Lakes Entrance Formation|37127|6|Mentioned|p349|||||||||
10081|Lakes Entrance Formation|37330|5|Briefly described|Table 4|||||||||
10081|Lakes Entrance Formation|37530|3|Fully described|p9|||||||||
10081|Lakes Entrance Formation|37783|6|Mentioned|Fig.12|||||||||
10081|Lakes Entrance Formation|37809|6|Mentioned|p7|||||||||
10081|Lakes Entrance Formation|38070|6|Mentioned|Fig.12|||Gippsland Basin||||||
10081|Lakes Entrance Formation|38313|6|Mentioned|Fig.2|||||||||
10081|Lakes Entrance Formation|38422|6|Mentioned|p151|||||||||
10081|Lakes Entrance Formation|38739|5|Briefly described|p285|||||||||
10081|Lakes Entrance Formation|38929|4|Described|p48|||See also Fig.6||||||
10081|Lakes Entrance Formation|38930|6|Mentioned|p59|||Also mentioned Fig.1||||||
10081|Lakes Entrance Formation|38973|6|Mentioned|p565|||||||||
10081|Lakes Entrance Formation|39446|5|Briefly described|p56|||||||||
10081|Lakes Entrance Formation|40716|5|Briefly described|p67|||||||||
10081|Lakes Entrance Formation|41171|6|Mentioned|p166|||||||||
10081|Lakes Entrance Formation|41193|6|Mentioned|p315|||||||||
10081|Lakes Entrance Formation|41213|5|Briefly described|Fig.2|||||||||
10081|Lakes Entrance Formation|41227|6|Mentioned|p4|||||||||
10081|Lakes Entrance Formation|41259|6|Mentioned|Fig.4|||||||||
10081|Lakes Entrance Formation|41282|6|Mentioned|p34|||||||||
10081|Lakes Entrance Formation|41534|5|Briefly described|p12|||||||||
10081|Lakes Entrance Formation|41537|6|Mentioned|Fig.2|||||||||
10081|Lakes Entrance Formation|41727|5|Briefly described|p433|||||||||
10081|Lakes Entrance Formation|41868|5|Briefly described|p522|||||||||
10081|Lakes Entrance Formation|42083|4|Described|Fig.9 P346|||||||||
10081|Lakes Entrance Formation|42311|5|Briefly described|Fig.2 P526|||||||||
10081|Lakes Entrance Formation|42649|6|Mentioned|Fig.6 P203|||of Seaspray Group||||||
10081|Lakes Entrance Formation|42827|3|Fully described|p331|||Of Seaspray Group.||||||12-FEB-08
10081|Lakes Entrance Formation|43145|4|Described|p11,p69||Early Oligocene|Of Seaspray Group.||||||12-FEB-08
10081|Lakes Entrance Formation|43667|6|Mentioned|Fig.3,p12||Miocene|||||||
10081|Lakes Entrance Formation|48631|5|Briefly described|p4,5,6,Pl.1,sh2||Oligocene|(J/55-11).||||||
10081|Lakes Entrance Formation|48636|4|Described|p.14,15,17,19,60|||(J55-11/Sale).||||||
10081|Lakes Entrance Formation|60538|5|Briefly described|p475 Fig. 14, 482 Fig. 21|Oligocene|Oligocene|Geological Province: Gippsland Basin. Of the Seaspray Group.||||||
10081|Lakes Entrance Formation|60666|5|Briefly described|p15 (Fig.)|||Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|61155|5|Briefly described|p18|Middle Miocene|Late Eocene|Of the Seaspray Group. Fine-grained deep-water marls and carbonates. Overlies the Latrobe Group (Gurnard Formation); overlain by Gippsland Limestone. Thickness: 500m (offshore). Geological Province: Gippsland Basin (offshore). See p3, p8.||||||01-JUL-08
10081|Lakes Entrance Formation|61212|5|Briefly described|p301 Fig. 2|Miocene|Early Oligocene|Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|61302|5|Briefly described|p5, p12|||Of Seaspray Group. Consists of a basal sand and gravel member, a glauconitic sandstone member, a micaceous marl member and an interbedded marl limestone member. Overlies Latrobe Group. Caps the Cunningham Greensand Member. Geol. Prov: Gippsland Basin.||||||02-JUN-06
10081|Lakes Entrance Formation|61323|5|Briefly described|p3 Fig. 3|Miocene|Oligocene|Geological Province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|61329|6|Mentioned|p130|||||||||
10081|Lakes Entrance Formation|61336|5|Briefly described|p(iv) Fig. 4|Late Oligocene|Late Oligocene|Of the Seaspray Group. Disconformably overlies Latrobe Group. Geological Province: Gippsland Basin. See also p(v) Fig. 5.||||||07-FEB-11
10081|Lakes Entrance Formation|61469|5|Briefly described|p33|||Overlies Gurnard Formation. Geological Province: Gippsland Basin.||||||12-OCT-05
10081|Lakes Entrance Formation|61552|6|Mentioned|p583 Fig.2. |Late Oligocene|Early Oligocene|||Unit in Latrobe Valley Subgroup.||||
10081|Lakes Entrance Formation|61627|6|Mentioned|p504|||Geological Province: Gippsland Basin.||||||07-FEB-11
10081|Lakes Entrance Formation|62899|5|Briefly described|p37 Fig. 2|||Includes Cunningname (misspelling?) Greensand Member and Metung Marl Member. Geological province: Lakes Entrance Platform.||||||12-DEC-06
10081|Lakes Entrance Formation|63173|5|Briefly described|p342 Fig. 9.2|Middle Miocene|Early Oligocene|Geological Province: Gippsland Basin, offshore. Regional sealing unit for underlying hydrocarbon traps in this basin. Correlates with uppermost Demons Bluff  Formation in the Bass Basin.||||||07-FEB-11
10081|Lakes Entrance Formation|63739|5|Briefly described|p37 Fig. 2|||Includes Colquhoun Sandstone, Cunningname Greensand and Metung Marl Members. Overlain by Gippsland Limestone. Geological province: Gippsland Basin.||||||
10081|Lakes Entrance Formation|64876|5|Briefly described|p145 Fig.2|Oligocene|Oligocene|Gippsland Basin.||Seaspray Group.||||
10081|Lakes Entrance Formation|65717|5|Briefly described|p4-7, p9 Fig.2.2, p11-17, p19-28, p30-34|Oligocene|Oligocene|See also p38; Appendix 1, 3. Considered to be a high quality regional top seal for CO2 containment, and one of the most important in the Gippsland Basin. Thickness (from 19m to 430m) and depth to basement (400m to 3,500m) increase offshore. MICP anlaysis results. Top, base, thickness from named offshore wells tabulated.||Basal Latrobe Valley Subgroup.|Cunningham Greenstone Member, Giffard Sandstone Member, Colquhoun Sandstone Member, Seacombe Marl, Metung Marl.|Unconformably overlies Burong, Gurnard Formations. Is overlain by Gippsland Limestone.|Thick calcareous mudstones, shales interbedded with marl and glauconite.|05-SEP-17
10081|Lakes Entrance Formation|65718|5|Briefly described|p4, p5, p10 Fig 3.2, p12, p18, pp22-26|Miocene|Oligocene|Hocking (1976). Gippsland Basin. Considered a basin-wide, high quality regional top seal to the oil and gas accumulations at the top Latrobe Group reservoirs. Early Miocene minimum age.||Basal unit of the Seaspray Group.|Includes the Cunninghame Greensand Member, Giffard Sandstone Member (basal unit), Colquhoun Sandstone Member, Seacombe Marl Member, and Metung Marl Member.|Overlain by the Gippsland Limestone and the Haunted Hills Formation. Interfingers with the Balook Formation.|Composed predominantly of smectite-rich calcareous mudstones and claystones, with some variation in composition across the basin.|10-JAN-17
10081|Lakes Entrance Formation|65973|5|Briefly described|p17, p21-22, p33, p57, p62, p65, p71|Oligocene|Oligocene|Gippsland Basin. Forms a  high-quality regional seal to oil and gas accumulations in the Latrobe interval. Varies in thickness from 100m to over 300m in deeper parts of the basin. Geophysical response is discussed briefly. Intersected in Kipper-1, Judith-1, Hammerhead-1, East Pilchard-1, Longtom-1, Longtom-1/ST-1, Northright-1, Sole-1, Sweep-1 and many more drillholes (see appendix). See also p74, p76-77, p78, p80, p82, p85, p102, p104, p108, p110-112, p116, p118-119, p123-126, p128-p136, p138-139, p142-144, p171, p180, p183.||Seaspray Group||Overlain by the Gippsland Limestone.|Marls.|
10081|Lakes Entrance Formation|67061|6|Mentioned|p554 Fig.10.|Miocene||Gippsland Basin, onshore.||Unit in Seaspray Group.||Is overlain by Gippsland Formation.||
10081|Lakes Entrance Formation|67727|5|Briefly described|p55, p58 Fig.2, p62, p78.|Oligocene|Oligocene|Gippsland Basin, mainly offshore. Equivalent to the Morwell Formation in the Latrobe Valley.||Unit in Seaspray Group.|Includes Giffard Sandstone.|Overlies Traralgon Formation. Is overlain by Haunted Hill Formation.|Marls and limestones.|
10081|Lakes Entrance Formation|69016|5|Briefly described|p88-89|||Of the Gippsland Basin.||Unit of Seaspray Group.||Laterally grades into lower unit of Balook Formation.|Sands and gravels at the base, developing to finer grained marls and mudstone on the top with fine interbeds of fossiliferous sandy limestone.|
10081|Lakes Entrance Formation|70028|5|Briefly described|p77-82, 86, 88-91|Oligocene|Oligocene|Gippsland Basin. Regional seal to the Latrobe Group reservoirs. Rated as excellent to good for CO2 storage.||Basal Seaspray Group.||Is overlain by the Gippsland Limestone.|Fine-grained sediments: mainly marl and rich in smectite clay.|
10081|Lakes Entrance Formation|70076|5|Briefly described|South-Eastern:p2. Regional: Fig.3; p3,p6|Burdigalian|Rupelian|Onlapping, marly sediments provide the principal regional seal across the Basin.||Basal unit in Seaspray Group.|Seacombe Marl, and Giffard Sandstone, Members.|Overlies Gurnard or Burong Formation. Is overlain by Gippsland Limestone.||
10081|Lakes Entrance Formation|70862|6|Mentioned|p48 Fig.1|||Latrobe Valley, Gippsland Basin.||Seaspray Group.||Overlies Traralgon Formation. Is overlain by Gippsland Limestone Formation.||
10081|Lakes Entrance Formation|73289|5|Briefly described|p765 Fig.2, 767, 770, 773-774|Oligocene|Oligocene|Lake Wellington, Seaspray Depressions, onshore Gippsland Basin.||Seaspray Group.|Giffard Sandstone Member.|Overlies Traralgon Formation. Is overlain by Gippsland Limestone Formation. Interfingers with (lateral facies variation of) Balook Formation.||
10081|Lakes Entrance Formation|73471|5|Briefly described|p86-87, p89|||Gippsland Basin. Overlies Latrobe Unconformity. Acts as the regional seal to oil and gas. See also Lakes Entrance Subgroup.||Seaspray Group||Overlies Gurnard Formation|Marls and marine carbonates.|
10081|Lakes Entrance Formation|73488|4|Described|p631-632, p634 Fig.4, p636-637, p646|Chattian|Rupelin|Gippsland Basin.||Seaspray Group||Overlies Giffard Sandstone, underlies Gippsland Limestone Formation|Marine carbonate sediments. Marls and glauconitic mudstones.|
10081|Lakes Entrance Formation|73562|5|Briefly described|p303-304|Miocene|Oligocene|Gippsland Basin; offshore. Has extensive submarine canyoning.||Basal Seaspray Group.||Equivalent to (lower part of) the Balook Formation.|Marine mudstone and limestone.|
10081|Lakes Entrance Formation|75065|5|Briefly described|p151-152, 154, 170-171|Pliocene|Eocene|Gippsland Basin; offshore.||Seaspray Group.||Overlies Gurnard Formation locally. Is overlain by Gippsland Limestone.|Deep-water marls.|
10088|Lal Lal Formation|23257|5|Briefly described|p208|Eocene|Paleocene|||||||
10088|Lal Lal Formation|39865|4|Described|p27|||||||||
10088|Lal Lal Formation|61181|5|Briefly described|p112|Eocene|Paleocene|At Lal Lal, white ligneous clay averaging 15-21m thick forms the upper part of this unit. This is a semi-plastic, refractory clay suitable for use in firebricks and ceramics. Geological Province: Lal Lal Basin.||||||07-NOV-08
10088|Lal Lal Formation|65715|5|Briefly described|p11 Tb.7|Paleogene|Paleogene|Some regard this as a junior synonym of Yaloak Formation, but see discussion p12.||||||06-FEB-15
39876|Lalgambook Breccia|24383|2|Defined|p7, p66, p65 Fig 42,  p69 Tb.9|Cenozoic|Cenozoic|Lalgambook is the Aboriginal name for Mount Franklin. Age: 0.4 +/- 0.2Ma. Geological Province: Lachlan Fold Belt||||||10-FEB-15
39876|Lalgambook Breccia|65715|5|Briefly described|p18 Tb.9|||Of Newer Volcanic Group. Defined in Wilman et al. (2002) p56.||||||
24352|Lalkaldarno Porphyry|23229|5|Briefly described|p16|||Intrusion?||||||
24352|Lalkaldarno Porphyry|23309|4|Described|p44, Table 2.14, p35. Tb 2.6/2.8|Cambrian|Cambrian|Age: 500+/-2 Ma.  Of Mount Stavely Volcanics.  See also Lalkaldarno Tonalite.||||||
24352|Lalkaldarno Porphyry|23402|3|Fully described|p12, p8 Tb. 1|Late Cambrian|Late Cambrian|Parent: Mount Stavely Volcanic Complex. Intrusion coeval with Towanway Tuff vulcanism (Buckland, 1987).||||||20-MAY-13
24352|Lalkaldarno Porphyry|24551|5|Briefly described|p79 Fig.3.9.  p717 Table 2.4|Early Ordovician|Late Cambrian|See also Lalkaldarno Tonalite.  Age: 500 +/- 2Ma.||||||
24352|Lalkaldarno Porphyry|38436|4|Described|p426|||See also Fig.2||||||
24352|Lalkaldarno Porphyry|40172|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
24352|Lalkaldarno Porphyry|40761|5|Briefly described|Table 1|||||||||
24352|Lalkaldarno Porphyry|40887|2|Defined|p21|Cambrian|Cambrian|Prob. Cambrian||||||
24352|Lalkaldarno Porphyry|41571|5|Briefly described|p39|||Mention Table 2.2||||||
24352|Lalkaldarno Porphyry|42827|5|Briefly described|p39|||of Mount Stavely Volcanic Complex||||||
24352|Lalkaldarno Porphyry|50371|5|Briefly described|Map Legend|Cambrian|Cambrian|Of Mount Stavely Volcanic Complex. Porphyritic hornblende quartz diorite||||||
24352|Lalkaldarno Porphyry|61183|6|Mentioned|p23|||Intruded the Williamson Road Serpentinite. ||||||
24352|Lalkaldarno Porphyry|61187|6|Mentioned|p69 Fig.2, pp130-131. |Early Cambrian|Early Cambrian|Nonmagnetic to weakly magnetic.||Unit in Mount Stavely Volcanic Complex.||||
24352|Lalkaldarno Porphyry|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Mount Stavely Volcanic Complex. Defined by Buckland 1986.||||||
24352|Lalkaldarno Porphyry|68116|5|Briefly described|Appendix, Map 39.|Middle Cambrian|Middle Cambrian||||||Porphyritic hornblende tonalite with phenocrysts of plagioclase, quartz, hornblende and augite in a fine grained quartzo-feldpathic mosaic; high-level intrusion.|
24352|Lalkaldarno Porphyry|70211|5|Briefly described|p1, p45-46|||Amphibole Ar-Ar plateau age.|496.0 +/- 3.0 Ma (Bucher, 1998).|Mount Stavely Volcanic Complex.||||
24352|Lalkaldarno Porphyry|70877|6|Mentioned|p69, p168, p172-p173|Cambrian|Cambrian||496 +/- 3 Ma (Bucher, 1998)|||||
24352|Lalkaldarno Porphyry|70967|6|Mentioned|p3, 28|||Ramsay (1983).|||||Intrusive.|
24352|Lalkaldarno Porphyry|71593|4|Described|p9, p39-p40, p57-p58|||Age is complicated by resetting of the Ar/Ar leading to many discordant spectra, the provided age is derived from the most concordant ones. This unit is unmineralised. See also p76, p95, p119, p135, p151, p163.|496 +/- 3 Ma (Ar/Ar, Bucher, 1998)|||||
24352|Lalkaldarno Porphyry|72445|6|Mentioned|p2.|||Intrusive. Correlated with hydrothermally-altered quartz porphyry at the base of Wickliffe No. 6 diamond drill hole.||||||
24352|Lalkaldarno Porphyry|73430|5|Briefly described|p496|||Youngest unit in the Mount Stavely volcanic stratigraphy (Bowman et al,. 2019). [Misspelt as Larnakardo porphyry?]|504.7+/-2 Ma LAICPMS U-Pb zircon|Mount Stavely Volcanic Complex|||Shallowly intrusive dacite porphyry.|
10150|Lang Lang Sands|30083|6|Mentioned|Map 1|||Quaternary age.||||||
23715|Langi Ghiran Granite|22756|5|Briefly described|P20, P43, Table2||Early Devonian|||||||
23715|Langi Ghiran Granite|23309|5|Briefly described|p435 App1|Devonian|Devonian|G376 I-Type. Supersedes Mount Langi Ghiran Granite. Age: 392 +/- 5 Ma. 407 +/- 22 Ma.||||||
23715|Langi Ghiran Granite|42726|5|Briefly described|map legend|Early Devonian||Reserved in 1993.||||||
23715|Langi Ghiran Granite|44186|5|Briefly described|Map Legend||Early Devonian|G376 I-type.||||||
23715|Langi Ghiran Granite|64314|6|Mentioned|p495 Fig. 2a|||||||||
23715|Langi Ghiran Granite|66002|5|Briefly described|p7 Tb.5|||Of Mount Cole Suite. G376. Called Mount Langhi Ghiran Granite by Cayley and McDonald (1995)||||||
23715|Langi Ghiran Granite|68116|5|Briefly described|Appendix, Map 31.|Early Devonian|Early Devonian||||||Biotite granite: highly fractionated; light grey; medium grained; equigranular.|
74893|Lanky Creek Sandstone Member|64010|5|Briefly described|p258 Fig.1. |Tournaisian|Tournaisian|||Of the Snowy Plains Formation.||||
74893|Lanky Creek Sandstone Member|64536|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation (Mansfield Group). Sandstone, lesser mudstone: sandstone is mostly quartzarenite, very thick bedded. Forms bold outcrops. Mudstone is red, forms packages tens of metres thick. Recessive. Fluvial deposits.||||||07-FEB-11
74893|Lanky Creek Sandstone Member|64537|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation (Mansfield Group). Sandstone, lesser mudstone: sandstone is mostly quartzarenite, very thick bedded. Forms bold outcrops. Mudstone is red, forms packages tens of metres thick. Recessive. Fluvial deposits.||||||07-FEB-11
74893|Lanky Creek Sandstone Member|64538|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Snowy Plains Formation (Mansfield Group). Sandstone, lesser mudstone: sandstone is mostly quartzarenite, very thick bedded. Forma bold outcrops. Mudstone is red, forms packages tens of metres thick. Recessive. Fluvial deposits.||||||07-FEB-11
74893|Lanky Creek Sandstone Member|64606|5|Briefly described|Map Legend|Neogene|Early Carboniferous|Of Snowy Plains Formation. Sandstone, lesser mudstone: alluvial deposits. Bright yellow to bright pink in RGB. Nonmagnetic.||||||
74893|Lanky Creek Sandstone Member|64616|4|Described|p140, p299|Early Carboniferous|Early Carboniferous|New member of Snowy Plains Formation. Conformably overlies Home Station Sandstone Member in south and Buttercup Mudstone Member in north. Conformably overlain by Hearns Mudstone Member. 150-200m thick. Interbedded red and grey fluvial sandstones, very thick-bedded; lesser red mudstone. Geophysical characteristics given.||||||19-SEP-17
24354|Lano Gully Sandstone|23309|5|Briefly described|p42, Fig. 2.14, p53. Tb 2.16|||||||||
24354|Lano Gully Sandstone|40136|5|Briefly described|p29|||||||||
24354|Lano Gully Sandstone|41050|6|Mentioned|p51|||||||||
24354|Lano Gully Sandstone|41570|4|Described|p85|||||||||
24354|Lano Gully Sandstone|42628|5|Briefly described|Map legend|Lancefieldian||||||||
24354|Lano Gully Sandstone|42826|2|Defined|p27|Early Ordovician||Of Romsey Group.||||||03-FEB-09
24354|Lano Gully Sandstone|42827|5|Briefly described|p85|||Of Romsey Group.||||||26-JUN-13
24354|Lano Gully Sandstone|64611|5|Briefly described|Map legend|Lancefieldian|Lancefieldian|Of the Romsey Subgroup (Castlemaine Group).  Sandstone and minor siltstone; massive, thick bedded, lithic, micaceous, quartz sandstone with minor grey siltstone interbeds; unfossiliferous; deep-marine turbidite fan deposits.||||||
24354|Lano Gully Sandstone|64612|4|Described|p37|||Of Romsey Subgroup. Conformably overlies Goldie Chert. Thickness: 180m. Quartz-rich sandstone, thickly bedded, lithic and micaceous.||||||26-JUN-13
24354|Lano Gully Sandstone|65715|5|Briefly described|p4 Tb.2|Ordovician|Ordovician|Of Romsey Subgroup. Formation rank.||||||
24354|Lano Gully Sandstone|68116|5|Briefly described|Appendix, Map 32.|Darriwilian|Late Cambrian|Minimum age as Lancefieldian in text.|||||Sandstone, siltstone: sandstone mostly thick-bedded; minor siltstone; grey; unfossiliferous.|
10182|Lara Limestone|24551|6|Mentioned|p609|Pleistocene|Pleistocene|||||||
10182|Lara Limestone|30988|6|Mentioned|p315|||||||||
10182|Lara Limestone|33231|5|Briefly described|p55|||Pleist.||||||
10182|Lara Limestone|33805|6|Mentioned|p43|||See also P41 & 44||||||
10182|Lara Limestone|35276|6|Mentioned|p242|||||||||
10182|Lara Limestone|37385|5|Briefly described|p18|||||||||
10182|Lara Limestone|38144|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
10182|Lara Limestone|41537|5|Briefly described|p352|||||||||
10182|Lara Limestone|42827|6|Mentioned|p316|||||||||
10182|Lara Limestone|44197|5|Briefly described|Map Legend||Pleistocene|||||||
10182|Lara Limestone|63445|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Lacustrine: limestone, minor sand.|
10182|Lara Limestone|70998|4|Described|p161|||Excursion details.||||||
30342|Larsen Creek Ignimbrite|23309|5|Briefly described|p122, 125, 133. Tb 2.45|||||||||
30342|Larsen Creek Ignimbrite|24133|5|Briefly described|p45|Devonian|Devonian|Parent: Dartella Volcanic Group.  Geological Province: Lachlan Fold Belt.||||||
30342|Larsen Creek Ignimbrite|24551|5|Briefly described|p149|Devonian|Devonian|Of Dartella Volcanics.||||||
30342|Larsen Creek Ignimbrite|60503|3|Fully described|p121-124, p41 Tb. 2|Early Devonian|Early Devonian|Of the Dartella Volcanics. Overlies Dart River Volcanic Breccia and Murtagh Creek Ignimbrite; nonconformably overlies Wallaby and Eustace Creek Granites; conformably underlies Sheevers Spur Ignimbrite.||||||17-FEB-10
30342|Larsen Creek Ignimbrite|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Ignimbrite, tuff; rhyolitic feldspar ignimbrite, variable phenocryst content and quartz:feldspar ratio, densely welded groundmass, often pumiceous with well developed eutaxitic foliation||||||21-OCT-04
30342|Larsen Creek Ignimbrite|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Ignimbrite, tuff; rhyolitic feldspar ignimbrite, variable phenocryst content and quartz:feldspar ratio, densely welded groundmass, often pumiceous with well developed eutaxitic foliation||||||21-OCT-04
30342|Larsen Creek Ignimbrite|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Ignimbrite, tuff; rhyolitic feldspar ignimbrite, variable phenocryst content and quartz:feldspar ratio, densely welded groundmass, often pumiceous with well developed eutaxitic foliation||||||21-OCT-04
30342|Larsen Creek Ignimbrite|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Ignimbrite, tuff; rhyolitic feldspar ignimbrite, variable phenocryst content and quartz:feldspar ratio, densely welded groundmass, often pumiceous with well developed eutaxitic foliation||||||21-OCT-04
30342|Larsen Creek Ignimbrite|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Dartella Volcanic Group. Ignimbrite: weakly magnetic (0-10 nT); moderate K, low to moderate total count, U, low Th||||||21-OCT-04
30342|Larsen Creek Ignimbrite|68116|5|Briefly described|Appendix, Map 27.|Early Devonian|Early Devonian|Contains fragments of Wallaby Granite, biotite schist and Bendoc Group rocks.|||||Rhyolitic ignimbrite, tuff: feldspar ignimbrite, variable phenocryst content and quartz/feldspar ratio, densely welded groundmass, often pumiceous with well developed eutaxitic foliation.|
10217|Latrobe Group|13323|4|Described|p391, p393 Fig. 2|Early Oligocene|Turonian|Includes the Emperor, Golden Beach, Halibut and Cobia Subgroups. Geological Province: Gippsland Basin. See also p394 Fig. 3.||||||
10217|Latrobe Group|13324|4|Described|p92, 93, p94 Fig. 4|Oligocene|Cenomanian|Gippsland Basin. Hosts all known offshore oil and gas discoveries in Gippsland Basin. Characterised by numerous stacked depositional cycles in various rift basin to open marine shelf settings. Includes non-marine fluvial sediments, coal measures, coastal plain, estuarine and marine sediments.|||Includes Emperor Subgroup, Golden Beach Subgroup, Latrobe Siliciclastics, Gurnard Formation, Angler Shale.|Unconformable over Strzelecki Group.||
10217|Latrobe Group|13332|5|Briefly described|p183, p184 Fig.2|Late Miocene|Late Cretaceous|Geological Province: Gippsland Basin.||||||
10217|Latrobe Group|13350|5|Briefly described|p93|Eocene|Late Cretaceous|Mainly non-marine deposits - major petroleum producer in the basin. Overlain by Seaspray Group. Geological Province: Gippsland Basin. See also p100 Fig. 7.||||||
10217|Latrobe Group|22454|5|Briefly described|p3, fig. 4|Tertiary|Late Cretaceous|Gippland Basin. Overlies Golden Beach Group, overlain by Seaspray Group||||||
10217|Latrobe Group|22487|6|Mentioned|p212 Fig. 3|Tertiary|Cretaceous|Geological province: Gippsland Basin.||||||11-SEP-08
10217|Latrobe Group|22495|6|Mentioned|P221, Fig2||Late Cretaceous|||||||
10217|Latrobe Group|22663|6|Mentioned|p10|||||||||
10217|Latrobe Group|23238|5|Briefly described|Fig10-3.3p108|Tertiary|Tertiary|||||||
10217|Latrobe Group|23309|6|Mentioned|p360|Eocene|Cretaceous|||||||
10217|Latrobe Group|23356|5|Briefly described|26 Tab.2|Late Cretaceous|Late Cretaceous|||||||
10217|Latrobe Group|23372|4|Described|p250,251 Fig.3|Eocene|Late Cretaceous|Equivalent to upper-middle Eastern View Coal Measures. of Gippsland Basin.||||||
10217|Latrobe Group|23625|5|Briefly described|p54|Tertiary|Tertiary|Overlying unit: Seaspray Group.  Geological Province: Gippsland Basin||||||
10217|Latrobe Group|23792|5|Briefly described|p22|Eocene|Late Cretaceous|Mainly non-marine sag phase sediments. Contains economic petroleum. Geological Province: Gippsland Basin.||||||
10217|Latrobe Group|23885|5|Briefly described|p163|Tertiary|Late Cretaceous|Min age: Middle Tertiary. Geological Province: Gippsland Basin.||||||18-FEB-05
10217|Latrobe Group|24002|5|Briefly described|p242|Eocene|Cretaceous|Geological Province: Gippsland Basin||||||
10217|Latrobe Group|24038|5|Briefly described|p439 Fig.2|Oligocene|Eocene|Geological Province: Gippsland Basin||||||
10217|Latrobe Group|24053|4|Described|p37|Miocene|Eocene|Geological Basin: Gippsland Basin.||||||
10217|Latrobe Group|24054|4|Described|p46|Late Eocene|Late Cretaceous|Max. thickness: 5000m.  Geological Basin: Gippsland Basin.||||||
10217|Latrobe Group|24056|6|Mentioned|p85|||Geological Basin: Gippsland Basin.||||||
10217|Latrobe Group|24090|5|Briefly described|p8 Fig.3|Oligocene|Late Cretaceous|Geological Province: Gippsland Basin.||||||
10217|Latrobe Group|24164|5|Briefly described|p11,15,18,20,22,24,29-32,34,40,41, more|Quaternary||Age: Neocomian (Early Cretaceous) - Quaternary. Coastal plain, coastal barrier, open marine, fluvio-deltaic / marine, alluvial fan / lacustrine. Northeast of Marlin and Turrum fields the top of Latrobe Group is seen as a strong erosional surface partly related to Eocene Marlin Channel system. Included in Figs.8,10,12,14,15,19,22,26, Tb.2.|||Gurnard Formation, Golden Beach Subgroup, Emperor Subgroup|Interleaved with Seaspray Group; unconformably overlies Strzelecki Group|Sandstone, mudstones, coal|
10217|Latrobe Group|24211|5|Briefly described|p86 Fig. 3||Late Cretaceous|Geological Province: Gippsland Basin.  See also p85 Fig. 2 and p84.||||||
10217|Latrobe Group|24403|5|Briefly described|p3|||Geological Province: Gippsland Basin. Maximum thickness: 2000m.||||||
10217|Latrobe Group|24405|6|Mentioned|p5|||Geological Province: Gippsland Basin.||||||12-AUG-04
10217|Latrobe Group|24407|5|Briefly described|p12, p13 Fig.2|Early Oligocene|Turonian|Includes the Halibut, Golden Beach, Emperor and Cobia subgroups. Geological Province: Gippsland Basin||||||
10217|Latrobe Group|24453|5|Briefly described|p809 Fig.2|Maastrichtian|Campanian|Unconfomably overlies Golden Beach Group. Geological Province: Gippsland Basin.||||||07-FEB-11
10217|Latrobe Group|24468|5|Briefly described|p405 Fig.2|||Geological Province: Gippsland Basin||||||
10217|Latrobe Group|24495|5|Briefly described|p9-10, p12|||Max. thickness: 3000m.  Geological Province: Gippsland Basin.||||||
10217|Latrobe Group|24551|5|Briefly described|p240, Fig. 9.2, 260, 475|Middle Tertiary|Late Cretaceous|Geological Province: Gippsland Basin.||||||
10217|Latrobe Group|24561|5|Briefly described|p44|Eocene|Cenomanian|Geological Province: Gippsland Basin. Includes non-marine to shallow marine sediments containing hydrocarbon-bearing units.||||||04-FEB-08
10217|Latrobe Group|24562|6|Mentioned|p141|||Geological Province: Gippsland Basin.||||||
10217|Latrobe Group|29650|6|Mentioned|p111|||||||||
10217|Latrobe Group|29721|6|Mentioned|p192|||||||||
10217|Latrobe Group|29736|6|Mentioned|p68|||||||||
10217|Latrobe Group|29974|6|Mentioned|p47|||||||||
10217|Latrobe Group|30365|6|Mentioned|p5|||Also Fig.5.||||||
10217|Latrobe Group|30836|4|Described|p1263|||Lower Cretaceous - Eocene age.||||||
10217|Latrobe Group|31159|6|Mentioned|p85|||See also P86, 87, 88.||||||
10217|Latrobe Group|31160|6|Mentioned|p78|||||||||
10217|Latrobe Group|31254|3|Fully described|p140|||See also p141.||||||20-JUL-06
10217|Latrobe Group|31480|4|Described|p71|||See also p72, 74.||||||20-JUL-06
10217|Latrobe Group|31646|6|Mentioned|p99|||||||||
10217|Latrobe Group|32162|5|Briefly described|p56|||Petroleum aspect||||||
10217|Latrobe Group|32245|6|Mentioned|p30|||||||||
10217|Latrobe Group|32374|6|Mentioned|p16|||||||||
10217|Latrobe Group|32574|6|Mentioned|p75|||Offshore environment||||||
10217|Latrobe Group|32679|5|Briefly described|p94|||||||||
10217|Latrobe Group|32712|6|Mentioned|Table 1|||||||||
10217|Latrobe Group|32715|6|Mentioned|p1176|||Oil||||||
10217|Latrobe Group|32995|6|Mentioned|Fig.10|||||||||
10217|Latrobe Group|33130|6|Mentioned|p60|||||||||
10217|Latrobe Group|33267|5|Briefly described|p70|||See also Fig.8||||||
10217|Latrobe Group|33319|6|Mentioned|p167|||Fauna||||||
10217|Latrobe Group|33320|4|Described|Fig.2|||Late Cret.-Late Eoc. 7 palynol. zones.||||||
10217|Latrobe Group|33321|6|Mentioned|p238|||||||||
10217|Latrobe Group|33362|5|Briefly described|p111|||||||||
10217|Latrobe Group|33425|6|Mentioned|Fig.2|||||||||
10217|Latrobe Group|35067|6|Mentioned|p1151|||||||||
10217|Latrobe Group|35151|6|Mentioned|p153|||||||||
10217|Latrobe Group|35573|6|Mentioned|Fig.3|||Chronostratigraphic section - Gippsland Basin||||||
10217|Latrobe Group|36102|6|Mentioned|p137|||||||||
10217|Latrobe Group|36310|6|Mentioned|p149|||||||||
10217|Latrobe Group|36331|6|Mentioned|Fig.1|||||||||
10217|Latrobe Group|36643|6|Mentioned|Fig.7|||||||||
10217|Latrobe Group|36751|6|Mentioned|p233|||||||||
10217|Latrobe Group|36916|6|Mentioned|p107|||||||||
10217|Latrobe Group|37130|5|Briefly described|p360|||||||||
10217|Latrobe Group|37809|6|Mentioned|p9|||||||||
10217|Latrobe Group|38313|6|Mentioned|Fig.2|||||||||
10217|Latrobe Group|38422|6|Mentioned|p145|||||||||
10217|Latrobe Group|38717|5|Briefly described|p21|||||||||
10217|Latrobe Group|38731|6|Mentioned|p26|||||||||
10217|Latrobe Group|38738|6|Mentioned|p262|||||||||
10217|Latrobe Group|38739|6|Mentioned|p285|||||||||
10217|Latrobe Group|38928|6|Mentioned|Fig.4|||||||||
10217|Latrobe Group|38931|5|Briefly described|p74|||Also mentioned Fig.5||||||
10217|Latrobe Group|39315|6|Mentioned|Fig.7|||||||||
10217|Latrobe Group|39757|6|Mentioned|p1603|||||||||
10217|Latrobe Group|40715|6|Mentioned|p59|||||||||
10217|Latrobe Group|40716|5|Briefly described|p67|||||||||
10217|Latrobe Group|41124|6|Mentioned|p253|||||||||
10217|Latrobe Group|41165|6|Mentioned|p368|||||||||
10217|Latrobe Group|41171|5|Briefly described|p166|||||||||
10217|Latrobe Group|41176|6|Mentioned|p215|||||||||
10217|Latrobe Group|41193|5|Briefly described|p313|||||||||
10217|Latrobe Group|41213|5|Briefly described|p242|||||||||
10217|Latrobe Group|41259|6|Mentioned|p448|||||||||
10217|Latrobe Group|41282|5|Briefly described|p32|||||||||
10217|Latrobe Group|41285|6|Mentioned|p101|||||||||
10217|Latrobe Group|41318|5|Briefly described|p181|||||||||
10217|Latrobe Group|41454|6|Mentioned|p63|||||||||
10217|Latrobe Group|41534|5|Briefly described|p12|||||||||
10217|Latrobe Group|41552|6|Mentioned|p459|||||||||
10217|Latrobe Group|41704|6|Mentioned|p110|||||||||
10217|Latrobe Group|41706|6|Mentioned|p145|||||||||
10217|Latrobe Group|41712|6|Mentioned|p272|||||||||
10217|Latrobe Group|41713|6|Mentioned|p290|||||||||
10217|Latrobe Group|41715|6|Mentioned|p317|||||||||
10217|Latrobe Group|41727|5|Briefly described|p433|||||||||
10217|Latrobe Group|41812|6|Mentioned|p18|||||||||
10217|Latrobe Group|41868|6|Mentioned|p504|||||||||
10217|Latrobe Group|41932|6|Mentioned|p22|||||||||
10217|Latrobe Group|41999|6|Mentioned|Fig.2 P3|||||||||
10217|Latrobe Group|42001|5|Briefly described|p79|||||||||
10217|Latrobe Group|42075|5|Briefly described|Fig.15 P253|||||||||
10217|Latrobe Group|42083|4|Described|p346|||See also Fig.9||||||
10217|Latrobe Group|42150|6|Mentioned|p67|||||||||
10217|Latrobe Group|42311|5|Briefly described|Fig.2 P526|early Tertiary|Late Cretaceous|||||||
10217|Latrobe Group|42555|5|Briefly described|p285|||||||||
10217|Latrobe Group|42649|5|Briefly described|Fig.3 P197-198|||||||||
10217|Latrobe Group|43145|4|Described|p9|Miocene|Cenomanian|See also p16. Onshore equivalent is Latrobe Valley Coal Measures.||||||20-JUL-06
10217|Latrobe Group|43578|6|Mentioned|p337|Oligocene|Late Cretaceous|||||||
10217|Latrobe Group|43711|6|Mentioned|p23|||||||||
10217|Latrobe Group|46961|6|Mentioned|p228|||||||||
10217|Latrobe Group|46988|6|Mentioned|p201|||||||||
10217|Latrobe Group|47045|6|Mentioned|p197|||||||||
10217|Latrobe Group|60538|5|Briefly described|p478, 483 Fig. 22|||Includes: Traralgon Coals. Geological Province: Gippsland Basin.||||||
10217|Latrobe Group|60666|5|Briefly described|p15 (Fig.)|||Includes the Golden Beach Subgroup.  Geological Province: Gippsland Basin.||||||23-DEC-04
10217|Latrobe Group|61155|5|Briefly described|p18|Late Miocene|Paleocene|Comprises Gurnard, Traralgon, Childers, Morwell and Yallourn Formations, and the Thorpdale Volcanics. Max. thickness: 4000m. Geological Province: Gippsland Basin. See p3, p8.||||||
10217|Latrobe Group|61212|6|Mentioned|p300, p301 Fig. 2|Early Eocene|Campanian|||||||
10217|Latrobe Group|61302|4|Described|p9|Oligocene|Paleocene|Overlies the Strzelecki Group. Geological Province: Gippsland Basin.||||||
10217|Latrobe Group|61323|5|Briefly described|p2, p3 Fig. 3|Tertiary|Cretaceous|Offshore marine mudstone. Geological Province: Gippsland Basin.||||||12-FEB-08
10217|Latrobe Group|61328|5|Briefly described|p111|Tertiary|Cretaceous|Geological Province: Gippsland Basin.||||||12-FEB-08
10217|Latrobe Group|61329|5|Briefly described|p121|Tertiary|Tertiary|Also referred to as Latrobe Valley Group.||||||
10217|Latrobe Group|61336|5|Briefly described|p(ii)|Late Eocene|Late Cretaceous|Name used interchangeably with Latrobe Valley Group. Predominantly non-marine coarse quartzose sands, clays and coals. Disconformably overlain by Lakes Entrance Formation (Seaspray Group).||||||07-FEB-11
10217|Latrobe Group|61469|5|Briefly described|p33|||Contains the Kingfish Formation, the sandstones of which are the main producing reservoir for the oil and gas fields of the basin.  Geological Province: Gippsland Basin.||||||12-OCT-05
10217|Latrobe Group|61470|6|Mentioned|p27|||||||||
10217|Latrobe Group|61552|4|Described|pp581-586, p590, p592, p595. |Early Oligocene|Turonian|Coal was continuously deposited in the Gippsland Basin from Turonian to Early Miocene. Middle Miocene compression produced folding and tilting of all the major structures that became the hosts for all the discovered commercial oil and gas accumulations in the Gippsland Basin.|||Includes Emperor, Golden Beach, Halibut and Cobia Subgroups.||Dominated by non-marine, fine- to medium-grained siliciclastics interspersed with coal horizons.|
10217|Latrobe Group|61607|6|Mentioned|p11, p5 Fig. 2|Oligocene|Late Cretaceous|Geological Province: Gippsland Basin.||||||12-MAR-09
10217|Latrobe Group|61627|6|Mentioned|p504|||Geological Province: Gippsland Basin.||||||07-FEB-11
10217|Latrobe Group|62370|6|Mentioned|p455|||Geological Province: Gippsland Basin.||||||
10217|Latrobe Group|63173|5|Briefly described|p342 Fig. 9.2|Early Oligocene|Late Cretaceous|Geological Province: Gippsland Basin, offshore.||||||07-FEB-11
10217|Latrobe Group|64876|5|Briefly described|p144-145|Late Cretaceous|Late Cretaceous|Gippsland Basin.|||Emperor, Golden Beach, Halibut, Cobia Subgroups.|Unconformably overlies Strzelecki Group. Is overlain by Seaspray Group (Latrobe Unconformity).||
10217|Latrobe Group|65717|5|Briefly described|p7, p9 Fig.2.2, p10, p12-15, p17, p25|Paleogene|Cretaceous|See also p28-32, p34-35, p37-38. Gippsland Basin. Is the primary reservoir of several oil and gas fields. Hosts all the known offshore hydrocarbon occurrences.|||Cobia, Halibut, Golden Beach, Emperor Subgroups.|Unconformably overlain by Seaspray Group.|Marine and non-marine siliciclastic sedimentary rocks.|05-SEP-17
10217|Latrobe Group|65718|5|Briefly described|p4, p5, p8, pp10-14, pp31-33, pp37-44|Eocene|Late Cretaceous|Hosts all known hydrocarbon occurences in the offshore. Distinct from the Latrobe Valley Group. > 1568 m to < 300 m thick. Contains onshore, non-marine alluvial, fluvial and coastal plain facies with extensive porous sand bodies.|||Includes Emperor Subgroup, Golden Beach Subgroup, Halibut Subgroup, and Cobia Subgroup.|Unconformably overlain by the Seaspray Group. Underlain by the Gurnard Formation.|Comprises a sequence of marine and non-marine siliclastics.|10-JAN-17
10217|Latrobe Group|65973|4|Described|p6, p12-14, p16-22, p24-25, p27, p29-35|Tertiary|Cretaceous|Gippsland Basin; hosts significant oil and gas accumulations and all known offshore accumulations. Structure is discussed. Marine and non-marine siliciclastics and fluvial, estuarine and coastal barrier depositional environments for sandstones. This unit is thickest in the Central Deep; at least 213m thick in Sole-1 drillhole. Intersected in Sole-1 drillhoe, Basker South-1, Basker-1, Dart-1 , Leatherjacket-1, Kipper-2, Judith-1, Hammerhead-1, East Pilchard-1, Longtom-1, Longtom-1/ST-1, Longtom-2/ST-1, Moby-1, Northright-1 , Sole-1 , Sweep-1, Gummy-1 and many more drillholes (see appendix). Petroleum characeristics are discussed. See alos p37-40, p57, p59, p61-62, p65, p70-71, p74, p76-78, p80-83, p85, p88-90, p92-93, p97, p100, p102, p104, p106, p108, p110, p112, p114-119, p123-144, p147, p149, p151, p155, p171, p182-184. |||Includes the Emperor Subgroup, Golden Beach Subgroup, Halibut Subgroup and Cobia Subgroup.|Overlain by the Seaspray Group.|Siliciclastic sedimentary rocks including sandstones, very coarse to granular, occasionally conglomeratic sandstones with minor siltstone.|
10217|Latrobe Group|66181|5|Briefly described|p310 Fig.5|Eocene|Turonian|Includes the Cobia, Halibut, Golden Beach and Emperor Subgroups. Unconformably underlies the Seaspray Group, unconformably overlies the Otway Group.||||||
10217|Latrobe Group|67367|5|Briefly described|p133.|Early Paleogene|Late Cretaceous|Coastal plain sediments are the major source interval for oil and gas in the offshore Gippsland Basin. Sherbrook, Wangerrip and Nirranda Groups are its stratigraphic equivalents in the Otway Basin.||||||
10217|Latrobe Group|67727|5|Briefly described|p58 Fig.2.|Middle Eocene|Lower Eocene|Offshore Gippsland Basin; paralic deposits, equivalent to the onshore fluvial Honeysuckle Hill Gravels.||||Overlain by Flounder and Turrum Formations.||
10217|Latrobe Group|69016|6|Mentioned|p89-101|||Of the Gippsland Basin. See Latrobe Valley Group.||||||
10217|Latrobe Group|69879|5|Briefly described|p417, p428|Turonian|Turonian|Gippsland Basin. Age inferred from Emperor Subgroup.|||Includes Emperor Subgroup, Halibut Subgroup.|||
10217|Latrobe Group|70028|5|Briefly described|p77, 79-82, p83 Fig.5, p91-92|Oligocene|Turonian|Gippsland Basin. Hydrocarbon reservoir.|||Emperor, Golden Beach, Halibut, Cobia Subgroups.|Unconformably overlies Strzelecki Group. Is overlain unconformably by Seaspray Group.|Includes thick layers of coal in the upper parts.|
10217|Latrobe Group|70076|5|Briefly described|South-Eastern: Fig.2; p1-2|Rupelian|Turonian|See also Regional: Fig.3; p1-8. Source and host of most hydrocarbon accumulations in the Gippsland Basin in fold structures related to Late Eocene compression. Mainly marginal marine to lower coastal plain depositional environments.|||Emperor, Golden Beach, Halibut, Cobia Subgroups.|Overlies Strzelecki Group. Is overlain by Seaspray Group.|Includes coals and carbonaceous shales.|
10217|Latrobe Group|70331|5|Briefly described|p69-70|Oligocene|Late Cretaceous|Gippsland Basin (western). Hosts all of the known hydrocarbon occurrences in the offshore Gippsland Basin.|||Emperor, Golden Beach, Halibut, Cobia Subgroups.|Unconformably overlies Strzelecki Group. Is overlain by Seaspray Group.|A sequence of marine and non-marine siliciclastics.|
10217|Latrobe Group|73289|5|Briefly described|p766 Fig.3, 774 Fig.10||||||Yallourn Coal Seam; Thorpdale, Carrajung Volcanics.|Is overlain unconformably by Haunted Hill Formation.||
10217|Latrobe Group|73471|5|Briefly described|p84, p86-87, p90, p100 Fig.10, p102|Rupelian|Cenomanian|Gippsland Basin. Hosts all currently known hydrocarbon accumulations in the Gippsland Basin. Overlies Otway Unconformity. Deposited in east-draining depositional system following the Albian-Cenomanian inversion.|95-32 Ma||Emperor Subgroup, Golden Beach Subgroup, Halibut Subgroup, Cobia Subgroup|Unconformably overlies Strzelecki Group, underlies Seaspray Group||
10217|Latrobe Group|73562|5|Briefly described|p300-303, 305-307, 312-316|Eocene|Late Cretaceous|Gippsland Basin. Late Cretaceous to Miocene deposition of 23 stacked, coastal plain - shoreface units was mainly driven by basin subsidence. The authors present a ""simplified [stratigraphic] nomenclature"". Hosts extensive hydrocarbon quantities sourced from coals lower in the Group.|||Gurnard, Traralgon, Turrum, Flounder Formations.|Overlies Strzelecki Group. Is overlain by Seaspray Group.|Non-marine to marginal marine sediments; sandstones, thick brown coal deposits, glauconitic sandstone.|
10217|Latrobe Group|73594|6|Mentioned|p8|Early Paleogene|Late Cretaceous|Gippsland Basin. Coastal plain and fluvio-deltaic.||||||
10217|Latrobe Group|73640|5|Briefly described|p2-3|Eocene|Late Cretaceous|Gippsland Basin. Post-rift passive sag stage deposits in shallow marine, barrier, back barrier swamp, fluvial, and lacustrine settings. Upper sucession forms hydrocarbon reservoirs sourced from lower succession Late Cretaceous to Paleocene coals. Onshore Oligocene-Miocene brown coals are mined.|||Flounder, Gurnard, Traralgon, Turrum Formations.|||
10217|Latrobe Group|75065|5|Briefly described|p149, 151-152, 154-156, 166, 168|Oligocene|Cenomanian|See also p170-171. Gippsland Basin. Fluvial and lacustrine sediments, becoming more coastal plain and shallow-marine up-section.|||Emperor, Golden Beach, Halibut Subgroups.|Unconformably overlies Strzelecki Group. Is overlain unconformably by Latrobe Valley and Seaspray Groups.||
39333|Latrobe Valley Subgroup|13323|5|Briefly described|p393 Fig. 2|Late Oligocene|Early Oligocene|Of the Seaspray Group (onshore). Non-marine to paralic clastics. Geological Province: Gippsland Basin. See also p394 Fig. 3.||||||26-JUN-06
39333|Latrobe Valley Subgroup|24090|5|Briefly described|p8 Fig.3|Oligocene|Oligocene|Geological Province: Gippsland Basin.||||||
39333|Latrobe Valley Subgroup|24407|5|Briefly described|p13 Fig.2|Oligocene|Oligocene|Geological Province: Gippsland Basin||||||
39333|Latrobe Valley Subgroup|61552|6|Mentioned|p583 Fig.2. |Late Oligocene|Early Oligocene|||Unit in Seaspray Group.|Includes Balook, Lakes Entrance and Swordfish Formations.|||
39333|Latrobe Valley Subgroup|64876|5|Briefly described|p145 Fig.2|Oligocene|Oligocene|Gippsland Basin.||Seaspray Group.||||
39333|Latrobe Valley Subgroup|65717|5|Briefly described|p9 Fig.2.2|Oligocene|Oligocene|||Seaspray Group|Includes Balook Formation, Lakes Entrance Formation|||05-SEP-17
39333|Latrobe Valley Subgroup|66181|6|Mentioned|p310 Fig.5|Miocene|Oligocene|In the Seaspray Group.||||||
39333|Latrobe Valley Subgroup|70028|6|Mentioned|p79|Miocene|Oligocene|Onshore Gippsland Basin.||||||
39333|Latrobe Valley Subgroup|70076|5|Briefly described|Regional: Fig.3|Tortonian|Rupelian||||Yallourn and Morwell Formations.|Overlies Traralgon Formation. Is overlain by Sale Subgroup.||
34333|Laura Formation|22674|4|Described|p718, Fig.2 p719|Barremian|Barremian|||||||
72945|Lauriston Sandstone|61186|5|Briefly described|p37, p81|Permian|Permian|Victorian dimension stone - fine-grained, pale brown featureless, massive rock with variable clay content. Probably an informal trade name.||||||
72945|Lauriston Sandstone|64769|6|Mentioned|p26|Permian|Permian|VIC.||||||06-MAY-09
22177|Lazarini Siltstone|23309|5|Briefly described|p145, 150, 152, 273, 274. Tb 2.53/2.57||Llandovery|||||||
22177|Lazarini Siltstone|24214|6|Mentioned|p788 Fig. 2|||||||||
22177|Lazarini Siltstone|24551|5|Briefly described|p123, p88 Fig. 3.15|Silurian|Silurian|Of Jordan River Group.||||||22-DEC-08
22177|Lazarini Siltstone|44187|5|Briefly described|Map Legend||Early Silurian|||||||
22177|Lazarini Siltstone|64535|5|Briefly described|Map legend|Silurian|Early Silurian|Of Jordan River Group. Siltstone -dark grey to green-grey, poorly bedded, strongly bioturbated to massive; minor quartz sandstone, pale, thin-bedded, fine- to very fine-grained; deep marine hemipelagic deposits.||||||
22177|Lazarini Siltstone|64536|5|Briefly described|Map legend|Silurian|Early Silurian|Of Jordan River Group. Siltstone -dark grey to green-grey, poorly bedded, strongly bioturbated to massive; quartz sandstone, pale, thin-bedded, fine- to very fine-grained; deep marine hemipelagic deposits.||||||07-FEB-11
22177|Lazarini Siltstone|64537|5|Briefly described|Map legend|Silurian|Early Silurian|Of Jordan River Group. Siltstone -dark grey to green-grey, poorly bedded, strongly bioturbated to massive; quartz sandstone, pale, thin-bedded, fine- to very fine-grained; deep marine hemipelagic deposits.||||||07-FEB-11
22177|Lazarini Siltstone|64538|5|Briefly described|Map legend|Silurian|Early Silurian|Of Jordan River Group. Siltstone -dark grey to green-grey, poorly bedded, strongly bioturbated to massive; quartz sandstone, pale, thin-bedded, fine- to very fine-grained; deep marine hemipelagic deposits.||||||07-FEB-11
22177|Lazarini Siltstone|64539|5|Briefly described|Map legend|Silurian|Early Silurian|Of Jordan River Group. Siltstone -dark grey to green-grey, poorly bedded, strongly bioturbated to massive; minor quartz sandstone, pale, thin-bedded, fine- to very fine-grained; deep marine hemipelagic deposits.||||||
22177|Lazarini Siltstone|64540|5|Briefly described|Map legend|Silurian|Early Silurian|Of Jordan River Group. Siltstone -dark grey to green-grey, poorly bedded, strongly bioturbated to massive; minor quartz sandstone, pale, thin-bedded, fine- to very fine-grained; deep marine hemipelagic deposits.||||||22-DEC-08
22177|Lazarini Siltstone|64605|5|Briefly described|Map legend|Silurian|Silurian|Of the Jordan River Group. Siltstone, minor sandstone; deep-marine deposits. Blue-brown to white in RGB. Nonmagnetic.||||||17-NOV-08
22177|Lazarini Siltstone|64606|5|Briefly described|Map Legend|Cambrian|Cambrian|Siltstone, minor sandstone: deep-marine deposits. Blue-brown to white in RGB. Nonmagnetic.||||||
22177|Lazarini Siltstone|64616|2|Defined|p76, p165, p183 Fig.6.29, p184-185, p189|Llandovery|Hirnantian|See also p197 Fig.6.34, p201 Tb.7.1, p281, p283-284, p292, p306. Basal unit of Jordan River Group. Conformable over Mount Easton Shale and under Donnellys Creek Siltstone. Type section location given. Age inferred from relationships - Bolindian (Bo4, Bo5) to Llandovery. 50-625m thick. Thick-bedded siltstone; large burrows; minor quartz sandstone, thin-bedded, fine- to very fine-grained. Geophysical characteristics given.||||||
22177|Lazarini Siltstone|68116|5|Briefly described|Appendix, Maps 25, 33-34, 43.|Rhuddanian|Katian|Maximum age as Bolindian in text.|||||Dark grey to green-grey siltstone with bedding in the form of colour banding; abundant dark bioturbation blebs; lowest portion contains interbedded quartz sandstone beds.|
30462|Lazy Bar Andesite|23309|5|Briefly described|p28-30. Tb 2.4|||Of the Heathcote Volcanics.||||||10-NOV-08
30462|Lazy Bar Andesite|24177|4|Described|p38|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Overlain by the Mount William Metabasalt. Overlies the Sheok Gully Boninite. Intruded by Commissioners Flat Granodiorite.||||||27-JUN-13
30462|Lazy Bar Andesite|24328|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics.||||||10-NOV-08
30462|Lazy Bar Andesite|24329|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics.||||||10-NOV-08
30462|Lazy Bar Andesite|24551|4|Described|p85|Cambrian|Cambrian|Of Heathcote Volcanics. Overlies Sheoak Gully Boninite.||||||
30462|Lazy Bar Andesite|60591|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Deep marine andesite: fine- to medium-grained, non-vesicular, porphyritic; minor hyaloclastite breccia, andesitic volcanic sandstone, ash with possible pumice.||||||27-JUN-13
30462|Lazy Bar Andesite|60592|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Deep marine andesite: fine- to medium-grained, non-vesicular, porphyritic; minor hyaloclastite breccia, andesitic volcanic sandstone, ash with possible pumice.||||||27-JUN-13
30462|Lazy Bar Andesite|60593|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Deep marine andesite: fine- to medium-grained, non-vesicular, porphyritic; minor hyaloclastite breccia, andesitic volcanic sandstone, ash with possible pumice.||||||27-JUN-13
30462|Lazy Bar Andesite|60595|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Deep marine andesite: fine- to medium-grained, non-vesicular, porphyritic; minor hyaloclastite breccia, andesitic volcanic sandstone, ash with possible pumice.||||||27-JUN-13
30462|Lazy Bar Andesite|60596|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Deep marine andesite: fine- to medium-grained, non-vesicular, porphyritic; minor hyaloclastite breccia, andesitic volcanic sandstone, ash with possible pumice.||||||27-JUN-13
30462|Lazy Bar Andesite|60597|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Nonmagnetic (<1 nT) with moderately magnetic trends; low K, Th and U.||||||27-OCT-08
30462|Lazy Bar Andesite|60599|2|Defined|p7, p24 Tb. 4, p35-36|Early Cambrian|Early Cambrian|Of Heathcote Volcanics (formerly an unnamed section of Heathcote Greenstone). Highly weathered,contains andesitic lava, andesitic sandstone, minor ash. Overlain by Mount William Metabasalt. Intruded by Commissioners Flat Granodiorite. Geol.Prov.: LFB. ||||||
30462|Lazy Bar Andesite|64611|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of Heathcote Volcanic Group. Fine- to medium-grained, non-vesicular, porphyritic andesite with minor hyaloclastic breccia, andesitic volcanic sandstone and ash with possible pumice; deep-marine volcanics and volcaniclastic deposits.||||||15-DEC-08
30462|Lazy Bar Andesite|64612|1|Redefined|p29, p32-33|Cambrian|Cambrian|Edwards et al. (1998).Of Heathcote Volcanic Group. Conformable relationship with Mount William Metabasalt. Thickness: 130m. Pale green, fine to medium-grained massive porphyritic andesite. Submarine environment.||||||27-JUN-13
30462|Lazy Bar Andesite|65715|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Heathcote Volcanic Group. Formation rank.||||||
30462|Lazy Bar Andesite|65969|6|Mentioned|p11|Cambrian|Cambrian|Of Heathcote Volcanic Group.||||||
30462|Lazy Bar Andesite|68116|5|Briefly described|Appendix, Map 24.|Cambrian|Cambrian||||||Andesite: fine- to medium-grained, non-vesicular, porphyritic; minor hyaloclastite breccia, andesitic volcanic sandstone, ash with possible pumice; marine to sub-aerial deposit.|
30462|Lazy Bar Andesite|70601|5|Briefly described|p44, p47|Early Cambrian|Early Cambrian|Kilmore/Heathcote area. Age range from Botomian trilobites (Jell, 2014).|ca 516-513 Ma. |Heathcote Volcanics||Correlated with lower part of Lickhole Volcanics. |Andesite.|
30462|Lazy Bar Andesite|73497|5|Briefly described|Map legend|Cambrian|Cambrian|||Heathcote Volcanic Group||Overlies Sheoak Gully Boninite, underlies Mount William Metabasalt|Andesite, volcanic sediment: nonmagnetic but with magnetic trends to 300 nT; low K, Th and U.|
10350|Lerderderg Gravel Member|39865|4|Described|p31|||||||||
10350|Lerderderg Gravel Member|65715|5|Briefly described|p13|||Formerly Lerderderg Formation. Only occurs in the subsurface. Included as a member of Werribee Formation by Roberts (1984).||||||
72621|Leviathan Formation|62741|5|Briefly described|p680 Fig. 2|||Contains a sand-rich unit. See also p682 Fig. 4b and p683 Fig. 5a.||||||
72621|Leviathan Formation|62742|5|Briefly described|p698|Early Cambrian|Early Cambrian|Conformably overlies Albion Formation. In the Stawell Zone. ||||||
72621|Leviathan Formation|62744|5|Briefly described|p709 Fig. 2|Cambrian|Cambrian|Quartz-rich sandstones and minor black mudstones. Overlies the intercalated Albion Formation and Magdala Basalt. Geological Province: Stawell Zone.||||||
72621|Leviathan Formation|62747|5|Briefly described|p734 Fig. 1|||Fine- to medium-grained sandstone; pervasively muscovite-altered.||||||28-NOV-06
72621|Leviathan Formation|62749|5|Briefly described|p722|||Mainly fine- to medium-grained quartz-rich sandstone. Conformably overlies Albion Formation. Max. thickness: 1500m.||||||
72621|Leviathan Formation|62751|5|Briefly described|p759|||Sandstone-dominated unit, recording a major flux of coarse-grained quatrz-rich detritus. Conformably overlies Albion Formation. See also p 761 Fig. 2||||||22-JAN-07
72621|Leviathan Formation|62752|5|Briefly described|p759, p761 Fig. 2|||Sandstone-dominated unit - records a major flux of coarse-grained quartz-rich detritus. Conformably overlies the Albion Formation.||||||
72621|Leviathan Formation|62753|5|Briefly described|p800, p802 Fig.2|||Quartz-rich unit. Overlies Albion Formation.||||||
72621|Leviathan Formation|64597|5|Briefly described|p760 Fig.1, p761. |||Pervasively muscovite altered.||||Overlies the Albion Formation.|Sandstone.|
72621|Leviathan Formation|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Saint Arnaud Group. Defined by Squire and Wilson 2005, p752||||||
72621|Leviathan Formation|67847|6|Mentioned|p10 fig 2.3|Ordovician|Ordovician|||||||
72621|Leviathan Formation|68116|5|Briefly described|Appendix, Map 30.|Early Cambrian|Early Cambrian||||||Fine- to medium-grained turbiditic, deep marine sandstone, with minor interbedded siltstone and shale; pervasively muscovite altered.|
72621|Leviathan Formation|68314|5|Briefly described|p750, p752, p754-757|Middle Cambrian|Early Cambrian|Stawell area. Three facies described. At least 1500 m thick. Age and detrital composition closely match those of the Junction Formation in New Zealand. Was buried rapidly to between 15 and 20 km during a late Botoman compressive regime in E Gondwana.||||Conformably overlies Albion Formation.|Pale grey to cream. Well-sorted, very fine-grained, massive siliceous siltstone; massive, well-sorted, calcareous sandstone and siltstone predominantly composed of calcite grains; thick-bedded, poorly sorted mudstone lithic breccia.|26-FEB-18
72621|Leviathan Formation|70493|6|Mentioned|p56|Early Cambrian|Early Cambrian|Western Stawell Zone, Lachlan Orogen.||||Overlies Albion Formation.||
72621|Leviathan Formation|73059|5|Briefly described|p1059-1061, 1064|Middle Cambrian|Early Cambrian|Western Stawell Zone. Detrital zircon age plots; 600-560 Ma interval.||Saint Arnaud Group.||Overlies Albion Formation.||
72621|Leviathan Formation|73177|6|Mentioned|1114 Fig.16|||||||||
72621|Leviathan Formation|73264|6|Mentioned|p1389 Fig.11|Early Cambrian|Early Cambrian|Lachlan Orogen.||||||
72621|Leviathan Formation|75072|6|Mentioned|p232, 237|Late Cambrian|Late Cambrian|Stawell Zone, Central Victoria. Zircon age distribution.||Saint Arnaud Group.||||
35111|Lewis Farm Conglomerate|22971|5|Briefly described|p18|Late Devonian|Middle Devonian|Fluvial and colluvial deposits.||||||19-JAN-06
35111|Lewis Farm Conglomerate|23309|5|Briefly described|p160, 169, 184. Tb 2.58/2.63/2.64|Frasnian|Givetian|Age: 370 Ma.||||||05-SEP-18
35111|Lewis Farm Conglomerate|24551|4|Described|p166, 170, 635|Givetian|Givetian|Maximum Thickness: 100m. Overlying unit: Hollands Creek Rhyodacite.||||||
35111|Lewis Farm Conglomerate|61163|5|Briefly described|p89 Tb. 8.1|||Grouped within Bennies Fm subdivision of Tolmie Igneous Complex. Upward-fining sequence of quartzose conglomerate and interbedded sandstone consisting of entirely of basement  clasts; conglomerate in thick-bedded showing channel structures; fish fauna.||||||
35111|Lewis Farm Conglomerate|64616|6|Mentioned|p157|Middle Devonian|Middle Devonian|Base of Tolmie Igneous Complex underneath Mansfield Basin. Among the oldest rocks to overlie unconformably Tabberabberan Orogeny-folded rocks. ||||||
35111|Lewis Farm Conglomerate|69669|5|Briefly described|p952|Devonian|Devonian|Givetian age from palaeontological evidence.|392-385 Ma; Long and Werdelin (1986).|||Underlies Tolmie Igneous Complex.||
37571|Lexington Schist|23309|5|Briefly described|p65, 227. Table 2.23|||Of Moornambool Metamorphic Complex.||||||
37571|Lexington Schist|60451|4|Described|p57, 72, 114, 167|||Of the Moornambool Metamorphic Complex. Warrak formation probably protolith of this unit. Derived from Saint Arnaud Group and Deenicull Schist. Type section in text. May grade laterally into Good Morning Bill Schist. Some contact metaorphism.||||||
37571|Lexington Schist|60454|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-biotite-muscovite-plagioclase (+/-actinolite+/-cordierite+/-andalusite) schist.||||||
37571|Lexington Schist|60456|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-biotite-muscovite-plagioclase (+/-actinolite+/-cordierite+/-andalusite) schist.||||||
37571|Lexington Schist|60457|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-biotite-muscovite-plagioclase (+/- actinolite +/- cordierite+/-andalusite) schist: banded schist with alternating quartz and pelite layers of transposed bedding.||||||20-MAY-13
37571|Lexington Schist|60458|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-biotite-muscovite-plagioclase (+/-actinolite+/-cordierite+/-andalusite) schist: banded schist with alternating quartz and pelite layers.||||||
37571|Lexington Schist|60459|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-biotite-muscovite-plagioclase (+/-actinolite+/-cordierite+/-andalusite) pelitic schist with minor intermediate and mafic igneous components. Greenschist to amphibolite grade.||||||
37571|Lexington Schist|61187|5|Briefly described|p82, p83 Fig.1, p84 Fig.2.|||Stawell Zone. Brought to the surface along the Moyston Fault. Part of this unit may have the Magdala Metabasalt as precursor. Has high total count/high-K radiometric response. Hosts a narrow, volcanigenic-banded sulphide (mainly chalcopyrite-pyrrhotite) body. Susceptibility measures given.||||Is intercalated with Carrolls Amphibolite.|Quartz actinolite schist and quartz biotite schist.|
37571|Lexington Schist|66002|5|Briefly described|p5 Tb.2|Cambrian|Cambrian|Of Moornambool Metamorphic Complex. Defined by Cayley and Taylor 2001.||||||
37571|Lexington Schist|68116|5|Briefly described|Appendix, Maps 22, 30.|Late Cambrian|Late Cambrian||||||Quartz-biotite-muscovite-plagioclase (+/-actinolite+/-cordierite+/-andalusite) schist: banded schist with alternating quartz and pelite layers of transposed bedding; low to moderately magnetic.|
37571|Lexington Schist|71593|6|Mentioned|p36|||||Moornambool Metamorphic Complex||||
22190|Lexton Granodiorite|22756|5|Briefly described|P49, Table2|Carboniferous|Early Devonian|Informally referred to as Burnbank Granodiorite||||||
22190|Lexton Granodiorite|23309|5|Briefly described|p435, App1|||G370 I-Type. Supersedes Burnbank Granodiorite. Age: 396 +/- 5 Ma, 383 +/- 5Ma, 384 +/- 12Ma, 374 +/- 11 Ma.||||||
22190|Lexton Granodiorite|43260|5|Briefly described|Map Legend||Early Devonian|of Glenlogie Suite. Hornblende-biotite granodiorite: pale grey to pink, medium grained; with accessory magnetite.||||||27-OCT-04
22190|Lexton Granodiorite|66002|5|Briefly described|p7 Tb.5|||Of Glenlogie Suite. G370.  Defined by Cayley and McDonald 1995.||||||
22190|Lexton Granodiorite|68116|5|Briefly described|Appendix, Map 31.|Early Devonian|Early Devonian||||||Hornblende-biotite granodiorite: pale grey to pink, medium grained; with accessory magnetite; fractionated, pale cream, fine grained, foliated phase forms Granite Hill.|
37572|Lickhole Volcanic Group|23309|5|Briefly described|p23,33, table 2.4|Cambrian|Cambrian|See also Lickhole Volcanics.||||||
37572|Lickhole Volcanic Group|24551|4|Described|p90|||||||||
37572|Lickhole Volcanic Group|62742|5|Briefly described|p699 Fig. 2|Early Cambrian|Early Cambrian|In the Mount Wellington Greenstone Belt.||||||
37572|Lickhole Volcanic Group|62744|5|Briefly described|p709 Fig. 2|Cambrian|Cambrian|Geological Province: Mount Wellington Greenstone Belt.||||||
37572|Lickhole Volcanic Group|64616|6|Mentioned|p148|Cambrian|Cambrian|Appears as Lickhole Volcanic Complex. Source of some clasts deposited by Howqua River.||||||
37572|Lickhole Volcanic Group|66196|6|Mentioned|p616|Early Cambrian||Tholeiitic basalt and boninite, conformably underlies the Howqua Chert. See also Lickhole Volcanics, same page.||||||04-SEP-14
37572|Lickhole Volcanic Group|66769|6|Mentioned|136|Cambrian|Cambrian|Stratigraphic and structural equivalent to the Dookie Igneous Complex.||||||
37572|Lickhole Volcanic Group|68314|6|Mentioned|p753-754|Early Cambrian|Early Cambrian|Mount Wellington Greenstone Belt.||||||
22192|Licola Volcanics|22708|6|Mentioned|p210|||||||||
22192|Licola Volcanics|23307|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||
22192|Licola Volcanics|23309|4|Described|p25, 34-39. Table 2.1/ 2.7|Cambrian|Cambrian|||||||
22192|Licola Volcanics|24002|4|Described|p237|Cambrian|Cambrian|||||||
22192|Licola Volcanics|24098|5|Briefly described|p27 Fig. 2, p30, p34|Cambrian|Cambrian|Geological Province: Melbourne Zone, Lachlan Fold Belt.||||||19-APR-05
22192|Licola Volcanics|24551|6|Mentioned|p87|||||||||
22192|Licola Volcanics|61187|5|Briefly described|p5 Fig.3. |Early Cambrian|Early Cambrian|Melbourne Zone. Correlated with Mount Stavely Volcanics (Glenelg Zone), Heathcote Volcanics (Bendigo Zone), Jamieson Volcanics (Melbourne Zone), and Lickhole Volcanics (Tabberabbera Zone, Benambra Terrane). Age interpreted from Fig.3.|c.560-c.540 Ma.|||||
22192|Licola Volcanics|64616|5|Briefly described|p62-63, p179, p181 Fig.6.28, p190, p192|Cambrian|Cambrian|See also p198 Fig.6.35, p199, p257 Fig.8.31, p259, p281. Variation on Licola Volcanic Group. Same unit. Includes pure limestone in andesitic breccia, suggesting shallow marine environment. Regionally metamorphosed. Overlain by Wahroonga Breccia.||||||
22192|Licola Volcanics|66769|5|Briefly described|121, 136, 156 Fig 8, 13, 15|Cambrian|Cambrian|Selwyn Block. Calcalkaline volcanics.||||||
22192|Licola Volcanics|67103|5|Briefly described|p613 Fig.6, 617-618|||Central Victoria.||||Correlated with Mount Read Volcanics (TAS).|Volcanic sequence with calc-alkaline magmatic arc signatures.|
22192|Licola Volcanics|67847|5|Briefly described|p10 fig 2.3|Upper Cambrian|Upper Cambrian||||||Andesitic volcanics. |
22192|Licola Volcanics|69876|6|Mentioned|p297 Fig.6.19|||Melbourne Zone, Vic. Shown as an overthrust belt of Cambrian volcanics.||||||
22192|Licola Volcanics|73059|6|Mentioned|p1062|||Eastern margin of the Melbourne Zone. Post-Delamerian collisional volcanism.||||||
25166|Lilly Pilly Granite|23309|6|Mentioned|p435 App1|||G256 S-Type.||||||
25166|Lilly Pilly Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
25166|Lilly Pilly Granite|68116|5|Briefly described|Appendix, Map 57.|Middle Devonian|Middle Devonian||||||Granite: red-brown biotite is ubiquitous and garnet is prominent in some rocks; S-type.|
28680|Lilydale Limestone|22530|6|Mentioned|p698|||||||||
28680|Lilydale Limestone|22570|6|Mentioned|p189|Pragian|Lochkovian|||||||
28680|Lilydale Limestone|22628|6|Mentioned|fig1p108|Devonian|Devonian|||||||
28680|Lilydale Limestone|23229|5|Briefly described|Table3-3p26, 28, 31|Pragian|Pragian|||||||
28680|Lilydale Limestone|23308|6|Mentioned|Map Legend|||Mine name?||||||
28680|Lilydale Limestone|23309|5|Briefly described|Tb 2.52, p140-141, 150, 153.||Devonian|||||||
28680|Lilydale Limestone|23522|5|Briefly described|p246|Middle Devonian|Early Devonian|||||||
28680|Lilydale Limestone|24002|5|Briefly described|p228 Fig.2|Devonian|Devonian|||||||
28680|Lilydale Limestone|24098|5|Briefly described|p27 Fig. 2|Emsian|Pragian|Of the Murrindindi Supergroup. Geological Province: Melbourne Zone, Lachlan Fold Belt.||||||19-APR-05
28680|Lilydale Limestone|24177|5|Briefly described|p50 Fig.22|Early Devonian|Early Devonian|Geological Province: Darraweit Guim Province||||||07-JUN-06
28680|Lilydale Limestone|24383|6|Mentioned|p88 Fig.57|||Geological Province: Lachlan Fold Belt.||||||14-APR-08
28680|Lilydale Limestone|24551|5|Briefly described|p126|||||||||
28680|Lilydale Limestone|24588|5|Briefly described|p12 Fig.3, p32|Pragian|Pragian|Geological Province: Darraweit Guim Province.||||||29-NOV-13
28680|Lilydale Limestone|30245|6|Mentioned|p79|||Conodonts listed and figured by Philip and Pedder||||||
28680|Lilydale Limestone|30253|6|Mentioned|Fig.4|||||||||
28680|Lilydale Limestone|30597|6|Mentioned|p31|||Early Siegenian age||||||
28680|Lilydale Limestone|31331|6|Mentioned|p182|||See also P189||||||
28680|Lilydale Limestone|31503|6|Mentioned|p2|||||||||
28680|Lilydale Limestone|32074|5|Briefly described|p180|||||||||
28680|Lilydale Limestone|32076|4|Described|p203|||See also stratigraphy p201.||||||15-JAN-09
28680|Lilydale Limestone|32077|4|Described|p33|||See also p34-35.||||||15-JAN-09
28680|Lilydale Limestone|32984|6|Mentioned|p343|||Fossil content||||||
28680|Lilydale Limestone|33326|6|Mentioned|p437|||Fauna.||||||
28680|Lilydale Limestone|33407|4|Described|p1|||Gastropod fauna.||||||
28680|Lilydale Limestone|33408|6|Mentioned|p232|||||||||
28680|Lilydale Limestone|33599|6|Mentioned|p6|||Refers Gill (1965).||||||
28680|Lilydale Limestone|33601|6|Mentioned|p33|||||||||
28680|Lilydale Limestone|33732|6|Mentioned|p105|||||||||
28680|Lilydale Limestone|33817|5|Briefly described|p121|||Ostracods. See also PP122, 128, 136. Early Siegenian||||||
28680|Lilydale Limestone|33968|4|Described|p5|Early Devonian|Early Devonian|Lower Devonian.||||||15-JAN-09
28680|Lilydale Limestone|34287|6|Mentioned|p96|||||||||
28680|Lilydale Limestone|34954|6|Mentioned|Fig.34|||||||||
28680|Lilydale Limestone|35193|6|Mentioned|p21|||||||||
28680|Lilydale Limestone|35237|6|Mentioned|p43|||||||||
28680|Lilydale Limestone|36587|6|Mentioned|p3|||||||||
28680|Lilydale Limestone|38787|6|Mentioned|p125|||||||||
28680|Lilydale Limestone|39331|6|Mentioned|Table 2-1|||||||||
28680|Lilydale Limestone|41585|4|Described|p110|||||||||
28680|Lilydale Limestone|42015|6|Mentioned|p316|||||||||
28680|Lilydale Limestone|42033|6|Mentioned|p653|||||||||
28680|Lilydale Limestone|42635|6|Mentioned|p46|||||||||
28680|Lilydale Limestone|42827|5|Briefly described|p110, Table 4.1|||same as Lilydale Limestone Member.||||||27-OCT-08
28680|Lilydale Limestone|42938|5|Briefly described|p576 Fig.3|||||||||
28680|Lilydale Limestone|43461|14|Not recorded|p627||Emsian|||||||
28680|Lilydale Limestone|43525|14|Not recorded|p130,Tb p131,132|||||||||
28680|Lilydale Limestone|43529|14|Not recorded|p233||Siegenian|Early Siegenian||||||
28680|Lilydale Limestone|43530|14|Not recorded|p1025,1028-30||Siegenian|L.Siegenian||||||
28680|Lilydale Limestone|43531|14|Not recorded|p795-797||Siegenian|Was regarded as L.or M.Devonian (Yearing Group) Correlated with Coopers Crk Fm (Early Siegenian)||||||
28680|Lilydale Limestone|43532|14|Not recorded|p201,211,216,220||Devonian|Revision of Devonian Mictophyllum. See also Lexicon||||||
28680|Lilydale Limestone|43537|14|Not recorded|p3,7,28|||Lilydale area. Devonian tetracorals||||||
28680|Lilydale Limestone|43547|14|Not recorded|p148,150,Table p152||Emsian|Part of Yering Group.||||||14-APR-08
28680|Lilydale Limestone|45075|6|Mentioned|p49|||Devonian||||||
28680|Lilydale Limestone|48971|6|Mentioned|p9|||See also P11,12,14,18,20,21,22,25,26,27,28,29,30.||||||
28680|Lilydale Limestone|60599|5|Briefly described|p47 Fig. 19|Pragian|Lochkovian|Geological Province: Darraweit Guim Province, Melbourne Zone, Lachlan Fold Belt.||||||
28680|Lilydale Limestone|61120|6|Mentioned|p2, p4.  |||Inner shelf marginal and littoral facies. Has a karstified surface.||||Is unconformably overlain by Cave Hill Sandstone.||
28680|Lilydale Limestone|61138|6|Mentioned|p208 Fig.1|||||||||
28680|Lilydale Limestone|61181|6|Mentioned|p129 Tb. 32|||Same unit as Lilyvale Limestone Member. ||||||
28680|Lilydale Limestone|61185|5|Briefly described|p21 Fig. 6|Pragian|Lochkovian|Overlies Humevale Siltstone. Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
28680|Lilydale Limestone|61186|5|Briefly described|p45 Fig. 14, p90|Early Devonian|Early Devonian|Victorian dimension stone - fine-grained, hard and dark grey in colour; part is coarse-grained with veins and patches; rich in fossil fragments displaying corals, brachiopods and crinoids. ||||||
28680|Lilydale Limestone|61187|5|Briefly described|p5 Fig.3. |Early Devonian|Early Devonian|Melbourne Zone, Melbourne Terrane. Correlative of Wentworth Group (Tabberabbera Zone, Benambra Terrane) and Buchan Group (Buchan and Mallacoota Zones, Benambra Terrane).||||||
28680|Lilydale Limestone|62469|5|Briefly described|p5 Fig. 2, p59 Fig. 23|Emsian|Pragian|In Lilydale area. Geological Province: Darraweit Guim Province.||||||12-FEB-15
28680|Lilydale Limestone|64616|6|Mentioned|p343 Fig.23, p386|Early Devonian|Early Devonian|Central Victoria. Contains no trilobites.||||||
28680|Lilydale Limestone|65214|6|Mentioned|p272|Devonian|Devonian|VIC, Melbourne Trough and Lilydale. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
28680|Lilydale Limestone|65940|6|Mentioned|p205|Pragian|Pragian|Lilydale, VIC. Contains Cyathophyllum cresswelli (Sterictophyllum sp.) (type locality, Pragian, kindlei - pireneae Zones; Mawson and Talent, 2000).||||||
28680|Lilydale Limestone|68116|5|Briefly described|Appendix, Map 42.|Early Devonian|Early Devonian||||||Limestone: variably dolomitised, well bedded, pale grey and orange-pink; fossiliferous.|
28680|Lilydale Limestone|70487|6|Mentioned|p7, p8|Emsian|Pragian|Conodont specimen indicates age range of unit.|||||Fossiliferous limestone.|
28680|Lilydale Limestone|70933|14|Not recorded|p94|||Rich coral-stromatoporoid-mollusc fauna.||||||
28680|Lilydale Limestone|73143|6|Mentioned|p11|Pragian|Pragian|Contains Heliolites (Jones and Hill, 1940) and Favosites grandipora tabulate corals (Etheridge, 1890; Philip, 1960).||||||
72946|Limestone Creek marble|61186|6|Mentioned|p45 Fig. 14|||Informal name for Victorian dimension stone. Probably named for the quarry locality.||||||
68626|Lindenow Sand Member|24551|5|Briefly described|p327 Fig. 10.33|Miocene|Miocene|Of Gippsland Limestone?||||||03-FEB-06
68626|Lindenow Sand Member|62899|5|Briefly described|p37 Fig. 2|||Of the Gippsland Limestone. Geological province: Lakes Entrance Platform.||||||12-DEC-06
68626|Lindenow Sand Member|63739|5|Briefly described|p37 Fig. 2|||Geological province: Gippsland Basin.||||||01-JUL-08
27047|Lintons Creek Conglomerate Member|22511|6|Mentioned|p659|||||||||
27047|Lintons Creek Conglomerate Member|22684|5|Briefly described|Fig.2 p746|Llandovery|Llandovery|See also Fig.5 p749||||||
27047|Lintons Creek Conglomerate Member|22886|6|Mentioned|p53|||||||||
27047|Lintons Creek Conglomerate Member|23309|5|Briefly described|p139. Tb 2.50||Silurian|||||||
27047|Lintons Creek Conglomerate Member|41585|5|Briefly described|p105|||||||||
27047|Lintons Creek Conglomerate Member|42628|5|Briefly described|Map legend|Llandovery||||||||
27047|Lintons Creek Conglomerate Member|42827|5|Briefly described|p105|||Of Springfield Formation.||||||14-APR-08
27047|Lintons Creek Conglomerate Member|63083|5|Briefly described|p215|Llandovery|Llandovery|Of the Springfield Formation.||||||07-FEB-11
26691|Liptrap Formation|23228|6|Mentioned|Fig2-3p11||Early Devonian|||||||
26691|Liptrap Formation|23229|5|Briefly described|Table3-3p27, 35|Zlichovian|Pragian|||||||
26691|Liptrap Formation|23266|5|Briefly described|p353, Fig13-5.1p354||Emsian|||||||
26691|Liptrap Formation|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Walhalla Group||||||
26691|Liptrap Formation|23309|5|Briefly described|p149-152, 274-277. Tb 2.57||Devonian|||||||
26691|Liptrap Formation|23522|5|Briefly described|p247 Fig 3|Early Devonian|Early Devonian|||||||
26691|Liptrap Formation|24002|5|Briefly described|p228 Fig.2|Devonian|Devonian|||||||
26691|Liptrap Formation|24098|5|Briefly described|p27 Fig. 2|Emsian|Emsian|Of the Walhalla Group (Murrindindi Supergroup). Geological Province: Melbourne Zone, Lachlan Fold Belt.||||||19-APR-05
26691|Liptrap Formation|24224|5|Briefly described|p264|Pragian|Pragian|Geological Province: Turtons Creek Inlier.||||||
26691|Liptrap Formation|24551|5|Briefly described|p123, 185, 616|||||||||
26691|Liptrap Formation|30570|5|Briefly described|p5|||||||||
26691|Liptrap Formation|30930|6|Mentioned|Map legend|Early Devonian|Early Devonian|Emsian. See Lexicon||||||
26691|Liptrap Formation|31508|6|Mentioned|Table 1|||Devonian||||||
26691|Liptrap Formation|33154|6|Mentioned|p6|||||||||
26691|Liptrap Formation|33156|4|Described|p132|||||||||
26691|Liptrap Formation|33159|5|Briefly described|p15|||L.Dev.||||||
26691|Liptrap Formation|33238|5|Briefly described|p642|||||||||
26691|Liptrap Formation|33601|6|Mentioned|Fig.6|||||||||
26691|Liptrap Formation|33604|6|Mentioned|p17|||L.Dev. Correlation chart.||||||
26691|Liptrap Formation|33732|5|Briefly described|p106|||||||||
26691|Liptrap Formation|34250|6|Mentioned|p3|||Emsian||||||
26691|Liptrap Formation|34815|6|Mentioned|p18|||||||||
26691|Liptrap Formation|34843|5|Briefly described|p8|||||||||
26691|Liptrap Formation|34954|6|Mentioned|Fig.34|||||||||
26691|Liptrap Formation|35283|3|Fully described|p57|||||||||
26691|Liptrap Formation|38787|6|Mentioned|p141|||||||||
26691|Liptrap Formation|39331|6|Mentioned|Table 2-1|||||||||
26691|Liptrap Formation|39858|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
26691|Liptrap Formation|41572|6|Mentioned|p13|||||||||
26691|Liptrap Formation|41585|4|Described|p117|||||||||
26691|Liptrap Formation|41758|5|Briefly described|p243|||||||||
26691|Liptrap Formation|42033|6|Mentioned|p654|||||||||
26691|Liptrap Formation|42577|6|Mentioned|Fig.4 P30|||||||||
26691|Liptrap Formation|42827|4|Described|p117|||see also Table 4.1||||||
26691|Liptrap Formation|43461|14|Not recorded|p627|||||||||
26691|Liptrap Formation|43525|14|Not recorded|Table p132||Emsian|||||||
26691|Liptrap Formation|43530|14|Not recorded|p1029|||||||||
26691|Liptrap Formation|43547|14|Not recorded|Table p153,154||Emsian|(M.Emsian)||||||
26691|Liptrap Formation|46053|14|Not recorded|p.444|||||||||
26691|Liptrap Formation|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Waratah Bay. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
26691|Liptrap Formation|65940|6|Mentioned|p204|Emsian|Emsian|Waratah Bay, VIC. Contains Phillipsastrea maculosa (Philip, 1962; Pragian, sulcatus to pireneae Zones, Mawson and Talent, 1994b).||||||
26691|Liptrap Formation|68116|5|Briefly described|Appendix, Maps 56-57.|Pragian|Lochkovian||||||Thin-bedded quartz-rich sandstone and siltstone with minor sandstone and gritstone, and rare diamictite which contains chert and limestone pebbles.|
26691|Liptrap Formation|70901|14|Not recorded|p6|||Stratigraphy||||||
41864|Little Mount Tambo Trachyte Member|60503|3|Fully described|p136, p41 Tb. 2|Triassic|Triassic|Of the Teapot Creek Formation. Trachyte with no intercalated volcaniclastic sediments. Unconformably overlies Omeo Metamorphic Complex. Overlies sediments of Teapot Creek Formation. Intruded by Bung Bung Syenite.||||||17-FEB-10
41864|Little Mount Tambo Trachyte Member|60504|5|Briefly described|Map Legend|Triassic|Triassic|Of the Teapot Creek Formation. Trachyte lava: dense, black, strongly porphyritic with feldspar phenocrysts in a dark groundmass.||||||20-OCT-04
41864|Little Mount Tambo Trachyte Member|60505|5|Briefly described|Map legend|Triassic|Triassic|Of the Teapot Creek Formation. Trachyte lava: dense, black, strongly porphyritic with feldspar phenocrysts in a dark groundmass.||||||21-OCT-04
41864|Little Mount Tambo Trachyte Member|60506|5|Briefly described|Map legend|Triassic|Triassic|Of the Teapot Creek Formation. Trachyte lava: dense, black, strongly porphyritic with feldspar phenocrysts in a dark groundmass.||||||21-OCT-04
41864|Little Mount Tambo Trachyte Member|60507|5|Briefly described|Map Legend|Triassic|Triassic|Of the Teapot Creek Formation.  Trachyte lava: dense, black, strongly porphyritic with feldspar phenocrysts in a dark groundmass.||||||21-OCT-04
41864|Little Mount Tambo Trachyte Member|60508|5|Briefly described|Map legend|Triassic|Triassic|Of the Teapot Creek Formation. Trachyte lava: intensely magnetic (1000 nT); high total count, K, moderate Th, U||||||
22204|Little River Subgroup|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Snowy River Volcanics.||||||25-SEP-08
22204|Little River Subgroup|23309|4|Described|p106-109, 114-115, 129-131. Tb 2.40|||Of the Snowy River Volcanics.||||||
22204|Little River Subgroup|23615|5|Briefly described|p112|Early Devonian|Early Devonian|Youngest, most diverse subgroup of the Snowy River Volcanics with twenty formations recognised.  Age: Early Devonian ~410-395Ma.||||||16-AUG-18
22204|Little River Subgroup|23938|5|Briefly described|p102 Fig. 42|Devonian|Devonian|Of the Snowy River Volcanics. Extrusive, fluvial, ignimbrite, felsic to mafic lava, conglomerate. See also p117. ||||||
22204|Little River Subgroup|24551|4|Described|p144, p141 Fig.  5.32|||Of Snowy River Volcanics. Includes 23 recognised formations.||||||
22204|Little River Subgroup|43206|5|Briefly described|map legend||Lochkovian|Of Snowy River Volcanics.||||||25-SEP-08
22204|Little River Subgroup|43312|5|Briefly described|Map Legend||Early Devonian|||||||
22204|Little River Subgroup|43313|5|Briefly described|Map Legend||Early Devonian|Of Snowy River Volcanics.||||||25-SEP-08
22204|Little River Subgroup|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Unit in Snowy River Volcanics.|||Extrusive, fluvial: felsic ignimbrite, felsic to mafic lava, ashstone, conglomerate, sandstone, mudstone, chert.|
22204|Little River Subgroup|60542|5|Briefly described|p60, p67|Early Devonian|Early Devonian|Of Snowy River Volcanics. Subaerial, mostly ignimbrites, with thin intercalations of fluvial and minor lacutrine sediments. ||||||
22204|Little River Subgroup|68115|6|Mentioned|p4.|Devonian|Devonian|Previously included Yellow Waterholes Ignimbrite (Orth et al. 1995), which was later moved into Tara Range Subgroup by VandenBerg et al. (2000).||||||
22204|Little River Subgroup|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Felsic ignimbrite, felsic to mafic lava, ashstone, conglomerate, sandstone, mudstone, chert.|
34853|Livingstone Creek Tonalite|22968|5|Briefly described|P71, P198||Late Silurian|New name, parent is Polar Star Suite||||||
34853|Livingstone Creek Tonalite|23029|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is the Polar Star Suite||||||
34853|Livingstone Creek Tonalite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Polar Star Suite.||||||
34853|Livingstone Creek Tonalite|23309|6|Mentioned|p435 App1|||G145 I-Type.||||||
34853|Livingstone Creek Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Biotite tonalite: grey; medium-grained equigranular; weakly foliated; zones of chlorite-epidote alteration.|
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|||||||||
74900|Locmany Formation|64535|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of Tyers River Subgroup (Otway Group). Mainly quartzarenite, sublitharenite, litharenite sandstones, minor conglomerate, coal; more lithological detail included. Contains  rich fossil flora. Fluvial deposits. ||||||
74900|Locmany Formation|64539|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of Tyers River Subgroup (Otway Group). Mainly quartzarenite, sublitharenite, litharenite sandstones, minor conglomerate, coal; more lithological detail included. Contains rich fossil flora. Fluvial deposits.||||||22-DEC-08
74900|Locmany Formation|64540|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of Tyers River Subgroup (Otway Group). Mainly quartzarenite, sublitharenite, litharenite sandstones, minor conglomerate, coal; more lithological detail included. Contains  rich fossil flora. Fluvial deposits. ||||||
74900|Locmany Formation|64605|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Tyers River Subgroup (Otway Group). Sandstone, siltstone, minor conglomerate, coal; alluvial deposits. Speckled blue-green-yellow in RGB. Nonmagnetic.||||||
74900|Locmany Formation|64616|3|Fully described|p142-144, p298|Early Cretaceous|Early Cretaceous|Formerly Locmany Member of Rintoul Creek Formation (Tosolini et al.,1999). Type section details given. Upper unit in Tyers River Subgroup, conformably overlying Tyers Conglomerate. Is overlain gradationally by Eumeralla Formation. Thickness to 360m. Siltstone, lesser sandstone; minor beds of conglomerate and coal. Rich plant fossil assemblage indicates Valanginian age. Geophysical characteristics given.||||||
74900|Locmany Formation|68116|5|Briefly described|Appendix, Map 52.|Hauterivian|Valanginian|Rich in fossil flora.|||||Sandstone, siltstone, minor conglomerate, coal: sandstones are quartzarenite, sublitharenite, litharenite, rare lithic arkose and feldsarenite; fine to medium-grained; thick-bedded; cross-bedded; siltstone pale grey to brown, thin-bedded.|
35339|Loddon River Group|24096|6|Mentioned|p4|||||||||
35339|Loddon River Group|24104|5|Briefly described|p149|Pliocene|Eocene|||||||
35339|Loddon River Group|24105|5|Briefly described|p155, 158|Eocene|Eocene|||||||
35339|Loddon River Group|24383|6|Mentioned|p82 Fig.52|||Geological Province: Lachlan Fold Belt||||||
35339|Loddon River Group|24439|5|Briefly described|p39 Fig. 21|Miocene|Eocene|Fluvial gravels.  See also p47 Fig. 22, p48 (unit Aep) Appendix 2.||||||
35339|Loddon River Group|24440|6|Mentioned|Map legend|||[Located in Interpreted Landscape Evolution map legend].||||||
35339|Loddon River Group|24551|6|Mentioned|p415, 421|||||||||
35339|Loddon River Group|62370|5|Briefly described|p447|Middle Miocene|Late Eocene|Deep-lead sedimentary sequence encompassing Calivil, Olney and Denicull Formations. Age determined by Carey and Hughes (2002) and Phillips and Hughes (2003) - but not used by Geoscience Victoria mapping as yet.||||||12-JAN-12
35339|Loddon River Group|66002|5|Briefly described|p12|||Definition by Highes et al. (1998) includes fluvial sediments in W VIC uplands that postdate White Hills Gravel & predate Moorabool Viaduct Formation & Newer Volcanic Group. Correlates with Calivil Formation & parts of Renmark Group. No longer used by GSV||||||
35339|Loddon River Group|66286|5|Briefly described|pp182-185, p189.|||Texturally variable unconsolidated sediments; interpreted as fluvial sediments sourced from Glenelg River Metamorphic Complex and Rocklands Volcanic Group, in adjacent Dundas Tableland to the south. Forms a westward-thickening wedge.||||Is overlain by Bookpurnong Formation.|Very fine- to coarse-grained, poorly to moderately sorted sands.|
10579|Loddon Vale Granite|42726|5|Briefly described|map legend|Early Devonian||699. Not variation on Loddon Member, reserved for use in NSW. Subsurface.||||||
10579|Loddon Vale Granite|65969|5|Briefly described|p6 Fig.2, p15|Early Devonian|Early Devonian|Magnetic. Peraluminous, high-Na chemistry. Contains hornblende, sphene and allanite or monazite, and strongly magnetic phases. Referred to as Loddon Vale pluton on p.15.||||||
10579|Loddon Vale Granite|73505|6|Mentioned|p7|||(G320). Considered part of the Mount Cole Suite based on magnetic character (White and Chappell, 1988).||Mount Cole Suite||||
37251|Loftus Creek Granodiorite|23309|5|Briefly described|p335, 337|Ordovician|Ordovician|G419, I-type.  Supersedes Sawpit Gully Granite.  Age: 484+/-7Ma.||||||
37251|Loftus Creek Granodiorite|24012|3|Fully described|p223 appendix 1|||Fomerly Sawpit Gully Granodiorite.||||||
37251|Loftus Creek Granodiorite|50154|2|Defined|p24, p75, p101-102|Early Ordovician|Early Ordovician|Formerly mapped as Sawpit Gully Granodiorite by Anderson & Gray, 1994. Age: 491 +/- 8 Ma & 484 +/- 7 Ma (U/Pb zircon). Corresponds to part of the Wando Granodiorite of Wells (1956).||||||15-SEP-04
37251|Loftus Creek Granodiorite|50155|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende biotite granodiorite; I-type||||||
37251|Loftus Creek Granodiorite|50156|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-biotite granodiorite: massive, grey, medium to coarse grained, porphyritic with phenocrysts of biotite and alkali feldspar; accessory magnetite and sphene; uncommon microgranitoid enclaves.||||||10-JUN-14
37251|Loftus Creek Granodiorite|50157|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-biotite granodiorite: massive, grey, medium to coarse grained, porphyritic with phenocrysts of biotite and alkali feldspar; accessory magnetite and sphene; uncommon microgranitoid enclaves.||||||
37251|Loftus Creek Granodiorite|50158|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-biotite granodiorite: massive, grey , medium to coarse grained, porphyritic with phenocrysts of biotite and alkali feldspar; accessory magnetite and sphene; uncommon microgranitoid enclaves.||||||
37251|Loftus Creek Granodiorite|50159|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-biotite granodiorite: massive, grey , medium to coarse grained, porphyritic with phenocrysts of biotite and alkali feldspar; accessory magnetite and sphene; uncommon microgranitoid enclaves.||||||24-JUN-04
37251|Loftus Creek Granodiorite|50160|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-biotite granodiorite||||||
37251|Loftus Creek Granodiorite|50161|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-biotite granodiorite: massive, grey , medium to coarse grained, porphyritic with phenocrysts of biotite and alkali feldspar; accessory magnetite and sphene; uncommon microgranitoid enclaves.||||||24-JUN-04
37251|Loftus Creek Granodiorite|50162|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-biotite granodiorite: massive, grey , medium to coarse grained, porphyritic with phenocrysts of biotite and alkali feldspar; accessory magnetite and sphene; uncommon microgranitoid enclaves.||||||24-JUN-04
37251|Loftus Creek Granodiorite|50163|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-biotite granodiorite: massive, grey , medium to coarse grained, porphyritic with phenocrysts of biotite and alkali feldspar; accessory magnetite and sphene; uncommon microgranitoid enclaves.||||||24-JUN-04
37251|Loftus Creek Granodiorite|50164|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende-biotite granodiorite; I-type. Age: 488 +/- 8 (U-Pb)||||||
37251|Loftus Creek Granodiorite|66002|6|Mentioned|p8 Tb.5|||G419. Defined by Morand et al. 2003.||||||
37251|Loftus Creek Granodiorite|68116|5|Briefly described|Appendix, Maps 29, 38.|Early Ordovician|Late Cambrian||||||Hornblende-biotite granodiorite: massive, grey, medium to coarse grained, porphyritic with phenocrysts of biotite and alkali feldspar; accessory magnetite and sphene; uncommon microgranitoid enclaves; magnetic.|
37251|Loftus Creek Granodiorite|73430|6|Mentioned|p518|Cambrian|Cambrian|Glenelg Terrane. Post-kinematic.|491+/-8 Ma|||||
10625|Long Point Formation|35720|6|Mentioned|Fig.2|||||||||
10625|Long Point Formation|41511|4|Described|p14|||||||||
10631|Longford Limestone|24551|6|Mentioned|p608|||Of the Gippsland Limestone||||||
10631|Longford Limestone|31351|6|Mentioned|p86|||||||||
10631|Longford Limestone|31850|6|Mentioned|p36|||Refers Carter (1964)||||||
10631|Longford Limestone|33459|6|Mentioned|Table 1|||||||||
10631|Longford Limestone|34421|6|Mentioned|p259|||||||||
10631|Longford Limestone|38070|6|Mentioned|Fig.12|||Gippsland Basin||||||
10631|Longford Limestone|44215|14|Not recorded|p360|||||||||
10631|Longford Limestone|70076|5|Briefly described|Regional: Fig.3|Langhian|Aquitanian|||Seaspray Group.||Overlies Lakes Entrance Formation. Is overlain by Wuk Wuk Marl.||
22216|Lookout Top Ignimbrite|23309|4|Described|p110. Tb 2.40|||Maximum Thickness: 330m.  Of ther Mount Dawson Subgroup.||||||
22216|Lookout Top Ignimbrite|23615|3|Fully described|p107|Early Devonian|Early Devonian|Of Mount Dawson Subgroup. Characterised by large quartz crystals commonly 3mm in size. with abundant red pumice (15%) and some red and green volcanic clast present. Underlain by Plumb Gully Ignimbrite.  Max. thickness: 300m.||||||
22216|Lookout Top Ignimbrite|43206|5|Briefly described|map legend||Ludlow|Of Mount Dawson Subgroup.||||||
22216|Lookout Top Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Quartz-feldspar ignimbrite with large quartz and orange feldspar phenocrysts, red pumice fragments.|
26701|Loomat Granite|22878|4|Described|p80|||||||||
26701|Loomat Granite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Of the Bemboka Supersuite. Biotite granite: pale pinkish grey, very coarse grained, massive to weakly foliated; prominent K-feldspar crystals to 40mm long.||||||01-OCT-04
26701|Loomat Granite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Bemboka Supersuite. Biotite granite: pale pinkish grey, very coarse grained, massive to weakly foliated; prominent K-feldspar crystals to 40mm long.||||||01-OCT-04
26701|Loomat Granite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Bemboka Supersuite. Biotite Granite: Highly magnetic (210-240 nT) to moderately magnetic (up to 150 nT). High K, low Th and U.||||||06-OCT-04
26701|Loomat Granite|23309|6|Mentioned|p436 App1|||G20 - I-Type. Supersedes Loomat Adamellite.||||||11-NOV-04
26701|Loomat Granite|42726|5|Briefly described|map legend|Early Devonian|Early Devonian|Variation on Loomat Adamellite (Vic).  Of the Coolangubra Suite (Bemboka Supersuite).||||||07-FEB-05
26701|Loomat Granite|68116|5|Briefly described|Appendix, Map 37.|Early Devonian|Llandovery||||||Biotite granite: pale pinkish grey, very coarse grained, massive to weakly foliated; prominent K-feldspar crystals to 40 mm long; I-type.|
10684|Loveday Soil|23818|5|Briefly described|p212 Fig.108|Late Pleistocene|Late Pleistocene|||||||
10684|Loveday Soil|24176|5|Briefly described|p21, p22 Tb. 1|Pleistocene|Pleistocene|Of Pooraka Formation.  Geological Province: Mount Painter Province.||||||
10684|Loveday Soil|30056|6|Mentioned|Table 4|||||||||
10684|Loveday Soil|30176|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
10684|Loveday Soil|30751|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
10684|Loveday Soil|30752|6|Mentioned|p4|||||||||
10684|Loveday Soil|30753|6|Mentioned|p14|||Recent age||||||
10684|Loveday Soil|30755|6|Mentioned|p169|||Tectonic map||||||
10684|Loveday Soil|30756|6|Mentioned|p4|||||||||
10684|Loveday Soil|30802|6|Mentioned|p10|||Pleistocene age||||||
10684|Loveday Soil|30807|6|Mentioned|p101|||Suggested map symbol||||||
10684|Loveday Soil|30922|6|Mentioned|Map legend|Holocene|Holocene|||||||
10684|Loveday Soil|30994|6|Mentioned|p250|||Refers to Firman (1969)||||||
10684|Loveday Soil|31966|6|Mentioned|p6|||||||||
10684|Loveday Soil|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
10684|Loveday Soil|32432|6|Mentioned|Fig.2|||See also Table 1||||||
10684|Loveday Soil|32561|6|Mentioned|p59|||See also Fig.4||||||
10684|Loveday Soil|33423|6|Mentioned|p15|||Strat.||||||
10684|Loveday Soil|33767|6|Mentioned|Fig.5|||||||||
10684|Loveday Soil|34180|6|Mentioned|p217|||Upper Pleistocene. See also P212||||||
10684|Loveday Soil|34536|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
10684|Loveday Soil|34758|6|Mentioned|Fig.2|||||||||
10684|Loveday Soil|35071|6|Mentioned|Fig.4|||||||||
10684|Loveday Soil|35200|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
10684|Loveday Soil|35232|6|Mentioned|Table.4|||||||||
10684|Loveday Soil|35673|6|Mentioned|Fig.1|||Location plan, Para Hills quartzite quarry.||||||
10684|Loveday Soil|35772|4|Described|Table 1|||||||||
10684|Loveday Soil|36626|6|Mentioned|Fig.1|||||||||
10684|Loveday Soil|36834|6|Mentioned|Fig.1|||||||||
10684|Loveday Soil|37853|6|Mentioned|Fig.1|||||||||
10684|Loveday Soil|38068|6|Mentioned|Fig.8|||||||||
10684|Loveday Soil|38107|6|Mentioned|p19|||||||||
10684|Loveday Soil|39349|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
10684|Loveday Soil|40442|6|Mentioned|p38|||||||||
10684|Loveday Soil|42717|5|Briefly described|map legend|Pleistocene||||||||
10684|Loveday Soil|42722|6|Mentioned|map legend|Pleistocene|Pleistocene|Developed locally in association with Wiabuna Formation.||||||07-APR-05
10684|Loveday Soil|43071|5|Briefly described|p17|||||||||
10684|Loveday Soil|43073|5|Briefly described|p18|||||||||
10684|Loveday Soil|44864|5|Briefly described|Map Legend||Pleistocene|||||||
10684|Loveday Soil|73112|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Contained in the Woorinen Formation (equivalent).|||||Carbonate.|
30588|Lower Tableland Granite|23309|5|Briefly described|p343.|||G116 - S-Type||||||
30588|Lower Tableland Granite|43220|6|Mentioned|p11||Devonian|||||||
30588|Lower Tableland Granite|44184|5|Briefly described|Map Legend||Early Devonian|||||||
30588|Lower Tableland Granite|60503|3|Fully described|p168, p42 Tb. 2|Early Devonian|Early Devonian|Imposes slight hornfels texture on Tongaro Formation; partly overlain by Morass Creek Basalt. Very felsic foliated granite, mostly  quartz and feldspar. This granite may possibly belong to the Silver Flat Porphyries, although it is much more crystallised.||||||16-NOV-09
30588|Lower Tableland Granite|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Biotite granite: I-type?; medium grained, grey, equigranular with leucocratic fine grained chilled border phase||||||
30588|Lower Tableland Granite|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Biotite granite: I-type?; medium grained, grey, equigranular with leucocratic fine grained chilled border phase||||||
30588|Lower Tableland Granite|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Biotite granite: I-type?; medium grained, grey, equigranular with leucocratic fine grained chilled border phase||||||
30588|Lower Tableland Granite|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Biotite granite: I-type?; medium grained, grey, equigranular with leucocratic fine grained chilled border phase||||||
30588|Lower Tableland Granite|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Biotite granite: I-type(?); moderately magnetic (50 nT); moderate to high Th, moderate K, U, low to moderate total count.||||||
30588|Lower Tableland Granite|68116|5|Briefly described|Appendix, Map 27.|Early Devonian|Early Devonian||||||Biotite-cordierite felsic granite: fine to medium-grained.|
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).||||||
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.|
37759|Ludrik Munjie Granite|23309|6|Mentioned|p436 App 1|||G82. See Ludrik-Munjie Granite.||||||
37759|Ludrik Munjie Granite|60503|3|Fully described|p150, p45 Tb. 2|Silurian|Silurian|Composed primarily of coarse- to medium-grained quartz and feldspar with some biotite and muscovite. Overlain by Eight Mile Loop Rhyolite. In faulted contact with Anglers Rest Granite. Also occurs as fine-grained felsic dykes.||||||17-FEB-10
37759|Ludrik Munjie Granite|60504|5|Briefly described|Map Legend|Wenlock|Wenlock|Biotite granite: S-type, well foliated granite with high compositional variability; numerous metasedimentary enclaves; dark grey to light grey, medium to coarse grained; generally weathered.||||||13-OCT-04
37759|Ludrik Munjie Granite|60505|5|Briefly described|Map legend|Wenlock|Wenlock|Biotite granite: S-type, well foliated granite with high compositional variability; numerous metasedimentary enclaves; dark grey to light grey, medium to coarse grained; generally weathered.||||||
37759|Ludrik Munjie Granite|60506|5|Briefly described|Map legend|Wenlock|Wenlock|Biotite granite: S-type, well foliated granite with high compositional variability; numerous metasedimentary enclaves; dark grey to light grey, medium to coarse grained; generally weathered.||||||
37759|Ludrik Munjie Granite|60507|5|Briefly described|Map Legend|Wenlock|Wenlock|Biotite granite: S-type, well foliated granite with high compositional variability; numerous metasedimentary enclaves; dark grey to light grey, medium to coarse grained; generally weathered.||||||
37759|Ludrik Munjie Granite|60508|5|Briefly described|Map legend|Early Silurian|Early Silurian|Biotite granite: S-type; nonmagnetic (0-5 nT) with weakly north-northwest trending dykes; high K except west of Mitta Mitta River, low Th, U, variable total count.||||||20-OCT-04
37759|Ludrik Munjie Granite|68116|5|Briefly described|Appendix, Map 27.|Wenlock|Llandovery||||||Biotite-muscovite granite: dark to light grey; medium to coarse-grained; well foliated; high compositional variability: numerous metasedimentary enclaves; generally weathered.|
27471|Lurg Granite|22971|5|Briefly described|p 34|||||||||
27471|Lurg Granite|23309|6|Mentioned|p436 App1|||G200 - I-Type.||||||
27471|Lurg Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
27471|Lurg Granite|68116|5|Briefly described|Appendix, Map 26.|Late Devonian|Late Devonian||||||Fractionated granite; fine to medium grained porphyritic phases and coarse-grained phases; contains miarolitic cavities and areas of granophyre; S-type.|
10904|Lysterfield Granodiorite|22885|5|Briefly described|map|||||||||
10904|Lysterfield Granodiorite|23268|6|Mentioned|p387, Fig14-2.1p388||Late Devonian|||||||
10904|Lysterfield Granodiorite|23269|5|Briefly described|p402, Fig14-3.3p405, 406||Late Devonian|||||||
10904|Lysterfield Granodiorite|23309|5|Briefly described|p161, 167, 347|Late Devonian|Late Devonian|G241- I-Type. Supersedes Lysterfield Granite. Age: 369+/-13Ma, 365+/-13 Ma, 365+/-13, 358+/-13Ma.||||||29-MAR-05
10904|Lysterfield Granodiorite|24222|5|Briefly described|p11|||Chemistry of samples reported. I-type granite.  Geological Province: Lachlan Fold Belt.||||||
10904|Lysterfield Granodiorite|24551|5|Briefly described|p162, 721 Table 8.4|Devonian|Devonian|Some debate over whether this is part of the Dandenong Ranges Igneous Complex.||||||05-NOV-07
10904|Lysterfield Granodiorite|29652|6|Mentioned|p4|||||||||
10904|Lysterfield Granodiorite|29653|6|Mentioned|p4|||||||||
10904|Lysterfield Granodiorite|31510|5|Briefly described|p9|||See also Table 1.||||||
10904|Lysterfield Granodiorite|32001|6|Mentioned|p78|||||||||
10904|Lysterfield Granodiorite|33140|6|Mentioned|p13|||||||||
10904|Lysterfield Granodiorite|33157|5|Briefly described|p42|||||||||
10904|Lysterfield Granodiorite|33462|6|Mentioned|p10|||Strat.table.||||||
10904|Lysterfield Granodiorite|33464|6|Mentioned|Table 1|||||||||
10904|Lysterfield Granodiorite|33598|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
10904|Lysterfield Granodiorite|33599|4|Described|p10|||||||||
10904|Lysterfield Granodiorite|33604|5|Briefly described|p19|||||||||
10904|Lysterfield Granodiorite|33607|6|Mentioned|Map legend|Devonian|Devonian|Granodiorite, medium, even-grained, hornblende-bearing||||||29-NOV-04
10904|Lysterfield Granodiorite|34843|6|Mentioned|p8|||||||||
10904|Lysterfield Granodiorite|34956|6|Mentioned|p82|||||||||
10904|Lysterfield Granodiorite|35012|6|Mentioned|p430|||||||||
10904|Lysterfield Granodiorite|35277|5|Briefly described|p95|||||||||
10904|Lysterfield Granodiorite|35278|6|Mentioned|p353|||||||||
10904|Lysterfield Granodiorite|35290|5|Briefly described|p22|||See also P20.||||||
10904|Lysterfield Granodiorite|35712|6|Mentioned|Table 6|||||||||
10904|Lysterfield Granodiorite|35943|6|Mentioned|p32|||||||||
10904|Lysterfield Granodiorite|37501|6|Mentioned|p405|||||||||
10904|Lysterfield Granodiorite|39291|6|Mentioned|Fig.13|||||||||
10904|Lysterfield Granodiorite|40171|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
10904|Lysterfield Granodiorite|41641|5|Briefly described|p165|||||||||
10904|Lysterfield Granodiorite|42154|6|Mentioned|Table 1 P334|||||||||
10904|Lysterfield Granodiorite|42827|5|Briefly described|p165|||see also Fig 5.5. Mafic hornblende-ilmenite granodiorite with red-brown biotite.||||||30-NOV-04
10904|Lysterfield Granodiorite|44187|5|Briefly described|Map Legend||Late Devonian|G241 I-type.||||||
10904|Lysterfield Granodiorite|44197|5|Briefly described|Map Legend||Late Devonian|G241 I-type.||||||
10904|Lysterfield Granodiorite|45087|5|Briefly described|p58|||Chemical analyses||||||
10904|Lysterfield Granodiorite|68116|5|Briefly described|Appendix, Maps 42, 51.|Late Devonian|Late Devonian||||||Biotite-hornblende granodiorite: grey, medium grained, containing quartz, plagioclase, orthoclase, biotite, minor hornblende, accessory apatite, ilmenite, allanite, sphene, tourmaline and zircon.|
10904|Lysterfield Granodiorite|71180|4|Described|p185|||||||||
10904|Lysterfield Granodiorite|71410|5|Briefly described|p1052|Late Devonian|Late Devonian|c.40km SE of Melbourne. Show LREE enriched over HREE; La concentrations 100-200 times chondritic levels. Potential for REE concentration in regolith and soil.||||||
10904|Lysterfield Granodiorite|75061|6|Mentioned|p60|||||||||
10904|Lysterfield Granodiorite|75062|6|Mentioned|p74 Fig.2|||Melbourne Zone.||||Intrudes Dandenong Ranges Igneous Complex.|S-type.|
10904|Lysterfield Granodiorite|75072|5|Briefly described|p230 Fig.2, 233-234, 244, 246, 248-249|Late Devonian|Late Devonian|See also p254. Melbourne Zone. Zircons crystals discussed; probability density distribution graph. Has the highest proportion of zircon inheritance of the samples graphed. Geochronology by Richards and Singleton (1981).|364 +/- 7 Ma.|||Intrudes Mount Dandenong Igneous Complex.|Hornblende-biotite bearing granodiorite. Strongly I-type.|
30687|Mac Creek Granodiorite|23309|6|Mentioned|p436 App1|||G85 - S-Type.||||||
30687|Mac Creek Granodiorite|60503|4|Described|p153-154, p44 Tb. 2|Silurian|Silurian|Foliated medium-grained quartz, feldspars, muscovite and chlorite in clay-rich groundmass. Intrudes the Omeo Metamorphic Complex. Overlain by Triassic Teapot Creek Group. See also Macs Creek Granodiorite and Mac Creek granite.||||||
30687|Mac Creek Granodiorite|60504|5|Briefly described|Map Legend|Wenlock|Wenlock|Muscovite granite: S-type, foliated, medium grained, grey: margins rich in metasedimentary enclaves||||||
30687|Mac Creek Granodiorite|60505|5|Briefly described|Map legend|Wenlock|Wenlock|Muscovite granite: S-type, foliated, medium grained, grey: margins rich in metasedimentary enclaves||||||
30687|Mac Creek Granodiorite|60506|5|Briefly described|Map legend|Wenlock|Wenlock|Muscovite granite: S-type; foliated, medium grained, grey; margins rich in metasedimentary enclaves||||||
30687|Mac Creek Granodiorite|60507|5|Briefly described|Map Legend|Wenlock|Wenlock|Muscovite granite: S-type; foliated, medium grained, grey; margins rich in metasedimentary enclaves||||||
30687|Mac Creek Granodiorite|60508|5|Briefly described|Map legend|Early Silurian|Early Silurian|Muscovite granite: S-type; nonmagnetic (0-5 nT) except where intruded by moderately magnetic syenite(?) (50 nT) or north-south dykes (20 nT); variable total count, K, Th, U.||||||10-JUN-14
30687|Mac Creek Granodiorite|68116|5|Briefly described|Appendix, Map 27.|Wenlock|Llandovery||||||Muscovite granite: grey; medium-grained; foliated; deeply weathered; margins rich in metasedimentary enclaves.|
30682|MacFarlane Syenite|60503|3|Fully described|p180, p40 Tb. 2|Triassic|Triassic|Of the Mount Leinster Igneous Complex.  Coarse even-grained texture with speckling produced by grey feldspars and black mafic minerals. See also MacFarlanes Syenite.||||||16-NOV-09
30682|MacFarlane Syenite|60504|5|Briefly described|Map Legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Hornblende-biotite-pyroxene syenite: A-type; grey to pale orange, medium to coarse grained, equigranular.||||||
30682|MacFarlane Syenite|60505|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Hornblende-biotite-pyroxene syenite: A-type; grey to pale orange, medium to coarse grained, equigranular.||||||
30682|MacFarlane Syenite|60506|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Hornblende-biotite-pyroxene syenite: A-type; grey to pale orange, medium to coarse grained, equigranular.||||||
30682|MacFarlane Syenite|60507|5|Briefly described|Map Legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Hornblende-biotite-pyroxene syenite: A-type; grey to pale orange, medium to coarse grained, equigranular.||||||
30682|MacFarlane Syenite|60508|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Syenite: A-type; 208+/-6 Ma (K/Ar hornblende); arcuate nonmagnetic and intensley magnetic bands (0-500 nT); high total count, K, Th, U except moderate Th, U, in north and south.||||||
30682|MacFarlane Syenite|68116|5|Briefly described|Appendix, Map 27.|Triassic|Triassic||||||Hornblende-biotite syenite: grey, coarse, equigranular; augite and aegirine present; local alkali granite with arfvedsonite.|
73662|MacRae Ignimbrite|63594|5|Briefly described|p1032 Fig. 1||Devonian|Of the Snowy River Volcanics.||||||04-OCT-07
10936|Macedon Igneous Complex|29709|6|Mentioned|p32|||||||||
10936|Macedon Igneous Complex|33602|6|Mentioned|Fig.2|||||||||
10936|Macedon Igneous Complex|35112|6|Mentioned|Fig.9|||||||||
10936|Macedon Igneous Complex|42827|5|Briefly described|Fig 5.7|||||||||
10936|Macedon Igneous Complex|65715|3|Fully described|p5-6, p7 Tb.4|Late Devonian|Late Devonian|Paper says newly defined here, but does not meet all definition criteria. Includes Barringo Granodiorite, Willimigongong Ignimbrite, Hesket Ignimbrite and an unnamed porphyry.  Includes all Late Devonian rocks of the Macedon Ranges.||||||02-FEB-15
10936|Macedon Igneous Complex|73199|6|Mentioned|p521, p524|||[Written as Macedon IC]. S-type. Inferred to have similar deep-crustal sources to plutonic granitic magmas.||||||
26714|Mackenzie River Granodiorite|23247|6|Mentioned|p194|||||||||
26714|Mackenzie River Granodiorite|23309|5|Briefly described|p436 App1|Late Devonian|Early Devonian|Same as McKenzie River Granodiorite. G398 I-Type. Age: 371 +/- 8Ma, 368 +/- 4 Ma, 402 +/- 4Ma, 399 +/- 5Ma, 402 +/- 8Ma, 400 +/- 8 Ma, 399Ma, 401Ma, 400 +/- 3 Ma.||||||
26714|Mackenzie River Granodiorite|30928|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|Post Lower Carboniferous||||||
26714|Mackenzie River Granodiorite|33232|5|Briefly described|p74|||||||||
26714|Mackenzie River Granodiorite|33602|6|Mentioned|p13|||||||||
26714|Mackenzie River Granodiorite|41585|5|Briefly described|p143|||||||||
26714|Mackenzie River Granodiorite|42827|5|Briefly described|p143|||||||||
26714|Mackenzie River Granodiorite|44929|5|Briefly described|Map Legend||Early Devonian|Hornblende -biotite granodiorite, medium- to coarse-grained, equigranular to porphyritic, pale pinkish-grey.||||||14-JUN-06
26714|Mackenzie River Granodiorite|44930|5|Briefly described|Map Legend||Early Devonian|Hornblende -biotite granodiorite, medium- to coarse-grained, equigranular to porphyritic, pale pinkish-grey.||||||13-JUN-06
26714|Mackenzie River Granodiorite|44931|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Hornblende biotite granodiorite.||||||14-JUN-06
26714|Mackenzie River Granodiorite|44932|5|Briefly described|Map Legend||Early Devonian|Hornblende -biotite granodiorite, medium- to coarse-grained, equigranular to porphyritic, pale pinkish-grey.||||||14-JUN-06
26714|Mackenzie River Granodiorite|44933|5|Briefly described|Map Legend||Early Devonian|Hornblende biotite granodiorite: medium to coarse-grained, equigranular to porphyritic, pinkish-grey; rare mafic and microgranitic enclaves, apitite and granophyric felsic dykes particularly at the margins, miarolitic cavitites; felsic, oxidised, I-type||||||25-JUL-06
26714|Mackenzie River Granodiorite|61183|6|Mentioned|p103|||Probably same unit as Mackenzie River Granite. Names used interchangeably.||||||
26714|Mackenzie River Granodiorite|63599|5|Briefly described|p976|Devonian|Devonian|Part of the Mafeking Suite. See also MacKenzie River Granodiorite. Geological Province: Grampians-Stavely Zone.||||||02-OCT-09
26714|Mackenzie River Granodiorite|64541|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Hornblende biotite granodiorite: medium to coarse grained, equigranular to porphyritic, pale pinkish-grey; rare mafic and microgranitic enclaves, aplite and granophyric felsic dykes, miarolitic cavities; felsic, oxidised, I-type.||||||07-FEB-11
26714|Mackenzie River Granodiorite|64610|5|Briefly described|Map legend|Early Devonian|Early Devonian|Part of Victoria Valley Batholith. Hornbl. biot.granodiorite: med-coarse-gr., equigran. to porphyritic; pinkish-grey; rare mafic+microgranitic enclaves, aplite+granophyric felsic dykes(partic'ly at margins); miarolitic cavities; felsic, oxidised, I-type.||||||17-NOV-08
32301|Mackerel Formation|13323|5|Briefly described|p393 Fig. 2|Early Eocene|Early Paleocene|Of the Halibut Subgroup (Latrobe Group). Geological Province: Gippsland Basin.||||||
32301|Mackerel Formation|24090|5|Briefly described|p8 Fig.3|Eocene|Paleocene|Geological Province: Gippsland Basin.||||||
32301|Mackerel Formation|24407|5|Briefly described|p13 Fig.2|||Geological Province: Gippsland Basin||||||
32301|Mackerel Formation|24551|6|Mentioned|p478 Fig 15.8|Eocene|Paleocene|Of the Halibut Subgroup.||||||
32301|Mackerel Formation|61552|5|Briefly described|p583 Fig.2, p589, p590, p592. |Early Eocene|Early Paleocene|Coastal and nearshore marine facies.||Unit in Halibut Subgroup.||Interfingers with Kingfish Formation.|Dominantly prograding sandstones with nearshore marine shales.|
32301|Mackerel Formation|64876|5|Briefly described|p145 Fig.2|Eocene|Paleocene|Gippsland Basin.||Halibut Subgroup.||||
32301|Mackerel Formation|65717|5|Briefly described|p9 Fig.2.2, p11, p13|Eocene|Paleocene|Nearshore marine facies with excellent reservoir qualities.||Halibut Subgroup||Overlies Kate Shale, unconformably overlain by Flounder Formation|Interbedded marine sandstones, marine shale and siltstone.|05-SEP-17
32301|Mackerel Formation|65973|5|Briefly described|p16, p108, p118, p139, p144, p171|||Gippsland Basin. Near-shore marine sediments with excellent reservoir qualities. Intersected in the Shark-1 drillhole.||Halibut Subgroup|||Marine sandstones and shales.|
32301|Mackerel Formation|70028|6|Mentioned|p79|Eocene|Paleocene|Offshore Gippsland Basin.||||||
32301|Mackerel Formation|70076|5|Briefly described|South-Eastern: Fig.2; p2, Regional: p3|Thanetian|Danian|Hydrocarbon reservoir. Also appears as Mackeral Formation in Fig.2.||Halibut Subgroup.||Overlies Kate Shale. Is overlain by Flounder Formation.|Near-shore marine sandstones with intercalated marine shales.|
32301|Mackerel Formation|73471|5|Briefly described|p86|||Gippsland Basin.||Halibut Subgroup||Overlies Kate Shale|Marine clastics.|
32301|Mackerel Formation|75065|5|Briefly described|p151|Eocene|Paleocene|Gippsland Basin; offshore.||Halibut Subgroup.||Abuts Kingfish and Volador Formations and Kate Shale. Is overlain by Flounder Formation.|Marine shale with lowstand fans.|
37574|Mackiesons Spur Tuff|23309|5|Briefly described|p123, 134, Table 2.47|||Of White Monkey Volcanics.  Maximum thickness 300m.||||||
37574|Mackiesons Spur Tuff|24551|5|Briefly described|p149|||Of White Monkey Volcanics.||||||
83403|Macorna pluton|73496|5|Briefly described|Map legend|Late Devonian|Late Devonian|G317.|||||Nonmagnetic; gravity low about 5 micrometres/second/second below the regional.|
83403|Macorna pluton|73497|5|Briefly described|Map legend|Late Devonian|Late Devonian|G317.|||||Nonmagnetic; possible gravity low of about 5 micrometres/second/second.|
79024|Macropleura band|62469|5|Briefly described|p5 Fig. 2, p20|Ludlow|Ludlow|In lowermost Notoparmella plentiensis Assemblage Zone. 130-140m above base of Eden Park Formation.||Of Eden Park Formation.||||12-FEB-15
26716|Mafeking Granodiorite|23247|5|Briefly described|p187||Early Devonian|||||||
26716|Mafeking Granodiorite|23309|5|Briefly described|p339, 342, 349.||Devonian|I-Type. Supersedes Mafeking Tonalite.||||||
26716|Mafeking Granodiorite|23402|5|Briefly described|p22|Devonian|Devonian|Geological Province: Adelaide Fold Belt||||||
26716|Mafeking Granodiorite|23810|5|Briefly described|Table 1, p886||Devonian|Mafic I-Type. Age: 398+/-2 Ma (SHRIMP U-Pb age). Geological Province: Lachlan Fold Belt.||||||
26716|Mafeking Granodiorite|24551|6|Mentioned|p384, p717 Table 2.4|Early Devonian|Early Devonian|Intrudes the Grampians Group.  Age: 398 +/- 2Ma.||||||
26716|Mafeking Granodiorite|30579|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26716|Mafeking Granodiorite|33232|5|Briefly described|p74|||||||||
26716|Mafeking Granodiorite|33238|6|Mentioned|p641|||||||||
26716|Mafeking Granodiorite|33602|6|Mentioned|p13|||||||||
26716|Mafeking Granodiorite|34990|6|Mentioned|p435|||||||||
26716|Mafeking Granodiorite|38436|6|Mentioned|p420|||||||||
26716|Mafeking Granodiorite|39446|6|Mentioned|p65|||||||||
26716|Mafeking Granodiorite|39967|5|Briefly described|p35|||||||||
26716|Mafeking Granodiorite|40761|6|Mentioned|p242|||||||||
26716|Mafeking Granodiorite|41585|5|Briefly described|p143 Tbl 4.4|||||||||
26716|Mafeking Granodiorite|41868|6|Mentioned|p455|||||||||
26716|Mafeking Granodiorite|42154|6|Mentioned|Table 1 P334|||||||||
26716|Mafeking Granodiorite|43058|6|Mentioned|p76|||||||||
26716|Mafeking Granodiorite|44929|5|Briefly described|Map Legend||Early Devonian|Hornblende biotite granodiorite, equigranular to porphyritic; mafic, oxidised, I-type.||||||14-JUN-06
26716|Mafeking Granodiorite|44930|5|Briefly described|Map Legend||Early Devonian|Hornblende -biotite granodiorite, medium-grained, equigranular to porphyritic, pale grey.||||||14-JUN-06
26716|Mafeking Granodiorite|44931|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Hornblende biotite granodiorite, equigranular to porphyritic; mafic, oxidised, I-type, Rb/Sr age 396+/-2 Ma: moderate to high magnetic response; high K.||||||14-JUN-06
26716|Mafeking Granodiorite|44932|5|Briefly described|Map Legend||Early Devonian|Hornblende -biotite granodiorite, medium-grained, equigranular to porphyritic, pale grey.||||||14-JUN-06
26716|Mafeking Granodiorite|44933|5|Briefly described|Map Legend||Early Devonian|Hornblende biotite granodiorite: medium grained, equigranular to porphyritic, pale grey; bipyramidal quartz, rare mafic enclaves and patchy deuteric alteration; deeply weathered to fresh; mafic, oxidised. I-type||||||27-OCT-04
26716|Mafeking Granodiorite|60451|4|Described|p79, 84|Early Devonian|Early Devonian|Of the Mafeking Suite. Type section in text. Overlain in places by: Grampians Group & Nekeeya Gravel. Age: 396 +/- 2Ma (Hergt, 1983), 398 +/- 2Ma (Bierlein et al, 1998a).||||||
26716|Mafeking Granodiorite|60456|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Mafeking Suite. Hornblende-biotite granodiorite: pale grey, medium grained, equigranular to porphyritic.||||||
26716|Mafeking Granodiorite|60458|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Mafeking Suite. Unit does not appear on this map.||||||
26716|Mafeking Granodiorite|60459|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Mafeking Suite. Hornblende-biotite granite: felsic, oxidised, I-Type.||||||
26716|Mafeking Granodiorite|61183|6|Mentioned|p126 Tb. 5|||Probably intended as Mafeking Granite. Names used interchangeably.||||||
26716|Mafeking Granodiorite|61410|5|Briefly described|p9 |||Minor gold was produced from alluvial mining and ferruginous quartz veins associated with molybdenite, in this unit.||||Intrudes the Grampians Group.||
26716|Mafeking Granodiorite|63599|5|Briefly described|p976|Devonian|Devonian|Of the Makefing Suite. Geological Province: Grampians-Stavely Zone.||||||02-OCT-09
26716|Mafeking Granodiorite|64541|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Hornblende biotite granodiorite: medium grained, equigranular to porphyritic, pale grey; bipyramidal quartz, rare mafic enclaves and patchy deuteric alterations; deeply weathered to fresh; mafic, oxidised, I-type.||||||10-JUN-14
26716|Mafeking Granodiorite|64610|5|Briefly described|Map legend|Early Devonian|Early Devonian|Part of Victoria Valley Batholith. Hornblende biotite granodiorite: medium-grained, equigranular to porphyritic; pale grey; bipyramidal quartz, rare mafic enclaves+ patchy deuteric alteration; deeply weathered to fresh; mafic, oxidised, I-type.||||||17-NOV-08
26716|Mafeking Granodiorite|66002|5|Briefly described|p8 Tb.5|||Of Mafeking Suite. G396. Defined by Spencer-Jones (1965). Called Mafeking Granite by Cayley and Taylor (1997)||||||
26716|Mafeking Granodiorite|67978|5|Briefly described|p496 Fig.1, p499 Tb.1|Emsian|Emsian|Stavely zone. Zircon dating by Bierlein et al. (2001b) from Mafeking.|398 +/- 2 Ma, SIMS U-Pb|||||19-SEP-14
26716|Mafeking Granodiorite|68116|5|Briefly described|Appendix, Map 30.|Early Devonian|Early Devonian||||||Hornblende-biotite granodiorite: pale grey; medium-grained, equigranular to porphyritic; bipyramidal quartz; rare mafic enclaves and patchy deuteric alteration; deeply weathered to fresh; oxidised; highly magnetic.|
26716|Mafeking Granodiorite|70877|4|Described|p153-p159, p170-p171, p202|Devonian|Devonian|SHRIMP ages derived from this study and represents the age of magmatic crystallisation. Petrography, zircon morphology and SHRIMP U-Pb results are discussed in detail for a sample of this unit.|404.3 +/- 1.6 Ma (SHRIMP U-Pb)||||Medium-grained, porphyritic, hornblende-biotite granodiorite.|
26716|Mafeking Granodiorite|71593|4|Described|p81, p148|Early Devonian|Early Devonian|Age derived from dating of similar rocks in the Victoria Valley Complex (Lewis et al., 2016)|c. 400 Ma|||||
10993|Mafeking Suite|23309|5|Briefly described|p342.|||||||||
10993|Mafeking Suite|23402|5|Briefly described|p22|Devonian|Devonian|Geological Province: Lachlan Fold Belt||||||
10993|Mafeking Suite|41563|6|Mentioned|p516|||||||||
10993|Mafeking Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
10993|Mafeking Suite|42827|6|Mentioned|p437|||||||||
10993|Mafeking Suite|60451|5|Briefly described|p84|||Includes: Mafeking Granodiorite and Epacris Hills Granite.||||||
10993|Mafeking Suite|60454|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Units do not appear on this map.||||||
10993|Mafeking Suite|60456|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Mafeking Granodiorite, Epacris Hills Granite.||||||
10993|Mafeking Suite|60457|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Units do not appear on this map.||||||
10993|Mafeking Suite|60458|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Mafeking Granodiorite, Epacris Hills Granite.||||||
10993|Mafeking Suite|60459|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Mafeking Granodiorite, Epacris Hills Granite.||||||29-SEP-04
10993|Mafeking Suite|61183|5|Briefly described|p7-8|Devonian|Devonian|Granites containing small amounts of gold. Intrudes the Grampians Group. ||||||
10993|Mafeking Suite|63599|5|Briefly described|p975|Devonian|Devonian|Comprises Mafeking Granodiorite, Mackenzie River Granodiorite and the Victoria Valley Complex. Geological Province: Grampians-Stavely Zone.||||||10-DEC-07
10993|Mafeking Suite|66002|5|Briefly described|p8 Tb.5|||Includes Mafeking Granodiorite and Epacris Hills Granite.  Defined in White and Chappell 1988.||||||
10993|Mafeking Suite|67806|6|Mentioned|p111|||The more felsic members show a strong trend of increasing Fe2O3/FeO.||||||
10993|Mafeking Suite|70877|6|Mentioned|p13|Early Devonian|Late Silurian|||||Intrudes the Grampians Group.||
10993|Mafeking Suite|70967|6|Mentioned|p11|||Mount Stavely Belt.||||Intrudes Grampians Group. Co-magmatic with Rocklands Volcanic Group.||
10993|Mafeking Suite|72445|5|Briefly described|p10.|Early Devonian|Late Silurian|||||Intrudes Grampians Group. Comagmatic with Rocklands Volcanic Group.||
39629|Magdala Basalt|24087|6|Mentioned|p336 Fig. 8|||See also Magdala balsat (misspelt). Geological Province: Lachlan Fold Belt.||||||30-SEP-14
39629|Magdala Basalt|24100|6|Mentioned|p99|||Mentioned in the context of tholeiitic Magdala Basalt domes.||||||
39629|Magdala Basalt|50546|5|Briefly described|p1232 Fig.1c, p1234 Fig.2a|||Mapped in Figures.||||||30-NOV-04
39629|Magdala Basalt|62742|5|Briefly described|p698, p699 Fig. 2|Early Cambrian|Early Cambrian|Boninitic, tholeiitic and ultramafic lavas and intrusions. Conformably overlain by Albion Formation and Knowsley East Shale. In the Stawell Zone. See also p702. ||||||
39629|Magdala Basalt|62744|5|Briefly described|p708, p709 Fig. 2|Early Cambrian|Early Cambrian|Overlies and is intercalated with Albion Formation; overlain by Leviathan Formation. Thickness at Stawell is up to 1km. Geological Province: Stawell Zone||||||
39629|Magdala Basalt|62747|5|Briefly described|p734 Fig. 1, p737|||Mafic volcanic rock - tholeiitic in composition. Overlain by Albion Formation.||||||
39629|Magdala Basalt|62749|5|Briefly described|p722, p731|Cambrian|Cambrian|Comprises various basalt nose structures, including the Dukes Nose. Hosts gold in steeply plunging ore-shoots contained in a complex shear/vein network on the southwest flank of the basalt.||||||
39629|Magdala Basalt|62751|5|Briefly described|p759|Cambrian|Cambrian|Inferred age: ca 515Ma (Squire and Wilson 2005). Locally intercalated with Albion Formation. See also p760 Fig. 1c.||||||
39629|Magdala Basalt|62752|5|Briefly described|p759, p760 Fig. 1b|Cambrian|Cambrian|At Stawell. Intercalated with Albion Formation. Age is inferred as ca 515 Ma (Squire and Wilson 2005)||||||
39629|Magdala Basalt|62753|5|Briefly described|p800, p802 Fig. 2|||Basalt, sheet-like flows that overlie the Dukes Nose structure. Overlain by Albion Formation.||||||
39629|Magdala Basalt|62754|5|Briefly described|p869|Cambrian|Cambrian|Seafloor volcanics in Stawell. Has the highest magnetic susceptability of all the rocks of Stawell corridor.||||||
39629|Magdala Basalt|62755|5|Briefly described|p882|Cambrian|Cambrian|Ultramafic rocks.||||||
39629|Magdala Basalt|64597|5|Briefly described|pp759-764, pp766-767, pp771-774.   |||Forms a regional basalt dome. Its hydrothermal alteration is discussed in detail.||||Is locally overlain by Albion Formation.||
39629|Magdala Basalt|68314|5|Briefly described|p750-754|Early Cambrian|Early Cambrian|Watchorn and Wilson (1989). Stawell area. Three facies described. Displays strikingly similar magmatic affinities with Mount William Metabasalt and Lickhole Volcanic Group.||||Is overlain by Albion Formation.|Tholeiitic basalt lavas: about 70% pillow basalt, 25% massive basalt and 5% monomictic basalt breccia.|
39629|Magdala Basalt|70493|6|Mentioned|p56|Early Cambrian|Early Cambrian|Western Stawell Zone, Lachlan Orogen.||||Is overlain by Albion Formation.||
39629|Magdala Basalt|70718|5|Briefly described|p37|||Deposited as submarine basalts in relatively deep water.||||Intercalated with the Albion Formation.||
39629|Magdala Basalt|71249|6|Mentioned|p9|||Interpreted as tholeiitic.||||||
39629|Magdala Basalt|71593|4|Described|p19, p35-p37, p115|||Stawell Zone. Geochemically similar to back-arc basalts. Age is poorly constrained by a high uncertainty Pb/Pb model age of 518 +/- 52 Ma (Crawford et al, 2003).||||Overlain by the Saint Arnaud Group.|Massive and pillowed basaltic lavas, volcaniclastic interflow sediments and minor chert deposits.|
39629|Magdala Basalt|73059|5|Briefly described|p1059|Early Cambrian|Early Cambrian|Western Stawell Zone.||||Is overlain by Albion Formation.||
39629|Magdala Basalt|73118|6|Mentioned|p74||||||||Tholeiite sequence typical of ocean floor basalts.|
39629|Magdala Basalt|73430|6|Mentioned|p517|||Stawell Zone. Also written as Magdala Basalts p493. See also Magdala basalt.||||||
33278|Maitland Beach Volcanics|23309|5|Briefly described|p25 Table 2.1, p28 table 2.4|Cambrian|Cambrian|||||||05-NOV-07
33278|Maitland Beach Volcanics|24002|5|Briefly described|p231|||||||||
33278|Maitland Beach Volcanics|24098|5|Briefly described|p27 Fig. 2, p30|Cambrian||Unconformably overlain by Bear Gully Chert and Digger Island Marlstone.  Geological Province: Melbourne Zone, Lachlan Fold Belt (Waratah Bay Platform).||||||19-APR-05
33278|Maitland Beach Volcanics|24164|6|Mentioned|p15 Fig.8|Cambrian|Neoproterozoic|Selwyn Block. Ages estimated from figure.|||||Mafic|
33278|Maitland Beach Volcanics|24551|4|Described|p89|Cambrian|Cambrian|Overlain by Bear Gully Chert||||||
30435|Major Mitchell Sandstone|23309|5|Briefly described|p82. Tb 2.27|||Maximum Thickness: 450m.  Of the Red Man Bluff Subgroup.||||||
30435|Major Mitchell Sandstone|24551|5|Briefly described|p122|||Of Red Man Bluff Subgroup.||||||
30435|Major Mitchell Sandstone|24581|5|Briefly described|p813|Silurian|Silurian|Of the Red Bluff Subgroup (Of the Grampians Group). Maximum thickness: 450m. Overlain by the Silverband Formation. Geological Province: Kanmantoo Fold Belt.||||||
30435|Major Mitchell Sandstone|44929|5|Briefly described|Map Legend|Silurian|Ordovician|Of Red Man Bluff Sub-Group. Quartz sandstone; reddish-yellow, medium- to coarse-grained, somewhat micaceous or feldspathic.||||||14-JUN-06
30435|Major Mitchell Sandstone|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Man Bluff Sub-Group (Grampians Group). Quartz sandstone, reddish-yellow, medium- to coarse-grained, somewhat micaceous or feldspathic; abundant Skolithos trace fossils.||||||13-JUN-06
30435|Major Mitchell Sandstone|44932|5|Briefly described|Map Legend|Silurian|Ordovician|Of Red Man Bluff Sub-Group. Quartz sandstone; reddish-yellow, medium- to coarse-grained, somewhat micaceous or feldspathic.||||||14-JUN-06
30435|Major Mitchell Sandstone|44933|5|Briefly described|Map Legend|Silurian|Ordovician|Of Red Man Bluff Sub-Group. Quartz sandstone; reddish-yellow, medium- to coarse-grained, somewhat micaceous or feldspathic.||||||14-JUN-06
30435|Major Mitchell Sandstone|60451|4|Described|p76, 80, 134|Early Devonian|Ordovician|Of the Red Man Bluff Subgroup (Grampians Group). Type section in text. Infaulted with Silverband Formation. Maximum Thickness: ~450m.||||||21-MAY-13
30435|Major Mitchell Sandstone|60456|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Man Bluff Sub-Group. Quartz sandstone: reddish yellow, medium to coarse grained, somewhat micaceous or feldspathic; with planar, trough and cross trough lamination, medium to thickly bedded.||||||21-MAY-13
30435|Major Mitchell Sandstone|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Man Bluff Subgroup. Quartz sandstone; reddish yellow, medium to coarse grained, micaceous or feldspathic.||||||
30435|Major Mitchell Sandstone|61183|3|Fully described|p30 Tb. 2, p40|||Of Red Man Bluff Subgroup (Grampians Group). Medium- to coarse-grained micaceous sandstone, minor feldspar; qtz silt matrix (haematite stained). Conformably overlying Silverband Formation. Overlies Kalymna Falls Sandstone. Max. thickness: 450m.||||||
30435|Major Mitchell Sandstone|61186|5|Briefly described|p79|||Of Red Man Bluff Subgroup (Grampians Group). Commonly contains Skolithos (worm burrow) trace fossils. Pinkish coloured rock with clots of fine-grained, pale green chlorite in the interstices of the grains, and coarse platy crystals of white mica. ||||||
30435|Major Mitchell Sandstone|61752|5|Briefly described|p15 Fig. 9|||See also p25 in site description for Golton Gorge.  Tabular cross-bedded deposits.||||||07-FEB-11
30435|Major Mitchell Sandstone|64541|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Red Man Bluff Sub-group. Quartz sandstone: reddish-yellow, medium to coarse-grained, somewhat micaceous or feldspathic; laminated, cross-laminated and trough cross-laminated, medium to thickly bedded. Abundant Skolithos trace fossils.||||||10-JUN-14
30435|Major Mitchell Sandstone|64610|5|Briefly described|Map legend|Ordovician|Ordovician|Of Red Man Bluff Subgroup (Grampians Gp). Quartz sandstone: reddish-yellow, med.to coarse-gr, somewhat micaceous or feldspathic; laminated, x-laminated and trough-x-laminated; med-thickly bedded; abundant Skolithos trace fossils - more lithological detail||||||
30435|Major Mitchell Sandstone|65313|6|Mentioned|p582-3, p581 Fig. 9,p582 Fig. 10|Wenlock|Llandovery|Includes the mid-Llandoverian Sandvika (?isotopic) Event at 436.2 Ma near base of unit. Includes trace fossils. Grampians National Park sections.||Of Red Man Bluff Subgroup.||Overlies Kalymna Falls Sandstone; underlies Silverbrand Formation.||26-MAR-12
30435|Major Mitchell Sandstone|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Red Man Bluff Subgroup. Defined by Cayley & Taylor, 1997.||||||
30435|Major Mitchell Sandstone|66589|6|Mentioned|p179|Silurian|Silurian|Case studies cited; not visited in the field by the authors of this study.||||||
30435|Major Mitchell Sandstone|68116|5|Briefly described|Appendix, Maps 22, 30, 39.|Ludlow|Late Ordovician|Contains abundant Skolithos trace fossils; occasional metre-scale low-angle burrows; pebbly lag horizons of sub-rounded vein quartz below Mount William; forms prominent outcrops.|||||Quartz sandstone: reddish-yellow, medium to coarse-grained, somewhat micaceous or feldspathic; laminated, cross-laminated and trough cross-laminated; medium to thickly bedded; thin interbeds of micaceous siltstone.|
11065|Malanganee Sand|30928|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
11065|Malanganee Sand|30932|6|Mentioned|Map legend|Quaternary|Quaternary|Equivalent in part to Lowan Sand||||||
11065|Malanganee Sand|30934|6|Mentioned|Map legend|Quaternary|Quaternary|Equivalence with Lowan Sand||||||
11065|Malanganee Sand|41848|3|Fully described|p369|||Age probably mid Pliocene to Holocene Lateral equivalent to Lowan Sand||||||
11065|Malanganee Sand|50154|6|Mentioned|p140|||Equivalent to the Lowan Sand.||||||
22248|Malcolm Creek Hyaloclastite|23309|5|Briefly described|p28 Table 2.4|||Of the Lickhole Volcanic Group.||||||
22248|Malcolm Creek Hyaloclastite|24551|5|Briefly described|p90|||Of the Lickhole Volcanic Group. Overlies Sheepyard Flat Andesite||||||
22248|Malcolm Creek Hyaloclastite|68116|5|Briefly described|Appendix, Map 34.|Cambrian|Cambrian||||||Boninitic hyaloclastite with occasional beds of pebbly grit and volcaniclastic sandstone.|
35571|Maldon Granodiorite|23261|5|Briefly described|p274, 287||Late Devonian|Max Age: 368 Ma.||||||
37575|Mammoth Porphyry|23309|5|Briefly described|p345|Early Devonian|Early Devonian|||||||
37575|Mammoth Porphyry|60503|5|Briefly described|p16, p112 Tb. 4|Early Devonian|Early Devonian|See also Mammoth lode porphyry, Mammoth lode complex and Mammoth complex.  Age: 402+/-7Ma [wrongly] shown as Ar/Ar p112. Geological Province: Cravensville Igneous Province. See also p144 Tb. 7, where age is shown as U/Pb zircon; p204.||||||19-SEP-18
37575|Mammoth Porphyry|68116|5|Briefly described|Appendix.|Eifelian|Pragian||||||Quartz-feldspar porphyry: phenocrysts of quartz, plagioclase and lesser alkali feldspar in a very fine groundmass that is altered to sericite, carbonate and clay; abundant pyrite; dyke margins have breccia with sulphide mineralisation.|
83443|Manangatang pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G316.|||||Granite; variably magnetic, to 80 nT; gravity low to 100 micrometres/second/second below regional.|
83443|Manangatang pluton|73505|6|Mentioned|p29|||G316. See also Manangatang Granite p18, 20.||||||
11187|Mannum Formation|9124|5|Briefly described|Map Legend|Miocene|Oligocene|Sandy limestones.||||||
11187|Mannum Formation|22799|5|Briefly described|p23 Fig.7|Early Miocene|Early Miocene|||||||
11187|Mannum Formation|22887|5|Briefly described|Fig.6 p13|Early Miocene|Late Oligocene|||||||
11187|Mannum Formation|22893|5|Briefly described|fig4 p9|Miocene|Miocene|||||||
11187|Mannum Formation|22938|5|Briefly described|fig5|Miocene|Miocene|In the Eastern Mount Lofty Ranges.||||||30-JAN-08
11187|Mannum Formation|23179|6|Mentioned|Fig.2|Middle Miocene|Late Oligocene|Divided informally in SA into late Oligocene lower Mannnum Formation and early Miocene upper Mannum Formation. parent: Murray Supergroup.||||||
11187|Mannum Formation|23226|2|Defined|p891|Longfordian|Janjukian|Informally divided into upper and lower members; includes the Swan Reach Dolomite Member in upper section.  Of Murray Supergroup.||||||30-JAN-08
11187|Mannum Formation|23768|4|Described|p28 Fig.5, p33-34|Middle Miocene|Early Miocene|Underlies Morgan Limestone. Geological Province: Murray Basin.  See also p125, p157-158.||||||11-SEP-09
11187|Mannum Formation|23818|5|Briefly described|p173 Fig.84, p182|Early Miocene|Early Miocene|Geological Province: Murray Basin. Overlain by Finniss Clay.||||||30-JAN-08
11187|Mannum Formation|24551|6|Mentioned|p323|||||||||
11187|Mannum Formation|24558|4|Described|p655 Fig. 3|Early Miocene|Oligocene|Low energy carbonate ramp sediments with common echinoids, bryozoans and molluscs. Conformably underlies Finnis Formation.||||||29-JUL-08
11187|Mannum Formation|29591|6|Mentioned|Table 20|||||||||
11187|Mannum Formation|29697|5|Briefly described|Table 1|||||||||
11187|Mannum Formation|30514|6|Mentioned|p105|||See also P106. Lower Miocene age||||||
11187|Mannum Formation|30750|6|Mentioned|p3|||Tertiary age||||||
11187|Mannum Formation|30751|6|Mentioned|Map legend|Miocene|Miocene|||||||
11187|Mannum Formation|30753|4|Described|Table 2|||Lower Miocene age||||||
11187|Mannum Formation|30754|5|Briefly described|p13|||See also p14, 22. Stratigraphic table.||||||30-JAN-08
11187|Mannum Formation|30758|6|Mentioned|p66|||Stratigraphy. Important source of coarse aggregate||||||
11187|Mannum Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
11187|Mannum Formation|30828|6|Mentioned|p115|||||||||
11187|Mannum Formation|31516|6|Mentioned|Fig. 6|||Ammatocarcinus distribution||||||
11187|Mannum Formation|31625|6|Mentioned|Fig. 5.2|||Miocene||||||
11187|Mannum Formation|31746|6|Mentioned|p195|||||||||
11187|Mannum Formation|31848|4|Described|p14|||Age: Lower Miocene and Oligo-Miocene.||||||30-JAN-08
11187|Mannum Formation|31922|6|Mentioned|Fig.2|||||||||
11187|Mannum Formation|31923|6|Mentioned|p17|||||||||
11187|Mannum Formation|32401|6|Mentioned|p103|||||||||
11187|Mannum Formation|32404|6|Mentioned|p18|||||||||
11187|Mannum Formation|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
11187|Mannum Formation|32432|6|Mentioned|Fig.2|||See also Table 1||||||
11187|Mannum Formation|32439|6|Mentioned|p99|||||||||
11187|Mannum Formation|32552|6|Mentioned|p84|||See also P184. Longfordian||||||
11187|Mannum Formation|32601|6|Mentioned|p672|||Type horizon for Paradoxechinus novus Laube||||||
11187|Mannum Formation|32653|6|Mentioned|p295|||||||||
11187|Mannum Formation|32862|5|Briefly described|Table 3|||||||||
11187|Mannum Formation|33224|6|Mentioned|Fig.35|||Photo||||||
11187|Mannum Formation|33826|6|Mentioned|p42|||Strat.table.||||||
11187|Mannum Formation|33834|5|Briefly described|p11|||||||||
11187|Mannum Formation|33982|6|Mentioned|p116|||||||||
11187|Mannum Formation|34029|5|Briefly described|Table 1|Early Miocene|Early Miocene|Aquifer. Lower Miocene.||||||30-JAN-08
11187|Mannum Formation|34114|4|Described|p50|||||||||
11187|Mannum Formation|34180|6|Mentioned|p212|||Tertiary||||||
11187|Mannum Formation|34248|6|Mentioned|p115|||||||||
11187|Mannum Formation|34296|5|Briefly described|p97|||||||||
11187|Mannum Formation|34308|4|Described|p180|||Correlation chart. Fig.84. Longfordian||||||
11187|Mannum Formation|34418|6|Mentioned|p506|||Equivalent||||||
11187|Mannum Formation|34421|6|Mentioned|p242|||See also PP243,244,259 etc||||||
11187|Mannum Formation|34460|6|Mentioned|Fig.3|||||||||
11187|Mannum Formation|34536|6|Mentioned|Map legend|Miocene|Miocene|||||||
11187|Mannum Formation|34758|6|Mentioned|Fig.2|||||||||
11187|Mannum Formation|34958|6|Mentioned|p88|||||||||
11187|Mannum Formation|35071|6|Mentioned|Table 1|||||||||
11187|Mannum Formation|35097|6|Mentioned|Fig.4|||||||||
11187|Mannum Formation|35200|6|Mentioned|Map legend|Miocene|Miocene|||||||
11187|Mannum Formation|35232|6|Mentioned|p11|||||||||
11187|Mannum Formation|35541|6|Mentioned|p12|||||||||
11187|Mannum Formation|36119|6|Mentioned|p58|||||||||
11187|Mannum Formation|37619|6|Mentioned|p2|||||||||
11187|Mannum Formation|38068|6|Mentioned|Fig.7|||||||||
11187|Mannum Formation|38070|6|Mentioned|Fig.12|||Murray Basin||||||
11187|Mannum Formation|38699|6|Mentioned|p8|||||||||
11187|Mannum Formation|39929|6|Mentioned|Fig.3|||||||||
11187|Mannum Formation|40003|5|Briefly described|p38|||||||||
11187|Mannum Formation|40820|6|Mentioned|Fig.4|||||||||
11187|Mannum Formation|41076|6|Mentioned|p56|||||||||
11187|Mannum Formation|41478|6|Mentioned|p86|||||||||
11187|Mannum Formation|41511|5|Briefly described|p18|||||||||
11187|Mannum Formation|41518|6|Mentioned|p146|||||||||
11187|Mannum Formation|41519|6|Mentioned|p168|||||||||
11187|Mannum Formation|41520|5|Briefly described|Fig.11|||||||||
11187|Mannum Formation|42125|5|Briefly described|p136|||||||||
11187|Mannum Formation|42127|5|Briefly described|p223|||||||||
11187|Mannum Formation|42130|6|Mentioned|Fig.3 P265|||||||||
11187|Mannum Formation|42134|6|Mentioned|Fig.3 P335|||||||||
11187|Mannum Formation|42137|6|Mentioned|p370|||||||||
11187|Mannum Formation|42138|6|Mentioned|Fig.2 P390|||||||||
11187|Mannum Formation|42371|6|Mentioned|p35, p41|||||||||
11187|Mannum Formation|42443|4|Described|p4|||||||||
11187|Mannum Formation|42473|6|Mentioned|p61|||||||||
11187|Mannum Formation|42499|5|Briefly described|Map legend|Miocene||||||||
11187|Mannum Formation|42717|5|Briefly described|map legend|Miocene||||||||
11187|Mannum Formation|42881|4|Described|Fig.3, P84|||||||||
11187|Mannum Formation|42966|2|Defined|Table 17, p128|Early Miocene|Late Oligocene|Of the Murray Group.||||||30-JAN-08
11187|Mannum Formation|43073|5|Briefly described|Table 3|||||||||
11187|Mannum Formation|43466|14|Not recorded|p3,Pl.1,fig.2|||Equivalent||||||
11187|Mannum Formation|43467|14|Not recorded|p3,19,25,31,32|||||||||
11187|Mannum Formation|43667|6|Mentioned|Fig.3,p12|Miocene|Oligocene|||||||
11187|Mannum Formation|43686|6|Mentioned|Fig.5,p233|||||||||
11187|Mannum Formation|43791|6|Mentioned|p372, Fig1|||||||||
11187|Mannum Formation|43804|6|Mentioned|Fig.2,p49|||||||||
11187|Mannum Formation|46802|6|Mentioned|Table 1|||||||||
11187|Mannum Formation|48971|6|Mentioned|p77|||||||||
11187|Mannum Formation|49038|5|Briefly described|p26|||||||||
11187|Mannum Formation|49040|6|Mentioned|p11|||||||||
11187|Mannum Formation|60785|5|Briefly described|p184 Fig.1, pp195-196.   |Burdigalian|Aquitanian|South Australia. Has yielded several fossil cetacean elements.|||||Yellow-orange calcarenite. Bryozoal calcarenite.|
11187|Mannum Formation|61155|5|Briefly described|p18|Early Miocene|Late Oligocene|Of the Murray Group. Overlies the Gambier Limestone; overlain by Finniss Clay. Age: ~24-20.5Ma. Thickness: 100m. Geological Province: Murray Basin.||||||25-MAY-06
11187|Mannum Formation|62899|6|Mentioned|p46, p48|Middle Miocene|Middle Miocene|In South Australia.||||||
11187|Mannum Formation|63460|4|Described|p839 Fig. 2b, p847|Early Miocene|Late Oligocene|Conformably overlies Ettrick Formation. Conformably overlain by Finniss Formation. Geological province: Murray Basin. Calcarenite, calcisiltite.||||||09-JUL-08
11187|Mannum Formation|63739|5|Briefly described|p46, p48|Middle Miocene|Middle Miocene|Contains ostracod assemblages in South Australia - eg. in Kingston-on-the-Murray.||||||01-JUL-08
11187|Mannum Formation|64237|5|Briefly described|p17, p18|Early Miocene|Late Oligocene|Part of the Ludbrook (1961) stratigraphic scheme for the Murray Group until 1995 when Rogers et al replaced it together with Morgan Limestone + Pata Limestone with the single unit, Mannum Limestone. Reinstated as Mannum Fm with reinstated Murray Gp.......||||||15-JUL-08
11187|Mannum Formation|65552|6|Mentioned|p5 Fig. 3|Miocene|Oligocene|Of Murray Group (western Murray Basin).||||||
11187|Mannum Formation|68715|5|Briefly described|p31 Fig.5|Burdigalian|Aquitanian|Murray Basin.||Of the Murray Group.||||
11187|Mannum Formation|70803|5|Briefly described|p24, p56, p60|Tertiary|Tertiary|Referred to as the Mannum Limestone on p24.|||||Fossiliferous marine limestone and calcareous sandstone.|
11187|Mannum Formation|72445|5|Briefly described|App.6 p1 Tb.1, p2 Fig.1, p6-7; App.7|Middle Miocene|Late Oligocene|Samples include bryozoans, molluscs and sponge spicules as well as benthic and planktic foraminifera in the Early Miocene M4 (17.54-16.39 Ma)and M5 (16.39-15.73 Ma) zones. App6 assigns the samples to upper Mannum Formation, but the well logs don't distinguish beyond Murray Group. Shown in App 7 Fig 4 (from Brown & Stephenson 1991).|Min age ~15.73 Ma from foraminifera.|Murray Supergroup/ Murray Group.||Overlies Renmark Group, Ettrick Formation. Underlies Finniss Formation. Shown as partially equivalent to Ettrick Formation.|Shown as limestone, App.7.|
11187|Mannum Formation|73118|6|Mentioned|p17|||||||||
11187|Mannum Formation|73188|6|Mentioned|p320|Miocene|Miocene|Murray Basin.||||||
11187|Mannum Formation|73228|4|Described|p50, p55-57|Middle Miocene|Early Miocene|Murray Basin. Deposited in shallow marine to littoral conditions.||Murray Group|||Cream to yellow-brown skeletal calcarenites, calcareous sandstone and sandy limestone, bryozoal limestone, marl, clay, and medium to coarse grained, sub-angular to well-rounded sand commonly cemented in a calcareous matrix.|
11187|Mannum Formation|73229|6|Mentioned|p66-67|Middle Miocene|Early Miocene|Murray Basin.||Murray Group||||
28720|Mansfield Group|22559|6|Mentioned|p589-590|Early Carboniferous|Late Devonian|||||||
28720|Mansfield Group|22628|6|Mentioned|fig1p108|Devonian|Devonian|||||||
28720|Mansfield Group|22729|4|Described|p583-4,590, 592||Carboniferous|Underlies Delatite Group.||||||28-FEB-08
28720|Mansfield Group|22857|6|Mentioned|p211|||Geological Province: Mount Howitt Province.||||||
28720|Mansfield Group|22859|5|Briefly described|p211,213|Early Carboniferous|Famennian|||||||
28720|Mansfield Group|22971|5|Briefly described|p18, p24|Carboniferous|Late Devonian|Comprises basal Mount Timbertop Conglomerate and Devils Plain Formation.  Age: 370-355Ma. "red bed" style sedimentation.||||||19-JAN-06
28720|Mansfield Group|23184|6|Mentioned|p177||Tournaisian|||||||
28720|Mansfield Group|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
28720|Mansfield Group|23309|5|Briefly described|Tb 2.68. p160, 171-186.|Early Carboniferous|Late Devonian|||||||28-FEB-08
28720|Mansfield Group|23456|6|Mentioned|p60|||||||||
28720|Mansfield Group|24004|5|Briefly described|p275 Fig.2|Devonian|Devonian|||||||
28720|Mansfield Group|24177|6|Mentioned|p14|||||||||
28720|Mansfield Group|24551|5|Briefly described|p88 Fig. 3.15, 168|Late Devonian|Late Devonian|||||||
28720|Mansfield Group|31713|5|Briefly described|p14|||||||||
28720|Mansfield Group|33602|6|Mentioned|Fig.2|||See also P24||||||
28720|Mansfield Group|35073|5|Briefly described|Table 5|||Mention P12 also.||||||
28720|Mansfield Group|35112|6|Mentioned|p280|||See also P281.||||||
28720|Mansfield Group|35277|3|Fully described|p109|||||||||
28720|Mansfield Group|40761|4|Described|p237|||||||||
28720|Mansfield Group|41047|6|Mentioned|p1|||||||||
28720|Mansfield Group|41571|6|Mentioned|Fig.2.7|||||||||
28720|Mansfield Group|41593|6|Mentioned|p3|||||||||
28720|Mansfield Group|41637|6|Mentioned|p209|||||||||
28720|Mansfield Group|41641|4|Described|p179|||||||||
28720|Mansfield Group|42547|4|Described|p57, 58|||||||||
28720|Mansfield Group|42827|3|Fully described|p179|||||||||
28720|Mansfield Group|43841|5|Briefly described|7||Carboniferous|||||||
28720|Mansfield Group|44187|5|Briefly described|Map Legend||Late Devonian|||||||
28720|Mansfield Group|60503|5|Briefly described|p28 Fig. 9|Carboniferous|Late Devonian|||||||
28720|Mansfield Group|60599|6|Mentioned|p14||Middle Devonian|Post Tabberabberan deformation.||||||
28720|Mansfield Group|61161|5|Briefly described|p131, p76-77 Fig 6.1|||Of Avon Supergroup. Includes Mount Kent Conglomerate. Overlies Delatite Group and Wellington Volcanic Group. Sedimentary. Age: estimated Early Carboniferous (Tournaisian?). GSV map code: Dam.||||||
28720|Mansfield Group|61163|4|Described|p14 Fig. 3.2|Late Devonian|Late Devonian|Of Avon Supergroup. Comprises Mount Kent Conglomerate and Snowy Plains Formation. Geological Province: Lachlan Fold Belt (Tabberabbera Zone).||||||
28720|Mansfield Group|61169|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Includes Mount Kent Conglomerate.||||||
28720|Mansfield Group|61170|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Includes Mount Kent Conglomerate.||||||07-FEB-11
28720|Mansfield Group|61171|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Includes Mount Kent Conglomerate.||||||
28720|Mansfield Group|61172|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Includes Mount Kent Conglomerate.||||||
28720|Mansfield Group|61173|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Includes Mount Kent Conglomerate.||||||
28720|Mansfield Group|61174|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Includes Snowy Plains Formation and Mount Kent Conglomerate.||||||07-FEB-11
28720|Mansfield Group|61175|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Includes Snowy Plains Formation and Mount Kent Conglomerate.||||||23-SEP-05
28720|Mansfield Group|61176|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Includes Snowy Plains Formation and Mount Kent Conglomerate.||||||23-SEP-05
28720|Mansfield Group|61177|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Includes Snowy Plains Formation and Mount Kent Conglomerate.||||||23-SEP-05
28720|Mansfield Group|61178|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Includes Snowy Plains Formation and Mount Kent Conglomerate.||||||
28720|Mansfield Group|61185|5|Briefly described|p14|||Thick redbeds and felsic volcanics of Avon and Mansfield groups.||||||07-FEB-11
28720|Mansfield Group|61187|5|Briefly described|p5 Fig.3.|Early Carboniferous|Late Devonian|Melbourne Zone, Melbourne Terrane. Correlative of Avon River and Mount Tambo Groups, Benambra Terrane.||||||
28720|Mansfield Group|63738|5|Briefly described|p3|Tournaisian||Of the Avon Supergroup. Includes the Snowy Plains Formation. Geological Province: Mansfield Basin.||||||11-MAR-08
28720|Mansfield Group|64010|5|Briefly described|p257, p258 Fig.1, p259, p260 Tb.1  |||||Of the Avon Supergroup.|Includes the Snowy Plains Formation and Mount Kent Conglomerate. |Overlies Wellington Volcanic Group.||
28720|Mansfield Group|64535|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of the Avon Supergroup. Contains Mount Kent Conglomerate.||||||22-DEC-08
28720|Mansfield Group|64536|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of the Avon Supergroup. Contains Mount Kent Conglomerate.||||||07-FEB-11
28720|Mansfield Group|64537|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of the Avon Supergroup. Contains Mount Kent Conglomerate.||||||07-FEB-11
28720|Mansfield Group|64538|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of the Avon Supergroup. Contains Mount Kent Conglomerate.||||||07-FEB-11
28720|Mansfield Group|64539|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of the Avon Supergroup. Contains Mount Kent Conglomerate.||||||22-DEC-08
28720|Mansfield Group|64540|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of the Avon Supergroup. Contains Mount Kent Conglomerate.||||||22-DEC-08
28720|Mansfield Group|64605|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of the Avon Supergroup. Includes Mount Kent Conglomerate.||||||
28720|Mansfield Group|64606|5|Briefly described|Map Legend|Quaternary|Early Carboniferous|Of Avon Supergroup. Includes Snowy Plains Formation and Mount Kent Conglomerate.||||||11-NOV-08
28720|Mansfield Group|64616|4|Described|p132, p137, p148, p157, p187-190, p253|Early Carboniferous|Early Carboniferous|See also p279, p299-300. Of Avon Supergroup. Redefined in 2000. Includes Mount Kent Conglomerate and Snowy Plains Formation. Unconformably overlies Wellington Volcanic Group; locally overlies Tolmie Igneous Complex. Age based on a single locality in Broken River. Gently folded and faulted by Kanimblan Orogeny to form the Mansfield Basin and Macalister Synclinorium. Geophysical characteristics given.||||||
28720|Mansfield Group|67847|6|Mentioned|p10 fig 2.3, p79|Upper Devonian|Upper Devonian|Hosts red-bed copper, uranium, vanadium and silver deposits. ||||||
28720|Mansfield Group|68297|5|Briefly described|p197|Early Carboniferous|Early Carboniferous|Includes Early Carboniferous vertebrate fauna.||||||
28720|Mansfield Group|69798|5|Briefly described|p4 Fig.2, p14, p17|Early Carboniferous|Late Devonian|Darling Basin. See Holdgate and Zillman (1992), Holdgate (1996). May have entered the oil generation window locally.||||||
28720|Mansfield Group|70629|6|Mentioned|p986|Late Devonian|Late Devonian|Melbourne Zone.||||||
75879|Manta Member|70076|6|Mentioned|South-Eastern: Fig.2|Maastrichtian|Maastrichtian|||Volador Formation.||||
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|||||||||
11247|Marble Creek Limestone|33407|6|Mentioned|p3|||Gastropod fauna||||||
11247|Marble Creek Limestone|39980|6|Mentioned|p20|||||||||
11247|Marble Creek Limestone|42826|6|Mentioned|p38|||||||||
27479|Marengo Granodiorite|23309|6|Mentioned|p436 App1|||G120 - I-Type.||||||
27479|Marengo Granodiorite|23710|14|Not recorded|p80|||Excursion details.||||||
27479|Marengo Granodiorite|23938|5|Briefly described|p38-39 Tb. 2|Devonian|Devonian|See also p86-87 Figs. 32 and 33.||||||25-SEP-08
27479|Marengo Granodiorite|24275|5|Briefly described|p1695|Devonian|Silurian|||||||
27479|Marengo Granodiorite|24551|6|Mentioned|p233|||See also Mount Leinster Granodiorite.||||||25-SEP-08
27479|Marengo Granodiorite|33393|6|Mentioned|p168|||||||||
27479|Marengo Granodiorite|35278|6|Mentioned|p360|||||||||
27479|Marengo Granodiorite|38145|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27479|Marengo Granodiorite|38367|6|Mentioned|Fig.9.|||||||||
27479|Marengo Granodiorite|39447|4|Described|p18|||||||||
27479|Marengo Granodiorite|43220|5|Briefly described|p11||Devonian|||||||
27479|Marengo Granodiorite|43770|6|Mentioned|p829|Devonian|Silurian|||||||
27479|Marengo Granodiorite|44184|5|Briefly described|Map Legend||Early Devonian|Shown as Marengo I-type.||||||
27479|Marengo Granodiorite|60503|4|Described|p166, p66-67|||Same as Marengo Granite? Unfoliated, weakly porphyritic and blue-grey, quartz, plagioclase and K-feldspar with finer grained hornblende, biotite and magnetite. Intrudes Omeo Metamorphic Complex. Intruded by Duggan Creek Granite. ||||||
27479|Marengo Granodiorite|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Hornblende-biotite granodiorite: I-type; medium to coarse grained, light grey to light green.||||||25-SEP-08
27479|Marengo Granodiorite|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Hornblende-biotite granodiorite: I-type; medium to coarse grained, light grey to light green||||||
27479|Marengo Granodiorite|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Hornblende-biotite granodiorite: I-type; medium to coarse grained, light grey to light green||||||
27479|Marengo Granodiorite|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Hornblende-biotite granodiorite: I-type; medium to coarse grained, light grey to light green||||||
27479|Marengo Granodiorite|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Hornblende-bitotie granodiorite: I-type; 426+/-7 Ma (U/Pb zircon); intensely magnetic (~1000 nT), less magnetic with northeast trends in south; very low total count, K, Th, U with northeast trends in south.||||||
27479|Marengo Granodiorite|61187|6|Mentioned|p25.|||||||||
27479|Marengo Granodiorite|68116|5|Briefly described|Appendix, Map 27.|Pridoli|Llandovery||||||Hornblende-biotite granodiorite: I-type; medium to coarse grained, weakly porphyritic; light grey to light green; with abundant mafic enclaves.|
27479|Marengo Granodiorite|71628|6|Mentioned|p2:57|||A pluton in Victoria. Not to be confused with Marengo Plain Monzogranite of the New England Orogen in NSW; this latter unit had been named the Marengo Adamellite by Paul (1984) who did not publish, and the Victorian unit has precedence.||||||
25207|Maretimo Clay Member|24551|5|Briefly described|p589|Tertiary|Tertiary|Of the Whalers Bluff Formation||||||
25207|Maretimo Clay Member|31625|6|Mentioned|Fig. 5.2|||Pliocene||||||
11300|Maribyrnong Alluvium|24551|6|Mentioned|p348|||||||||
11300|Maribyrnong Alluvium|30995|5|Briefly described|p31|||||||||
11300|Maribyrnong Alluvium|31512|5|Briefly described|p308|||||||||
11300|Maribyrnong Alluvium|41848|5|Briefly described|p386|||||||||
11300|Maribyrnong Alluvium|71203|14|Not recorded|p207|||River Terraces.||||||
33133|Marn Mering Granodiorite|23309|5|Briefly described|p335.|||G411, S-Type.||||||
33133|Marn Mering Granodiorite|23319|4|Described|p408 Fig. 1, p415|Ordovician|Cambrian|||||||07-FEB-07
33133|Marn Mering Granodiorite|24012|5|Briefly described|p217|||||||||
33133|Marn Mering Granodiorite|24551|5|Briefly described|p77|||Of the Glenelg River Complex||||||
33133|Marn Mering Granodiorite|50154|2|Defined|p92, p97, p247 App.5|||Of the Glenelg River Metamorphic Complex. Crosscuts the Scrubby Juction Granodiorite and Dunmore Leucotonalite.||||||15-SEP-04
33133|Marn Mering Granodiorite|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Muscovite-biotite leucogranodiorite; S-type||||||
33133|Marn Mering Granodiorite|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite leucogranodiorite||||||20-AUG-04
33133|Marn Mering Granodiorite|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite leucogranodiorite||||||20-AUG-04
33133|Marn Mering Granodiorite|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite leucogranodiorite||||||20-AUG-04
33133|Marn Mering Granodiorite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite leucogranodiorite||||||20-AUG-04
33133|Marn Mering Granodiorite|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite leucogranodiorite||||||20-AUG-04
33133|Marn Mering Granodiorite|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite leucogranodiorite||||||20-AUG-04
33133|Marn Mering Granodiorite|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite leucogranodiorite||||||20-AUG-04
33133|Marn Mering Granodiorite|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite leucogranodiorite||||||20-AUG-04
33133|Marn Mering Granodiorite|66002|6|Mentioned|p8 Tb.5|||G411. Defined by Kemp and Gray 1999.||||||
33133|Marn Mering Granodiorite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Muscovite-biotite leucogranodiorite: massive to weakly foliated, light grey, medium to coarse grained, weakly microcline-phyric; accessory garnet in western part of pluton; non-magnetic.|
11344|Maronna Granite|39967|6|Mentioned|p106|||||||||
22271|Marroo Subgroup|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Snowy River Volcanics||||||
22271|Marroo Subgroup|23309|4|Described|p110. Tb 2.40|||Of the Snowy River Volcanics.   Overlies: Wombargo Subgroup, Windarra Formation & overlies and is Partly intruded by Deddick Lava.||||||
22271|Marroo Subgroup|23615|3|Fully described|p98, p22|Early Devonian|Early Devonian|Of Snowy River Volcanics. Comprises Statham,  Black Satin, Currie Creek and Glen Sheil Ignimbrites.  Age: Early Devonian ~410-395Ma.||||||16-AUG-18
22271|Marroo Subgroup|24551|4|Described|p143, p141 Fig.  5.32|||Of Snowy River Volcanics. Consists of 4 thick subaerial ignimbrite accumulations.||||||
22271|Marroo Subgroup|43206|5|Briefly described|map legend||Ludlow|Of Snowy River Volcanics||||||
22271|Marroo Subgroup|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Unit in Snowy River Volcanics.|||Extrusive, fluvial: felsic ignimbrite, minor conglomerate, sandstone.|
74936|Marshall Creek Member|64535|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Norton Gully Sandstone (Walhalla Group). Medium to thick bedded sandstone, quartz-mica lithic, Tabc turbiditic; graphitic black-dk.grey mudstone, medium- to thick bedded; deep-marine turbidite fan and hemipelagic deposits. ||||||
74936|Marshall Creek Member|64539|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Norton Gully Sandstone (Walhalla Group). Medium to thick bedded sandstone, quartz-mica lithic, Tabc turbiditic; graphitic black-dk.grey mudstone, medium- to thick bedded; deep-marine turbidite fan and hemipelagic deposits. ||||||
74936|Marshall Creek Member|64540|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Norton Gully Sandstone (Walhalla Group). Medium to thick bedded sandstone, quartz-mica lithic, Tabc turbiditic; graphitic black-dk.grey mudstone, medium- to thick bedded; deep-marine turbidite fan and hemipelagic deposits. ||||||
74936|Marshall Creek Member|64616|3|Fully described|p116, p163, p303|Emsian|Emsian|New name. Basal unit of Norton Gully Sandstone. Conformable on underlying Wilson Creek Shale. 50-400m thick. Medium- to thick-bedded, quartz-mica-lithic sandstone; graphitic black to dark grey mudstone. Age inferred from stratigraphic position. Geophysical characteristics given.||||||
32564|Marthavale Tonalite|22968|5|Briefly described|P193||Early Devonian|New name, age of unit is 404+/-6 Ma||||||
32564|Marthavale Tonalite|23020|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Mount Baldhead Igneous Complex. G547a: highly to intensely magnetic; low K, Th, moderate U. G547b: covered by hornfels: moderately magnetic. G547c: covered by hornfels: highly magnetic. For G547d to G547i see map legend.||||||15-SEP-04
32564|Marthavale Tonalite|23030|5|Briefly described|Map legend|Late Silurian|Late Silurian|Parent is the Mount Baldhead Igneous Complex||||||
32564|Marthavale Tonalite|23309|5|Briefly described|p161-166, 342|Early Devonian|Early Devonian|G547 - I-Type. Age: 404+/-6 Ma.||||||
32564|Marthavale Tonalite|24551|6|Mentioned|p44 Fig. 2.51|||||||||
32564|Marthavale Tonalite|61161|5|Briefly described|p95, p76-77 Fig 6.1|Early Devonian|Early Devonian|Of Mount Baldhead Igneous Complex. Intruded by Mount Baldhead Granodiorite. Concentric magnetic and nonmagnetic zones. More magnetic: tonalite or quartz diorite; less magnetic: less mafic tonalite or granodiorite. GSV map code: G547.||||||
32564|Marthavale Tonalite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende granodiorite, tonalite, quartz diorite: concentrically zoned; outer phase: homogeneous granodiorite; inner phases: biotite-hornblende granodiorite, tonalite, quartz diorite. I-type intrusion. GSV map code: G547.||||||
32564|Marthavale Tonalite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende granodiorite, tonalite, quartz diorite: concentrically zoned; outer phase: homogeneous granodiorite; inner phases: biotite-hornblende granodiorite, tonalite, quartz diorite. I-type intrusion. GSV map code: G547.||||||07-FEB-11
32564|Marthavale Tonalite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende granodiorite, tonalite, quartz diorite: concentrically zoned; outer phase: homogeneous granodiorite; inner phases: biotite-hornblende granodiorite, tonalite, quartz diorite. I-type intrusion. GSV map code: G547.||||||
32564|Marthavale Tonalite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende granodiorite, tonalite, quartz diorite: concentrically zoned; outer phase: homogeneous granodiorite; inner phases: biotite-hornblende granodiorite, tonalite, quartz diorite. I-type intrusion. GSV map code: G547.||||||
32564|Marthavale Tonalite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende granodiorite, tonalite, quartz diorite: zoned with 3 of 10 phases occurring in DARGO: high gravity response, moderate K, low Th, low to moderate U, and moderate total radioelements. GSV map code: G547.||||||
32564|Marthavale Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Biotite-hornblende granodiorite, tonalite, quartz diorite: concentrically zoned with variable composition ranging from granodiorite and tonalite to hornblende-bearing quartz diorite; equigranular, fine to medium grained; concentric magnetic zones.|
11424|Marysville Igneous Complex|22768|6|Mentioned|p188|||||||||
11424|Marysville Igneous Complex|22857|5|Briefly described|p188, p203|Late Devonian|Late Devonian|Sedimentary intercalations contain Late Devonian fish fossils. Unconformably overlies the Cathedral Group.||||||
11424|Marysville Igneous Complex|22859|6|Mentioned|p203|||||||||
11424|Marysville Igneous Complex|23229|5|Briefly described|Table3-3p27|Late Devonian|Late Devonian|||||||
11424|Marysville Igneous Complex|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
11424|Marysville Igneous Complex|23309|5|Briefly described|p160-166, 259, 349|||||||||
11424|Marysville Igneous Complex|23938|5|Briefly described|p117|Late Devonian|Late Devonian|Contains the Cerberean Caudron ring dyke.||||||25-SEP-08
11424|Marysville Igneous Complex|24004|5|Briefly described|p275 Fig.2|Devonian|Devonian|||||||
11424|Marysville Igneous Complex|24551|4|Described|p162|||||||||
11424|Marysville Igneous Complex|24588|5|Briefly described|p33|Late Devonian|Late Devonian|Age: 373+/-4 Ma (Richards and Singleton, 1981). Unconformably overlies: Cathedral Group unconformably.||||||29-NOV-13
11424|Marysville Igneous Complex|32001|6|Mentioned|p78|||||||||
11424|Marysville Igneous Complex|32074|6|Mentioned|p181|||||||||
11424|Marysville Igneous Complex|33238|6|Mentioned|p643|||||||||
11424|Marysville Igneous Complex|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
11424|Marysville Igneous Complex|33732|6|Mentioned|p107|||||||||
11424|Marysville Igneous Complex|34989|6|Mentioned|p81|||||||||
11424|Marysville Igneous Complex|35073|4|Described|p8|||||||||
11424|Marysville Igneous Complex|35186|6|Mentioned|Fig.2|||||||||
11424|Marysville Igneous Complex|35277|3|Fully described|p83|||||||||
11424|Marysville Igneous Complex|39291|4|Described|p217|||||||||
11424|Marysville Igneous Complex|39331|6|Mentioned|Fig.1-1|||||||||
11424|Marysville Igneous Complex|40761|5|Briefly described|p234|||||||||
11424|Marysville Igneous Complex|41641|4|Described|p153|||Mention on P161||||||
11424|Marysville Igneous Complex|41868|6|Mentioned|p485|||||||||
11424|Marysville Igneous Complex|42827|3|Fully described|p153|||||||||
11424|Marysville Igneous Complex|44187|5|Briefly described|Map Legend||Late Devonian|||||||
11424|Marysville Igneous Complex|64616|5|Briefly described|p131|||Lies mostly to the west of the project area. Includes Buxton Granite.||||||
11424|Marysville Igneous Complex|67804|6|Mentioned|p65|Late Devonian|Middle Devonian|Includes the Cerberean caldera, whose ring dyke hosts the Blue Gum and Wild Dog gold prospects.||||||
11424|Marysville Igneous Complex|68311|6|Mentioned|p272-273, 277, 286|Late Devonian|Late Devonian|Central Victoria. Includes the Cerberean Cauldron, filled with 900 km3 of intra-cauldron ignimbrites.|||Taggerty, Cerberean Subgroups.|||
11424|Marysville Igneous Complex|70742|5|Briefly described|p162-164|Late Devonian|Late Devonian|Occupies the centre of the Cerberean Cauldron, S of Lake Eildon.|||Teggarty, Cerberean Subgroups; Buxton Granite.|Overlies Cathedral and Walhalla Groups.|Volcanics, with minor intercalated sediments containing a fish fauna.|
11424|Marysville Igneous Complex|70933|14|Not recorded|p97||Late Devonian|||||||
11424|Marysville Igneous Complex|73199|6|Mentioned|p521, p524-525|Frasnian|Frasnian|Dominantly S-type with minor I-type. Inferred to have similar deep-crustal sources to plutonic granitic magmas.|374 Ma|||||
11424|Marysville Igneous Complex|75062|6|Mentioned|p74 Fig.2, p87 Fig.14|Devonian|Devonian|Melbourne Zone. Harker-type plots.|||||S-type.|
11424|Marysville Igneous Complex|75072|6|Mentioned|p230 Fig.2, 233|Late Devonian|Late Devonian|Melbourne Zone.|||Lake Mountain Rhyodacite.|||
68588|Massacre Shale|12796|4|Described|p460, p456 Fig. 2|Danian|Maastrichtian|Previously within Pebble Point Formation but classed as separate formation. In Wangerrip Group. Overlies Timboon Sandstone; underlies Pebble Point Formation. Geological Province: Otway Basin. ||||||
68588|Massacre Shale|24551|5|Briefly described|p257 Fig. 9.25, p292 Fig. 10.3|||Of the Sherbrook Group.||||||14-APR-08
68588|Massacre Shale|61017|5|Briefly described|p5 Fig. 2|Maastrichtian|Maastrichtian|Of the Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
68588|Massacre Shale|61470|5|Briefly described|p28 Fig. 5|Maastrichtian|Maastrichtian|Of the Sherbrook Group. Overlies Timboon Sandstone. Geological Province: Otway Basin.||||||12-OCT-05
68588|Massacre Shale|67366|5|Briefly described|p103 Fig.2. |Paleocene|Paleocene|||Unit in Wangerrip Group.||Unconformably overlies Timboon Sandstone. Is overlain by Pebble Point Formation.|Shelf to open marine shale.|
68588|Massacre Shale|67367|5|Briefly described|p131 Fig.2. |Early Paleocene|Late Cretaceous|||Unit in Wangerrip Group.||||
68588|Massacre Shale|69297|5|Briefly described|p79, p98|Danian|Maastrichtian|Otway Basin. ||Wangerrip Group||Overlies the Timboon Sandstone and the Wiridjil Gravel. Overlain by the Pebble Point Formation. |Shale. |
68588|Massacre Shale|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4; p5|Danian|Maastrichtian|Otway Basin: Gambier Embayment and Voluta Trough. Represents the first major transgression of the incipient Southern Ocean.||Wangerrip Group.||Overlies Timboon Sandstone and Wiridjil Gravel. Is overlain by Pebble Point Formation.||
68588|Massacre Shale|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Paleocene|Late Cretaceous|Gambier Embayment and Voluta Trough.||Wangerrip Group.||Overlies Timboon Sandstone. Is overlain by Pebble Point Formation.||
68588|Massacre Shale|70193|6|Mentioned|p284 Fig 2, p285 fig 3|Danian|Maastrichtian|Geological province: Otway Basin.  Part of the Sherbrook Supersequence.||||||
68588|Massacre Shale|73357|6|Mentioned|p24|Maastrichtian|Maastrichtian|Otway Basin. K/Pg Boundary Shale represents a widespread marine transgression, referred to as Massacre Shale by Partridge, (2001).||||||
68588|Massacre Shale|73386|5|Briefly described|p5, p12|||Otway Basin. Also referred to as Cretaceous/Paleogene boundary shale. Represents first marine flooding over Sherbrook Group.||||Unconformably overlies Sherbrook Group|Silty shale to argillaceous fine-grained sandstone.|
41776|Matheson pluton|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: low to moderate gravity response (-400 to -430 ums^-2); nonmagnetic, background is weakly magnetic (50 nT). GSV map code: G471.||||||21-SEP-05
41776|Matheson pluton|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: low to moderate gravity response (-400 to -430 ums^-2); nonmagnetic, background is weakly magnetic (50 nT). GSV map code: G471.||||||07-FEB-11
41776|Matheson pluton|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: low to moderate gravity response (-400 to -430 ums^-2); nonmagnetic, background is weakly magnetic (50 nT). GSV map code: G471.||||||21-SEP-05
41776|Matheson pluton|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: low to moderate gravity response (-400 to -430 ums^-2); nonmagnetic, background is weakly magnetic (50 nT). GSV map code: G471.||||||21-SEP-05
41776|Matheson pluton|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: low to moderate gravity response (-400 to -350 ums^-2); nonmagnetic, background is weakly magnetic (50 nT). GSV map code: G471.||||||
11453|Matlock Formation|31852|6|Mentioned|p720|||U.Sil.-L.Dev. See also Fig.5.||||||
11453|Matlock Formation|32074|6|Mentioned|Table 1|||Section. P180||||||
11453|Matlock Formation|32285|6|Mentioned|Fig. 4|||||||||
11453|Matlock Formation|33326|6|Mentioned|p437|||Fauna.||||||
11453|Matlock Formation|33601|6|Mentioned|p5|||P16||||||
11453|Matlock Formation|33732|5|Briefly described|p105|||||||||
11453|Matlock Formation|43461|14|Not recorded|p627|||||||||
11453|Matlock Formation|43547|14|Not recorded|Table p153|Gedinnian||(Skalian-Gedinnian)||||||
11453|Matlock Formation|70933|14|Not recorded|Table 1|Devonian|Silurian|Generalised east west section Silurian and Devonian,Victoria refers to Talent 1965.||||||
11464|Maude Basalt|23239|4|Described|Table1p109, 114-6||Oligocene|||||||
11464|Maude Basalt|29356|6|Mentioned|p145|||Appears on Table, dates given.||||||
11464|Maude Basalt|30929|6|Mentioned|Map legend|Miocene|Miocene|Torquay Group||||||
11464|Maude Basalt|33228|5|Briefly described|p4|||||||||
11464|Maude Basalt|33240|5|Briefly described|p4|||||||||
11464|Maude Basalt|33604|6|Mentioned|p20|||||||||
11464|Maude Basalt|34954|6|Mentioned|Fig.35|||||||||
11464|Maude Basalt|35262|5|Briefly described|p2|||See also p1.||||||07-JUL-20
11464|Maude Basalt|37035|6|Mentioned|p142|||||||||
11464|Maude Basalt|37385|6|Mentioned|p10|||See also p13.||||||07-JUL-20
11464|Maude Basalt|37547|6|Mentioned|p150|||||||||
11464|Maude Basalt|38070|6|Mentioned|Fig.12|||Bass Basin||||||
11464|Maude Basalt|44197|6|Mentioned|Map Legend||Oligocene|||||||
11464|Maude Basalt|60083|5|Briefly described|Map legend|Miocene|Miocene|Dense olivine basalt; minor pillow structure.||||||
11464|Maude Basalt|60084|5|Briefly described|Map legend|Tertiary|Tertiary|Olivine basalt.||||||19-JUL-04
11464|Maude Basalt|63445|5|Briefly described|Map legend.|Oligocene|Oligocene|||Maude Formation.|||Olivine basalt lava.|
11464|Maude Basalt|65715|5|Briefly described|p14 Tb.8, p15, p59-60|Neogene|Miocene|Of Bowler (1963) p90. Under- and overlain by limestone similar to Batesford Limestone. Also overlies Calivil Formation.||||||
11464|Maude Basalt|68116|5|Briefly described|Appendix, Maps 41, 50.|Aquitanian|Aquitanian||||||Alkali olivine basalt: dark grey-green; phenocrysts of olivine; commonly deeply weathered.|
11464|Maude Basalt|71419|6|Mentioned|p8 Fig 2|Miocene|Miocene|||||||
11496|Mayrung Member|29898|4|Described|p213|||||||||
11496|Mayrung Member|34735|6|Mentioned|p41|||||||||
11496|Mayrung Member|35272|5|Briefly described|p279|||||||||
11496|Mayrung Member|41848|5|Briefly described|p355|||Postdates Widgella Pedoderm. Member of Shepparton Formation.||||||27-OCT-08
11496|Mayrung Member|42827|5|Briefly described|p355|||Of Shepparton Formation.||||||14-JAN-09
11496|Mayrung Member|42966|2|Defined|Table 30 p197|Quaternary||Of Shepparton Formation.||||||27-OCT-08
11496|Mayrung Member|60599|5|Briefly described|p92|Quaternary|Quaternary|Informal name. Of Shepparton Formation.||||||
11496|Mayrung Member|70961|4|Described|p133|||Refers to Lawrence (1966). Alluvial.||||||
11503|McAdam Sandstone|23229|4|Described|Table3-2p21, 27, 32|Llandovery|Llandovery|||||||
11503|McAdam Sandstone|23266|5|Briefly described|Fig13-5.1p354||Wenlock|||||||
11503|McAdam Sandstone|23309|5|Briefly described|p143, 150, 152-153, 155|Llandovery|Llandovery|||||||
11503|McAdam Sandstone|24177|5|Briefly described|p50 Fig.22|Llandovery|Llandovery|Geological Province: Mount Easton Province.||||||
11503|McAdam Sandstone|24224|6|Mentioned|p264|||Geological Province: Turtons Creek Inlier.||||||
11503|McAdam Sandstone|24551|5|Briefly described|p128|Llandovery|Llandovery|||||||
11503|McAdam Sandstone|24588|5|Briefly described|p18-19, p12 Fig.3|Silurian|Silurian|Geological Province: Mount Easton Province. Of the Jordan River Group. See also p15 Tb.2, p17, 21, 26, 27, 28, 29. Shown as McAdam sandstone p29.||||||29-NOV-13
11503|McAdam Sandstone|33601|2|Defined|p6|Early Silurian|Early Silurian|||||||
11503|McAdam Sandstone|33604|6|Mentioned|p17|||Correlation chart. Sil.||||||
11503|McAdam Sandstone|33607|6|Mentioned|Map legend|Silurian|Silurian|||||||
11503|McAdam Sandstone|34843|6|Mentioned|p6|||||||||
11503|McAdam Sandstone|35092|5|Briefly described|Table 1|||||||||
11503|McAdam Sandstone|35281|6|Mentioned|p23|||||||||
11503|McAdam Sandstone|35283|4|Described|p49|||||||||
11503|McAdam Sandstone|36389|6|Mentioned|p41|||||||||
11503|McAdam Sandstone|37727|3|Fully described|p70|||Junior synonym of Enochs Point Beds. See also P30.||||||
11503|McAdam Sandstone|39331|6|Mentioned|Table 2-1|||||||||
11503|McAdam Sandstone|39858|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
11503|McAdam Sandstone|41571|6|Mentioned|Fig.2.6|||||||||
11503|McAdam Sandstone|41585|4|Described|p112|||||||||
11503|McAdam Sandstone|42827|4|Described|p112|||Of Jordan River Group.||||||27-OCT-08
11503|McAdam Sandstone|44187|5|Briefly described|Map Legend||Early Silurian|||||||
11503|McAdam Sandstone|60599|5|Briefly described|p47 Fig. 19|Llandovery|Llandovery|Geological Province: Mount Easton Province, Melbourne Zone, Lachlan Fold Belt.||||||
11503|McAdam Sandstone|61185|5|Briefly described|p37, p21 Fig. 6|Llandovery|Llandovery|Of Jordan River Group (VandenBerg, 1975). Faulted contact with underlying Mount Easton Shale; underlies Bullung Siltstone. Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
11503|McAdam Sandstone|62099|5|Briefly described|p331|Early Silurian|Early Silurian|In eastern Melbourne Zone of the Lachlan Orogen. ||||||
11503|McAdam Sandstone|64535|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp. Mid-pale grey, thin-thick bedded sst; Tabc, Tbc and Tc turbidites, generally med.to fine-gr., micaceous; mid-dark grey siltstone, laminated+bioturbated; shale contains rare Llandovery graptolites; deep marine trubidite fan deposits.||||||22-DEC-08
11503|McAdam Sandstone|64536|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp. Mid-pale grey, thin-thick bedded sst; Tabc, Tbc and Tc turbidites, generally med.to fine-gr., micaceous; mid-dark grey siltstone, laminated+bioturbated; shale contains rare Llandovery graptolites; deep marine trubidite fan deposits.||||||07-FEB-11
11503|McAdam Sandstone|64537|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp. Mid-pale grey, thin-thick bedded sst; Tabc, Tbc and Tc turbidites, generally med.to fine-gr., micaceous; mid-dark grey siltstone, laminated+bioturbated; shale contains rare Llandovery graptolites; deep marine trubidite fan deposits.||||||07-FEB-11
11503|McAdam Sandstone|64538|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp. Mid-pale grey, thin-thick bedded sst; Tabc, Tbc and Tc turbidites, generally med.to fine-gr., micaceous; mid-dark grey siltstone, laminated+bioturbated; shale contains rare Llandovery graptolites; deep marine trubidite fan deposits.||||||07-FEB-11
11503|McAdam Sandstone|64539|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp. Mid-pale grey, thin-thick bedded sst; Tabc, Tbc and Tc turbidites, generally med.to fine-gr., micaceous; mid-dark grey siltstone, laminated+bioturbated; shale contains rare Llandovery graptolites; deep marine trubidite fan deposits.||||||22-DEC-08
11503|McAdam Sandstone|64540|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp. Mid-pale grey, thin-thick bedded sst; Tabc, Tbc and Tc turbidites, generally med.to fine-gr., micaceous; mid-dark grey siltstone, laminated+bioturbated; shale contains rare Llandovery graptolites; deep marine trubidite fan deposits.||||||22-DEC-08
11503|McAdam Sandstone|64605|5|Briefly described|Map legend|Silurian|Silurian|Of the Jordan River Group. Sandstone, siltstone, minor shale; deep-marine deposits. Speckled pink-blue to brown and speckled light blue-yellow in RGB. Nonmagnetic.||||||17-NOV-08
11503|McAdam Sandstone|64606|5|Briefly described|Map Legend|Silurian|Silurian|Of Jordan River Group. Sandstone, siltstone, minor shale: deep-marine deposits. Speckled pink-blue to brown and speckled light blue-yellow in RGB. Nonmagnetic.||||||11-NOV-08
11503|McAdam Sandstone|64616|1|Redefined|p80, p155, p163-165, p170 Fig.6.17|Llandovery|Llandovery|See also p183 Fig.6.29, p197 Fig.6.34, p284, p286-287, p292, p305. Type locality revised. Of Jordan River Group. Conformable between underlying Donnellys Creek Siltstone and overlying Bullung Siltstone. Overlies Lazarini Siltstone in Matlock and Aberfeldy areas. Thick-bedded, medium- to fine-grained, micaceous sandstone; laminated and bioturbated siltstone; minor shale. Folded. 180-220m thick in type area but up to 700m elsewhere. Geophysical characteristics given.||||||
11503|McAdam Sandstone|68116|5|Briefly described|Appendix, Maps 25, 33-34, 43.|Telychian|Aeronian||||||Sandstone, siltstone, minor shale: sandstone mid- to pale grey, thick to thin-bedded, turbidites, generally medium to fine-grained, micaceous; siltstone mid- to dark grey, laminated and bioturbated; shale contains rare Llandovery graptolites.|
37576|McCarty Limestone|23309|5|Briefly described|p94|Llandovery|Llandovery|Of Cowombat Siltstone.||||||
83255|McEachern Member|73356|3|Fully described|p1, p7, p11-13, p19-20, p29|Valanginian|Berriasian|Otway Basin, Penola Trough. Revised unit; rank changed to member. [Misspelt as McEachern member on p7]. Unofficial type section is from McEachern-1 well where sidewall core samples were described by Cundill (1965). Core of this unit includes sections from Casterton-1, Jolly-1 ST1 and Bungaloo-1. Conformable with the overlying and underlying units of the Sawpit Formation. Corresponds to the S1-P2 chemostratigraphic package (Forbes et al., 2020). Thickness of 226.3 m in McEachern-1; maximum thickness of 344 m (Jolly-1 ST1). Age constraint is from palynologic biostratigraphy.||Sawpit Formation, Crayfish Subgroup, Otway Group||Disconformably underlain by Casterton Formation.|Medium grained to conglomeratic micaceous and carbonaceous sandstone including intraclasts, garnet and serpentine, with thin interbeds of siltstone and shale.|
83255|McEachern Member|73386|4|Described|p4, p6, p8, Attachment A1|Valanginian|Berriasian|Otway Basin. Basal unit of the Sawpit Formation. Belongs to the latest Berriasian to Valanginian Upper Ruffordiaspora australienses Spore-Pollen Subzone and the S1-P2 chemostratigraphic package (Eid et al., 2021a). Distribution restricted to the Penola Trough. Occurs in McEachern-1, Bus Swamp-1, Casterton-1 and Gordon-1 boreholes.||Sawpit Formation||Overlies Casterton Formation|Fluvial sandstones, quartz arenites and subarkoses, with thin interbeds of siltstone and shale.|
11550|McIvor Sandstone|22684|6|Mentioned|Fig.2 p746|Ludlow|Ludlow|||||||
11550|McIvor Sandstone|22885|5|Briefly described|map|Late Silurian|Late Silurian|||||||
11550|McIvor Sandstone|22886|5|Briefly described|p13|Late Silurian|Late Silurian|||||||
11550|McIvor Sandstone|23229|4|Described|Table3-3p26, 29|Pridolian|Ludlow|||||||
11550|McIvor Sandstone|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
11550|McIvor Sandstone|23309|5|Briefly described|p136, 138, 141, 152-153, 155|Devonian|Silurian|||||||
11550|McIvor Sandstone|24177|4|Described|p52, p50 Fig.22|Pridolian|Ludlow|Includes the Hylands Member. Overlain by the Mount Ida Formation. Overlies the Dargile Formation. Geological Province: Darraweit Guim Province. Maximum Thickness: 1900m.||||||27-OCT-08
11550|McIvor Sandstone|24328|5|Briefly described|Map legend|Late Silurian|Late Silurian|Includes the Hylands Member.||||||
11550|McIvor Sandstone|24329|5|Briefly described|Map legend|Late Silurian|Late Silurian|Includes the Hylands Member.||||||27-OCT-08
11550|McIvor Sandstone|24551|5|Briefly described|p123, 606|Upper Silurian|Upper Silurian|Included in the Murrindindi Supergroup.||||||
11550|McIvor Sandstone|33604|6|Mentioned|p17|||Correlation chart. Sil.||||||
11550|McIvor Sandstone|35283|3|Fully described|p48|||||||||
11550|McIvor Sandstone|37727|3|Fully described|p71|||||||||
11550|McIvor Sandstone|38378|6|Mentioned|p133|||||||||
11550|McIvor Sandstone|39331|6|Mentioned|Table 2-1|||||||||
11550|McIvor Sandstone|41585|5|Briefly described|p107|||||||||
11550|McIvor Sandstone|44197|5|Briefly described|Map Legend||Late Silurian|||||||
11550|McIvor Sandstone|60591|5|Briefly described|Map Legend|Pridoli|Ludlow|Includes the Hylands Member. Overlain by the Mount Ida Formation. Overlies the Dargile Formation. Consists of fine- to medium-grained sandstone, minor pebbly sandstone and conglomerate; massive to thickly bedded; shelly fossils.||||||
11550|McIvor Sandstone|60592|5|Briefly described|Map Legend|Pridoli|Ludlow|Includes the Hylands Member. Overlain by the Mount Ida Formation. Overlies the Dargile Formation. Consists of fine- to medium-grained sandstone, minor pebbly sandstone and conglomerate; massive to thickly bedded; shelly fossils.||||||25-NOV-04
11550|McIvor Sandstone|60593|5|Briefly described|Map Legend|Pridoli|Ludlow|Includes the Hylands Member. Overlain by the Mount Ida Formation. Overlies the Dargile Formation. Consists of fine- to medium-grained sandstone, minor pebbly sandstone and conglomerate; massive to thickly bedded; shelly fossils.||||||26-NOV-04
11550|McIvor Sandstone|60595|5|Briefly described|Map Legend|Pridoli|Ludlow|Includes the Hylands Member. Overlain by the Mount Ida Formation. Overlies the Dargile Formation. Consists of fine- to medium-grained sandstone, minor pebbly sandstone and conglomerate; massive to thickly bedded; shelly fossils.||||||26-NOV-04
11550|McIvor Sandstone|60596|5|Briefly described|Map Legend|Pridoli|Ludlow|Includes the Hylands Member. Overlain by the Mount Ida Formation. Overlies the Dargile Formation. Consists of fine- to medium-grained sandstone, minor pebbly sandstone and conglomerate; massive to thickly bedded; shelly fossils.||||||
11550|McIvor Sandstone|60597|5|Briefly described|Map Legend|Pridoli|Ludlow|Includes the Hylands Member. Low magnetic response, with weak magnetic linear features; moderate to high K, moderate Th, variable U.||||||29-NOV-04
11550|McIvor Sandstone|60599|3|Fully described|p14, p56-57, p106|Pridolian|Ludlow|Includes Hylands Member (lower part). Supersedes McIvor Beds (Thomas (1937), upper+lower "Camarotoechia beds" separated by "Grammysia band". Hard, pale grey quartzite, massive to thickly bedded. Relationships included. Max.thickness: ~1900m. ||||||
11550|McIvor Sandstone|61185|5|Briefly described|p22, p23, p21 Fig.6|Pridolian|Ludlow|Unit relationships with Dargile Formation in text p22 conflict with p21 Fig 6. Includes unit 4 of Dargile Beds of Thomas (1937); and Hylands Member. Humevale Siltstone equivalent. See McIvor Formation (possibly used interchangeably with).||||||07-FEB-11
11550|McIvor Sandstone|62469|5|Briefly described|p16, p15|Lochkovian|Ludlow|See also McIvor Formation p5, p6 - both names used in study.||||||12-FEB-15
11550|McIvor Sandstone|64611|5|Briefly described|Map legend|Pridoli|Ludlow|Of Murrindindi Supergroup. Contains Hyland Member. Sandstone - fine- to medium-grained, well sorted quartz arenite, minor pebbly sandstone and conglomerate beds also present; massive to thickly bedded, shelly fossils. Shallow marine, near-shore deposits.||||||16-DEC-08
11550|McIvor Sandstone|64612|2|Defined|p19, p27, p40-41, p52, p54, p68|Pridoli|Late Ludlow|Of Murrindindi Supergroup. Includes Hylands Member. Confomably overlied Dargile Formation. Thickness: 1900m. Pale grey, massive to thick-bedded, well sorted fine to medium-grained quartz arenite. Abundant shelly fossils.||||||07-FEB-11
11550|McIvor Sandstone|65969|6|Mentioned|p17 Fig.7|||||||||
11550|McIvor Sandstone|66244|5|Briefly described|p2.||||||Includes Hylands Member.|||
11550|McIvor Sandstone|68116|5|Briefly described|Appendix, Maps 24, 32.|Pridoli|Llandovery||||||Sandstone: fine to medium grained, well-sorted quartz arenite, minor pebbly sandstone and conglomerate beds also present; massive to thickly bedded; shelly fossils; shallow-marine nearshore deposit.|
11550|McIvor Sandstone|69089|5|Briefly described|Map legend|Late Silurian|Late Silurian||||||Marine: sandstone, mudstone, thick to thin bedded.|
11550|McIvor Sandstone|70487|6|Mentioned|p8, p11 Fig.5|Pridoli|Ludlow|Said to be correlative of Broadford Formation and overlying Puckapunyal Formation in VandenBerg et al. (2000: 141) but same publication (p106) shows McIvor Formation as older and correlation with Mount Ida Formation instead.||||Overlies Dargile Formation and underlies Mount Ida Formation.|Sandstone.|
11550|McIvor Sandstone|73497|5|Briefly described|Map legend|Silurian|Silurian|Marine.||Murrindindi Supergroup|||Quartz sandstone, minor conglomerate: low magnetic responses, weak magnetic linear features of short strike length (~2km); moderate-high K, moderate Th, variable U.|
28738|McKillops Bridge Granodiorite|23309|5|Briefly described|App1||| Indistinguishable from Amboyne Granodiorite.||||||
28738|McKillops Bridge Granodiorite|41850|6|Mentioned|p431|||||||||
28738|McKillops Bridge Granodiorite|42827|5|Briefly described|p431|||||||||
11561|McLarty Limestone Member|23309|5|Briefly described|p117-118. Tb 2.41|||Of the Murrindal Limestone.  Maximum Thickness: 190m.||||||
11561|McLarty Limestone Member|23615|3|Fully described|p141|Devonian|Devonian|Of Murrindal Limestone.  Flanks and interbeds with the Rocky Camp Limestone Member. Orginally defined by Teichert and Talent (1958) and redefined by Wallace (1982) to include all the dark limestone in Murrindal Limestone. Max. thickness: 190m.||||||
11561|McLarty Limestone Member|24551|5|Briefly described|p147, p606|||Of the Murrindal Limestone. Mx. thickness: 190m. Generally well-bedded, organic-rich,lagoonal carbonate; macrofossil-poor.||||||30-JAN-07
11561|McLarty Limestone Member|41585|6|Mentioned|p128|||||||||
11561|McLarty Limestone Member|42827|6|Mentioned|p128|||Of Cowombat Siltstone.||||||30-JAN-07
11561|McLarty Limestone Member|43206|5|Briefly described|map legend||Emsian|Of Murrindal Limestone.||||||30-JAN-07
22295|McRaes Ignimbrite|23309|4|Described|p108, 130-131. Tb 2.4|||Maximum Thickness: 120m.  Of the Little River Subgroup.||||||
22295|McRaes Ignimbrite|23615|3|Fully described|p127|Early Devonian|Early Devonian|Of Little River Subgroup.  Underlain by Fairy Sandstone.  Maximum thickness: 200m.  Distinctive unit containing large quartz phenocrysts in a bright red matrix.||||||
22295|McRaes Ignimbrite|43206|5|Briefly described|map legend||Lochkovian|Of Little River Subgroup.||||||22-FEB-07
22295|McRaes Ignimbrite|43312|5|Briefly described|Map Legend||Early Devonian|Of Little River Group.||||||22-FEB-07
22295|McRaes Ignimbrite|43313|5|Briefly described|Map Legend||Early Devonian|Of Little River Group.||||||22-FEB-07
22295|McRaes Ignimbrite|60542|3|Fully described|p61, p22 Tb. 2|Devonian|Devonian|Of Little River Subgp. Coarse grained quartz ignimbrite, overlain by epiclastic sediments. Overlies the Fairy Sst; overlain by Older Volc's. May be included in the Tara Range Subgp due to its composition and origin.||||||19-DEC-07
22295|McRaes Ignimbrite|68116|5|Briefly described|Appendix, Maps 36, 45.|Pragian|Pragian||||||Quartz ignimbrite, red, with large quartz and small feldspar phenocrysts, and overlying volcaniclastic sandstone and mudstone.|
75845|Meadow Creek Megabreccia|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Blocks of ignimbrite from Marroo Subgroup, White Monkey Volcanics and Yalmy Group quartzite in matrix of breccia and conglomerate.|
83437|Meatian pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G650.||Of Glenloth Suite|||Strongly magnetic (to 300 nT) above surrounds); a 10 micrometres/second/second gravity high.|
83437|Meatian pluton|73505|5|Briefly described|p18, p20|||Newly named unit in Swan Hill and parts of Balranald and Deniliquin 1:250 000 map areas, (G650). Named after Meatian, a minor town and parish. Subcircular intrusion about 4 km in diameter, on the northeast edge of Lalbert Batholith. Strongly magnetic, to 300 nT above surrounds. Gravity high of 10 micrometres/second/second.|||||Granite.|
11622|Melbourne Formation|13996|6|Mentioned|p146-147|Ludlow|Ludlow|Echinoderm taxa Table.||||||
11622|Melbourne Formation|22511|6|Mentioned|p661||Silurian|||||||
11622|Melbourne Formation|22542|6|Mentioned|p662|||||||||
11622|Melbourne Formation|22628|6|Mentioned|fig1p108|Silurian|Silurian|||||||
11622|Melbourne Formation|22684|4|Described|p753, Fig.2 p746|Ludlow|Ludlow|See also p745, p755.||||||27-OCT-08
11622|Melbourne Formation|22882|4|Described|p 11||Silurian|||||||
11622|Melbourne Formation|22885|5|Briefly described|map|Late Silurian|Late Silurian|||||||
11622|Melbourne Formation|22886|5|Briefly described|p13|Silurian|Silurian|||||||
11622|Melbourne Formation|23268|6|Mentioned|Fig14-2.1p388||Late Silurian|||||||
11622|Melbourne Formation|23269|5|Briefly described|Fig14-3.3p405|Early Devonian|Silurian|||||||
11622|Melbourne Formation|23272|6|Mentioned|Fig14-4.1p415||Late Silurian|||||||
11622|Melbourne Formation|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
11622|Melbourne Formation|23309|4|Described|p140-155|Silurian|Silurian|||||||
11622|Melbourne Formation|23522|5|Briefly described|p247 Fig 3|Silurian|Silurian|||||||
11622|Melbourne Formation|24177|5|Briefly described|p50 Fig.22|Silurian|Silurian|Geological Province: Darraweit Guim Province.||||||27-OCT-08
11622|Melbourne Formation|24551|5|Briefly described|p123, 622|||||||||
11622|Melbourne Formation|24588|5|Briefly described|p20-21, p12 Fig.3, p13, 27, 28|Ludlow|Ludlow|Geological Province: Darraweit Guim Province.Also shown as Melbourne Sandstone in Table 5 p27, p28.||||||29-NOV-13
11622|Melbourne Formation|33020|6|Mentioned|p232|||Semi-logarithmic plot of basal section.||||||
11622|Melbourne Formation|41585|4|Described|p109|||||||||
11622|Melbourne Formation|42826|6|Mentioned|p45|||||||||
11622|Melbourne Formation|42827|5|Briefly described|p109|||see also Table 4.1||||||
11622|Melbourne Formation|43282|5|Briefly described|p9,p19,p80.|Late Silurian||Age given p9 as 430-440my, p61, p19-Late Silurian.(430-440 is Ordovician - Early Silurian.)||||||14-APR-08
11622|Melbourne Formation|44187|5|Briefly described|Map Legend||Late Silurian|||||||
11622|Melbourne Formation|44197|5|Briefly described|Map Legend||Late Silurian|||||||
11622|Melbourne Formation|60599|6|Mentioned|p13, p54|Ludlow||The lower Melbourne Formation is equivalent to part of the redefined Dargile Formation. Geological Province: Melbourne Zone, Lachlan Fold Belt.||||||16-DEC-08
11622|Melbourne Formation|61185|5|Briefly described|p13, p22|Ludlow|Ludlow|Predominantly hemipelagic mud deposits. Conformable under Humevale Siltstone; Overlies Anderson Creek Formation. Geological Province: Lachlan Fold Belt, Melbourne Zone. See also Melbourne Formation, lower.||||||07-FEB-11
11622|Melbourne Formation|61187|6|Mentioned|p5 Fig.3.|Silurian|Silurian|Melbourne Zone, Melbourne Terrane.||||||
11622|Melbourne Formation|62469|5|Briefly described|p5 Fig. 2, p16, p15, p20|Ludlow|Ludlow|Geological Province: Darraweit Guim Province. See also p20 Fig. 11.||||||12-FEB-15
11622|Melbourne Formation|63083|6|Mentioned|p225|||Overlies Yan Yean Formation.||||||07-FEB-11
11622|Melbourne Formation|64612|6|Mentioned|p27|Late Ludlow|Late Ludlow|||||||07-FEB-11
11622|Melbourne Formation|66244|5|Briefly described|p2.|||The unit mapped as Dargile Formation in the Melbourne area is now considered to be this unit.|||||A sandstone-rich unit.|
11622|Melbourne Formation|68116|5|Briefly described|Appendix, Maps 33, 41-42.|Silurian|Silurian||||||Siltstone and sandstone: mainly thin-bedded; most beds show undisturbed Bouma sequences.|
11622|Melbourne Formation|71277|5|Briefly described|p303 Tb.1, p309 Fig.8|Silurian|Silurian|Basement to the Yarra Delta Group. Source of conglomerate-sized clasts in the Punt Road Sands. |||||Low- to medium-strength siltstone with interbedded high-strength sandstone. Folded, faulted and jointed. Dark grey when slightly weathered, white to brown when weathered. Some intrusions by porphyritic dykes.|
41961|Melbourne Suite|60543|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|Age: 370Ma (Rb/Sr).||||||28-OCT-04
41961|Melbourne Suite|60544|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|Age: 370Ma (Rb/Sr).||||||23-DEC-09
30559|Mellick Munjie Granodiorite|22968|6|Mentioned|P175|||Parent is Nunniong Batholith||||||
30559|Mellick Munjie Granodiorite|23309|5|Briefly described|p338.|Early Devonian|Late Silurian|G127 S-Type. Age: 418+/-3Ma.||||||
30559|Mellick Munjie Granodiorite|23615|3|Fully described|p157, p153 Tb.2|Silurian|Silurian|Of Bullenbalong Supersuite.  Intrudes the Nunniong Granodiorite.  Age: 418+/-3Ma (Henley and Webb, 1990).  See also p209 App. 1.||||||
30559|Mellick Munjie Granodiorite|24551|6|Mentioned|p234|||||||||
30559|Mellick Munjie Granodiorite|43206|5|Briefly described|map legend||Wenlock|Of Bullenbalong Suite. Granodiorite: pale grey, coarse to medium grained; minor cordierite||||||08-SEP-04
30559|Mellick Munjie Granodiorite|44185|5|Briefly described|Map legend.|Silurian|Silurian|S-type.||||||
30559|Mellick Munjie Granodiorite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Biotite-cordierite granodiorite: pale grey, coarse-medium grained; minor cordierite; S-type.|
11654|Mepunga Formation|22587|6|Mentioned|p79 Fig.7|Late Eocene|Middle Eocene|of the Nirranda Group||||||
11654|Mepunga Formation|22674|5|Briefly described|Fig.2 p719|Middle Eocene|Middle Eocene|||||||
11654|Mepunga Formation|22875|3|Fully described|p59|Early Oligocene|Eocene|Of the Nirranda Group.||||||07-MAR-07
11654|Mepunga Formation|22944|5|Briefly described|Fig3|Oligocene|Eocene|||||||
11654|Mepunga Formation|23230|5|Briefly described|Table4-1p40||Eocene|||||||
11654|Mepunga Formation|23238|5|Briefly described|p106||Tertiary|||||||
11654|Mepunga Formation|23322|5|Briefly described|957 Fig.2|Middle Eocene|Middle Eocene|Of the Nirranda Group.  Geological Province: Gambier Basin.||||||07-SEP-09
11654|Mepunga Formation|24200|5|Briefly described|p411|Oligocene|Eocene|Geological Province: Otway Basin.||||||
11654|Mepunga Formation|24314|5|Briefly described|p61 Fig.2|Middle Eocene|Middle Eocene|Geological Province: Otway Basin. Of the Nirranda Group.||||||
11654|Mepunga Formation|24397|5|Briefly described|p245|Late Eocene|Late Eocene|Geological Province: Otway Basin.||||||
11654|Mepunga Formation|24455|6|Mentioned|p327|||Overlain unconformably in some areas by Dilwyn Formation.||||||22-MAR-05
11654|Mepunga Formation|24551|5|Briefly described|p246, 296, p292 Fig. 10.3|Eocene|Eocene|Of the Nirrandra Group.  Max thickness: 160m.||||||
11654|Mepunga Formation|24562|5|Briefly described|p7,8 Fig.2|Eocene|Eocene|Conformably underlies Narrawaturk Marl.  Geological Province: Otway Basin.  Of the Nirranda Group.||||||07-MAR-07
11654|Mepunga Formation|29823|6|Mentioned|p14|||||||||
11654|Mepunga Formation|29825|5|Briefly described|p18|||||||||
11654|Mepunga Formation|29856|6|Mentioned|p36|||||||||
11654|Mepunga Formation|30576|5|Briefly described|Table 2|||||||||
11654|Mepunga Formation|30578|6|Mentioned|p9|||||||||
11654|Mepunga Formation|30580|6|Mentioned|Map legend|Eocene|Eocene|||||||
11654|Mepunga Formation|30675|5|Briefly described|p253|||||||||
11654|Mepunga Formation|30676|5|Briefly described|p12|||||||||
11654|Mepunga Formation|30932|6|Mentioned|Map legend|Eocene|Eocene|Part of Heytesbury Group.||||||20-SEP-07
11654|Mepunga Formation|31036|5|Briefly described|p194|||See also Table 9-1, p210. Unit of Nirranda Group.||||||07-MAR-07
11654|Mepunga Formation|31245|4|Described|p81|||See also p82. M.-U. Eocene.||||||07-MAR-07
11654|Mepunga Formation|31372|6|Mentioned|p12|||||||||
11654|Mepunga Formation|31424|4|Described|p14|||See also p7. Described from core.||||||07-MAR-07
11654|Mepunga Formation|31534|6|Mentioned|p363|||See also Table 19-1 ? aquifer in well. Water analysis.||||||
11654|Mepunga Formation|31625|6|Mentioned|Fig. 5.2|||Eocene||||||
11654|Mepunga Formation|32852|6|Mentioned|p10|||||||||
11654|Mepunga Formation|33155|5|Briefly described|p122|||||||||
11654|Mepunga Formation|33940|6|Mentioned|p414|||||||||
11654|Mepunga Formation|34063|6|Mentioned|p2|||Table. Upper Eocene.||||||20-SEP-07
11654|Mepunga Formation|34360|6|Mentioned|p11|||||||||
11654|Mepunga Formation|35066|4|Described|p209|||||||||
11654|Mepunga Formation|35285|6|Mentioned|p414|||||||||
11654|Mepunga Formation|35772|6|Mentioned|p9|||||||||
11654|Mepunga Formation|36913|6|Mentioned|p79|||||||||
11654|Mepunga Formation|37548|6|Mentioned|p131|||||||||
11654|Mepunga Formation|38625|6|Mentioned|Fig.2|||||||||
11654|Mepunga Formation|38932|4|Described|p98|||||||||
11654|Mepunga Formation|40003|5|Briefly described|p44|||See also Table 10||||||
11654|Mepunga Formation|40560|6|Mentioned|p6|||||||||
11654|Mepunga Formation|41185|6|Mentioned|Fig.4|||||||||
11654|Mepunga Formation|41269|5|Briefly described|p246|||||||||
11654|Mepunga Formation|41517|6|Mentioned|p134|||See also P139||||||
11654|Mepunga Formation|41642|6|Mentioned|Fig.8.6|||||||||
11654|Mepunga Formation|41701|6|Mentioned|Map legend|Oligocene||||||||
11654|Mepunga Formation|41704|6|Mentioned|Fig.3|||||||||
11654|Mepunga Formation|41714|6|Mentioned|Fig.2|||||||||
11654|Mepunga Formation|41726|6|Mentioned|Fig.5|||||||||
11654|Mepunga Formation|41769|4|Described|p25|||||||||
11654|Mepunga Formation|41868|5|Briefly described|p535|||||||||
11654|Mepunga Formation|42318|6|Mentioned|Fig.2 P10|||||||||
11654|Mepunga Formation|42453|6|Mentioned|p11|||Port Campbell Embayment||||||
11654|Mepunga Formation|42524|5|Briefly described|Fig.3 P27|||||||||
11654|Mepunga Formation|42601|6|Mentioned|Fig.2 p15|||||||||
11654|Mepunga Formation|42827|5|Briefly described|p283|||Of Nirranda Sub-group.||||||07-MAR-07
11654|Mepunga Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
11654|Mepunga Formation|43171|6|Mentioned|5-8|||Of Nirranda Group. Age: 40-45Ma||||||12-SEP-18
11654|Mepunga Formation|43195|5|Briefly described|Map Legend||Middle Eocene|See also commentary on back of map. Of Nirranda Group.||||||
11654|Mepunga Formation|43208|5|Briefly described|map legend|Early Oligocene|Middle Eocene|||||||
11654|Mepunga Formation|43219|5|Briefly described|Fig.3,p6.||Eocene|Of Nirranda Group.||||||07-MAR-07
11654|Mepunga Formation|43590|4|Described|p21|Early Oligocene|Middle Eocene|||||||
11654|Mepunga Formation|43660|6|Mentioned|Fig.6,p15|Oligocene|Eocene|||||||
11654|Mepunga Formation|43667|6|Mentioned|Fig.3,p12||Middle Eocene|||||||
11654|Mepunga Formation|43733|6|Mentioned|Fig.2.11,p65||Eocene|||||||
11654|Mepunga Formation|43744|6|Mentioned|Fig.3,p3|||||||||
11654|Mepunga Formation|43814|6|Mentioned|Fig.3,p115|||||||||
11654|Mepunga Formation|43937|5|Briefly described|Map Legend|Middle Eocene|Paleocene|||||||
11654|Mepunga Formation|44133|4|Described|p155|Late Eocene|Middle Eocene|Of the Nirranda Group. Geological Province: Gambier Basin. Thickness: 12m. Conformably underlies Narrawaturk Marl.||||||20-SEP-07
11654|Mepunga Formation|48911|6|Mentioned|Chart 1|||||||||
11654|Mepunga Formation|48977|6|Mentioned|Fig.5|||||||||
11654|Mepunga Formation|60563|6|Mentioned|p47|||||||||
11654|Mepunga Formation|61155|5|Briefly described|p3, p18|Early Oligocene|Middle Eocene|Of the Nirranda Group. Calcareous sands.Partly interfingers with Demons Bluff Formation. Max. thickness: 380m. Geological Province: Otway Basin.||||||07-MAR-07
11654|Mepunga Formation|61182|3|Fully described|p25-26, p33|Early Oligocene|Middle Eocene|Of Nirranda Gp. Variously interpreted based on its sand and mudstone units. The Sturgess Point Mbr has two informally named units, the upper and lower Mepunga sands, above and below it. Disconformable over Dilwyn Fm; conformable below the Narrawaturk Marl||||||04-FEB-08
11654|Mepunga Formation|61547|6|Mentioned|p461 Fig.2. |Eocene|Eocene|||Unit in Nirranda Group.||Is overlain by Narrawaturk Marl.||
11654|Mepunga Formation|61623|6|Mentioned|p449 Fig. 4|Oligocene|Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
11654|Mepunga Formation|61624|6|Mentioned|p466 Fig. 2|Oligocene|Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
11654|Mepunga Formation|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4|Eocene|Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
11654|Mepunga Formation|61628|5|Briefly described|p509 Fig. 3|Early Oligocene|Middle Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
11654|Mepunga Formation|63124|3|Fully described|p87 Fig. 5.29, p90-91|Middle Eocene|Middle Eocene|Of Nirranda Group. Unconformably overlies Dilwyn Formation; conformably overlain by Narrawaturk Marl and Greenways Member of Gambier Limestone. Age: 46-39.5Ma. Thickness: ~12m. Geol.prov: Gambier Basin. Synonymous with Kongorong Sand (Ludbrook 1971).||||||31-JAN-08
11654|Mepunga Formation|63269|5|Briefly described|p605|Oligocene|Eocene|Otway Basin.||Nirranda Group.||||
11654|Mepunga Formation|63431|5|Briefly described|p677 Fig. 2|Eocene|Eocene|Of the Nirranda Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
11654|Mepunga Formation|65891|6|Mentioned|p221 Fig.5. |Paleogene|Paleogene|Central Otway Basin. Includes Sturgess Point Member. Age shown as Bartonian to Priabonian.||||||
11654|Mepunga Formation|66002|5|Briefly described|p10 Tb.7, p16, p26 Fig.7, p58|Paleogene|Paleogene|Of Nirranda Group. Overlies Dilwyn Formation. Underlies Narrawaturk Marl. Similar to Wiridjil Gravel, and therefore some outcrops reassigned to Wiridjil herein. ||||||
11654|Mepunga Formation|66245|6|Mentioned|p6 Fig.5. |Priabonian|Lutetian|||Unit in Nirranda Group.||||
11654|Mepunga Formation|67061|6|Mentioned|p546 Fig.3.|Eocene|Eocene|||Unit in Nirranda Group.||||
11654|Mepunga Formation|67366|5|Briefly described|p103 Fig.2. |Eocene|Eocene|||Unit in Nirranda Group.||Unconformably overlies Dilwyn Formation. Is overlain by Narrawaturk Marl.|Shallow to nearshore marine sandstone and shale.|
11654|Mepunga Formation|67367|5|Briefly described|p131 Fig.2. |Late Eocene|Middle Eocene|||Unit in Nirranda Group.||||
11654|Mepunga Formation|68116|5|Briefly described|Appendix, Maps 54-55.|Eocene|Eocene|Contains barrier island, beach and near shore, estuarine and lagoonal deposits.|||||Quartz sand: medium to coarse grained, iron-stained, minor detrital limonite, with gastropod and mollusc fragments; foraminifers; unconsolidated, locally cemented with calcite, interbedded with carbonaceous clayey silt to silty clay.|
11654|Mepunga Formation|69297|5|Briefly described|p79, p98|Bartonian|Bartonian|Otway Basin. ||Nirranda Group||Unconformably overlies the Dilwyn Formation. Overlain by the Narrawaturk Marl. |Siltstone. |
11654|Mepunga Formation|69651|5|Briefly described|p10|Oligocene|Eocene|||Nirranda Group.||Unconformably overlies Dilwyn Formation. Is overlain by Narrawaturk Marl.||
11654|Mepunga Formation|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4; p5|Eocene|Eocene|Otway Basin. Prograding nearshore to offshore marine clastics. Time-equivalent to Demons Bluff Formation and Eastern View Coal Measures.||Basal unit in Nirranda Group.||Overlies Dilwyn Formation. Is overlain by Narrawaturk Marl.||
11654|Mepunga Formation|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Eocene|Eocene|Gambier Embayment and Voluta Trough.||Nirranda Group.||Overlies Dilwyn Formation. Is overlain by Narrawaturk Marl.||
11654|Mepunga Formation|70193|6|Mentioned|p285 fig 3|||||||||
11654|Mepunga Formation|70880|6|Mentioned|p77|Oligocene|Eocene|Otway Basin.||||||
11654|Mepunga Formation|70942|4|Described|p126, 119|||||||||17-FEB-17
11654|Mepunga Formation|71266|6|Mentioned|p614 Fig.3|Oligocene|Eocene|Otway Basin.||||||
11654|Mepunga Formation|71437|4|Described|Fig. 1 opp 154, p155, p160|Eocene|Eocene|||Of Nirranda Group.||Sharp or transitional contact with [p155] Interfingers with  overlying Narrawaturk Marl [p160].|Mainly brown limonitic quartz sands, calcareous limonitic sands, and limonitic  sandy limestones, with some pyritic carbonaceous sandy mudstones.|
11654|Mepunga Formation|73357|5|Briefly described|p28-29, p31, p44, p46, p48|Priabonian|Bartonian|Otway Basin. Contains the Nothofagidites asperus Spore-Pollen Zone, non-marine to nearshore marine depositional environment. Correlated with Corrudinium incompositum Dinocyst Zone.||Of Nirranda Group||Overlies Dilwyn Formation, underlies Narrawaturk Marl.|Includes shales.|
11654|Mepunga Formation|73383|5|Briefly described|p3, p10 Tb.3.7, p21, p25, p165, p258|Eocene|Eocene|Otway Basin. Approximately equivalent to chemostratigraphic package S5-P10 which has high Si/Al and Th/Sc values. The top of the package is defined by an increase in Ca abundance into the overlying sequence. Lithologies based on geochemistry using the ChemLith classification includes calcareous and argillaceous sandstones, and using the Herron classification (1988) includes quartz arenite and Fe-sand. See also vi, p11 Tb.3.9, p34-35, p131, p137, p264.||Nirranda Group||Overlies Dilwyn Formation, Wangerrip Group, underlies Narrawaturk Marl|Very mature quartz-rich sandstone.|
11654|Mepunga Formation|73385|5|Briefly described|p5|Eocene|Eocene|Otway Basin.||Nirranda Group||Overlies Dilwyn Formation, underlies Narrawaturk Marl.|Shallow marine and nearshore sandstones.|
11654|Mepunga Formation|73386|4|Described|p4, p6, p13, Attachment A1|Priabonian|Bartonian|Otway Basin. Interpreted to comprise multiple transgressive sandstone units which step landwards in a north-westward direction, range of high energy siliciclastic shoreline to shelf facies. Shallow marine and nearshore depositional environments. Belongs to the Lower-Middle Nothofagidites asperus spore-pollen subzones.||Nirranda Group||Overlies Dilwyn Formation, Wangerrip Group, underlies Narrawaturk Marl|Sandstones and shales.|
11654|Mepunga Formation|73486|6|Mentioned|p511 Fig.2|Rupelian|Lutetian|Otway Basin.||Nirranda Group||||
11654|Mepunga Formation|73594|5|Briefly described|p4|Eocene|Eocene|Otway Basin.||Nirranda Group||Underlies Narrawaturk Marl|Shallow marine and nearshore sandstones.|
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.||||||
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|||||||
11725|Merrimu Gravel Member|23258|5|Briefly described|Fig12-3.1p214, 215, 217||Miocene|||||||
11725|Merrimu Gravel Member|39865|4|Described|p32|||See also P29||||||
11725|Merrimu Gravel Member|41868|6|Mentioned|p582|||||||||
11725|Merrimu Gravel Member|42827|5|Briefly described|p582|||of Werribee Formation||||||
11725|Merrimu Gravel Member|65715|5|Briefly described|p13|||Of Werribee Formation. Well exposed on the eastern bank of Lake Merrimu. Also referred to as Merrimu Conglomerate Member in this report.||||||
37760|Merrymbuela Gabbro|23309|6|Mentioned|p437, Appendix 1|||G404.||||||
37760|Merrymbuela Gabbro|60451|5|Briefly described|p87, 90|Early Devonian|Early Devonian|Dark coarse grained rock that may be associated with the Ararat Pluton. Probably early Devonian.||||||21-MAY-13
37760|Merrymbuela Gabbro|60454|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Ararat Suite. Gabbro: dark, coarse grained, porphyritic||||||
37760|Merrymbuela Gabbro|60459|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Ararat Suite. Gabbro.||||||
37760|Merrymbuela Gabbro|66002|6|Mentioned|p8 Tb.5|||G404. Defined by Cayley and Taylor 2001.||||||
37760|Merrymbuela Gabbro|68116|5|Briefly described|Appendix, Map 30.|Early Devonian|Early Devonian||||||Gabbro: dark, coarse grained porphyritic (6mm); with plagioclase and orthopyroxene phenocrysts; accessory clinopyroxene, K-feldspar, quartz, biotite and hornblende.|
38293|Metcalfe Granite|24383|5|Briefly described|p9 Fig.1|||Parent: Harcourt Suite. Geological Province: Lachlan Fold Belt||||||
38293|Metcalfe Granite|24384|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Harcourt Suite. Biotite granite, pale grey, medium to coarse-grained, commonly strongly porphyritic in K-feldspar.||||||
38293|Metcalfe Granite|24385|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Harcourt Suite.||||||
38293|Metcalfe Granite|24386|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Harcourt Suite. Biotite granite: pale grey, medium- to coarse-grained; commonly strongly porphyritic in K-feldspar.||||||
38293|Metcalfe Granite|24387|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Harcourt Suite. Biotite granite; pale grey, medium- to coarse-grained; commonly strongly porphyritic in K-feldspar.||||||
38293|Metcalfe Granite|24388|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Harcourt Suite.  Biotite granite; reduced I-type; nonmagnetic with weakly magnetic aureole in Ordovician rocks;  high K, moderate-high Th, moderate U, high total radioelements, areas of deeper weathering have low K and Th.||||||
38293|Metcalfe Granite|65715|5|Briefly described|p8 Tb.4|||G291. Of Harcourt Batholith.||||||
38293|Metcalfe Granite|68116|5|Briefly described|Appendix, Map 32.|Late Devonian|Late Devonian||||||Biotite granite: pale grey, medium to coarse grained; commonly strongly porphyritic in K-feldspar; numerous metasedimentary enclaves and leucocratic dykes; nonmagnetic.|
38293|Metcalfe Granite|75061|6|Mentioned|p65|||Bendigo Zone, Lachlan Fold Belt. Forms a narrow and partial fringe on the SE lobe of the Mount Alexander pluton, Harcourt batholith.||||||
39636|Metropolitan Sandstone|24088|6|Mentioned|p355 Fig. 4||| Geological Province: Lachlan Fold Belt.||||||
11748|Metung Marl Member|24551|5|Briefly described|p327 Fig. 10.33|Miocene|Oligocene|||||||
11748|Metung Marl Member|31922|6|Mentioned|p166|||||||||
11748|Metung Marl Member|35273|4|Described|p259|||||||||
11748|Metung Marl Member|42827|3|Fully described|p333|||Of Lakes Entrance Formation.||||||01-JUL-08
11748|Metung Marl Member|62899|5|Briefly described|p37 Fig. 2|||Of the Lakes Entrance Formation. Geological province: Lakes Entrance Platform.||||||
11748|Metung Marl Member|63739|5|Briefly described|p37 Fig. 2|||Of Lakes Entrance Formation. Geological province: Gippsland Basin.||||||01-JUL-08
11748|Metung Marl Member|65718|6|Mentioned|p10 Fig 3.2|Miocene|Oligocene|Early Miocene minimum age. Also appears as Metung Marl (p12, p18, p19).||Of the Lakes Entrance Formation.||||10-JAN-17
22332|Milky Creek Ignimbrite|23309|5|Briefly described|p108. Tb 2.40|||Of the Little River Subgroup.||||||
22332|Milky Creek Ignimbrite|23615|3|Fully described|p126, p29|Early Devonian|Early Devonian|Of Little River Subgroup.  Underlain by Wulgulmerang Ashstone.  Densely welded vitric-rich pink purple ignimbrite with green pumice fragments.  The remnant has a thickness of 25-50m. See also p226 App. 2.||||||10-JUN-14
22332|Milky Creek Ignimbrite|24551|5|Briefly described|p145|||Of Little River Subgroup.||||||
22332|Milky Creek Ignimbrite|43206|5|Briefly described|map legend||Lochkovian|of Little River Subgroup.||||||
22332|Milky Creek Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Vitric ignimbrite with green pumice and red to pink lithic clasts.|
28128|Millewa Group|22799|2|Defined|p18|Albian|Aptian|||||||
28128|Millewa Group|22857|5|Briefly described|p318, p548 App.1 Tb.A1.12|Early Cretaceous|Early Cretaceous|Max. thickness: 279m. Geological Province: Berri Basin. See also p350 Fig.24.5.||||||
28128|Millewa Group|22865|6|Mentioned|p318|||(Lawrence 1972).||||||
28128|Millewa Group|22887|4|Described|Fig.5 p12, p31|Early Cretaceous|Early Cretaceous|Proposed to be equivalent of Cretaceous sedimentary units in Booligal. Renmark Trough.||||||
28128|Millewa Group|22893|3|Fully described|p22,23 table3 fig4||Early Cretaceous|Overlies Urana Fm; underlies Olney Fm (Describes unamed equivalents of this unit concealed in the mapping area.||||||13-AUG-07
28128|Millewa Group|23252|5|Briefly described|Map Legend||Cretaceous|Equivalent to Taperoo Sandstone.||||||
28128|Millewa Group|24551|5|Briefly described|p270|||||||||
28128|Millewa Group|30905|5|Briefly described|p146|||||||||
28128|Millewa Group|31745|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
28128|Millewa Group|37873|4|Described|p1|||||||||
28128|Millewa Group|39211|6|Mentioned|Fig.23|||||||||
28128|Millewa Group|41642|4|Described|p224|||||||||
28128|Millewa Group|42184|6|Mentioned|Fig.2 P348|||||||||
28128|Millewa Group|42318|6|Mentioned|Fig.5 P12|||||||||
28128|Millewa Group|42827|5|Briefly described|p216|||see also Table 7.3||||||
28128|Millewa Group|42966|2|Defined|Fig.37 p71, Table 9|Albian|Aptian|||||||
28128|Millewa Group|43218|4|Described|Fig.3,p22|Albian|Aptian|||||||
28128|Millewa Group|44093|5|Briefly described|p145 App. 1|Cretaceous|Cretaceous|See also p245 Appendix 1. Geological Province: Kanmantoo Belt.||||||
28128|Millewa Group|44133|5|Briefly described|p127|||Includes: Taparoo Sandstone and Morkalla Formation.||||||
28128|Millewa Group|44188|6|Mentioned|Map Legend||Cretaceous|Includes Taparoo Sandstone and Urana Formation. Marine units at top,? fluvial in mid-sequence, and a basal lacustrine evaporitic sequence.||||||15-MAY-08
28128|Millewa Group|44191|5|Briefly described|Map Legend||Early Cretaceous|||||||
28128|Millewa Group|49038|5|Briefly described|p23|||||||||
28128|Millewa Group|49040|6|Mentioned|p8|||||||||
28128|Millewa Group|50154|6|Mentioned|p26|||||||||
28128|Millewa Group|60451|5|Briefly described|p95 Fig. 61|||||||||
83447|Mincha pluton|73497|5|Briefly described|Map legend|Devonian|Silurian|G750.||Mount Cole Suite|||Granite: intensely magnetic (up to 700 nT), gravity low of about 60 micrometres/second/second, estimated depth of 80-200 m.|
30555|Minchin Ignimbrite|23309|5|Briefly described|p123. Tb 2.47|||||||||
30555|Minchin Ignimbrite|23615|3|Fully described|p97|Early Devonian|Early Devonian|Of White Monkey Subgroup. Previously included in the Black Mountain Rhyodacite (of Ringwood, 1955a).  Overlies Bowen Track Ignimbrite and Yalmy Group.  Overlain by Bass Camp Ignimbrite.   Maximum thickness: ~80m.||||||
30555|Minchin Ignimbrite|24551|5|Briefly described|p149, p132 Fig.5.23|||Of White Monkey Volcanics||||||
30555|Minchin Ignimbrite|43206|5|Briefly described|map legend||Ludlow|White Monkey Subgroup||||||
30555|Minchin Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Early Devonian|Early Devonian||||||Vitric ignimbrite, small quartz and feldspar phenocrysts in green-grey or red fine matrix; lithic clasts include ignimbrite, glassy lava, sediment from Yalmy Group.|
11955|Miralie Member|29898|6|Mentioned|p218|||||||||
11955|Miralie Member|35272|6|Mentioned|p286|||||||||
11955|Miralie Member|41848|5|Briefly described|p361|||Member of Woorinen Formation.||||||
11955|Miralie Member|42264|6|Mentioned|Fig.5 P12|||||||||
11955|Miralie Member|42827|5|Briefly described|Table 9.1|||of Woorinen Formation||||||
11955|Miralie Member|42966|2|Defined|Table35 p236|Late Pleistocene||of Woorinen Formation||||||
11955|Miralie Member|44133|6|Mentioned|p253|Holocene|Middle Pleistocene|Of the Woorinen Formation. Geological Province: Murray Basin.||||||
11955|Miralie Member|70961|14|Not recorded|p138|||Stratigraphic sequence.||||||
25244|Mirimbah Granodiorite|22625|6|Mentioned|P726|||||||||
25244|Mirimbah Granodiorite|22971|6|Mentioned|p 24|||||||||
25244|Mirimbah Granodiorite|23309|5|Briefly described|p169.|||G186 - I-Type. Supersedes Mount Buller Granite||||||
25244|Mirimbah Granodiorite|32074|6|Mentioned|p181|||||||||
25244|Mirimbah Granodiorite|33602|6|Mentioned|p22|||||||||
25244|Mirimbah Granodiorite|42827|5|Briefly described|p151|||||||||
25244|Mirimbah Granodiorite|44187|5|Briefly described|Map Legend||Middle Devonian|G186 Unassigned.||||||
25244|Mirimbah Granodiorite|66252|6|Mentioned|p211 Fig.1.|||||||||
25244|Mirimbah Granodiorite|68116|5|Briefly described|Appendix, Map 34.|Middle Devonian|Middle Devonian||||||Hornblende granodiorite, diorite, gabbro: medium to coarse grained.|
25244|Mirimbah Granodiorite|70933|14|Not recorded|p95|Late Devonian|Middle Devonian|Late Middle to Early Upper Devonian igneous activity.||||||
30445|Mirranatwa Granite|23309|5|Briefly described|p339-342.||Early Devonian|G402 A-Type||||||
30445|Mirranatwa Granite|44929|5|Briefly described|Map Legend||Early Devonian|Part of the Victoria Valley Batholith. Hornblende soda granite, medium- to coarse-grained, equigranular to porphyritic, pink.||||||14-JUN-06
30445|Mirranatwa Granite|44930|5|Briefly described|Map Legend||Early Devonian|Part of the Victoria Valley Batholith. Hornblende soda granite, medium- to coarse-grained, equigranular to porphyritic, pink.||||||14-JUN-06
30445|Mirranatwa Granite|44932|5|Briefly described|Map Legend||Early Devonian|Part of the Victoria Valley Batholith. Hornblende soda granite, medium- to coarse-grained, equigranular to porphyritic, pink.||||||14-JUN-06
30445|Mirranatwa Granite|44933|5|Briefly described|Map Legend||Early Devonian|Of the Victoria Valley Batholith. Hornblende soda granite: medium to coarse grained, equigranular to porphyritic, pink; often granophyric; felsic, oxidised, I-type.||||||27-OCT-04
30445|Mirranatwa Granite|61183|4|Described|p60|Early Devonian|Early Devonian|Of Victoria Valley batholith intrusion. Medium to coarse-grained, equigranular, porphyritic soda granite of perthitic alkali feldspar, qtz, minor plagioclase and mafic crystals of soda-rich minerals. Age: 377+/-7Ma (young, not considered as cooling age). 393+/-3 Rb/Sr whole rock isochron of 16 samples from many of the intrusive phases of the Victoria Valley batholith (C.Gray pers. comm. 1995) may apply to this unit.||||||05-OCT-10
30445|Mirranatwa Granite|63457|5|Briefly described|p124-126, p130-137.    |||Apparently, formerly called Knights Hill Aegirine Granite and Western Aegirine Granite. Major and trace element data provided. Peralkaline nature discussed. A-type.|||||Pinkish, medium- to coarse-grained, typically even-grained but with some porphyritic variants; contains distinctive apple-green aegirine and Na-rich amphiboles.|
30445|Mirranatwa Granite|64541|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Victoria Valley Batholith. Hornblende soda granite: medium to coarse grained, equigranular to porphyritic, pink; often granophyric; felsic, oxidised, I-type.||||||02-MAY-13
30445|Mirranatwa Granite|64610|5|Briefly described|Map legend|Early Devonian|Early Devonian|Part of Victoria Valley Batholith. Hornbl. biotite adamellite to granite: fine- to med.-gr., gen'ly porph'tic; reddish to pale pinkish-grey; often strongly granophyric, miarolitic cavities; flow folded and banded rhyolitic dykes; felsic, oxidised, I-type||||||12-NOV-08
30445|Mirranatwa Granite|65313|6|Mentioned|p582, p581 Fig. 9|Devonian|Devonian|Grampians National Park.||||||26-MAR-12
30445|Mirranatwa Granite|66002|5|Briefly described|p8 Tb.5|||In Victoria Valley Batholith area.G402. Defined by Cayley and Taylor (1997).||||||
30445|Mirranatwa Granite|68116|5|Briefly described|Appendix, Map 30.|Early Devonian|Early Devonian||||||Hornblende granite: pink; often granophyric; medium to coarse-grained, equigranular to porphyritic, soda-rich; oxidised; small stocks.|
30445|Mirranatwa Granite|70877|4|Described|p13, p153, p161-p166, p170-p171, p202|Devonian|Devonian|SHRIMP ages derived from this study and represents the age of magmatic crystallisation. Outcrops as scattered whale-backs. Petrography, zircon morphology and SHRIMP U-Pb results are discussed in detail for a sample of this unit.|403.3 +/- 1.6 Ma (SHRIMP U-Pb)||||Medium-coarse grained, equigranular to feldspar phyric, biotite-hornblende bearing, quartz monzonite.|
30445|Mirranatwa Granite|70967|6|Mentioned|p11|||Mount Stavely Belt.||||Intrudes Grampians Group. Co-magmatic with Rocklands Volcanic Group.||
30445|Mirranatwa Granite|71410|6|Mentioned|p1052|||Shows REE enrichment: between 16.3 and 300 ppm La.||||||
30445|Mirranatwa Granite|72445|6|Mentioned|p10.|Early Devonian|Late Silurian|||||Intrudes Grampians Group. Comagmatic with Rocklands Volcanic Group.||
32392|Mitta Mitta Rhyolite|22708|6|Mentioned|p212|||||||||
32392|Mitta Mitta Rhyolite|22968|6|Mentioned|P121|||||||||
32392|Mitta Mitta Rhyolite|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
32392|Mitta Mitta Rhyolite|23309|5|Briefly described|p61, 90-97, 290, 294. Tb 2.32|Late Silurian|Late Silurian|||||||
32392|Mitta Mitta Rhyolite|23454|5|Briefly described|p27|Silurian|Silurian|Of Wombat Creek Group.||||||25-SEP-08
32392|Mitta Mitta Rhyolite|23938|5|Briefly described|p31-32 Fig. 12|Early Silurian|Early Silurian|See also p83 and p139 Tb. 1 Appendix.||||||25-SEP-08
32392|Mitta Mitta Rhyolite|24133|5|Briefly described|p40|||Geological Province: Lachlan Fold Belt.||||||
32392|Mitta Mitta Rhyolite|24551|4|Described|p136|||Not part of the Wombat Creek Group.||||||
32392|Mitta Mitta Rhyolite|44184|5|Briefly described|Map Legend|Early Silurian|Early Silurian|||||||
32392|Mitta Mitta Rhyolite|60503|3|Fully described|p89, p27|Late Silurian|Late Silurian|Of the Wombat Creek Group. Rhyolite, two horizons of volcaniclastic sediments. Silver Flat Porphyries intrusions were included until recognised that they are younger. Overlain by Wombat Creek Group; Undowah Siltstone.||||||16-NOV-09
32392|Mitta Mitta Rhyolite|60504|5|Briefly described|Map Legend|Ludlow|Ludlow|Rhyolite lava; pale grey, massive to autobrecciated, with minor intercalated reworked rhyolitic pyroclastics.||||||20-OCT-04
32392|Mitta Mitta Rhyolite|60505|5|Briefly described|Map legend|Ludlow|Ludlow|Rhyolite lava; pale grey, massive to autobrecciated, with minor intercalated reworked rhyolitic pyroclastics.||||||20-OCT-04
32392|Mitta Mitta Rhyolite|60506|5|Briefly described|Map legend|Ludlow|Ludlow|Rhyolite lava; pale grey, massive to autobrecciated, with minor intercalated reworked rhyolitic pyroclastics.||||||20-OCT-04
32392|Mitta Mitta Rhyolite|60507|5|Briefly described|Map Legend|Ludlow|Ludlow|Rhyolite lava; pale grey, massive to autobrecciated, with minor intercalated reworked rhyolitic pyroclastics.||||||20-OCT-04
32392|Mitta Mitta Rhyolite|60508|5|Briefly described|Map legend|Late Silurian|Late Silurian|Rhyolite lava: discontinuous nonmagnetic and highly (100-150 nT) magnetic north-northwest trends; low Th, U, bands of high K with low K unit in the east.||||||
32392|Mitta Mitta Rhyolite|61163|6|Mentioned|p9|||Geological Province: Lachlan Fold Belt.||||||
32392|Mitta Mitta Rhyolite|68116|5|Briefly described|Appendix, Map 27.|Pridoli|Ludlow||||||Rhyolite lava: pale grey, massive to autobrecciated; minor intercalated, reworked rhyolitic pyroclastics.|
32392|Mitta Mitta Rhyolite|71040|6|Mentioned|p9, p10 Fig.6|||Wombat Creek Graben, NE Victoria. Associated with Bindian (= Bowning) Orogeny.||||||
83444|Moah pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G651.|||||Magnetic response to 150 nT but with nonmagnetic core; gravity response about 10 micrometres/second/second.|
83444|Moah pluton|73505|5|Briefly described|p18, p20|||Newly named unit in Swan Hill and parts of Balranald and Deniliquin 1:250 000 map areas, (G651). Named after Moah Parish. Subcircular intrusion of about 6 km in diameter and about 5 km northeast of Sea Lake. Magnetic response to 150 nT but with nonmagnetic core. Gravity response of about 10 micrometres/second/second.|||||Granite.|
11999|Mocamboro Member|24551|6|Mentioned|p247|||At Killara Bluff in the Casterton area. Name proposed to be abandoned by Duddy (1983). Equivalent to Eumeralla Formation.||||||12-JAN-10
11999|Mocamboro Member|30905|4|Described|p148|||||||||
11999|Mocamboro Member|31920|5|Briefly described|p49|||Merino Gp.||||||
11999|Mocamboro Member|34148|6|Mentioned|p272|||||||||
11999|Mocamboro Member|41642|5|Briefly described|Table 7.2|||||||||
11999|Mocamboro Member|42318|6|Mentioned|Fig.5 P12|||||||||
11999|Mocamboro Member|42827|5|Briefly described|Table 7.2|||see also Table 7.3||||||
83671|Moe A Seam|73488|6|Mentioned|p632 Fig.2|Langhian|Burdigalian|Gippsland Basin. Shown as laterally equivalent to Yallourn Seam.||Of Yarragon Formation?||||
83672|Moe B Seam|73488|6|Mentioned|p632 Fig.2|Burdigalian|Burdigalian|Gippsland Basin. Shown as laterally equivalent (in part) to the uppermost Morwell Formation coal seam - M1A (Morwell 1A seam)||Of Yarragon Formation?||||
68592|Moitun Creek laterite|24551|6|Mentioned|p330|||||||||
30348|Mole Hill Syenite|60503|4|Described|p181, p41 Tb. 2|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Medium-to coarse-grained, pale grey to pale orange depending on amount of K-feldspar; feldspars interlock with small clots of mafic minerals.  Intrudes the Teapot Creek Formation. See also p135. ||||||
30348|Mole Hill Syenite|60504|5|Briefly described|Map Legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Hornblende-biotite-pyroxene syenite: A-type; grey to pale orange, medium to coarse grained, equigranular.||||||
30348|Mole Hill Syenite|60505|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Hornblende-biotite-pyroxene syenite: A-type; grey to pale orange, medium to coarse grained, equigranular.||||||
30348|Mole Hill Syenite|60506|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Hornblende-biotite-pyroxene syenite: A-type; grey to pale orange, medium to coarse grained, equigranular.||||||
30348|Mole Hill Syenite|60507|5|Briefly described|Map Legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Hornblende-biotite-pyroxene syenite: A-type; grey to pale orange, medium to coarse grained, equigranular.||||||
30348|Mole Hill Syenite|60508|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Syenite: A-type; intensely magnetic (0-750 nT); high total count, K, Th, U||||||
30348|Mole Hill Syenite|68116|5|Briefly described|Appendix, Map 27.|Triassic|Triassic||||||Hornblende-biotite-pyroxene syenite: grey to pale orange, medium to coarse grained, equigranular.|
36976|Moliagul Granodiorite|23309|5|Briefly described|p342, 437|Early Devonian|Early Devonian|G350, I-type.  Age: 390+/-20Ma F-T sphene, Gleadow & Lovering (1978), 387+/-5Ma, 391+/-5Ma, K/Ar biotite cooling age, Richards and Singleton (1981).||||||04-JUN-21
36976|Moliagul Granodiorite|23603|4|Described|p21|Early Devonian|Early Devonian|||||||
36976|Moliagul Granodiorite|23604|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
36976|Moliagul Granodiorite|23605|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
36976|Moliagul Granodiorite|23606|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
36976|Moliagul Granodiorite|23607|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Granodiorite: slightly porphyritic, felsic, minor biotite, molybdenite-bearing quartz veining.||||||12-NOV-04
36976|Moliagul Granodiorite|24178|5|Briefly described|p69|||An extension of the Tarnagulla intrusion||||||
36976|Moliagul Granodiorite|24551|6|Mentioned|p448|Early Devonian|Early Devonian|Includes molybdenite. See also [misspelt] Moliagal pluton p723.||||||03-FEB-15
36976|Moliagul Granodiorite|65715|5|Briefly described|p8 Tb.4|||Superseded name for Moliagul Granite. Used by Marlow and Bushell (1995).||||||03-FEB-15
36976|Moliagul Granodiorite|67804|5|Briefly described|p67|Early Devonian|Early Devonian|Contact metamorphoses auriferous quartz veins at Mooliagul.|~400 Ma (old K/Ar biotite and Rb/Sr data).|||||
36976|Moliagul Granodiorite|68116|5|Briefly described|Appendix, Map 23.|Early Devonian|Early Devonian||||||Granodiorite: slightly porphyritic, felsic, minor biotite, molybdenite-bearing quartz veins.|
36976|Moliagul Granodiorite|68189|6|Mentioned|p42 App.2|||Ages from Richards & Singleton (K-Ar, 1981) and Gleadow & Lovering (F-T, 1978) respectively.|391 +/- 5 to 276 +/- 13 Ma.||||Granodiorite, granite.|30-JUN-14
36976|Moliagul Granodiorite|73576|5|Briefly described|p802-805, p810-811, p814-815, p819, p821|Early Devonian|Early Devonian|Lachlan Fold Belt, Bendigo Zone. I-type intrusion. Exposed in a hill at Mount Moliagul. Hosts primary mineralisation. Associated with a strong magnetic anomaly. May be a late magmatic phase of the Tarnagulla intrusion.|399.95+/-0.27 Ma CA-ID-TIMS U-Pb zircon|||Hosted by Castlemaine Group|Medium- to coarse-grained, equigranular granodiorite.|
12040|Molineaux Sand|22857|5|Briefly described|p354|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
12040|Molineaux Sand|23089|6|Mentioned|p649|||||||||
12040|Molineaux Sand|23560|5|Briefly described|p150|||Referred to as Lowan Sand in Vic.||||||
12040|Molineaux Sand|23818|5|Briefly described|p212 Fig.108|Recent|Recent|Geological Province: Murray Basin and Otway Basin. Yellow in colour.||||||27-OCT-08
12040|Molineaux Sand|29697|5|Briefly described|Table 3|||||||||
12040|Molineaux Sand|29829|6|Mentioned|p178|||||||||
12040|Molineaux Sand|30750|6|Mentioned|p4|||||||||
12040|Molineaux Sand|30751|6|Mentioned|Map legend|Recent|Recent|||||||
12040|Molineaux Sand|30752|6|Mentioned|p2|||||||||
12040|Molineaux Sand|30754|2|Defined|Appendix 1|Recent|Recent|Section on p28.||||||27-OCT-08
12040|Molineaux Sand|30755|6|Mentioned|p169|||Tectonic map||||||
12040|Molineaux Sand|30758|6|Mentioned|p66|||Aeolian. Source of fine aggregate P67||||||01-JUL-13
12040|Molineaux Sand|30807|6|Mentioned|p101|||Suggested map symbol||||||
12040|Molineaux Sand|30996|6|Mentioned|p48|||Time equivalent of Coonambidgal Formation.||||||27-OCT-08
12040|Molineaux Sand|31241|6|Mentioned|p97|||Geological map||||||
12040|Molineaux Sand|31625|6|Mentioned|Fig. 5.2|||Pleistocene||||||
12040|Molineaux Sand|32323|6|Mentioned|p9|||Recent, aeolian.||||||
12040|Molineaux Sand|32432|6|Mentioned|Fig.2|||See also Table 1||||||
12040|Molineaux Sand|32433|6|Mentioned|p80|||See also Table 2||||||
12040|Molineaux Sand|32438|6|Mentioned|p42|||||||||
12040|Molineaux Sand|32439|6|Mentioned|p99|||||||||
12040|Molineaux Sand|33767|6|Mentioned|Fig.5|||||||||
12040|Molineaux Sand|34180|6|Mentioned|p212|||Recent. See also p217.||||||27-OCT-08
12040|Molineaux Sand|34191|6|Mentioned|Map legend|Pleistocene|Pleistocene|Pleistocene - Recent||||||
12040|Molineaux Sand|34536|6|Mentioned|Map legend|Recent|Recent|||||||
12040|Molineaux Sand|35071|6|Mentioned|Table 1|||||||||
12040|Molineaux Sand|35097|6|Mentioned|Fig.4|||||||||
12040|Molineaux Sand|35272|6|Mentioned|p285|||||||||
12040|Molineaux Sand|35772|6|Mentioned|p14|||||||||
12040|Molineaux Sand|36621|6|Mentioned|Fig.1|||||||||
12040|Molineaux Sand|36623|6|Mentioned|Fig.1|||||||||
12040|Molineaux Sand|38068|6|Mentioned|Fig.8|||||||||
12040|Molineaux Sand|40003|5|Briefly described|Table 10|||See also Table 11||||||
12040|Molineaux Sand|40230|6|Mentioned|p6|||||||||
12040|Molineaux Sand|41848|6|Mentioned|p360|||Part equivalent to Lowan Sand||||||
12040|Molineaux Sand|42125|6|Mentioned|p139|||||||||
12040|Molineaux Sand|42129|6|Mentioned|Table 1 P253|||||||||
12040|Molineaux Sand|42499|6|Mentioned|Map legend|||||||||
12040|Molineaux Sand|42717|5|Briefly described|map legend|Holocene||||||||
12040|Molineaux Sand|42966|1|Redefined|p270|Holocene|Late Pleistocene|||||||
12040|Molineaux Sand|43073|4|Described|p18,Table 4|||||||||
12040|Molineaux Sand|43195|5|Briefly described|Map Legend|Holocene|Late Pleistocene|see also commentary on back of map.||||||
12040|Molineaux Sand|44133|5|Briefly described|p220 Fig. 11.2, 253|Holocene|Middle Pleistocene|Equivalent to the Lowan Sand. Geological Province: Murray Basin. ||||||
12040|Molineaux Sand|44660|14|Not recorded|map legend|||Recent.||||||
12040|Molineaux Sand|49038|4|Described|Table 2|||Briefly described p32.||||||27-OCT-08
12040|Molineaux Sand|50154|6|Mentioned|p140|||Equivalent to the Lowan Sand||||||
12040|Molineaux Sand|61964|6|Mentioned|p170|||Noted by Brown and Stephenson (1991a) that this unit in SA and the Lowan Sand of Victoria are essentially the same unit. ||||||
12040|Molineaux Sand|63124|6|Mentioned|p93|||Geological Province: Gambier Basin.||||||
12040|Molineaux Sand|65715|6|Mentioned|p25 Fig.1a|||Map symbol implies Quarternary age.||||||
12040|Molineaux Sand|68116|5|Briefly described|Appendix and many maps (see Comments). |Holocene|Pleistocene|Maps  3-4, 6-7, 9-11, 14-15, 21-22, 29-30, 38-39, 47-48.|||||Aeolian dune sand, fine to medium grained; quartz-rich and clay-poor.|
12040|Molineaux Sand|70334|6|Mentioned|p69|||Of Murray Basin.||||||
12040|Molineaux Sand|71129|6|Mentioned|p155|Pleistocene|Pleistocene|Of Murray Basin. Equivalent to Pleistocene aeolian sand sheets in SIX MILE HILL.||||||
12040|Molineaux Sand|71593|5|Briefly described|p56|||Formed from wind-blown Loxton Sand sediment.|||||Windblown sand dune fields.|
12040|Molineaux Sand|73112|5|Briefly described|Map legend.|Holocene|Holocene|Age given is Recent.|||||Off-white, pale yellow-brown or orange sand of the inland dune spread.|
12040|Molineaux Sand|73228|6|Mentioned|p53|||Fluvio-aeolian depositional environment. Identified in Nadda 1 drillhole.||||Underlain by Loxton Sand.|Red to white, fine to coarse sands.|
37761|Mollys Plain Granite|23309|6|Mentioned|p437, Appendix 1|||G514, I-Type.||||||
37761|Mollys Plain Granite|43312|5|Briefly described|Map Legend|Wenlock|Wenlock|G514. Felsic biotite granite, medium grained, with graphic intergrowth of quartz and perthitic K-Feldspar, I-Type.||||||
37761|Mollys Plain Granite|44185|5|Briefly described|Map legend.|Middle Devonian|Middle Devonian|I-type.||||||
37761|Mollys Plain Granite|60542|4|Described|p96, p19 Fig. 3|Late Silurian|Late Silurian|Medium-grained and greenish grey. No truly fresh specimen has been found. Consists of a graphic intergrowth quartz and perthitic feldspar, so finely intergrown that it is impossible to estimate mineral averages. ||||||
37761|Mollys Plain Granite|68116|5|Briefly described|Appendix, Map 45.|Middle Devonian|Middle Devonian||||||Felsic biotite granite: medium-grained, with graphic intergrowth of quartz and perthitic K-feldspar; I-type.|
35117|Molyullah Ignimbrite|22971|5|Briefly described|p18, p24|Middle Devonian|Middle Devonian|Thickness in outcrop: 200m. (probaly was much thicker).||||||19-JAN-06
35117|Molyullah Ignimbrite|23309|5|Briefly described|p169. Tb 2.63/2.64|||||||||
35117|Molyullah Ignimbrite|24551|5|Briefly described|p167|||Maximum Thickness: 200m||||||
76938|Monbulk Volcanic Group|66244|5|Briefly described|p6, p7.|Miocene|Miocene|New name. Includes the mafic lavas between Cranbourne and Seville. Part of the Melbourne Province of Wellman (1974) and Melbourne Subprovince of Price et al. (2003). Has similar age to the nearby Greensborough Basalt; the two units may be the same.|22 Ma (McKenzie et al. 1984).||||Tholeiite, alkali olivine basalt and basanite.|
76938|Monbulk Volcanic Group|68116|5|Briefly described|Appendix, Maps 42, 51.|Miocene|Miocene||||||Basaltic lava flows: basanite, olivine tholeiite, hawaiite.|
27199|Monegeetta Shale|22886|5|Briefly described|p9|Cambrian|Cambrian|Now know as Knowsley East Formation.||||||
27199|Monegeetta Shale|22971|5|Briefly described|p 20||Middle Cambrian|||||||
27199|Monegeetta Shale|23229|4|Described|Table3-1p16, 17|Middle Cambrian|Middle Cambrian|||||||
27199|Monegeetta Shale|24177|5|Briefly described|p39 Fig.15, p43|Middle Cambrian|Middle Cambrian|Equivalent to Knowsley East Shale.||||||11-MAY-04
27199|Monegeetta Shale|24551|5|Briefly described|p85|||Superseded by Knowsley East Shale.||||||
27199|Monegeetta Shale|40761|5|Briefly described|Table 1|||||||||
27199|Monegeetta Shale|41570|6|Mentioned|p81|||||||||
27199|Monegeetta Shale|41571|4|Described|p46|||||||||
27199|Monegeetta Shale|42628|5|Briefly described|Map legend|Middle Cambrian||||||||
27199|Monegeetta Shale|42790|5|Briefly described|Fig.14 P189|||||||||
27199|Monegeetta Shale|42826|2|Defined|p22||Middle Cambrian|||||||
27199|Monegeetta Shale|42827|4|Described|p46|||||||||
27199|Monegeetta Shale|73059|5|Briefly described|p1060-1061, 1064|Middle Cambrian|Middle Cambrian|Eastern margin of the Bendigo Zone, Lachlan Fold Belt, central Victoria. Detrital zircon age plots; 550-500 Ma age of arc. Now included in the Knowsley East Formation (Crawford et al., 2003).|||||Hemipelagic deposits.|
25253|Monkey Creek Formation|34842|2|Defined|p47|late Tertiary|middle Tertiary|Middle to Late Tertiary||||||
25253|Monkey Creek Formation|42649|5|Briefly described|Fig.3 P197-198|||||||||
25253|Monkey Creek Formation|42827|5|Briefly described|p337|||||||||
25253|Monkey Creek Formation|61336|5|Briefly described|p(ix) Fig. 9|Pliocene|Pliocene|Geological Province: Gippsland Basin.||||||07-FEB-11
74888|Monkey Gully Sandstone Member|64010|5|Briefly described|p258 Fig.1. |||||Of the Kevington Creek Formation.||||
74888|Monkey Gully Sandstone Member|64536|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Of Kevington Creek Formation (Delatite Group). Sandstone, pebbly sandstone, minor mudstone: lithic sandstone and pebble litharenite thick bedded. Forms prominent outcrops and strike ridges. Contains plants/fish fossils. Fluvial deposits.||||||07-FEB-11
74888|Monkey Gully Sandstone Member|64537|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Of Kevington Creek Formation (Delatite Group). Sandstone, pebbly sandstone, minor mudstone: lithic sandstone and pebble litharenite thick bedded. Forms prominent outcrops and strike ridges. Contains plants/fish fossils. Fluvial deposits.||||||07-FEB-11
74888|Monkey Gully Sandstone Member|64538|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Of Kevington Creek Formation (Delatite Group). Sandstone, pebbly sandstone, minor mudstone: lithic sandstone and pebble litharenite thick bedded. Forms prominent outcrops and strike ridges. Contains plants/fish fossils. Fluvial deposits.||||||07-FEB-11
74888|Monkey Gully Sandstone Member|64606|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of Kevington Creek Formation. Sandstone, pebbly sandstone, minor mudstone: alluvial deposits. Red-pink to yellow-green in RGB. Nonmagnetic.||||||11-NOV-08
74888|Monkey Gully Sandstone Member|64616|4|Described|p135, p279, p301|Givetian|Givetian|New. Sandstone unit at top of Kevington Creek Formation in the Blue Range, N of Delatite River. Thickness ~300m. Dominantly interbedded sublitharenite, pebbly litharenite and quartz-arenite, thickly bedded; minor mudstone. Contains plant and fish fossils. Is unconformably overlain by Highton Volcanics. Geophysical characteristics given.||||||
12109|Monoman Formation|23818|5|Briefly described|p212 Fig.108|Recent|Recent|Geological Province: Murray Basin.||||||
12109|Monoman Formation|30750|6|Mentioned|p3|||||||||
12109|Monoman Formation|30751|6|Mentioned|Map legend|Recent|Recent|||||||
12109|Monoman Formation|30753|4|Described|p14|||Recent age||||||
12109|Monoman Formation|30754|2|Defined|Appendix 1|Recent|Recent|||||||
12109|Monoman Formation|30996|3|Fully described|p45|||Refers Firman (1971). L. Holocene - Uppermost Pleistocene.||||||
12109|Monoman Formation|32007|4|Described|p161|||Late Pleistocene. Fossils discussed||||||
12109|Monoman Formation|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
12109|Monoman Formation|34180|6|Mentioned|p212|||Recent||||||
12109|Monoman Formation|34758|6|Mentioned|p27|||||||||
12109|Monoman Formation|35071|6|Mentioned|Fig.4|||||||||
12109|Monoman Formation|35097|6|Mentioned|Fig.4|||||||||
12109|Monoman Formation|35174|6|Mentioned|p167|||||||||
12109|Monoman Formation|35200|6|Mentioned|Map legend|Holocene|Holocene|||||||
12109|Monoman Formation|35232|6|Mentioned|Table.4|||||||||
12109|Monoman Formation|35272|6|Mentioned|p280|||||||||
12109|Monoman Formation|38383|6|Mentioned|Table 1|||||||||
12109|Monoman Formation|41848|5|Briefly described|p356|||Old subdivision at base of Coonambidgal Formation, not used in this book||||||07-APR-17
12109|Monoman Formation|42128|5|Briefly described|p227|||See also Fig.2||||||
12109|Monoman Formation|42264|4|Described|p9|||See also Fig.3||||||
12109|Monoman Formation|42827|5|Briefly described|p356|||||||||
12109|Monoman Formation|42966|1|Redefined|Table 39 p278|Holocene|Late Pleistocene|||||||
12109|Monoman Formation|43655|5|Briefly described|p40-846|||||||||
12109|Monoman Formation|44133|6|Mentioned|p254 Fig. 11.28|Holocene|Holocene|||||||
12109|Monoman Formation|61155|5|Briefly described|p18|Pleistocene|Pleistocene|Geological Province: Murray Basin.||||||
12109|Monoman Formation|68716|6|Mentioned|p39 Fig.3, p40, p41|||A source of lateral flow, saline groundwater discharges to the Murray River.||||Overlain by the Coonambidgal Formation. Underlain by the Bookpurnong Formation.||07-APR-17
12109|Monoman Formation|73188|6|Mentioned|p320|Holocene|Holocene|Murray Basin.|||||Sand, clay, gravel, loam.|
26039|Montys Hut Formation|22882|5|Briefly described|p 11|Devonian|Devonian|||||||
26039|Montys Hut Formation|22885|5|Briefly described|map|Early Devonian|Early Devonian|Walhalla Group.||||||22-DEC-08
26039|Montys Hut Formation|22886|4|Described|p14|Middle Devonian|Middle Devonian|Of Walhalla Group.||||||27-OCT-08
26039|Montys Hut Formation|23229|4|Described|Table3-3p27, 35|Zlichovian||||||||
26039|Montys Hut Formation|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Walhalla Group.||||||22-DEC-08
26039|Montys Hut Formation|23309|5|Briefly described|p146, 164, 270-271. Tb 2.55|||||||||
26039|Montys Hut Formation|24177|3|Fully described|p60, p50 Fig.22|Middle Devonian|Middle Devonian|Of the Walhalla Group. Overlies the Norton Gully Sandstone. Overlain by Cathedral Group in the Cerberean Caldera area; not exposed at BENDIGO. Metamorphosed by the Strathbogie Granite. Geological Province: Mount Easton Province. Maximum Thickness: >1000m.||||||27-OCT-08
26039|Montys Hut Formation|24328|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Walhalla Group.||||||15-JAN-07
26039|Montys Hut Formation|24329|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Walhalla Group.||||||15-JAN-07
26039|Montys Hut Formation|24588|5|Briefly described|p12 Fig.3|Eifelian|Emsian|Geological Province: Mount Easton Province. Of the Walhalla Group.||||||29-NOV-13
26039|Montys Hut Formation|33601|2|Defined|p32|Middle Devonian|Middle Devonian|||||||
26039|Montys Hut Formation|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
26039|Montys Hut Formation|35073|6|Mentioned|p7|||See also Table 1.||||||
26039|Montys Hut Formation|35283|5|Briefly described|p57|||||||||
26039|Montys Hut Formation|38787|6|Mentioned|Fig.2|||||||||
26039|Montys Hut Formation|39551|6|Mentioned|Map legend|Zlichovian|Zlichovian|||||||
26039|Montys Hut Formation|39555|6|Mentioned|Map legend|Zlichovian|Zlichovian|||||||
26039|Montys Hut Formation|41585|4|Described|p115|||||||||
26039|Montys Hut Formation|42383|6|Mentioned|p5|||Used 1983, Superseded by Walhalla Group?||||||
26039|Montys Hut Formation|42827|5|Briefly described|p115|||Of the Walhalla Group.||||||15-JAN-07
26039|Montys Hut Formation|44187|5|Briefly described|Map Legend||Early Devonian|||||||
26039|Montys Hut Formation|44197|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
26039|Montys Hut Formation|60529|5|Briefly described|Map Legend|Givetian|Eifelian|Of the Walhalla Group. Shelf Deposit: hemipelagic siltstone; brown, laminated to thickly bedded, parallel and ripple drift cross laminations, cross beds with overturned foresets.||||||27-OCT-04
26039|Montys Hut Formation|60599|5|Briefly described|p14|Middle Devonian|Early Devonian|Of Walhalla Group. Geological Province: Melbourne Zone, Lachlan Fold Belt. ||||||
26039|Montys Hut Formation|61185|2|Defined|p45-47, p21Fig.6, p43, p14, p49, p24-25|Middle Devonian|Middle Devonian|Of Walhalla Gp. Incl: former Roberts and Coulson Sst mbrs and Freeman mbr. Over Norton Gully Sst; under Cathedral Gp. Thick: >1000m. Siltstone, sandstone, shales. Low-grade contact metamorphosed aureole of Strathbogie Granite.||||||07-FEB-11
26039|Montys Hut Formation|61701|5|Briefly described|Map Legend|Givetian|Eifelian|Of the Walhalla Group. Shelf Deposit: hemipelagic siltstone; brown, laminated to thickly bedded, parallel and ripple drift cross laminations, cross beds with overturned foresets.||||||10-JUN-14
26039|Montys Hut Formation|61702|5|Briefly described|Map Legend|Givetian|Eifelian|Of the Walhalla Group. Shelf Deposit: hemipelagic siltstone; brown, laminated to thickly bedded, parallel and ripple drift cross laminations, cross beds with overturned foresets.||||||10-JUN-14
26039|Montys Hut Formation|61703|5|Briefly described|Map Legend|Givetian|Eifelian|Of the Walhalla Group. Shelf Deposit: hemipelagic siltstone; brown, laminated to thickly bedded, parallel and ripple drift cross laminations, cross beds with overturned foresets.||||||15-JAN-07
26039|Montys Hut Formation|61704|6|Mentioned|Map legend|Devonian|Devonian|Masked by high K and Th from granite colluvium.||||||
26039|Montys Hut Formation|64535|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Dk.green-grey-black siltstone, thinly bedded, shaly, occasional flat burrows; pale grey sandstone, thin to minor medium-, rarely thick-bedded; very fine to med.-gr., well sorted, quartz-rich;deep-marine hemipelagic + turbidite deposits.||||||22-DEC-08
26039|Montys Hut Formation|64536|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Contains Goughs Bay Sandstone Member. Siltstone and sandstone - more lithological detail included. Deep-marine hemipelagic + turbidite deposits.||||||07-FEB-11
26039|Montys Hut Formation|64537|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Contains Goughs Bay Sandstone Member. Siltstone and sandstone - more lithological detail included. Deep-marine hemipelagic + turbidite deposits||||||07-FEB-11
26039|Montys Hut Formation|64538|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Contains Goughs Bay Sandstone Member. Siltstone and sandstone - more lithological detail included. Deep-marine hemipelagic + turbidite deposits||||||07-FEB-11
26039|Montys Hut Formation|64539|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Dk.green-grey-black siltstone, thinly bedded, shaly, occasional flat burrows; pale grey sandstone, thin to minor medium-, rarely thick-bedded; very fine to med.-gr., well sorted, quartz-rich;deep-marine hemipelagic + turbidite deposits.||||||22-DEC-08
26039|Montys Hut Formation|64540|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Dk.green-grey-black siltstone, thinly bedded, shaly, occasional flat burrows; pale grey sandstone, thin to minor medium-, rarely thick-bedded; very fine to med.-gr., well sorted, quartz-rich;deep-marine hemipelagic + turbidite deposits.||||||22-DEC-08
26039|Montys Hut Formation|64605|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Siltstone, sandstone; deep-marine deposits. Yellow, brown-pink to white-pink-blue in RGB, with variation probably due to weathering. Nonmagnetic.||||||
26039|Montys Hut Formation|64606|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of Walhalla Group. Includes Goughs Bay Sandstone Member. Siltstone, sandstone: deep-marine deposits. Yellow, brown-pink to white-pink-blue in RGB, with variation probably due to weathering. Nonmagnetic.||||||
26039|Montys Hut Formation|64616|3|Fully described|p117, p151-152, p155 Fig.6.4, p157|Emsian|Emsian|See also p159, p164 Fig.6.10, p167, p169-173, p175, p177 Fig.6.25, p183 Fig.6.29, p189 Fig.6.32, p197 Fig.6.34, p201 Tb.7.1, p205, p208 Fig.8.1, p215, p230, p233-235, p237 Fig.8.20, p239 Fig.8.23, p242, p279-280, p290-292, p295, p302, p434-435. Of Walhalla Group. Conformable on Norton Gully Sandstone and probably conformably overlain by Cathedral Group outside project area. Includes Goughs Bay Sandstone Member. Thickness uncertain but 700+ m. Age inferred from strat. position. Radiometric ages from 372 +/- 2 Ma to 396 +/- 4 Ma. Mainly thinly interbedded siltstone and minor fine sandstone. Hosts gold-mineralised veins in the Cohens Fault Zone, and the Royal Standard workings. Deformation age discussed. Geophysical characteristics given.||||||
26039|Montys Hut Formation|66576|5|Briefly described|p972.|Devonian|Devonian|||Unit in Walhalla Group.||Overlies Norton Gully Sandstone.|Thinly bedded siltstone with thin interbedded fine-grained sandstone units.|
26039|Montys Hut Formation|67847|6|Mentioned|p44 fig 3.2.2.|Early Devonian|Early Devonian|||Walhalla Group||||
26039|Montys Hut Formation|68116|5|Briefly described|Appendix, Maps 25, 33-34, 42-43, 52.|Emsian|Emsian||||||Mainly siltstone, sometimes interbedded with sandstone; thin-bedded, planar and laterally continuous beds. Siltstone: dark green-grey to black. Sandstone: pale grey, thin- to minor medium-bedded, fine to medium-grained, well sorted, quartz-rich.|
26039|Montys Hut Formation|69089|5|Briefly described|Map legend|Early Devonian|Early Devonian|||Unit in Walhalla Group.|||Marine: thin-bedded sandstone, siltstone.|
26039|Montys Hut Formation|70742|5|Briefly described|p161-163, p165, p168-169, p171, p175|Emsian|Emsian|Contains a distinctive low-diversity fossil assemblage, dominated by two species of chonetoid brachiopods including Taungurungetes taggertyensis. Thickness estimates range from 1000m to possibly more than 2000m. Deformed during the Tabberabberan Orogeny c.390 Ma. Systematic palaeontology.||Topmost Walhalla Group.||Overlies Norton Gully Sandstone conformably.||
26039|Montys Hut Formation|73497|5|Briefly described|Map legend|Devonian|Devonian|Marine.||Walhalla Group|||Siltstone, minor sandstone: generally weak magnetic responses, but some moderate magnetic responses (15-20 nT); radiometric response masked by high K and Th from granite colluvium.|
22372|Moomowroong Sand|12796|5|Briefly described|p460|||Consists of fine-grained micaceous sands and minor grey clays.  Overlies Wiridjil Gravels. Interpreted as a marginal facies equivalent of Massacre Shale. ||||||
22372|Moomowroong Sand|22875|5|Briefly described|p14|Paleocene|Paleocene|Wangerrip Group||||||
22372|Moomowroong Sand|23322|5|Briefly described|957 Fig.2|Paleocene|Paleocene|Of the Wangerrip Group.  Geological Province: Otway Basin.||||||07-SEP-09
22372|Moomowroong Sand|24551|5|Briefly described|p292, 467|Paleocene|Paleocene|Together with Wiridjil Gravel, lateral equivalents of Pebble Point Formation. Overlies Wiridjil Gravel. Geological province: Otway Basin.||||||30-JAN-07
22372|Moomowroong Sand|43590|4|Described|p16||Paleocene|||||||
22372|Moomowroong Sand|43937|5|Briefly described|Map Legend|Paleocene|Santonian|||||||
22372|Moomowroong Sand|61182|3|Fully described|p19, p21, p169|||Of Wangerrip Gp. Marginal marine, grading out of Pebble Point Fm.and into Wiridjil Gravel (non-marine). Thick: ~45m. In Otway Basin. Grades laterally into Pebble Point Fm; also, grades laterally into, and locally disconformably overlies, Wiridjil Gravel. ||||||
22372|Moomowroong Sand|65715|5|Briefly described|p11 Tb.7|Paleogene|Paleogene|Of Wangerrip Group. Formation rank.||||||
22372|Moomowroong Sand|66002|4|Described|p10 Tb.7, p10 Tb.8, p11-12, p60-68|Paleogene|Paleogene|Of Wangerrip Group. Poor exposure. Well sorted sand, often with no obvious bedding. Interfingers with Wiridjil Gravel. Overlies Otway Group rocks. Marginal marine facies. Outcrops indistinguishable from Dilwyn Formation. Defined by Tickell et al 1992.||||||
22372|Moomowroong Sand|68116|5|Briefly described|Appendix, Maps 49, 54.|Paleocene|Late Cretaceous||||||Quartz sand, minor clay: micaceous, fine-grained, friable, generally massive; minor planar cross-bedding; minor gravel; marginal marine and beach deposits.|
78486|Moonfish Volcanics|66181|6|Mentioned|p310 Fig.5|||Lithological identifier not used in figure, only in caption; an episode of volcanism in Gippsland Basin, presented as Moonfish.||||||
34884|Moonip Sandstone Member|22968|4|Described|P122, P124|Late Silurian|Late Silurian|New name, Intercalated within the Berrawan Conglomerate||||||
34884|Moonip Sandstone Member|23021|5|Briefly described|Map legend|Ludlow|Ludlow|Parent is Berrawan Conglomerate||||||
34884|Moonip Sandstone Member|23030|5|Briefly described|Map legend|Late Silurian|Late Silurian|Parent is the Berrawan Conglomerate||||||
34884|Moonip Sandstone Member|23309|5|Briefly described|p103, 129. Tb 2.37|||Parent: Mount Tambo Group.||||||
34884|Moonip Sandstone Member|24551|4|Described|p138, p140|||Of Berrawan Conglomerate.||||||
34884|Moonip Sandstone Member|60503|5|Briefly described|p129, p130|Early Devonian|Early Devonian|Of the Berrawan Conglomerate (Mount Tambo Group). Occurs at the top of Mount Tambo. Contains planar laminated sandstones and mudstones which contain a few fossils including plant remains.||||||
34884|Moonip Sandstone Member|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Berrawan Conglomerate (Mount Tambo Group). Fluvial sediments: sandstone, greywacke, mudstone||||||20-OCT-04
34884|Moonip Sandstone Member|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Berrawan Conglomerate (Mount Tambo Group). Fluvial sediments: sandstone, greywacke, mudstone||||||21-OCT-04
34884|Moonip Sandstone Member|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Berrawan Conglomerate, Mount Tambo Group. Fluvial sediments: sandstone, greywacke, mudstone||||||20-OCT-04
34884|Moonip Sandstone Member|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Berrawan Conglomerate, Mount Tambo Group. Fluvial sediments: sandstone, greywacke, mudstone||||||20-OCT-04
12244|Moonkan Ignimbrite|23309|4|Described|p109, 130-131. Tb 2.40|||Of the Little River Subgroup.  Maximum Thickness: 600m.||||||
12244|Moonkan Ignimbrite|23615|3|Fully described|p115|Early Devonian|Early Devonian|Of Little River Subgroup.  Overlain by Detarka Ignimbrite.  Max. thickness: >600m.  Composed of densely welded red quartz-rich ignimbrite.  Overlies Tulloch Ard Ignimbrite in the north; interfingers with Bally Hooley Ignimbrite and Mount Tabby Formation.||||||
12244|Moonkan Ignimbrite|23938|6|Mentioned|p54-55 Tb. 4|||Of the Snowy River Volcanics. See also p59-65 Figs. 21-24.||||||25-SEP-08
12244|Moonkan Ignimbrite|24551|5|Briefly described|p144|||Of Little River Subgroup.||||||
12244|Moonkan Ignimbrite|41585|6|Mentioned|p135|||||||||
12244|Moonkan Ignimbrite|42827|5|Briefly described|p136|||||||||
12244|Moonkan Ignimbrite|43206|5|Briefly described|map legend||Lochkovian|of Little River Subgroup.||||||
12244|Moonkan Ignimbrite|60542|5|Briefly described|p67|||Currently assigned to the Little River Subgroup but also considered that it should perhaps be included in the Tara Range Subgroup due to its composition suggesting origin to be Waiwera Graben. Red quartz ignimbrite. ||||||
12244|Moonkan Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Quartz ignimbrite: red to purple, with large quartz and small feldspar phenocrysts.|
25259|Moonlight Head beds|38734|6|Mentioned|p10|||||||||
25259|Moonlight Head beds|63124|4|Described|p73|||Lower section of Eumeralla Formation that outcrops on coastline of the Otway Ranges; consists of stacked channel sandstones mainly; contains diverse fauna including turtles, fish and at least 3 species of dinosaurs.  ||||||
30441|Moora Moora Sandstone|44929|5|Briefly described|Map Legend|Silurian|Ordovician|Of Mount Difficult Sub-Group (Grampians Group).  Quartz sandstone, pale, fine- to coarsely-grained, with minor feldspar.||||||14-JUN-06
30441|Moora Moora Sandstone|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Of Mount Difficult Sub-Group (Grampians Group). Quartz sandstone, pale, fine- to coarse-grained with minor feldspar.||||||13-JUN-06
30441|Moora Moora Sandstone|44932|5|Briefly described|Map Legend|Silurian|Ordovician|Of Mount Difficult Sub-Group (Grampians Group).  Quartz sandstone, pale, fine- to coarsely-grained, with minor feldspar.||||||14-JUN-06
30441|Moora Moora Sandstone|44933|5|Briefly described|Map Legend|Silurian|Ordovician|Of Mount Difficult Group. Quartz sandstone, pale, fine- to coarse-grained, with minor feldspar.||||||14-JUN-06
30441|Moora Moora Sandstone|60451|5|Briefly described|p82|Early Devonian|Ordovician|Of the Mount Difficult Subgroup (Grampians Group).||||||
30441|Moora Moora Sandstone|60456|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Mount Difficult Sub-Group.  Quartz sandstone: pale, fine to coarse grained with minor feldspar; planar and cross lamination, thin to medium bedded.||||||
30441|Moora Moora Sandstone|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Mount Difficult Subgroup. Quartz sandstone: pale, fine to coarse grained with minor feldspar, with planar and cross lamination; thin to medium bedded.||||||
30441|Moora Moora Sandstone|61183|4|Described|p48-49|||Of Mount Difficult Subgroup (Grampians Gp). Thin bedded grey to red sandstone with minor interbeds of micaceous mudstone; contains horizons rich in Skolithos and other trace fossils. Conformable under Wartook Sst; overlies Serra Sst. Thick: 500m in south.||||||
30441|Moora Moora Sandstone|64541|5|Briefly described|Map Legend|Silurian|Silurian|Of Mount Difficult Sub-group. Quartz sandstone: pale, fine to coarse-grained with minor feldspar; laminated and cross-laminated, thin to medium bedded; mud rip-up clast, Skolithos horizons and ripple surfaces.||||||02-MAY-13
30441|Moora Moora Sandstone|64610|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Difficult Subgroup (Grampians Gp). Quartz sandstone: pale, fine- to coarse-grained, + minor feldspar; laminated and x-laminated, thin to medium bedded; mud rip-up clasts, Skolithos horizons and ripple surfaces; minor interbeds; poorly outcropping||||||11-NOV-08
30441|Moora Moora Sandstone|65313|6|Mentioned|p583, p581 Fig. 9, p582 Fig. 10|Pragian|Early Devonian|Includes the basal Pragian Prague-Lochov  (?isotopic) Event at 411.2 Ma.  Grampians National Park sections.||Of Mount Difficult Subgroup.||Is overlain by Wartook Sandstone.||26-MAR-12
30441|Moora Moora Sandstone|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Mount Difficult Subgroup.  Defined by Cayley & Taylor, 1997. ||||||
30441|Moora Moora Sandstone|68116|5|Briefly described|Appendix, Maps 22, 30, 39.|Pridoli|Ludlow||||||Quartz sandstone: pale; fine to coarse-grained with minor feldspar; planar and cross-laminated, thin to medium-bedded; mud rip-up clasts; Skolithos horizons and ripple surfaces; poorly outcropping; sparse micaceous mudstone.|
30441|Moora Moora Sandstone|73118|6|Mentioned|p64, 70|Silurian|Silurian|||Grampians Group.||||
37876|Mooral granodiorite|24180|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Informal name.  Granodiorite, medium-grained, equigranular to slightly porphyritic, with plagioclase (albite, andesine and labradorite), orthoclase, quartz and biotite, accessory apatite, ilmenite, sphene and zircon.||||||
30450|Mooralla Ignimbrite|23309|5|Briefly described|p81|||Of the Rocklands Volcanics.||||||
30450|Mooralla Ignimbrite|44929|5|Briefly described|Map Legend||Early Devonian|Of Rocklands Volcanics. Feldspar ignimbrite, pinky-brown to grey with sparse crystals up to 2mm.||||||14-JUN-06
30450|Mooralla Ignimbrite|44930|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Rocklands Volcanics. Feldspar ignimbrite, pinky-brown to grey with sparse crystals up to 2mm.||||||14-JUN-06
30450|Mooralla Ignimbrite|44931|6|Mentioned|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanics.||||||14-JUN-06
30450|Mooralla Ignimbrite|44932|5|Briefly described|Map Legend||Early Devonian|Of Rocklands Volcanics. Feldspar ignimbrite, pinky-brown to grey with sparse crystals up to 2mm.||||||14-JUN-06
30450|Mooralla Ignimbrite|44933|5|Briefly described|Map Legend||Early Devonian|Of Rocklands Volcanics. Feldspar ignimbrite, pinky-brown to grey with sparse crystals up to 2mm.||||||14-JUN-06
30450|Mooralla Ignimbrite|50154|5|Briefly described|p114|||Of the Rocklands Volcanic Group.||||||26-NOV-08
30450|Mooralla Ignimbrite|61183|4|Described|p63|Early Devonian|Early Devonian|Of Rocklands Volcanics Group. Appears to be a single flow unit of very fine-grained, crystal-poor ignimbrite. Younger than the adjacent Gatum Ignimbrite, a clast of which has been identified in this rock. Thickness: >20m.||||||
30450|Mooralla Ignimbrite|64541|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanics. Feldspar ignimbrite.||||||07-FEB-11
30450|Mooralla Ignimbrite|64610|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Rocklands Volcanics.Feldspar ignimbrite: pinky brown with sparse crystals up to 2mm; very rare greenstone lithics up to 10mm; eutaxitic texture with  devitrified pumice and perlitic cracks; strongly attentuated fiamme foliation.||||||
30450|Mooralla Ignimbrite|66002|5|Briefly described|p6 Tb.4|Devonian|Devonian|Of Rocklands Volcanic Group. Defined in Simpson 1997, p63.||||||
37246|Mooree Granodiorite|24012|3|Fully described|p223 appendix 1|Ordovician|Cambrian|||||||
37246|Mooree Granodiorite|50154|2|Defined|p89, p247 App.5|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex.||||||15-SEP-04
37246|Mooree Granodiorite|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Muscovite-biotite granodiorite||||||25-JUN-04
37246|Mooree Granodiorite|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite-biotite granodiorite.||||||21-MAY-13
37246|Mooree Granodiorite|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite-biotite granodiorite.||||||21-MAY-13
37246|Mooree Granodiorite|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite-biotite granodiorite.||||||21-MAY-13
37246|Mooree Granodiorite|50159|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite-biotite granodiorite.||||||21-MAY-13
37246|Mooree Granodiorite|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite-biotite granodiorite.||||||21-MAY-13
37246|Mooree Granodiorite|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite-biotite granodiorite.||||||21-MAY-13
37246|Mooree Granodiorite|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite-biotite granodiorite.||||||21-MAY-13
37246|Mooree Granodiorite|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite-biotite granodiorite.||||||21-MAY-13
37246|Mooree Granodiorite|66002|6|Mentioned|p9 Tb.5|||G442. Defined by Kemp et al. 2002||||||
37246|Mooree Granodiorite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Muscovite-biotite granodiorite: massive to weakly foliated, pale grey-buff, medium grained equigranular to weakly alkali feldspar-phyric; accessory magnetite and epidote; uncommon biotite-rich mafic microgranitoid enclaves; magnetic.|
22379|Moores Ford Andesite|23309|4|Described|p108. Tb 2.40|||Of the Little River Subgroup.||||||
22379|Moores Ford Andesite|23615|3|Fully described|p129|Early Devonian|Early Devonian|Of Little River Subgroup. Maximum thickness:180m. Consists of several different lava flows, predominantly andesitic.||||||25-SEP-08
22379|Moores Ford Andesite|23938|6|Mentioned|p55 Tb. 4|||Overlain by Buchan Caves Limestone?||||||25-SEP-08
22379|Moores Ford Andesite|24551|5|Briefly described|p145|||Of Little River Subgroup.||||||
22379|Moores Ford Andesite|43206|5|Briefly described|map legend||Lochkovian|Of Little River Subgroup.||||||25-SEP-08
22379|Moores Ford Andesite|43312|5|Briefly described|Map Legend||Early Devonian|Of Little River Group.||||||25-SEP-08
22379|Moores Ford Andesite|43313|5|Briefly described|Map Legend||Early Devonian|Of Little River Subgroup.||||||25-SEP-08
22379|Moores Ford Andesite|60542|5|Briefly described|p63|Early Devonian|Early Devonian|Of Little River Subgroup. Lava flows ranging from basalt to andesite and high-Si trachyte. Overlies Raymond Falls Lava; and Jellung Ignimbrite; also overlies Balley Hooley Ignimbrite. Overlain by Buchan Caves Limestone. ||||||
22379|Moores Ford Andesite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Andesite, trachyte and basalt lava flows: massive grey to dark green-black porphyritic andesite lava is most common. Basalt lavas are grey and have olivine, generally show elongate silica-filled amygdales; minor ash and pyroclastic deposits.|
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.||
37578|Moornambool Metamorphic Complex|23309|4|Described|p64-65, p226-231, Table 2.23|Cambrian|Cambrian|||||||
37578|Moornambool Metamorphic Complex|24098|6|Mentioned|p25, p30 Fig. 4|||Structural term in this context? Geological Province: Lachlan Fold Belt.||||||19-APR-05
37578|Moornambool Metamorphic Complex|24221|4|Described|p891|||Geological Province:  Lachlan Fold Belt.||||||17-JAN-07
37578|Moornambool Metamorphic Complex|24311|5|Briefly described|p1058|Cambrian|Cambrian|||||||
37578|Moornambool Metamorphic Complex|24551|5|Briefly described|p82|||||||||
37578|Moornambool Metamorphic Complex|24600|5|Briefly described|p479, p481|||Geological Province: Lachlan Fold Belt.||||||
37578|Moornambool Metamorphic Complex|60451|4|Described|p20, 24, 63, 108, 147, 155|||Upper greenschist (biotite grade) to amphibolite grade. 15km belt of highly strained and metamorphosed rocks. Includes: Saint Arnaud Group and Magdala Volcanics.||||||
37578|Moornambool Metamorphic Complex|60454|5|Briefly described|Map Legend|Early Devonian|Silurian|Includes: Lexington Schist, Good Morning Bill Schist, Deenicull Schist, Rhymney Schist, Carrolls Amphibolite.||||||
37578|Moornambool Metamorphic Complex|60456|5|Briefly described|Map Legend|Early Devonian|Silurian|Includes: Carrolls Amphibolite, Good Morning Bill Schist, Lexington Schist.||||||
37578|Moornambool Metamorphic Complex|60457|5|Briefly described|Map Legend|Early Devonian|Silurian|Includes: Lexington Schist, Good Morning Bill Schist, Deenicull Schist, Rhymney Schist, Carrolls Amphibolite.||||||24-SEP-04
37578|Moornambool Metamorphic Complex|60458|5|Briefly described|Map Legend|Early Devonian|Silurian|Includes: Lexington Schist, Good Morning Bill Schist, Deenicull Schist, Rhymney Schist, Carrolls Amphibolite.||||||
37578|Moornambool Metamorphic Complex|60459|5|Briefly described|Map Legend|Early Devonian|Silurian|Includes: Lexington Schist, Good Morning Bill Schist, Deenicull Schist, Rhymney Schist, Carrolls Amphibolite.||||||
37578|Moornambool Metamorphic Complex|60904|5|Briefly described|p784 Fig. 10|||Of the Lachlan Orogen.||||||
37578|Moornambool Metamorphic Complex|61187|5|Briefly described|p4, p81, p82, p84 Fig.2.|Early Silurian|Early Silurian|Western edge of Stawell Zone. Bounded by Moyston Fault to the west and Coongee Fault to the east. Metamorphic grade increases westwards, from greenschist to amphibolite facies. Generated during Benambran Orogeny.||||||
37578|Moornambool Metamorphic Complex|61726|4|Described|p922 Fig.2a||Early Cambrian|Ages: 505-490Ma and 450-440Ma. Hosts the Stawell Gold Mine. Geological Province: Delamerian Fold Belt/Stawell Zone (part of which is in this fold belt as well as in Lachlan Fold Belt). See also p925-926, p933-934.||||||
37578|Moornambool Metamorphic Complex|61752|4|Described|p5-6, p18-20|Silurian|Silurian|Largest greenstone belt in Victoria. High-grade coarsely schistose rocks. Geological Province: Lachlan Fold Belt.||||||07-FEB-11
37578|Moornambool Metamorphic Complex|62741|5|Briefly described|p678 Fig. 1|Early Cambrian|Early Cambrian|Sediments; polydeformed rocks. See also p683.||||||
37578|Moornambool Metamorphic Complex|62744|5|Briefly described|p708 Fig. 1, p710|||||||||
37578|Moornambool Metamorphic Complex|62747|6|Mentioned|p736|||Hosts the Magdala gold deposit.||||||31-OCT-06
37578|Moornambool Metamorphic Complex|62749|6|Mentioned|p722|Cambrian|Cambrian|||||||
37578|Moornambool Metamorphic Complex|62754|6|Mentioned|p863|||||||||
37578|Moornambool Metamorphic Complex|62755|6|Mentioned|p877|Ordovician|Ordovician|Polydeformed structure in the Stawell area. Age: ca 440Ma. See also p885 Fig.8.||||||
37578|Moornambool Metamorphic Complex|64314|5|Briefly described|p493, p495 Fig. 2a|||Characterised by schist, quartzite and amphibolite. ||||||
37578|Moornambool Metamorphic Complex|64597|6|Mentioned|p761. |||Lower greenschist facies. Hosts the Magdala gold deposit.||||||
37578|Moornambool Metamorphic Complex|65665|6|Mentioned|p1144 Fig.1, p1149, p1160 Fig.14|Cambrian|Cambrian|Sediments. In western Stawell Zone.||||||10-MAY-12
37578|Moornambool Metamorphic Complex|65716|5|Briefly described|p17-24|||From Ararat 1:50k sheet. Includes Good Morning Bill Schist, which is what was dated. Most zirons appear to be detrital. Some evidence of  metamorphic overgrowths at 568.8 +/- 6.2 Ma, and detrital ages grouped around 589.5 +/- 7.7 may record a significant event in the source area.||||||04-OCT-16
37578|Moornambool Metamorphic Complex|66002|5|Briefly described|p5 Tb.2|Cambrian|Cambrian|Includes Carrolls Amphibolite, Deenicull Schist, Good Morning Bill Schist, Lexington Schist and Rhymney Schist||||||
37578|Moornambool Metamorphic Complex|66769|5|Briefly described|115 Fig.1, 122, 128, 140, 143-144 fig 15|Cambrian|Cambrian|Western margin of the Stawell Zone. Highly deformed. Amphibolite facies rocks in hanging-wall of Moyston Fault. Pelitic metasedimentary rocks that predominate over mafic meta-igneous rocks. Tectonic melange implies subduction-accretion process operated in Late Cambrian.||||||
37578|Moornambool Metamorphic Complex|67103|5|Briefly described|p614|||Located immediately E of the Grampians-Stavely Zone, and exhumed in the hangingwall of the Moyston Fault. Tectonically reworked and more highly metamorphosed than the Magdala Volcanics. Metamorphosed at 500 Ma.||||||
37578|Moornambool Metamorphic Complex|67104|6|Mentioned|p635, p645, p632|||Stawell Zone. Amphibolite-grade showing scaly fabrics and tectonic melange.||||||
37578|Moornambool Metamorphic Complex|67847|6|Mentioned|p78|||Stawell Zone, Lachlan Orogen. ||||||
37578|Moornambool Metamorphic Complex|67978|5|Briefly described|p496 Fig.1, p513, p514, p520|||See also Mount Moornambool Metamorphic Complex. Characterised by metamorphic grades decreasing from amphibolite facies conditions in the west to lower greenschist conditions in the east.||||||
37578|Moornambool Metamorphic Complex|68189|6|Mentioned|p3, p15 Fig.6, p17 Fig.7, p29|||||||||
37578|Moornambool Metamorphic Complex|68194|5|Briefly described|p20-21, p31, p75, p77-78, p80|Late Ordovician|Late Ordovician|Cayley and Taylor (2001). Product of Benambran Orogeny. In situ regolith described.||||Is overlain conformably by Saint Arnaud Group.|Faulted packages of polydeformed amphibolite, quartz-mica schist and metapsammite.|
37578|Moornambool Metamorphic Complex|68314|6|Mentioned|p750|||Stawell Zone. Includes an amphibolite-facies western zone and a lower-greenschist facies turbidites eastern zone, on either side of the Coongee Break.||||||
37578|Moornambool Metamorphic Complex|71593|4|Described|p8, p12, p36-p37, p71|||Stawell Zone. Metamorphism is not directly dated but unroofing and cooling of the complex is constrained by Ar/Ar cooling ages of c. 508-390 Ma (Miller et al, 2005; Phillips et al, 2012). Maximum temperatures and pressures of metamorphism are 600 degrees C and between 0.7-0.8 GPa (Radojkovic, 1989; Phillips et al, 2002). See also p73-p74, p102, p133, p168, p174.|||Includes the Carrolls Amphibolite, Lexington Schist and Good Morning Bill Schist.||Metamorphosed, greenschist to amphibolite grade turbidites and volcanic rocks.|
37578|Moornambool Metamorphic Complex|72445|5|Briefly described|App.1, App.2; App.5.|Late Cambrian|Middle Cambrian|More intensely veined and deformed from 209 m in Stavely 01. Shown as part of the target basement. App.2 is a .csv format file.|||Carrolls Amphibolite|Shown as underlying Heytesbury Group with sharp contact.|Includes Foliated and deformed amphibolite (Carrols Amphibolite).|
37578|Moornambool Metamorphic Complex|73059|6|Mentioned|p1061|||Western Stawell Zone. Mis-spelt as Moorambool Metamorpic Complex. Garnet amphibolites with Ar/Ar ages ~500 Ma have been exhumed from a west-dipping Delamerian subduction zone.||||||
37578|Moornambool Metamorphic Complex|73505|6|Mentioned|p6|||||||||
37524|Moornapa Sandstone|61161|5|Briefly described|p83-84, p125, p32, p76-77 Fig 6.1|Silurian|Silurian|Of Cobbannah Group. Underlies Moroka Glen Formation (angular unconformity) and Dandongadale Siltstone. Overlies Bendoc Group (faulted relationship). Interbedded sandstone and mudstone. Thickness 3050 m in STRATFORD (Fergusson 1987a). GSV map code: Scm.||||||
37524|Moornapa Sandstone|61163|6|Mentioned|p27|||Of the Cobbannah Group. Dominated by sandstone. Geological Province: Lachlan Fold Belt.||||||
37524|Moornapa Sandstone|61169|5|Briefly described|map legend|Early Silurian|Early Silurian|Of the Cobbannah Group. Sandstone, minor siltstone: sandstone quartzitic; thick, medium and thin-bedded; interbedded siltstone dark grey; deep-marine turbidite fan deposits. GSV map code: Scm.||||||
37524|Moornapa Sandstone|61170|5|Briefly described|map legend|Early Silurian|Early Silurian|Of the Cobbannah Group. Sandstone, minor siltstone: sandstone quartzitic; thick, medium and thin-bedded; interbedded siltstone dark grey; deep-marine turbidite fan deposits. GSV map code: Scm.||||||07-FEB-11
37524|Moornapa Sandstone|61171|5|Briefly described|map legend|Early Silurian|Early Silurian|Of the Cobbannah Group. Sandstone, minor siltstone: sandstone quartzitic; thick, medium and thin-bedded; interbedded siltstone dark grey; deep-marine turbidite fan deposits. GSV map code: Scm.||||||
37524|Moornapa Sandstone|61172|5|Briefly described|map legend|Early Silurian|Early Silurian|Of the Cobbannah Group. Sandstone, minor siltstone: sandstone quartzitic; thick, medium and thin-bedded; interbedded siltstone dark grey; deep-marine turbidite fan deposits. GSV map code: Scm.||||||
37524|Moornapa Sandstone|61173|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Cobbannah Group. Sandstone, minor siltstone: moderate gravity response; nonmagnetic to weakly magnetic; varying radiometric response over upper slopes, and over slopes and gullies are low to moderate K, Th, U and total radioelements. GSV map code: Scm.||||||
12294|Moorngag Granite|24551|6|Mentioned|p222|||See also Swanpool Granite.  Of the Strathbogie Province.||||||
12294|Moorngag Granite|35111|4|Described|p5|||||||||
12294|Moorngag Granite|42154|6|Mentioned|Table 1 P334|||||||||
12294|Moorngag Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
12294|Moorngag Granite|66244|5|Briefly described|p4.|||A pluton first named on the Winton 1:50 000 geological sheet (O'Shea 1977); has precedence over its naming as Swanpool Granite in the Wangaratta 1:250 000 sheet (VandenBerg 1997).||||||
12294|Moorngag Granite|68116|5|Briefly described|Appendix, Map 26.|Late Devonian|Late Devonian||||||Biotite granite, porphyritic with K-feldspar phenocrysts in a fine to medium grained groundmass of quartz, orthoclase, plagioclase, biotite and rare muscovite.|
26314|Moralana Supergroup|23309|5|Briefly described|p38-40, 45, 46.|Early Cambrian|Early Cambrian|Was "Glenelg River beds".  Ages:  572+/-9Ma, 558+/-6Ma, 556+/-6Ma, 553+/-9Ma, 551+/-6Ma, but noted as " Probably geologically meaningless mixed ages between detrital mica and new growth in the Delamerian".||||||04-MAY-10
26314|Moralana Supergroup|24551|5|Briefly described|p74|||||||||
26314|Moralana Supergroup|24586|5|Briefly described|p51 Fig. 1|Early Cambrian|Early Cambrian|Includes the Hawker Group. Geological Province: Adelaide Geosyncline.||||||05-JUL-06
26314|Moralana Supergroup|38004|2|Defined|p82|Precambrian|Precambrian|||||||
26314|Moralana Supergroup|38703|6|Mentioned|p131|||||||||
26314|Moralana Supergroup|38704|6|Mentioned|p133|||||||||
26314|Moralana Supergroup|39344|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
26314|Moralana Supergroup|41401|5|Briefly described|p32|||||||||
26314|Moralana Supergroup|42028|6|Mentioned|p137|||||||||
26314|Moralana Supergroup|42215|6|Mentioned|Fig.2 P448|||||||||
26314|Moralana Supergroup|42239|6|Mentioned|Fig.2 P151|||||||||
26314|Moralana Supergroup|42882|5|Briefly described|Table 1 P3|||||||||
26314|Moralana Supergroup|43052|5|Briefly described|p172|||||||||
26314|Moralana Supergroup|43595|5|Briefly described|p545||Cambrian|||||||
26314|Moralana Supergroup|43845|5|Briefly described|Fig2 p42||Early Cambrian|||||||12-JUL-16
26314|Moralana Supergroup|50154|2|Defined|p47, p52, p249 App.5|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt.||||||15-SEP-04
26314|Moralana Supergroup|50155|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50156|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50157|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50158|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50159|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50160|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50161|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50162|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50163|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|50164|5|Briefly described|Map Legend|||||||||
26314|Moralana Supergroup|60451|5|Briefly described|p21 Fig. 7, 106|Late Cambrian|Middle Cambrian|Geological Province: Adelaide Geosyncline.||||||
26314|Moralana Supergroup|60959|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|||||||
26314|Moralana Supergroup|62592|5|Briefly described|p50 Table 5.1.|Early Cambrian|Early Cambrian|Adelaide Geosyncline.|||Includes Hawker and Lake Frome Groups, Billy Creek Formation and Wirrealpa Limestone.|Disconformably overlies Heysen Supergroup.||
26314|Moralana Supergroup|62742|5|Briefly described|p698|Cambrian|Cambrian|Contains a quartz-rich sandstone.||||||21-OCT-08
26314|Moralana Supergroup|64314|5|Briefly described|p495 Fig. 2a|Cambrian|Cambrian|||||||
26314|Moralana Supergroup|64801|6|Mentioned|p110 Fig.2, p111|Middle Cambrian|Early Cambrian|Arrowie Basin.||||Overlies Heysen Supergroup.||
26314|Moralana Supergroup|65375|5|Briefly described|p33.|Cambrian|Cambrian||||Includes all Cambrian units on Yorke Peninsula, from Winulta Formation to Yuruga Formation.|||
26314|Moralana Supergroup|65376|5|Briefly described|p9 Fig.1.2. |Paleozoic|Paleozoic||||||Largely marine sediments and metasediments including limestone and dolomite; minor volcanics.|
26314|Moralana Supergroup|65379|5|Briefly described|p643|||Includes Normanville and Hawker Groups. A major stratigraphic subdivision of the Adelaide Geosyncline.||||||07-MAR-12
26314|Moralana Supergroup|65716|5|Briefly described|p4|Cambrian|Ediacaran|Sedimentary rocks. Enclose Truro Volcanics. Thought to be Early Cambrian. Younger than 500-600 Ma (detrital zircons).||||||
26314|Moralana Supergroup|65925|5|Briefly described|Appendix 2.||||||||Red, white feldspathic sandstone; minor pyritic shale; siltstone; fossiliferous oolitic stromatolitic limestone with minor sandstone and siltstone.|
26314|Moralana Supergroup|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Includes Glenelg River Metamorphic Complex, Nangeela Formation and Truro Volcanics. Defined in Preiss 1982. See also VandenBerg et al 2000.||||||
26314|Moralana Supergroup|68030|6|Mentioned|p236|||Flinders Ranges.||||||
26314|Moralana Supergroup|68131|5|Briefly described|p2 Fig.1|Cambrian|Cambrian|Largely marine.|||||Sediments and metasediments including limestone and dolomite, minor volcanics.|
26314|Moralana Supergroup|69019|5|Briefly described|p66-70.|Cambrian|Cambrian|Of Preiss (1982) for all Cambrian sediments of the Adelaide Geosyncline: Stansbury and Arrowie Basins.|||Includes Hawker and Lake Frome Groups.|||
26314|Moralana Supergroup|70407|5|Briefly described|p102 Fig 1, p103 Fig 2|Early Cambrian|Early Cambrian||||Includes Hawker Group.|||
26314|Moralana Supergroup|70718|5|Briefly described|p37|Middle Cambrian|Neoproterozoic|||||||
26314|Moralana Supergroup|71593|4|Described|p20-p21, p198|Cambrian|Cambrian||||Includes the Normanville and Kanmantoo Groups.|||
26314|Moralana Supergroup|72445|6|Mentioned|App.7 p6 Fig.3.|Cambrian|Cambrian|Shown only on the geological map covering the Stavely Project area (from Geology of Victoria 2003: 21).||||||
26314|Moralana Supergroup|73177|6|Mentioned|p1114||||||Billy Creek Formation.|||
26314|Moralana Supergroup|73222|6|Mentioned|p6|Cambrian|Early Cambrian|Adelaide Rift Complex.|||Hawker Group|||
26314|Moralana Supergroup|74367|5|Briefly described|p4, p6, p22|Cambrian|Cambrian||||Normanville Group, Kanmantoo Group, Lake Frome Group||Sandstones, carbonates and shales.|
12311|Morang Granodiorite|22885|5|Briefly described|map|||||||||
12311|Morang Granodiorite|23273|5|Briefly described|Fig14-5.1p435|||||||||
12311|Morang Granodiorite|23309|6|Mentioned|p437 App 1|||G275 - S-Type.||||||
12311|Morang Granodiorite|33604|5|Briefly described|p19|||||||||
12311|Morang Granodiorite|35278|4|Described|p355|||||||||
12311|Morang Granodiorite|41850|6|Mentioned|p435|||||||||
12311|Morang Granodiorite|42827|6|Mentioned|p435|||||||||
12311|Morang Granodiorite|44197|5|Briefly described|Map Legend||Late Devonian|G275 I-type.||||||
12311|Morang Granodiorite|68116|5|Briefly described|Appendix, Map 42.|Late Devonian|Late Devonian||||||Biotite granodiorite with rare hornblende: equigranular with a coarse porphyritic marginal phase.|
12312|Morass Creek Basalt|22968|6|Mentioned|P160||Pliocene|||||||
12312|Morass Creek Basalt|24133|6|Mentioned|p23|||Geological Province: Lachlan Fold Belt.||||||
12312|Morass Creek Basalt|29860|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
12312|Morass Creek Basalt|38151|6|Mentioned|p35|||||||||
12312|Morass Creek Basalt|39860|5|Briefly described|p32|||||||||
12312|Morass Creek Basalt|44184|5|Briefly described|Map Legend|Miocene|Eocene|||||||
12312|Morass Creek Basalt|60503|3|Fully described|p16-17, p138|Pliocene|Pliocene|Described as the "Newer Basalts" and as Older Basalts. A series of basalt flows - olivine basalt , ranging from dense blue-black basalt with olivine, to glassy basalt, to vesicular olivine basalt. Underlies Japan Creek Gravel. Max. thickness: ~260m.||||||31-AUG-05
12312|Morass Creek Basalt|60504|5|Briefly described|Map Legend|Tertiary|Tertiary|Basalt lava: olivine basalt; blue-black to grey when fresh, dense to moderately vesicular, with well developed columnar jointing||||||
12312|Morass Creek Basalt|60505|5|Briefly described|Map legend|Tertiary|Tertiary|Basalt lava: olivine basalt; blue-black to grey when fresh, dense to moderately vesicular, with well developed columnar jointing||||||
12312|Morass Creek Basalt|60506|5|Briefly described|Map legend|Tertiary|Tertiary|Basalt lava: olivine basalt; blue-black to grey when fresh, dense to moderately vesicular, with well developed columnar jointing||||||
12312|Morass Creek Basalt|60507|5|Briefly described|Map Legend|Tertiary|Tertiary|Basalt lava: olivine basalt; blue-black to grey when fresh, dense to moderately vesicular, with well developed columnar jointing||||||
12312|Morass Creek Basalt|60508|5|Briefly described|Map legend|Quaternary|Tertiary|Olivine basalt lava: reversely magnetised, intensely magnetic (~1000 nT); very low total count, K, Th, U||||||
12312|Morass Creek Basalt|64588|5|Briefly described|p26|Pliocene|Pliocene|Volcanic rocks near Benambra which would be excluded from a proposed redefinition of the 'Newer Volcanics' into an igneous province named Western District Province.||||||02-OCT-08
12312|Morass Creek Basalt|68116|5|Briefly described|Appendix, Map 27.|Pliocene|Pliocene||||||Basalt lava: olivine basalt, blue-black to grey when fresh, dense to moderately vesicular, with well developed columnar jointing.|
12317|Moray Street Gravels|23237|5|Briefly described|p103|||||||||
12317|Moray Street Gravels|23537|6|Mentioned|Fig 7 p 449|||||||||
12317|Moray Street Gravels|24551|5|Briefly described|p338 Fig. 11.2, p734 Table 17.4|Early Pleistocene|Early Pleistocene|Max thickness: 30m.||||||
12317|Moray Street Gravels|29982|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
12317|Moray Street Gravels|30986|5|Briefly described|p197|||See also P198,201. Quaternary||||||
12317|Moray Street Gravels|33604|5|Briefly described|p25|||||||||
12317|Moray Street Gravels|35011|3|Fully described|p311|||||||||
12317|Moray Street Gravels|41848|4|Described|p389|||||||||
12317|Moray Street Gravels|42827|3|Fully described|p389|||||||||
12317|Moray Street Gravels|60083|5|Briefly described|Map legend|Recent|Pleistocene|Silty clay, sometimes fossiliferous; sands, minor gravel of the Yarra delta.||||||
12317|Moray Street Gravels|71277|5|Briefly described|p301,p303 Tb.1,p304,p306,p308,p309 Fig.8|Quaternary|Quaternary|Gill (1962). Up to 10m thick. May infill basal sections of old river valleys, and may be locally fossiliferous.||Yarra Delta Group.||Is overlain by Fishermens Bend Silt, and locally by Burnley Basalt.|Dense to very dense, uncemented medium- to coarse-grained sand, some gravel and some silt and clay, variably carbonaceous.|
12324|Morewell Group|35273|6|Mentioned|p266|||||||||
35129|Morilla Granite|22971|5|Briefly described|p 33, p12 Tb. 1|||Coarse-grained, slightly porphyritic in all felsic minerals.||||||19-JAN-06
35129|Morilla Granite|23309|6|Mentioned|p437 App1|||G194 - I-Type. Supersedes Morilla Adamellite.||||||
35129|Morilla Granite|68116|5|Briefly described|Appendix, Map 19.|Late Devonian|Late Devonian||||||Biotite granite: coarse grained, slightly porphyritic in pink K-feldspar, plagioclase and quartz; accessory allanite, topaz, ilmenite, magnetite, sphene and monazite.|
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.||||||
76939|Mornington Volcanic Group|66244|5|Briefly described|pp5-6.|Eocene|Eocene|This name replaces the Flinders Province of Wellman (1974); formerly the Flinders plateau lava of Keble (1950), who appears to have included his Mornington Lava Field in the Flinders Province. Holdgate et al. (2002) used the term Mornington Volcanics for the Eocene basaltic volcanics in the Port Phillip Basin. The unit covers much of the Mornington Peninsula, Phillip Island, part of French Island and some mainland around southern Westernport Bay.|||||Includes alkali olivine basalt, basanite, nepheline hawaiite and nepheline mugearite; minor shallow intrusives, pyroclastics and interbedded sediments.|
76939|Mornington Volcanic Group|68116|5|Briefly described|Appendix, Maps 50-51, 56.|Lutetian|Lutetian||||||Basanite with lesser alkali basalt, nepheline hawaiite, nepheline mugearite, hawaiite, mugearite and nephelinite; lava flows, shallow intrusives and pyroclastics; minor interbedded fluvial sediments and lignite.|
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.|
69699|Morris Peak pluton|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Subsurface pluton: no gravity data over pluton; moderately to highly magnetic (130 nT). GSV map code: G561.||||||
69699|Morris Peak pluton|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Subsurface pluton: no gravity data over pluton; moderately to highly magnetic (130 nT). GSV map code: G561.||||||07-FEB-11
69699|Morris Peak pluton|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Subsurface pluton: no gravity data over pluton; moderately to highly magnetic (130 nT). GSV map code: G561.||||||
69699|Morris Peak pluton|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Subsurface pluton: no gravity data over pluton; moderately to highly magnetic (130 nT). GSV map code: G561.||||||
69699|Morris Peak pluton|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Subsurface pluton: no gravity data; moderately to highly magnetic (130 nT). GSV map code: G561.||||||
25267|Morton Conglomerate Member|23258|5|Briefly described|p220|||||||||
25267|Morton Conglomerate Member|39865|4|Described|p21|||See also P16||||||
25267|Morton Conglomerate Member|64532|4|Described|p374-377, p379, p382|Sakmarian|Sakmarian|Described by Selwyn (1861); named by Roberts (1984). Marine: contains rare conulariids (Notoconularia).||Bacchus Marsh Formation|||Matrix-supported conglomerate, 1-5m thick with rounded/subrounded clasts up to 28cm across of granite, hornfels, sandstone, slate, quartz; patches of dolomite cement.|
25267|Morton Conglomerate Member|65715|5|Briefly described|p9 Tb.5|Permian|Permian|Of Bacchus Marsh Formation.||||||
12392|Morwell Formation|23230|5|Briefly described|Table4-1p40|Miocene|Oligocene|||||||
12392|Morwell Formation|23264|5|Briefly described|Table13-3.1p325|Miocene|Oligocene|||||||
12392|Morwell Formation|23909|5|Briefly described|p290 Fig.3|Miocene|Oligocene|Of Latrobe Valley Group.  Geological Province: Gippsland Basin.||||||
12392|Morwell Formation|24002|5|Briefly described|p241 fig. 10|Miocene|Oligocene|Geological Province: Gippsland Basin||||||
12392|Morwell Formation|24053|5|Briefly described|p37|Miocene|Eocene|Of Latrobe Group.  Geological Basin: Gippsland Basin.||||||
12392|Morwell Formation|24551|5|Briefly described|p325, p498 Fig. 16.8|Miocene|Oligocene|Of the Latrobe Valley Group.||||||
12392|Morwell Formation|31352|6|Mentioned|p133|||See also Fig. 3. Oligocene - Miocene||||||
12392|Morwell Formation|32679|6|Mentioned|p94|||Strat. diagram||||||
12392|Morwell Formation|34815|6|Mentioned|p15|||||||||
12392|Morwell Formation|34843|5|Briefly described|p10|||||||||
12392|Morwell Formation|34991|6|Mentioned|p382|||||||||
12392|Morwell Formation|35273|5|Briefly described|p257|||See also P266.||||||
12392|Morwell Formation|37530|5|Briefly described|p9|||||||||
12392|Morwell Formation|38417|6|Mentioned|p87|||||||||
12392|Morwell Formation|38928|6|Mentioned|Fig.14|||||||||
12392|Morwell Formation|38929|6|Mentioned|p51|||||||||
12392|Morwell Formation|38930|6|Mentioned|p58|||||||||
12392|Morwell Formation|38973|6|Mentioned|p563|||||||||
12392|Morwell Formation|40114|6|Mentioned|Fig.3|||||||||
12392|Morwell Formation|40117|6|Mentioned|p61|||||||||
12392|Morwell Formation|41868|5|Briefly described|p521|||||||||
12392|Morwell Formation|42184|6|Mentioned|p350|||||||||
12392|Morwell Formation|42648|5|Briefly described|p45|||||||||
12392|Morwell Formation|42649|4|Described|p201|||||||||
12392|Morwell Formation|42827|4|Described|p331, p340|||see also Table 8.21||||||
12392|Morwell Formation|43145|6|Mentioned|p10|Early Miocene|Early Oligocene|of Latrobe Valley Coal Measures.||||||
12392|Morwell Formation|60538|5|Briefly described|p472 Fig. 11, 488 Fig. 22|Middle Miocene|Oligocene|||||||
12392|Morwell Formation|61155|5|Briefly described|p4, p18|Middle Miocene|Early Oligocene|Of the Latrobe Group. Thick sequences of lignite (up to 160m) and clastics accumulated in peat swamps. Overlies Childers Formation and Thorpdale Volcanics. Thickness: 200m. Geological Province: Gippsland Basin (LaTrobe Valley). ||||||
12392|Morwell Formation|61181|5|Briefly described|p105|Early Miocene|Late Oligocene|Of the Latrobe Valley Group. Contains a clay bed which reaches a thickness of 10m and consists of kaolin, with some grit and organic matter. Geological Province: Gippsland Basin. ||||||
12392|Morwell Formation|61302|5|Briefly described|p9|Miocene|Oligocene|Overlies the Thorpdale Volcanics. Geological Province: Gippsland Basin.||||||
12392|Morwell Formation|61336|4|Described|p(v) Fig. 5|Early Miocene|Late Oligocene|Of Seaspray Group. Conformably overlies Traralgon Formation; conformably overlain by Yallourn Formation. Geological Province: Gippsland Basin. See also Morwell formation.||||||07-FEB-11
12392|Morwell Formation|63217|5|Briefly described|p96 Fig.1, p97 Fig.2.|Miocene|Oligocene|Gippsland Basin. Lateral equivalent to Gippsland Limestone, and Lakes Entrance, Formations.|33.0 - 16.4 Ma.|||Unconformably overlies Traralgon Formation. Is overlain by the Yallourn Formation.||
12392|Morwell Formation|65718|6|Mentioned|p10 Fig 3.2, p12|Miocene|Oligocene|||Of the Latrobe Valley Group.||||
12392|Morwell Formation|67061|6|Mentioned|p554 Fig.10.|Miocene||Latrobe Valley, Gippsland Basin.||Unit in Latrobe Valley Group.||Is overlain by Yallourn Formation.||
12392|Morwell Formation|67727|5|Briefly described|p55, p58 Fig.2. |Neogene|Neogene|Latrobe Valley. Onshore coal-bearing equivalent of the Seaspray Group, Balook Formation, and lower Lakes Entrance Formation.||Unit in Latrobe Valley Group.||Overlies Traralgon Formation.||
12392|Morwell Formation|69016|5|Briefly described|p88-89|||Of the Gippsland Basin. Sands are major aquifers with hydraulic conductivities of up to 100 m/day.||Unit of Latrobe Valley Group.||Laterally grades into lower unit of Balook Formation.|Predominantly coal seams interbedded with sands and clays.|
12392|Morwell Formation|69750|6|Mentioned|p68|Miocene|Oligocene|On-shore Gippsland Basin.||Latrobe Valley Group.||Overlies Traralgon Formation. Is overlain by Yallourn Formation.|Brown coal seams separated by thin marine sand and silt sequences.|
12392|Morwell Formation|70076|5|Briefly described|Regional: Fig.3|Burdigalian|Rupelian|Includes subunits marked (Seam 1A), (Clay 1A), (Seam 1B), (Clay 1B) and (Seam 2).||Latrobe Valley Subgroup.||Overlies Traralgon Formation. Is overlain by Yallourn Formation.||
12392|Morwell Formation|70862|5|Briefly described|p48 Fig.1, p49-50|Miocene|Oligocene|Latrobe Valley, Gippsland Basin. Late Oligocene to late Early Miocene.|28.4-15.9 Ma (Partridge, 1971).|Latrobe Valley Group.|Morwell 1A, 1B and 2 Seams.|Overlies Traralgon Formation. Is overlain by Yallourn Formation.||
12392|Morwell Formation|73289|5|Briefly described|p764, 765 Fig.2, 767, 770, 773-774, 776|Burdigalian|Rupelian|Deposition commenced with a major marine transgresson into the Latrobe Valley at c.32.5 Ma. See also p779.|||Morwell 1A, 1B, 2, Seams.|Overlies Traralgon 0 Seam (Traralgon Formation) disconformably. Is overlain by Yallourn Formation.|Thick (>200m) coal seams and interseam sediments.|16-MAY-23
12392|Morwell Formation|73488|4|Described|p630-632, p634 Fig.4, p636-637, p646-647|Burdigalian|Rupelian|Gippsland Basin, Latrobe Valley depression. Falls within Proteacidites tuberculatus (miospore) Zone (Partridge, 1971). Coal seams and their subdivisions are given varying names and abbreviations within text and diagrams. Paleoenvironmental reconstruction maps provided for interseam sediments p643-644 based on lithofacies and fossils; characterised by gradual regression. Also referred to as Morwell seams p635, 647, and Morwell coal seams p634, 644.|||Morwell 1A Seam, Morwell 1B Seam, Morwell 2 Seam|Overlies Traralgon Formation, underlies Yallourn Formation, grades laterally into Balook Formation. Correlated with Lakes Entrance Formation and Gippsland Limestone.|Brackish marine sandstones, brown coal seams, non-marine claystones and sandstones.|
12392|Morwell Formation|73562|5|Briefly described|p303-304, 306, 310|Miocene|Oligocene|Gippsland Basin; onshore.||||Interfingers with Balook Formation.|Coastal plain clastic sediments including thick brown coals.|
12392|Morwell Formation|75065|5|Briefly described|p151|Miocene|Oligocene|Gippsland Basin; onshore.||Latrobe Valley Group.||Unconformably overlies Childers Formation (Cobia Subgroup). Is overlain by Yallourn Formation.|Coal, volcanics.|
34909|Moscow Villa Granodiorite|22968|5|Briefly described|P175, P215|Early Devonian|Late Silurian|New name, intrudes Nunniong Granodiorite and Bentleys Plain Granodiorite, type locality location given on P215||||||
34909|Moscow Villa Granodiorite|23021|6|Mentioned|Map legend|||||||||
34909|Moscow Villa Granodiorite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is unassigned||||||
34909|Moscow Villa Granodiorite|23309|6|Mentioned|p437 App1|||G524 - I-Type.||||||
34909|Moscow Villa Granodiorite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Biotite granodiorite: grey-green; medium-grained; porphyritic with phenocrysts of all main minerals; biotite has replaced hornblende.|
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.|
30688|Mount Anderson Hornblende Porphyry|60503|6|Mentioned|p238|||See also Mount Anderson Porphyry.||||||07-SEP-05
30688|Mount Anderson Hornblende Porphyry|68115|5|Briefly described|p8.|||Omeo Zone. Formerly Mount Anderson Diorite; name changed to reflect better the rock description in VandenBerg et al. (1998a).|||||Hornblende porphyry of diorite composition.|
69711|Mount Angus Granodiorite|61163|5|Briefly described|p119-121|Early Devonian|Early Devonian|Of Murmungee Suite (Chappell 1988). Small elliptical pluton intruding Pinnak Sandstone. Massive, medium-grained, equigranular biotite-hornblende granodiorite, I-type. Geological Province: Lachlan Fold Belt. See also Yackandandah granite. See also p130.||||||
69711|Mount Angus Granodiorite|61174|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende granodiorite: grey; medium-grained; equigranular; rare microgranitoid enclaves. I-type intrusion. GSV map code: G160.||||||07-FEB-11
69711|Mount Angus Granodiorite|61175|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende granodiorite: grey; medium-grained; equigranular; rare microgranitoid enclaves. I-type intrusion. GSV map code: G160.||||||
69711|Mount Angus Granodiorite|61176|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende granodiorite: grey; medium-grained; equigranular; rare microgranitoid enclaves. I-type intrusion. GSV map code: G160.||||||
69711|Mount Angus Granodiorite|61177|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende granodiorite: grey; medium-grained; equigranular; rare microgranitoid enclaves. I-type intrusion. GSV map code: G160.||||||
69711|Mount Angus Granodiorite|61178|5|Briefly described|map legend|Early Devonian|Early Devonian|Two phases distinguished: biotite-hornblende granodiorite (I-type; surrounded by +700m hornfels ridge) and prehnite-albite-chlorite-sericite altered granodiorite cataclasite. GSV map code: G160 alpha and beta respectively.||||||
69711|Mount Angus Granodiorite|68116|5|Briefly described|Appendix, Map 26.|Early Devonian|Early Devonian||||||Biotite-hornblende granodiorite: grey; medium-grained; equigranular; rare microgranitoid enclaves.|
34134|Mount Ararat Granite|22628|5|Briefly described|fig1p108|Middle Devonian|Middle Devonian|||||||
34134|Mount Ararat Granite|23810|5|Briefly described|p888||Devonian|Spelt Mt Ararat Granite. Age: 401+/-3 Ma (SHRIMP U-Pb zircon dating). Lachlan Fold Belt.||||||
34134|Mount Ararat Granite|23814|6|Mentioned|p751|||Mount is Mt in text.||||||
34848|Mount Baldhead Granodiorite|22968|5|Briefly described|P66, P191||Early Devonian|Parent is Baldhead Igneous Complex||||||
34848|Mount Baldhead Granodiorite|23020|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Mount Baldhead Igneous Complex. G139a: highly magnetic (400 nT); low K, Th, low to moderate U. G139b: moderately magnetic (200 nT); low to moderate K, Th, U. G139c: moderately magnetic (125 nT); low to moderate K, Th, U||||||15-SEP-04
34848|Mount Baldhead Granodiorite|23030|5|Briefly described|Map legend|Late Silurian|Late Silurian|Parent is the Mount Baldhead Igneous Complex||||||
34848|Mount Baldhead Granodiorite|23309|6|Mentioned|p343|||G139. I-Type.||||||
34848|Mount Baldhead Granodiorite|24551|6|Mentioned|p44 Fig. 2.51|||||||||
34848|Mount Baldhead Granodiorite|61161|5|Briefly described|p96, p76-77 Fig 6.1, p92 Fig. 6.11|Early Devonian|Early Devonian|Of Mount Baldhead Igneous Complex. Intrudes northern part of Marthavale Tonalite. Homogeneous biotite granodiorite: medium to coarse-grained, equigranular, unfoliated. Moderately magnetic. I-type. GSV map code: G139.||||||12-JUN-14
34848|Mount Baldhead Granodiorite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite +/- hornblende granodiorite: pale to mid-grey; coarse-grained; homogeneous; rare mafic enclaves. I-type intrusion. GSV map code: G139.||||||
34848|Mount Baldhead Granodiorite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite +/- hornblende granodiorite: pale to mid-grey; coarse-grained; homogeneous; rare mafic enclaves. I-type intrusion. GSV map code: G139.||||||07-FEB-11
34848|Mount Baldhead Granodiorite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite +/- hornblende granodiorite: pale to mid-grey; coarse-grained; homogeneous; rare mafic enclaves. I-type intrusion. GSV map code: G139.||||||
34848|Mount Baldhead Granodiorite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite +/- hornblende granodiorite: pale to mid-grey; coarse-grained; homogeneous; rare mafic enclaves. I-type intrusion. GSV map code: G139.||||||
34848|Mount Baldhead Granodiorite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite +/- hornblende granodiorite: zoned with 1 of 3 phases occurring in DARGO: moderate to high gravity response; moderately magnetic; low to moderate K and Th, moderate U and total radioelements. GSV map code: G139.||||||
34848|Mount Baldhead Granodiorite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Biotite granodiorite: pale to mid-grey; coarse-grained; homogeneous; rare mafic enclaves.|
69411|Mount Beauty pluton|61160|4|Described|p87, p32 Tb. 5.2|Devonian|Devonian|See also Mount Beauty Pluton. Elongate magnetic pluton within the Kiewa Shear Zone. ||||||
69411|Mount Beauty pluton|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Intrusive intrusion; subsurface only. GSV map code: G144.||||||
69411|Mount Beauty pluton|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Intrusion; subsurface only. GSV map code: G144.||||||13-SEP-05
69411|Mount Beauty pluton|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Intrusion; subsurface only. GSV map code: G144.||||||13-SEP-05
69411|Mount Beauty pluton|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Intrusion; subsurface only. GSV map code: G144.||||||07-FEB-11
69411|Mount Beauty pluton|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Intrusion: linear dyke-like magnetic highs and lows (50-200 nT); gravity low (-460 ums ^-2); subsurface only. GSV map code: G144.||||||
12524|Mount Black Granite|23309|6|Mentioned|p437 App 1|||G288.||||||
12524|Mount Black Granite|24177|4|Described|p63, p29|Late Devonian|Late Devonian|Intrudes the Puckapunyal Formation.||||||
12524|Mount Black Granite|24328|5|Briefly described|Map legend|Devonian|Devonian|||||||
12524|Mount Black Granite|24329|5|Briefly described|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
12524|Mount Black Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
12524|Mount Black Granite|60591|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Biotite granite: non-magnetic, S-type; medium grained, equigranular; composed of quartz, alkali feldspar, plagioclase and biotite; irregularly jointed.||||||
12524|Mount Black Granite|60592|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Biotite granite: non-magnetic, S-type; medium grained, equigranular; composed of quartz, alkali feldspar, plagioclase and biotite; irregularly jointed.||||||
12524|Mount Black Granite|60593|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Biotite granite: non-magnetic, S-type; medium grained, equigranular; composed of quartz, alkali feldspar, plagioclase and biotite; irregularly jointed.||||||
12524|Mount Black Granite|60595|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Biotite granite: non-magnetic, S-type; medium grained, equigranular; composed of quartz, alkali feldspar, plagioclase and biotite; irregularly jointed.||||||
12524|Mount Black Granite|60596|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Biotite granite: non-magnetic, S-type; medium grained, equigranular; composed of quartz, alkali feldspar, plagioclase and biotite; irregularly jointed.||||||
12524|Mount Black Granite|60597|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Biotite granite; S-type: nonmagnetic, circular feature with a circular magnetic core (5 nT), discontinuous moderately magnetic aureole (5-15 nT); high K, low Th and U.||||||27-OCT-08
12524|Mount Black Granite|60599|3|Fully described|p24 Tb. 4, p104, p20, p107|Late Devonian|Late Devonian|Small intrusive body, highly weathered, holocrystalline rock, med.gr.in which principal minerals can usually be identified by the naked eye; equigranular+ evenly distributed throughout - include quartz, alkali feldspar, plagioclase,biotite.||||||27-OCT-08
12524|Mount Black Granite|61185|6|Mentioned|p126|||Not a formal name. Construction stone used in Goulburn Weir.||||||07-FEB-11
12524|Mount Black Granite|65969|6|Mentioned|p19, p22 Fig.11|||Has a 5 nT magnetic high beneath it. Seems to be the source for alluvial gold in creeks to the SW of Mount Black.||||||
12524|Mount Black Granite|68116|5|Briefly described|Appendix, Map 24.|Late Devonian|Late Devonian||||||Biotite granite: nonmagnetic, medium grained, equigranular; composed of quartz, alkali feldspar, plagioclase and biotite; S-type.|
12524|Mount Black Granite|73497|5|Briefly described|Map legend|Late Devonian|Late Devonian|G288.|||||Biotite granite: S-type; nonmagnetic, with a magnetic core (5 nT), moderately magnetic metamorphic aureole (5-15 nT); high K, low Th and U.|
12527|Mount Blomford Granite|23309|6|Mentioned|p437 App 1|||G141. Unclassified granite type.||||||04-NOV-14
12527|Mount Blomford Granite|24551|6|Mentioned|p230|||Underlies: Wellington Rhyolite.||||||
12527|Mount Blomford Granite|42726|5|Briefly described|map legend|||||||||
12527|Mount Blomford Granite|68116|5|Briefly described|Appendix, Map 44.|Early Devonian|Early Devonian||||||Pink granite: coarse-grained; contains altered biotite, which was probably red-brown originally, and micaceous aggregates after cordierite.|
27499|Mount Bruno Granite|22971|5|Briefly described|p28,34|||||||||
27499|Mount Bruno Granite|23309|5|Briefly described|App1 p437|||G205 S-Type.||||||27-AUG-04
27499|Mount Bruno Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
27499|Mount Bruno Granite|68116|5|Briefly described|Appendix, Map 19.|Late Devonian|Late Devonian||||||Biotite-muscovite granite with accessory garnet, evenly medium grained to porphyritic, pale grey.|
12549|Mount Buffalo Granite|22628|6|Mentioned|fig1p108|Devonian|Devonian|spelt "Mt" in the text||||||
12549|Mount Buffalo Granite|22971|5|Briefly described|p 30|Early Devonian||Age: 394+/-4Ma.||||||
12549|Mount Buffalo Granite|23309|5|Briefly described|p343.|Middle Devonian|Early Devonian|G161 - I-Type. Age: 394+/-16, 397+/-16, 386+/-15 Ma, 397+/-16, 392+/-16 Ma.||||||
12549|Mount Buffalo Granite|24551|6|Mentioned|p38|||||||||
12549|Mount Buffalo Granite|30906|6|Mentioned|Map legend|Devonian|Devonian|||||||
12549|Mount Buffalo Granite|31713|5|Briefly described|p12|||||||||
12549|Mount Buffalo Granite|42089|6|Mentioned|p19|||||||||
12549|Mount Buffalo Granite|42726|5|Briefly described|map legend|||||||||
12549|Mount Buffalo Granite|50086|5|Briefly described|p10 Fig. 5, p20 Fig. 10|Early Devonian|Early Devonian|Mount is Mt. in text of figure.  Geological Province:  Lachlan Fold Belt.||||||10-MAR-05
12549|Mount Buffalo Granite|61161|6|Mentioned|p30|||Gravity low.||||||12-JUN-14
12549|Mount Buffalo Granite|61163|3|Fully described|p115-116, p37 Tb. 6.2|Early Devonian|Early Devonian|Age: 394+/-4Ma. Medium, elliptical pluton- homogeneous med-coarse-grained biotite leucogranite with minor muscovite; equigranular, but has phenocrysts of orthoclase locally. Intrudes Pinnak Sandstone. Geol Prov: Lachlan Fold Belt. See also p130.||||||
12549|Mount Buffalo Granite|61174|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-muscovite leucogranite: grey to pinkish grey; coarse-grained, mostly equigranular; some porphyritic phases with orthoclase phenocrysts. I-type intrusion. GSV map code: G161.||||||07-FEB-11
12549|Mount Buffalo Granite|61175|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-muscovite leucogranite: grey to pinkish grey; coarse-grained, mostly equigranular; some porphyritic phases with orthoclase phenocrysts. I-type intrusion. GSV map code: G161.||||||
12549|Mount Buffalo Granite|61176|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-muscovite leucogranite: grey to pinkish grey; coarse-grained, mostly equigranular; some porphyritic phases with orthoclase phenocrysts. I-type intrusion. GSV map code: G161.||||||
12549|Mount Buffalo Granite|61177|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-muscovite leucogranite: grey to pinkish grey; coarse-grained, mostly equigranular; some porphyritic phases with orthoclase phenocrysts. I-type intrusion. GSV map code: G161.||||||
12549|Mount Buffalo Granite|61178|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite+/-muscovite leucogranite (I- or A- type; 394+/-4Ma [K/Ar]): low frequency, weakly magnetic; low gravity extending beyond outcrop; high total radio element, K and U especially around margins, low Th. GSV map code: G161.||||||
12549|Mount Buffalo Granite|61187|5|Briefly described|p5 Fig.3. |Early Devonian|Early Devonian|Tabberabbera Zone, Benambra Terrane. Age interpreted from Fig.3.|c.390 Ma.|||||
12549|Mount Buffalo Granite|65900|5|Briefly described|p156 Fig. 2, p157,p158, Fig. 3, p162||Early Devonian|Tabberabbera Zone. Appears as gravity low. Written Mt in text.||||||10-MAY-12
12549|Mount Buffalo Granite|68116|5|Briefly described|Appendix, Map 26.|Early Devonian|Early Devonian||||||Interlayered Mount Burt Granite and gneiss, layers 1-10 m thick.|
12551|Mount Buller Granodiorite|33602|6|Mentioned|Fig.2|||||||||
12551|Mount Buller Granodiorite|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
12551|Mount Buller Granodiorite|35073|6|Mentioned|p22|||||||||
12551|Mount Buller Granodiorite|35112|6|Mentioned|p280|||||||||
12551|Mount Buller Granodiorite|64616|6|Mentioned|p344|||I-type intrusion. Associated with a set of conjugate faults which may have assisted emplacement of the intrusion.||||||
37579|Mount Buller Suite|23309|4|Described|p322, 346|Middle Devonian|Middle Devonian|Consists of Mount Stirling Granodiorite, Bindaree Diorite and Mirimbah Granodiorite.||||||
37579|Mount Buller Suite|65900|5|Briefly described|p156 Fig. 2, p158, p162|Middle Devonian|Middle Devonian|Tabberabbera Zone.|||||I-type highly magnetic granites. Diorite and gabbro.|10-MAY-12
37868|Mount Burrowa Volcanic Group|24133|3|Fully described|p41|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37868|Mount Burrowa Volcanic Group|24142|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37868|Mount Burrowa Volcanic Group|24143|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37868|Mount Burrowa Volcanic Group|24144|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37868|Mount Burrowa Volcanic Group|24145|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Geological Province: Lachlan Fold Belt||||||
37868|Mount Burrowa Volcanic Group|24146|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37868|Mount Burrowa Volcanic Group|24551|5|Briefly described|p118 Fig. 5.1|Devonian|Devonian|see also Mount Burrowa Cauldron Complex.||||||
34842|Mount Burt Granite|22968|5|Briefly described|P60, P180|Silurian|Early Silurian|New name, nonmagnetic, intruded by the Doctors Flat Tonalite||||||
34842|Mount Burt Granite|23020|5|Briefly described|Map legend||Late Silurian|||||||
34842|Mount Burt Granite|23029|5|Briefly described|Map legend|Wenlock|Wenlock|Parent is unassigned||||||
34842|Mount Burt Granite|23030|5|Briefly described|Map legend|Silurian|Silurian|parent is unassigned||||||
34842|Mount Burt Granite|23309|5|Briefly described|p256, 338|||G519 S-Type||||||
34842|Mount Burt Granite|68116|5|Briefly described|Appendix, Map 35.|Ludlow|Wenlock||||||Biotite granite and tonalite: medium-grained; equigranular; well foliated; contains some garnet and cordierite; grey.|
12560|Mount Bute Granite|23308|6|Mentioned|Map Legend|||Mine name?||||||
12560|Mount Bute Granite|23309|5|Briefly described| p256||Late Devonian|G308 I-Type. Age: 358+/-4 Ma, 370+/-4 Ma. Supersedes Mount Bute Adamellite.||||||
12560|Mount Bute Granite|23810|5|Briefly described|p888||Devonian|Age: 370+/-4 Ma (SHRIMP U-Pb). Spelt Mt Bute Granite in literature. Lachlan Fold Belt.||||||
12560|Mount Bute Granite|23814|5|Briefly described|p745|Devonian|Devonian|Age: 370+/-4Ma.  Geological Province: Stawell Zone.||||||
12560|Mount Bute Granite|24551|6|Mentioned|p408|Late Devonian|Late Devonian|Age: 370 +/- 4Ma.||||||
12560|Mount Bute Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
12560|Mount Bute Granite|44186|5|Briefly described|Map Legend||Early Devonian|G307 I-type.||||||
12560|Mount Bute Granite|50352|5|Briefly described|Map Legend|Devonian|Devonian|Coarse-grained hornblende biotite granite||||||21-MAY-13
12560|Mount Bute Granite|66002|5|Briefly described|p6 Tb.5|||Of Beckworth Suite. G308. Defined in Taylor et al. (1995).||||||21-MAY-13
12560|Mount Bute Granite|66012|3|Fully described|p10 Tb.1, p11 Tb.2, p11-16|Devonian|Devonian|Of Beckworth Suite. Unconformably overlain by White Hills Gravel. Coarse-grained I-type granite. Intrudes Saint Arnaud Group and Mount Emu Granodiorite. Crops out poorly as boulders on low hills. Also called Mount Bute Adamellite. Oxidised| | | | | |13-JUN-13
12560|Mount Bute Granite|67804|6|Mentioned|p67||||~370 Ma (40 Ar/ 39 Ar).|||||
12560|Mount Bute Granite|67978|6|Mentioned|p496 Fig.1|Famennian|Frasnian|Mount is spelt Mt in text. Zircon dating from Mt Bute granite by Arne et al. (1998).|370 +/- 4 Ma, SIMS U-Pb|||||19-SEP-14
12560|Mount Bute Granite|68116|5|Briefly described|Appendix, Maps 30, 40.|Late Devonian|Middle Devonian||||||Hornblende biotite granite: medium to coarse grained, pale grey; mafic enclaves and host-rock inclusions; aplite dykes; weathered to kaolinised, magnetic.|
12560|Mount Bute Granite|75061|6|Mentioned|p60, 64, 67, 70|Late Devonian|Late Devonian|Stawell Zone, Lachlan Fold Belt.|371.3 +/- 2.8 Ma.||||I-type biotite granite.|
12560|Mount Bute Granite|75072|5|Briefly described|p230 Fig.2, 233, 240-241, 249, 253|Late Devonian|Late Devonian|Stawell Zone. Zircon age distribution listed and discussed; probability density graph.|371.3 +/- 2.8 Ma (Clemens et al., 2022)||||Monzogranite. I-type.|
40660|Mount Chief Andesite|23309|5|Briefly described|p28 Table 2.4|||Of the Lickhole Volcanic Group.||||||
12585|Mount Clear Granodiorite|29953|6|Mentioned|p3|||||||||
12588|Mount Cole Granite|23164|6|Mentioned|p34|||||||||
12588|Mount Cole Granite|23232|6|Mentioned|p63|||Written: Mt Cole Granite.||||||21-OCT-08
12588|Mount Cole Granite|23309|5|Briefly described|p339, 341|Middle Devonian|Early Devonian|G378 I-Type. Age: 393+/-17, 392+/-5, 389+/-5 Ma, 391+/-9 Ma. Supersedes Mount Cole Adamellite.||||||
12588|Mount Cole Granite|42726|5|Briefly described|map legend|Early Devonian||No. 739.||||||15-FEB-05
12588|Mount Cole Granite|42745|6|Mentioned|p14|||Actually spelt Mt Cole Granite.||||||
12588|Mount Cole Granite|64314|6|Mentioned|p495 Fig. 2a|||||||||
12588|Mount Cole Granite|66002|5|Briefly described|p7 Tb.5|||Of Mount Cole Suite.G378. Called Mount Cole Adamellite by Cayley and McDonald (1995)||||||
12588|Mount Cole Granite|68116|5|Briefly described|Appendix, Map 31.|Early Devonian|Early Devonian||||||Hornblende-biotite granite: pale pink to grey; coarse grained; porphyritic.|
28790|Mount Cole Suite|22531|6|Mentioned|p17|||Mount is written Mt in text||||||
28790|Mount Cole Suite|22532|6|Mentioned|map legend|Devonian|Devonian|Mount is written Mt in text||||||
28790|Mount Cole Suite|22756|5|Briefly described|P40|||||||||
28790|Mount Cole Suite|23164|6|Mentioned|p20|||Mount is Mt in text.||||||
28790|Mount Cole Suite|23166|5|Briefly described|Map legend||Devonian|||||||
28790|Mount Cole Suite|23167|5|Briefly described|Map legend||Devonian|||||||
28790|Mount Cole Suite|23168|5|Briefly described|Map legend||Devonian|||||||
28790|Mount Cole Suite|23169|5|Briefly described|Map legend||Devonian|||||||
28790|Mount Cole Suite|23300|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
28790|Mount Cole Suite|23301|5|Briefly described|Map Legend|Devonian|Devonian|Mount is Mt in text||||||
28790|Mount Cole Suite|23302|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
28790|Mount Cole Suite|23303|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
28790|Mount Cole Suite|23304|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
28790|Mount Cole Suite|23305|4|Described|p42||Early Devonian|In the Stawell Province.||||||07-MAR-07
28790|Mount Cole Suite|23309|5|Briefly described|p224, 339-340, 342||Early Devonian|||||||
28790|Mount Cole Suite|23549|5|Briefly described|p525|||Granites with distinctive magnetic patterns.  Geological Province: Lachlan Fold Belt.  Mount is  Mt in text.||||||05-APR-05
28790|Mount Cole Suite|23810|5|Briefly described|p888|||Includes Mt Cole Adamellite, Buangor Granite and the Hickman Creek Granite. Mount is Mt in text.  In the Lachlan Fold Belt.||||||07-MAR-07
28790|Mount Cole Suite|24002|5|Briefly described|p241|Early Devonian|Early Devonian|Mount is Mt. in text.||||||
28790|Mount Cole Suite|24098|5|Briefly described|p31|||Geological Province: Selwyn Block.  Mount is Mt in text.||||||
28790|Mount Cole Suite|24178|6|Mentioned|p70, 71|Early Devonian|Early Devonian|Of the Stawell Basement Terrane and includes the Mount Hoogly, Tarnagulla and Korong plutons (White and Chappell, 1988)||||||
28790|Mount Cole Suite|24551|5|Briefly described|p226|||Of the Stawell Province.||||||
28790|Mount Cole Suite|41563|6|Mentioned|p515|||||||||
28790|Mount Cole Suite|42726|5|Briefly described|map legend|Late Devonian|Early Devonian|||||||
28790|Mount Cole Suite|42827|5|Briefly described|p436, 437|||||||||03-FEB-15
28790|Mount Cole Suite|43260|5|Briefly described|Map Legend||Early Devonian|||||||
28790|Mount Cole Suite|43627|14|Not recorded|Map Key|||||||||
28790|Mount Cole Suite|43846|4|Described|12||Devonian|Isotopic age near 390Ma.||||||07-MAR-07
28790|Mount Cole Suite|60452|5|Briefly described|p52|||See also Mount Cole suite. Component outcrop pluton: Wedderburn, and buried plutons: Loddon Vale, Lyndger.||||||27-OCT-04
28790|Mount Cole Suite|60461|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes the Wedderburn Granodiorite, and the Loddon Vale and Lyndger plutons.||||||28-SEP-04
28790|Mount Cole Suite|60462|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||28-SEP-04
28790|Mount Cole Suite|60491|5|Briefly described|p50|||Includes Wychitella Granite.||||||
28790|Mount Cole Suite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Wychitella Granite.||||||
28790|Mount Cole Suite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Includes: Wychitella Granite. Mount is Mt in text of legend.||||||30-SEP-04
28790|Mount Cole Suite|60543|6|Mentioned|Map legend|Early Devonian|Early Devonian|Age: 400-380Ma (Rb/Sr).   Mount is Mt in text.||||||23-DEC-09
28790|Mount Cole Suite|60544|6|Mentioned|Map legend|Early Devonian|Early Devonian|Age: 400-380Ma (Rb/Sr).  Mount is Mt in text.||||||
28790|Mount Cole Suite|60585|6|Mentioned|p23|Late Devonian|Late Devonian|||||||
28790|Mount Cole Suite|62755|5|Briefly described|p882|Devonian|Devonian|High magnetic susceptibility Devonian plutons which are in alignment along northeast and northwest trends. Mount is Mt in text.||||||21-MAY-13
28790|Mount Cole Suite|65715|5|Briefly described|p8 Tb.4|||Includes Wedderburn Granodiorite, Kooyoora Granite, Moliagul Granite, Tarnagulla Granite and Natte Yallock Granite.||||||
28790|Mount Cole Suite|65969|6|Mentioned|p15|Early Devonian|Early Devonian|~400 Ma. Possibly similar to Loddon Vale and Yarraberb plutons in BENDIGO 1:250 000 sheet which are strongly magnetic, distinctively peraluminous, high-Na chemistry.||||||
28790|Mount Cole Suite|66002|5|Briefly described|p7 Tb.5|||Includes Natte Yallock Granite, Carapooee Granodiorite, Wychitella Granite, Elmhurst Granite, Ben Nevis Granite, Eversley Granite, Langi Ghiran Granite, Buangor Granite, Mount Cole Granite, Dunneworthy Granodiorite, Hickman Creek Granite & Kooreh Granite. Defined in White and Chappell 1988.||||||
28790|Mount Cole Suite|66769|6|Mentioned|142|Early Devonian|Early Devonian|Stawell and northern Bendigo Zones. Highly magnetic, hornblende-bearing, metaluminous granites (I-type) occur above middle and lower crust dominated by mafic meta-igneous rocks.||||||
28790|Mount Cole Suite|67978|5|Briefly described|p496 Fig.1, p499 Tb.1|||Mount is spelt Mt in text. Stawell zone.|||Includes Buangor Granite and Eversley Granite.|||
28790|Mount Cole Suite|68189|6|Mentioned|p15 Fig.6|||Presented as Mt Cole Suite.|||||granites|
28790|Mount Cole Suite|68194|6|Mentioned|p11|||Erosion has produced feldspathic quartzose sediments which give K-rich radiometric images.||||||
28790|Mount Cole Suite|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian||||Includes Loddon Vale pluton.|||
28790|Mount Cole Suite|73497|5|Briefly described|Map legend|Devonian|Silurian||||Loddon Vale pluton, Mincha pluton|||21-OCT-22
28790|Mount Cole Suite|73505|5|Briefly described|p7|Early Devonian|Early Devonian|The magnetic granites form a strong alignment at about 020 degrees. Distinctive peraluminous, high-Na chemistry, often contains hornblende, sphene and allanite or monazite (White and Chappell, 1988).|400 Ma||Loddon Vale Granite||Granites.|
31532|Mount Cole Supersuite|42726|5|Briefly described|map legend|||||||||
40922|Mount Dandenong Volcanic Group|24177|5|Briefly described|p50 Fig.22|Late Devonian|Late Devonian|Mount is Mt. in text of figure. Geological Province: Darraweit Guim Province||||||
40922|Mount Dandenong Volcanic Group|60599|5|Briefly described|p47 Fig. 19|Late Devonian|Late Devonian|Geological Province: Darraweit Guim Province, Melbourne Zone, Lachlan Fold Belt. Mount is Mt in text of figure. G109||||||
40922|Mount Dandenong Volcanic Group|61185|5|Briefly described|p21 Fig. 6|Late Devonian|Late Devonian|Geological Province: Lachlan Fold Belt, Melbourne Zone. Presented as Mt Dandenong Volcanic Group.||||||07-FEB-11
40922|Mount Dandenong Volcanic Group|73199|6|Mentioned|p521, p524|Late Devonian|Late Devonian|[Written as Mt Dandenong Volcanic Group and Mount Dandenong Volcanic Group]. Dominantly S-type volcanic rocks with minor I-type. Inferred to have similar deep-crustal sources to plutonic granitic magmas.||||||
22409|Mount Dawson Subgroup|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Snowy River Volcanics||||||
22409|Mount Dawson Subgroup|23309|4|Described|p110, Tb 2.40|||Of the Snowy River Volcanics.||||||
22409|Mount Dawson Subgroup|23615|3|Fully described|p104, p23|Early Devonian|Early Devonian|Of Snowy River Volcanics.  Comprises 7 ignimbrites: Woolshed Creek, Dead Cattle Gully, Doonarlick, Doyle Gully, Bimmarn, Plumb Gully and Lookout Top Ignimbrites.  Overlies Marroo and Timbarra Subgroups in the north.  Age: Early Devonian ~410-395Ma.||||||16-AUG-18
22409|Mount Dawson Subgroup|24551|4|Described|p143, p141 Fig.  5.32|||Of Snowy River Volcanics.||||||
22409|Mount Dawson Subgroup|43206|5|Briefly described|map legend||Ludlow|Of Snowy River Volcanics||||||
22409|Mount Dawson Subgroup|43312|5|Briefly described|Map Legend||Early Devonian|of Snowy River Volcanics||||||
22409|Mount Dawson Subgroup|43313|5|Briefly described|Map Legend||Early Devonian|of Snowy River Volcanics||||||12-JUN-14
22409|Mount Dawson Subgroup|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Unit in Snowy River Volcanics.|||Extrusive, fluvial: felsic ignimbrite, mostly densely welded.|
22409|Mount Dawson Subgroup|60542|5|Briefly described|p53|Early Devonian|Early Devonian|Of the Snowy River Volcanics. Tentatively includes the Yellow Waterholes Ignimbrite - the only unit in the subgroup to extend into ORBOST. ||||||
22409|Mount Dawson Subgroup|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Vitric and feldspar-phyric red pumice ignimbrite; ash, volcaniclastic sandstone and breccia lenses.|
30438|Mount Difficult Subgroup|23307|5|Briefly described|Map Legend|Silurian|Silurian|Of Grampians Group||||||
30438|Mount Difficult Subgroup|23309|5|Briefly described|p79-83. Tb 2.27|||||||||
30438|Mount Difficult Subgroup|23402|3|Fully described|p28|Silurian|Silurian|Of the Grampians Group. Thickness: 1300m. Overlies the Silverband Formation. Geological Province: Adelaide Fold Belt||||||12-NOV-08
30438|Mount Difficult Subgroup|24551|4|Described|p120|||Of the Grampians Group. Appoximately 1050m thick. Consists of 3 formations.||||||02-MAY-13
30438|Mount Difficult Subgroup|24581|5|Briefly described|p813|||Mount is Mt. in text. Of the Grampians Group. Geological Province: Kanmantoo Fold Belt.||||||
30438|Mount Difficult Subgroup|50154|5|Briefly described|p113|||Of the Grampians Group.||||||
30438|Mount Difficult Subgroup|60451|4|Described|p76, 81|Early Devonian|Ordovician|Of the Grampians Group. Maximum Thickness: 1050m. Overlies: Silverband Formation. Includes: Serra, Moora Moora and Wartook Sandstones.||||||
30438|Mount Difficult Subgroup|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Includes: Wartook Sandstone, Moora Moora Sandstone, Serra Sandstone, Teddy Bear Conglomerate Member.||||||
30438|Mount Difficult Subgroup|61183|4|Described|p28-29, p44-45|||Supersedes Mount Difficult Formation. Upper part of the Grampians Group. Includes Serra, Moora Moora and Wartook Sandstones. Quartzose sandstone unit. Overlies the Silverband Formation conformably. Thickness: 1050m. See also p30 Tb. 2, p56.||||||
30438|Mount Difficult Subgroup|61186|5|Briefly described|p77|||Of the Grampians Group. Includes the Wartook Sandstone at the top of the unit. ||||||
30438|Mount Difficult Subgroup|61749|5|Briefly described|p14|||Of the Grampians Group. Quartzose sandstone package. Overlies Silverband Formation. Thickness: 1050m.||||||02-MAY-13
30438|Mount Difficult Subgroup|61752|5|Briefly described|p10|||Uppermost unit of the Grampians Group. Quartzose sandstone package. Overlies Silverband Formation. Thickness: 1050m. Geological Province: Lachlan Fold Belt. Mount may be Mt in text.||||||07-FEB-11
30438|Mount Difficult Subgroup|64610|5|Briefly described|Map legend|Silurian|Silurian|Of the Grampians Group. Includes Serra, Moora Moora and Wartook Sandstones. Mainly sandstones; some conglomerate.||||||11-NOV-08
30438|Mount Difficult Subgroup|65313|6|Mentioned|p582 Fig.10|Devonian|Silurian||||Includes Serra Sandstone, Moora Moora Sandstone, Wartook Sandstone.|||26-MAR-12
30438|Mount Difficult Subgroup|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Grampians Group. Includes Wartook Sandstone, Moora Moora Sandstone and Serra Sandstone. Defined by Spencer-Jones, 1965. Redefined by Cayley & Taylor, 1997.||||||
30438|Mount Difficult Subgroup|68116|5|Briefly described|Appendix, Map 39.|Pridoli|Ludlow|Quartz sandstone, minor siltstone and mudstone, minor conglomerate; Skolithos horizons and ripple surfaces. |||||Sandstone: pale, medium to coarse grained with sub-rounded vein quartz pebbles; laminated to trough cross-laminated, medium to thickly bedded; conglomerate: pale grey; polymictic; poorly sorted with open framework; micaceous siltstone and sandstone.|
12638|Mount Disappointment Granodiorite|22882|5|Briefly described|p 13|||Dargile Formation||||||
12638|Mount Disappointment Granodiorite|22885|5|Briefly described|map|||||||||
12638|Mount Disappointment Granodiorite|22886|4|Described|Table.1|||Age: Rb/Sr 370Ma.||||||
12638|Mount Disappointment Granodiorite|23269|6|Mentioned|Fig14-3.1p403|||||||||
12638|Mount Disappointment Granodiorite|23309|5|Briefly described|p347|||G221- I-Type. Supersedes Mount Disappointment Granite.||||||
12638|Mount Disappointment Granodiorite|30867|6|Mentioned|p15|||||||||
12638|Mount Disappointment Granodiorite|32001|6|Mentioned|p78|||||||||
12638|Mount Disappointment Granodiorite|35283|6|Mentioned|p48|||||||||
12638|Mount Disappointment Granodiorite|39331|6|Mentioned|Fig.0-3|||||||||
12638|Mount Disappointment Granodiorite|41641|6|Mentioned|Fig.5.1|||||||||
12638|Mount Disappointment Granodiorite|42154|6|Mentioned|Table 1 P334|||||||||
12638|Mount Disappointment Granodiorite|44197|5|Briefly described|Map Legend||Late Devonian|G221 I-type.||||||
12638|Mount Disappointment Granodiorite|45087|5|Briefly described|p40|||Chemical analyses.||||||
12638|Mount Disappointment Granodiorite|68116|5|Briefly described|Appendix, Map 33.|Late Devonian|Late Devonian|Informally subdivided into granodiorite and pophyritic phases. Biotite granodiorite phase contains accessory zircon, ilmenite and apatite, whilst the porphyritic phase contains accessory apatite; common microgranitoid enclaves.|||||Biotite granodiorite: medium-grained, equigranular; quartz, oligoclase, orthoclase, biotite; occasional xenoliths. Porphyritic phase: biotite granodiorite, with perthitic orthoclase phenocrysts in a quartz, oligoclase, orthoclase, biotite groundmass.|
12638|Mount Disappointment Granodiorite|70629|6|Mentioned|p986, p1000|Devonian|Devonian|Melbourne Zone. Has a similar major element composition as the nearby Mo- and W-bearing granitic intrusions at Monkey Gully.||||||
12638|Mount Disappointment Granodiorite|75061|5|Briefly described|p60, 65, 67, 70|Late Devonian|Late Devonian|Forms a prominent peak near Whittlesea. Melbourne Zone.|375.2 +/- 2.5 Ma.||||Transitional S-type monzogranitic nested laccolith. Biotite monzogranites, with a K-feldspar-megacrystic phase.|
32175|Mount Dryden Volcanics|23061|6|Mentioned|293 fig 1|||||||||
32175|Mount Dryden Volcanics|24551|6|Mentioned|p24 Fig 2.13|Cambrian|Cambrian|||||||
32175|Mount Dryden Volcanics|43227|6|Mentioned|p7|||Actually spelt Mt Dryden Volcanics.||||||
32175|Mount Dryden Volcanics|61187|5|Briefly described|p82, p83 Fig.1, p84 Fig.2.|Late Cambrian|Middle Cambrian|Associated with Delamerian Orogeny. Forms narrow linear belt with high magnetic responses.|||||Calc-alkaline intermediate volcanics.|
32175|Mount Dryden Volcanics|61410|6|Mentioned|p7 Fig.2|Cambrian|Cambrian|||||||
32175|Mount Dryden Volcanics|61752|5|Briefly described|p3 Fig. 1|Cambrian|Cambrian|Mount is Mt in text of figure.  Geological Province: Adelaide Fold Belt.||||||07-FEB-11
32175|Mount Dryden Volcanics|70967|6|Mentioned|p13, 17|||||||||
32175|Mount Dryden Volcanics|72445|6|Mentioned|p12, p16.|Cambrian|Cambrian|Target basement prior to drilling Stavely 01. Was identified as Carolls Amphibolite of Moornambool Metamorphic Complex.||||||
12668|Mount Easton Shale|22628|6|Mentioned|fig1p108|Ordovician|Ordovician|spelt "Mt" in the text.||||||22-DEC-08
12668|Mount Easton Shale|22708|5|Briefly described|p210|Late Ordovician|Late Ordovician|||||||
12668|Mount Easton Shale|22971|5|Briefly described|p 17||Ordovician|||||||
12668|Mount Easton Shale|23229|4|Described|Table3-2p21, 24|Bolindian|Darriwilian|Written: Mt Easton Shale.||||||25-SEP-08
12668|Mount Easton Shale|23309|5|Briefly described|p59-61, 148, 155, 273, 274.||Ordovician|||||||
12668|Mount Easton Shale|23938|5|Briefly described|p11|Late Ordovician|Late Ordovician|||||||
12668|Mount Easton Shale|24002|5|Briefly described|p247|Late Ordovician|Late Ordovician|||||||
12668|Mount Easton Shale|24098|5|Briefly described|p31|||Geological Province: Selwyn Block.  Mount is Mt in text.||||||
12668|Mount Easton Shale|24134|5|Briefly described|p6 Fig. 2|Middle Ordovician|Early Ordovician|||||||
12668|Mount Easton Shale|24177|5|Briefly described|p50 Fig.22|Bolindian|Bolindian|Mount is Mt. in text of figure. Geological Province: Mount Easton Province.||||||
12668|Mount Easton Shale|24178|5|Briefly described|p15 Fig.2|Middle Ordovician|Early Ordovician|Geological Province: Bendigo Zone.||||||22-DEC-08
12668|Mount Easton Shale|24214|6|Mentioned|p788 Fig. 2|||||||||
12668|Mount Easton Shale|24551|4|Described|p105, 606|Late Ordovician|Late Ordovician|Correlated with the Bendoc Group.||||||02-FEB-15
12668|Mount Easton Shale|24576|5|Briefly described|p727, 729, 744|Late Ordovician|Late Ordovician|Age: 419 Ma (Ar/Ar) from black shales no younger than Late Ordovician (Mt Easton Shale). Overlain by the Jordan River Group. Geological Province: Lachlan Fold Belt.||||||03-SEP-18
12668|Mount Easton Shale|24600|5|Briefly described|p479|Late Ordovician|Late Ordovician|Mount is Mt in text.  Geological Province: Lachlan Fold Belt.||||||
12668|Mount Easton Shale|29709|4|Described|p33|||||||||
12668|Mount Easton Shale|33601|6|Mentioned|Fig.2|||||||||
12668|Mount Easton Shale|33602|6|Mentioned|p3|||||||||
12668|Mount Easton Shale|34843|6|Mentioned|p5|||||||||
12668|Mount Easton Shale|35073|6|Mentioned|p5|||||||||
12668|Mount Easton Shale|35112|6|Mentioned|p276|||||||||
12668|Mount Easton Shale|35281|6|Mentioned|p16|||See also P23.||||||
12668|Mount Easton Shale|35283|6|Mentioned|p49|||||||||
12668|Mount Easton Shale|39551|6|Mentioned|Map legend|Bolindian|Gisbornian|Bolindian to Gisbornian||||||
12668|Mount Easton Shale|39858|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
12668|Mount Easton Shale|40127|6|Mentioned|p5|||||||||
12668|Mount Easton Shale|40136|5|Briefly described|p32|||||||||
12668|Mount Easton Shale|40761|5|Briefly described|Table 1|||Mention p223.||||||03-SEP-18
12668|Mount Easton Shale|41570|3|Fully described|p88|||||||||
12668|Mount Easton Shale|41571|6|Mentioned|Fig.2.6|||||||||
12668|Mount Easton Shale|41572|6|Mentioned|p13|||||||||
12668|Mount Easton Shale|41585|6|Mentioned|p118|||||||||
12668|Mount Easton Shale|42089|5|Briefly described|Fig.16 P27|||||||||
12668|Mount Easton Shale|42560|6|Mentioned|p53|||||||||
12668|Mount Easton Shale|42827|4|Described|p88|||see also Table 4.1||||||
12668|Mount Easton Shale|44187|5|Briefly described|Map Legend||Late Ordovician|||||||
12668|Mount Easton Shale|60536|5|Briefly described|p550|Ordovician|Ordovician|Age: ca. 420 Ma (Ar-Ar, Spaggiari et al, 2003c).||||||
12668|Mount Easton Shale|60599|5|Briefly described|p47 Fig. 19|Bolindian|Bolindian|Geological Province: Mount Easton Province, Melbourne Zone, Lachlan Fold Belt. Mount is Mt in text of figure.||||||
12668|Mount Easton Shale|61185|5|Briefly described|p21 Fig. 6|Bolindian|Bolindian|Faulted contact with overlying McAdam Sandstone. Geological Province: Lachlan Fold Belt, Melbourne Zone. Presented as Mt Easton Shale.||||||07-FEB-11
12668|Mount Easton Shale|61187|5|Briefly described|p4, p5 Fig.3, p51 Fig.2.|Late Ordovician|Late Ordovician|Melbourne Zone, Melbourne Terrane. Correlative of Warbisco Shale and Bendoc Group in the Benambra Terrane.||||||
12668|Mount Easton Shale|62099|5|Briefly described|p331|Late Ordovician|Late Ordovician|Black shale dominates. In the Melbourne Zone of the Lachlan Orogen. Mount is Mt in text.||||||
12668|Mount Easton Shale|64535|5|Briefly described|Map legend|Late Ordovician|Middle Ordovician|Black shale, thick-bedded, rarely with soft-sediment folding; minor sandstone, pale grey, thin to thick bedded, fine- to medium-grained; turbidites, micaceous; shale commonly with Late Ordovician graptolite faunas; deep marine hemipelagic deposits.||||||22-DEC-08
12668|Mount Easton Shale|64536|5|Briefly described|Map legend|Late Ordovician|Middle Ordovician|Black shale, thick-bedded, rarely with soft-sediment folding; minor sandstone, pale grey, thin to thick bedded, fine- to medium-grained; turbidites, micaceous; shale commonly with Middle-Late Ordovician graptolite faunas; deep marine hemipelagic deposits.||||||07-FEB-11
12668|Mount Easton Shale|64537|5|Briefly described|Map legend|Late Ordovician|Middle Ordovician|Black shale, thick-bedded, rarely with soft-sediment folding; minor sandstone, pale grey, thin to thick bedded, fine- to medium-grained; turbidites, micaceous; shale commonly with Middle-Late Ordovician graptolite faunas; deep marine hemipelagic deposits.||||||07-FEB-11
12668|Mount Easton Shale|64538|5|Briefly described|Map legend|Late Ordovician|Middle Ordovician|Black shale, thick-bedded, rarely with soft-sediment folding; minor sandstone, pale grey, thin to thick bedded, fine- to medium-grained; turbidites, micaceous; shale commonly with Middle-Late Ordovician graptolite faunas; deep marine hemipelagic deposits.||||||07-FEB-11
12668|Mount Easton Shale|64539|5|Briefly described|Map legend|Late Ordovician|Middle Ordovician|Black shale, thick-bedded, rarely with soft-sediment folding; minor sandstone, pale grey, thin to thick bedded, fine- to medium-grained; turbidites, micaceous; shale commonly with Late Ordovician graptolite faunas; deep marine hemipelagic deposits.||||||22-DEC-08
12668|Mount Easton Shale|64540|5|Briefly described|Map legend|Late Ordovician|Middle Ordovician|Black shale, thick-bedded, rarely with soft-sediment folding; minor sandstone, pale grey, thin to thick bedded, fine- to medium-grained; turbidites, micaceous; shale commonly with Late Ordovician graptolite faunas; deep marine hemipelagic deposits.||||||22-DEC-08
12668|Mount Easton Shale|64605|5|Briefly described|Map legend|Ordovician|Ordovician|Black shale, minor sandstone; deep-marine deposits. Bright to dark blue in RGB. Nonmagnetic.||||||17-NOV-08
12668|Mount Easton Shale|64606|5|Briefly described|Map Legend|Cambrian|Cambrian|Black shale, minor sandstone: deep-marine deposits. Bright to dark blue in RGB. Nonmagnetic.||||||
12668|Mount Easton Shale|64616|3|Fully described|p68, p155, p160, p163-166|Katian|Darriwilian|See also p170 Fig.6.17, p175, p179-187, p190-192, p197 Fig.6.34, p200-202, p212, p254, p278, p281, p283-286, p292, p295, p306. Disconformably overlies Wahroonga Breccia. Conformably overlain by Lazarini Siltstone. Thrust-faulted against Norton Gully Sandstone. Age well constrained by graptolites and other fossils - Darriwillian-Bolindian. Min ~650m thick. Dominantly thick-bedded black shale, bleached by weathering; thin beds of fine-grained micaceous sandstone; local phosphate deposits; abundant graptolites. Geophysical characteristics given.||||||16-FEB-17
12668|Mount Easton Shale|65715|5|Briefly described|p4 Tb.2|Ordovician|Ordovician|Formation rank. Called Mount Easton Beds by VandenBerg (1975).||||||
12668|Mount Easton Shale|65900|5|Briefly described|p161, 155, 158, 167, 171, 159 Table 1||Late Ordovician|Melbourne Zone. Upper Ordovician. Name written Mt in text.||||Overlain by Murrindindi Supergroup, Dargile Formation.|Thick sequence of marine clastic sediments.|10-MAY-12
12668|Mount Easton Shale|67802|5|Briefly described|p28|Late Ordovician|Late Ordovician|Throughout Melbourne Zone.|||||Black shales.|
12668|Mount Easton Shale|68116|5|Briefly described|Appendix, Maps 33-34, 43, 56-57.|Hirnantian|Dariwilian|Contains late Darriwilian to mid-Bolindian graptolite faunas.|||||Black shale, minor sandstone: shale thick-bedded, rarely with soft-sediment folding; sandstone pale grey, thin to thick-bedded, fine to medium-grained, minor turbidites, micaceous.|
12668|Mount Easton Shale|70629|6|Mentioned|p986|Late Ordovician|Late Ordovician|Melbourne Zone.||||||
12668|Mount Easton Shale|73186|6|Mentioned|p227, p229 Fig.2, p237|Katian|Sandbian|Melbourne Zone. ~650 m thick.|||||Pelitic black shale.|
25276|Mount Eccles Volcanics Complex|35891|5|Briefly described|p228|||||||||
25276|Mount Eccles Volcanics Complex|43112|6|Mentioned|p32|||||||||
12676|Mount Egbert Granite|23309|5|Briefly described|p438 App 1|Middle Devonian|Early Devonian|G337 S-Type. Age: 393 +/- 17 Ma. 392 +/- 5, 389 +/- 5 Ma, 375 +/- 18 Ma.||||||
12676|Mount Egbert Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
12676|Mount Egbert Granite|60452|4|Described|p55|Middle Devonian|Early Devonian|Medium-grained biotite granite. Appears to have intruded the Wedderburn Granite. Age: 399-382Ma. See also p28.||||||
12676|Mount Egbert Granite|60461|5|Briefly described|Map legend|Early Devonian|Early Devonian|Biotite granite: medium-grained; S-type.||||||06-OCT-04
12676|Mount Egbert Granite|60462|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Granite: reduced; moderately magnetic circular layer to 30 nT, elsewhere nonmagnetic; K, Th and U responses all high.||||||
12676|Mount Egbert Granite|65715|6|Mentioned|p8 Tb.4|||G337. Of Edwards et al (2001) p55.||||||
12676|Mount Egbert Granite|68116|5|Briefly described|Appendix, Map 16.|Early Devonian|Early Devonian||||||Biotite granite: medium grained; S-type; nonmagnetic with subsurface weakly magnetic phase.|
12676|Mount Egbert Granite|68189|6|Mentioned|p42 App.2|||Ages from Richards & Singleton (1981): Rb-Sr and K-Ar respectively. An intermediate age is also given.|396 +/- 2 and 388 +/- 6 Ma.|||||30-JUN-14
30232|Mount Egerton Granodiorite|23104|5|Briefly described|p543||Late Devonian|||||||
30232|Mount Egerton Granodiorite|23300|5|Briefly described|Map Legend|Devonian|Devonian|Of Mount Egeron Suite||||||
30232|Mount Egerton Granodiorite|23301|5|Briefly described|Map Legend|Devonian|Devonian|Mount is Mt. in text. Of Mount Egerton Suite||||||
30232|Mount Egerton Granodiorite|23302|5|Briefly described|Map Legend|Devonian|Devonian|Of Mount Egerton Suite||||||
30232|Mount Egerton Granodiorite|23303|5|Briefly described|Map Legend|Devonian|Devonian|Of Mount Egerton Suite||||||
30232|Mount Egerton Granodiorite|23304|5|Briefly described|Map Legend|Devonian|Devonian|Of Mount Egerton Suite||||||
30232|Mount Egerton Granodiorite|23305|4|Described|p46. Table 6, 7||Late Devonian|of White and Chappell (1988) and defined by Taylor et al. (1996). Age: K/Ar - 355+/-4 Ma. Of Mount Egerton Suite. Central Victorian Magmatic Province.||||||
30232|Mount Egerton Granodiorite|23309|5|Briefly described|p438 App1|Early Carboniferous|Late Devonian|G280 I-Type. Age: 355 +/- 4 Ma.||||||
30232|Mount Egerton Granodiorite|24383|6|Mentioned|p29 Fig.9B|||Parent: Mount Egerton Suite. Geological Province: Lachlan Fold Belt||||||
30232|Mount Egerton Granodiorite|24384|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Mount Egerton Suite.||||||
30232|Mount Egerton Granodiorite|24385|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Mount Egerton Suite.||||||
30232|Mount Egerton Granodiorite|24386|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Mount Egerton Suite. Biotite granodiorite, pale grey, fine- to coarsely-grained; occasionally porphyritic in feldspar.||||||01-JUL-13
30232|Mount Egerton Granodiorite|24387|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Mount Egerton Suite. Biotite granodiorite; pale grey, fine- to coarse-grained; occasionally porphyritic in feldspar.||||||01-JUL-13
30232|Mount Egerton Granodiorite|24388|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Mount Egerton Suite.   Age:355+/-4Ma (K/Ar).   Subsurface biotite granodiorite; reduced I-type; nonmagnetic, low gravity response.||||||
30232|Mount Egerton Granodiorite|24438|5|Briefly described|p4, p14, p22, p32|Late Devonian|Late Devonian|Radiometric response probably due to discontinuous thin layer of colluvium derived from adjacent basalt plain|||||granitic bedrock|
30232|Mount Egerton Granodiorite|24551|6|Mentioned|p218, 722 Table 8.5|||||||||
30232|Mount Egerton Granodiorite|60581|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Mount Egerton Suite.||||||
30232|Mount Egerton Granodiorite|60582|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Mount Egerton Suite.||||||
30232|Mount Egerton Granodiorite|60583|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Mount Egerton Suite.||||||
30232|Mount Egerton Granodiorite|60584|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Mount Egerton Suite.||||||
30232|Mount Egerton Granodiorite|60585|4|Described|p23, p24|Late Devonian|Late Devonian|G280. Of the Mount Egerton Suite. Medium to coarse grained, pale grey; reduced I-type; biotite granodiorite transitional to adamellite.||||||
30232|Mount Egerton Granodiorite|65715|5|Briefly described|p7 Tb.4|||Of Mount Egerton Suite. G280. Called Gong Gong-Lal Lal Cupola by Yates (1954). Gong Gong Granodiorite of White and Chappell (1988) included in Mount Egerton Granodiorite by Taylor et al. (1995). Lal Lal Granodiorite included by VandenBerg (1997).||||||
30232|Mount Egerton Granodiorite|68116|5|Briefly described|Appendix, Maps 40-41.|Late Devonian|Late Devonian||||||Biotite granodiorite: pale grey; fine to coarse-grained, occasionally feldspar-phyric; mafic microgranular enclaves and mineral clots; nonmagnetic; fresh to kaolinised.|
12677|Mount Egerton Suite|23300|5|Briefly described|Map Legend|Devonian|Devonian|||||||
12677|Mount Egerton Suite|23301|5|Briefly described|Map Legend|Devonian|Devonian|||||||
12677|Mount Egerton Suite|23302|5|Briefly described|Map Legend|Devonian|Devonian|||||||
12677|Mount Egerton Suite|23303|5|Briefly described|Map Legend|Devonian|Devonian|||||||
12677|Mount Egerton Suite|23304|5|Briefly described|Map Legend|Devonian|Devonian|||||||
12677|Mount Egerton Suite|23305|5|Briefly described|p46||Late Devonian|Similar to Beckworth Suite. Central Victorian Magmatic Province.||||||
12677|Mount Egerton Suite|24383|6|Mentioned|p40 Fig.17|||Geological Province: Lachlan Fold Belt||||||
12677|Mount Egerton Suite|24384|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes Mount Egerton Granodiorite.||||||
12677|Mount Egerton Suite|24385|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes the Mount Egerton Granodiorite.||||||
12677|Mount Egerton Suite|24386|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes the Mount Egerton Granodiorite.||||||
12677|Mount Egerton Suite|24387|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes the Mount Egerton Granodiorite.||||||
12677|Mount Egerton Suite|24388|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes the Mount Egerton Granodiorite.||||||
12677|Mount Egerton Suite|24551|6|Mentioned|p228|||||||||
12677|Mount Egerton Suite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
12677|Mount Egerton Suite|42827|6|Mentioned|p433|||||||||
12677|Mount Egerton Suite|60581|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Includes: Mount Egerton Granodiorite.||||||
12677|Mount Egerton Suite|60582|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Includes the Mount Egerton Granodiorite.||||||
12677|Mount Egerton Suite|60583|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Includes: Mount Egerton Granodiorite.||||||
12677|Mount Egerton Suite|60584|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Includes: Mount Egerton Granodiorite.||||||
12677|Mount Egerton Suite|60585|5|Briefly described|p23|Late Devonian|Late Devonian|Includes the Mount Egerton Granodiorite and the Gong Gong Granodiorite.||||||
12677|Mount Egerton Suite|65715|5|Briefly described|p7 Tb.4|||Includes Mount Egerton Granodiorite.||||||
12677|Mount Egerton Suite|66012|6|Mentioned|p12|||| | | | | |13-JUN-13
12682|Mount Eliza Granodiorite|23274|6|Mentioned|p446||Late Devonian|Written: Mt Eliza Granodiorite||||||
12682|Mount Eliza Granodiorite|23309|6|Mentioned|p438 App 1|||G264 I-Type. Supersedes Mount Eliza Granite.||||||
12682|Mount Eliza Granodiorite|24551|6|Mentioned|p717 Table 2.4|Late Devonian|Late Devonian|Age: 363 +/- 2Ma, 362 +/- 2Ma.||||||
12682|Mount Eliza Granodiorite|31080|6|Mentioned|p48|||||||||
12682|Mount Eliza Granodiorite|31510|5|Briefly described|p10|||See also Table 1||||||
12682|Mount Eliza Granodiorite|35290|5|Briefly described|p22|||See also P20.||||||
12682|Mount Eliza Granodiorite|35712|6|Mentioned|Table 6|||||||||
12682|Mount Eliza Granodiorite|68116|5|Briefly described|Appendix, Map 51.|Late Devonian|Late Devonian||||||Biotite granodiorite: grey, equigranular; contains quartz, plagioclase, orthoclase, biotite, minor hornblende and accesory sphene, allanite and ilmenite; I-type.|
12682|Mount Eliza Granodiorite|71205|5|Briefly described|p215|||Refers to Keble(1950).||||||
34812|Mount Elizabeth Caldera Complex|22968|4|Described|P15, P130, P213||Early Devonian|Includes the Saint Patricks Creek Granite.  All contacts are faulted||||||
34812|Mount Elizabeth Caldera Complex|23020|5|Briefly described|Map legend|Early Devonian|Early Devonian|Overlying unit is Snowy River Volcanics, unconformably overlies the Dead Bird Suite||||||
34812|Mount Elizabeth Caldera Complex|23021|5|Briefly described|Map legend|Pragian|Lochkovian|||||||
34812|Mount Elizabeth Caldera Complex|23028|5|Briefly described|Map legend|Pragian|Lochkovian|||||||
34812|Mount Elizabeth Caldera Complex|23029|5|Briefly described|Map legend|Pragian|Lochkovian|||||||
34812|Mount Elizabeth Caldera Complex|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
34812|Mount Elizabeth Caldera Complex|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
34812|Mount Elizabeth Caldera Complex|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian||||||Ignimbrite.|
34812|Mount Elizabeth Caldera Complex|60542|6|Mentioned|p96|||Surrounded by the ring dyke of Saint Patricks Creek Granite. ||||||
34812|Mount Elizabeth Caldera Complex|68115|5|Briefly described|p5.|Devonian|Devonian|The Fainting Range Ignimbrite was moved into this unit by Willman et al. (1999) from the Tara Range Subgroup, a distinct entity (Simpson et al. 1996).|||Includes Fainting Range Ignimbrite.|||
34812|Mount Elizabeth Caldera Complex|68116|5|Briefly described|Appendix, Maps 35, 44.|Early Devonian|Early Devonian||||||Rhyolite: aphyric to sparsely porphyritic; massive to flow-banded; fine sugary texture where weathered; small phenocrysts of quartz, feldspar, altered biotite.|
12687|Mount Elizabeth Granodiorite|22968|5|Briefly described|P66, P214||Early Devonian|Highly magnetic, parent is Mount Elizabeth Caldera Complex||||||
12687|Mount Elizabeth Granodiorite|23021|5|Briefly described|Map legend|Pragian|Lochkovian|Parent is Mount Elizabeth Caldera Complex.||||||
12687|Mount Elizabeth Granodiorite|23028|5|Briefly described|Map legend|Pragian|Lochkovian|Parent is Mount Elizabeth Caldera Complex.||||||
12687|Mount Elizabeth Granodiorite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Mount Elizabeth Caldera Complex.||||||
12687|Mount Elizabeth Granodiorite|23309|5|Briefly described|p123, 134, 343.|||G126 I-Type.||||||
12687|Mount Elizabeth Granodiorite|24551|5|Briefly described|p151|||Included in the Mount Elizabeth Cauldron Complex.||||||
12687|Mount Elizabeth Granodiorite|38367|6|Mentioned|Table 3|||||||||
12687|Mount Elizabeth Granodiorite|42110|6|Mentioned|Fig.1 P120|||||||||
12687|Mount Elizabeth Granodiorite|43284|5|Briefly described|Map Legend||Early Devonian|||||||
12687|Mount Elizabeth Granodiorite|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|I-type. Written as Mt Elizabeth Granodiorite on legend.||||||
12687|Mount Elizabeth Granodiorite|68116|5|Briefly described|Appendix, Maps 35, 44.|Early Devonian|Early Devonian||||||Hornblende-biotite granodiorite: green-grey; fine-grained; with acicular to tabular hornblende.|
41883|Mount Elliot volcanics|60451|6|Mentioned|p50 Fig. 21|||||||||
69712|Mount Emu Granodiorite|61163|5|Briefly described|p121, p37 Tb. 6.2, p130|Early Devonian|Early Devonian|Mod.-sized pluton intruding Cobbannah Gp. - as a larger southern body and a smaller northern body. Ranges from granite to tonalite with biotite and hornblende in most samples; most is porphyritic; I-type. Geol Prov: LFB. See also Mount Emu granodiorite.||||||
69712|Mount Emu Granodiorite|61174|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende granite, granodiorite, tonalite: grey; coarse-grained; porphyritic, with phenocrysts of plagioclase, quartz, rare orthoclase; fine-grained near the margin. I-type intrusion. GSV map code: G162.||||||07-FEB-11
69712|Mount Emu Granodiorite|61175|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende granite, granodiorite, tonalite: grey; coarse-grained; porphyritic, with phenocrysts of plagioclase, quartz, rare orthoclase; fine-grained near the margin. I-type intrusion. GSV map code: G162.||||||
69712|Mount Emu Granodiorite|61176|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende granite, granodiorite, tonalite: grey; coarse-grained; porphyritic, with phenocrysts of plagioclase, quartz, rare orthoclase; fine-grained near the margin. I-type intrusion. GSV map code: G162.||||||
69712|Mount Emu Granodiorite|61177|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende granite, granodiorite, tonalite: grey; coarse-grained; porphyritic, with phenocrysts of plagioclase, quartz, rare orthoclase; fine-grained near the margin. I-type intrusion. GSV map code: G162.||||||
69712|Mount Emu Granodiorite|61178|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende granite, granodiorite, tonalite (I-type): nonmagnetic in N, broad moderate high in S; gravity low in N and high in S; low to moderate total radioelement, K, U and Th in N, low Th in S; surrounded by hornfels ridges. GSV map code: G162.||||||
69712|Mount Emu Granodiorite|66012|3|Fully described|p10 Tb.1, p11 Tb.2, p11-15|Devonian|Devonian|[These comments relate to the former Mount Emu Granite near Ballarat, later included in Tiac Granite]. Of Beckworth Suite. Coarse-grained, equigranular biotite granite. Intrudes Saint Arnaud Group. Intruded by Mount Bute Granite and possibly Lismore Granodiorite. Crops out as pavements and boulders on a series of monadnocks and small hills N of Pittong.|360+/-5Ma K/Ar Richards & Singleton (1981).| | | | |16-FEB-15
69712|Mount Emu Granodiorite|68116|5|Briefly described|Appendix, Map 26.|Early Devonian|Early Devonian||||||Biotite-hornblende granite, granodiorite, tonalite: grey; coarse-grained; porphyritic, with phenocrysts of plagioclase, quartz, rare orthoclase; fine-grained near the margin.|
12701|Mount Evelyn Rhyodacite|23268|6|Mentioned|Fig14-2.1p388, Fig14-2.2(b)p389||Devonian|Written: Mt Evelyn Rhyodacite.||||||
12701|Mount Evelyn Rhyodacite|23269|4|Described|p402-4, Fig14-3.3p405||Late Devonian|Written: Mt Evelyn Rhyodacite||||||
12701|Mount Evelyn Rhyodacite|23309|5|Briefly described|p166 Tb 2.62|||||||||
12701|Mount Evelyn Rhyodacite|29652|6|Mentioned|Table 4|||||||||
12701|Mount Evelyn Rhyodacite|29653|6|Mentioned|p4|||||||||
12701|Mount Evelyn Rhyodacite|30867|6|Mentioned|Fig.2|||Refers Garratt,Gill,Vandenberg & Williams.||||||
12701|Mount Evelyn Rhyodacite|33157|4|Described|p40|||See also P41||||||
12701|Mount Evelyn Rhyodacite|33598|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
12701|Mount Evelyn Rhyodacite|33599|4|Described|p8|||Dev.||||||
12701|Mount Evelyn Rhyodacite|34956|5|Briefly described|p82|||||||||
12701|Mount Evelyn Rhyodacite|35012|5|Briefly described|p430|||||||||
12701|Mount Evelyn Rhyodacite|35277|4|Described|p93|||||||||
12701|Mount Evelyn Rhyodacite|39291|6|Mentioned|Fig.13|||||||||
12701|Mount Evelyn Rhyodacite|41641|4|Described|p163|||||||||
12701|Mount Evelyn Rhyodacite|42827|4|Described|p163|||of Mount Dandenong Volcanics||||||
12701|Mount Evelyn Rhyodacite|44197|5|Briefly described|Map Legend||Late Devonian|||||||
12701|Mount Evelyn Rhyodacite|60083|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Mount Dandenong Volcanics Group.  Rhyodacite, rhyolite, tuff; often fragmented.||||||
12701|Mount Evelyn Rhyodacite|68116|5|Briefly described|Appendix, Map 42.|Late Devonian|Late Devonian|||||Contains lithic fragments of bedrock and Coldstream Rhyolite.|Rhyolite to rhyodacite ignimbrite: welded; phenocryst-rich with gradation from quartz rich to more abundant oligoclase and orthoclase, and plagioclase on top. Uppermost part is a thin band of volcanigenic sediments.|
12720|Mount Fraser basalt|41895|6|Mentioned|p80|||||||||
27504|Mount Ida Formation|5252|5|Briefly described|p66, p81, p86.|Lochkovian|Lochkovian|Quartz-rich, clastic. Unit 3 dated as early Gedinnian. Heathcote district, VIC.||||||
27504|Mount Ida Formation|13996|6|Mentioned|p144|||Heathcote district. Contains a few Pridoli trilobites; not determinable to generic level.||||||
27504|Mount Ida Formation|22628|6|Mentioned|fig1p108|Devonian|Devonian|Spelt "Mt" in the text.||||||14-APR-08
27504|Mount Ida Formation|22708|5|Briefly described|p210|Early Devonian|Early Devonian|||||||
27504|Mount Ida Formation|22886|6|Mentioned|p13|||||||||
27504|Mount Ida Formation|23229|5|Briefly described|Table3-3p26|Pragian|Lochkovian|||||||
27504|Mount Ida Formation|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
27504|Mount Ida Formation|23309|4|Described|Table 2.49, p135, 138, 148-155, 245, 385|Early Devonian|Silurian|Consists of Cornella, Dealba and Stoddart Members.||||||
27504|Mount Ida Formation|23522|5|Briefly described|p246|Middle Devonian|Early Devonian|||||||
27504|Mount Ida Formation|24019|6|Mentioned|p362, p373|Lochkovian|Lochkovian|Mount is Mt in text.||||||16-MAR-05
27504|Mount Ida Formation|24177|4|Described|p54, p50 Fig.22|Lochkovian|Lochkovian|Includes the Cornella, Dealba and Stoddart Members (Edwards et al 1998). Overlies the McIvor Sandstone. Geological Province: Darraweit Guim Province.||||||
27504|Mount Ida Formation|24328|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
27504|Mount Ida Formation|24329|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes the Stoddart, Dealba and Cornella Members.||||||27-OCT-08
27504|Mount Ida Formation|24551|5|Briefly described|p120, p123|||||||||
27504|Mount Ida Formation|29889|6|Mentioned|p137|||||||||
27504|Mount Ida Formation|30075|6|Mentioned|p11|||||||||
27504|Mount Ida Formation|31161|5|Briefly described|PA10|||||||||
27504|Mount Ida Formation|31654|6|Mentioned|Map legend|Gedinnian|Gedinnian|||||||
27504|Mount Ida Formation|31852|6|Mentioned|p720|||See alsoo P721||||||
27504|Mount Ida Formation|32074|5|Briefly described|p180|||||||||
27504|Mount Ida Formation|32305|5|Briefly described|p164|||||||||
27504|Mount Ida Formation|32986|6|Mentioned|p35|||Refers Talent (1965)||||||
27504|Mount Ida Formation|33238|6|Mentioned|p642|||||||||
27504|Mount Ida Formation|33326|6|Mentioned|p431|||Fauna.||||||
27504|Mount Ida Formation|33394|5|Briefly described|p75|||||||||
27504|Mount Ida Formation|33602|6|Mentioned|Fig.2|||||||||
27504|Mount Ida Formation|33732|5|Briefly described|p105|||||||||
27504|Mount Ida Formation|34346|6|Mentioned|p6|||See also P7. Gedinnian or Siegenian.||||||
27504|Mount Ida Formation|35112|6|Mentioned|Fig.9|||||||||
27504|Mount Ida Formation|35283|3|Fully described|p53|||||||||
27504|Mount Ida Formation|36214|6|Mentioned|p62|||||||||
27504|Mount Ida Formation|36775|6|Mentioned|p366|||||||||
27504|Mount Ida Formation|37013|6|Mentioned|p39|||||||||
27504|Mount Ida Formation|37727|6|Mentioned|p71|||||||||
27504|Mount Ida Formation|38208|5|Briefly described|p1741|||Palaeontology||||||
27504|Mount Ida Formation|38378|5|Briefly described|p133|||||||||
27504|Mount Ida Formation|38787|6|Mentioned|p124|||||||||
27504|Mount Ida Formation|39331|5|Briefly described|p17|||||||||
27504|Mount Ida Formation|39886|6|Mentioned|p439|||||||||
27504|Mount Ida Formation|41585|4|Described|p111|||||||||
27504|Mount Ida Formation|41637|6|Mentioned|p207|||||||||
27504|Mount Ida Formation|42033|6|Mentioned|p650|||||||||
27504|Mount Ida Formation|42790|5|Briefly described|Fig.8 P183|||||||||
27504|Mount Ida Formation|43202|6|Mentioned|p17|||||||||
27504|Mount Ida Formation|43461|14|Not recorded|p628|||||||||
27504|Mount Ida Formation|43547|14|Not recorded|p148,Tb p152,157,159|Siegenian|Gedinnian|||||||
27504|Mount Ida Formation|43871|14|Not recorded|p1-55||Early Devonian|Fauna||||||
27504|Mount Ida Formation|48971|6|Mentioned|p30|||||||||
27504|Mount Ida Formation|60591|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Includes: Cornella Member, Dealba Member, Stoddart Member.||||||
27504|Mount Ida Formation|60592|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Includes: Cornella Member, Dealba Member, Stoddart Member.||||||
27504|Mount Ida Formation|60593|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Includes: Cornella Member, Dealba Member, Stoddart Member.||||||
27504|Mount Ida Formation|60595|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Includes: Cornella Member, Dealba Member, Stoddart Member.||||||
27504|Mount Ida Formation|60596|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Includes: Cornella Member, Dealba Member, Stoddart Member.||||||
27504|Mount Ida Formation|60597|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Weakly magnetic, moderate K and Th, high U.||||||27-OCT-08
27504|Mount Ida Formation|60599|3|Fully described|p14, p24 Tb. 4, p60-61, p83, p106|Early Devonian|Early Devonian|Supersedes Mount Ida Beds. Includes: Stoddart, Dealba and Cornella Members - broadly corresponding to the divisions of Thomas (1937) in his Mount Ida Beds. Conformable over McIvor Sandstone. Thickness: ~ 2100m. Mount may be Mt in text.||||||27-OCT-08
27504|Mount Ida Formation|61185|5|Briefly described|p14, p21 Fig. 6, p23|Pragian|Lochkovian|Includes: Cornella, Dealba and Stoddart Members. Near shore shallow water deposits. Eqivalent to Humevale Siltstone. Geological Province: Lachlan Fold Belt, Melbourne Zone. Mount may be Mt in text.||||||07-FEB-11
27504|Mount Ida Formation|61187|5|Briefly described|p5 Fig.3.|Early Devonian|Late Silurian|Melbourne Zone, Melbourne Terrane. Correlative of Enano and Wombat Creek Groups, Buchan and Mallacoota Zones, Benambra Terrane. ||||||
27504|Mount Ida Formation|62469|5|Briefly described|p5 Fig. 2, p6, p16|Lochkovian|Ludlow|Medium to coarse sandstones. Geological Province: Darraweit Guim Province. Mount is Mt in text.||||||12-FEB-15
27504|Mount Ida Formation|62735|6|Mentioned|p987|Lochkovian|Lochkovian|Contains scutellum fossils.  In Victoria.||||||
27504|Mount Ida Formation|63083|6|Mentioned|p252|Early Devonian|Early Devonian|Records acastid fossils. Mount is Mt in text.||||||07-FEB-11
27504|Mount Ida Formation|64612|6|Mentioned|p27|Late Ludlow|Late Ludlow|||||||07-FEB-11
27504|Mount Ida Formation|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Heathcote. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
27504|Mount Ida Formation|65969|6|Mentioned|p15, p17 Fig.7|Devonian|Devonian|Tabberabberan folds in this unit are truncated by the Mount William Fault.||||||
27504|Mount Ida Formation|68116|5|Briefly described|Appendix, Map 24.|Lochkovian|Pridoli||||||Sandstone, mudstone, conglomerate; marginal marine deposits.|
27504|Mount Ida Formation|68298|5|Briefly described|p220|Lochkovian|Lochkovian|Includes Acanthodian spines reported by Neil (1981).||||||
27504|Mount Ida Formation|69089|5|Briefly described|Map legend|Early Devonian|Early Devonian||||||Marine: sandstone, off-white; siltstone, minor conglomerate.|
27504|Mount Ida Formation|70487|6|Mentioned|p7, p10, p11 Fig.5|Lochkovian|Llandovery|Some correlation with trilobite fauna found in Puckapunyal Formation. Some corals resemble those in Flowerdale Member.|||Stoddart Member|Stoddart Member.|Fossiliferous strata.|
27504|Mount Ida Formation|70904|4|Described|p 34|||||||||
27504|Mount Ida Formation|70933|14|Not recorded|p94|||Stratigraphy.||||||
27504|Mount Ida Formation|73497|5|Briefly described|Map legend|Devonian|Devonian|Marine.||Murrindindi Supergroup|||Mudstone, shale, sandstone, conglomerate: weakly magnetic; moderate K and Th, and high U.|
37763|Mount Jack Granite|23309|6|Mentioned|p438, Appendix 1|||G506, S-Type.||||||
37763|Mount Jack Granite|68116|5|Briefly described|Appendix, Map 45.|Wenlock|Llandovery||||||Biotite-muscovite granodiorite: with cordierite, garnet; medium-grained; foliated with numerous schistose enclaves; S-type.|
75952|Mount Jim Volcanic Group|68115|5|Briefly described|p9.|Cenozoic|Cenozoic|New name, after Mount Jim on the Bogong High Plains. Includes former Older Volcanic Group basalt flows on the Bogong High Plains, Dinner Plain area, Mount Hotham area and Dargo High Plains: all potentially one originally continuous sheet of basalt. Largely coincident with the Bogong Subprovince of Price et al. (2003).|||||Flows, plugs and dykes of alkali olivine basalt, basanite, picrobasalt, olivine nephelinite and phonolite, with minor interbedded lacustrine and fluvial siltstone, shale, gravel, peat and coal.|
75952|Mount Jim Volcanic Group|68116|5|Briefly described|Appendix, Maps 27, 35.|Oligocene|Priabonian||||||Basaltic lava flows: alkali olivine basalt, basanite, picrobasalt, olivine nephelinite, phonolite; olivine phenocrysts are common; minor interbedded lacustrine and fluvial sedimentary rocks including siltstone, shale, gravel, peat and coal.|
12867|Mount Kent Conglomerate|23309|4|Described|p169-183, Table 2.68|Frasnian|Frasnian|Of Mansfield Group. Maximum thickness: 340m.  Geological Province: Wobonga Caldera/ Howitt Province.||||||
12867|Mount Kent Conglomerate|23329|6|Mentioned|1048|||||||||
12867|Mount Kent Conglomerate|24551|5|Briefly described|p88 Fig. 3.15, 178|Late Devonian|Late Devonian|Of Mansfield Group.  Maximum Thickness: 600m.  Overlies: Wellington Rhyolite.  ||||||
12867|Mount Kent Conglomerate|31706|6|Mentioned|p645|||Devonian correlation chart||||||
12867|Mount Kent Conglomerate|32399|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
12867|Mount Kent Conglomerate|33602|6|Mentioned|p21|||||||||
12867|Mount Kent Conglomerate|33603|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
12867|Mount Kent Conglomerate|33607|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
12867|Mount Kent Conglomerate|35073|6|Mentioned|p24|||See also Table 5.||||||
12867|Mount Kent Conglomerate|35112|6|Mentioned|p280|||||||||
12867|Mount Kent Conglomerate|35277|3|Fully described|p102|||||||||
12867|Mount Kent Conglomerate|37330|5|Briefly described|p19|||||||||
12867|Mount Kent Conglomerate|38367|6|Mentioned|p108|||||||||
12867|Mount Kent Conglomerate|40761|5|Briefly described|p237|||||||||
12867|Mount Kent Conglomerate|40995|6|Mentioned|p370|||||||||
12867|Mount Kent Conglomerate|41641|4|Described|p172|||||||||
12867|Mount Kent Conglomerate|42827|5|Briefly described|p172|||||||||
12867|Mount Kent Conglomerate|43461|14|Not recorded|Table p625|Early Carboniferous|Late Devonian|||||||
12867|Mount Kent Conglomerate|43547|14|Not recorded|Table p153||Famennian|Part of Avon River Group.||||||11-JAN-07
12867|Mount Kent Conglomerate|44185|5|Briefly described|Map legend.|Late Devonian|Late Devonian|||Unit in Avon River Group.|||Fluvial: conglomerate, sandstone.|
12867|Mount Kent Conglomerate|44187|5|Briefly described|Map Legend||Late Devonian|||||||
12867|Mount Kent Conglomerate|61161|5|Briefly described|p131-132, p76-77 Fig 6.1, p35|||Lower formation of Mansfield Group. Overlies Wellington Volcanic Group. Red sandstone, pebbly sandstone and microconglomerate. Non-magnetic. Max. thickness: 600m. GSV map code: Damk.||||||
12867|Mount Kent Conglomerate|61163|3|Fully described|p97, p36 Tb. 6.2|Late Devonian|Late Devonian|Of Mansfield Group (Avon Supergroup). Upward-fining sequence of mainly conglomerate rocks - lenticular and discontinuous. Overlain by Snowy Plains Formation; overlies Bennies Formation (Tolmie Igneous Complex). Thick: 500m Geol Prov: Lachlan Fold Belt.||||||
12867|Mount Kent Conglomerate|61169|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Mansfield Group and Avon Supergroup. Fluvial deposits: massive to crudely bedded conglomerate, pebbly sandstone, minor red mudstone; GSV map code: Damk.||||||
12867|Mount Kent Conglomerate|61170|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Mansfield Group and Avon Supergroup. Fluvial deposits: massive to crudely bedded conglomerate, pebbly sandstone, minor red mudstone; GSV map code: Damk.||||||07-FEB-11
12867|Mount Kent Conglomerate|61171|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Mansfield Group and Avon Supergroup. Fluvial deposits: massive to crudely bedded conglomerate, pebbly sandstone, minor red mudstone; GSV map code: Damk.||||||
12867|Mount Kent Conglomerate|61172|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Mansfield Group and Avon Supergroup. Fluvial deposits: massive to crudely bedded conglomerate, pebbly sandstone, minor red mudstone; GSV map code: Damk.||||||
12867|Mount Kent Conglomerate|61173|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Mansfield Group and Avon Supergroup. Conglomerate, sandstone, mudstone: moderate gravity response (-350 to -320 ums^-2); weakly magnetic (20 nT, K < 1 x10^-6 cgs); low K, moderate Th and U, low to moderate total radioelements; GSV map code: Damk.||||||
12867|Mount Kent Conglomerate|61174|5|Briefly described|map legend|Late Devonian|Late Devonian|Of the Mansfield Group. Conglomerate, pebbly sandstone, minor red mudstone. GSV map code: Damk.||||||07-FEB-11
12867|Mount Kent Conglomerate|61175|5|Briefly described|map legend|Late Devonian|Late Devonian|Of the Mansfield Group. Conglomerate, pebbly sandstone, minor red mudstone. GSV map code: Damk.||||||
12867|Mount Kent Conglomerate|61176|5|Briefly described|map legend|Late Devonian|Late Devonian|Of the Mansfield Group. Conglomerate, pebbly sandstone, minor red mudstone. GSV map code: Damk.||||||
12867|Mount Kent Conglomerate|61177|5|Briefly described|map legend|Late Devonian|Late Devonian|Of the Mansfield Group. Conglomerate, pebbly sandstone, minor red mudstone. GSV map code: Damk.||||||
12867|Mount Kent Conglomerate|61178|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Mansfield Group. Conglomerate, sandstone, minor mudstone (fluvial): nonmagnetic; low gravity (-530 ms^-2); very low total radioelement, K, Th and U. GSV map code: Damk.||||||
12867|Mount Kent Conglomerate|61329|5|Briefly described|p122|||Of Avon River Group. Geological Province: Gippsland Basin.||||||17-NOV-08
12867|Mount Kent Conglomerate|64010|5|Briefly described|p258 Fig.1, p259. |||||Of the Mansfield Group.||Is overlain by Snowy Plains Formation.||
12867|Mount Kent Conglomerate|64535|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Mansfield Gp (Avon Supergp).Conglom/pebbly sst/minor red mudst: conglom. is massive to crudely bedded, well sorted, forms large outcrops; clasts are rounded, mostly of sst.q'ztite; sst tabular,commonly with lg-scale x-bedding+channelled bases.Fluvial.||||||22-DEC-08
12867|Mount Kent Conglomerate|64536|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Mansfield Gp (Avon Supergp).Conglom/pebbly sst/minor red mudst: conglom. is massive to crudely bedded, well sorted, forms large outcrops; clasts are rounded, mostly of sst.q'ztite; sst tabular,commonly with lg-scale x-bedding+channelled bases.Fluvial.||||||07-FEB-11
12867|Mount Kent Conglomerate|64537|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Mansfield Gp (Avon Supergp).Conglom/pebbly sst/minor red mudst: conglom. is massive to crudely bedded, well sorted, forms large outcrops; clasts are rounded, mostly of sst.q'ztite; sst tabular,commonly with lg-scale x-bedding+channelled bases.Fluvial.||||||07-FEB-11
12867|Mount Kent Conglomerate|64538|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Mansfield Gp (Avon Supergp).Conglom/pebbly sst/minor red mudst: conglom. is massive to crudely bedded, well sorted, forms large outcrops; clasts are rounded, mostly of sst.q'ztite; sst tabular,commonly with lg-scale x-bedding+channelled bases.Fluvial.||||||07-FEB-11
12867|Mount Kent Conglomerate|64539|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Mansfield Gp (Avon Supergp).Conglom/pebbly sst/minor red mudst: conglom. is massive to crudely bedded, well sorted, forms large outcrops; clasts are rounded, mostly of sst.q'ztite; sst tabular,commonly with lg-scale x-bedding+channelled bases.Fluvial||||||
12867|Mount Kent Conglomerate|64540|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Mansfield Gp (Avon Supergp).Conglom/pebbly sst/minor red mudst: conglom. is massive to crudely bedded, well sorted, forms large outcrops; clasts are rounded, mostly of sst.q'ztite; sst tabular,commonly with lg-scale x-bedding+channelled bases.Fluvial.||||||22-DEC-08
12867|Mount Kent Conglomerate|64605|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Mount Kent Conglomerate (Avon Supergroup). Conglomerate, pebbly sandstobne, minor red mudstone; alluvial deposits. Speckled blue and red in RGB. Nonmagnetic.||||||
12867|Mount Kent Conglomerate|64606|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of Mansfield Group. Conglomerate, pebbly sandstone, minor red mudstone: alluvial deposits. Speckled blue and red in RGB. Nonmagnetic.||||||11-NOV-08
12867|Mount Kent Conglomerate|64616|4|Described|p137, p190, p279, p300|Early Carboniferous|Early Carboniferous|Basal conglomerate of Mansfield Group. Thin but extensive. Massive to crudely bedded polymictic conglomerate with interbeds of massive red pebbly sandstone; minor red mudstone. Unconformably overlies Wellington Volcanic Group, Highton Volcanics, Delatite Group. Gradational contact with overlying Snowy Plains Formation. 120-340m thick. Geophysical characteristics given.||||||
12867|Mount Kent Conglomerate|66252|5|Briefly described|p211-213 Figs.1-3, p214,  p216 Fig.6.|Late Devonian|Late Devonian|See also p222-223 Figs.8-9, p226-230. Written as Mt Kent Conglomerate throughout. Unit in Avon River Group. Overlies Howitt Spur Formation; is overlain by Snowy Plains Formation. Widespread succession of cobble conglomerate and pebbly sandstone. Thickness varies to maximum 200m. Imbrication indicates northwesterly directed palaeocurrents.||||||
12867|Mount Kent Conglomerate|68116|5|Briefly described|Appendix, Maps 26, 34-35, 43-44.|Famennian|Famennian||||||Conglomerate, pebbly sandstone, minor red mudstone: conglomerate massive to crudely bedded, well-sorted, generally pale, clasts rounded, mostly sandstone/quartzite; sandstone tabular, commonly with large-scale cross bedding and channeled bases.|
26764|Mount Leinster Igneous Complex|22487|6|Mentioned|p212 Fig. 13, p213|Jurassic|Triassic|Mount is Mt in text.||||||11-SEP-08
26764|Mount Leinster Igneous Complex|22968|5|Briefly described|P16, P33, P221||Late Triassic|Ages of unit are around 201-209 Ma||||||
26764|Mount Leinster Igneous Complex|23020|5|Briefly described|Map legend|Triassic|Triassic|Unconformably overlies the Buchan Group.||||||25-SEP-08
26764|Mount Leinster Igneous Complex|23021|5|Briefly described|Map legend|Triassic|Triassic|||||||
26764|Mount Leinster Igneous Complex|23028|5|Briefly described|Map legend|Triassic|Triassic|Unconformably and nonconformably overlies the Buchan Group.||||||25-SEP-08
26764|Mount Leinster Igneous Complex|23029|5|Briefly described|Map legend|Triassic|Triassic|Nonconformably overlain by the Older Volcanics.||||||25-SEP-08
26764|Mount Leinster Igneous Complex|23030|5|Briefly described|Map legend|Triassic|Triassic|||||||
26764|Mount Leinster Igneous Complex|23307|5|Briefly described|Map Legend|Triassic|Triassic|||||||
26764|Mount Leinster Igneous Complex|23309|5|Briefly described|p290|||||||||
26764|Mount Leinster Igneous Complex|23938|5|Briefly described|p31-32 Fig. 12|Triassic|Triassic|Intrusive: syenites, syenite and granite. See also p86-87 Figs. 32 and 33, p139 Tb. 1 Appendix. ||||||
26764|Mount Leinster Igneous Complex|24097|5|Briefly described|p14||Triassic|Alkaline rocks.  Geological Province: Lachlan Fold Belt.  Mount is Mt in text.||||||22-APR-05
26764|Mount Leinster Igneous Complex|24551|5|Briefly described|p242|Late Triassic|Middle Triassic|||||||
26764|Mount Leinster Igneous Complex|33603|6|Mentioned|Map legend|Triassic|Triassic|||||||
26764|Mount Leinster Igneous Complex|35112|6|Mentioned|Table 1|||||||||
26764|Mount Leinster Igneous Complex|35278|4|Described|p359|||||||||
26764|Mount Leinster Igneous Complex|37330|4|Described|p18|||||||||
26764|Mount Leinster Igneous Complex|41572|6|Mentioned|p19|||||||||
26764|Mount Leinster Igneous Complex|42827|5|Briefly described|p19|||||||||
26764|Mount Leinster Igneous Complex|43220|5|Briefly described|p11||Triassic|||||||
26764|Mount Leinster Igneous Complex|44184|5|Briefly described|Map Legend||Middle Triassic|||||||
26764|Mount Leinster Igneous Complex|44185|5|Briefly described|Map legend.|Triassic|Triassic||||||Intrusive: syenites, syenite porphyry, granite porphyry.|
26764|Mount Leinster Igneous Complex|60503|4|Described|p16, p31, p131|Triassic|Triassic|Trachyte, volcaniclastics, volcanogenic sediments, syenites and porphyritic granites. The volcanics are grouped into the Teapot Creek Formation, with trachytes grouped into the Little Mount Tambo Trachyte Member. See also Mount Leinster Complex. ||||||
26764|Mount Leinster Igneous Complex|60504|5|Briefly described|Map Legend|Triassic|Triassic|Includes: Teapot Creek Formation, Grand View Syenite, Percydale Granite, Mount Bung Bung Syenite, Beloka Gap Granite, Duggan Creek Granite, Mole Hill Syenite, MacFarlane Syenite, Brothers Syenite.||||||
26764|Mount Leinster Igneous Complex|60505|5|Briefly described|Map legend|Triassic|Triassic|Includes: Teapot Creek Formation, Grand View Syenite, Percydale Granite, Mount Bung Bung Syenite, Beloka Gap Granite, Duggan Creek Granite, Mole Hill Syenite, MacFarlane Syenite, Brothers Syenite.||||||20-OCT-04
26764|Mount Leinster Igneous Complex|60506|5|Briefly described|Map legend|Triassic|Triassic|Includes: Teapot Creek Formation, Grand View Syenite, Percydale Granite, Mount Bung Bung Syenite, Beloka Gap Granite, Duggan Creek Granite, Mole Hill Syenite, MacFarlane Syenite, Brothers Syenite.||||||
26764|Mount Leinster Igneous Complex|60507|5|Briefly described|Map Legend|Triassic|Triassic|Includes: Teapot Creek Formation, Grand View Syenite, Percydale Granite, Mount Bung Bung Syenite, Beloka Gap Granite, Duggan Creek Granite, Mole Hill Syenite, MacFarlane Syenite, Brothers Syenite.||||||
26764|Mount Leinster Igneous Complex|60508|5|Briefly described|Map legend|Triassic|Triassic|Includes: Grandview Syenite, Percydale Granite, Mount Bung Bung Syenite, Beloka Gap Granite, Duggan Creek Granite, Mole Hill Syenite, MacFarlance Syenite, Brothers Syenite.||||||
26764|Mount Leinster Igneous Complex|61163|5|Briefly described|p13|Triassic|Triassic|A-type granites. Geological Province: Lachlan Fold Belt (Omeo Zone).||||||
26764|Mount Leinster Igneous Complex|61187|6|Mentioned|p26 Fig.2, p29 Fig.4. |||||||||
26764|Mount Leinster Igneous Complex|62897|5|Briefly described|p125|Late Triassic|Middle Triassic|Includes intrusions, trachyte lavas and pyroclastics. Near Benambra. Mount is Mt in text. ||||||18-MAR-08
22430|Mount Lonarch Granite|23309|6|Mentioned|p438 App1|||G371 I-Type. Supersedes Mount Lonarch Adamellite and Ampitheatre Granodiorite.||||||
22430|Mount Lonarch Granite|24551|6|Mentioned|p228|||||||||
22430|Mount Lonarch Granite|66002|5|Briefly described|p7 Tb.5|||Of Glenlogie Suite. G371. Called Mount Lonarch Adamellite by Cayley and McDonald (1995)||||||
22430|Mount Lonarch Granite|68116|5|Briefly described|Appendix, Map 31.|Early Devonian|Early Devonian||||||Hornbende-biotite granite: pale grey, fine to medium grained.|
12918|Mount Martha Granodiorite|23274|5|Briefly described|p446, 456||Late Devonian|Written: Mt Martha Granodiorite||||||
12918|Mount Martha Granodiorite|23309|5|Briefly described|p343-347.|||G263 I-Type. Supersedes Mount Martha Granite.||||||
12918|Mount Martha Granodiorite|24551|6|Mentioned|p225, 721 Table 8.4|||||||||
12918|Mount Martha Granodiorite|31080|5|Briefly described|p48|||||||||
12918|Mount Martha Granodiorite|31510|5|Briefly described|p10|||See also Table 1||||||
12918|Mount Martha Granodiorite|34017|6|Mentioned|p2|||Palaeozoic.  See also PP3,8,12,14,18,20.||||||
12918|Mount Martha Granodiorite|35290|5|Briefly described|p21|||See also P20.||||||
12918|Mount Martha Granodiorite|35712|6|Mentioned|Table 6|||||||||
12918|Mount Martha Granodiorite|68116|5|Briefly described|Appendix, Maps 50-51.|Late Devonian|Late Devonian||||||Biotite granodiorite: grey, medium grained; consists of quartz, oligoclase, orthoclase (including microperthite), biotite and minor hornblende; I-type.|
12918|Mount Martha Granodiorite|71205|4|Described|p215|||||||||
12919|Mount Martha Sand Bed|33604|6|Mentioned|p21|||Stratigraphic diagram||||||
12919|Mount Martha Sand Bed|42827|5|Briefly described|p316|||actually spelt Mt Martha Sand Bed||||||
30563|Mount McLeod Tonalite|23309|5|Briefly described| p344|Early Devonian|Late Silurian|G65 I-Type.||||||
30563|Mount McLeod Tonalite|23615|3|Fully described|p159, p42|Early Devonian|Early Silurian|Mount is Mt in text. See also p203 App 1.||||||04-NOV-14
30563|Mount McLeod Tonalite|24551|6|Mentioned|p234|||||||||
30563|Mount McLeod Tonalite|43206|5|Briefly described|map legend||Wenlock|Hornblende-biotite tonalite: green to grey, medium grained; massive; very weathered.||||||08-SEP-04
30563|Mount McLeod Tonalite|44185|5|Briefly described|Map legend.|||I-type. Age uncertain: shown as SDg, ie Silurian-Devonian.||||||
30563|Mount McLeod Tonalite|68116|5|Briefly described|Appendix, Map 36.|Devonian|Silurian||||||Hornblende tonalite: medium grained, massive; green to grey; I-type.|
12938|Mount Mittamatite Granite|23309|5|Briefly described|p344, 350.||Early Devonian|G98 A-Type Age: 427+/-32Ma.||||||
12938|Mount Mittamatite Granite|24133|3|Fully described|p78|Early Devonian|Late Silurian|Intrudes the Corryong Granite.  Age: 418+/-32Ma.  Geological Province: Lachlan Fold Belt.||||||
12938|Mount Mittamatite Granite|24142|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
12938|Mount Mittamatite Granite|24143|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
12938|Mount Mittamatite Granite|24144|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
12938|Mount Mittamatite Granite|24145|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Geological Province: Lachlan Fold Belt||||||
12938|Mount Mittamatite Granite|29953|5|Briefly described|p3|||||||||
12938|Mount Mittamatite Granite|31800|6|Mentioned|p211|||||||||
12938|Mount Mittamatite Granite|35278|5|Briefly described|p358|||||||||
12938|Mount Mittamatite Granite|35283|6|Mentioned|p49|||||||||
12938|Mount Mittamatite Granite|37501|6|Mentioned|p413|||||||||
12938|Mount Mittamatite Granite|37727|6|Mentioned|p26|||||||||
12938|Mount Mittamatite Granite|39860|5|Briefly described|p21|||||||||
12938|Mount Mittamatite Granite|40328|6|Mentioned|p204|||||||||
12938|Mount Mittamatite Granite|42089|6|Mentioned|p19|||||||||
12938|Mount Mittamatite Granite|42726|5|Briefly described|map legend|Silurian||475.  Of the Mount Mittamatite Suite (Boggy Plain Supersuite).  Mount is Mt in map legend.||||||08-FEB-05
12938|Mount Mittamatite Granite|44184|5|Briefly described|Map Legend||Early Devonian|Shown as Mount Mittamatite I-type.||||||
12938|Mount Mittamatite Granite|45087|5|Briefly described|p28|||Chemical analyses.||||||
12938|Mount Mittamatite Granite|61187|6|Mentioned|pp15-16.|||Mentioned as possibly prospective for copper-gold mineralisation, although may be less prospective than NSW mineralisation, having formed on continental crust.||Unit in Boggy Plains Supersuite.||||
12938|Mount Mittamatite Granite|68116|5|Briefly described|Appendix, Map 20.|Middle Devonian|Early Devonian||||||Biotite-rare amphibole granite: pale pink, fine to medium grained; minor fine grained porphyritic granite pods; slightly pervasively altered; highly magnetic.|
12938|Mount Mittamatite Granite|70910|14|Not recorded|p52|||Itinerary.||||||
12957|Mount Napier Volcanic Complex|31006|4|Described|p167|||See also p168-174.||||||01-MAY-07
12972|Mount Nelse Schist|31800|5|Briefly described|p208|||||||||
12972|Mount Nelse Schist|39860|6|Mentioned|p6|||||||||
12972|Mount Nelse Schist|45087|5|Briefly described|p224|||See also p227, 233. Chem. analyses.||||||31-MAR-17
37764|Mount Norgate Granite|23309|6|Mentioned|p439 Appendix 1|||G255, S-Type. Supersedes South Point Granite.||||||
37764|Mount Norgate Granite|68116|5|Briefly described|Appendix.|Middle Devonian|Middle Devonian||||||Granite, S-type.|
34908|Mount Nugong Tonalite|22968|5|Briefly described|P175, P208|Early Devonian|Late Silurian|Type locality location given on P209, age of unit is 413+/-6 Ma, intensely magnetic, parent is Boggy Plain Supersuite||||||13-JUN-14
34908|Mount Nugong Tonalite|23021|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is Boggy Plain Supersuite||||||
34908|Mount Nugong Tonalite|23028|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is Boggy Plain Supersuite||||||
34908|Mount Nugong Tonalite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Boggy Plain Supersuite. G123a biotite-hornblende tonalite: I-type; intensely magnetic (600 nT); low K, Th, U. G123b hornblende granodiorite: I-type; highly magnetic (400 nT); low to moderate K, Th, U||||||14-SEP-04
34908|Mount Nugong Tonalite|23309|6|Mentioned|p439 App1|||G123 I-Type. Supersedes Mount Nugong Granite and Granodiorite.||||||
34908|Mount Nugong Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian|Informally subdivided into a granodiorite phase, consisting of granodiorite: medium grained with hornblende and biotite, and rare clinopyroxene; I-type.|||||Biotite-hornblende-clinopyroxene tonalite: grey; medium-grained; massive; equigranular; clinopyroxene rimmed by hornblende; occasional rounded mafic enclaves.|
13026|Mount Phillipa Member|23229|5|Briefly described|Table3-3p26, 29|Pridolian|Ludlow|Written: Mt Phillipa Member.||||||27-OCT-08
13026|Mount Phillipa Member|24177|5|Briefly described|p50 Fig.22|Pridolian|Pridolian|Of the Humevale Siltstone. Mount is Mt in text of figure. Geological Province: Darraweit Guim Province.||||||27-OCT-08
13026|Mount Phillipa Member|30931|6|Mentioned|Map legend|Silurian|Silurian|||||||
13026|Mount Phillipa Member|35283|6|Mentioned|p51|||||||||
13026|Mount Phillipa Member|38146|6|Mentioned|Map legend|Silurian|Silurian|||||||
13026|Mount Phillipa Member|41585|6|Mentioned|p109|||||||||
13026|Mount Phillipa Member|42033|6|Mentioned|p650|||||||||
13026|Mount Phillipa Member|42827|5|Briefly described|p109|||Same as Mount Phillipa Sandstone Member.||||||14-JAN-09
13026|Mount Phillipa Member|43547|14|Not recorded|p148|||Part of Humevale Formation.||||||27-OCT-08
13026|Mount Phillipa Member|60599|5|Briefly described|p47 Fig. 19, p56, p67|Pridolian|Pridolian|Considered by authors as part of Dargile Fm - unit 3 of former Dargile Beds (Thomas 1937)) - equiv. to Hylands Member (McIvor Sst)?. Geol.Prov: Darraweit Guim Province, Melbourne Zone, Lachlan Fold Belt. Overlain by Flowerdale Sandstone Member.||||||11-FEB-15
13026|Mount Phillipa Member|61185|5|Briefly described|p22, p21 Fig. 6, p23, p45|Pridolian|Ludlow|Formerly of Humevale Formation (Williams 1964) occuring at base with Clonbinane Sandstone Member. Now incorporated into Dargile Formation (Edwards et al. in prep). Geological Province: Lachlan Fold Belt, Melbourne Zone. Age: fauna indicate early Pridoli.||||||07-FEB-11
13026|Mount Phillipa Member|66244|5|Briefly described|pp2-3.|||Mapped in the Merriang Syncline. This article does not make clear of which Formation this unit was a Member; but it appears it is now part of the Humevale Siltstone. Lateral  equivalent of Broadford Formation in the Whittlesea area.||Unit in Humevale Siltstone.||Overlies Yan Yean Formation. Is overlain by Humevale Siltstone.|A thin sandy unit, with length along strike of 10 km.|
35534|Mount Pilot Granite|23234|6|Mentioned|p86|||Written: Mt Pilot Granite||||||
31480|Mount Pinnabar Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Mount Pinnabar Suite (Boggy Plain Supersuite).  Contains the Mount Pinnabar granite.  Mount is Mt in mal legend.||||||08-FEB-05
26770|Mount Puggaree Conglomerate Member|22878|5|Briefly described|p39|Late Devonian|Late Devonian|||||||
26770|Mount Puggaree Conglomerate Member|22879|5|Briefly described|map|Late Devonian|Late Devonian|Conglomerate, pebbly sandstone and coarse grained quartz sandstone, discontinuous unit up to 40m thick at base of formation.||||||13-JUN-14
26770|Mount Puggaree Conglomerate Member|22880|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Conglomerate, pebbly sandstone and coarse grained quartz sandstone, discontinuous unit up to 40m thick at base of formation.||||||13-JUN-14
26770|Mount Puggaree Conglomerate Member|23309|6|Mentioned|p182 Table 2.69|||||||||
26770|Mount Puggaree Conglomerate Member|24551|6|Mentioned|p189|||||||||
26770|Mount Puggaree Conglomerate Member|42627|5|Briefly described|Map legend|Late Devonian|Late Devonian|||||||
26770|Mount Puggaree Conglomerate Member|42647|4|Described|p33|||||||||
26770|Mount Puggaree Conglomerate Member|43314|5|Briefly described|Map Legend||Late Devonian|of Combyingbar Formation.||||||
26770|Mount Puggaree Conglomerate Member|43315|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Of the Combyingbar Formation. Massive or crudely bedded conglomerate, with interbedded red mudstone.||||||03-MAY-05
26770|Mount Puggaree Conglomerate Member|60541|4|Described|p58-59|Late Devonian|Late Devonian|Basal unit of Combyingbar Formation. Thin, discontinuous conglomerate, both matrix and clast supported. Max. thickness: 40m.||||||21-JUN-05
26770|Mount Puggaree Conglomerate Member|68116|6|Mentioned|Maps 36-37.|||Code Dxcp. Mentioned in the legend for Maps 36-37 but does not appear on the maps; nor in the Appendix.||||||
13052|Mount Raymond Granite|23309|5|Briefly described| p314|||G43 - I-Type||||||
13052|Mount Raymond Granite|24551|6|Mentioned|p235|||||||||
13052|Mount Raymond Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
13052|Mount Raymond Granite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|I-type. Foliated, medium grained hornblende (reibeckite) biotite granite.||||||22-OCT-04
13052|Mount Raymond Granite|43315|5|Briefly described|Map Legend|Wenlock|Wenlock|I-type granite. Foliated, medium-grained hornblende (reibeckite) biotite granite.||||||03-MAY-05
13052|Mount Raymond Granite|60541|4|Described|p74|Silurian|Silurian|Intrusive within the Kuark Metamorphic Complex. A-type due to alkalinity, but this is debatable because petrography /geochemistry indicates alteration.... .  Age is Middle Silurian. See also p16 (and p18 Tb. 1 - presented only as Mt Raymond).||||||12-JAN-06
13052|Mount Raymond Granite|68116|5|Briefly described|Appendix, Map 45.|Early Devonian|Early Devonian||||||Riebeckite-biotite granite: medium-grained; foliated; I-type intrusive.|
13052|Mount Raymond Granite|71206|6|Mentioned|p373|||Lachlan Fold Belt.|||||Aluminous A-type granite.|
77888|Mount Robertson Diorite|68116|5|Briefly described|Appendix, Map 33.|Late Devonian|Late Devonian||||||Quartz-enstatite diorite: medium to fine-grained; mesocratic slightly greenish; andesine with occasionally zoned augite and enstatite; some alteration of enstatite to hornblende; interstitial cloudy orthoclase and quartz.|13-JUN-14
28811|Mount Samaria Volcanics|32074|6|Mentioned|p90|||Map legend. U. Devonian||||||
28811|Mount Samaria Volcanics|35277|6|Mentioned|Fig.5.8|||||||||
28811|Mount Samaria Volcanics|41641|6|Mentioned|Fig.5.8|||||||||
28811|Mount Samaria Volcanics|70933|14|Not recorded|p91|||Geological map.||||||
13093|Mount Selwyn Granite|22971|5|Briefly described|p 30|||Mount is Mt in text.||||||27-NOV-08
13093|Mount Selwyn Granite|23309|5|Briefly described| p343|||G158 I-Type||||||
13093|Mount Selwyn Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|Variation on Selwyn Granite?||||||
13093|Mount Selwyn Granite|44187|5|Briefly described|Map Legend||Early Devonian|G158 Unassigned. Shown as Mount Selwyn only.||||||27-NOV-08
13093|Mount Selwyn Granite|68116|5|Briefly described|Appendix, Map 34.|Early Devonian|Early Devonian||||||Biotite granodiorite with some tonalite and quartz diorite; hornblende present in most rock types.|
26771|Mount Singapore Granite|23309|6|Mentioned|p439 App1|||G257 S-Type.||||||
26771|Mount Singapore Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
26771|Mount Singapore Granite|68116|5|Briefly described|Appendix, Map 57.|Middle Devonian|Middle Devonian||||||Cordierite-biotite granite: medium to coarse grained, creamy grey; contains red-brown biotite and garnet; S-type.|
27848|Mount Sisters Porphyry|38145|6|Mentioned|Map legend|Triassic|Triassic|||||||
27848|Mount Sisters Porphyry|39447|4|Described|p18|||||||||
28812|Mount Stanley Granite|22971|5|Briefly described|p 33|||||||||
28812|Mount Stanley Granite|23309|5|Briefly described| p288, 298||Early Devonian|G183 I-Type.||||||
28812|Mount Stanley Granite|24551|6|Mentioned|p229|||Of the Tabberabbera Province.||||||
28812|Mount Stanley Granite|31713|5|Briefly described|p14|||||||||
28812|Mount Stanley Granite|38879|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Middle to Lower Devonian||||||
28812|Mount Stanley Granite|42726|5|Briefly described|map legend|||||||||
28812|Mount Stanley Granite|61163|6|Mentioned|p170|||||||||
28812|Mount Stanley Granite|68116|5|Briefly described|Appendix, Map 19.|Early Devonian|Early Devonian||||||Biotite granite: pinkish, medium grained, equigranular.|
13108|Mount Stavely Volcanic Complex|22603|6|Mentioned|p99|||Cambrian(?)||||||
13108|Mount Stavely Volcanic Complex|22643|6|Mentioned|p189|||Spelt "Mt" in text.||||||
13108|Mount Stavely Volcanic Complex|22708|6|Mentioned|p209|||||||||
13108|Mount Stavely Volcanic Complex|22857|5|Briefly described|p88 Fig. 14.7A, p97|Cambrian|Cambrian|Mount is Mt. in text of figure.||||||
13108|Mount Stavely Volcanic Complex|22858|6|Mentioned|p97,Fig14.7ap88-9|||||||||
13108|Mount Stavely Volcanic Complex|23309|5|Briefly described|p25, 34, 288, 298, Tb 2.1|Cambrian|Cambrian|||||||
13108|Mount Stavely Volcanic Complex|23402|3|Fully described|p9, p8 Tb. 1|Late Cambrian|Late Cambrian|Age: ~495Ma. Geological Province: Adelaide Fold Belt.||||||21-OCT-08
13108|Mount Stavely Volcanic Complex|23991|5|Briefly described|p188 Fig.1|Cambrian|Cambrian|Mount is Mt. in text.||||||
13108|Mount Stavely Volcanic Complex|24002|6|Mentioned|p226|||Mount is Mt in text.||||||
13108|Mount Stavely Volcanic Complex|24098|6|Mentioned|p30||Precambrian|||||||19-APR-05
13108|Mount Stavely Volcanic Complex|24214|6|Mentioned|p798|||||||||
13108|Mount Stavely Volcanic Complex|24311|5|Briefly described|p1060, p1059 Fig. 2|Cambrian|Cambrian|Mount is Mt. in text||||||
13108|Mount Stavely Volcanic Complex|24551|4|Described|p79|||Mount is Mt. in text.||||||
13108|Mount Stavely Volcanic Complex|24570|5|Briefly described|p397|Middle Cambrian|Middle Cambrian|Age: 501+/-9Ma and 495+/-5Ma (Stuart smith and Black 1999).  Mount is Mt in text.||||||
13108|Mount Stavely Volcanic Complex|38436|3|Fully described|p420|||||||||
13108|Mount Stavely Volcanic Complex|39967|4|Described|p27|||||||||
13108|Mount Stavely Volcanic Complex|40172|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
13108|Mount Stavely Volcanic Complex|40761|5|Briefly described|p219|||||||||
13108|Mount Stavely Volcanic Complex|40887|2|Defined|p10|Cambrian|Cambrian|Prob. Cambrian.||||||21-OCT-08
13108|Mount Stavely Volcanic Complex|41571|4|Described|p38|||||||||
13108|Mount Stavely Volcanic Complex|41868|6|Mentioned|p584|||See also Table 12.3||||||
13108|Mount Stavely Volcanic Complex|42827|4|Described|p38|||see also Table 2.2||||||
13108|Mount Stavely Volcanic Complex|43218|5|Briefly described|p21|Cambrian|Precambrian|||||||
13108|Mount Stavely Volcanic Complex|43627|6|Mentioned|p6|Cambrian|Cambrian|U-Pb Ages: 501+/-9 Ma, 495+/-5 Ma. Mount is Mt. in text.||||||28-OCT-04
13108|Mount Stavely Volcanic Complex|43753|6|Mentioned|p623||Cambrian|||||||
13108|Mount Stavely Volcanic Complex|44133|6|Mentioned|p14|||||||||
13108|Mount Stavely Volcanic Complex|44929|5|Briefly described|Map Legend|Cambrian|Cambrian|Intermediate to felsic volcanics, volcaniclastics and intrusives, weakly metamorphosed and deformed.||||||14-JUN-06
13108|Mount Stavely Volcanic Complex|44930|5|Briefly described|Map Legend|Cambrian|Cambrian|Intermediate to felsic volcanics, volcaniclastics and intrusives, weakly metamorphosed and deformed.||||||14-JUN-06
13108|Mount Stavely Volcanic Complex|44931|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Intermediate to felsic volcanics, volcaniclastics and intrusives, weakly metamorphosed and deformed.||||||14-JUN-06
13108|Mount Stavely Volcanic Complex|44932|5|Briefly described|Map Legend|Cambrian|Cambrian|Intermediate to felsic volcanics, volcaniclastics and intrusives, weakly metamorphosed and deformed.||||||14-JUN-06
13108|Mount Stavely Volcanic Complex|44933|5|Briefly described|Map Legend||Cambrian|||||||
13108|Mount Stavely Volcanic Complex|50154|2|Defined|p24, p47, p72, p143|Late Cambrian|Middle Cambrian|Geological Province: Grampians-Stavely Zone, Delamerian Fold Belt. Age: 490-502 Ma. Overlain by the Glenthompson Sandstone.||||||15-SEP-04
13108|Mount Stavely Volcanic Complex|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Ultramafic to intermediate metavolcanics and intrusives.||||||21-OCT-08
13108|Mount Stavely Volcanic Complex|50156|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Ultramafic to intermediate metavolcanics and intrusives: basalt, andesite, serpentinite.||||||21-OCT-08
13108|Mount Stavely Volcanic Complex|50157|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Ultramafic to intermediate metavolcanics and intrusives: basalt, andesite, serpentinite.||||||21-OCT-08
13108|Mount Stavely Volcanic Complex|50158|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Ultramafic to intermediate metavolcanics and intrusives: basalt, andesite, serpentinite.||||||21-OCT-08
13108|Mount Stavely Volcanic Complex|50159|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Ultramafic to intermediate metavolcanics and intrusives: basalt, andesite, serpentinite||||||
13108|Mount Stavely Volcanic Complex|50160|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Ultramafic to intermediate metavolcanics and intrusives: basalt, andesite, serpentinite||||||16-JUN-04
13108|Mount Stavely Volcanic Complex|50161|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Ultramafic to intermediate metavolcanics and intrusives: basalt, andesite, serpentinite||||||22-JUN-04
13108|Mount Stavely Volcanic Complex|50162|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Ultramafic to intermediate metavolcanics and intrusives: basalt, andesite, serpentinite||||||
13108|Mount Stavely Volcanic Complex|50163|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Ultramafic to intermediate metavolcanics and intrusives: basalt, andesite, serpentinite||||||
13108|Mount Stavely Volcanic Complex|50371|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||
13108|Mount Stavely Volcanic Complex|60412|6|Mentioned|p229, 232, 235-238, 242|||Western subprovince of the Lachlan Fold Belt. Hosts small mineral deposits.|||Mount Stavely dacite.||Mafic to felsic volcanic rocks with a very low metamorphic imprint.|
13108|Mount Stavely Volcanic Complex|60451|4|Described|p21 Fig. 7, 43|Late Cambrian|Middle Cambrian|||||||
13108|Mount Stavely Volcanic Complex|60454|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delarmerian Fold Belt. Andesite to dacite lava and sills, Volcanolithic sediment and interlayered lava.||||||
13108|Mount Stavely Volcanic Complex|60456|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delarmerian Fold Belt. Andesite to dacite lava and sills: massive greenish lava, volcanic conglomerate, volcanolithic sediment and interlayered lava.||||||
13108|Mount Stavely Volcanic Complex|60457|5|Briefly described|Map Legend|Cambrian|Cambrian|Units do not appear on this map. Geological Province: Delamerian Fold Belt.||||||
13108|Mount Stavely Volcanic Complex|60458|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delarmerian Fold Belt.  Andesite to dacite lava and sills, volcanic conglomerate, volcanolithic sediment, lava, diorite.||||||
13108|Mount Stavely Volcanic Complex|60459|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delarmerian Fold Belt. Andesite to dacite lava, rare basalt and rhyolite, abundant volcanic breccia and sandstone. Prenhite-pumpeyllite grade.||||||
13108|Mount Stavely Volcanic Complex|60544|6|Mentioned|Map legend|Cambrian|Cambrian|Age: 501+/-9-495+/-5Ma (SHRIMP: Stuart-Smith and Black, 1994).  Mount is Mt in text.||||||
13108|Mount Stavely Volcanic Complex|61183|4|Described|p23, p26|||Includes the Williamson Road Serpentinite. See also p69, p73.||||||
13108|Mount Stavely Volcanic Complex|61187|5|Briefly described|p1, p3, p14, pp67ff, pp129ff.|Cambrian|Cambrian|Calc-alkaline arc-type volcanics. Hosts Wickliffe and Thursdays Gossan uneconomic base metal prospects, the latter being the first porphyry copper style deposit identified in western Victoria. Similar geochemistry, and same age, as Mount Read Volcanics in Tasmania. Extends northwards under shallow cover of Murray Basin.|||Includes Fairview Andesitic Breccia; Nanapundah and Towanway Tuffs; Williamsons Road Serpentinite; and Lalkaldarno Porphyry.||A sequence of andesitic to rhyolitic lavas, volcaniclastics and intrusive rocks.|
13108|Mount Stavely Volcanic Complex|61726|5|Briefly described|p923, p936|Late Cambrian|Late Cambrian|Calc-alkaline volcanics. Age: 495+/-5Ma (SHRIMP zircon on tuffaceous unit in upper part of complex). Mount is Mt in text.||||||
13108|Mount Stavely Volcanic Complex|61752|5|Briefly described|p4, p6 Fig. 2|Cambrian|Cambrian|Intermediate calc-alkaline volcanics and intrusives. Infaulted with Glenthompson Sandstone. Geological Province: Adelaide Fold Belt. See also Mount Stavely Volcanics.||||||07-FEB-11
13108|Mount Stavely Volcanic Complex|62741|5|Briefly described|p678 Fig. 1|Cambrian|Cambrian|Calc-alkaline post-collisional association.||||||
13108|Mount Stavely Volcanic Complex|64314|5|Briefly described|p495 Fig. 2a|Cambrian|Cambrian|||||||
13108|Mount Stavely Volcanic Complex|64541|5|Briefly described|Map Legend|Cambrian|Cambrian|Comprises; Intermediate to felsic volcanics, volcaniclastics and intrusives, deep marine deposits that are deeply weathered, intermediate to felsic metavolcanics, ultra-mafic to intermediate metavolcanics and intrusives.||||||07-FEB-11
13108|Mount Stavely Volcanic Complex|64571|6|Mentioned|p839|||VIC. Andesites and dacites.||||||15-DEC-08
13108|Mount Stavely Volcanic Complex|64610|5|Briefly described|Map legend|Cambrian|Cambrian|||||||12-NOV-08
13108|Mount Stavely Volcanic Complex|65665|6|Mentioned|p1144 Fig.1|Cambrian|Cambrian|Calc-alkaline and post-collisional association.||||||10-MAY-12
13108|Mount Stavely Volcanic Complex|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Includes Fairview Andesite Breccia, Lalkaldarno Porphyry, Nanapundah Tuff and Towanway Tuff. Defined by Buckland 1986.||||||
13108|Mount Stavely Volcanic Complex|66769|6|Mentioned|117|Late Cambrian|Middle Cambrian|Grampians-Stavely Zone. Calcalkaline volcanic rocks. Also called Mount Stavely Volcanic Group p117. Similar age and chemistry to the Mount Read Volcanics (TAS). Is overlain by Glenthompson Sandstone.||||||
13108|Mount Stavely Volcanic Complex|67103|6|Mentioned|p613 Fig.6|||||||||
13108|Mount Stavely Volcanic Complex|68116|5|Briefly described|Appendix, Maps 30. 39.|Middle Cambrian|Middle Cambrian||||||Intermediate to felsic volcanics, volcaniclastics and intrusives: weakly metamorphosed and deformed; moderate to high magnetic response.|
13108|Mount Stavely Volcanic Complex|68189|6|Mentioned|p3, p19|||||||||
13108|Mount Stavely Volcanic Complex|68822|5|Briefly described|p331, p346|Paibian|Drumian|Chert bands in andesites contain middle Cambrian acritarchs ca 504 Ma (Squire et al. 2006b) which pass into 495 Ma dacites (Crawford et al. 1996; Stuart-Smith and Black 1999).|ca. 504 - 495 Ma||||Passes up from sheared 'boninitic' ultramafics through largely post-collisional andesites into dacites.|27-JUL-15
13108|Mount Stavely Volcanic Complex|70211|5|Briefly described|p1, p3, p5-6, p21, p45, p58|Cambrian|Cambrian|Buckland (1987). Grampians-Stavely Zone, western Victoria. Age from an unnamed granodiorite from drill hole SNDD002 that appears to be a fault slice within the Mount Stavely Volcanic Complex.|511.3 +/- 2.9 Ma U/Pb SHRIMP||Lalkaldarno Porphyry, Towanway Tuff.|Is overlain by Glenthompson Sandstone.|Andesitic to rhyolitic lavas and volcaniclastic rocks overlying scattered occurrences of tholeiitic to boninitic lavas; granodiorite.|05-JAN-18
13108|Mount Stavely Volcanic Complex|70493|5|Briefly described|p54, 56, 63-64|Middle Cambrian|Middle Cambrian|Grampians-Stavely Zone, Lachlan Orogen. A likely major source of sediments of the Adaminaby Group. Also appears as Mount Stavely Volcanics (p63).||||Is overlain by Nargoon Group.|Contains medium- to high-K calc-alkaline volcanic rocks, with less common shoshonites and granodiorites.|
13108|Mount Stavely Volcanic Complex|70877|4|Described|p1, p9-p10, p12, p14,  p23|Cambrian|Cambrian|See also p32, p48-p49, p61,  p69-p70, p77, p84, p91, p109, p167-p170. Grampians-Stavely Zone. Rough age derived from three volcanic rocks within this group.|c. 504-502 Ma||Includes Fairview Andesite Breccia, Towanway Tuff and the Nanapundah Tuff.|Overlies the Glenthompson Sandstone.|Intermediate to felsic calc-alkaline lava, breccia, interbedded subaqueous tuffaceous and volcaniclastic to dacitic rocks and fault slices of ultramafic rocks, terrigenous marine sediments and pelagic marine sediments.|
13108|Mount Stavely Volcanic Complex|70967|5|Briefly described|p2, 10, 13-14, 17, 20|Cambrian|Cambrian|Crawford and Keays (1978). Mount Stavely Belt.|510-500 Ma.|||Is overlain by Glenthompson Sandstone.|Interbedded subaqueous tuffaceous and volcaniclastic rocks.|
13108|Mount Stavely Volcanic Complex|71249|6|Mentioned|p7|||||||||
13108|Mount Stavely Volcanic Complex|71593|4|Described|p6, p12-p14, p19, p24-p31, p35|||Delamerian Orogen, Grampians-Stavely Zone. Intecalated with fault slices of tholeiitic mafic rocks, terrigenous marine sediments and pelagic marine sediments. Considered equivalent to rocks in Dryden Belt segment. Outcrops poorly in the Black Range area. See also p39-p40, p57, p70-p72, p75-p76, p82, p94-p95, p102, p107, p120-p121, p124, p131-p133, p150, p157, p161, p165, p167-p168, p171, p182-p183, p185, p188, p201.|||Includes the Fairview Andesite Breccia, Nanapundah Tuff, Towanway Tuff, Williamsons Road Serpentinite.|Conformably (gradationally) overlain by the Glenthompson Sandstone. Faulted against the Glenelg River Metamorphic Complex.|Intermediate to felsic, dominantly calc-alkaline lava, breccia and interbedded subaqeous tuffaceous volcaniclastic rocks.|
13108|Mount Stavely Volcanic Complex|72445|5|Briefly described|p1, p8-9, p12-13, p16, 19; App.1, App.7.|Cambrian|Cambrian|Shown as part of the target basement. Spelt Mt Stavely Volcanic Complex in geological map p6 Fig.3. See also App.7 p6 Fig.3; App.1, App.2; App.5. App.2 is a .csv format file. Shown in Stavely 02, 10, with various descriptions. Lithology also includes Sheared amygdaloidal basalt and serpentinite breccia. Overlain by the Glenthompson Sandstone.|510-500 Ma in part.||Includes Williamsons Road Serpentinite.|Shown as in faulted or sheared contact with overlying Grampians Group. Overlain by Renmark Group. Sharp contact.|Includes interbedded subaqueous tuffaceous and volcaniclastic rocks.Ferruginous fault breccia with intermingled basalt and sandstone/conglomerate. Mafic volcanic sandstone and breccia with 0.6-4.95m intervals of mafic volcanics and dykes.|15-OCT-20
13108|Mount Stavely Volcanic Complex|73059|6|Mentioned|p1059|Late Cambrian|Late Cambrian|Grampians-Stavely Zone. See also references to Mount Stavely Complex (p1062) and Stavely Volcanic Complex (p1062 Fig.9).||||||
13108|Mount Stavely Volcanic Complex|73118|5|Briefly described|p6, 9, 14-15, 73, 223, 225-227, 229|||Glenelg Zone, Western Victoria. Island arc volcanics intruded through Upper Proterozoic continental crust basement. Hosts Cu (Duval Mining Aust.) dated as coeval with Mount Read Volcanics (TAS).|501 +/- 9 Ma.|||Correlated with Mount Read Volcanics (TAS).|Calc-alkaline andesites, rhyolites and dacites with adakitic affinities; contains VHMS style gold and base metal mineralisation.|
13108|Mount Stavely Volcanic Complex|73177|5|Briefly described|p1100|||Activity could have started as early as c.525 Ma. Has similarities with Mount Wright Volcanics along strike to the N.|511-500 Ma.|||||
13108|Mount Stavely Volcanic Complex|73264|6|Mentioned|p1385 Fig.8|Cambrian|Cambrian Stage 5|Delamerian Orogen, Grampians-Stavely Zone.||||||
13108|Mount Stavely Volcanic Complex|73430|5|Briefly described|p493, p496|Cambrian|Cambrian|Described as a volcanic arc. Deformation ceased at ~498+/-5 Ma. The volcanics occur within siliciclastic sediment sequences of the Nargoon Group and Glenthompson Beds. Written as Mt Stavely Volcanic Complex. See also Mount Stavely Complex, Mount Stavely Volcanics, Mount Stavely volcanic suite p506.|510 to 503 Ma (Lewis et al., 2016)||Lalkaldarno Porphyry||Slightly metamorphosed basaltic, andesitic and dacitic lavas, dacitic porphyry and tuffs and volcaniclastic sediments.|
13111|Mount Stewart Granite|45087|6|Mentioned|p40|||Chemical analyses||||||
37583|Mount Stinton Granodiorite|23309|5|Briefly described|p165|||G 227, S-type.  Supersedes Mount Stinton Granite.||||||
37583|Mount Stinton Granodiorite|24551|6|Mentioned|p223, 720 Table 8.3|||See also Talbot Drive Granodiorite.  Of the Acheron Volcanic Complex.||||||
37583|Mount Stinton Granodiorite|68116|5|Briefly described|Appendix, Maps 33, 42.|Late Devonian|Late Devonian||||||Biotite granodiorite: medium grained, sub-equigranular, abundant xenoliths.|
13114|Mount Stirling Granodiorite|22625|6|Mentioned|P726|||||||||
13114|Mount Stirling Granodiorite|23269|6|Mentioned|Fig14-3.1p403|||Written: Mt Stirling Granodiorite.||||||
13114|Mount Stirling Granodiorite|23309|5|Briefly described|p439, App1|Late Devonian|Middle Devonian|G184 I-Type. Age: 385 +/- 14 Ma, 379+/-13Ma, 373+/-13Ma, 384+/-14Ma, 377+/-13 Ma.||||||
13114|Mount Stirling Granodiorite|24551|5|Briefly described|p158|||Of the Mount Buller suite.||||||
13114|Mount Stirling Granodiorite|30329|6|Mentioned|p30|||On table P30||||||
13114|Mount Stirling Granodiorite|32001|6|Mentioned|p78|||||||||
13114|Mount Stirling Granodiorite|32074|6|Mentioned|p181|||||||||
13114|Mount Stirling Granodiorite|33602|6|Mentioned|p22|||||||||
13114|Mount Stirling Granodiorite|34989|4|Described|p81|||||||||
13114|Mount Stirling Granodiorite|35277|6|Mentioned|p107|||||||||
13114|Mount Stirling Granodiorite|41641|4|Described|p177|||||||||
13114|Mount Stirling Granodiorite|42827|6|Mentioned|p151|||||||||
13114|Mount Stirling Granodiorite|44187|5|Briefly described|Map Legend||Middle Devonian|G184 Unassigned.||||||
13114|Mount Stirling Granodiorite|64616|6|Mentioned|p344|||I-type intrusion. Associated with a set of conjugate faults which may have assisted emplacement of the intrusion.||||||
13114|Mount Stirling Granodiorite|68116|5|Briefly described|Appendix, Map 34.|Middle Devonian|Middle Devonian||||||Hornblende granodiorite, diorite, gabbro: medium to coarse grained.|
13114|Mount Stirling Granodiorite|70933|14|Not recorded|p95|Late Devonian|Middle Devonian|Late Middle to Early Upper Devonian igneous activity.||||||
30551|Mount Tabby Formation|23309|4|Described|p109. Tb 2.40|||Of the Little River Subgroup.  Maximum Thickness: 600m.||||||22-FEB-10
30551|Mount Tabby Formation|23615|3|Fully described|p116|Early Devonian|Early Devonian|Of Little River Subgroup.  600m thick at type section. Interfingers with Moonkan Ignimbrite.  Composed of various rock types including feldspar ignimbrite, basalt, and andesite lava, breccia and sediment lenses.||||||
30551|Mount Tabby Formation|24551|5|Briefly described|p144|||Of Little River Subgroup. Is a lens in the Moonkan Ignimbrite.||||||
30551|Mount Tabby Formation|43206|5|Briefly described|map legend||Lochkovian|of Little River Subgroup.||||||
30551|Mount Tabby Formation|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Quartz-feldspar and feldspar ignimbrite, basalt lava, breccia, sandstone.|
26773|Mount Tambo Group|22628|6|Mentioned|fig1p108|||spelt "Mt" in the text||||||
26773|Mount Tambo Group|22968|4|Described|p14, p122-130||Late Silurian|Faulted contacts with surrounding units, correlates to the Enano and Wombat Creek Groups, maximum thickness is 5700m. Rediometric age 416+/-5 Ma U/pb zircons from Vitric Ignimbrite Member, Blackfellows Flat Formation.||||||10-SEP-18
26773|Mount Tambo Group|23020|5|Briefly described|Map legend|Pridoli|Ludlow|||||||
26773|Mount Tambo Group|23021|5|Briefly described|Map legend|Pridoli|Ludlow|||||||
26773|Mount Tambo Group|23028|5|Briefly described|Map legend|Pridoli|Ludlow|||||||
26773|Mount Tambo Group|23029|5|Briefly described|Map legend|Pridoli|Ludlow|||||||
26773|Mount Tambo Group|23030|5|Briefly described|Map legend|Late Silurian|Late Silurian|||||||
26773|Mount Tambo Group|23307|5|Briefly described|Map Legend|Silurian|Silurian|Mount is Mt. in text||||||
26773|Mount Tambo Group|23309|5|Briefly described|p5 Fig. 1.3, 125-129|Early Devonian|Silurian|||||||
26773|Mount Tambo Group|23522|5|Briefly described|p247 Fig 3||Devonian|||||||
26773|Mount Tambo Group|23710|14|Not recorded|p71|||Geological map.||||||
26773|Mount Tambo Group|23938|5|Briefly described|p31-32 Fig. 12|Early Devonian|Early Devonian|Mount is Mt in text of figure.||||||25-SEP-08
26773|Mount Tambo Group|24004|5|Briefly described|p275 fig.2|Early Devonian|Early Devonian|Mount is Mt. in text.||||||
26773|Mount Tambo Group|24275|5|Briefly described|p1696 Fig. 2, p1698 Tb. 1|Late Devonian|Middle Devonian|Proximal submarine fan of quartz sandstone turbidites and siltstones, fossiliferous chert pebble conglomerates; minor rhyolitic volcanics. Geological Province: Lachlan Fold Belt.||||||24-JAN-06
26773|Mount Tambo Group|24551|4|Described|p138, p47 Fig. 2.58|Devonian|Silurian|||||||03-NOV-14
26773|Mount Tambo Group|31161|5|Briefly described|PA11|||||||||
26773|Mount Tambo Group|33393|5|Briefly described|p164|||||||||
26773|Mount Tambo Group|33732|6|Mentioned|Table III|||||||||
26773|Mount Tambo Group|34519|5|Briefly described|p45|||||||||
26773|Mount Tambo Group|35277|6|Mentioned|p116|||||||||
26773|Mount Tambo Group|38145|6|Mentioned|Map legend|Devonian|Silurian|Devonian or Silurian||||||
26773|Mount Tambo Group|38367|6|Mentioned|Fig.9.|||||||||
26773|Mount Tambo Group|39447|4|Described|p14|||||||||
26773|Mount Tambo Group|39860|4|Described|p12|||||||||
26773|Mount Tambo Group|40761|6|Mentioned|p238|||||||||
26773|Mount Tambo Group|41572|6|Mentioned|p19|||||||||
26773|Mount Tambo Group|41641|6|Mentioned|p186|||||||||
26773|Mount Tambo Group|42089|6|Mentioned|Fig.12 P12|||||||||
26773|Mount Tambo Group|42791|5|Briefly described|p216|||see also Fig.10 P215||||||
26773|Mount Tambo Group|44184|5|Briefly described|Map Legend||Early Devonian|||||||
26773|Mount Tambo Group|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian||||||Fluvial, marine, extrusive: conglomerate, sandstone, mudstone, ignimbrite.|
26773|Mount Tambo Group|60503|3|Fully described|p15, p129|Early Devonian|Early Devonian|Complex sedimentary and volcanic sequence. New mapping has led to three-fold subdivision: Berrawan Conglomerate, Blackfellows Flat Formation and Mount Shanahan Sandstone. Geological Province: Scrubby Creek Syncline.||||||16-NOV-09
26773|Mount Tambo Group|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Berrawan Conglomerate, Blackfellows Flat Conglomerate.||||||20-OCT-04
26773|Mount Tambo Group|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes: Berrawan Conglomerate, Blackfellows Flat Conglomerate.||||||
26773|Mount Tambo Group|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes: Berrawan Conglomerate, Blackfellows Flat Conglomerate.||||||20-OCT-04
26773|Mount Tambo Group|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Berrawan Conglomerate, Blackfellows Flat Conglomerate.||||||20-OCT-04
26773|Mount Tambo Group|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Conglomerate: mostly nonmagnetic with northwest trending highs (50 nT) on western margin; bands of northwest trending low to moderate total count, K, Th, U.||||||25-SEP-08
26773|Mount Tambo Group|60541|5|Briefly described|p11 Fig. 2|Late Devonian|Late Devonian|Mount is Mt in text of figure.||||||
26773|Mount Tambo Group|60542|5|Briefly described|p11 Fig. 2|Late Devonian|Late Devonian|||||||
26773|Mount Tambo Group|61161|5|Briefly described|p153|Early Devonian|Early Devonian|Age: 416 +-5 Ma, VandenBerg et al. (2000)||||||
26773|Mount Tambo Group|61163|5|Briefly described|p13|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt (Omeo Zone).||||||
26773|Mount Tambo Group|61187|5|Briefly described|p5 Fig.3, p26 Fig.2, p29 Fig.4.  |Early Carboniferous|Late Devonian|Benambra Terrane. Correlative of Avon River Group (Benambra Terrane) and Mansfield Group (Melbourne Zone, Melbourne Terrane).||||||
26773|Mount Tambo Group|65214|6|Mentioned|p281|Devonian|Devonian|VIC, Buchan. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
26773|Mount Tambo Group|66197|5|Briefly described|p634|Early Devonian|Early Devonian|Written Mt in text. Basement-derived conglomerate and silicic volcanics.||||||14-MAR-12
13129|Mount Taylor Granite|23309|5|Briefly described|p282||Silurian|G132 S-Type. Supersedes Mount Taylor Porphyry.||||||
13129|Mount Taylor Granite|24551|6|Mentioned|p224|||||||||
13129|Mount Taylor Granite|42726|5|Briefly described|map legend|Middle Devonian||584. NOT variation on Mount Taylor Porphyry. Invalid name.||||||
13129|Mount Taylor Granite|61161|5|Briefly described|p30|Silurian|Silurian|S-type granite. South of DARGO. GSV map code: G132.||||||
13129|Mount Taylor Granite|66769|6|Mentioned|142|||Tabberabbera Zone. Ba-rich||||||
13129|Mount Taylor Granite|68116|5|Briefly described|Appendix, Map 44.|Late Devonian|Late Devonian||||||Cordierite-garnet granite porphyry: coarsely K-feldspar phyric, mid-grey; S-type.|
26774|Mount Timbertop Conglomerate|22559|6|Mentioned|p589|||Mount spelled Mt in text||||||
26774|Mount Timbertop Conglomerate|22729|4|Described|p583, 584||Carboniferous|Mount spelled Mt in text||||||
26774|Mount Timbertop Conglomerate|22971|5|Briefly described|p18|Late Devonian|Late Devonian|Basal unit of Mansfield Group.  Conglomerate and sandstone. Overlain by Devils Plain Formation.||||||19-JAN-06
26774|Mount Timbertop Conglomerate|24551|4|Described|p170, 177|||Of the Mansfield Group.  Overlies the Delatite Group (u), Warrambat Volcanics (u).    ||||||
26774|Mount Timbertop Conglomerate|33607|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26774|Mount Timbertop Conglomerate|64616|6|Mentioned|p137|||Junior synonym of Mount Kent Conglomerate dropped in 2000.||||||
37765|Mount Unicorn Porphyry|23309|6|Mentioned|p439, Appendix 1|||G582.||||||
37765|Mount Unicorn Porphyry|24133|3|Fully described|p81|||~Early Devonian.  Geological Province: Lachlan Fold Belt.||||||
37765|Mount Unicorn Porphyry|24142|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37765|Mount Unicorn Porphyry|24143|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37765|Mount Unicorn Porphyry|24144|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37765|Mount Unicorn Porphyry|24145|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Geological Province: Lachlan Fold Belt||||||
37765|Mount Unicorn Porphyry|24146|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37765|Mount Unicorn Porphyry|68116|5|Briefly described|Appendix, Map 20.|Middle Devonian|Early Devonian||||||Quartz-feldspar porphyry: pale cream to buff coloured; bipyramidal quartz phenocrysts and altered feldspar; patchily to pervasively altered; nonmagnetic and magnetic phases.|
34876|Mount Walterson Conglomerate Member|22968|5|Briefly described|P113|Silurian|Silurian|Parent is Cowombat Siltstone, maximum thickness is 350m||||||
34876|Mount Walterson Conglomerate Member|23309|5|Briefly described|p116-117.|||Parent: Enano Group?||||||
34876|Mount Walterson Conglomerate Member|24551|5|Briefly described|p135|||Of Cowombat Siltstone.||||||
69709|Mount Warrick Rhyolite|61163|3|Fully described|p28, p36 Tb. 6.2|Late Devonian|Late Devonian|Supersedes Mount Warrick Mylonite (Gaul 1982). Intrusive marginal dyke complex - part of volcanic sequence of Tolmie Igneous Complex, comprising rhyolitic lava and porphyry. May be a composite unit (of intrusions of variable ages). Geol Prov: Lachlan F.B.||||||06-JUL-07
69709|Mount Warrick Rhyolite|61174|5|Briefly described|map legend|Late Devonian|Late Devonian|Of the Tolmie Igneous Complex. Rhyolitic lava and porphyry: mostly very glassy, massive to flow-banded, commonly perlitic; rare volcaniclastic sandstone and conglomerate; cream to pale brown colours. GSV map code: Dtw.||||||07-FEB-11
69709|Mount Warrick Rhyolite|61175|5|Briefly described|map legend|Late Devonian|Late Devonian|Of the Tolmie Igneous Complex. Rhyolitic lava and porphyry: mostly very glassy, massive to flow-banded, commonly perlitic; rare volcaniclastic sandstone and conglomerate; cream to pale brown colours. GSV map code: Dtw.||||||
69709|Mount Warrick Rhyolite|61176|5|Briefly described|map legend|Late Devonian|Late Devonian|Of the Tolmie Igneous Complex. Rhyolitic lava and porphyry: mostly very glassy, massive to flow-banded, commonly perlitic; rare volcaniclastic sandstone and conglomerate; cream to pale brown colours. GSV map code: Dtw.||||||
69709|Mount Warrick Rhyolite|61177|5|Briefly described|map legend|Late Devonian|Late Devonian|Of the Tolmie Igneous Complex. Rhyolitic lava and porphyry: mostly very glassy, massive to flow-banded, commonly perlitic; rare volcaniclastic sandstone and conglomerate; cream to pale brown colours. GSV map code: Dtw.||||||
69709|Mount Warrick Rhyolite|61178|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Tolmie Igneous Complex. Rhyolitic lava and porphyry; rare volcaniclastic sandstone and conglomerate: nonmagnetic (k = 0 -20 x10^-6 cgs); low gravity (-510 ms^-2); high total radioelement, K and U, moderate Th. GSV map code: Dtw.||||||
69709|Mount Warrick Rhyolite|68116|5|Briefly described|Appendix, Maps 26, 34.|Late Devonian|Late Devonian||||||Rhyolitic lava and porphyry: mostly very glassy, massive to flow-banded, commonly perlitic; rare volcaniclastic sandstone and conglomerate; cream to pale brown colours.|
13208|Mount Wellington Rhyolite|40761|5|Briefly described|p237|||||||||
13220|Mount William Metabasalt|23229|4|Described|Table3-1p16, 17|Middle Cambrian||||||||
13220|Mount William Metabasalt|23309|5|Briefly described|p28, 42. Tb 2.4. Fig. 2.14.||Cambrian|Of the Heathcote Volcanics.||||||
13220|Mount William Metabasalt|24002|6|Mentioned|p231|||Of Heathcote Volcanics.||||||
13220|Mount William Metabasalt|24177|4|Described|p40, p78 Fig.36|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Overlain by the Knowsley East Shale. Overlies the Lazy Bar Andesite.||||||
13220|Mount William Metabasalt|24328|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Parent: Heathcote Volcanics||||||
13220|Mount William Metabasalt|24329|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Parent: Heathcote Volcanics.||||||27-OCT-08
13220|Mount William Metabasalt|24551|4|Described|p85|Cambrian|Cambrian|Of Heathcote Volcanics. Overlain by Knowsley East Shale.||||||
13220|Mount William Metabasalt|40761|5|Briefly described|Table 1|||||||||
13220|Mount William Metabasalt|41570|6|Mentioned|Fig.3.8|||||||||
13220|Mount William Metabasalt|41571|4|Described|p42|||||||||
13220|Mount William Metabasalt|42628|5|Briefly described|Map legend|Early Cambrian||||||||
13220|Mount William Metabasalt|42790|5|Briefly described|Fig.14 P189|||||||||
13220|Mount William Metabasalt|42826|2|Defined|p20||Early Cambrian|||||||
13220|Mount William Metabasalt|60591|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Overlain by the Knowsley East Shale. Consists of deepwater hemipelagic deposits and dolerite sills.||||||
13220|Mount William Metabasalt|60592|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Overlain by the Knowsley East Shale. Consists of deepwater hemipelagic deposits and dolerite sills.||||||25-NOV-04
13220|Mount William Metabasalt|60593|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Overlain by the Knowsley East Shale. Consists of deepwater hemipelagic deposits and dolerite sills.||||||
13220|Mount William Metabasalt|60595|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Overlain by the Knowsley East Shale. Consists of deepwater hemipelagic deposits and dolerite sills.||||||
13220|Mount William Metabasalt|60596|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Overlain by the Knowsley East Shale. Consists of deepwater hemipelagic deposits and dolerite sills.||||||
13220|Mount William Metabasalt|60597|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Variable magnetic response; low K, Th and U||||||
13220|Mount William Metabasalt|60599|3|Fully described|p7, p24 Tb. 4, p37, p105, p147|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Formerly Mount William beds, and part of former Heathcote Greenstone). Lithological details presented. Overlain by Knowsley East Shale; overlies Sheoak Gully Boninite. Max.thickness: >2500m. LFB.||||||27-OCT-08
13220|Mount William Metabasalt|62742|5|Briefly described|p699 Fig. 2|Early Cambrian|Early Cambrian|In the Heathcote Greenstone Belt. ||||||
13220|Mount William Metabasalt|62744|5|Briefly described|p709 Fig. 2|Cambrian|Cambrian|Geological Province: Heathcote Greenstone Belt.||||||
13220|Mount William Metabasalt|64611|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of Heathcote Volcanic Group. Comprises an unnamed chert/siltstone/black shale and sandstone member; and an amphibolite component (metabasalt, minor diorite and interflow sediments). Further lithological detail included.||||||16-DEC-08
13220|Mount William Metabasalt|64612|2|Defined|p30-31, p47, p53, p60|Cambrian|Cambrian|Usage of name follows VandenBerg (1992). Of Heathcote Volcanic Group.  Underlies Knowsley East Shale (sharp contact). Thickness: 1600m. Mainly metabasalts, but with interbedded shale and chert. Deep marine setting.||||||07-FEB-11
13220|Mount William Metabasalt|64619|5|Briefly described|Map legend|Cambrian|Cambrian|Of Heathcote Volcanic Group. Age: Middle Cambrian. Dark green basalt, fine-gr.+ phenocrysts of plagioclase and clinopyroxene; rare pillow structures; dolerite sills; with a chert/shale/breccia/sandstone component - lithological details included.||||||03-NOV-08
13220|Mount William Metabasalt|65715|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Heathcote Volcanic Group. Formation rank.||||||
13220|Mount William Metabasalt|65969|5|Briefly described|p11, p17 Fig.7, p21 Fig.10|Cambrian|Cambrian|Unit in Heathcote Volcanic Group. Contains 65 ppb Au: suggested source for gold mineralisation at Bendigo. Hosts Mount Camel Cu-Zn mineralisation. Mapped as conformably overlain by Knowsley East Shale, but contact may be faulted instead.||||||
13220|Mount William Metabasalt|66769|6|Mentioned|132|||Upper (hangingwall) part of Mt William Fault zone, Bendigo Zone. Massive layered volcanic rocks.||||||
13220|Mount William Metabasalt|68116|5|Briefly described|Appendix, Maps 17, 24, 32.|Middle Cambrian|Early Cambrian|Contains rare pillow structures.|||||Basalt, microgabbro: basalt dark green, fine-grained, phenocrysts of plagioclase and clinopyroxene; microgabbro sills: medium to coarse-grained, equigranular, columnar jointing in some; interflow pyritic shale, black shale, chert, jasper.|
13220|Mount William Metabasalt|68314|6|Mentioned|p753-754|Early Cambrian|Early Cambrian|Heathcote Greenstone Belt.||||Is overlain conformably by Knowsley East Shale.||
13220|Mount William Metabasalt|70601|5|Briefly described|p44|Middle Cambrian|Early Cambrian|Kilmore/Heathcote area.||||Underlies Knowsley East Shale. Unconformably Overlies Heathcote Volcanics.||
13220|Mount William Metabasalt|73497|5|Briefly described|Map legend|Cambrian|Cambrian|Magnetic response to 800 nT; gravity high to 100 micrometres/second/second; low K, Th and U.||Heathcote Volcanic Group||Overlies Lazy Bar Andesite, underlies Dookie Igneous Complex|Basalt: fine-grained, phenocrysts of plagioclase and clinopyroxene, pillow basalt; pyritic shale, black shale, chert, jasper; dolerite sills, medium- to coarse-grained, equigranular, phenocrysts of plagioclase and clinopyroxene.|
13225|Mount Wills Granite|23309|5|Briefly described|p338, 346|Early Devonian|Late Silurian|G111 S-Type. Age: 434+/-17Ma, 399+/-10Ma, 412+/-16Ma, 416+/-17 Ma.  Of the Koetong Supersuite?||||||10-JAN-07
13225|Mount Wills Granite|24551|6|Mentioned|p233|||||||||
13225|Mount Wills Granite|35278|6|Mentioned|p357|||||||||
13225|Mount Wills Granite|39860|4|Described|p20|||See also P35. Coarse-grained; consists of orthoclase, quartz, plagioclase, abundant deformed muscovite, biotite and tourmaline.||||||30-NOV-04
13225|Mount Wills Granite|41868|5|Briefly described|p476|||||||||
13225|Mount Wills Granite|42726|5|Briefly described|map legend|Silurian||||||||
13225|Mount Wills Granite|60503|5|Briefly described|p214 Tb. 16|Silurian|Silurian|S-type. Intruded the Omeo Metamorphic Complex. Primary gold mineralisation occurs in quartz veins, occupying shears and fractures at or near the contact of granites with the metamorphics. ||||||
13225|Mount Wills Granite|61160|3|Fully described|p56, p33 Tb. 5.2|Silurian|Silurian|Formerly Mt Wills Muscovite Granite (Crohn 1950) and Mount Wills Leucoadamellite (Fagan 1979). S-type. Medium- to coarse-gr.muscovite leucogranite; common pegmatite phases. Intrudes schist and gneiss of Omeo Metamorphic Complex and Cobungra Granite. ||||||
13225|Mount Wills Granite|61164|5|Briefly described|map legend|Early Silurian|Early Silurian|Muscovite-biotite leucogranite: coarse to fine grained; accessory tourmaline, garnet and topaz; pegmatitic phases common; numerous roof pendants; S-type intrusion. GSV map code: G111.||||||
13225|Mount Wills Granite|61165|5|Briefly described|map legend|Early Silurian|Early Silurian|Muscovite-biotite leucogranite: coarse to fine grained; accessory tourmaline, garnet and topaz; pegmatitic phases common; numerous roof pendants; S-type intrusion. GSV map code: G111.||||||
13225|Mount Wills Granite|61166|5|Briefly described|map legend|Early Silurian|Early Silurian|Muscovite-biotite leucogranite: coarse to fine grained; accessory tourmaline, garnet and topaz; pegmatitic phases common; numerous roof pendants; S-type intrusion. GSV map code: G111.||||||
13225|Mount Wills Granite|61167|5|Briefly described|map legend|Early Silurian|Early Silurian|Muscovite-biotite leucogranite: coarse to fine grained; accessory tourmaline, garnet and topaz; pegmatitic phases common; numerous roof pendants; S-type intrusion. GSV map code: G111.||||||07-FEB-11
13225|Mount Wills Granite|61168|5|Briefly described|map legend|Early Silurian|Early Silurian|Muscovite-biotite leucogranite: S-type; 415 +/- 15 Ma K/Ar muscovite; nonmagnetic (kv = 0-50 x10^-6 cgs); low gravity (-500 to -450 ums^-2); low to moderate total radioelement, high K, low Th, low to moderate U. GSV map code: G111.||||||
13225|Mount Wills Granite|68116|5|Briefly described|Appendix, Map 27.|Silurian|Silurian||||||Muscovite-biotite leucogranite: coarse to fine grained; accessory tourmaline, garnet and topaz; pegmatitic phases common; numerous roof pendants; S-type.|
31663|Mount Wills Suite|42726|5|Briefly described|Map Legend||Silurian|||||||
22456|Mountain Chief Andesite|23309|5|Briefly described|p32 Tb 2.4|||||||||
22456|Mountain Chief Andesite|24551|5|Briefly described|p90|||Basal unit of the Lickhole Volcanic Group. Overlain by the Sheepyard Flat Andesite||||||
22456|Mountain Chief Andesite|68116|5|Briefly described|Appendix, Map 34.|Cambrian|Cambrian||||||Andesitic lava and breccia, volcaniclastic mafic boninite, minor hyaloclastite.|
34844|Mountain Maid Granite|22968|5|Briefly described|P60, Table7, P178||Early Silurian|Age of unit is 425+/-9 Ma (U/Pb zircon), New name||||||13-SEP-04
34844|Mountain Maid Granite|23029|5|Briefly described|Map legend|Wenlock|Wenlock|Parent is unassigned||||||
34844|Mountain Maid Granite|23030|5|Briefly described|Map legend|Silurian|Silurian|Parent is unassigned||||||
34844|Mountain Maid Granite|23309|5|Briefly described|p338||Silurian|G119 I-Type. Age: 425+/-9 Ma.||||||
34844|Mountain Maid Granite|24551|6|Mentioned|p717 Table 2.4|Wenlock|Wenlock|Age: ~425Ma.||||||
34844|Mountain Maid Granite|61160|5|Briefly described|p120|Early Silurian|Early Silurian|Pluton on OMEO. Age: 425+/-9Ma||||||
34844|Mountain Maid Granite|68116|5|Briefly described|Appendix, Map 35.|Wenlock|Llandovery||||||Biotite granite: pale grey; fine-grained; equigranular; massive.|
30683|Mowamba Porphyries|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
30683|Mowamba Porphyries|23309|6|Mentioned|p345|||||||||
30683|Mowamba Porphyries|23938|6|Mentioned|p84|||Shows strong magnetic alteration.||||||25-SEP-08
30683|Mowamba Porphyries|60503|4|Described|p171, p42 Tb. 2|Early Devonian|Early Devonian|Collective name for the 3 small plutons adjacent to Wombat Creek Graben, including the Mowamba Porphyry. Consist of phenocrysts of embayed quartz and sericitised feldspar in a groundmass of altered feldspar laths. Age: 413+/-6Ma.||||||25-SEP-08
30683|Mowamba Porphyries|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Intrusive stocks: green, medium grained, strong epidote, sericite and chlorite alteration of relict hornblende and feldspar.||||||20-OCT-04
30683|Mowamba Porphyries|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Intrusive stocks: green, medium grained, strong epidote, sericite and chlorite alteration of relict hornblende and feldspar.||||||21-OCT-04
30683|Mowamba Porphyries|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Intrusive stocks: green, medium grained, strong epidote, sericite and chlorite alteration of relict hornblende and feldspar.||||||21-OCT-04
30683|Mowamba Porphyries|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Intrusive stocks: green, medium grained, strong epidote, sericite and chlorite alteration of relict hornblende and feldspar.||||||21-OCT-04
30683|Mowamba Porphyries|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Stocks: 413+/-6 Ma (U/Pb zircon); small moderately magnetic (50 nT) on larger sub-surface high; moderate total count, K, Th, U.||||||25-SEP-08
30683|Mowamba Porphyries|68116|5|Briefly described|Appendix, Map 27.|Early Devonian|Early Devonian||||||Quartz-feldspar porphyry: green; medium-grained; strong epidote, sericite and chlorite alteration of relict hornblende and feldspar.|
27209|Mowambah Granodiorite|22815|4|Described|p45|Silurian|Silurian|||||||
27209|Mowambah Granodiorite|35109|2|Defined|p55|Early Devonian|Late Silurian|Late Silurian-Early Devonian||||||
27209|Mowambah Granodiorite|35263|6|Mentioned|p222|||Correct spelling of Mowamba||||||
27209|Mowambah Granodiorite|37544|6|Mentioned|p496|||||||||
27209|Mowambah Granodiorite|41898|6|Mentioned|p1184|||||||||
27209|Mowambah Granodiorite|41905|4|Described|p78|||||||||
27209|Mowambah Granodiorite|41933|5|Briefly described|Map legend|Late Silurian||||||||
27209|Mowambah Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Bullenbalong Suite.||||||
27209|Mowambah Granodiorite|49705|6|Mentioned|p19|||||||||
27209|Mowambah Granodiorite|68115|5|Briefly described|p7.|||Deddick Zone. White et al.(1977). Previously shown on GSV maps as Ingeegoodbee Granodiorite; the usage Mowambah Granodiorite has precedence.||||||
27209|Mowambah Granodiorite|68116|5|Briefly described|Appendix, Map 28.|Wenlock|Wenlock||||||Biotite granodiorite: contains cordierite, sillimanite and accessory monazite, ilmenite and pyrrhotite; common metasedimentary xenoliths; mafic S-type.|
13290|Moyne Alluvium|24551|5|Briefly described|p343, 345||Holocene|Age: 18ka to present.  Of the Bridgewater Group.||||||
13290|Moyne Alluvium|34993|5|Briefly described|p303|||||||||
13290|Moyne Alluvium|35722|6|Mentioned|Table 2|||Quaternary stratigraphic units and nature of components.||||||
13290|Moyne Alluvium|41769|4|Described|p55|||||||||
13290|Moyne Alluvium|41848|5|Briefly described|p378|||Age mid and late Holocene||||||
13290|Moyne Alluvium|73386|6|Mentioned|p14|||||Bridgewater Formation||||
35599|Mudgee Granite|23275|6|Mentioned|p472||Carboniferous|||||||
23845|Mullum Mullum Sandstone Member|22542|6|Mentioned|p661|||||||||
23845|Mullum Mullum Sandstone Member|22684|5|Briefly described|p753, Fig.2 p746|Wenlock|Wenlock|||||||
23845|Mullum Mullum Sandstone Member|23309|5|Briefly described|p140|||||||||
23845|Mullum Mullum Sandstone Member|38787|6|Mentioned|Fig.2|||||||||
23845|Mullum Mullum Sandstone Member|62469|6|Mentioned|p5 Fig. 2|Wenlock|Wenlock|Of Yan Yean Formation.||||||
13426|Mundawandra Granite|42726|5|Briefly described|map legend|||||||||
34835|Mungobabba Tonalite|22968|5|Briefly described|P40, Table7, P184||Early Devonian|Age of unit is 408+/-16Ma, New name||||||
34835|Mungobabba Tonalite|23029|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Rileys Creek Suite. Biotite tonalite: I-type; grey, medium grained, massive; rare small dark enclaves||||||14-SEP-04
34835|Mungobabba Tonalite|23030|5|Briefly described|Map legend|Early Devonian|Late Silurian|Parent is the Rileys Creek Suite. Biotite tonalite: I-type; 408+/-16Ma (K/Ar): moderately to highly magnetic (on northern margin), elevated magnetic intensity directly north of pluton; moderate K & Th, low U; low K, high Th, moderate U in northwest.||||||14-SEP-04
34835|Mungobabba Tonalite|23309|5|Briefly described|p439 App1|Early Devonian|Silurian|G143 I-Type. Supersedes Tongio Gap Tonalite.  Age: 408+/-16 Ma.||||||
34835|Mungobabba Tonalite|61161|5|Briefly described|p93|Early Devonian|Early Silurian|Of Rileys Creek Suite. GSV map code: G143.||||||
34835|Mungobabba Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Biotite tonalite: grey; medium-grained; equigranular; massive.|
22481|Murderers Hill Siltstone|23309|5|Briefly described|p146, 148, 151, 155. Tb 2.54|Silurian|Silurian|Age: Pridoli/Wenlock.||||||22-DEC-08
22481|Murderers Hill Siltstone|24214|6|Mentioned|p788 Fig. 2|||||||||
22481|Murderers Hill Siltstone|24551|6|Mentioned|p33|Late Silurian|Middle Silurian|||||||
22481|Murderers Hill Siltstone|44187|5|Briefly described|Map Legend||Late Silurian|||||||
22481|Murderers Hill Siltstone|64535|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Brown, purple and green siltstone, thinly laminated; pale sandstone, thin bedded, fine-grained, quartzose and lithic; deep marine hemipelagic and turbidite deposits.||||||22-DEC-08
22481|Murderers Hill Siltstone|64536|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Contains Snake-Edwards Sandstone Member. Brown, purple, green siltstone, thinly laminated; pale, thin-bedded sandstone, fine-grained, quartzose and lithic. Deep-marine hemipelagic and turbidite deposits.||||||07-FEB-11
22481|Murderers Hill Siltstone|64537|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Contains Snake-Edwards Sandstone Member. Brown, purple, green siltstone, thinly laminated; pale, thin-bedded sandstone, fine-grained, quartzose and lithic. Deep-marine hemipelagic and turbidite deposits.||||||07-FEB-11
22481|Murderers Hill Siltstone|64538|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Contains Snake-Edwards Sandstone Member. Brown, purple, green siltstone, thinly laminated; pale, thin-bedded sandstone, fine-grained, quartzose and lithic. Deep-marine hemipelagic and turbidite deposits.||||||07-FEB-11
22481|Murderers Hill Siltstone|64539|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Brown, purple and green siltstone, thinly laminated; pale sandstone, thin bedded, fine-grained, quartzose and lithic; deep marine hemipelagic and turbidite deposits.||||||22-DEC-08
22481|Murderers Hill Siltstone|64540|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Brown, purple and green siltstone, thinly laminated; pale sandstone, thin bedded, fine-grained, quartzose and lithic; deep marine hemipelagic and turbidite deposits.||||||22-DEC-08
22481|Murderers Hill Siltstone|64605|5|Briefly described|Map legend|Silurian|Silurian|Of the Jordan River Group. Siltstone, minor sandstone; deep-marine deposits. Blue-pink-white in RGB. Nonmagnetic.||||||17-NOV-08
22481|Murderers Hill Siltstone|64606|5|Briefly described|Map Legend|Silurian|Silurian|Of Jordan River Group. Includes Snake-Edwards Sandstone Member. Siltstone, minor sandstone: deep-marine deposits. Blue-pink-white in RGB. Nonmagnetic.||||||11-NOV-08
22481|Murderers Hill Siltstone|64616|3|Fully described|p79, p173-176, p185, p291, p305-306|Ludlow|Wenlock|VandenBerg et al., (1995). Of Jordan River Group. Conformably overlies Serpentine Creek Sandstone. Equivalent to Whitelaw Siltstone. Thinly laminated siltstone; minor thin-bedded, fine-grained, quartzose and lithic sandstone. Top faulted. Includes Snake-Edwards Sandstone Member, containing early Ludlow graptolites. Appears as Murderers Creek Siltstone on p173. Geophysical characteristics given.||||||
22481|Murderers Hill Siltstone|68116|5|Briefly described|Appendix, Maps 34, 43, 52.|Lochkovian|Telychian||||||Siltstone, minor sandstone: siltstone brown, purple and green, thinly laminated; sandstone pale, thin-bedded, fine-grained, quartzose and lithic.|
13522|Murmungee Granodiorite|23309|5|Briefly described|p346||Devonian|G199 I-Type Age: 376+/-4 Ma. Supersedes Murmungee Granite and Murmungee Basin Granodiorite.||||||27-NOV-09
13522|Murmungee Granodiorite|24551|6|Mentioned|p229, 725 Table 8.8|||Of the Tabberabbera Province.||||||
13522|Murmungee Granodiorite|41563|6|Mentioned|p514|||||||||
13522|Murmungee Granodiorite|41850|6|Mentioned|p432|||||||||
13522|Murmungee Granodiorite|42827|6|Mentioned|p432|||||||||
13522|Murmungee Granodiorite|68116|5|Briefly described|Appendix, Map 19.|Late Devonian|Late Devonian||||||Hornblende-biotite granodiorite: grey, medium grained, equigranular with accessory magnetite, sphene, allanite and pyroxene; marginal leucocratic granite; I-type; highly magnetic.|
31654|Murmungee Suite|42726|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|||||||
31654|Murmungee Suite|61163|6|Mentioned|p119|||Contains Mount Angus Granodiorite according to Chappell (1988) as it has the same chemical features.||||||
83436|Murnungin pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G649.||Of Glenloth Suite|||Distinctly magnetically layered, with alternating nonmagnetic and magnetic (to 80 nT) layers; a 10 micrometres/second/second gravity high in the northeast, but a 50 micrometres/second/second low in the south.|
83436|Murnungin pluton|73505|5|Briefly described|p18, p20|||Newly named unit in Swan Hill and parts of Balranald and Deniliquin 1:250 000 map areas, (G649). Named after Murnungin Parish. Irregularly shaped intrusion about 10km west of Meatian and 35km east of Sea Lake, on the northeast edge of Lalbert Batholith. Distinctly magnetically layered, with alternating nonmagnetic and magnetic (to 80 nT) layers. Gravity response of a 10 micrometres/second/second gravity high in the northeast, and a 50 micrometres/second/second low in the south.|||||Granite.|
83409|Murrabit pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G657.|||||Magnetic response shows a strongly zoned pluton, with the northwestern part nonmagnetic and the southeastern part with responses to 80 nT;  gravity about 40 micrometres/second/second lower than the regional.|
73494|Murraduc Basalt|65715|3|Fully described|p14 Tb.8, p15|Neogene|Neogene|Newly defined here. Main constituent of Bellarine Volcanic Group. Basalt lavas. Type locality is the basalt quarry on Murraduc Hill (MGA ref given). Includes all inland outcrops of 'Older Basalt' on Bellarine Peninsula and  coastal cliffs at Curlewis. Unconformably overlies Eumeralla Formation. Underlies Clifton Springs Tuff.||||||09-FEB-15
73494|Murraduc Basalt|68116|5|Briefly described|Appendix, Map 50.|Miocene|Miocene||||||Olivine basalt.|
37766|Murray Gates Leucogranite|23309|6|Mentioned|p439, Appendix 1|||G577, A-Type.||||||
37766|Murray Gates Leucogranite|24133|3|Fully described|p81|||Intrudes Harringtons Tonalite.  Geological Province: Lachlan Fold Belt.||||||
37766|Murray Gates Leucogranite|24142|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37766|Murray Gates Leucogranite|24143|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37766|Murray Gates Leucogranite|24144|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37766|Murray Gates Leucogranite|24145|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Geological Province: Lachlan Fold Belt||||||
37766|Murray Gates Leucogranite|24146|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37766|Murray Gates Leucogranite|68116|5|Briefly described|Appendix.|Middle Devonian|Early Devonian||||||Leucogranite: grey to pink, medium to coarse grained; up to 5% biotite; massive and equigranular with some porphyritic phases; nonmagnetic. Includes small pods of pegmatite, which occur as dykes and blebs.|
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.|
30432|Murray Hill Sandstone|23309|5|Briefly described|p205, 78|||Maximum Thickness: 300m.  Of the Red Man Bluff Subgroup.||||||
30432|Murray Hill Sandstone|44929|5|Briefly described|Map Legend|Silurian|Ordovician|Of Red Man Bluff Sub-Group (Grampians Group). Pale yellow, pebbly quartzo-feldspathic sandstone, fine- to coarse-grained.||||||14-JUN-06
30432|Murray Hill Sandstone|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Man Bluff Sub-Group (Grampians Group). Pale yellow, pebbly quartzo-feldspathic sandstone, fine- to coarse-grained.||||||13-JUN-06
30432|Murray Hill Sandstone|44932|5|Briefly described|Map Legend|Silurian|Ordovician|Of Red Man Bluff Sub-Group (Grampians Group). Pale yellow, pebbly quartzo-feldspathic sandstone, fine- to coarse-grained.||||||14-JUN-06
30432|Murray Hill Sandstone|44933|5|Briefly described|Map Legend|Silurian|Ordovician|Of Red Man Bluff Sub-Group. Pale yellow, pebbly quartzo-feldspathic sandstone, fine- to coarse-grained.||||||14-JUN-06
30432|Murray Hill Sandstone|60451|4|Described|p76, 79|Early Devonian|Ordovician|Of the Red Man Bluff Subgroup (Grampians Group). Maximum Thickness: ~300m. Type section in text. Consists of medium grained quartzo-feldspathic sandstone with numerous pebble lag horizons in the east.||||||
30432|Murray Hill Sandstone|60456|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Man Bluff Sub-Group. Sandstone:pale yellow, pebbly quartzo-feldspathic, fine to coarse grained; with planar, cross and trough cross lamination, medium to thickly bedded.||||||30-SEP-04
30432|Murray Hill Sandstone|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Man Bluff Subgroup. Sandstone, pale yellow; pebbly quartzo-feldspathic, fine to coarse grained; with planar, cross and trough cross lamination, medium to thickly bedded.||||||
30432|Murray Hill Sandstone|61183|4|Described|p17, p30 Tb. 2, p38, p79|||Of Red Man Bluff Subgp (Grampians Gp). Includes Pohlner Conglomerate Bed (member). Thick-bedded, coarse-grained, quartzo-feldspathic sst with laminated fine grained sst intervals. Overlies Watgania Gap Sst; underlies Kalymna Falls Sst. Thickness: ~300m.||||||
30432|Murray Hill Sandstone|64541|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Red Man Bluff Sub-group. Sandstone: pale yellow, pebbly quartzo-feldspathic, fine to coarse grained; laminated, cross-laminated and trough cross-laminated, medium to thickly bedded.||||||07-FEB-11
30432|Murray Hill Sandstone|64610|5|Briefly described|Map legend|Ordovician|Ordovician|Of Red Man Bluff Subgroup (Grampians Gp). Contains the Pohlner Conglomerate Bed. Sandstone pale yellow, pebbly quartzo-feldspathic; fine- to coarse-grained; laminated, x -laminated + trough x-laminated, medium to thickly bedded; forms prominent outcrops.||||||11-NOV-08
30432|Murray Hill Sandstone|65313|6|Mentioned|p582, Fig 10, p581 Fig. 9|Llandovery|Llandovery|Basal age of ~444 Ma supported by pedostratigraphy. Grampians National Park sections.||Of Red Man Bluff Subgroup.||Overlies Watgania Gap Sandstone; underlies Kalymna Falls Sandstone.||26-MAR-12
30432|Murray Hill Sandstone|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Red Man Bluff Subgroup. Includes Pohlner Conglomerate Member. Defined by Cayley & Taylor, 1997.||||||
30432|Murray Hill Sandstone|68116|5|Briefly described|Appendix, Maps 22, 30.|Ludlow|Late Ordovician||||||Sandstone: pale yellow; pebbly; quartzo-feldspathic; fine to coarse-grained; variably laminated; medium to thick-bedded; forms prominent outcrops; strong thorium radiometric response suggests relatively high detrital monazite content.|
26788|Murrindal Limestone|22520|6|Mentioned|p18|Emsian|Emsian|||||||
26788|Murrindal Limestone|23309|4|Described|p118, Tb 2.41||Emsian|Of the Buchan Group.||||||
26788|Murrindal Limestone|23522|5|Briefly described|p247 Fig 3|Early Devonian|Early Devonian|||||||
26788|Murrindal Limestone|23615|3|Fully described|p141, p189|Early Devonian|Early Devonian|Of Buchan Group.  See also p216 App 2.  Lenticular unit divided into two members; McLarty Limestone Member (lower) and Rocky Camp Limestone Member (upper).  Age: late Early to Middle Devonian ~395-385Ma.  Max. thickness: 290m.||||||16-AUG-18
26788|Murrindal Limestone|23710|14|Not recorded|p74|||Facies relationships.||||||
26788|Murrindal Limestone|24551|4|Described|p147, p141 Fig.  5.32|Early Devonian|Early Devonian|Of Buchan Group. ||||||
26788|Murrindal Limestone|24598|5|Briefly described|p514|||Overlain by Taravale Limestone.  Max. thickness: ~360m.  Geological Province: Lachlan Orogen.||||||
26788|Murrindal Limestone|30245|6|Mentioned|p80|||||||||
26788|Murrindal Limestone|30597|6|Mentioned|p33|||Lower Devonian age||||||
26788|Murrindal Limestone|31331|6|Mentioned|p181|||See also p182.||||||30-JAN-07
26788|Murrindal Limestone|31502|5|Briefly described|p95|||Devonian corals. Age||||||
26788|Murrindal Limestone|32585|6|Mentioned|p212|||||||||
26788|Murrindal Limestone|32984|6|Mentioned|p344|||Fossil content||||||
26788|Murrindal Limestone|32985|6|Mentioned|Fig.2|||Correlation chart||||||
26788|Murrindal Limestone|33393|6|Mentioned|p163|||||||||
26788|Murrindal Limestone|33434|6|Mentioned|p19|||||||||
26788|Murrindal Limestone|33481|6|Mentioned|Fig.1|||||||||
26788|Murrindal Limestone|33602|6|Mentioned|Map legend|Devonian|Devonian|||||||
26788|Murrindal Limestone|33606|5|Briefly described|p65|||||||||
26788|Murrindal Limestone|33732|6|Mentioned|Table III|||||||||
26788|Murrindal Limestone|34250|5|Briefly described|p22|||Emsian or Couvinian||||||
26788|Murrindal Limestone|34519|6|Mentioned|p45|||||||||
26788|Murrindal Limestone|34926|6|Mentioned|p120|||||||||
26788|Murrindal Limestone|34954|6|Mentioned|Fig.34|||Analysis Fig.33.||||||
26788|Murrindal Limestone|34964|6|Mentioned|p452|||||||||
26788|Murrindal Limestone|35112|6|Mentioned|p285|||||||||
26788|Murrindal Limestone|35274|4|Described|p420|||||||||
26788|Murrindal Limestone|35283|6|Mentioned|p49|||||||||
26788|Murrindal Limestone|36201|5|Briefly described|p6|||||||||
26788|Murrindal Limestone|37330|5|Briefly described|p15|||||||||
26788|Murrindal Limestone|38367|6|Mentioned|Fig.11|||||||||
26788|Murrindal Limestone|39447|6|Mentioned|Fig.2|||||||||
26788|Murrindal Limestone|40728|6|Mentioned|p173|||||||||
26788|Murrindal Limestone|41585|5|Briefly described|p138|||||||||
26788|Murrindal Limestone|41868|5|Briefly described|p574|||||||||
26788|Murrindal Limestone|42032|5|Briefly described|p498|||||||||
26788|Murrindal Limestone|42577|5|Briefly described|p27|||Previously informally called "Shanahan Limestone"||||||
26788|Murrindal Limestone|42635|5|Briefly described|p27|||||||||
26788|Murrindal Limestone|42827|5|Briefly described|p138|||||||||
26788|Murrindal Limestone|42967|5|Briefly described|p76 Fig.1|||||||||
26788|Murrindal Limestone|43206|5|Briefly described|map legend||Emsian|Of Buchan Group||||||
26788|Murrindal Limestone|43228|5|Briefly described|p10||Early Devonian|||||||
26788|Murrindal Limestone|43431|14|Not recorded|p1263,1265|||L.Devn.conodont||||||
26788|Murrindal Limestone|43525|14|Not recorded|Table p132|||||||||
26788|Murrindal Limestone|43529|14|Not recorded|p235,text-fig 1||Emsian|||||||
26788|Murrindal Limestone|43530|14|Not recorded|p1028||Emsian|||||||
26788|Murrindal Limestone|43532|14|Not recorded|p204||Devonian|Revision of Devonian Mictophyllum. See also Lexicon||||||
26788|Murrindal Limestone|43533|14|Not recorded|p121,122,130||Emsian|L.Devn corals||||||
26788|Murrindal Limestone|43537|14|Not recorded|p21|||||||||
26788|Murrindal Limestone|43547|14|Not recorded|p151,Tb p153,161|Eifelian|Emsian|(U.Emsian-Eifelian) Equivalent to Taravale Formation. Part of Buchan Group||||||
26788|Murrindal Limestone|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Unit in Buchan Group.|||Marine: massive, pale grey recrystallised limestone.|
26788|Murrindal Limestone|44216|14|Not recorded|p390|||||||||
26788|Murrindal Limestone|45075|6|Mentioned|p29|||Devonian||||||
26788|Murrindal Limestone|48971|6|Mentioned|p26|||||||||
26788|Murrindal Limestone|50077|6|Mentioned|p7|||Contains the McLarty Member.  Well bedded and massive limestones with subordinate mudstones.  Overlies the Buchan Caves Limestone.||||||
26788|Murrindal Limestone|61181|5|Briefly described|p69, p127|Devonian|Devonian|Top of Buchan Group. Includes McLarty (lower) and Rocky Camp (top) Members. Pale to dark grey limestone interbedded with mudstone, grading into argillaceous limestone of overlying Taravale Limestone. Overlies Buchan Caves Limestone. Max. thickness: 250m.||||||
26788|Murrindal Limestone|61187|6|Mentioned|p138, p139 Fig.1, p142 Fig.3.|Early Devonian|Early Devonian|||Unit in Buchan Group.||||
26788|Murrindal Limestone|62735|6|Mentioned|p987|Emsian|Emsian|Contains scutellum fossils.  In Victoria.||||||
26788|Murrindal Limestone|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Buchan. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
26788|Murrindal Limestone|65940|6|Mentioned|p210|Emsian|Emsian|Buchan, VIC. Contains Alveolites stamineus (Hill, 1950).||||||
26788|Murrindal Limestone|68116|5|Briefly described|Appendix, Map 36.|Emsian|Emsian||||||Limestone: massive, pale grey, recrystallized; also fossiliferous bedded limestone.|
26788|Murrindal Limestone|70742|6|Mentioned|p168|Early Devonian|Early Devonian|Hosted the type specimens of Parachonetes buchanensis.||||||
35522|Murrindindi Supergroup|23309|5|Briefly described|p134-156, 247, 258|Early Devonian|Silurian|||||||
35522|Murrindindi Supergroup|24002|5|Briefly described|p245|Devonian|Silurian|||||||
35522|Murrindindi Supergroup|24098|5|Briefly described|p27 Fig. 2|Devonian|Silurian|Geological Province: Melbourne Zone,  Lachlan Fold Belt (Darraweit Guim and Mount Easton).||||||19-APR-05
35522|Murrindindi Supergroup|24133|5|Briefly described|p20 Fig. 8|Early Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||
35522|Murrindindi Supergroup|24134|5|Briefly described|p6 Fig. 2|Early Devonian|Silurian|||||||
35522|Murrindindi Supergroup|24178|5|Briefly described|p15 Fig.2|Early Devonian|Silurian|Geological Province: Bendigo Zone||||||
35522|Murrindindi Supergroup|24383|6|Mentioned|p88 Fig.57|||Geological Province: Lachlan Fold Belt||||||
35522|Murrindindi Supergroup|24439|5|Briefly described|p7 Fig. 2|Devonian|Ordovician|||||||
35522|Murrindindi Supergroup|24551|3|Fully described|p123|Middle Devonian|Silurian|Overlies Sunbury Group. First introduced by VandenBerg (2000).||||||
35522|Murrindindi Supergroup|24588|5|Briefly described|p10, p12, p23 Fig.11, p29|Early Devonian|Silurian|Geological Province: Lachlan Fold Belt. Basal unit is Deep Creek Siltstone. Overlies: Sunbury Group.||||||29-NOV-13
35522|Murrindindi Supergroup|64611|5|Briefly described|Map legend|Silurian|Silurian|Comprises Broadford Formation,  McIvor Sandstone, Dargile and Wapentake Formations, Kilmore Siltstone, Chintin Formation and Springfield Sandstone.||||||15-DEC-08
35522|Murrindindi Supergroup|64612|2|Defined|p25 Fig. 5.1, p27, p37, p42, p57|Early Devonian|Silurian|Includes 6 formations. Underlain by Bolinda Shale. Geological province: Melbourne Zone. Basal unit shows burrows. Figure 5.1 has been misspelt.||||||01-JUL-13
35522|Murrindindi Supergroup|64616|4|Described|p72, p152, p159, p178-179, p181-183|Middle Devonian|Ordovician|See also p186, p188, p192, p197 Fig.6.34, p212, p343 Fig.23. Includes Jordan River and Walhalla Groups in this project area. Dominated by siltstone and quartz rich sandstone. Affected by Tabberabberan and Kanimblan Orogenies. Also appears as Murrindindi Group on p192 and Fig.6.34. Marked E-W differences in thickness. Hosts Late Devonian gold mineralisation.||||||
35522|Murrindindi Supergroup|65715|6|Mentioned|p5|||In Melbourne Zone.||||||
35522|Murrindindi Supergroup|65900|5|Briefly described|p161|Early Devonian|Silurian||||Includes the Jordan River Group and the Walhalla Group.|Overlies Mount Easton Shale.|Thick sequence of marine clastic sediments.|10-MAY-12
35522|Murrindindi Supergroup|65969|5|Briefly described|p13, p31|Devonian|Silurian|Darraweit Guim Province; Melbourne Zone. Sandstone and siltstone turbidite rocks; sandier in the W and siltier in the SE. Stratigraphic thickness of >7 km. Deformed c.380 Ma in the Tabberabberan Orogeny.||||||
35522|Murrindindi Supergroup|66576|6|Mentioned|p972.||||||Includes Walhalla Group.|||
35522|Murrindindi Supergroup|66769|5|Briefly described|119, 123, 133|Devonian|Ordovician|Thick wedge of sediments, conformably overlies Ordovician turbidites and shales. Up to 10km thick. Deformed during Tabberabberan Orogeny to form the Melbourne Zone.||||||
35522|Murrindindi Supergroup|68116|5|Briefly described|Appendix, Map 51.|Middle Devonian|Late Ordovician||||||Siltstone, shale, sandstone, rare conglomerate and limestone; sandstone typically quartz-rich in the lower part and lithic in the upper part; siltstone commonly bioturbated; marine to fluvial.|
35522|Murrindindi Supergroup|70629|6|Mentioned|p986|Early Devonian|Silurian|Melbourne Zone.||||||
35522|Murrindindi Supergroup|70742|5|Briefly described|p161, p163|Middle Devonian|Early Silurian|VandenBerg et al.(2000). Melbourne Structural Zone. Dates are uncertain for the upper parts.|||Jordan River, Walhalla, Cathedral Groups.|||
35522|Murrindindi Supergroup|73497|5|Briefly described|Map legend|Devonian|Silurian||||Waranga Formation, Humevale Siltstone, Mount Ida Formation, Puckapunyal Formation, Broadford Formation, McIvor Sandstone, Dargile Formation, Wapentake Formation, Costerfield Siltstone|||
26789|Murrungowar Granite|23309|6|Mentioned|p440 App1|||Superseded by Murrungowar Granodiorite.||||||21-OCT-10
26789|Murrungowar Granite|33238|6|Mentioned|p644|||||||||
26789|Murrungowar Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
26789|Murrungowar Granite|60541|4|Described|p69|||Intrusive in Kuark Met.Complex. A-type. May also intrude Tarlton pluton. Xenoliths of folded schist are common; foliation is defined by dark tabular inclusions of biotite schist and anastomosing biotite-rich bands in the groundmass; lg,aligned K-feldspar||||||21-JUN-05
26789|Murrungowar Granite|68116|5|Briefly described|Appendix, Map 45.|Wenlock|Llandovery||||||Biotite-muscovite granite: coarse-grained porphyritic; foliated; contains numerous aligned orthoclase phenocrysts and mafic enclaves.|
26789|Murrungowar Granite|71206|6|Mentioned|p373, 377, 382, 384|||Lachlan Fold Belt. Geochemistry graphs.||Murrungowar Suite.|||Aluminous A-type granite.|
31631|Murrungowar Suite|42726|5|Briefly described|map legend||Middle Devonian|||||||
31631|Murrungowar Suite|71206|6|Mentioned|p373, 377, 387|||Lachlan Fold Belt. Sr/Nd plot.|||Murrungowar Granite.||Aluminous A-type granite.|
37584|Murtagh Creek Ignimbrite|23309|5|Briefly described|p122, 124, 133. Table 2.45|||Of Dartella Volcanics.||||||
37584|Murtagh Creek Ignimbrite|24133|3|Fully described|p48|Devonian|Devonian|Parent: Dartella Volcanic Group.||||||
37584|Murtagh Creek Ignimbrite|24142|5|Briefly described|Map Legend|Devonian|Devonian|Of Dartella Volcanic Group. Geological Province: Lachlan Fold Belt.||||||
37584|Murtagh Creek Ignimbrite|24143|5|Briefly described|Map Legend|Devonian|Devonian|Of Dartella Volcanic Group. Geological Province: Lachlan Fold Belt.||||||
37584|Murtagh Creek Ignimbrite|24144|5|Briefly described|Map Legend|Devonian|Devonian|Of Dartella Volcanic Group. Geological Province: Lachlan Fold Belt.||||||
37584|Murtagh Creek Ignimbrite|24145|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of Dartella Volcanic Group. Geological Province: Lachlan Fold Belt||||||
37584|Murtagh Creek Ignimbrite|24146|5|Briefly described|Map Legend|Devonian|Devonian|Of Dartella Volcanic Group. Geological Province: Lachlan Fold Belt.||||||
37584|Murtagh Creek Ignimbrite|24551|5|Briefly described|p149|Devonian|Devonian|Of Dartella Volcanics.||||||
37584|Murtagh Creek Ignimbrite|60503|3|Fully described|p117-121, p41 Tb. 2|Early Devonian|Early Devonian|Of the Dartella Volcanics. Ignimbrite. Conformably overlies Dart River Volcanic Breccia, Tabor Volcanics; unconformable on Dartmouth Granite. Underlies Larsen Creek Ignimbrite. Max. thickness: >600m.||||||16-NOV-09
37584|Murtagh Creek Ignimbrite|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Ignimbrite: minor bedrock-lithic breccia, lahar deposits: rhyolitic red quartz ignimbrite with large quartz and feldspar ignimbrite and cognate porphyry pyroclasts, with very abundant shale lithic fragments in the west.||||||21-OCT-04
37584|Murtagh Creek Ignimbrite|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Ignimbrite: minor bedrock-lithic breccia, lahar deposits: rhyolitic red quartz ignimbrite with large quartz and feldspar ignimbrite and cognate porphyry pyroclasts, with very abundant shale lithic fragments in the west.||||||21-OCT-04
37584|Murtagh Creek Ignimbrite|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Ignimbrite: minor bedrock-lithic breccia, lahar deposits: rhyolitic red quartz ignimbrite with large quartz and feldspar ignimbrite and cognate porphyry pyroclasts, with very abundant shale lithic fragments in the west.||||||21-OCT-04
37584|Murtagh Creek Ignimbrite|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Ignimbrite: minor bedrock-lithic breccia, lahar deposits: rhyolitic red quartz ignimbrite with large quartz and feldspar ignimbrite and cognate porphyry pyroclasts, with very abundant shale lithic fragments in the west.||||||21-OCT-04
37584|Murtagh Creek Ignimbrite|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Dartella Volcanic Group. Ignimbrite: weakly and moderately magnetic flows (5-50 nT); low to moderate K, low total count, Th, U||||||21-OCT-04
37584|Murtagh Creek Ignimbrite|68116|5|Briefly described|Appendix, Maps 20, 27.|Middle Devonian|Early Devonian||||||Rhyolitic ignimbrite, minor breccia, lahar deposits: rhyolitic red quartz ignimbrite with large quartz and feldspar ignimbrite and cognate porphyry pyroclasts, with very abundant slate lithic fragments in the west; breccias rich in bedrock lithics.|
13610|Mussel Formation|22944|5|Briefly described|Fig3|Eocene|Paleocene|||||||
13610|Mussel Formation|41185|6|Mentioned|Fig.4|||||||||
13610|Mussel Formation|41704|6|Mentioned|Fig.3|||||||||
13610|Mussel Formation|42524|5|Briefly described|Fig.3 P27|||||||||
13610|Mussel Formation|42555|5|Briefly described|Fig.2 P285|||||||||
13610|Mussel Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
13610|Mussel Formation|43660|6|Mentioned|Fig.6,p15|Eocene|Paleocene|||||||
13610|Mussel Formation|61155|5|Briefly described|p18|Late Paleocene|Late Paleocene|Over and under and interfingers with Pember Mudstone. ||||||
13643|Myaring beds|31624|4|Described|p115|||See also P117 and Table 5-3||||||
74868|Mystic Park Formation|65719|5|Briefly described|p7|Miocene|Oligocene|In Murray Basin. Lateral equivalent of Geera Clay and Parilla Sand. Marginal marine or paralic.||||||10-MAY-12
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.|
31537|Nalbaugh Suite|22815|5|Briefly described|p82|||||||||
31537|Nalbaugh Suite|22878|6|Mentioned|p74|||||||||
31537|Nalbaugh Suite|24551|6|Mentioned|p235|||||||||
31537|Nalbaugh Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31537|Nalbaugh Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||
73909|Nampoo Member|64961|2|Defined|p262, p263 Fig. 3, 270|Early Pleistocene|Early Pleistocene|A very distinctive unit of Blanchetown Clay, overlying the main clay sequence above the basal Chowilla Sand. Age: 1.6-1.4Ga. Type section given. Max. thickness: 3m. Comprises a basal pure quartz silt, often laminated, etc.||||||
24418|Nanapundah Tuff|23229|5|Briefly described|Table3-1p16, 16|Early Cambrian|Cambrian|||||||
24418|Nanapundah Tuff|23309|5|Briefly described|p35 Table 2.6|Cambrian|Cambrian|||||||
24418|Nanapundah Tuff|23402|3|Fully described|p10, p8 Tb. 1|Late Cambrian|Late Cambrian|Parent: Mount Stavely Volcanic Complex.   Thickness: 800m.   Overlies/intertongues with Fairview Andesite Breccia.   Geological Province: Adelaide Fold Belt||||||
24418|Nanapundah Tuff|24551|5|Briefly described|p79|||Of the Mount Stavely Volcanic Complex.||||||03-AUG-05
24418|Nanapundah Tuff|38436|4|Described|p425|||See also Fig.2.||||||
24418|Nanapundah Tuff|40172|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
24418|Nanapundah Tuff|40761|5|Briefly described|Table 1|||||||||
24418|Nanapundah Tuff|40887|2|Defined|p15|Cambrian|Cambrian|Prob. Cambrian||||||
24418|Nanapundah Tuff|41571|6|Mentioned|Table 2.2|||||||||
24418|Nanapundah Tuff|50371|5|Briefly described|Map Legend|Cambrian|Cambrian|Of Mount Stavely Volcanic Complex. Andesitic crystal lithic volcanic sandstone||||||11-JUN-04
24418|Nanapundah Tuff|61187|5|Briefly described|p69 Fig.2, p130. |Early Cambrian|Early Cambrian|Nonmagnetic to weakly magnetic.||Unit in Mount Stavely Volcanic Complex.||||
24418|Nanapundah Tuff|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Mount Stavely Volcanic Complex. Defined by Buckland 1986.||||||
24418|Nanapundah Tuff|68116|5|Briefly described|Appendix, Map 39.|Cambrian|Cambrian||||||Andesitic crystal lithic volcanic sandstone: massive, variably sorted, partly laminated.|
24418|Nanapundah Tuff|70877|6|Mentioned|p48, p61|||||Mount Stavely Volcanic Complex||Structurally overlain by the Towanway Tuff.||
24418|Nanapundah Tuff|70967|6|Mentioned|p28|||Stavely Belt.||||||
24418|Nanapundah Tuff|71593|4|Described|p9, p29, p39, p163|||The type locality for this unit occurs in the Stavely Belt segment.||Mount Stavely Volcanic Complex||||
41179|Nangeela Formation|50154|2|Defined|p22, p52, p62|Early Cambrian|Early Cambrian|Of the Moralana Supergroup. Interlayered with the Truro Volcanics. Includes Steep Bank Greywacke Member and Warrock LImestone Member. Correlates with the Normanville and Kanmantoo groups. Geological Province: Glenelg Zone, Delamerian Fold Belt.||||||15-SEP-04
41179|Nangeela Formation|50156|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Overlain by Eumeralla Formation. Black graphite slate with pyrite; black dolomitic slate with pyrite; chlorite-sericite slate and metasiltstone; thin greywacke interbeds.||||||25-JUN-04
41179|Nangeela Formation|50157|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Black graphite slate with pyrite; black dolomitic slate with pyrite; chlorite-sericite slate and metasiltstone; thin greywacke interbeds.||||||24-JUN-04
41179|Nangeela Formation|50158|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Includes: Warrock Limestone Member, Steep Bank Greywacke Member. Black graphitic and dolomitic slate with pyrite; chlorite-sericite slate and metasiltstone; thin greywacke interbeds.||||||
41179|Nangeela Formation|50159|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Black graphite slate with pyrite; black dolomitic slate with pyrite; chlorite-sericite slate and metasiltstone; thin greywacke interbeds.||||||
41179|Nangeela Formation|50160|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Includes: Warrock Limestone Member, Steep Bank Greywacke Member. Black graphitic and dolomitic slate with pyrite; chlorite-sericite slate and metasiltstone; thin greywacke interbeds.||||||16-JUN-04
41179|Nangeela Formation|50161|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Includes Steep Bank Greywacke Member and Warrock Limestone Member. Black graphite slate with pyrite; black dolomitic slate with pyrite; chlorite-sericite slate and metasiltstone; thin greywacke interbeds.||||||22-JUN-04
41179|Nangeela Formation|50162|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Black graphite slate with pyrite; black dolomitic slate with pyrite; chlorite-sericite slate and metasiltstone; thin greywacke interbeds.||||||
41179|Nangeela Formation|50163|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup. Overlain by Duddo Limestone. Black graphite slate with pyrite; black dolomitic slate with pyrite; chlorite-sericite slate and metasiltstone; thin greywacke interbeds.||||||25-JUN-04
41179|Nangeela Formation|50164|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Overlain by Otway Group. Of Glenelg River Metamorphic Complex (Moralana Supergroup).||||||25-JUN-04
41179|Nangeela Formation|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Moralana Supergroup. Includes Steep Bank Greywacke Member and Warrock Limestone Member. Defined  by Morand et al. 2003||||||
41179|Nangeela Formation|68116|5|Briefly described|Appendix, Map 29.|Middle Cambrian|Early Cambrian||||||Black graphitic slate with pyrite; black dolomitic slate with pyrite; grey to green chlorite-sericite slate and metasiltstone; thin greywacke interbeds.|
41179|Nangeela Formation|71593|4|Described|p8, p12, p20-p22, p102, p133, p150|Cambrian|Cambrian|Glenelg Zone.|||Includes the Steep Bank Greywacke Member.|Equivalent (in part) to the Kanmantoo Group.|Shale marl and carbonate rich units including slates.|
41179|Nangeela Formation|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Black graphitic and dolomitic slate with pyrite; grey to green chlorite-sericite slate and metasiltstone; thin greywacke interbeds.|09-DEC-21
41188|Nangkita Granite|50154|2|Defined|p96, p247 App.5|Cambrian|Cambrian|Of the Glenelg Metamorphic Complex. Intruded by dykes of the Chin Chap Meladiorite.||||||25-SEP-09
41188|Nangkita Granite|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Muscovite leucogranite; S-type||||||
41188|Nangkita Granite|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite leucogranite||||||20-AUG-04
41188|Nangkita Granite|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite leucogranite||||||20-AUG-04
41188|Nangkita Granite|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite leucogranite||||||20-AUG-04
41188|Nangkita Granite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite leucogranite||||||20-AUG-04
41188|Nangkita Granite|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite leucogranite||||||20-AUG-04
41188|Nangkita Granite|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite leucogranite||||||20-AUG-04
41188|Nangkita Granite|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite leucogranite||||||20-AUG-04
41188|Nangkita Granite|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Muscovite leucogranite||||||20-AUG-04
41188|Nangkita Granite|66002|6|Mentioned|p8 Tb.5|||G408. Defined by Kemp et al. 2002||||||
41188|Nangkita Granite|68116|5|Briefly described|Appendix, Map 38.|Middle Ordovician|Middle Cambrian|Nonmagnetic.|||||Muscovite leucogranite: massive, white, medium to coarse grained, porphyritic with microcline megacrysts; minor biotite and locally abundant garnet; large enclaves of schist and gneiss are locally abundant, with biotite schlieren and selvedges.|
13839|Nar Nar Goon basalt|33462|6|Mentioned|p43|||||||||
37331|Nargoon Group|23309|4|Described|p40, p5 Fig. 1.3|Cambrian|Cambrian|||||||22-FEB-10
37331|Nargoon Group|24311|5|Briefly described|p1059 Fig. 2|Cambrian|Cambrian|||||||
37331|Nargoon Group|24551|4|Described|p80|Late Cambrian|Late Cambrian|Intruded by Bushy Creek Granite.||||||03-AUG-05
37331|Nargoon Group|50154|2|Defined|p24, p47, p72, p143|Late Cambrian|Middle Cambrian|Overlies the Mount Stavely Volcanics. Unconformably overlain by the Grampians Group and quartz-cobble conglomerate of the Renmark Group. Geological Province: Grampians-Stavely Zone, Delamerian Fold Belt.||||||15-SEP-04
37331|Nargoon Group|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Marine turbidites||||||22-MAY-13
37331|Nargoon Group|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Marine turbidites: cleaved quartz wacke and slate; thin bedded.||||||22-MAY-13
37331|Nargoon Group|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Marine turbidites: cleaved quartz wacke and slate; thin bedded.||||||22-MAY-13
37331|Nargoon Group|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Unconformably overlain by Grampians Group. Marine turbidites: cleaved quartz wacke and slate; thin bedded.||||||22-MAY-13
37331|Nargoon Group|50159|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Overlain by Grampians Group and Shepparton Formation. Marine turbidites: cleaved quartz wacke and slate; thin bedded.||||||22-MAY-13
37331|Nargoon Group|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Marine turbidites: quartz wacke and slate.||||||22-MAY-13
37331|Nargoon Group|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Marine turbidites: cleaved quartz wacke and slate; thin bedded.||||||22-MAY-13
37331|Nargoon Group|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Marine turbidites: cleaved quartz wacke and slate; thin bedded.||||||22-MAY-13
37331|Nargoon Group|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Marine turbidites: cleaved quartz wacke and slate; thin bedded.||||||22-MAY-13
37331|Nargoon Group|60451|6|Mentioned|p21, Fig. 7|||||||||
37331|Nargoon Group|60454|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt. Includes: Glenthompson Sandstone.||||||22-MAY-13
37331|Nargoon Group|60456|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt. Includes: Glenthompson Sandstone.||||||22-MAY-13
37331|Nargoon Group|60457|5|Briefly described|Map Legend|Cambrian|Cambrian|Includes: Glenthompson Sandstone. Geological Province: Delamerian Fold Belt.||||||22-MAY-13
37331|Nargoon Group|60458|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt. Includes: Glenthompson Sandstone.||||||22-MAY-13
37331|Nargoon Group|60459|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt. Includes: Glenthompson Sandstone.||||||22-MAY-13
37331|Nargoon Group|62755|5|Briefly described|p876 Fig. 1|Cambrian|Cambrian|Includes the Glenthompson Sandstone.||||||
37331|Nargoon Group|64314|5|Briefly described|p495 Fig. 2a|Cambrian|Cambrian|||||||
37331|Nargoon Group|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Includes Glenthompson Sandstone. Defined by VandenBerg et al. 2000 p38.||||||
37331|Nargoon Group|67104|6|Mentioned|p635|||May correlate with the Mariner Group in Antarctica.||||||
37331|Nargoon Group|68116|5|Briefly described|Appendix, Maps 29, 30.|Late Cambrian|Early Cambrian||||||Quartz wacke and slate; thin-bedded.|
37331|Nargoon Group|68194|6|Mentioned|p21||||||Includes Glenthompson Sandstone.|||
37331|Nargoon Group|70211|5|Briefly described|p3, p35|||VandenBerg et al. (2000).|||Glenthompson Sandstone.|Overlies Mount Stavely Volcanic Complex. Is overlain unconformably by Grampians Group.||
37331|Nargoon Group|70493|6|Mentioned|p56|Late Cambrian|Late Cambrian|Grampians-Stavely Zone, Lachlan Orogen.||||Overlies Mount Stavely Volcanic Complex. Is overlain unconformably by Grampians Group.||
37331|Nargoon Group|70877|4|Described|p10, p13-p21, p167, p196||Ediacaran|Grampians-Stavely Zone. Horsham 1:250k and NHill 1:100k Map sheets. Previously interpreted to include the Glenthompson Sandstone, in this volume the old Glenthompson Sandstone is separated from the younger Nargoon Group. SHRIMP age derived from this volume and represents a maximum possible age of deposition. Petrography, zircon morphology and SHRIMP U-Pb results of an undifferentiated sample of this group is discussed in detail.|552 +/- 8 Ma (SHRIMP U-Pb)|||Overlain by the Grampians Group.|Sandstone and siltstone; dominated by albitised feldspar and chlorite, contains detrital amphibole and garnet.|
37331|Nargoon Group|70967|6|Mentioned|p9, 11, 18-19|||Grampians-Stavely Zone. Sedimentary rocks. Deformed during the Delamerian Orogeny.|||Glenthompson Sandstone.|||
37331|Nargoon Group|71593|4|Described|p1, p8, p12, p19, p22|Cambrian|Cambrian|Delamerian Orogen, Grampians-Stavely Zone. A type locality is mentioned but not provided. Petrography briefly discussed. See also p24, p26, p43, p72, p102, p133, p188-p189, p194.||||Faulted against the Glenelg River Metamorphic Complex. Unconformably overlain by the Grampians Group. |Graphitic slate, chert and cleaved sandstone with sedimentary features such as low angle cross-bedding.|
37331|Nargoon Group|72445|5|Briefly described|p8, p10, p17, p18; App.1, App.2, App.5|Early Cambrian|Early Cambrian|Shown as part of the target basement. App.2 is a .csv format file. Identified in Stavely 05,14. Overlies the Stavely arc. See also app 7 p6.|||Includes Glenthompson Sandstone.|Shown as underlying Renmark Group with sharp contact. Overlain by the Grampians Group.|Fine-grained sandstone with 0.2-6.3 m siltstone intervals. Variably weathered, fine to medium grained sandstone with 0.1-1.5 m siltstone intervals towards base.|15-OCT-20
37331|Nargoon Group|73059|6|Mentioned|p1059|Late Cambrian|Late Cambrian|Grampians-Stavely Zone.||||||
37331|Nargoon Group|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Marine turbiditic, cleaved quartz wacke and slate.|09-DEC-21
37331|Nargoon Group|73430|6|Mentioned|p493||||||||Variably deformed siliciclastic sediment sequences.|
26799|Nariel Granite|23309|6|Mentioned|p440 App1|||G94 S-Type.||||||
26799|Nariel Granite|24133|3|Fully described|p61|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
26799|Nariel Granite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
26799|Nariel Granite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
26799|Nariel Granite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
26799|Nariel Granite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Two-mica granite: light yellow-brown, equigranular; massive; S-type; nonmagnetic||||||09-SEP-04
26799|Nariel Granite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Biotite-muscovite granite: S-type; nonmagnetic; high K, moderate to low Th, variable U.||||||09-SEP-04
26799|Nariel Granite|42726|5|Briefly described|map legend|Silurian||||||||
26799|Nariel Granite|44184|5|Briefly described|Map Legend||Early Silurian|Shown as Nariel Unassigned.||||||
26799|Nariel Granite|68116|5|Briefly described|Appendix, Map 20.|Pridoli|Wenlock||||||Muscovite-biotite granite: leuco- to mesocratic, light yellow-brown, equigranular to weakly porphyritic in feldspar; medium-grained; massive; S-type; nonmagnetic.|
77120|Narimba Sequence|61553|5|Briefly described|p605 Fig.4, p609-611.   |Early Eocene|Late Paleocene|Reference section is in Narimba-1 well. High rate of sedimentation deposited a >700 m syn-tectonic succession in aggradational fluvio-deltaic to floodplain environments.||Unit in Bass Megasequence.||Overlies Tilana Sequence. |Sandstones, shales, thin coal beds.|
77120|Narimba Sequence|69879|5|Briefly described|p431-433|Eocene|Paleocene|Covers most of Bass Basin. Fossil controls. Thickness varies markedly from less than 100m to over 900m.||Bass Megasequence||Overlies Tilana Sequence unconformably. Underlies Aroo Sequence unconformably. Equivalent to Upper Eastern View Coal Measures.|Non-marine fining up sandstone, shale and coal deposited in fluvio-deltaic to brackish lacustrine and lagoonal environments.|
37585|Narooma Accretionary Complex|23309|4|Described|p320-322, 372|||||||||
37585|Narooma Accretionary Complex|24551|6|Mentioned|p113 Fig. 4.22|||||||||03-AUG-05
37585|Narooma Accretionary Complex|60904|5|Briefly described|p777 Fig. 4, p793|||Of the eastern Lachlan Orogen. Interbedded sandstone and mudstone as well as disrupted sandstone and mudstone in the Batemans Bay-Narooma-Bermagui area of NSW south coast. See also p809.||||||10-JAN-07
37585|Narooma Accretionary Complex|61160|6|Mentioned|p13 Fig. 3.1|||Probably a structural term?||||||
37585|Narooma Accretionary Complex|64312|6|Mentioned|p443 Fig. 5|||See also p445. ||||||
37585|Narooma Accretionary Complex|67847|6|Mentioned|p78|||||||||
37585|Narooma Accretionary Complex|67849|5|Briefly described|pp21-22, pp28-29, Fig.9, p30.|||Lachlan Orogen. Also written as Narooma accretionary complex. Kubler Index measurements indicate sub-greenschist/greenschist boundary conditions of c.15 km depth and a geothermal gradient of c.20 degrees C during subduction; ie they formed in the underplated section of the complex.|||Includes Wagonga and Adaminaby Groups and Narooma Complex(?).|||02-OCT-15
37585|Narooma Accretionary Complex|68309|5|Briefly described|p225|||Considered the easternmost, W-dipping subduction zone in the Lachlan Orogen. Shown as comprising the ""coastal zone"" of the Adaminaby Group, and the Wagonga Group. See also references to Narooma accretionary complex (p224-225, 232-233).||||||
37585|Narooma Accretionary Complex|70601|5|Briefly described|p23-24, p46, p56, p58|Ordovician|Ordovician|Postulated role in development of Lachlan Orogen discussed. Presented also as Narooma 'Accretionary Complex'.|||Wagonga Group, Adaminaby Group.||Quartzose clastic sediments.|
13892|Narracan Group|29821|6|Mentioned|Table 1|||||||||
13892|Narracan Group|31045|6|Mentioned|p140|||Stratigraphic diagram||||||
13892|Narracan Group|33358|6|Mentioned|Fig.2|||||||||
13892|Narracan Group|33459|6|Mentioned|Table 1|||||||||
13892|Narracan Group|37127|5|Briefly described|p347|||||||||
13892|Narracan Group|71202|14|Not recorded|p196|||Subdivision and stratigraphic table.||||||
83413|Narraport pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G607.||Of Glenloth Suite|||Nonmagnetic inner phase surrounded by magnetic phases with responses to 100 nT; inner phase has gravity response about 30 micrometres/second/second less than outer phases.|
83413|Narraport pluton|73505|6|Mentioned|p7|||(G607). Of Lalbert Batholith. Shows apparent dextral shear sense not apparent in surrounding sedimentary rocks.||||||
13900|Narrapumelap Road Dacite Member|23309|5|Briefly described|p35 Tb 2.6, p44 Tb 2.14|Cambrian|Cambrian|Of the Towanway Tuff.  Age: 495 +/- 5Ma.||||||
13900|Narrapumelap Road Dacite Member|23402|4|Described|p11, p14, p8 Tb. 1|Late Cambrian|Late Cambrian|Parent:  Mount Stavely Volcanic Complex.   Age: 495+/-5Ma (U-Pb zircon).   Thickness: 100m.  Geological Province: Adelaide Fold Belt||||||
13900|Narrapumelap Road Dacite Member|40172|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
13900|Narrapumelap Road Dacite Member|40887|2|Defined|p19|Cambrian|Cambrian|Prob. Cambrian. Supersedes Narrapumelap Road Rhyolite Member.||||||
13900|Narrapumelap Road Dacite Member|41571|6|Mentioned|Table 2.2|||||||||
13900|Narrapumelap Road Dacite Member|42827|6|Mentioned|p41|||||||||
13900|Narrapumelap Road Dacite Member|50371|5|Briefly described|Map Legend|Cambrian|Cambrian|Of Towanway Tuff (Mount Stavely Volcanic Complex). Dacitic to rhyolitic lava||||||
13900|Narrapumelap Road Dacite Member|61187|6|Mentioned|p69 Fig.2.|Early Cambrian|Early Cambrian|||Unit in Towanway Tuff.||||
13900|Narrapumelap Road Dacite Member|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Towanway Tuff. Defined by Buckland 1986.||||||
13900|Narrapumelap Road Dacite Member|70211|5|Briefly described|p3, p5, p45-46|||Stavely region.|495.0 +/- 5.0 Ma (Stuart-Smith and Black, 1999).|Mount Stavely Volcanic Complex.||||
13900|Narrapumelap Road Dacite Member|70877|4|Described|p2, p48-p49, p54-p59, p80|Cambrian|Cambrian|See also  p167-p168, p172-p173, p192. Grampians-Stavely Zone. Ballarat 1:250k and Willaura 1:100k map sheets. SHRIMP ages derived from this study and represent the age of magmatic crystallisation. Also dated as 495 +/- 5 Ma (Stuart Smith and Black, 1999). Petrography, zircon morphology and SHRIMP U-Pb results are discussed in detail for a sample of this unit.|503.2 +/- 2.3 Ma (SHRIMP U-Pb)|||Overlies the Fairview Andesite Breccia.||
13900|Narrapumelap Road Dacite Member|71593|4|Described|p29, p39-p40|||The type locality for this unit occurs in the Stavely Belt segment.|495 +/- 5 Ma (SHRIMP U-Pb)|Mount Stavely Volcanic Complex||||
13904|Narrawaturk Marl|12781|6|Mentioned|p386|Eocene|Eocene|Otway Basin. Maximum thickness 21m.||Nirranda Group.||Unconformably overlies Dilwyn Formation. Is overlain unconformably by Compton Conglomerate and Gellibrand Marl.||
13904|Narrawaturk Marl|22587|6|Mentioned|p79 Fig.7|Late Eocene|Middle Eocene|||||||
13904|Narrawaturk Marl|22674|5|Briefly described|Fig.2 p719|Early Oligocene|Middle Eocene|||||||
13904|Narrawaturk Marl|22875|3|Fully described|p62|Early Oligocene|Late Eocene|Of the Nirranda Group.||||||31-JAN-07
13904|Narrawaturk Marl|22944|5|Briefly described|Fig3|Oligocene|Eocene|||||||
13904|Narrawaturk Marl|23230|5|Briefly described|Table4-1p40|Oligocene||||||||
13904|Narrawaturk Marl|23307|5|Briefly described|Map Legend|Oligocene|Eocene|Of Nirranda Group.||||||31-JAN-07
13904|Narrawaturk Marl|23322|5|Briefly described|957 Fig.2|Oligocene|Eocene|Of the Nirranda Group.  Geological Province: Gambier Basin.  See also p968.||||||07-SEP-09
13904|Narrawaturk Marl|24056|5|Briefly described|p85|Eocene|Eocene|Of Nirranda Group.  Geological Basin: Otway Basin.||||||
13904|Narrawaturk Marl|24202|5|Briefly described|p313 Fig. 2|Late Eocene|Middle Eocene|Geological Province: Gambier Sub-basin.||||||
13904|Narrawaturk Marl|24314|5|Briefly described|p61 Fig.2|Eocene|Eocene|Of the Nirranda Group. Geological Province: Otway Basin. Max. Thickness 21m.||||||09-DEC-08
13904|Narrawaturk Marl|24551|5|Briefly described|p292 Fig. 10.3|||||||||
13904|Narrawaturk Marl|24562|5|Briefly described|p7, 8 Fig. 2|Oligocene|Eocene|Of the Nirranda Group. Conformably overlies Mepunga Formation.  Geological Province: Otway Basin.||||||09-DEC-08
13904|Narrawaturk Marl|29823|6|Mentioned|p14|||||||||
13904|Narrawaturk Marl|30576|5|Briefly described|Table 2|||||||||
13904|Narrawaturk Marl|30578|6|Mentioned|p9|||||||||
13904|Narrawaturk Marl|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
13904|Narrawaturk Marl|30675|5|Briefly described|p253|||Lithology and radioactivity.||||||31-JAN-07
13904|Narrawaturk Marl|30932|6|Mentioned|Map legend|Miocene|Oligocene|Part of Gellibrand Marl? Oligocene to Miocene||||||31-JAN-07
13904|Narrawaturk Marl|31036|6|Mentioned|p210|||Unit of Nirranda Gp. See also Table 9-1.||||||
13904|Narrawaturk Marl|31245|6|Mentioned|p82|||||||||
13904|Narrawaturk Marl|31424|4|Described|p14|||See also p7. Described from core.||||||31-JAN-07
13904|Narrawaturk Marl|31625|6|Mentioned|Fig. 5.2|||Eocene-Oligocene||||||
13904|Narrawaturk Marl|32852|6|Mentioned|p10|||||||||
13904|Narrawaturk Marl|33155|5|Briefly described|p122|||||||||
13904|Narrawaturk Marl|33940|6|Mentioned|p414|||||||||
13904|Narrawaturk Marl|34063|6|Mentioned|p2|||U.Eocene. Table||||||
13904|Narrawaturk Marl|34954|6|Mentioned|Fig.35|||||||||
13904|Narrawaturk Marl|35066|5|Briefly described|p209|||||||||
13904|Narrawaturk Marl|36913|6|Mentioned|Fig.2|||||||||
13904|Narrawaturk Marl|37548|6|Mentioned|Fig.5|||||||||
13904|Narrawaturk Marl|38625|6|Mentioned|Table 2|||||||||
13904|Narrawaturk Marl|38932|5|Briefly described|p98|||See also Fig.4||||||
13904|Narrawaturk Marl|40003|5|Briefly described|p44|||||||||
13904|Narrawaturk Marl|40560|6|Mentioned|p6|||||||||
13904|Narrawaturk Marl|41016|5|Briefly described|Table 1|||||||||
13904|Narrawaturk Marl|41185|6|Mentioned|Fig.4|||||||||
13904|Narrawaturk Marl|41269|5|Briefly described|p246|||||||||
13904|Narrawaturk Marl|41517|6|Mentioned|p135|||See also p139.||||||31-JAN-07
13904|Narrawaturk Marl|41642|6|Mentioned|Fig.8.6|||||||||
13904|Narrawaturk Marl|41701|6|Mentioned|Map legend|Oligocene||||||||
13904|Narrawaturk Marl|41704|6|Mentioned|Fig.3|||||||||
13904|Narrawaturk Marl|41714|6|Mentioned|Fig.2|||||||||
13904|Narrawaturk Marl|41726|6|Mentioned|Fig.5|||||||||
13904|Narrawaturk Marl|41769|4|Described|p30|||||||||
13904|Narrawaturk Marl|41868|5|Briefly described|p535|||||||||
13904|Narrawaturk Marl|42318|6|Mentioned|Fig.2 P10|||||||||
13904|Narrawaturk Marl|42524|5|Briefly described|Fig.3 P27|||||||||
13904|Narrawaturk Marl|42601|6|Mentioned|Fig.2 p15|||||||||
13904|Narrawaturk Marl|42827|5|Briefly described|p283|||see also Fig 12.30||||||
13904|Narrawaturk Marl|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
13904|Narrawaturk Marl|43171|6|Mentioned|5-8|||Of Nirranda Group. Age: 30-40Ma.||||||31-JAN-07
13904|Narrawaturk Marl|43195|5|Briefly described|Map Legend||Late Eocene|See also commentary on back of map. Of Nirranda Group.||||||
13904|Narrawaturk Marl|43208|5|Briefly described|map legend|Early Oligocene|Middle Eocene|Of Nirranda Group.||||||
13904|Narrawaturk Marl|43219|5|Briefly described|Fig.3,p6.|Oligocene|Eocene|Of the Nirranda Group.||||||31-JAN-07
13904|Narrawaturk Marl|43590|4|Described|p22|Early Oligocene|Late Eocene|||||||
13904|Narrawaturk Marl|43660|6|Mentioned|Fig.6,p15|Oligocene|Eocene|||||||
13904|Narrawaturk Marl|43733|6|Mentioned|Fig.2.11,p65||Eocene|||||||
13904|Narrawaturk Marl|43744|6|Mentioned|Fig.3,p3|||||||||
13904|Narrawaturk Marl|43814|6|Mentioned|Fig.3,p115|||||||||
13904|Narrawaturk Marl|43937|5|Briefly described|Map Legend|Middle Eocene|Paleocene|||||||
13904|Narrawaturk Marl|44133|5|Briefly described|p155|Early Oligocene|Middle Eocene|Of the Nirranda Group. Geological Province: Gambier Basin. Thickness: 15m. Conformably overlies: Mepunga Formation. ||||||
13904|Narrawaturk Marl|48911|6|Mentioned|Chart 1|||||||||
13904|Narrawaturk Marl|60563|5|Briefly described|p47|||Of the Nirranda Group. See also the Narrawaturk Formation.||||||
13904|Narrawaturk Marl|61155|5|Briefly described|p18|Early Oligocene|Middle Eocene|Of the Nirranda Group. Partly overlies and interfingers with Mepunga Formation. Underlies Clifton Formation. Age: 48-30.5Ma. Thickness: 130m. Geological Province: Otway Basin (Tyrendarra and Port Campbell Embayments). ||||||
13904|Narrawaturk Marl|61182|3|Fully described|p24, p26, p33|Oligocene|Eocene|Of Nirranda Gp. Incorporates Browns Creek Clay, Castle Cove Limest., Glen Aire Clay.Grades into/conformable over Mepunga Fm; interfingers with Demons Bluff Fm. Max.thick: 131m. Disconformable below Clifton Fm; and Gellibrand Marl in places. Fossils common||||||
13904|Narrawaturk Marl|61547|6|Mentioned|p461 Fig.2. |Eocene|Eocene|||Unit in Nirranda Group.||Overlies Mepunga Formation. Is overlain by Gellibrand Marl.||
13904|Narrawaturk Marl|61622|5|Briefly described|p436 Fig. 2|Eocene|Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-FEB-11
13904|Narrawaturk Marl|61623|6|Mentioned|p449 Fig. 4|Oligocene|Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
13904|Narrawaturk Marl|61624|6|Mentioned|p466 Fig. 2|Oligocene|Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
13904|Narrawaturk Marl|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4|Oligocene|Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
13904|Narrawaturk Marl|61627|5|Briefly described|p504, p500 Fig. 2|Late Eocene|Middle Eocene|Of Nirranda Group. Underlain by Mepunga Sandstone. Geological Province: Otway Basin.||||||07-FEB-11
13904|Narrawaturk Marl|61628|5|Briefly described|p509 Fig. 3|Early Oligocene|Middle Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
13904|Narrawaturk Marl|63122|5|Briefly described|p17 Fig. 4.3|Late Eocene|Middle Eocene|Of the Nirranda Group. Max. thickness: 21m. Geological Province: Otway Basin. ||||||
13904|Narrawaturk Marl|63124|3|Fully described|p49 Fig. 5.2, p87 Fig. 5.29, p91|Late Eocene|Middle Eocene|Of Nirranda Gp. Conformable on Mepunga Fm; unconformable on Dilwyn Fm. Conformable below Greenways Mbr (Gambier Lst) or unconformable below Camelback Mbr. Age: ~39.5-~36.5Ma). Max.thickness:21m. In Otway Basin. Synonym: Lacepede Formation (Ludbrook 1971).||||||31-JAN-08
13904|Narrawaturk Marl|63129|6|Mentioned|p139|||Geological Province: Otway Basin. Acts as a regional seal.||||||30-JAN-08
13904|Narrawaturk Marl|63130|5|Briefly described|p146|Tertiary|Tertiary|Overlies Dilwyn Formation. Geological Province: Otway Basin.||||||06-FEB-08
13904|Narrawaturk Marl|63269|5|Briefly described|p605|Oligocene|Eocene|Otway Basin.||Nirranda Group.||||
13904|Narrawaturk Marl|63431|5|Briefly described|p677 Fig. 2|Eocene|Eocene|Of the Nirranda Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
13904|Narrawaturk Marl|65715|5|Briefly described|p11 Tb.7, p25 Fig.1a|Paleogene|Paleogene|Of Nirranda Group. Formation status.||||||
13904|Narrawaturk Marl|66002|4|Described|p10 Tb.7, p16, p26 Fig.7|Paleogene|Paleogene|Of Nirranda Group. Overlies Mepunga Formation. Calcareous mudstone, minor thin calcarenite beds, locally carbonaceous and burrowed, locally abundant glauconite pellets, polished quartz sands. Contains foraminifers, bryozoans, brachiopods and molluscs. Defined by White 1968.||||||
13904|Narrawaturk Marl|66245|6|Mentioned|p6 Fig.5. |Rupelian|Bartonian|||Unit in Nirranda Group.||||
13904|Narrawaturk Marl|67061|6|Mentioned|p546 Fig.3.|Oligocene|Eocene|||Unit in Nirranda Group.||||
13904|Narrawaturk Marl|67366|5|Briefly described|p103 Fig.2. |Oligocene|Eocene|||Unit in Nirranda Group.||Overlies Mepunga Formation. Is unconformably overlain by Clifton Formation.|Open marine marl and calcareous mudstone.|
13904|Narrawaturk Marl|68116|5|Briefly described|Appendix, Maps 54-55.|Oligocene|Eocene||||||Calcareous mudstone, minor thin calcarenite beds: locally carbonaceous and burrowed, locally abundant glauconite pellets and polished quartz sand, foraminifers, bryozoans, brachiopods and molluscs; open marine (below storm wave base) deposits.|
13904|Narrawaturk Marl|69297|5|Briefly described|p79|Rupelian|Bartonian|Otway Basin. ||Nirranda Group||Overlies the Mepunga Formation. Overlain by the Gambier Limestone and the Wangoom Sand or unconformably by the Clifton Formation. |Marl.|
13904|Narrawaturk Marl|69651|5|Briefly described|p10|Oligocene|Eocene|||Nirranda Group.||Overlies Mepunga Formation. Is overlain unconformably by Clifton Formation.||
13904|Narrawaturk Marl|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4; p5|Eocene|Eocene|Otway Basin. Increasingly open marine carbonates. Time-equivalent to Demons Bluff Formation and Eastern View Coal Measures.||Nirranda Group.||Overlies Mepunga Formation. Is overlain by Clifton Formation or Greenways Member (Gambier Limestone). Is locally interbedded with Wangoom Sand.||
13904|Narrawaturk Marl|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Eocene|Eocene|Gambier Embayment and Voluta Trough.||Nirranda Group.||Overlies Mepunga Formation. Is overlain by Gambier Limestone.||
13904|Narrawaturk Marl|70880|6|Mentioned|p77|Oligocene|Eocene|Otway Basin.||||||
13904|Narrawaturk Marl|70942|4|Described|p126, 119|||||||||17-FEB-17
13904|Narrawaturk Marl|71266|6|Mentioned|p614 Fig.3|Oligocene|Eocene|Otway Basin.||||||
13904|Narrawaturk Marl|71437|4|Described|Fig. 1 opp 154, p155, p160|Oligocene|Eocene|||Of Nirranda Group.||Interfingers with Mepunga Formation. Succeeded partially disconformably by Clifton Formation.|Sequence of richly fossiliferous marls, grading down in carbonate content to marly mudstones, or up to marly limestones.|
13904|Narrawaturk Marl|73357|5|Briefly described|p28-30, p44, p46, p48|Rupelian|Priabonian|Otway Basin. Contains Nothofagidites asperus Spore-Pollen Zone, Proteacidites tuberculatus Spore-Pollen Zone, Spiniferites ramosus Dinocyst Zone and Operculodinium Dinocyst Superzone, typically nearshore to offshore marine depositional environments. Lower part correlated with Corrudinium incompositum Dinocyst Zone.||Of Nirranda Group|Includes Wangoom Sand Member|Overlies Mepunga Formation, underlies Clifton Formation.||
13904|Narrawaturk Marl|73383|5|Briefly described|p3, p10 Tb.3.8, p25, p28, p164-165, p258|Oligocene|Eocene|Otway Basin. Approximately equivalent to chemostratigraphic package S6-P1 which has high Fe/Al values, the top of the package is defined by a decrease in Ti/Cr values and an increase in Ca. Lithologies based on geochemistry using the ChemLith classification includes calcareous sandstone and calcareous limestone, and using the Herron classification (1988) includes Fe-sand, Fe-shale and quartz-arenite. See also vi, p11 Tb.3.9, p34, p131.||Nirranda Group||Overlies Mepunga Formation, underlies Heytesbury Group, Gellibrand Marl|Marls and calcareous mudstones.|
13904|Narrawaturk Marl|73385|5|Briefly described|p5|Oligocene|Eocene|Otway Basin.||Nirranda Group||Overlies Mepunga Formation, underlies Gellibrand Marl, Clifton Formation.|Open marine marls and calcareous mudstones.|
13904|Narrawaturk Marl|73386|4|Described|p4, p6, p13, Attachment A1|Rupelian|Priabonian|Otway Basin. Widespread unit. Open marine depositional environment. Belongs to the Middle Nothofagidites asperus to Lower Proteacidites tuberculatus spore-pollen subzones, latest Priabonian to Rupelian in age.||Nirranda Group||Overlies Mepunga Formation, underlies Clifton Formation, Gellibrand Marl, Heytesbury Group|Marls and calcareous mudstones.|
13904|Narrawaturk Marl|73486|6|Mentioned|p511 Fig.2|Rupelian|Bartonian|Otway Basin.||Nirranda Group||||
13904|Narrawaturk Marl|73594|5|Briefly described|p4|Oligocene|Eocene|Otway Basin.||Nirranda Group||Overlies Mepunga Formation|Marine marls and calcareous mudstones.|
80022|Narrawaturk Marl, Lower|69297|5|Briefly described|p79, p98|Priabonian|Bartonian|Port Campbell Embayment, Otway Basin.||Nirranda Group||Overlies the Mepunga Formation. Overlain by the Wangoom Sand in the Port Campbell Embayment.|Marl.|20-SEP-17
80023|Narrawaturk Marl, Upper|69297|5|Briefly described|p79, p98|Rupelian|Rupelian|Port Campbell Embayment, Otway Basin.||Nirranda Group||Overlies the Wangoom Sand. Unconformably overlain by the Clifton Formation. ||20-SEP-17
13908|Narree Worran Dyke Swarm|42827|5|Briefly described|p165|||||||||
41778|Narrewillock Granite|60462|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Coonooer Suite. Possibly granite; S-type, reduced; nonmagnetic; subsurface only||||||
41778|Narrewillock Granite|60491|6|Mentioned|p36|||Of the Coonooer Suite. Probably misspelt - should be Narrewillock pluton.||||||
37767|Narrowleaf Leucogranite|23309|6|Mentioned|p440, Appendix 1|||G576, A-Type.||||||
37767|Narrowleaf Leucogranite|24133|3|Fully described|p81|||~Early Devonian.  Geological Province: Lachlan Fold Belt.||||||
37767|Narrowleaf Leucogranite|24142|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37767|Narrowleaf Leucogranite|24143|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37767|Narrowleaf Leucogranite|24144|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
37767|Narrowleaf Leucogranite|24145|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Geological Province: Lachlan Fold Belt||||||
37767|Narrowleaf Leucogranite|24146|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
13933|Native Cat Volcaniclastic Member|22968|6|Mentioned|p111|||Parent is Thorkidaan Volcanics, maximum thickness is 800m||||||
13933|Native Cat Volcaniclastic Member|41585|5|Briefly described|p127|||||||||
13933|Native Cat Volcaniclastic Member|42827|5|Briefly described|p127|||of Thorkidaan Volcanics||||||
13933|Native Cat Volcaniclastic Member|60503|5|Briefly described|p108, p15, p28 Fig. 9|Silurian|Silurian|Of the Thorkidaan Volcanics. Consists of thick beds of coarse-grained, poorly sorted juvenile pumice and subordinate rhyolite lava fragments, alternating with thinner beds of siliceous, planar laminated vitric ash.||||||
13933|Native Cat Volcaniclastic Member|60504|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Thorkidaan Volcanics (Enano Group). Tuffaceous breccia, sandstone, siltstone; composed of rhyolitic pumice, shards and crystals, minor rhyolite lava clasts||||||20-OCT-04
13933|Native Cat Volcaniclastic Member|60505|5|Briefly described|Map legend|Ludlow|Ludlow|Of the Thorkidaan Volcanics (Enano Group). Tuffaceous breccia, sandstone, siltstone; composed of rhyolitic pumice, shards and crystals, minor rhyolite lava clasts||||||21-OCT-04
13933|Native Cat Volcaniclastic Member|60506|5|Briefly described|Map legend|Ludlow|Ludlow|Of the Thorkidaan Volcanics (Enano Group). Tuffaceous breccia, sandstone, siltstone; composed of rhyolitic pumice, shards and crystals, minor rhyolite lava clasts||||||21-OCT-04
13933|Native Cat Volcaniclastic Member|60507|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Thorkidaan Volcanics  (Enano Group). Tuffaceous breccia, sandstone, siltstone; composed of rhyolitic pumice, shards and crystals, minor rhyolite lava clasts||||||21-OCT-04
79441|Native Dog Granite|70629|5|Briefly described|p1006|Early Carboniferous|Late Devonian|Also mis-spelt as Native Dog Granita on p1006. This (new) name appears at the very end of the article; the structural term Native Dog Pluton is used up to the last two paragraphs. Associated Mo and W mineralisation is analysed for mineralisation, structural controls and geochronology. Emplaced between the Tabberabberan and Kanimblan Orogenies.|||||Granite, granodiorite and tonalite. A reduced I-type transitional (post-orogenic) pluton showing extended fractionation and magma mixing, crosscut by dacite dykes.|
25332|Natte Yallock Granite|22756|6|Mentioned|Table4 P116|||||||||
25332|Natte Yallock Granite|23300|5|Briefly described|Map Legend|Devonian|Ordovician|Of Mount Cole Suite||||||
25332|Natte Yallock Granite|23301|5|Briefly described|Map Legend|Devonian|Devonian|Of Mount Cole Suite. Age: 397 +/- 9 Ma (Rb-Sr).||||||13-SEP-04
25332|Natte Yallock Granite|23302|5|Briefly described|Map Legend|Devonian|Ordovician|Of Mount Cole Suite||||||
25332|Natte Yallock Granite|23303|5|Briefly described|Map Legend|Devonian|Ordovician|Of Mount Cole Suite||||||
25332|Natte Yallock Granite|23304|5|Briefly described|Map Legend|Devonian|Ordovician|Of Mount Cole Suite||||||
25332|Natte Yallock Granite|23305|3|Fully described|p43 Table 6, 7||Early Devonian|Name preferred to Mount Hooghly Granite, which has been used, because Mt Hooghly erroneously used as a synonym for the Wedderburn Granite. Age: 397+/-9 / 398+/- 5 K-Ar and Rb-Sr. Of Mount Cole Suite. Stalwell Granite Province.||||||22-MAY-13
25332|Natte Yallock Granite|23309|5|Briefly described|p232, 258, 339.||Early Devonian|G354 I-Type. Supersedes Mount Hooghly Granite. Age: 384+/-17Ma, 397+/-9Ma, 398+/-8 Ma.||||||
25332|Natte Yallock Granite|42726|5|Briefly described|map legend|||720. Subsurface unit.||||||
25332|Natte Yallock Granite|65715|5|Briefly described|p8 Tb.4|||Of Mount Cole Suite. G354. Called Natte Yallock pluton by King (1966).||||||
25332|Natte Yallock Granite|66002|5|Briefly described|p7 Tb.5|||Of Mount Cole Suite. G354. Called Mount Hooghly Granite by Marlow and Bushell (1995), but Natte Yallock used for same intrusion in 1988.||||||
25332|Natte Yallock Granite|68116|5|Briefly described|Appendix, Map 23.|Middle Devonian|Early Devonian||||||Biotite-hornblende tonalite; medium grained, equigranular; includes hornblende-biotite-orthopyroxene quartz diorite enclaves; magnetic, oxidised.|
25332|Natte Yallock Granite|68189|6|Mentioned|p42 App.2|||Ages from Bowen (K-Ar, 1975) and Gleadow & Lovering (F-T, 1978) respectively. Intermediate ages also given.|398 +/- 8 to 337 +/- 11 Ma.|||||30-JUN-14
28855|Navarre Granite|23309|5|Briefly described|p440 App1|Middle Devonian|Early Devonian|G364 I-Type. Age: 401+/-4 Ma.||||||
28855|Navarre Granite|42726|5|Briefly described|map legend|||721. Subsurface unit.||||||
28855|Navarre Granite|68189|6|Mentioned|p42 App.2||||401 +/- 4 Ma (K-Ar, McKenzie et al., 1984).|||||30-JUN-14
76940|Neerim Volcanic Group|66244|5|Briefly described|p6.|Neogene|Paleogene|New name. Includes the Neerim Volcanic Province of Wellman (1974) and the Neerim Subprovince of Price et al. (2003), excluding the Fumina Basalt. Crops out in the Drouin - Neerim area;  boundaries with Thorpdale Volcanic Group somewhat arbitrary and Fumina Basalt not well defined.|25 - 22 Ma (Wellman 1974).|||Overlies unconformably the Wonthaggi Formation in the south. Is overlain by Haunted Hills Formation to the east.|Olivine tholeiite, alkali olivine basalt and K-hawaiite; minor nephelinite, basanite and nepheline hawaiite.|
76940|Neerim Volcanic Group|68116|5|Briefly described|Appendix, Maps 42-43, 51-52.|Burdigalian|Oligocene||||||Basaltic lava flows: olivine tholeiite, alkali olivine basalt, K-hawaiite, with minor nephelinite, basanite and nepheline hawaiite.|
30444|Nekeeya Gravel|44929|5|Briefly described|Map Legend||Mesozoic|Colluvium; polymictic conglomerate, poorly sorted and unconsolidated.||||||14-JUN-06
30444|Nekeeya Gravel|44930|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Colluvium; polymictic conglomerate, poorly sorted and unconsolidated.||||||14-JUN-06
30444|Nekeeya Gravel|44932|5|Briefly described|Map Legend||Mesozoic|Colluvium; polymictic conglomerate, poorly sorted and unconsolidated.||||||14-JUN-06
30444|Nekeeya Gravel|44933|5|Briefly described|Map Legend||Mesozoic|Colluvium; polymictic conglomerate, poorly sorted and unconsolidated.||||||14-JUN-06
30444|Nekeeya Gravel|60451|4|Described|p30, 95|Mesozoic|Mesozoic|Type section in text. Maximum Thickness: 25m. Overlies: Mafeking Granodiorite (nonconformably), Grampians Group (unconformably).||||||
30444|Nekeeya Gravel|60454|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Unit does not appear on this map.||||||
30444|Nekeeya Gravel|60456|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Colluvium: polymictic conglomerate: poorly sorted and unconsolidated; variably rounded clasts of granodiorite and sandstone up to boulder size in a sand matrix.||||||
30444|Nekeeya Gravel|60457|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Unit does not appear on map.||||||
30444|Nekeeya Gravel|60458|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Unit does not appear on this map.||||||
30444|Nekeeya Gravel|60459|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Thin cover unit upon the Mafeking Granite not depicted on this map.||||||
30444|Nekeeya Gravel|61183|4|Described|p67, p122|Jurassic|Jurassic|Poorly sorted and polymictic gravel that forms a dissected sheet of unconsolidated deposits overlying the Mafeking Granite; auriferous gravel. Max. thickness: 25m. See also p127. ||||||
30444|Nekeeya Gravel|64541|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Colluvium: polymictic conglomerate: poorly sorted and unconsolidated; variably rounded clasts of granodiorite and Grampians Group sandstone up to boulder size in a sand matrix.||||||13-JUN-14
30444|Nekeeya Gravel|64610|5|Briefly described|Map legend|Mesozoic|Mesozoic|Colluvium: polymictic conglomerate; poorly sorted and unconsolidated; variably rounded clasts of granodiorite and Grampians Group sandstone up to boulder size in a sand matrix; auriferous at base.||||||12-NOV-08
30444|Nekeeya Gravel|66002|5|Briefly described|p9 Tb.6|Mesozoic|Mesozoic|Defined in Cayley and Taylor 1997.||||||
30444|Nekeeya Gravel|68116|5|Briefly described|Appendix, Map 30.|Neogene|Cretaceous||||||Polymictic conglomerate: poorly sorted and unconsolidated; variably rounded clasts of granodiorite and sandstone up to boulder size in a sandstone matrix; auriferous at base.|
13978|Nelson Bay Formation|24551|5|Briefly described|p338 Fig. 11.2, 342|Early Pleistocene|Early Pleistocene|Maximum Thickness:>30m.  Age 1.0-1.4 Ma, from Figure 11.2, p 338.|1.0 - 1.4 Ma||||Subhorizontal biocalcarenite, lagoonal sediments and paleosols|20-JUN-12
13978|Nelson Bay Formation|33160|6|Mentioned|p301|||See also P304||||||
13978|Nelson Bay Formation|34988|3|Fully described|p290|||||||||
13978|Nelson Bay Formation|40643|5|Briefly described|p145|||||||||
13978|Nelson Bay Formation|41206|6|Mentioned|p365|||||||||
13978|Nelson Bay Formation|41848|3|Fully described|p365|||Overlain by Bridgewater Formation Probably early Pleistocene. Shown as Nelson Formation on p366||||||
13978|Nelson Bay Formation|42827|6|Mentioned|p373|||||||||
13978|Nelson Bay Formation|44133|5|Briefly described|p222|||Underlies: Bridgewater Formation. ||||||
13978|Nelson Bay Formation|44221|14|Not recorded|p.95|||||||||
13978|Nelson Bay Formation|50079|6|Mentioned|p46|||Lacustrine sediments largely of nearby Portland Limestone which was levelled and redeposited; calcarenite beds interspersed with clay beds.||||||
13978|Nelson Bay Formation|62068|5|Briefly described|p135 Fig.2,p135,p136,p138,|Pleistocene|Pleistocene|Said to have a Lower Member where fossil vertebrate material collected, mostly from Unit B (of Hann, 1983). Dated by magnetic polarity stratigraphy. Constrained to the Matuyama Chron (1.77-0.78 Ma) by foraminiferan Globorotalia truncatulinoides (F.A.D. 1.9 Ma) and K-Ar dates of 2.76 and 3.20 Ma for the underlying basalts (McFadden et al. 1987)||||Unconformably overlies a basalt of the Newer Volcanics. Unconformably overlain by the Bridgewater Formation.|Series of horizontal and cross-bedded calcarenite, clay and sand.|
37521|Nelson Creek Granite|61163|4|Described|p124, p37 Tb. 6.2|Early Devonian|Early Devonian|Stock of altered granite surrounded by hydrothermally altered and magnetic Pinnak Sandstone. Nonmagnetic, equigranular and dominated (in thin section) by interlocking grains of quartz and rosettes of hydrothermal muscovite.||||||
37521|Nelson Creek Granite|61174|5|Briefly described|map legend|Early Devonian|Early Devonian|Granite: equigranular, interlocking grains of quartz and rosettes of hydrothermal muscovite; feldspar replaced by masses of sericite and hematite; biotite by chlorite and sericite. GSV map code: G191.||||||07-FEB-11
37521|Nelson Creek Granite|61175|5|Briefly described|map legend|Early Devonian|Early Devonian|Granite: equigranular, interlocking grains of quartz and rosettes of hydrothermal muscovite; feldspar replaced by masses of sericite and hematite; biotite by chlorite and sericite. GSV map code: G191.||||||
37521|Nelson Creek Granite|61176|5|Briefly described|map legend|Early Devonian|Early Devonian|Granite: equigranular, interlocking grains of quartz and rosettes of hydrothermal muscovite; feldspar replaced by masses of sericite and hematite; biotite by chlorite and sericite. GSV map code: G191.||||||
37521|Nelson Creek Granite|61177|5|Briefly described|map legend|Early Devonian|Early Devonian|Granite: equigranular, interlocking grains of quartz and rosettes of hydrothermal muscovite; feldspar replaced by masses of sericite and hematite; biotite by chlorite and sericite. GSV map code: G191.||||||
37521|Nelson Creek Granite|61178|5|Briefly described|map legend|Early Devonian|Early Devonian|Highly altered granite (S-type?): nonmagnetic, surrounded by altered magnetic Pinnak Sandstone; no discenrible gravity response; low total radioelement, K, Th and U. GSV map code: G191.||||||
37521|Nelson Creek Granite|68116|5|Briefly described|Appendix, Map 26.|Devonian|Silurian||||||Granite: equigranular, interlocking grains of quartz and rosettes of hydrothermal muscovite; feldspar replaced by masses of sericite and hematite; biotite by chlorite and sericite.|
34702|New Country Sandstone|22876|6|Mentioned|p16|||Bendoc Group||||||
34702|New Country Sandstone|22968|6|Mentioned|P103|||Parent is Bendoc Group||||||
34702|New Country Sandstone|23309|5|Briefly described|p15, 59, 60  Tb 2.19||Ordovician|||||||
34702|New Country Sandstone|24004|5|Briefly described|p275 Fig.2|Ordovician|Ordovician|||||||
34702|New Country Sandstone|24551|4|Described|p106|Bolindian|Bolindian|Of the Bendoc Group. Overlain by Akuna Mudstone, overlies Warbisco Shale. Previously included in the Yalmy Group.||||||03-AUG-05
34702|New Country Sandstone|60503|3|Fully described|p87-88, p29|Late Ordovician|Late Ordovician|Initially basal unit of the Yalmy Group. Now in Bendoc Group because of its black shale and siltstone. Pale to dark grey sandstone, with interbedded mudstone; minor shale. Conformably overlies Warbisco Shale; overlain by Yalmy Group.||||||16-NOV-09
34702|New Country Sandstone|60504|5|Briefly described|Map Legend|Bolindian|Bolindian|Of the Bendoc Group. Sandstone; dark to mid grey, quartzitic to micaceous, turbiditic, and interbedded black to grey siltstone and shale.||||||20-OCT-04
34702|New Country Sandstone|60505|5|Briefly described|Map legend|Bolindian|Bolindian|Of the Bendoc Group. Sandstone; dark to mid grey, quartzitic to micaceous, turbiditic, and interbedded black to grey siltstone and shale.||||||21-OCT-04
34702|New Country Sandstone|60506|5|Briefly described|Map legend|Bolindian|Bolindian|Of the Bendoc Group. Sandstone; dark to mid grey, quartzic to micaceous, turbitic, and interbedded black to grey siltstone and shale.||||||20-OCT-04
34702|New Country Sandstone|60507|5|Briefly described|Map Legend|Bolindian|Bolindian|Of the Bendoc Group. Sandstone; dark to mid grey, quartzitic to micaceous, turbiditic, and interbedded black to grey siltstone and shale.||||||21-OCT-04
34702|New Country Sandstone|61160|5|Briefly described|p48|Late Ordovician|Late Ordovician|Of the Bendoc Group. Geological Province: Lachlan Fold Belt.||||||
34702|New Country Sandstone|61161|5|Briefly described|p31-32, p82|||Of Bendoc Group in BUFFALO. Overlies Warbisco Shale. Underlies Akuna Mudstone. Thick-bedded laminated micaceous sandstone and siltstone indicating turbiditc sedimentation derived from a continental source, probably in relatively deep anaerobic waters.||||||
34702|New Country Sandstone|61163|4|Described|p82-83, p14 Fig. 3.2|Late Ordovician|Late Ordovician|Of the Bendoc Group. Consists of thick-bedded laminated micaceous sandstone, siltstone and mudstone. Overlies Warbisco Shale; overlain by Akuna Mudstone. Geological Province: Lachlan Fold Belt (Tabberabbera Zone). See also p38 Tb. 6.2.||||||
34702|New Country Sandstone|61174|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Sandstone, siltstone, minor black shale: sparse Bolindian graptolites. Deep-marine turbidite fan and hemipelagic deposits. GSV map code: Obn.||||||07-FEB-11
34702|New Country Sandstone|61175|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Sandstone, siltstone, minor black shale: sparse Bolindian graptolites. Deep-marine turbidite fan and hemipelagic deposits. GSV map code: Obn.||||||
34702|New Country Sandstone|61176|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Sandstone, siltstone, minor black shale: sparse Bolindian graptolites. Deep-marine turbidite fan and hemipelagic deposits. GSV map code: Obn.||||||
34702|New Country Sandstone|61177|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Sandstone, siltstone, minor black shale: sparse Bolindian graptolites. Deep-marine turbidite fan and hemipelagic deposits. GSV map code: Obn.||||||
34702|New Country Sandstone|61178|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of Bendoc Group. Thick- to thin-bedded sandstone, siltstone, minor black shale (turbidite): nonmagnetic (up to 5 nT; k up to 15 x10^-5 cgs); moderate to high gravity; low to moderate radioelements. GSV map code: Obn.||||||
34702|New Country Sandstone|61964|5|Briefly described|p25 Fig. 8|Bolindian|Bolindian|Of the Bendoc Group in Victoria - represented by Willandra Sandstone in NSW. ||||||
34702|New Country Sandstone|64963|5|Briefly described|p184|||Renewed quartz-rich trubidites deposited in a mega-fan environment, west of West Wyalong.||||||
34702|New Country Sandstone|67322|5|Briefly described|p16|Late Ordovician|Late Ordovician|VandenBerg et al. (1998); VandenBerg et al. (2004). Distribution is sporadic. In Victoria, the New Country Sandstone is laterally equivalent to, or overlain by the Akuna Mudstone of late Bolindian age (equivalent to Late Ordovician). The New Country Sandstone is thus older than this.||||Overlies the Warbisco Shale. Overlain by and laterally equivalent to the Akuna Mudstone.|Medium- to fine- grained, pale to dark grey quartz sandstone with common detrital muscovite, interbedded with subordinate black mudstone.|22-FEB-18
34702|New Country Sandstone|68116|5|Briefly described|Appendix, Map 27.|Hirnantian|Katian|Age written as Bolindian in text.|||||Sandstone: dark to mid grey, quartzitic to micaceous; thin to very thick-bedded; interbedded black to grey siltstone and shale, partly micaceous.|
34702|New Country Sandstone|68592|5|Briefly described|p320, p351, p363-4|Late Ordovician|Late Ordovician|||Unit in Bendoc Group.||Conformably overlies Warbisco Shale. Correlative of Poidevins and Willandra Sandstones.|Contains subordinate black graptolitic shale in metre-thick packages throughout.|
34702|New Country Sandstone|70661|6|Mentioned|p19|||In Eastern Victoria.||Bendoc Group||||
34702|New Country Sandstone|71069|5|Briefly described|p72, p77, p87|Early Silurian|Late Ordovician|||Bendoc Group||Is equivalent to the Willandra Sandstone and members of the Margules Group. Conformably overlies the Warbisco Shale.|Sandstone.|
34702|New Country Sandstone|71700|6|Mentioned|CD|||||Bendoc Group||Equivalent to the Mundoonen Sandstone and Willandra Sandstone.||
34702|New Country Sandstone|73140|5|Briefly described|p495|Bolindian|Bolindian|Proposed to be reassigned from the Bendoc Group to Margules Group.||Margules Group||Overlies Warbisco Shale, underlies Akuna Mudstone||
38291|Newer Volcanic Group|24383|4|Described|p13, 18|Pleistocene|Late Miocene|Age: 8.5 - 0.1Ma. Underlying Unit: Calivil Formation and Castlemaine Group (unconformable). Max Thickness: <100m. Geological Province: Lachlan Fold Belt.||||||03-FEB-09
38291|Newer Volcanic Group|24384|5|Briefly described|Map legend|Miocene|Eocene|||||||
38291|Newer Volcanic Group|24385|5|Briefly described|Map legend|Miocene|Eocene|||||||
38291|Newer Volcanic Group|24386|5|Briefly described|Map legend|Miocene|Eocene|||||||
38291|Newer Volcanic Group|24387|5|Briefly described|Map legend|Miocene|Eocene|||||||
38291|Newer Volcanic Group|24388|5|Briefly described|Map legend|Pliocene|Eocene|||||||
38291|Newer Volcanic Group|24438|5|Briefly described|p17, p34|Quaternary|Miocene|Lava flows and scoria cones. Covers deep lead drainage system of White Hills Gravel. See Newer Volcanics.|||||Flood basalts, scoria cones.|10-MAY-17
38291|Newer Volcanic Group|24439|5|Briefly described|p7 Fig. 2, p8|Quaternary|Cenozoic|||||||19-NOV-08
38291|Newer Volcanic Group|24440|5|Briefly described|Map legend|||||||||
38291|Newer Volcanic Group|50155|5|Briefly described|Map Legend|Pleistocene|Miocene|Basaltic lava flow, scoria, ash.||||||
38291|Newer Volcanic Group|50156|5|Briefly described|Map Legend|Pleistocene|Miocene|Lava flows: olivine basalt, tholeiitic; moderately to well vesiculated.||||||03-FEB-09
38291|Newer Volcanic Group|50157|5|Briefly described|Map Legend|Pleistocene|Miocene|Lava flows: olivine basalt, tholeiitic; moderately to well vesiculated.||||||03-FEB-09
38291|Newer Volcanic Group|50158|5|Briefly described|Map Legend|Pleistocene|Miocene|Lava flows: olivine basalt, tholeiitic; moderately to well vesiculated.||||||03-FEB-09
38291|Newer Volcanic Group|50159|5|Briefly described|Map Legend|Pleistocene|Miocene|Lava flows: olivine basalt, tholeiitic; moderately to well vesiculated.||||||03-FEB-09
38291|Newer Volcanic Group|50160|5|Briefly described|Map Legend|Pleistocene|Miocene|||||||16-JUN-04
38291|Newer Volcanic Group|50161|5|Briefly described|Map Legend|Pleistocene|Miocene|Lava Flows.||||||26-AUG-04
38291|Newer Volcanic Group|50162|5|Briefly described|Map Legend|Pleistocene|Miocene|Lava flows: olivine basalt, tholeiitic; moderately to well vesiculated.||||||03-FEB-09
38291|Newer Volcanic Group|50163|5|Briefly described|Map Legend|Pleistocene|Miocene|Lava flows: olivine basalt, tholeiitic; moderately to well vesiculated.||||||03-FEB-09
38291|Newer Volcanic Group|62370|5|Briefly described|p447|Holocene|Miocene|Includes all basaltic flows in the Central Highlands palaeovalleys region - infilling deep-lead palaeochannels. Lavas are fine-grained, moderately weathered, variably vesicular black to grey olivine basalt. Age: 7.0Ma to Holocene era. See Newer Volcanics.||||||09-JUN-06
38291|Newer Volcanic Group|64612|2|Defined|p31, p40, p47, p48, p49-52, -72|Early Pliocene|Miocene|Overlies Castlemaine Supergroup, Heathcote Volcanic Group and Murrindindi Supergroup via angular unconformity. Overlies disconformable, Bacchus Marsh Formation. Age: 5.57+/-0.06 and 4.82+/- 0.05Ma. Thickness: 100m. Tholeiitic olivine basalt.||||||03-JUL-13
38291|Newer Volcanic Group|64619|5|Briefly described|Map legend|Pliocene|Miocene|Includes Smokers Creek Volcanic Subgroup and unnamed sheetflow basalt, unnamed scoria deposits and unnamed lavas.||||||
38291|Newer Volcanic Group|64769|6|Mentioned|p26|Cenozoic|Cenozoic|Age: 5 to 0.1Ma. Alkalic to mainly tholeiitic composition. VIC.||||||06-MAY-09
38291|Newer Volcanic Group|65715|4|Described|p17-18, p110||Tortonian|Includes Smokers Creek Volcanic Subgroup. Overlies Werribee Formation. Overlain by Darley Gravel, Deutgam Silt. <10 Ma predominantly basaltic volcanic rocks with minor intermediate and felsic volcanic rocks, as well as minor dykes, plugs and sills.||||||
38291|Newer Volcanic Group|65969|6|Mentioned|p17 Fig.7|||||||||
38291|Newer Volcanic Group|66002|5|Briefly described|p12, p13 Tb.9, p18|Neogene|Neogene|Includes Tower Hill Tuff. Of Krause 1874. Defined VandenBerg 2009. Also referred to as Newer Volcanic rocks (p12). Replaces Newer Volcanics||||||
38291|Newer Volcanic Group|66012|4|Described|p4, p6, p7-8, p9-10 Tb.1, p13-21, p23|Pleistocene|Pliocene|Unconformably overlies Pyrenees Formation and disconformably overlies Lismore Granodiorite. Interfingers with Moorabool Viaduct Sand. Several unnamed units recognised. Tholeiitic to strongly alkaline. Late Pliocene to Pleistocene| | | | | |13-JUN-13
38291|Newer Volcanic Group|66244|5|Briefly described|p7.|||Includes units <10 Ma, eg the Hildene Basalt of Edwards et al. (1997).||||||
38291|Newer Volcanic Group|66769|6|Mentioned|121|Late Pliocene|Late Pliocene|Contains c.580 Ma charnockitic xenoliths, suggesting the Selwyn Block basement is continuous with Proterozoic rocks on King Island and Tasmania.||||||
38291|Newer Volcanic Group|68116|5|Briefly described|Maps 23-25, 30-33, 38-42, 47-50.|Holocene|Miocene|Also occurs in the Appendix. Informally subdivided into alkaline, basalt, icelandite, scoria, stony, trachyte, tuff rings, and valley-filling basalt divisions.|||||Mafic to lesser intermediate and ultramafic lavas and pyroclastics and minor intrusive rocks, interbedded sedimentary rocks.|
38291|Newer Volcanic Group|68189|6|Mentioned|p15 Fig.6, p17 Fig.7, pp30-32|||Exhibits high frequency magnetic responses.||||||
38291|Newer Volcanic Group|70877|5|Briefly described|p13|||Referred to mistakenly as the Newer Volcanics on p41.|||||Basaltic lava flows.|
38291|Newer Volcanic Group|70967|6|Mentioned|p3, 11, 17, 20, 28|Cenozoic|Cenozoic||||||Thin basalt lava flows.|
38291|Newer Volcanic Group|71593|4|Described|p55-56, p44-p45, p47|Holocene|Miocene|Covers up to 15000km ^2 in western victoria. Interpreted as a large intraplate basalt province. Thickness is typically tens of metres. Basalt goechemistry is between alkali Appears as the Newer Volcanics on p45 and p138. See also p8-p9, p12, p60, p102, p133, p198, p203.|2-4 Ma (Gray and McDougall, 2009) in area.|||Unconformably overlies the Rocklands Volcanic Group.|Intraplate basaltic lavas developed as sheet and valley-fill flows.|17-SEP-18
38291|Newer Volcanic Group|72445|5|Briefly described|p2, p10, p16, p19; App.1; App.2; App.5|Pliocene|Pliocene|Murray and Otway basins. Part of the cover rocks in the Stavely Project area. Massive to highly vesicular basalt. Aproximately 30cm interflow gravel/soil interval developed at 13.9 m in Stavely01.||||Unconformably overlies Wunghnu Group.|Massive to highly vesicular basalt. C. 30 cm interflow gravel/soil interval developed at 13.9 m in Stavely01.|15-OCT-20
38291|Newer Volcanic Group|73497|5|Briefly described|Map legend|Holocene|Holocene||||||Lava flows, minor scoria: high frequency, moderately reversely magnetised responses (-85 nT); low K, Th and U.|
74848|Newham Diatomite|64619|5|Briefly described|Map legend|Pliocene|Pliocene|Off-white diatomite, moderately consolidated, cross-bedded; lacustrine deposits.||||||30-OCT-08
74848|Newham Diatomite|65715|2|Defined|p15 Tb.8, p17, p95|Pliocene|Miocene|Newly defined here. Formation rank. Consists of 11.5 m of diatomite and minor tuff. Exposed in the Newham diatomite mine (MGA ref given). Overlies Yungabulla Formation. Overlain by basalt. Interpreted lake deposit. Miocene or early Pliocene age.||||||
30448|Nigretta Ignimbrite|23309|5|Briefly described|p81|||Of the Rocklands Volcanics.||||||
30448|Nigretta Ignimbrite|44929|5|Briefly described|Map Legend||Early Devonian|Of Rocklands Volcanics.  Quartz-feldspar ignimbrite, pinkish-grey with abundant crystals up to 4mm.||||||14-JUN-06
30448|Nigretta Ignimbrite|44930|5|Briefly described|Map Legend||Early Devonian|Of Rocklands Volcanics.  Quartz-feldspar ignimbrite, pinkish-grey with abundant crystals up to 4mm.||||||14-JUN-06
30448|Nigretta Ignimbrite|44931|6|Mentioned|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanics.||||||14-JUN-06
30448|Nigretta Ignimbrite|44932|5|Briefly described|Map Legend||Early Devonian|Of Rocklands Volcanics.  Quartz-feldspar ignimbrite, pinkish-grey with abundant crystals up to 4mm.||||||14-JUN-06
30448|Nigretta Ignimbrite|44933|5|Briefly described|Map Legend||Early Devonian|Of Rocklands Volcanics.  Quartz-feldspar ignimbrite, pinkish-grey with abundant crystals up to 4mm.||||||14-JUN-06
30448|Nigretta Ignimbrite|50154|2|Defined|p114-116, p121|Early Devonian|Early Devonian|Of the Rocklands Volcanic Group. Overlain by the Newer Volcanics. Max. thickness at type section: 85m. Age: 410 +/- 3 Ma.||||||15-SEP-04
30448|Nigretta Ignimbrite|50155|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Quartz-feldspar ignimbrite. Overlies the Glenelg River Metamorphic Complex.||||||25-JUN-04
30448|Nigretta Ignimbrite|50156|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pinkish-grey with abundant lithics of quartz sandstone and metavolcanics at base, fiamme occassionally attenuated to rheomorphic flow banding||||||
30448|Nigretta Ignimbrite|50157|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pinkish-grey with abundant lithics of quartz sandstone and metavolcanics at base, fiamme occassionally attenuated to rheomorphic flow banding||||||24-JUN-04
30448|Nigretta Ignimbrite|50158|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Overlies Glenelg River Metamorphic Complex. Overlain by Parilla Sand.Quartz feldspar ignimbrite: pinkish-grey with abundant lithics of quartz sandstone and metavolcanics at base, fiamme.||||||25-JUN-04
30448|Nigretta Ignimbrite|50159|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pinkish-grey with abundant lithics of quartz sandstone and metavolcanics at base, fiamme occassionally attenuated to rheomorphic flow banding||||||24-JUN-04
30448|Nigretta Ignimbrite|50160|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz-feldspar ignimbrite.||||||26-NOV-08
30448|Nigretta Ignimbrite|50161|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pinkish-grey with abundant lithics of quartz sandstone and metavolcanics at base, fiamme occassionally attenuated to rheomorphic flow banding||||||24-JUN-04
30448|Nigretta Ignimbrite|50162|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pinkish-grey with abundant lithics of quartz sandstone and metavolcanics at base, fiamme occassionally attenuated to rheomorphic flow banding||||||24-JUN-04
30448|Nigretta Ignimbrite|50163|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pinkish-grey with abundant lithics of quartz sandstone and metavolcanics at base, fiamme occassionally attenuated to rheomorphic flow banding.||||||26-NOV-08
30448|Nigretta Ignimbrite|60421|5|Briefly described|p412, 414 Fig. 4|||Of the Rocklands Volcanic Group. Underlies Dorodong Sands.||||||12-NOV-08
30448|Nigretta Ignimbrite|61183|4|Described|p62|Early Devonian|Early Devonian|Of Rocklands Volcanics Gp. 22-25% phenocrysts (quartz, orthoclase, rare plagioclase) in matrix of densely welded relict glass shards; abundant angular lithic fragments of quartz sandstone and metavolcanics in base. Overlain by Gatum Ignimbrite. Thick: 85m||||||
30448|Nigretta Ignimbrite|64541|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanics. Quartz-feldspar ignimbrite.||||||07-FEB-11
30448|Nigretta Ignimbrite|64610|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Rocklands Volcanics. Qtz feldspar ignimbrite: pinkish-grey +abundant crystals up to 4mm; abundant lithics of qtz.sst. and metavolcanics up to 20cm at base; eutaxitic texture often devitrified;fiamme occasionally attenuated to rheomorphic flow banding.||||||12-NOV-08
30448|Nigretta Ignimbrite|66002|5|Briefly described|p6 Tb.4|Devonian|Devonian|Of Rocklands Volcanic Group. Defined in Simpson 1997, p62.||||||
30448|Nigretta Ignimbrite|71593|6|Mentioned|p48|||||||||
41779|Nine Mile Suite|60452|5|Briefly described|p53|||See also Nine Mile suite. Component outcrop pluton: Aughaderry, and buried plutons: Cannon Hills, Marmal. See also p49.||||||
41779|Nine Mile Suite|60461|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes the Aughaderry Tonalite, Cannon Hills and Marmal plutons.||||||
41779|Nine Mile Suite|60462|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes Aughaderry Tonalite||||||
41779|Nine Mile Suite|60491|6|Mentioned|p50|||Characterised by circular granites||||||
41779|Nine Mile Suite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Woosang Granite, Whitimaria Granite, Nine Mile Tonalite.||||||
41779|Nine Mile Suite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Includes: Woosang Granite, Whitimaria Granite, Nine Mile Tonalite.||||||30-SEP-04
41779|Nine Mile Suite|66002|5|Briefly described|p6 Tb.5|||Includes Aughaderry Tonalite, Whitimaria Granite and Woosang Granite. Defined in Bibby and Moore 1998.||||||
41779|Nine Mile Suite|68189|6|Mentioned|p15 Fig.6||||||||granites|
36861|Ninnie Subgroup|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Snowy River Volcanics||||||
36861|Ninnie Subgroup|23309|4|Described|p111 Table 2.40|||Of Snowy River  Volcanics.||||||22-FEB-10
36861|Ninnie Subgroup|24551|4|Described|p143, 141 Fig. 5.32|||Of the Snowy River Volcanics.||||||03-AUG-05
36861|Ninnie Subgroup|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Unit in Snowy River Volcanics.|||Extrusive: ignimbrite, sandstone, conglomerate.|
36861|Ninnie Subgroup|60542|5|Briefly described|p54, p14|Early Devonian|Early Devonian|Of the Snowy River Volcanics. Includes the Kanni Ignimbrite, Boggy Creek Sandstone and Nowa Nowa Conglomerate. Feldspathic ignimbrites and rhyolitic sedimentary breccias. Within the Waiwera Graben. ||||||
83433|Ninyuenook pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G611.||Of Glenloth Suite|||Nonmagnetic; possibly a slight gravity low.|
14185|Nirranda Group|12781|6|Mentioned|p386|Eocene|Eocene|Otway Basin. Appears as NIRR. GP.|||Narrawaturk Mark.|Overlies Wangerip Group. Is overlain by Heytsbury Group.||
14185|Nirranda Group|22587|6|Mentioned|p79 Fig.7|Late Eocene|Middle Eocene|||||||
14185|Nirranda Group|22674|5|Briefly described|p718, Fig.2 p719|Early Oligocene|Middle Eocene|||||||
14185|Nirranda Group|22875|4|Described|p59|Early Oligocene|Middle Eocene|Age: 29-45Ma.||||||31-JAN-07
14185|Nirranda Group|22944|5|Briefly described|Fig3|Oligocene|Eocene|||||||
14185|Nirranda Group|23249|5|Briefly described|p143 Fig.2|Early Oligocene|Late Eocene|In the Otway Basin.||||||31-JAN-07
14185|Nirranda Group|23307|5|Briefly described|Map Legend|Oligocene|Eocene|||||||
14185|Nirranda Group|23322|5|Briefly described|957 Fig.2|Oligocene|Eocene|Geological Province: Gambier Basin (SA) and Otway Basin (VIC).||||||07-SEP-09
14185|Nirranda Group|23778|5|Briefly described|p660|||Geological Province: Otway Basin.||||||
14185|Nirranda Group|23792|5|Briefly described|p26|Recent|Eocene|Carbonates and siliciclastics. Geological Province: Otway Basin.||||||01-JUL-13
14185|Nirranda Group|23939|6|Mentioned|Fig.5|||May be Middle Eocene to Early Oligocene in age.||||||
14185|Nirranda Group|24056|5|Briefly described|p84, p85|||Geological Basin: Otway Basin.||||||
14185|Nirranda Group|24177|5|Briefly described|p14|Eocene|Eocene|Age: ~45 Ma. Geological Province: Otway Basin.||||||
14185|Nirranda Group|24200|5|Briefly described|p417|||See also p423 Figs. 15, 16, p428 Fig. 18.  Nirranda Group Equivalents discussed throughout text.||||||
14185|Nirranda Group|24314|5|Briefly described|p61 Fig.2|Eocene|Eocene|Geological Province: Otway Basin.||||||
14185|Nirranda Group|24323|5|Briefly described|p136 Fig. 3|Oligocene|Eocene|Overlies the Wangerrip Group. Unconformably overlain by the Heytesbury Group. Geological Province: Otway Basin.||||||
14185|Nirranda Group|24344|5|Briefly described|p69, 79|Oligocene|Eocene|||||||
14185|Nirranda Group|24551|5|Briefly described|p246|Oligocene|Eocene|Consists of: Mepunga Formation, Demons Bluff Formation, Narrawaturk Formation.||||||24-JUL-08
14185|Nirranda Group|24562|5|Briefly described|p7, 8, 35 Fig. 2|Oligocene|Eocene|Geological Province: Otway Basin.||||||
14185|Nirranda Group|29591|6|Mentioned|p91|||||||||
14185|Nirranda Group|29823|5|Briefly described|p14|||||||||
14185|Nirranda Group|29856|6|Mentioned|p41|||||||||
14185|Nirranda Group|30499|6|Mentioned|p92|||Stratigraphy||||||
14185|Nirranda Group|30578|4|Described|p9|||||||||
14185|Nirranda Group|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14185|Nirranda Group|30932|6|Mentioned|Map legend|Tertiary|Tertiary|Partly equivalent to Heytesbury Gp. & Glenelg Gp.||||||
14185|Nirranda Group|31036|1|Redefined|p210|middle Tertiary|middle Tertiary|Contains Narrawaturk Marl and Mepunga Formation.||||||31-JAN-07
14185|Nirranda Group|31372|6|Mentioned|p11|||||||||
14185|Nirranda Group|31424|6|Mentioned|Table 2|||Lithostratigraphy||||||
14185|Nirranda Group|31534|6|Mentioned|p369|||See also Table 19-3||||||
14185|Nirranda Group|31583|6|Mentioned|p18|||Section||||||
14185|Nirranda Group|31624|6|Mentioned|p101|||See also P111||||||
14185|Nirranda Group|31625|6|Mentioned|Fig. 5.2|||Eocene - Oligocene||||||
14185|Nirranda Group|32162|6|Mentioned|p58|||Fig.5||||||
14185|Nirranda Group|32852|6|Mentioned|p10|||||||||
14185|Nirranda Group|33940|6|Mentioned|p414|||||||||
14185|Nirranda Group|34063|6|Mentioned|p2|||Upper Eocene. Table||||||14-JAN-09
14185|Nirranda Group|35066|6|Mentioned|p208|||||||||
14185|Nirranda Group|35285|6|Mentioned|p414|||||||||
14185|Nirranda Group|36913|6|Mentioned|p81|||||||||
14185|Nirranda Group|38625|6|Mentioned|p272|||||||||
14185|Nirranda Group|38717|5|Briefly described|p20|||||||||
14185|Nirranda Group|39315|6|Mentioned|Fig.7|||||||||
14185|Nirranda Group|39446|6|Mentioned|p35|||||||||
14185|Nirranda Group|41016|5|Briefly described|Mention|||||||||
14185|Nirranda Group|41185|5|Briefly described|p175|||||||||
14185|Nirranda Group|41269|5|Briefly described|p246|||||||||
14185|Nirranda Group|41487|5|Briefly described|p625|||||||||
14185|Nirranda Group|41701|6|Mentioned|Map legend|middle Oligocene||||||||
14185|Nirranda Group|41704|6|Mentioned|p100|||||||||
14185|Nirranda Group|41714|6|Mentioned|p301|||||||||
14185|Nirranda Group|41726|6|Mentioned|p421|||||||||
14185|Nirranda Group|41769|4|Described|p25|||||||||
14185|Nirranda Group|41868|5|Briefly described|p535|||||||||
14185|Nirranda Group|42075|5|Briefly described|Fig.13 P252|||||||||
14185|Nirranda Group|42152|6|Mentioned|Fig.2 P4|||||||||
14185|Nirranda Group|42524|5|Briefly described|Fig.3 P27|||||||||
14185|Nirranda Group|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
14185|Nirranda Group|43171|6|Mentioned|2-8|Oligocene|Middle Eocene|||||||
14185|Nirranda Group|43195|5|Briefly described|Map Legend||Eocene|See also commentary on back of map.||||||
14185|Nirranda Group|43208|5|Briefly described|map legend|Early Oligocene|Middle Eocene|||||||
14185|Nirranda Group|43219|5|Briefly described|Fig.3,p6.|Oligocene|Eocene|||||||
14185|Nirranda Group|43590|4|Described|p20|||||||||
14185|Nirranda Group|43604|6|Mentioned|p145|||||||||
14185|Nirranda Group|43660|6|Mentioned|Fig.6,p15|Oligocene|Eocene|||||||
14185|Nirranda Group|43667|6|Mentioned|Fig.3,p12||Eocene|||||||
14185|Nirranda Group|43733|6|Mentioned|Fig.2.11,p65|Oligocene|Eocene|||||||
14185|Nirranda Group|43744|6|Mentioned|Fig.3,p3|||||||||
14185|Nirranda Group|43783|6|Mentioned|Fig14, p11|Early Oligocene|Late Eocene|||||||
14185|Nirranda Group|43784|6|Mentioned|Fig10, p12|Early Oligocene|Late Eocene|||||||
14185|Nirranda Group|43814|6|Mentioned|Fig.3,p115|||||||||
14185|Nirranda Group|43937|5|Briefly described|Map Legend|Middle Eocene|Paleocene|||||||
14185|Nirranda Group|44133|5|Briefly described|p155|Late Eocene|Middle Eocene|Geological Province: Gambier Basin.  Includes: Mepunga Formation, Narrawaturk Marl.||||||
14185|Nirranda Group|46802|6|Mentioned|Table 1|||||||||
14185|Nirranda Group|48911|6|Mentioned|p49|||U.Eocene and Oligocene. Chart 1||||||
14185|Nirranda Group|48977|6|Mentioned|Fig.5|||See also Table 3||||||
14185|Nirranda Group|49060|5|Briefly described|Fig.33|||||||||
14185|Nirranda Group|60451|5|Briefly described|p95 Fig. 61|||||||||
14185|Nirranda Group|60452|5|Briefly described|p15|Eocene|Eocene|Age: 45Ma. Geological Province: Otway Basin.||||||
14185|Nirranda Group|60538|5|Briefly described|p470, Fig. 10, 473 Fig. 12, 474 Fig. 13|Early Oligocene|Late Eocene|Marl, littoral deposits. Includes: Gambier Limestone. Geological Province: Otway Basin.||||||
14185|Nirranda Group|60563|5|Briefly described|p45|||Carbonates. Includes the Narrawaturk Formation and Castle Cove Limestone. Overlies the Wangerrip Group. Geological Province: Otway Basin.||||||
14185|Nirranda Group|60599|5|Briefly described|p15|Middle Miocene|Middle Eocene|Fine-grained marginal marine sediments. Age: ~45Ma. Geological Province:Otway  Basin.||||||
14185|Nirranda Group|61182|3|Fully described|p20, p24, p36|Early Oligocene|Middle Eocene|Comprises Mepunga Fm and Narrawaturk Marl. Overlies Wangerrip Gp; overlain by Heytesbury Group. Formerly Nirranda Sub-group of the Heytesbury Gp; also known as Hanson Plain Sand in Heytesbury Group by some authors. Age: 45-29Ma. ||||||
14185|Nirranda Group|61185|5|Briefly described|p15|Middle Miocene|Middle Eocene|Fine-grained marginal marine sediments. Geological Province: Otway Basin.||||||07-FEB-11
14185|Nirranda Group|61547|6|Mentioned|p461. |Eocene|Eocene|Written as Nirr. Group in the diagram, but shown in full, and in context, in the text on the same page.||||Overlies Wangerrip Group. Is overlain by Heytesbury Group.||
14185|Nirranda Group|61607|6|Mentioned|p5 Fig. 2|Oligocene|Eocene|Geological Province: Otway Basin.||||||12-MAR-09
14185|Nirranda Group|61608|6|Mentioned|p41 Fig. 5|||Refers to equivalent unit.||||||
14185|Nirranda Group|61622|4|Described|p436, p437, p436 Fig. 2|Miocene|Eocene|Includes Narrawaturk Marl. Geological Province: Otway Basin. Thin marls and carbonates deposited in mid to inner shelf environment.||||||07-FEB-11
14185|Nirranda Group|61623|5|Briefly described|p447, p449 Fig. 4|Tertiary|Tertiary|Includes Narrawaturk Marl and Mepunga Formation. Geological Province: Otway Basin.||||||07-APR-09
14185|Nirranda Group|61624|6|Mentioned|p465|Tertiary|Tertiary|Geological Province: Otway Basin.||||||07-APR-09
14185|Nirranda Group|61626|5|Briefly described|p486, p487, p486 Fig. 2, p488, p493|Oligocene|Eocene|Includes; Narrawaturk Marl, Mepunga Formation and Demons Bluff Formation. Geological Province: Otway Basin.||||||
14185|Nirranda Group|61627|5|Briefly described|p500 Fig. 2|Eocene|Eocene|Includes Mepunga Sandstone and Narrawaturk Marl. Geological Province: Otway Basin.||||||07-FEB-11
14185|Nirranda Group|61628|5|Briefly described|p509 Fig. 3|Early Oligocene|Middle Eocene|Includes Demons Bluff and Mepunga Formations and Narrawaturk Marl. Geological Province: Otway Basin.||||||07-APR-09
14185|Nirranda Group|62370|6|Mentioned|p455|||Geological Province: Otway Basin.||||||
14185|Nirranda Group|62896|6|Mentioned|p88|Tertiary|Tertiary|||||||07-FEB-11
14185|Nirranda Group|63122|5|Briefly described|p17 Fig. 4.3, p21|Late Eocene|Middle Eocene|Includes Narrawaturk Marl. Geological Province: Otway Basin. Presented in figure as Nirr. Gp. ||||||
14185|Nirranda Group|63124|4|Described|p49 Fig. 5.2, p87 Fig. 5.29, p90-91|Late Eocene|Middle Eocene|Includes Narrawaturk Marl and Mepunga Formation. Geological Province: Otway Basin. Defined by Bock and Glenie (1965) but was downgraded to subgroup rank in the Heytesbury Group by some authors (Abele et al 1976); this was not generally accepted.||||||23-MAY-13
14185|Nirranda Group|63173|5|Briefly described|p342 Fig. 9.2|Late Oligocene|Middle Eocene|Geological Province: Otway Basin, offshore. Transgressive, shallow marine sedimentation.||||||07-FEB-11
14185|Nirranda Group|63269|5|Briefly described|p604-605|Oligocene|Eocene|Otway Basin.|||Demons Bluff, Mepunga Formations; Narrawaturk Marl.|Unconformably overlies Wangerrip Group. Is overlain unconformably by Heytesbury Group.||
14185|Nirranda Group|63431|5|Briefly described|p677 Fig. 2|Eocene|Eocene|Includes Narrawaturk Marl and Mepunga Formation.  Overlies Wangerrip Group; overlain by Heytesbury Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
14185|Nirranda Group|63740|6|Mentioned|p88|Tertiary|Tertiary|||||||07-FEB-11
14185|Nirranda Group|65316|6|Mentioned|p597|||Largely subsurface; part of the Otway Basin; thought to correlate with the Demons Bluff Group.||||||23-APR-12
14185|Nirranda Group|65715|5|Briefly described|p11 Tb.7|Paleogene|Paleogene|Includes Narrawaturk Marl.||||||
14185|Nirranda Group|66002|5|Briefly described|p10 Tb.7, p16, p26 Fig.7|Paleogene|Paleogene|Includes Narrawaturk Marl and Mepunga Formation. Defined by Glenie 1971. Some outcrops in Port Campbell Embayment area reassigned to Wiridjil Gravel.||||||
14185|Nirranda Group|66181|6|Mentioned|p312|Eocene||Gippsland Basin||||||
14185|Nirranda Group|66245|5|Briefly described|p6 Fig.5, p8. |Rupelian|Lutetian|Coastal and shallow marine, progradational sequence of carbonates. Helped in building out the present day shelf.|||Includes Mepunga, Demons Bluff and ?Eastern View Formations and Narrawaturk Marl.|||
14185|Nirranda Group|67061|6|Mentioned|p546 Fig.3.|Oligocene|Eocene||||Includes Mepunga Formation and Narrawaturk Marl.|||
14185|Nirranda Group|67366|6|Mentioned|p103 Fig.2. |Oligocene|Eocene||||Includes Mepunga Formation and Narrawaturk Marl.|Unconformably overlies Wangerrip Group. Is unconformably overlain by Heytesbury Group.||
14185|Nirranda Group|67367|5|Briefly described|p130, p131 Fig.2. |Early Oligocene|Middle Eocene|Siliciclastics. Stratigraphic equivalent to Latrobe Group, offshore Gippsland Basin.|||Includes Mepunga, Demons Bluff and Narrawaturk Formations.|||
14185|Nirranda Group|69297|6|Mentioned|p78, p79, p98, p112, p115|Priabonian|Bartonian|Otway and Sorell Basins. Coastal plain to open marine siliciclastic and carbonate sediments. Potential reservoir in the Sorell Basin. |||Includes the Mepunga Formation, Narrawaturk Marl and the Wangoom Sand. |Unconformably overlies the Wangerrip Group. Overlain by the Heytesbury Group. ||
14185|Nirranda Group|69651|5|Briefly described|p6, p10, p12, p32, p38|Miocene|Eocene|Otway Basin. Mixed carbonate/siliciclastic rocks. Modelling diagrams.|||Eastern View, Mepunga, Demons Bluff Formations; Narrawaturk Marl.|Unconformably overlies Wangerrip Group. Is overlain unconformably by Heytesbury Group.||
14185|Nirranda Group|69879|5|Briefly described|p418, p424|Oligocene|Eocene|Strahan Sub-basin. Shown as Nirranda Group equivalent. Offshore exploration well Cape Sorell 1.||||Overlies Wangerrip Group. Underlies Heytesbury Group. |Alternating beds of silty claystone/clayey siltstone (with organic content and terrestrial input) with clastics, and quartzitic sandstone. Fine sandstone and calcareous mudstone deposited in a shelfal marine environment.|
14185|Nirranda Group|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4; p5|Oligocene|Eocene|Otway Basin: Gambier Embayment and Voluta Trough. Prograding nearshore to offshore marine clastics grading upwards into increasingly open marine carbonates.|||Narrawaturk Marl, Mepunga Formation, Wangoom Sand.|Overlies Wangerrip Group. Is overlain by Heytesbury Group.||
14185|Nirranda Group|70078|5|Briefly described|Northern: Fig.2; p2. Regional: Fig.4; p5|Eocene|Eocene|Otway Basin. Sandstones equivalent to this unit in the Sorell Basin are potential hydrocarbon sources; sealed by Heytesbury Group marls and fine-grained carbonates.|||Mepunga Formation, Narrawaturk Marl.|Overlies Wangerrip Group. Is overlain by Heytesbury Group.||
14185|Nirranda Group|70379|6|Mentioned|p724-727|||Otway Basin.||||Overlies Wangerrip Group. Is overlain by Heytesbury Group.||
14185|Nirranda Group|71437|4|Described|Fig. 1 opp 154, p155, p159-160|Oligocene|Eocene|Marine sediments include foraminifera and macrofossils.|||Includes Mepunga Group, Narrawaturk Marl.|Disconformably overlies Wangerrip Group. Overlain by Heytesbury Group.|Marl-sandy limestone suite.|
14185|Nirranda Group|71593|5|Briefly described|p51|Miocene|Oligocene|||||||
14185|Nirranda Group|73356|6|Mentioned|p3, p15-16|Oligocene|Eocene|Prograding marine clastics and carbonates.||||Unconformably overlain by Heytesbury Group.||
14185|Nirranda Group|73357|6|Mentioned|p44, p46, p48|Rupelian|Bartonian|Otway Basin.|||Includes Mepunga Formation, Narrawaturk Marl.|Overlies Wangerrip Group, underlies Heytesbury Group.||
14185|Nirranda Group|73383|4|Described|p3, p7 Tb.3.1, p10, p21, p27|Oligocene|Eocene|Otway Basin. Mid to late Eocene. Clastic units of Nirranda Group are equivalent to chemostratigraphic Sequence S5 which has generally lower Ti/Th values than other sequences in the Otway Basin. Carbonate units are equivalent to chemostratigraphic Sequence S6, primarily defined by high Ca values.|||Narrawaturk Marl, Demons Bluff Formation, Mepunga Formation|Overlies Wangerrip Group, underlies Heytesbury Group|Clastic and carbonate units including sandstones, mudstones, marls and calcareous mudstones.|
14185|Nirranda Group|73385|5|Briefly described|p3-5|Oligocene|Eocene|Otway Basin. Overlies intra-Lutein unconformity from localised inversion, underlies intra-Oligocene unconformity.|||Demons Bluff Formation, Mepunga Formation, Narrawaturk Marl|Unconformably overlies Wangerrip Group, unconformably underlies Heytesbury Group.|Prograding marine clastics and carbonates.|
14185|Nirranda Group|73386|4|Described|p1-2, p4-7, p13-14, iii, Attachment A1|Rupelian|Bartonian|Otway Basin, absent along northern margin. Thins to the northeast, onlapping the top of the Wangerrip Group or the top of the Eumeralla Formation. Represents change from siliciclastic to carbonate-dominated deposition with flooding of marine margin, chemostratigraphic division into sequences S5 and S6 of Forbes et al. (2020). Separated from underlying Wangerrip Group by an intra-Lutetian unconformity. Nothofagidites asperus to Lower Proteacidites tuberculatus spore-pollen zones.|||Narrawaturk Marl, Mepunga Formation|Unconformably overlies Wangerrip Group, unconformably underlies Heytesbury Group|Marine clastics and carbonates.|
14185|Nirranda Group|73486|5|Briefly described|p511 Fig.2, p516|Rupelian|Lutetian|Otway Basin.|||Eastern View Formation, Demons Bluff Formation, Mepunga Formation, Narrawaturk Marl|Underlies Heytesbury Group||
14185|Nirranda Group|73594|5|Briefly described|p4-5|Oligocene|Eocene|Otway Basin. Maximum thickness of ~200m in onshore areas, reaches 800m at the present-day shelf break.|||Demons Bluff Formation, Mepunga Formation, Narrawaturk Marl|Overlies Wangerrip Group, underlies Heytesbury Group||
73299|Nirranda Supersequence|63134|2|Defined|111-112|||||||||
73299|Nirranda Supersequence|63269|5|Briefly described|p605|Oligocene|Eocene|Otway Basin.||||Overlies Wangerrip Supersequence. Is overlain by Heytesbury Supersequence.||
73299|Nirranda Supersequence|69297|6|Mentioned|p80, p98, p110, p111|||Misspelt as the Nirrandra Supersequence on p98. ||||||
73299|Nirranda Supersequence|69651|5|Briefly described|p10, p12-15, p17-19, p22-23, p29, p39|Oligocene|Eocene|See also p44-47, p49-50. Relatively thin and undeformed open marine deposits; marks a major marine transgression. Possible seals. Modelling diagrams.||||Overlies Wangerrip Supersequence conformably [!]. Is overlain by Heytesbury Supersequence.|Calcareous claystone overlain by marls, calcarenite and calcilutite; shaly limestone overlain by calcarenite and calcilutite; quartz sandstone overlain by silty mudstone, and limestone.|
73299|Nirranda Supersequence|70077|5|Briefly described|Regional: Fig.4; p4-5|Oligocene|Eocene|Otway Basin.||||Overlies Wangerrip Supersequence. Is overlain by Heytesbury Supersequence.||
73299|Nirranda Supersequence|70078|5|Briefly described|Regional: Fig.4; p3|Oligocene|Eocene|Deposition was truncated by a major mid-Oligocene unconformity.||||Overlies Wangerrip Supersequence. Is overlain unconformably by Heytesbury Supersequence.|Shallow-marine sandstones, marls and limestones.|
73299|Nirranda Supersequence|70880|5|Briefly described|p77|Oligocene|Eocene|Otway Basin. Open marine environment.||||Overlies Wangerrip Supersequence. Is overlain by Heytesbury Supersequence.|Mixed carbonate/siliciclastic sediments.|
73299|Nirranda Supersequence|71266|5|Briefly described|p614 Fig.3, p615|Oligocene|Eocene|Otway Basin.||||Overlies Wangerrip Supersequence. Is overlain by Heytesbury Supersequence.||
31415|Nobby Road Sandstone|22968|3|Fully described|P31, Fig32, P116||Silurian|Type section location given on P119, parent is Barmouth Group, conformably underlain by Koomberar Formation, maximum thickness is 500m||||||
31415|Nobby Road Sandstone|23020|5|Briefly described|Map legend|Pridoli|Pridoli|Parent is Barmouth Group||||||
31415|Nobby Road Sandstone|23309|5|Briefly described|p90-92. Tb 2.33|||||||||
31415|Nobby Road Sandstone|24551|4|Described|p137|Silurian|Silurian|Of the Barmouth Group.||||||03-AUG-05
31415|Nobby Road Sandstone|68116|5|Briefly described|Appendix, Map 35.|Silurian|Silurian||||||Sandstone, siltstone: sandstone quartzose to arkosic, medium to fine-grained; minor feldspathic granule conglomerate.|
14226|Noora Sand|37661|6|Mentioned|p8.2.5|||||||||
29296|Noorinbee Granodiorite|22878|4|Described|p76|||||||||
29296|Noorinbee Granodiorite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Of the Tonghi Supersuite. Biotite hornblende granodiorite: dark greenish grey, coarse grained, weakly to strongly foliated; abundant mafic inclusions||||||01-OCT-04
29296|Noorinbee Granodiorite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Tonghi Supersuite. Biotite hornblende granodiorite: dark greenish grey, coarse grained, weakly to strongly foliated; abundant mafic inclusions||||||01-OCT-04
29296|Noorinbee Granodiorite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Tonghi Supersuite. Biotite-hornblende granodiorite: Moderately magnetic (up to 120 nT). High K, low Th and U.||||||06-OCT-04
29296|Noorinbee Granodiorite|23309|5|Briefly described|p323.|||G15 I-Type - Supersedes Noorinbee Granite.||||||
29296|Noorinbee Granodiorite|30574|5|Briefly described|p11|||||||||
29296|Noorinbee Granodiorite|30938|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
29296|Noorinbee Granodiorite|35277|6|Mentioned|Fig.5.14|||||||||
29296|Noorinbee Granodiorite|35278|6|Mentioned|p359|||||||||
29296|Noorinbee Granodiorite|38367|6|Mentioned|Table 3|||||||||
29296|Noorinbee Granodiorite|40889|5|Briefly described|p97|||||||||
29296|Noorinbee Granodiorite|41641|6|Mentioned|Fig.5.14|||||||||
29296|Noorinbee Granodiorite|41850|6|Mentioned|p430|||||||||
29296|Noorinbee Granodiorite|42827|5|Briefly described|Fig 5.15|||||||||
29296|Noorinbee Granodiorite|68116|5|Briefly described|Appendix, Maps 37, 46.|Early Devonian|Early Devonian||||||Biotite-hornblende granodiorite: dark greenish grey, coarse grained, weakly to strongly foliated; abundant mafic inclusions: I-type.|
14255|Normanville Group|22573|5|Briefly described|p 47||Cambrian|U-Pb zircon age 526Ma||||||
14255|Normanville Group|22581|5|Briefly described|Fig.2,p37||Cambrian|Kanmantoo Basin||||||
14255|Normanville Group|22603|6|Mentioned|p99||Early Cambrian|540 Ma (?)||||||
14255|Normanville Group|22634|5|Briefly described|p506|Cambrian|Neoproterozoic|||||||
14255|Normanville Group|22643|5|Briefly described|p186, fig3p187|Early Cambrian|Early Cambrian|||||||
14255|Normanville Group|22671|6|Mentioned|p846,848||Early Cambrian|Max Age: 526 (+/-) 4 Ma. Top of the group generally equated with Truro Volcanics.||||||18-JAN-06
14255|Normanville Group|22726|6|Mentioned|p233||Early Cambrian|||||||
14255|Normanville Group|22755|4|Described|p547, p548, p555||Early Cambrian|Of Stansbury Basin.||||||03-FEB-09
14255|Normanville Group|22766|4|Described|Fig.2 p561, p562||Tommotian|||||||
14255|Normanville Group|22772|5|Briefly described|Table 13.1|Early Cambrian|Early Cambrian|||||||
14255|Normanville Group|22830|6|Mentioned|P25||Cambrian|||||||
14255|Normanville Group|22857|5|Briefly described|Tb. 13.1 (insert p70-71), p88 Fig. 14.7A|Early Cambrian|Early Cambrian|Of the Moralana Supergroup. Age: <545Ma. Geological Province: Kanmantoo Trough; in the Stansbury Basin also. See also p93-94.||||||03-MAY-13
14255|Normanville Group|22858|6|Mentioned|p93,Fig14.7ap88-9|||||||||
14255|Normanville Group|23023|6|Mentioned|p1797|||||||||
14255|Normanville Group|23309|5|Briefly described|p26-27, 40, 46, 195||Cambrian|||||||
14255|Normanville Group|23317|5|Briefly described|377|Early Cambrian|Early Cambrian|||||||
14255|Normanville Group|23539|5|Briefly described|p 467|||||||||
14255|Normanville Group|23854|6|Mentioned|p863|||||||||
14255|Normanville Group|23869|5|Briefly described|p15 Fig. 3|Cambrian|Cambrian|||||||
14255|Normanville Group|23932|5|Briefly described|p667|Early Cambrian|Early Cambrian|Geological province: Adelaide Fold Belt.||||||
14255|Normanville Group|23981|5|Briefly described|p13, p20|Early Cambrian|Early Cambrian|Thickness: ~1000m. Geological Province: Stansbury (Fleurieu Peninsula) Basin. Comprises basal sandstones, shelf and ramp carbonates and includes relatively deep water phosphatic Heatherdale Shale.||||||04-FEB-08
14255|Normanville Group|24465|5|Briefly described|p343|Early Cambrian|Early Cambrian|Overlain by Kanmantoo Group. Geological Province: Stansbury Basin.||||||31-JAN-08
14255|Normanville Group|24551|5|Briefly described|p74|Cambrian|Cambrian|Of the Moralana Supergroup in SA.||||||
14255|Normanville Group|30381|6|Mentioned|p222|||||||||
14255|Normanville Group|32457|6|Mentioned|p88|||||||||
14255|Normanville Group|33471|5|Briefly described|p555|||||||||
14255|Normanville Group|34615|6|Mentioned|p7|||Shown on Figure.||||||
14255|Normanville Group|35092|6|Mentioned|p108|||||||||
14255|Normanville Group|35255|6|Mentioned|Fig.8|||||||||
14255|Normanville Group|36731|5|Briefly described|p124|||||||||
14255|Normanville Group|37461|6|Mentioned|Table 5.I|||||||||
14255|Normanville Group|38004|6|Mentioned|Table 1|||||||||
14255|Normanville Group|38157|6|Mentioned|Table V|||||||||
14255|Normanville Group|38703|6|Mentioned|p131|||||||||
14255|Normanville Group|38704|6|Mentioned|p133|||||||||
14255|Normanville Group|38873|4|Described|Table 2|||||||||
14255|Normanville Group|39344|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
14255|Normanville Group|39352|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
14255|Normanville Group|39489|6|Mentioned|Fig.1|||||||||
14255|Normanville Group|39806|6|Mentioned|p207|||||||||
14255|Normanville Group|39842|6|Mentioned|p5|||||||||
14255|Normanville Group|40228|5|Briefly described|Fig.1|||||||||
14255|Normanville Group|40442|4|Described|p13|||||||||
14255|Normanville Group|40454|6|Mentioned|p43|||||||||
14255|Normanville Group|40455|5|Briefly described|p67|||||||||
14255|Normanville Group|40456|6|Mentioned|Fig.2|||||||||
14255|Normanville Group|40503|4|Described|p107|||||||||
14255|Normanville Group|40763|5|Briefly described|p206|||||||||
14255|Normanville Group|40852|6|Mentioned|p32|||||||||
14255|Normanville Group|41103|6|Mentioned|p261|||||||||
14255|Normanville Group|41401|5|Briefly described|p32|||||||||
14255|Normanville Group|41526|6|Mentioned|p3|||See also P11||||||
14255|Normanville Group|41853|6|Mentioned|p195|||||||||
14255|Normanville Group|41947|6|Mentioned|p16|||||||||
14255|Normanville Group|42222|4|Described|p20|||||||||
14255|Normanville Group|42225|6|Mentioned|Fig.4 P224|||||||||
14255|Normanville Group|42232|6|Mentioned|p283|||||||||
14255|Normanville Group|42243|5|Briefly described|p207|||||||||
14255|Normanville Group|42266|6|Mentioned|p290|||||||||
14255|Normanville Group|42268|5|Briefly described|p328|||||||||
14255|Normanville Group|42269|6|Mentioned|Fig.1 P335|||||||||
14255|Normanville Group|42270|5|Briefly described|p353|||||||||
14255|Normanville Group|42271|5|Briefly described|p386|||||||||
14255|Normanville Group|42272|6|Mentioned|Fig.2 P400|||||||||
14255|Normanville Group|42275|5|Briefly described|p468|||||||||
14255|Normanville Group|42357|5|Briefly described|p10|||||||||
14255|Normanville Group|42488|5|Briefly described|p185, Fig.2 p187|||||||||
14255|Normanville Group|42505|5|Briefly described|Map legend|Cambrian||||||||
14255|Normanville Group|42506|5|Briefly described|Map legend|Early Cambrian||||||||
14255|Normanville Group|42600|6|Mentioned|p10|||||||||
14255|Normanville Group|42788|6|Mentioned|p148|||||||||
14255|Normanville Group|42982|6|Mentioned|Table 1,p333|||||||||
14255|Normanville Group|43052|5|Briefly described|Fig.2.14|||||||||
14255|Normanville Group|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Marine shelf to basinal carbonate, minor basal sandstone.||||||25-MAY-05
14255|Normanville Group|43190|5|Briefly described|Fig.1,p28.|||||||||
14255|Normanville Group|43192|6|Mentioned|p58||Cambrian|||||||
14255|Normanville Group|43258|5|Briefly described|Map Legend||Cambrian|||||||
14255|Normanville Group|43298|5|Briefly described|Map Legend||Cambrian|||||||
14255|Normanville Group|43595|6|Mentioned|p545||Cambrian|||||||
14255|Normanville Group|43703|6|Mentioned|p75|||||||||
14255|Normanville Group|43759|6|Mentioned|p446|||||||||
14255|Normanville Group|44133|5|Briefly described|p6, 18, 50|Cambrian|Cambrian|Metasediments and volcanics. Includes: Angaston Marble.||||||
14255|Normanville Group|50154|5|Briefly described|p22, p65|Early Cambrian|Early Cambrian|Of the Moralana Supergroup. Overlain by the Kanmantoo Group. Geological Province: Stansbury Basin.||||||16-SEP-04
14255|Normanville Group|60567|5|Briefly described|p39, 41|||Includes the Heatherdale Shale.||||||
14255|Normanville Group|60712|5|Briefly described|p27, p28 Fig. 1|Early Cambrian|Early Cambrian|Metamorphosed clastics and carbonates. Overlain by Kanmantoo Group. Geological Province: Kanmantoo Trough (Adelaide Geosyncline).||||||31-MAY-05
14255|Normanville Group|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Marine shelf to basinal carbonate, minor basal sandstone. Includes acid to basic volcanics near the Murray River.||||||
14255|Normanville Group|61046|5|Briefly described|p8 Fig. 2|Early Cambrian|Early Cambrian|Black shale, limestone. Includes Truro Volcanics.||||||
14255|Normanville Group|61108|5|Briefly described|map legend|Cambrian|Cambrian|Marine shelf to basinal carbonate; minor basal sandstone.||||||
14255|Normanville Group|61307|5|Briefly described|p3-4 Figs. 1 and 2|||Max. thickness: ~1km. Geological Province: Adelaide Fold Belt. See also p23.||||||15-JAN-08
14255|Normanville Group|62664|5|Briefly described|p138 Fig.2.|Cambrian|Early Cambrian|||||Unconformably overlies Wilpena Group of Heysen Supergroup.|Siltstone, carbonates, sandstone.|
14255|Normanville Group|63020|5|Briefly described|p973|Early Cambrian|Early Cambrian|||||||
14255|Normanville Group|63124|6|Mentioned|p49|||Geological Province: Otway Basin.||||||
14255|Normanville Group|63848|6|Mentioned|p533 Fig.2,  p534 Fig.4.||||||Includes Mount Terrible, Wangkonda and Sellick Hill Formations; Fork Tree Limestone; Truro Volcanics and Heatherdale Shale.|||
14255|Normanville Group|64281|5|Briefly described|p29|Cambrian|Cambrian|On Yorke Peninsula, Fleurieu Peninsula. Correlate with Kangaroo Island Group.||||||23-DEC-09
14255|Normanville Group|64647|5|Briefly described|p38 Fig. 1, p46|||Overlies Burra Group. Marine sediments.||||||
14255|Normanville Group|65375|5|Briefly described|p33.|Cambrian|Cambrian|Correlative of Hawker Group above that unit's Uratanna Formation.|||Includes Mount Terrible, Wangkonda and Sellick Hill Formations; Fork Tree Limestone and Heatherdale Shale.|Is overlain by Kanmantoo Group.||
14255|Normanville Group|65376|6|Mentioned|p92 Fig. 2.82. |Cambrian|Cambrian|||||||
14255|Normanville Group|65379|5|Briefly described|p643|||Of Moralana Supergroup. Includes Heatherdale Shale and Angaston Marble. Asbestos occurrence hosted in dolomite and/or limestones in this group.||||||07-MAR-12
14255|Normanville Group|65664|5|Briefly described|p1096, p1103, p1106 Fig.5|Early Cambrian|Early Cambrian||||Includes Heatherdale Shale and Sellicks Hill Formation.|Unconformably overlain by Kanmantoo Group. Unconformably overlies Wilpena Group.||09-MAY-12
14255|Normanville Group|65686|6|Mentioned|p408|||Of the Fleurieu Peninsula. Includes a few poorly preserved trilobites.||||||07-MAY-12
14255|Normanville Group|65892|5|Briefly described|p9 Fig.4, p13, p16, p19.|Early Cambrian|Early Cambrian|Fleurieu Peninsula.|||Includes Mount Terrible, Wangkonda, Sellick Hill Formations; Fork Tree Limestone; Heatherdale Shale; Truro Volcanics.|Is overlain by Kanmantoo Group.||
14255|Normanville Group|67103|6|Mentioned|p612|||||||||
14255|Normanville Group|67536|4|Described|Map Legend|Stage 3|Stage 2|Kanmantoo Province; basement to Murray Basin.|522 +/- 2 Ma|||Intercalated wuth Truro Volcanics.|Marine shelf to basinal carbonate, minor basal sandstone and tuff.|
14255|Normanville Group|68735|5|Briefly described|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin.|||Includes Mount Terrible Formation, Wangkonda Formation, Sellick Hill Formation, Fork Tree Limestone, Heatherdale Shale and Truro Volcanics.|Is overlain by Kanmantoo Group.||10-APR-17
14255|Normanville Group|68822|5|Briefly described|p324|Cambrian|Cambrian|Shallow water depositional environment.|||Includes the Truro Volcanics.|Overlain by the Kanmantoo Formation.||
14255|Normanville Group|68993|5|Briefly described|p544 Fig.1|Early Cambrian|Early Cambrian||||Includes Heatherdale Shale, Truro Volcanics, Fork Tree Limestone; Sellick Hill, Wangkonda and Mount Terrible Formations.|||28-JUL-15
14255|Normanville Group|69255|6|Mentioned|p771|Cambrian|Cambrian||Between 522-515 Ma.|||||
14255|Normanville Group|70125|6|Mentioned|p400 Tb.5||||522 Ma (tuff).|||||
14255|Normanville Group|70493|6|Mentioned|p56|Early Cambrian|Early Cambrian|Delamerian Orogen, SA.||||Is overlain by Kanmantoo Group.||
14255|Normanville Group|71139|6|Mentioned|p152-153, 161|||Adelaide Geosyncline.|c.526 Ma.||Heatherdale Shale.|Is overlain by Kanmantoo Group.||
14255|Normanville Group|71322|5|Briefly described|p52 Fig.1, p73-74|Cambrian|Cambrian||||Marne River Volcanics, Truro Volcanics.|Intrercalated with Truro Volcanics.|Limestone, sandstone, shale, volcanics.|
14255|Normanville Group|71593|5|Briefly described|p19-p21, p170|Early Cambrian|Early Cambrian|||Moralana Supergroup||Unconformably overlies the Heysen Supergroup. Disconformably overlain by the Kanmantoo Group.|Shallow marine sediments including fossiliferous shale and sandstone, limestone, marble, calcareous dolomite and fossiliferous shale.|
14255|Normanville Group|72450|5|Briefly described|Brochure, Brochure map|Early Cambrian|Early Cambrian|Contains some of the oldest shelly fossils (cup-shaped double walled archaeocyaths). Deformed by the Delamerian Orogeny.|||Includes the Heatherdale Shale, Fork Tree Limestone, Sellick Hill Formation, Wangkonda Formation and Mount Terrible Formation.|Overlies the ABC Range Quartzite.||
14255|Normanville Group|73059|5|Briefly described|p1059, 1061|Early Cambrian|Early Cambrian|Delamerian Fold Belt, South Australia. Formed in a synorogenic basinal setting, not in an extensional basin setting.|||Heatherdale Shale, Mount Terrible Formation.|Is overlain by Kanmantoo Group.|Shallow marine succession.|
14255|Normanville Group|73129|6|Mentioned|p45|||||||||
14255|Normanville Group|73188|5|Briefly described|p315-316, p343, p349-351, p353|Early Cambrian|Early Cambrian|Mount Lofty Ranges. Shelf sediments. Records marine transgression and overall upward deepening.|||Heatherdale Shale, Fork Tree Limestone, Sellick Hill Formation, Wangkonda Formation, Mount Terrible Formation|Disconformably underlain by ABC Range Quartzite and Bunyeroo Formation. Disconformably overlain by Kanmantoo Group.|Carbonate dominated with sands and silts.|
14255|Normanville Group|73236|6|Mentioned|p47|Cambrian|Cambrian|Fleurieu Peninsula; eroded from the Hallett Cove area.|c. 530-510 Ma||||Carbonate-dominated.|
14255|Normanville Group|73264|6|Mentioned|p1387 Fig.10, p1388|||Grenvillian zircon population (1000-1200 Ma), small Panafrican peak at 645 Ma.|||Heatherdale Shale, Mount Terrible Formation|||
14255|Normanville Group|73430|5|Briefly described|p491-p493, p497|Early Cambrian|Early Cambrian|Delamerian Orogen. Records rapidly increasing water depth towards the Heatherdale Shale. Deformed in the middle to late Cambrian.|||Truro Volcanics|Underlies Kanmantoo Group|Carbonates. Includes alkali basalt lavas.|
14255|Normanville Group|74367|5|Briefly described|p6, p19|Cambrian|Cambrian|||Moralana Supergroup|Heatherdale Shale||Limestone, sandstone, shale and volcanics.|
14269|North East Metamorphic Complex|38367|6|Mentioned|p122|||See also Table 3||||||
14304|Norton Gully Sandstone|22882|5|Briefly described|p 11|Devonian|Devonian|||||||
14304|Norton Gully Sandstone|22885|5|Briefly described|map|Early Devonian|Early Devonian|Walhalla Group.||||||22-DEC-08
14304|Norton Gully Sandstone|22886|4|Described|p14|Middle Devonian|Early Devonian|Of Walhalla Group.||||||14-APR-08
14304|Norton Gully Sandstone|23229|4|Described|Table3-3p27, 33, 35||Pragian|||||||
14304|Norton Gully Sandstone|23265|5|Briefly described|p342, Fig13-4.4p343|Devonian|Silurian|||||||
14304|Norton Gully Sandstone|23309|5|Briefly described|p146-154. Tb 2.55||Devonian|||||||
14304|Norton Gully Sandstone|24177|3|Fully described|p59, p50 Fig.22|Middle Devonian|Early Devonian|Of the Walhalla Group. Overlain by the Montys Hut Formation. Overlies the Wilson Creek Shale. Geological Province: Mount Easton Province. Interbedded with Wilson Creek Shale and Montys Hut Formation. Age indicated as Emsian, or possibly lower Eifelian.||||||
14304|Norton Gully Sandstone|24224|5|Briefly described|p264|Emsian|Emsian|Geological Province: Turtons Creek Inlier.||||||
14304|Norton Gully Sandstone|24328|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Walhalla Group.||||||17-NOV-08
14304|Norton Gully Sandstone|24329|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Walhalla Group||||||17-NOV-08
14304|Norton Gully Sandstone|24551|5|Briefly described|p123|||||||||
14304|Norton Gully Sandstone|24588|5|Briefly described|p23-26, p12 Fig.3, p15-17|Emsian|Emsian|Geological Province: Mount Easton Province. Of the Walhalla Group. See also p16 Tb.3,  p22, 27, 28, 31.||||||29-NOV-13
14304|Norton Gully Sandstone|32074|6|Mentioned|p180|||||||||
14304|Norton Gully Sandstone|33601|2|Defined|p24|Middle Devonian|Early Devonian|Early - Middle Devonian.||||||14-JAN-09
14304|Norton Gully Sandstone|33604|6|Mentioned|p17|||Correlation chart.||||||14-APR-08
14304|Norton Gully Sandstone|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
14304|Norton Gully Sandstone|34287|6|Mentioned|p95|||||||||
14304|Norton Gully Sandstone|34815|6|Mentioned|p18|||||||||
14304|Norton Gully Sandstone|35073|6|Mentioned|p17|||See also Table 1.||||||
14304|Norton Gully Sandstone|35283|3|Fully described|p56|||||||||
14304|Norton Gully Sandstone|36389|5|Briefly described|p39|||||||||
14304|Norton Gully Sandstone|37270|6|Mentioned|p203|||||||||
14304|Norton Gully Sandstone|37727|6|Mentioned|p65|||||||||
14304|Norton Gully Sandstone|38367|6|Mentioned|p115|||||||||
14304|Norton Gully Sandstone|38787|6|Mentioned|p124|||||||||
14304|Norton Gully Sandstone|39331|6|Mentioned|Table 2-1|||||||||
14304|Norton Gully Sandstone|39551|6|Mentioned|Map legend|Zlichovian|Zlichovian|||||||
14304|Norton Gully Sandstone|39555|6|Mentioned|Map legend|Zlichovian|Zlichovian|||||||
14304|Norton Gully Sandstone|41555|6|Mentioned|Fig.3|||||||||
14304|Norton Gully Sandstone|41585|4|Described|p115|||||||||
14304|Norton Gully Sandstone|42089|6|Mentioned|p26|||||||||
14304|Norton Gully Sandstone|42383|5|Briefly described|Fig.19 P26|||||||||
14304|Norton Gully Sandstone|42827|4|Described|p115|||see also Table 4.1. Of Walhalla Group.||||||17-NOV-08
14304|Norton Gully Sandstone|43461|14|Not recorded|p627|||||||||
14304|Norton Gully Sandstone|43547|14|Not recorded|p150,Table p152||Siegenian|||||||
14304|Norton Gully Sandstone|44187|5|Briefly described|Map Legend||Early Devonian|||||||
14304|Norton Gully Sandstone|44197|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
14304|Norton Gully Sandstone|60529|5|Briefly described|Map Legend|Eifelian|Emsian|Of the Walhalla Group. Moderate to deep water deposit: turbiditic sandstone; thinly to thickly bedded, fine to coarse grained massive sandstone, minor pebbly sandstone and conglomerate.||||||
14304|Norton Gully Sandstone|60599|5|Briefly described|p14, p56|Emsian|Emsian|Of Walhalla Group. Highly variable lithology. Geological Province: Melbourne Zone, Lachlan Fold Belt. See also p47 Fig. 19. ||||||
14304|Norton Gully Sandstone|61185|2|Defined|p43-46, p37, p39, p52, p22, p24-25|Eifelian|Emsian|Of Walhalla Gp. Formerly 'Upper Sandstone Beds' and Norton's Creek Sst. Incl: former Burlington, Wallis, Wilkie and O'Sullivan mbrs, and Flowerdale Sandstone Mbr. Over Wilson Creek Shale; under Montys Hut Fm (conformable); Strathbogie Granite aureole.||||||07-FEB-11
14304|Norton Gully Sandstone|61701|5|Briefly described|Map Legend|Eifelian|Emsian|Of the Walhalla Group. Moderate to deep water deposit: turbiditic sandstone; thinly to thickly bedded, fine to coarse grained massive sandstone, minor pebbly sandstone and conglomerate.||||||
14304|Norton Gully Sandstone|61702|5|Briefly described|Map Legend|Eifelian|Emsian|Of the Walhalla Group. Moderate to deep water deposit: turbiditic sandstone; thinly to thickly bedded, fine to coarse grained massive sandstone, minor pebbly sandstone and conglomerate.||||||
14304|Norton Gully Sandstone|61703|5|Briefly described|Map Legend|Eifelian|Emsian|Of the Walhalla Group. Moderate to deep water deposit: turbiditic sandstone; thinly to thickly bedded, fine to coarse grained massive sandstone, minor pebbly sandstone and conglomerate.||||||
14304|Norton Gully Sandstone|61704|6|Mentioned|Map legend|Devonian|Devonian|Low K (high K in east from granite colluvium), moderate-high Th.||||||
14304|Norton Gully Sandstone|62099|5|Briefly described|p331|Early Devonian|Early Devonian|In eastern Melbourne Zone of the Lachlan Orogen. ||||||
14304|Norton Gully Sandstone|62469|5|Briefly described|p5 Fig. 2|Emsian|Pragian|Geological Province: Darraweit Guim Province.||||||07-FEB-11
14304|Norton Gully Sandstone|64535|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Sandstone, siltstone, minor shale, conglomerate, diamictite, limestone: more lithological detail included: deep-marine turbidite fan and hemipelagic deposits. ||||||
14304|Norton Gully Sandstone|64536|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Sandstone, siltstone, minor shale, conglomerate, diamictite, limestone: more lithological detail included: deep-marine turbidite fan and hemipelagic deposits. Also includes an unnamed conglomerate member and unnamed limestone lenses.||||||07-FEB-11
14304|Norton Gully Sandstone|64537|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Sandstone, siltstone, minor shale, conglomerate, diamictite, limestone: more lithological detail included: deep-marine turbidite fan and hemipelagic deposits. Also includes an unnamed conglomerate member and unnamed limestone lenses.||||||07-FEB-11
14304|Norton Gully Sandstone|64538|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Sandstone, siltstone, minor shale, conglomerate, diamictite, limestone: more lithological detail included: deep-marine turbidite fan and hemipelagic deposits. Also includes an unnamed conglomerate member and unnamed limestone lenses.||||||07-FEB-11
14304|Norton Gully Sandstone|64539|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Sandstone, siltstone, minor shale, conglomerate, diamictite, limestone: more lithological detail included: deep-marine turbidite fan and hemipelagic deposits. ||||||
14304|Norton Gully Sandstone|64540|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Sandstone, siltstone, minor shale, conglomerate, diamictite, limestone: more lithological detail included: deep-marine turbidite fan and hemipelagic deposits. ||||||
14304|Norton Gully Sandstone|64605|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Siltstone, sandstone, minor shale, conglomerate; deep-marine deposits; Speckled brown to speckled pink-blue in RGB. Nonmagnetic.||||||17-NOV-08
14304|Norton Gully Sandstone|64606|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Walhalla Group. Sandstone, siltstone, minor shale, conglomerate: deep-marine deposits. Speckled brown to speckled blue-pink in RGB. Nonmagnetic.||||||11-NOV-08
14304|Norton Gully Sandstone|64616|3|Fully described|p107, p155, p159, p160-161, p163-164|Emsian|Pragian|See also p166-174, p179, p182-183, p185-186, p192, p197 Fig.6.34, p201 Tb.7.1, p204, p208 Fig.8.1, p214, p220-221, p226-229, p249-251, p254, p278, p280-281, p283, p285-286, p288-291, p293-295, p303, p385 Tb.1, p386-387. Of Walhalla Group. Conformable between the Easts Lookout Formation (or the Wilson Creek Shale) below and the Montys Hut Formation above. 450-2700+m thick. Includes basal Marshall Creek Member. Diverse lithology: thick-bedded turbidite sandstone and shaly siltstone most common; minor shale, conglomerate (or granulestone) in the northeast, limestone lenses. Abundant shelly fossils, flora & some conodonts. Hosts Thomson River Cu deposit. Has been mined for ornamental stone and quicklime. Geophysical characteristics given. Trilobite fossils described.||||||
14304|Norton Gully Sandstone|65716|5|Briefly described|p33-39||Emsian|From Warburton 250k sheet. Of Walhalla Group. Massive, fine-grained tuff, several metres thick and ~100m above fossiiferous horizon in Norton Gully Sandstone.Dated by SHRIMP zircon U-Pb at 403.8 +/- 3.2 Ma which constrains max depositional age.||||||20-AUG-18
14304|Norton Gully Sandstone|66576|5|Briefly described|pp972-973, p975.|Devonian|Devonian|||Basal unit in Walhalla Group.|Misspelled as Norton Gully sandstone on p972.|Is overlain by Montys Hut Formation.|Thick-bedded, medium- to fine-grained sandstone with interbedded shaly siltstone, which displays coarse to fine turbiditic grading.|04-SEP-14
14304|Norton Gully Sandstone|66769|6|Mentioned|135, fig 13|Early Devonian|Early Devonian|North dipping and younging.||||||
14304|Norton Gully Sandstone|67847|6|Mentioned|p44 fig 3.2.2.|Early Devonian|Early Devonian|||Walhalla Group||||
14304|Norton Gully Sandstone|68116|5|Briefly described|Appendix, Maps 18, 25, 33-34, 42-43, 52.|Emsian|Emsian|Limestone lenses occur in the Maindample area. Conglomerate often contains abundant fossils. Dark grey to black siltstone and shale.|||||Sandstone, siltstone, minor shale, conglomerate, diamictite, limestone: sandstone thick to thin bedded, turbidites, granulestone to fine-grained sandstone; siltstone and shale well laminated; conglomerate and diamictite with well rounded pebbles. |
14304|Norton Gully Sandstone|69089|5|Briefly described|Map legend|Early Devonian|Early Devonian|||Unit in Walhalla Group.|||Marine: sandstone, thick to thin bedded; siltstone, minor conglomerate, limestone lenses.|
14304|Norton Gully Sandstone|70487|6|Mentioned|p12, p14, p11 Fig.5|Emsian|Emsian|Presently, 'Plectodonta bipartita' has (sic not) been found in the Norton Gully Sandstone, and its presence is therefore a good indicator of a Lochkovian (or earlier) rather than Pragian-Emsian age. (Earp 2015). Possibly meaning 'has'been found.||||Overlies Wilson Creek Shale, Easts Lookout Siltstone.|Fossiliferous sandstone.|
14304|Norton Gully Sandstone|70742|5|Briefly described|p161-163, p165, p173, p175|Emsian|Emsian|Now known to contain the anetoceratid ammonoid Ivoites (Becker pers. comm. 2011); useful for extending intenational ammonoid zonations to central Victoria. Probably several thousand metres thick. Systematic palaeontology.|403.8 +/- 3.2 Ma (Morand and Fanning, 2006).|Walhalla Group.||Is overlain conformably by Montys Hut Formation.||
14304|Norton Gully Sandstone|70933|14|Not recorded|p94|||Stratigraphy.||||||
14304|Norton Gully Sandstone|73264|6|Mentioned|p1394 Fig.16|Emsian|Emsian|Melbourne Trough.||||||
14304|Norton Gully Sandstone|73497|5|Briefly described|Map legend|Devonian|Devonian|Marine.||Walhalla Group|||Sandstone, shale, siltstone and conglomerate: weakly-moderately magnetic; low K, moderate-high Th.|
14304|Norton Gully Sandstone|74367|6|Mentioned|p16|Early Cambrian|Early Cambrian|||||||
14304|Norton Gully Sandstone|75072|6|Mentioned|p232, 240|Early Devonian|Early Devonian|Melbourne Zone. Zircon age distribution.||||||
83453|Norval Regolith|73505|6|Mentioned|p11, p13, p36|||At the top of Olney Formation.||||Overlies Olney Formation, underlies Geera Clay||
28876|Notostrea Greensand|22706|6|Mentioned|Fig2,p79||Late Eocene|||||||
28876|Notostrea Greensand|24551|6|Mentioned|p297 Fig. 10.7|||||||||03-AUG-05
28876|Notostrea Greensand|41626|6|Mentioned|Fig.2|||||||||
28876|Notostrea Greensand|61182|5|Briefly described|p33|||Part of Mepunga Formation. Overlain by marl (unnamed). ||||||
37586|Nowa Nowa Conglomerate|23309|4|Described|p111 table 2.40|||Of Ninnie Subgroup.  Maximum Thickness: ~150m.||||||
37586|Nowa Nowa Conglomerate|24551|4|Described|p143|||Of the Ninnie Subgroup.||||||03-AUG-05
37586|Nowa Nowa Conglomerate|60542|3|Fully described|p57, p54, p13 |Early Devonian|Early Devonian|Of the Ninnie Subgp. Volcanolithic conglomerate and sandstone; high proportion of grains and clasts of lava, mostly rhyolite, and some andesite. Conformably overlies Boggy Creek Sandstone. Max. thick. at Mt Nowa Nowa: ~150m. ||||||
37586|Nowa Nowa Conglomerate|68116|5|Briefly described|Appendix, Map 45.|Pragian|Pragian||||||Volcanolithic breccia, conglomerate and sandstone with clasts predominantly of glassy rhyolite and minor andesite; lava dome flank deposits.|
69412|Nowyeo Granite|61160|4|Described|p60, p33 Tb. 5.2|Early Silurian|Early Silurian|S-type. Described by Willing (1975) as an alkali granite laccolith.  Rock is a muscovite-biotite leucogranite. Intrudes the Omeo Metamorphic Complex sillimanite gneiss and Cobungra Granite. G70See also p58-59 Fig. 6.8.||||||
69412|Nowyeo Granite|61164|5|Briefly described|map legend|Early Silurian|Early Silurian|Muscovite-biotite leucogranite: variable from fine grained and equigranular to coarse feldspar-phyric; alteration common; metamorphosed; weak foliation; S-type intrusion. GSV map code: G165.||||||
69412|Nowyeo Granite|61165|5|Briefly described|map legend|Early Silurian|Early Silurian|Muscovite-biotite leucogranite: variable from fine grained and equigranular to coarse feldspar-phyric; alteration common; metamorphosed; weak foliation; S-type intrusion. GSV map code: G165.||||||
69412|Nowyeo Granite|61166|5|Briefly described|map legend|Early Silurian|Early Silurian|Muscovite-biotite leucogranite: variable from fine grained and equigranular to coarse feldspar-phyric; alteration common; metamorphosed; weak foliation; S-type intrusion. GSV map code: G165.||||||
69412|Nowyeo Granite|61167|5|Briefly described|map legend|Early Silurian|Early Silurian|Muscovite-biotite leucogranite: variable from fine grained and equigranular to coarse feldspar-phyric; alteration common; metamorphosed; weak foliation; S-type intrusion. GSV map code: G165.||||||07-FEB-11
69412|Nowyeo Granite|61168|5|Briefly described|map legend|Early Silurian|Early Silurian|Muscovite-biotite leucogranite: S-type; nonmagnetic; no mapped gravity response; high total radioelement, K, Th and U. GSV map code: G165.||||||06-OCT-05
69412|Nowyeo Granite|68116|5|Briefly described|Appendix, Map 27.|Silurian|Silurian||||||Muscovite-biotite leucogranite: variable from fine grained and equigranular to coarse feldspar-phyric; alteration common; metamorphosed; weak foliation; S-type.|
36808|Nuggetty Reef Granite|23810|5|Briefly described|Table 1, p886||Devonian|Felsic I-Type. Age: 369+/-2 Ma (SHRIMP U-Pb age).  Geological Province: Lachlan Fold Belt.||||||
36808|Nuggetty Reef Granite|67978|5|Briefly described|p500 Tb.1, p515|Famennian|Famennian|Zircon dating of aplite from Maldon (Bierlein et al. 1999a).|368 +/- 3 Ma, SIMS U-Pb|||||19-SEP-14
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||||||
14374|Nullawarre Greensand|12796|4|Described|p460, p456 Fig. 2|Santonian|Santonian|Of Sherbrook Gp. Originally basal member of Paarratte Fm. Fine-coarse-grained sandstone of quartz grains and glauconite pellets. Interfingering and overlying Belfast Mdst; underlies Skull Creek Mdst. Geol. Prov: Otway Basin/Port Campbell Embayment.||||||
14374|Nullawarre Greensand|22470|5|Briefly described|p13 Fig. 17|Santonian|Santonian|Of Sherbrook Group.||||||
14374|Nullawarre Greensand|22674|5|Briefly described|Fig.2 p719|Campanian|Santonian|||||||
14374|Nullawarre Greensand|22875|3|Fully described|p44|Late Cretaceous|Late Cretaceous|Of the Sherbrook Group.||||||26-SEP-07
14374|Nullawarre Greensand|22944|5|Briefly described|Fig3|||||||||
14374|Nullawarre Greensand|24551|6|Mentioned|p257 Fig. 9.25|||Of the Sherbrook Group.||||||04-FEB-08
14374|Nullawarre Greensand|24562|5|Briefly described|p6, 8 Fig. 2|Late Cretaceous|Late Cretaceous|Of the Sherbrook Group.  Geological Province: Otway Basin.||||||
14374|Nullawarre Greensand|30578|5|Briefly described|p7|||||||||
14374|Nullawarre Greensand|30580|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14374|Nullawarre Greensand|30932|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|Part of Paaratte Formation.||||||04-FEB-08
14374|Nullawarre Greensand|31424|6|Mentioned|Fig.2|||||||||
14374|Nullawarre Greensand|36913|6|Mentioned|Fig.2|||||||||
14374|Nullawarre Greensand|41016|5|Briefly described|Table 1|||||||||
14374|Nullawarre Greensand|41185|6|Mentioned|p177|||||||||
14374|Nullawarre Greensand|41642|4|Described|p244|||||||||
14374|Nullawarre Greensand|41704|6|Mentioned|Fig.3|||||||||
14374|Nullawarre Greensand|41868|6|Mentioned|p533|||||||||
14374|Nullawarre Greensand|42524|5|Briefly described|Fig.3 P27|||||||||
14374|Nullawarre Greensand|42555|5|Briefly described|p285|||||||||
14374|Nullawarre Greensand|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
14374|Nullawarre Greensand|43171|6|Mentioned|5|||Of Sherbrook Formation||||||
14374|Nullawarre Greensand|43208|5|Briefly described|map legend|Campanian|Santonian|Of Sherbrook Group.||||||
14374|Nullawarre Greensand|43590|4|Described|p14|Campanian|Santonian|||||||
14374|Nullawarre Greensand|43660|6|Mentioned|Fig.6,p15||Late Cretaceous|||||||
14374|Nullawarre Greensand|43744|6|Mentioned|Fig.3,p3|||||||||
14374|Nullawarre Greensand|43937|5|Briefly described|Map Legend|Santonian|Aptian|||||||
14374|Nullawarre Greensand|61017|5|Briefly described|p5 Fig. 2|Santonian|Santonian|Of the Sherbrook Group. Geological Province: Otway Basin. See also p6 Fig. 3.||||||07-FEB-11
14374|Nullawarre Greensand|61182|3|Fully described|p17-18, p31, p88|Campanian|Santonian|Of Sherbrook Gp. Conformably overlies/interfingers with Belfast Mudstone; conformably overlain by Paaratte Fm. Max. thickness: ~130m. Geol.Prov: Otway Basin. Light greenish-grey, fine- to coarse-gr. sandstone. Formerly regarded as part of Paarratte Fm.||||||
14374|Nullawarre Greensand|61230|6|Mentioned|p319 Fig.2.|Santonian|Coniacian|||Unit in Sherbrook Group.||||
14374|Nullawarre Greensand|61470|5|Briefly described|p28 Fig. 5|Santonian|Santonian|Of the Sherbrook Group. Overlies and interfingers with Belfast Mudstone; underlies Skull Creek Mudstone. Geological Province: Otway Basin.||||||12-OCT-05
14374|Nullawarre Greensand|61625|5|Briefly described|p475, p476 Fig. 1, p477, p480, p483|Late Creatceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin. Coarsening upward profile of fine- very coarse-grained glaconitic sandstone.||||||07-FEB-11
14374|Nullawarre Greensand|61628|5|Briefly described|p509 Fig. 3|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||31-MAR-09
14374|Nullawarre Greensand|63124|5|Briefly described|p48 Fig. 5.1|||Previously Nullawarre Greensand Member (Sprigg 1986) as a member of his Paaratte Formation; elevated to formation status by Williamson et al (1987). Interfingers with Belfast Mudstone representing a shelf equivalent. Geological Province: Otway Basin.||||||
14374|Nullawarre Greensand|63269|5|Briefly described|p605|Late Cretaceous|Late Cretaceous|Otway Basin.||Sherbrook Group.||||
14374|Nullawarre Greensand|66245|5|Briefly described|p6 Fig.5. |Campanian|Santonian|||Unit in Sherbrook Group.||Is intercalated with Belfast Mudstone and Paaratte Formation.||
14374|Nullawarre Greensand|67061|6|Mentioned|p546 Fig.3.|Late Cretaceous|Late Cretaceous|||Unit in Sherbrook Group.||||
14374|Nullawarre Greensand|67367|5|Briefly described|p131 Fig.2. |Late Cretaceous|Late Cretaceous|||Unit in Sherbrook Group.||||
14374|Nullawarre Greensand|69297|5|Briefly described|p79, p98|Santonian|Santonian|Otway Basin. ||Sherbrook Group||Overlies the Belfast Mudstone. Overlain by the Skull Creek Mudstone. |Mudstone and greensand. |
14374|Nullawarre Greensand|69651|5|Briefly described|p10|Late Cretaceous|Late Cretaceous|||Sherbrook Group.||Is interbedded with Belfast Mudstone and Paaratte Formation.||
14374|Nullawarre Greensand|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Santonian|Santonian|Otway Basin: Port Campbell Embayment.||Sherbrook Group.||Overlies Belfast Mudstone. Is overlain by Skull Creek Mudstone.||
14374|Nullawarre Greensand|70193|6|Mentioned|p284 Fig 2, p285 fig 3|Santonian|Santonian|Geological province: Otway Basin. Part of the Sherbrook Supersequence.||||||
14374|Nullawarre Greensand|70880|6|Mentioned|p77|Santonian|Santonian|Otway Basin.||||||
14374|Nullawarre Greensand|71266|6|Mentioned|p614 Fig.3|Late Cretaceous|Late Cretaceous|Otway Basin.||||||
14374|Nullawarre Greensand|71437|6|Mentioned|p157|Late Cretaceous|Late Cretaceous|Abbreviation of Nullawarre Greensand Member.||Of Paaratte Formation.||||
14374|Nullawarre Greensand|73357|5|Briefly described|p21, p31, p45|Santonian|Santonian|Otway Basin. Correlated with the Isabelidinium cretaceum Dinocyst Zone and Tricolpites apoxyexinus Spore-Pollen Zone.||Of Sherbrook Group.||Overlies Belfast Mudstone, underlies Skull Creek Mudstone.||
14374|Nullawarre Greensand|73383|5|Briefly described|p3, p10 Tb.3.7, p21-22, p27, p200, p261|Santonian|Santonian|Otway Basin. Approximately equivalent to chemostratigraphic package S5-P5, defined by high Fe, P, Th/K and Sm/U values. Attributed to berthierine or glauconite, and phosphate cements. Lithologies based on geochemistry using the ChemLith classification includes argillaceous sandstone, and using the Herron classification (1988) includes Fe-sand and quartz arenite. See also vi, p11 Tb.3.9, p67-68, p133-134.||Sherbrook Group||Overlies Belfast Mudstone, underlies Skull Creek Mudstone, Paaratte Formation|Shallow marine and nearshore sandstones.|
14374|Nullawarre Greensand|73385|5|Briefly described|p5|Santonian|Santonian|Otway Basin.||Sherbrook Group||Overlies Belfast Mudstone, underlies Skull Creek Mudstone, Paaratte Formation.|Shallow marine and nearshore sandstones.|
14374|Nullawarre Greensand|73386|4|Described|p4, p6, p10-11, Attachment A1|Santonian|Santonian|Otway Basin. Originally described as part of the Paaratte Formation. Type section is defined between 1344 m and 1514 m in Nullawarre-3. Shallow marine depositional environment, represents progradation of marine upper deltaic, nearshore, beach-barrier facies. Top of unit is a regional maximum flooding/transgressive surface. Occurs with the Tricolporites apoxyexinus Spore-Pollen Zone. Predominantly restricted to Port Campbell and Tyrendarra embayments.||Sherbrook Group||Overlies Belfast Mudstone, conformably underlies Skull Creek Mudstone, underlies Paaratte Formation|Distinctive grey-green, glauconitic, fine- to coarse-grained sandstone.|
14374|Nullawarre Greensand|73594|5|Briefly described|p4-5, p31|Santonian|Santonian|Otway Basin. Shallow marine.||Sherbrook Group||Overlies Flaxman Formation, Belfast Mudstone, underlies Skull Creek Mudstone, Paaratte Formation|Glauconitic sandstones.|
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.|
31490|Nungatta Suite|22815|5|Briefly described|p82|||Consists of one pluton: Nungatta Granodiorite.||||||
31490|Nungatta Suite|22878|6|Mentioned|p82|||||||||
31490|Nungatta Suite|24551|6|Mentioned|p235|||||||||
31490|Nungatta Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Candelo Supersuite.  Includes the Nungatta Granite.||||||09-FEB-05
31490|Nungatta Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||
77103|Nunnett Plains Volcanic Group|68116|5|Briefly described|Appendix, Maps 35-36.|Rupelian|Lutetian||||||Basalt flows and minor dykes: quartz tholeiitic basalt, olivine tholeiitic basalt, nepheline basanite, hawaiite.|
27525|Nunniong Granodiorite|22968|4|Described|P21, Fig49, P175|Silurian|Early Silurian|Intruded by Mount Nugong Tonalite, Moscow Villa Granodiorite, Cocks Break Granodiorite, Emu Vale Tonalite and Bentleys Plain Granodiorite, Age of unit is 430+/-13, 417+/-2 and 424 Ma, parent is Bullenbalong Supersuite.||||||25-SEP-08
27525|Nunniong Granodiorite|23021|5|Briefly described|Map legend|Wenlock|Wenlock|Parent is Bullenbalong Suite||||||
27525|Nunniong Granodiorite|23028|5|Briefly described|Map legend|Wenlock|Wenlock|Parent is Bullenbalong Suite||||||
27525|Nunniong Granodiorite|23030|5|Briefly described|Map legend|Silurian|Silurian|Parent is the Bullenbalong Supersuite. Age: 417+/-2 Ma (K/Ar). Biotite-muscovite-cordierite granodiorite, and contaminated granite: S-type. G125a: nonmagnetic; low to moderate K, Th, U. G125b: nonmagnetic; moderate to high K, low to moderate Th, U.||||||15-SEP-04
27525|Nunniong Granodiorite|23309|5|Briefly described|p296, 303-308, 338.|Early Devonian|Late Silurian|G125. S-Type. Supersedes Nunniong Granite. Age: 417+/-2Ma, 430+/-13 Ma, 424 Ma.||||||
27525|Nunniong Granodiorite|23615|3|Fully described|p156, p32|Silurian|Silurian|Of Bullenbalong Suite.  Formerly sudivided into Nunniong Granite and Nunnett Granite (White and Chappell, 1988).  Age: 430+/-13Ma (Evernden and Richards, 1962); 417+/-2Ma (Henley and Webb, 1990).  See also p206 App. 1.||||||
27525|Nunniong Granodiorite|23938|5|Briefly described|p38-39 Tb. 2|Middle Silurian|Middle Silurian|See also p68 and p70 Tb. 6.||||||25-SEP-08
27525|Nunniong Granodiorite|38145|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
27525|Nunniong Granodiorite|38367|6|Mentioned|Fig.9|||||||||
27525|Nunniong Granodiorite|39447|4|Described|p17|||||||||
27525|Nunniong Granodiorite|41850|6|Mentioned|p431|||||||||
27525|Nunniong Granodiorite|42827|6|Mentioned|p431|||||||||
27525|Nunniong Granodiorite|43206|5|Briefly described|map legend||Wenlock|Of Bullenbalong Suite. Biotite-cordierite granodiorite: grey; fine to medium grained, generally massive but foliated at the northern margin; minor red microgranite on Pink Rocks Road; minor leucogranite and adamellite.||||||23-JUN-14
27525|Nunniong Granodiorite|44185|5|Briefly described|Map legend.|Silurian|Silurian|S-type.||||||
27525|Nunniong Granodiorite|61187|5|Briefly described|p126.|||Contains very low copper and molybdenum content; supergene enrichment does not produce an economic prospect. See also references to Nunniong Granite (p5 Fig.3, pp113-114, p122).||||||
27525|Nunniong Granodiorite|66181|6|Mentioned|p301|||Nunniong Plateau||||||
27525|Nunniong Granodiorite|68116|5|Briefly described|Appendix, Maps 35-36.|Devonian|Silurian||||||Biotite-cordierite granodiorite: grey; fine to medium-grained; massive to foliated; abundant gneissic enclaves in north, west and southwest.|
14407|Nuntin Clay Member|24468|5|Briefly described|p419|Early Pleistocene|Late Pliocene|Geological Province: Gippsland Basin. Of the Boisdale Formation||||||
14407|Nuntin Clay Member|24551|5|Briefly described|p327 Fig. 10.33|Pliocene|Pliocene|||||||
14407|Nuntin Clay Member|35273|4|Described|p262|||||||||
14407|Nuntin Clay Member|42827|5|Briefly described|p336|||of Boisdale Formation||||||
14407|Nuntin Clay Member|60538|5|Briefly described|p488 Fig. 27|||Geological province: Gippland Basin or Latrobe Valley.||||||
14407|Nuntin Clay Member|65718|6|Mentioned|p10 Fig 3.2|Pleistocene|Pliocene|||||||
14431|Nyerimalang Formation|33689|6|Mentioned|Table 3|||||||||
14431|Nyerimalang Formation|35720|6|Mentioned|p132|||See also Fig.2, stratigraphic column.||||||
14431|Nyerimalang Formation|41511|4|Described|p15|||||||||
34972|O'Dell Tonalite|22968|5|Briefly described|P186, P189||Early Devonian|New name, parent is Swifts Creek Igneous Complex||||||
34972|O'Dell Tonalite|23020|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Swifts Creek Igneous Complex||||||
34972|O'Dell Tonalite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Swifts Creek Igneous Complex. G526a: biotite tonalite: I-type; highly magnetic (300 nT); low to moderate K, Th, U. G526b: hornblende tonalite: I-type; weakly to moderately magnetic (100 nT); low K, Th, U.||||||15-SEP-04
34972|O'Dell Tonalite|68116|5|Briefly described|Appendix, Map 35.|Devonian|Silurian||||||Biotite tonalite: grey; medium to coarse-grained; mostly massive and equigranular; with core of dark green-grey, fine-grained horblende tonalite.|
26816|O'Mearas Granite|23309|6|Mentioned|p440 App1|||G30 I-Type.||||||
26816|O'Mearas Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
14456|O'Sullivan Sandstone Member|35283|6|Mentioned|p55|||||||||
14475|Oaks Grit|33732|5|Briefly described|p105|||||||||
14475|Oaks Grit|70933|14|Not recorded|Table 1|||Generalised east west section Silurian and Devonian,Victoria refers to Talent 1965.||||||
37768|Ocean View Granite|23309|5|Briefly described|p440 Appendix 1|||G508, S-type. Supersedes Jack Rich Granite. Of the Ocean View Suite.||||||
37768|Ocean View Granite|60541|4|Described|p75|||Of Ocean View Suite. See also Ocean View Granodiorite. Small, elongate, composite pluton - of strongly foliated, medium-grained granite with numerous schistose inclusions. Type locality given. Fresh rock is light grey, medium-grained with mod-well-dev....||||||
37768|Ocean View Granite|68116|5|Briefly described|Appendix, Map 45.|Wenlock|Llandovery|Informally subdivided into a mylonitic granodiorite phase.|||||Biotite-muscovite granodiorite: with cordierite; medium-grained; foliated with numerous schistose enclaves; S-type. Mylonitic granodiorite: muscovite-biotite granodiorite: coarse-grained; mylonitic; with sparse enclaves; S-type.|
37587|Ocean View Suite|23309|5|Briefly described|p338||Early Silurian|Includes Bee Tree Granodiorite, Towzer Creek Granite, Pike Hill Granodiorite, Mount Jack Granite, Kent Road Granite and Ocean View Granite.||||||
37587|Ocean View Suite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|Includes: Ocean View Granodiorite, Kent Road Granite, Mount Jack Granodiorite, Pike Hill Granodiorite, Bee Tree Granodiorite, Purgagoolah Granite||||||
37587|Ocean View Suite|43315|5|Briefly described|Map Legend|Wenlock|Wenlock|Includes: Ocean View Granodiorite, Kent Road Granite, Mount Jack Granodiorite, Pike Hill Granodiorite, Bee Tree Granodiorite, Purgagoolah Granite||||||
37587|Ocean View Suite|60541|4|Described|p75|||Occurs in Kuark Met. Belt. as isolated pods of granite. New grouping proposed in this study - comprising Ocean View, Mt Jack, Towzer Creek, Pike Hill, Kent Road, Bee Tree Granodiorites, and possibly Tommy Roundhead and Kanuka Granodiorites (on BENDOC).||||||21-JUN-05
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||||||
34885|Old Mill Ignimbrite Member|22968|4|Described|P122, P127|Late Silurian|Late Silurian|New name, lies at base of Shanahan Sandstone, type section location given on P127, maximum thickness is 250m||||||
34885|Old Mill Ignimbrite Member|23021|5|Briefly described|Map legend|Ludlow|Ludlow|Parent is Shanahan Sandstone||||||
34885|Old Mill Ignimbrite Member|23030|5|Briefly described|Map legend|Late Silurian|Late Silurian|Parent is the Mount Tambo Group||||||
34885|Old Mill Ignimbrite Member|23309|5|Briefly described|p103. Tb 2.37|||||||||
34885|Old Mill Ignimbrite Member|24551|5|Briefly described|p140|||Basal member of the Shanahan Sandstone.||||||03-AUG-05
32566|Old Sheep Station Granodiorite|22968|5|Briefly described|P16, P183|Early Devonian|Late Silurian|New name, parent is Rileys Creek Suite||||||
32566|Old Sheep Station Granodiorite|23020|5|Briefly described|Map legend|Lochkovian|Pridoli|||||||
32566|Old Sheep Station Granodiorite|23030|5|Briefly described|Map legend|Early Devonian|Late Silurian|Parent is the Rileys Creek Suite||||||
32566|Old Sheep Station Granodiorite|23309|5|Briefly described|p284.|||(G136) I-Type||||||
32566|Old Sheep Station Granodiorite|24004|6|Mentioned|p282|||||||||
32566|Old Sheep Station Granodiorite|61161|6|Mentioned|p150|||Contact metamorphism - cordierite isograd follows shape of this unit.||||||
32566|Old Sheep Station Granodiorite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Biotite granodiorite: grey; medium to coarse-grained; foliated, with rare hornfels and mafic igneous enclaves.|
39878|Older Volcanic Group|24383|5|Briefly described|p59, 60|Eocene|Eocene|Age: 42 - 57Ma. Geological Province: Lachlan Fold Belt||||||
39878|Older Volcanic Group|61160|3|Fully described|p92-93, p11, p29 Tb. 5.2.|Late Eocene|Cenozoic|Previously these Cainozoic basalts referred to as Bogong Volcanics (Beavis 1962). See also Older Volcanics - names used interchangeably. Consists of tholeiitic to alkalic basaltic lavas, dykes and plugs older than 5Ma (Price etal 1988). Age: 36.3+/-0.6Ma||||||19-NOV-08
39878|Older Volcanic Group|61161|5|Briefly described|p133-138, p5, p8, p76-77 Fig 6.1, p94|Early Oligocene|Eocene|Alluvial deposits (gravel, sand, peat), and lavas [Po1], dykes and  plugs [Po2]. Non- to highly magnetic tholeiitic to alkalic basalts. Flowed onto high-relief landscape. Thickness >200m in places. Age: K-Ar 36.3+-0.6Ma. GSV map code: Po.||||||
39878|Older Volcanic Group|61163|4|Described|p99, p125, p36 Tb. 6.2|Paleogene|Paleogene|Includes: basalts plugs - vesicular and porphyritic with olivine phenocrysts; and float from a dyke of phonolite, occuring extensively within the Cobbannah Group; and a dyke of olivine basalt intruding the Tolmie Igneous Complex.||||||07-NOV-08
39878|Older Volcanic Group|61164|5|Briefly described|map legend|Paleogene|Paleogene|Unnamed subaerial lava flows: alkali olivine basalt, nepheline basanite, picrobasalt, nephelinite; includes interflow sediments; GSV map code: -Po1. Unnamed plugs and dykes: alkali olivine basalt, nepheline basanite and phonolite. GSV map code: -Po2.||||||07-NOV-08
39878|Older Volcanic Group|61165|5|Briefly described|map legend|Paleogene|Paleogene|Unnamed subaerial lava flows: alkali olivine basalt, nepheline basanite, picrobasalt, nephelinite; includes interflow sediments; GSV map code: -Po1. Unnamed plugs and dykes: alkali olivine basalt, nepheline basanite and phonolite. GSV map code: -Po2.||||||07-NOV-08
39878|Older Volcanic Group|61166|5|Briefly described|map legend|Paleogene|Paleogene|Unnamed subaerial lava flows: alkali olivine basalt, nepheline basanite, picrobasalt, nephelinite; includes interflow sediments; GSV map code: -Po1. Unnamed plugs and dykes: alkali olivine basalt, nepheline basanite and phonolite. GSV map code: -Po2.||||||07-NOV-08
39878|Older Volcanic Group|61167|5|Briefly described|map legend|Paleogene|Paleogene|Unnamed subaerial lava flows: alkali olivine basalt, nepheline basanite, picrobasalt, nephelinite; includes interflow sediments; GSV map code: -Po1. Unnamed plugs and dykes: alkali olivine basalt, nepheline basanite and phonolite. GSV map code: -Po2.||||||07-FEB-11
39878|Older Volcanic Group|61168|5|Briefly described|map legend|Paleogene|Paleogene|Lava flows: nepheline basanite, alkali olivine basalt; interflow sediments, mudstone. Plugs and dykes: also include phonolite. GSV map code: -Po1 and -Po2 respectively. Both subdivisions highly magnetic and are each normally and reversely magnetised.||||||07-NOV-08
39878|Older Volcanic Group|61169|5|Briefly described|map legend|Paleogene|Paleogene|Unnamed subaerial lava flows: basalt, basanite, hawaiite, alkali basalt, olivine basalt; includes interflow sediments; GSV map code: -Po1. Unnamed plugs and dykes: basalt and phonolite; GSV map code: -Po2.||||||07-NOV-08
39878|Older Volcanic Group|61170|5|Briefly described|map legend|Paleogene|Paleogene|Unnamed subaerial lava flows: basalt, basanite, hawaiite, alkali basalt, olivine basalt; includes interflow sediments; GSV map code: -Po1. Unnamed plugs and dykes: basalt and phonolite; GSV map code: -Po2.||||||07-FEB-11
39878|Older Volcanic Group|61171|5|Briefly described|map legend|Paleogene|Paleogene|Unnamed subaerial lava flows: basalt, basanite, hawaiite, alkali basalt, olivine basalt; includes interflow sediments; GSV map code: -Po1. Unnamed plugs and dykes: basalt and phonolite; GSV map code: -Po2.||||||07-NOV-08
39878|Older Volcanic Group|61172|5|Briefly described|map legend|Paleogene|Paleogene|Unnamed subaerial lava flows: basalt, basanite, hawaiite, alkali basalt, olivine basalt; includes interflow sediments; GSV map code: -Po1. Unnamed plugs and dykes: basalt and phonolite; GSV map code: -Po2.||||||07-NOV-08
39878|Older Volcanic Group|61173|5|Briefly described|map legend|Paleogene|Paleogene|Unnamed subaerial lava flows: basalt, basanite, hawaiite, alkali and olivine basalts, possibly trachyte; GSV map code: -Po1. Unnamed plugs and dykes: basalt, phonolite; GSV map code: -Po2. Both subdivided into 3 units of differing geophysical responses.||||||07-NOV-08
39878|Older Volcanic Group|61174|5|Briefly described|map legend|Paleogene|Paleogene|Basalt: alkali olivine basalt; black, fine grained, vesicular, with small olivine phenocrysts. GSV map code: -Po.||||||07-FEB-11
39878|Older Volcanic Group|61175|5|Briefly described|map legend|Paleogene|Paleogene|Basalt: alkali olivine basalt; black, fine grained, vesicular, with small olivine phenocrysts. GSV map code: -Po.||||||07-NOV-08
39878|Older Volcanic Group|61176|5|Briefly described|map legend|Paleogene|Paleogene|Basalt: alkali olivine basalt; black, fine grained, vesicular, with small olivine phenocrysts. GSV map code: -Po.||||||07-NOV-08
39878|Older Volcanic Group|61177|5|Briefly described|map legend|Paleogene|Paleogene|Basalt: alkali olivine basalt; black, fine grained, vesicular, with small olivine phenocrysts. GSV map code: -Po.||||||07-NOV-08
39878|Older Volcanic Group|61178|5|Briefly described|map legend|Paleogene|Paleogene|Unnamed plugs: normally (50nT, highly magnetic, probably alkali-olivine basalt) and reversely (-50nT, highly magnetic k = 900 to 1400 x10^-6 cgs, alkali-olivine basalt) magnetised. GSV map code: -Po.||||||07-NOV-08
39878|Older Volcanic Group|64535|5|Briefly described|Map legend|Paleogene|Paleogene|Contains unnamed lava flows, plugs and dykes including alkali olivine basal, olivine tholeiite, hawaiite, picrobasalt; minor peridotite enclaves. ||||||
39878|Older Volcanic Group|64539|5|Briefly described|Map legend|Paleogene|Paleogene|Contains unnamed lava flows, plugs and dykes including alkali olivine basal, olivine tholeiite, hawaiite, picrobasalt; minor peridotite enclaves. ||||||
39878|Older Volcanic Group|64540|5|Briefly described|Map legend|Paleogene|Paleogene|Contains unnamed lava flows, plugs and dykes including alkali olivine basal, olivine tholeiite, hawaiite, picrobasalt; minor peridotite enclaves. ||||||
39878|Older Volcanic Group|64605|5|Briefly described|Map legend|Paleogene|Paleogene|Includes unnamed lava flows, unnamed plugs and dykes, and unnamed alluvium.||||||17-NOV-08
39878|Older Volcanic Group|64616|3|Fully described|p144-147, p292, p297-298, p434-435|Oligocene|Oligocene|Encompasses Palaeogene basic volcanic rocks in Victoria. Occurs as basaltic lava flows and as plugs and dykes. Also appears as Older Volcanics Group on p144 and p147, and as Older Volcanics on p434. Whole-rock K-Ar ages from 21.6 +/- 0.4 Ma to 27.9 +/- 0.7 Ma. Is overlain disconformably by Haunted Hills Gravel. Thickness variable; typically 50-100m. Alkali olivine basalt, olivine tholeiite and hawaiite; interflow laminated mudstone. Geophysical characteristics given.||||||
39878|Older Volcanic Group|66002|6|Mentioned|p18|||Currently used name for Older Volcanics||||||
39878|Older Volcanic Group|68115|5|Briefly described|pp8-10.|Paleogene|Paleogene|Wellman (1974) divided these rocks into several volcanic provinces; Price et al. (2003) modified this scheme, forming an Eastern province divided into subprovinces. Earlier maps showed this unit as including Gallows Hill Phonolite, but it has been dated as Jurassic by McDougall and Wellman (1976). |||||Mafic volcanic rocks.|
39878|Older Volcanic Group|68189|6|Mentioned|p18 Fig.8|||||||||
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.|||||
68520|Opah Formation|13323|5|Briefly described|p393 Fig. 2|Middle Eocene|Middle Eocene|Marine clastics. Geological Province: Gippsland Basin.||||||
68520|Opah Formation|24551|6|Mentioned|p478 Fig. 15.8||Eocene|||||||
68520|Opah Formation|61552|6|Mentioned|p583 Fig.2. |Eocene|Eocene|||||||
68520|Opah Formation|65717|5|Briefly described|p9 Fig.2.2|Eocene|Eocene|Gippsland Basin.||Latrobe Group.||Overlies Kingfish Formation. Is overlain unconformably by Gurnard Formation.|Marine clastics.|05-SEP-17
68520|Opah Formation|70076|5|Briefly described|Regional: Fig.3|Lutetian|Lutetian|||Cobia Subgroup.||Overlies Flounder Formation. Is overlain by Turrum Formation.||
37770|Orbost Tonalite|23309|6|Mentioned|p441, Appendix 1|||G44, I-Type. Supersedes Orbost Granite.||||||
37770|Orbost Tonalite|23938|6|Mentioned|p101|Early Devonian|Early Devonian|||||||
37770|Orbost Tonalite|24551|6|Mentioned|p235|||||||||
37770|Orbost Tonalite|60541|5|Briefly described|p17 Tb. 1|Silurian|Silurian|Previously known as Youngs Creek Granite. Rock has been quarried and used for public buildings base courses. Greenish-grey, medium-grained and quite mafic containing numerous xenoliths up to 0.5mm in size.||||||
37770|Orbost Tonalite|60542|4|Described|p91-92, p20 Fig. 4|Late Silurian|Late Silurian|Medium-grained, grey-green when fresh and green when weathered; quite mafic in composition with enclaves of both mafic composition and rarer sedimentary material; complexly twinned and zoned plagioclases. ||||||
37770|Orbost Tonalite|68116|5|Briefly described|Appendix.|Devonian|Silurian||||||Hornblende-biotite tonalite: fine to medium-grained; medium to dark grey; with small enclaves; altered; I-type.|
34816|Oriental Claims Gravel|22968|5|Briefly described|P16, P158||Late Pliocene|New name, nonmagnetic||||||
34816|Oriental Claims Gravel|23021|5|Briefly described|Map legend|Pliocene|Pliocene|||||||
34816|Oriental Claims Gravel|23029|5|Briefly described|Map legend|Pliocene|Pliocene|||||||
34816|Oriental Claims Gravel|23030|5|Briefly described|Map legend|Neogene|Neogene|||||||
34816|Oriental Claims Gravel|68116|5|Briefly described|Appendix, Map 35.|Neogene|Neogene||||||Conglomerate, sandstone: colour variable, mainly brown; predominantly vein quartz pebbles but with lithic cobbles and boulders {granite, high-grade metamorphic rocks} at base; moderately to well bedded; local channel erosion.|
14685|Otway Group|12796|6|Mentioned|p455|||Geological Province: Otway Basin.||||||
14685|Otway Group|13323|5|Briefly described|p392|||Raised to rank of supergroup following introduction of Crayfish Group (Kopsen abd Scholefield 1990) but this caused discontinuity of nomenclature and was considered to have 'limited usefulness' by many (Morton et al 1994). Geol.Prov: Otway Basin.||||||26-JUN-06
14685|Otway Group|13350|5|Briefly described|p95, p106||Early Cretaceous|Geological Province: Otway Basin, Bass and Boobyalla Sub-basins and probably the Sorrell Basin west of Tasmania.||||||29-JAN-07
14685|Otway Group|22495|6|Mentioned|P220|||||||||
14685|Otway Group|22706|6|Mentioned|Fig1,p78|||||||||
14685|Otway Group|22875|4|Described|p25|Early Cretaceous|Late Jurassic|Age: 157-95 Ma.||||||29-JAN-07
14685|Otway Group|22938|6|Mentioned|p233||Early Cretaceous|||||||
14685|Otway Group|22944|5|Briefly described|Fig3|Albian|Tithonian|||||||
14685|Otway Group|23010|6|Mentioned|p333-341||Early Cretaceous|||||||
14685|Otway Group|23041|6|Mentioned|p116||Cretaceous|||||||
14685|Otway Group|23230|5|Briefly described|p39, Table4-1p40|Early Cretaceous||||||||
14685|Otway Group|23239|5|Briefly described|Table1p109, 116||Early Cretaceous|||||||
14685|Otway Group|23241|5|Briefly described|p133, 135, Fig11-3.6p140|Late Cretaceous|Early Cretaceous|||||||
14685|Otway Group|23243|5|Briefly described|Fig11-5.1p170||Late Cretaceous|||||||
14685|Otway Group|23249|6|Mentioned|Fig.1|||of Otway Basin.||||||
14685|Otway Group|23307|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||||||
14685|Otway Group|23357|5|Briefly described|52|Early Cretaceous|Early Cretaceous|||||||
14685|Otway Group|23372|4|Described|p251 Fig3,p249|Albian|Barremian|Of Bass Basin.||||||01-JUL-08
14685|Otway Group|23427|5|Briefly described|Table 11.2 p418.|||||||||
14685|Otway Group|23537|5|Briefly described|p 440|||||||||
14685|Otway Group|23778|5|Briefly described|p660|Early Cretaceous|Early Cretaceous|Overlain by Eastern View Group. In the Otway Basin.||||||29-JAN-07
14685|Otway Group|23792|6|Mentioned|Fig.B13||Early Cretaceous|Forms basement for Sandy Cape Sub-basin. See also Otway Supergroup.||||||
14685|Otway Group|23818|4|Described|p150, 161|Late Jurassic|Late Jurassic|Geological Province: Otway Basin. Age: 153+/-5 Ma. Max. thickness: >10 000 ft. Overlain by Sherbrook Group.||||||29-JAN-07
14685|Otway Group|23824|6|Mentioned|p102|||Geological Province: Otway Basin.||||||
14685|Otway Group|23830|5|Briefly described|Fig. 6|Early Cretaceous|Late Jurassic|Geological Province: Gambier Embayment, Otway Basin.||||||24-JAN-06
14685|Otway Group|23909|5|Briefly described|p291|Early Cretaceous|Early Cretaceous|Geological Province: Otway Basin.||||||
14685|Otway Group|23911|5|Briefly described|p95 Fig. 9B|Albian|Late Jurassic|Geological Province: Otway Basin.||||||
14685|Otway Group|24002|5|Briefly described|p236|Cretaceous|Cretaceous|||||||
14685|Otway Group|24038|5|Briefly described|p438 Fig.1|Early Cretaceous|Early Cretaceous|||||||
14685|Otway Group|24055|4|Described|p71|Early Cretaceous|Jurassic|Geological Basin: Otway Basin.||||||
14685|Otway Group|24056|4|Described|p84|Early Cretaceous|Jurassic|Max. thickness: 3500m.  Geological Basin: Otway Basin.||||||
14685|Otway Group|24085|6|Mentioned|p42 Tb.2|Early Cretaceous|Early Cretaceous|||||||
14685|Otway Group|24113|5|Briefly described|p284|||See also p282 Tb 2.||||||
14685|Otway Group|24160|6|Mentioned|p19|Early Cretaceous|Early Cretaceous|Gellibrand, northern Otway Ranges. Hosts bentonite deposits.|||||Includes arkose, mudstone and shale.|
14685|Otway Group|24200|6|Mentioned|p416|||||||||
14685|Otway Group|24238|5|Briefly described|p8|Early Cretaceous|Jurassic|Geological Province: Otway Basin.||||||
14685|Otway Group|24323|6|Mentioned|p144|||Geological Province: Otway Basin||||||
14685|Otway Group|24453|5|Briefly described|p808, p809 Fig.2|Albian|Late Jurrasic|Geological Province: Otway Basin.||||||07-FEB-11
14685|Otway Group|24455|5|Briefly described|p327|Early Cretaceous|Early Cretaceous|Bears dinosaur remains.  Transgressively overlapped by Pebble Point Formation.||||||
14685|Otway Group|24551|4|Described|p240 Fig. 9.2, p247|Cretaceous|Late Jurassic|Duddy (1983) proposed to replace this name with Otway Formation due to objections to the term 'group'; also, Otway Supergroup was proposed (Kopsen and Scholefield 1990) but rejected due to its limited use.||||||29-JAN-07
14685|Otway Group|24561|5|Briefly described|p27|||Geological Province: Otway and Bass Basins. Includes volcanogenic sediments.||||||04-FEB-08
14685|Otway Group|24562|5|Briefly described|p20, 91|Early Cretaceous|Early Cretaceous|Overlies: Pretty Hill Formation.  Geological Province: Otway Basin.||||||
14685|Otway Group|29591|6|Mentioned|p92|||||||||
14685|Otway Group|29697|6|Mentioned|Fig.11|||||||||
14685|Otway Group|29823|6|Mentioned|p14|||||||||
14685|Otway Group|29856|6|Mentioned|p36|||||||||
14685|Otway Group|29877|6|Mentioned|p33|||||||||
14685|Otway Group|30018|5|Briefly described|p15|||||||||
14685|Otway Group|30499|6|Mentioned|p92|||Stratigraphy||||||
14685|Otway Group|30512|6|Mentioned|p51|||||||||
14685|Otway Group|30522|6|Mentioned|Map legend|Early Cretaceous|Jurassic|Jurassic-Lower Cretaceous||||||
14685|Otway Group|30539|6|Mentioned|p7|||Late Albian angiosperms||||||
14685|Otway Group|30576|6|Mentioned|Table 1|||||||||
14685|Otway Group|30578|6|Mentioned|p4|||||||||
14685|Otway Group|30580|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14685|Otway Group|30675|5|Briefly described|p253|||Lithology and radioactivity||||||29-JAN-07
14685|Otway Group|30754|5|Briefly described|p4|||Stratigraphic divisions. See also P12,24||||||
14685|Otway Group|30905|4|Described|p148|||||||||
14685|Otway Group|30928|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14685|Otway Group|30929|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14685|Otway Group|30932|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14685|Otway Group|30990|6|Mentioned|p125|||Refers Edwards & Barkes (1943)||||||
14685|Otway Group|31001|6|Mentioned|p7|||||||||
14685|Otway Group|31010|6|Mentioned|p51|||||||||
14685|Otway Group|31036|6|Mentioned|Table 9-1|||See also P215||||||
14685|Otway Group|31160|6|Mentioned|p77|||See also P78||||||
14685|Otway Group|31202|5|Briefly described|p218|||Unconformity with Sherbrook Gp. and rift formation..||||||29-JAN-07
14685|Otway Group|31212|6|Mentioned|p318|||Gravity data. L. Cretaceous. See also P320||||||
14685|Otway Group|31242|6|Mentioned|p12|||Refers hydrogeology||||||
14685|Otway Group|31372|6|Mentioned|p2|||See also P9||||||
14685|Otway Group|31424|4|Described|p20|||See also p7. Described from core.||||||29-JAN-07
14685|Otway Group|31510|6|Mentioned|p12|||See also Table 1.||||||
14685|Otway Group|31534|6|Mentioned|p363|||See also Table 19-3. L.Cretaceous||||||
14685|Otway Group|31616|6|Mentioned|p202|||L.Cret.||||||
14685|Otway Group|31624|6|Mentioned|p93|||See also P96. L.Cret.||||||
14685|Otway Group|31625|6|Mentioned|Fig. 5.2|||L.Cret||||||
14685|Otway Group|31629|6|Mentioned|Fig. 5.1|||L.Cret.||||||
14685|Otway Group|31714|6|Mentioned|Fig. 8|||||||||
14685|Otway Group|31920|4|Described|p49|||L.Cret. See also Fig.3-2||||||
14685|Otway Group|31923|6|Mentioned|p16|||||||||
14685|Otway Group|32162|4|Described|p58|||Petroleum apsect||||||
14685|Otway Group|32167|6|Mentioned|p.340||Early Cretaceous|||||||
14685|Otway Group|32168|6|Mentioned|p32|||||||||
14685|Otway Group|32232|6|Mentioned|p19|||||||||
14685|Otway Group|32344|6|Mentioned|Fig.2|||||||||
14685|Otway Group|32712|6|Mentioned|Table 1|||||||||
14685|Otway Group|32841|6|Mentioned|p6|||||||||
14685|Otway Group|32852|6|Mentioned|p9|||||||||
14685|Otway Group|32894|4|Described|p286|||U.Jur.-L.Cret. See also p293.||||||29-JAN-07
14685|Otway Group|32897|6|Mentioned|p177|||L.Cret.||||||
14685|Otway Group|32898|6|Mentioned|Table 2-1|||||||||
14685|Otway Group|32899|4|Described|p164|||See also pp165-176.||||||29-JAN-07
14685|Otway Group|33135|5|Briefly described|p17|||||||||
14685|Otway Group|33155|5|Briefly described|p114|||||||||
14685|Otway Group|33165|6|Mentioned|Chart|||Correlation chart only||||||
14685|Otway Group|33228|6|Mentioned|p2|||||||||
14685|Otway Group|33229|4|Described|p242|||Jur.- L.Cret.||||||
14685|Otway Group|33230|6|Mentioned|Encl.12.1|||L.Cret.||||||
14685|Otway Group|33236|5|Briefly described|p19|||L.Cret. See also p22.||||||29-JAN-07
14685|Otway Group|33240|6|Mentioned|p2|||||||||
14685|Otway Group|33319|6|Mentioned|p178|||Strat.||||||
14685|Otway Group|33354|6|Mentioned|p187|||L.Cret.||||||
14685|Otway Group|33412|6|Mentioned|p218|||L.Cret.||||||
14685|Otway Group|33602|6|Mentioned|Table 1|||||||||
14685|Otway Group|33627|6|Mentioned|p595|||||||||
14685|Otway Group|33663|6|Mentioned|p3|||||||||
14685|Otway Group|33936|6|Mentioned|Fig.6|||U.Jur. - L.Cret.||||||
14685|Otway Group|33940|4|Described|p387|||L.Cret. See p400.||||||29-JAN-07
14685|Otway Group|33943|6|Mentioned|p378|||L.Cret.||||||
14685|Otway Group|34001|6|Mentioned|p14|||In Hindaugh No.1 Well||||||
14685|Otway Group|34063|6|Mentioned|p3|||L.Cret. Table||||||
14685|Otway Group|34148|6|Mentioned|p10|||Lower Cretaceous. See also PP272,285,286.||||||
14685|Otway Group|34191|6|Mentioned|Map legend|Albian|Neocomian|Neocomian - Albian||||||
14685|Otway Group|34308|6|Mentioned|Fig.86|||||||||
14685|Otway Group|34343|5|Briefly described|p96|||||||||
14685|Otway Group|34611|6|Mentioned|p161|||Mesozoic. Non marine.||||||
14685|Otway Group|34928|5|Briefly described|p55|||||||||
14685|Otway Group|34966|6|Mentioned|p364|||||||||
14685|Otway Group|34967|6|Mentioned|p347|||||||||
14685|Otway Group|34987|5|Briefly described|p170|||||||||
14685|Otway Group|34988|6|Mentioned|Table 9.4|||||||||
14685|Otway Group|34993|6|Mentioned|p302|||||||||
14685|Otway Group|35013|4|Described|p390|||||||||
14685|Otway Group|35066|6|Mentioned|p203|||||||||
14685|Otway Group|35112|6|Mentioned|Table 1|||||||||
14685|Otway Group|35151|6|Mentioned|p150|||||||||
14685|Otway Group|35274|6|Mentioned|p421|||||||||
14685|Otway Group|35276|6|Mentioned|p231|||||||||
14685|Otway Group|35290|6|Mentioned|p23|||||||||
14685|Otway Group|35712|6|Mentioned|Table 6|||||||||
14685|Otway Group|35722|6|Mentioned|p3|||Stratigraphy.||||||
14685|Otway Group|36366|6|Mentioned|p5|||||||||
14685|Otway Group|36499|3|Fully described|p17|||||||||
14685|Otway Group|36553|6|Mentioned|p364|||||||||
14685|Otway Group|36824|6|Mentioned|p65|||||||||
14685|Otway Group|36913|6|Mentioned|p78|||See also Fig.4.||||||
14685|Otway Group|37065|5|Briefly described|p42|||||||||
14685|Otway Group|37129|5|Briefly described|p359|||||||||
14685|Otway Group|37131|6|Mentioned|p364|||||||||
14685|Otway Group|37548|6|Mentioned|p131|||||||||
14685|Otway Group|38008|6|Mentioned|p1|||||||||
14685|Otway Group|38068|4|Described|p72|||||||||
14685|Otway Group|38221|6|Mentioned|Fig.4|||Otway Basin||||||
14685|Otway Group|38625|6|Mentioned|p271|||||||||
14685|Otway Group|38928|6|Mentioned|p12|||||||||
14685|Otway Group|39022|6|Mentioned|p397|||||||||
14685|Otway Group|39077|6|Mentioned|Table 2|||||||||
14685|Otway Group|39211|6|Mentioned|Fig.45|||||||||
14685|Otway Group|39666|6|Mentioned|p111|||||||||
14685|Otway Group|40003|5|Briefly described|p43|||See also Fig.10||||||
14685|Otway Group|40560|6|Mentioned|p4|||||||||
14685|Otway Group|40641|4|Described|p295|||||||||
14685|Otway Group|40947|6|Mentioned|p3|||||||||
14685|Otway Group|41016|5|Briefly described|p213|||||||||
14685|Otway Group|41057|6|Mentioned|p60|||||||||
14685|Otway Group|41124|4|Described|p255|||||||||
14685|Otway Group|41171|6|Mentioned|p167|||||||||
14685|Otway Group|41185|5|Briefly described|p175|||See also Fig.4||||||
14685|Otway Group|41201|6|Mentioned|p7|||||||||
14685|Otway Group|41269|5|Briefly described|p244|||||||||
14685|Otway Group|41318|6|Mentioned|p182|||||||||
14685|Otway Group|41426|6|Mentioned|p3|||||||||
14685|Otway Group|41487|6|Mentioned|p624|||||||||
14685|Otway Group|41521|6|Mentioned|p239|||||||||
14685|Otway Group|41552|6|Mentioned|p459|||||||||
14685|Otway Group|41642|4|Described|p224|||See also p 217?||||||
14685|Otway Group|41701|6|Mentioned|Map legend|Cretaceous||||||||
14685|Otway Group|41704|5|Briefly described|p99|||See also p100.||||||29-JAN-07
14685|Otway Group|41706|6|Mentioned|p145|||||||||
14685|Otway Group|41714|6|Mentioned|p301|||||||||
14685|Otway Group|41715|6|Mentioned|p312|||||||||
14685|Otway Group|41726|5|Briefly described|p420|||||||||
14685|Otway Group|41769|4|Described|p9|||||||||
14685|Otway Group|41797|5|Briefly described|p223|||||||||
14685|Otway Group|41818|6|Mentioned|p40|||||||||
14685|Otway Group|41848|6|Mentioned|p377|||Age Lower Cretaceous||||||
14685|Otway Group|41849|6|Mentioned|p413|||||||||
14685|Otway Group|41868|4|Described|p531|||||||||
14685|Otway Group|41936|6|Mentioned|p77|||||||||
14685|Otway Group|42152|6|Mentioned|Fig.2 P4|||||||||
14685|Otway Group|42153|6|Mentioned|p351|||See also Table 1||||||
14685|Otway Group|42184|6|Mentioned|Fig.2 P348|||||||||
14685|Otway Group|42318|5|Briefly described|p5|||||||||
14685|Otway Group|42357|6|Mentioned|p11|||||||||
14685|Otway Group|42361|4|Described|p4|||||||||
14685|Otway Group|42415|5|Briefly described|p177|||Otway Basin||||||
14685|Otway Group|42423|5|Briefly described|p327|||||||||
14685|Otway Group|42452|5|Briefly described|Map legend|Albian|Neocomian|||||||
14685|Otway Group|42453|4|Described|p10|Albian|Neocomian|||||||
14685|Otway Group|42524|5|Briefly described|p27|||||||||
14685|Otway Group|42545|6|Mentioned|p4|||Otway Basin||||||
14685|Otway Group|42555|5|Briefly described|p284|||||||||
14685|Otway Group|42599|5|Briefly described|Fig.3 P614|||||||||
14685|Otway Group|42635|6|Mentioned|p88|||||||||
14685|Otway Group|42827|3|Fully described|p217|||||||||
14685|Otway Group|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
14685|Otway Group|42966|6|Mentioned|p68|||||||||
14685|Otway Group|43171|6|Mentioned|8|Early Cretaceous|Late Jurassic|Age: 105-155Ma||||||
14685|Otway Group|43208|5|Briefly described|map legend|Albian|Oxfordian|||||||
14685|Otway Group|43219|5|Briefly described|Fig.3,p6.|Albian|Oxfordian|||||||
14685|Otway Group|43590|4|Described|p7|Early Cretaceous|Late Jurassic|||||||
14685|Otway Group|43604|6|Mentioned|p144,Fig.1||Cretaceous|||||||
14685|Otway Group|43660|6|Mentioned|p9||Early Cretaceous|||||||
14685|Otway Group|43686|5|Briefly described|p233||Early Cretaceous|||||||
14685|Otway Group|43702|6|Mentioned|Fig.2,p398||Early Cretaceous|||||||
14685|Otway Group|43705|6|Mentioned|p14||Cretaceous|||||||
14685|Otway Group|43733|6|Mentioned|Fig.1.10,p24|||||||||
14685|Otway Group|43783|6|Mentioned|Fig14, p11|||||||||
14685|Otway Group|43784|6|Mentioned|Fig10, p12|||||||||
14685|Otway Group|43814|6|Mentioned|Fig.3,p115|||||||||
14685|Otway Group|43937|5|Briefly described|Map Legend|Aptian|Kimmeridgian|||||||
14685|Otway Group|44135|5|Briefly described|p46, p47|Early Cretaceous|Early Cretaceous|Age: 126-103Ma.Thickness: 1200m.  Geological province: Otway, Bass and Durroon Basins. Rift-fill succession of immature volcaniclastic lithic sandstone, siltstone, rare conglomerate and thin coal seams.||||||07-DEC-09
14685|Otway Group|46909|6|Mentioned|Fig.1|||||||||
14685|Otway Group|46970|6|Mentioned|Fig.17|||||||||
14685|Otway Group|46988|6|Mentioned|p201|||||||||
14685|Otway Group|48581|4|Described|p26-31|||See also p1,2,16,35,40. Fig.6,Pl.2. (J54-12).||||||
14685|Otway Group|48631|14|Not recorded|p7|||non-marine, Otway Basin.||||||
14685|Otway Group|48911|5|Briefly described|p11|||Formations in the group.||||||
14685|Otway Group|48977|5|Briefly described|p26|||See also P1 & Table 3. Lower Cret.||||||
14685|Otway Group|49060|5|Briefly described|Fig.33|||||||||
14685|Otway Group|50043|6|Mentioned|p2, p10, 12|Early Albian|Late Aptian||||Includes Eumeralla Formation.|||27-MAR-12
14685|Otway Group|50154|4|Described|p25, p108, p131|Cretaceous|Cretaceous|Age: ca. 140-100 Ma. Nonconformably overlies the Dergholm Granite.||||||05-JAN-16
14685|Otway Group|50155|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Includes Eumeralla Formation.||||||27-OCT-08
14685|Otway Group|50156|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Includes Eumeralla Formation.||||||27-OCT-08
14685|Otway Group|50157|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Includes Eumeralla Formation||||||
14685|Otway Group|50158|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Includes Eumeralla Formation||||||24-JUN-04
14685|Otway Group|50159|5|Briefly described|Map Legend|||Includes Eumeralla Formation.||||||29-JAN-07
14685|Otway Group|50160|5|Briefly described|Map Legend|||Includes Eumeralla Formation||||||16-JUN-04
14685|Otway Group|50161|5|Briefly described|Map Legend|||Includes Eumeralla Formation||||||
14685|Otway Group|50162|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Includes Eumeralla Formation||||||22-JUN-04
14685|Otway Group|50163|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
14685|Otway Group|50164|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Overlies Nangeela Formation. Overlain by Renmark Group. Fluvial; sandstone, siltstone, minor conglomerate, coal.||||||25-JUN-04
14685|Otway Group|50594|5|Briefly described|p27|Early Cretaceous|Late Jurassic|Geological Province: Otway Basin.||||||
14685|Otway Group|60299|5|Briefly described|p228 Tb.5|Cretaceous|Cretaceous|Age: 110/115 Ma. Palaeopole position given.||||||
14685|Otway Group|60421|5|Briefly described|p408 Fig. 1, 409, 411|Cretaceous|Cretaceous|Sedimentary.||||||
14685|Otway Group|60451|5|Briefly described|p95 Fig. 61|||||||||
14685|Otway Group|60563|5|Briefly described|p45|Cretaceous|Cretaceous|Geological Province: Otway Basin.||||||
14685|Otway Group|61017|5|Briefly described|p5|Albian|Oxfordian|Includes the Crayfish Subgroup. Geological Province: Otway Basin.||||||07-FEB-11
14685|Otway Group|61181|5|Briefly described|p16, p25, p133|Early Cretaceous|Early Cretaceous|Bentonite occurs interbedded within the sediments which comprise arkose, mudstone and shale in the Gellibrand area. Rare ligneous mudstone and thin coal seams are also present. Unconformably overlain by the Jan Juc Formation. ||||||
14685|Otway Group|61182|4|Described|p10, p35|Early Cretaceous|Late Jurassic|Comprises Casterton, Pretty Hill and Eumeralla Formations. Unconformably overlain by Sherbrook Group. Geological Province: Otway Basin. Sequence of basalt, pyroclastics, lithic sandstone, siltstone and shale. Age: 157-97Ma. ||||||
14685|Otway Group|61328|6|Mentioned|p116-117|Early Cretaceous|Early Cretaceous|Age: ~95Ma.||||||
14685|Otway Group|61336|6|Mentioned|p(i)|||Geological Province: Otway Basin.||||||07-FEB-11
14685|Otway Group|61470|5|Briefly described|p28 Fig. 5|Albian|Oxfordian|Includes the Casterton Formation, Crayfish Subgroup (Pretty Hill and Laira Formations and Katnook Sandstone) and Eumeralla Formation. Geological Province: Otway Basin.||||||12-OCT-05
14685|Otway Group|61552|6|Mentioned|p584.|||Otway Basin. This is the western rift equivalent to the Strzelecki Group in the Gippsland Basin.||||||
14685|Otway Group|61607|6|Mentioned|p5 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Otway Basin.||||||12-MAR-09
14685|Otway Group|61608|6|Mentioned|p37|||||||||
14685|Otway Group|61624|6|Mentioned|p465|Cretaceous|Late Jurassic|Geological Province: Otway Basin.||||||07-APR-09
14685|Otway Group|61625|6|Mentioned|p476 Fig. 2|||||||||07-FEB-11
14685|Otway Group|61626|5|Briefly described|p487, p486 Fig. 2, p493, p493 Fig. 14|Early Cretaceous|Jurassic|Includes; Casterton, Gletwood Beach and Eumeralla Formations, Windermere and Heathfield Sandstones. Geological Province: Otway Basin.||||||
14685|Otway Group|61628|5|Briefly described|p509 Fig. 3, p510 Fig. 4|Early Cretaceous|Late Jurassic|Includes the Crayfish Subgroup, Casterton and Eumeralla Formations. Geological Province: Otway Basin.||||||
14685|Otway Group|61726|5|Briefly described|p924 Fig.3|Cretaceous|Cretaceous|||||||
14685|Otway Group|61841|6|Mentioned|p242|Cretaceous|Cretaceous|||||||03-JUL-06
14685|Otway Group|62896|6|Mentioned|p88|Mesozoic|Mesozoic|||||||07-FEB-11
14685|Otway Group|63173|5|Briefly described|p341, p342 Fig. 9.2, p351|Early Cretaceous|Late Jurassic|Geological Province: Otway Basin.||||||07-FEB-11
14685|Otway Group|63263|6|Mentioned|p36|||Mentioned as Late Jurassic-mid-Cretaceous correlates.||||||07-FEB-11
14685|Otway Group|63269|5|Briefly described|p604-606, p609, p618, p622-624|Early Cretaceous|Late Jurassic|Otway Basin. Terrestrial source rocks. Details of oils and oil stains in named wells tabulated.|||Crayfish Subgroup; Casterton, Eumeralla Formations.|Is overlain unconformably by Sherbrook Group.||
14685|Otway Group|63445|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous||||Eumeralla Formation.|||
14685|Otway Group|63446|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||Includes Eumeralla Formation.|||
14685|Otway Group|63740|6|Mentioned|p88|Mesozoic|Mesozoic|||||||07-FEB-11
14685|Otway Group|64535|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Includes Tyers River Subgroup and Eumeralla Formation.||||||22-DEC-08
14685|Otway Group|64539|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Includes Tyers River Subgroup and Eumeralla Formation.||||||22-DEC-08
14685|Otway Group|64540|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Includes Tyers River Subgroup and Eumeralla Formation.||||||22-DEC-08
14685|Otway Group|64605|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Includes Tyers River Subgroup amd Eumeralla Formation.||||||17-NOV-08
14685|Otway Group|64616|5|Briefly described|p141-144, p298|Early Cretaceous|Early Cretaceous|Gippsland Basin. Proposed to replace the "still largely informally used" Strzelecki Group which has the same rift basin sediments. Includes Tyers River Subgroup and Eumeralla Formation.||||||
14685|Otway Group|65107|6|Mentioned|p297 Fig 15|Early Cretaceous|Early Cretaceous |100-105 Ma||||||
14685|Otway Group|65316|5|Briefly described|p596||Early Cretaceous|Basal sedimentary package in the central coast Otway and Gippsland Basins; called the Strzelecki Group in the Gippsland Basin.||||Overlain unconfomably by Eastern View Group.|Volcaniclastic and fluvial sediments.|23-APR-12
14685|Otway Group|65715|5|Briefly described|p9 Tb.6, p10, p37|Cretaceous|Cretaceous|Includes Barwon River Conglomerate and Eumeralla Formation. Early Cretaceous.||||||
14685|Otway Group|65717|6|Mentioned|p10|||Otway Basin. Has strong affinities with the Strzelecki Group in the Gippsland Basin.||||||
14685|Otway Group|65718|6|Mentioned|p11|||Otway Basin.||||||
14685|Otway Group|65973|6|Mentioned|p14||||||Includes the Eumeralla Formation.|||
14685|Otway Group|66002|5|Briefly described|p9 Tb.6, p11, p16|Mesozoic|Mesozoic|Includes Eumeralla Formation. Overlain by Wiridjil Gravel and Moomowroong Sand in places. See discussion in VandenBerg 2009.||||||
14685|Otway Group|66181|5|Briefly described|p310 Fig.5|Albian|Berriasian|Includess the Eumeralla Formation and the Tyers River Subgroup. Unconformably underlies the Latrobe Group.||||||
14685|Otway Group|66244|5|Briefly described|p4.|Early Cretaceous|Early Cretaceous|Name applied by VandenBerg et al. (2006) and VandenBerg (2008) to all the Early Cretaceous clastic sedimentary rocks in the Otway, Bass and Gippsland Basins, thus replacing the Strzelecki Group. Because of its entrenched nature in the petroleum industry, the name (Strzelecki Group) is retained for the Early Cretaceous equivalent of the Otway Group in the Gippsland Basin.||||||
14685|Otway Group|66245|5|Briefly described|p6 Fig.5, p15, p53, pp65-67 Figs.D1-D3.|Early Cretaceous|Late Jurassic|This unit may extend well beyond the shelf edge. The lower part was deposited in a well-developed E - W half graben, with 3 sequences of lacustrine shale basin centre and infilling lacustrine delta facies. During Late Cretaceous, early parts of this unit were uplifted and eroded to form the shallow marine shelf of the Mussel Platform. The top of this unit is used to correlate well logs in this study.|||Includes Casterton and Eumeralla Formations and Crayfish Subgroup.|||
14685|Otway Group|67061|5|Briefly described|p545, p546 Fig.3, p557.|Early Cretaceous|Late Jurassic|Largely non-marine. Up to 3 km of rocks from this and older units were removed during exhumation that accompanied deformation between 100 and 95 Ma.|||Includes Pretty Hill Sandstone and Eumeralla Formation.|Is overlain unconformably by the Eastern View Group.||
14685|Otway Group|67366|6|Mentioned|p103 Fig.2. |Early Cretaceous||||||Is overlain unconformably by Sherbrook Group.||
14685|Otway Group|67367|5|Briefly described|p130, p131 Fig.2. |Early Cretaceous|Late Jurassic|Non-marine sands and shales.|||Includes Casterton and Eumeralla Formations and Crayfish Subgroup.|||
14685|Otway Group|67655|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|Angular unconformity at the top of this group. Geol. Prov: Bass Basin.||||||28-MAY-14
14685|Otway Group|68189|6|Mentioned|p25|||Of the Otway Basin.|||Includes the Casterton Formation and the Eumeralla Formation.|||
14685|Otway Group|68206|6|Mentioned|p27||||||||Contains carbonate concretions.|
14685|Otway Group|69297|5|Briefly described|p79, p97, p99 fig 2.32, p104, p400|Cenomanian|Tithonian|Otway Basin. |||Includes the Crayfish Subgroup and the Eumeralla Formation.|||
14685|Otway Group|69651|5|Briefly described|p10, p12|Early Cretaceous|Late Jurassic|Comprises Crayfish and Eumeralla Supersequences.|||Casterton, Eumeralla Formations; Crayfish Subgroup.|Is overlain unconformably by Sherbrook Group.||
14685|Otway Group|69879|5|Briefly described|p417, p435-436, p462|Albian|Aptian|Otway and Bass Basins. Volcanogenic material may come from a volcanic arc/backarc system along the Lord Howe Rise, or Cape Portland shoshonite complex and/or Cygnet Alkaline Complex. Coal and lacustrine shale provide the main hydrocarbon source rocks in Bass Basin.|||||Non-marine volcanogenic sediments from dacitic volcanism, coal and lacustrine shale.|
14685|Otway Group|70077|5|Briefly described|Nelson: Fig.2; p1-2. Regional: Fig.4; p1|Early Cretaceous|Early Cretaceous|See also Regional: p3, p9. Otway Basin: Gambier Embayment and Voluta Trough. Distal equivalents in the Nelson Sub-basin may be petroleum sources.|||Crayfish Subgroup; Eumeralla, Casterton Formations.|Is overlain by Sherbrook Group.||
14685|Otway Group|70078|5|Briefly described|Northern: Fig.2; p2. Regional: Fig.4|Albian|Albian|Otway Basin. Fluvio-lacustrine, coaly rocks equivalent to this unit in the Sorell Basin are potential hydrocarbon sources.|||Eumeralla Formation.|Is overlain by Sherbrook Group.||
14685|Otway Group|70942|14|Not recorded|p117||Mesozoic|||||||
14685|Otway Group|71419|5|Briefly described|p8 Fig 2, p16 Fig 17|Cretaceous|Cretaceous|Fluvial sediments.|||Includes Eumeralla Formation.|||02-FEB-18
14685|Otway Group|71593|6|Mentioned|p45, p138|||Otway Basin.||||||
14685|Otway Group|73153|6|Mentioned|p287||||||Eumeralla Formation|||
14685|Otway Group|73356|6|Mentioned|p1, p4, p14, p17, p20||||||Eumeralla Formation, Heathfield Sandstone, Windermere Sandstone, Casterton Formation, and Crayfish Subgroup and units therein|||
14685|Otway Group|73357|6|Mentioned|p2 Fig.1.1, p43, p45, p47|Albian|Berriasian|Otway Basin.|||Crayfish Subgroup|||
14685|Otway Group|73383|4|Described|v-vi, p2-4, p6, p11|Cenomanian|Tithonian|Otway Basin. Equivalent to chemostratigraphic sequences S0 to S4.|||Casterton Formation, Crayfish Subgroup, Eumeralla Formation|Underlies Sherbrook Group|Includes lacustrine mudstones and alluvial sandstones with initial basaltic volcanics, fluvial channel sandstones, and fluvial volcanoclastics, lithicarenites, mudstones, coal, fluvial overbank and floodplain deposits.|
14685|Otway Group|73385|5|Briefly described|p4-5, p28|Albian|Tithonian|Otway Basin. Previously referred to as the 'Merino Group'.|||Crayfish Subgroup, Eumeralla Formation, Windermere Sandstone, Hawkesdale Volcanics, Heathfield sandstone|Underlies Sherbrook Group.|Includes lacustrine mudstones and alluvial sandstones with initial basaltic volcanics, fluvial channel sandstones, and fluvial volcanoclastics, lithicarenites, mudstones, coal, fluvial overbank and floodplain deposits.|
14685|Otway Group|73386|4|Described|p1, p4-7, p10, p12, iii, Attachment A1|Albian|Tithonian|Otway Basin. Unconformably overlies Paleozoic basement. Belongs to Retitriletes watherooensis - Phimopollenites pannosus spore pollen zones. Chemostratigraphic division into sequences S0-S4 of Forbes et al. (2020). Top boundary represents a sequence boundary characterised by uplift and erosion during the Cenomanian inversion. Contact with overlying Sherbrook Group varies from conformable or mildly disconformable to unconformable. Wangerrip Group onlaps the Otway Group along northern margin of basin.|||Casterton Formation, Crayfish Subgroup, Eumeralla Formation|Underlies Sherbrook Group|Includes lacustrine mudstones and alluvial sandstones with initial basaltic volcanics, fluvial channel sandstones, volcanoclastics, lithicarenites, mudstones, coal, fluvial overbank and floodplain deposits.|
14685|Otway Group|73505|6|Mentioned|p2, p14|Early Cretaceous|Late Jurassic|||||||
14685|Otway Group|73594|5|Briefly described|p2, p4, p14|Cenomanian|Tithonian|Otway Basin.|||Casterton Formation, Crayfish Subgroup, Eumeralla Formation|Underlies Sherbrook Group||
14695|Ovens Group|34148|6|Mentioned|p10|||Upper Palaeozoic.||||||
14730|Paaratte Formation|12781|6|Mentioned|p386|Late Cretaceous|Late Cretaceous|Otway Basin. Maximum thickness 1987m.||Sherbrook Group.||Overlies Belfast Mudstone and Flaxman Formation. Abuts Timboon Sandstone.||
14730|Paaratte Formation|12796|4|Described|p460, p456 Fig. 2|Campanian|Santonian|Of  Sherbrook Gp. Originally included members - Belfast Mdst Mbr, Nullawarre Greensand and Timboon Sand Mbr - which are now formations. Interfingers with and overlies Skull Creek Mdst. Geol. Prov: Otway Basin.||||||
14730|Paaratte Formation|22674|5|Briefly described|Fig.2 p719|Maastrichtian|Santonian|||||||
14730|Paaratte Formation|22875|3|Fully described|p44|Late Cretaceous|Late Cretaceous|Sherbrook Group.||||||14-APR-08
14730|Paaratte Formation|22944|5|Briefly described|Fig3|||||||||
14730|Paaratte Formation|23818|4|Described|p164|Late Cretaceous|Late Cretaceous|Overlain by Curdie Formation. Underlain by Belfast Mudstone. Max. thickness: 5 800 ft.||||||29-JAN-07
14730|Paaratte Formation|23830|6|Mentioned|Fig. 6|||Geological Province: Gambier Embayment, Otway Basin.||||||24-JAN-06
14730|Paaratte Formation|24056|5|Briefly described|p85|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||14-APR-08
14730|Paaratte Formation|24314|5|Briefly described|p61 Fig.2||Santonian|Geological Province: Otway Basin. Max. Thickness 1987m. Of the Sherbrook Group.||||||30-NOV-04
14730|Paaratte Formation|24453|5|Briefly described|p809 Fig.2|Maastrichtian|Santonian|Of Sherbrook Group. Overlain by Tomboon Sandstone Member, overlies Belfast Mudstone and Nullawarre Greensand. Geological Province: Otway Basin.||||||07-FEB-11
14730|Paaratte Formation|24551|6|Mentioned|p245|||Of the Sherbrook Group.||||||14-APR-08
14730|Paaratte Formation|24562|5|Briefly described|p3, 8|Late Cretaceous|Late Cretaceous|Of the Sherbrook Group. Geological Province: Otway Basin.||||||14-APR-08
14730|Paaratte Formation|29697|6|Mentioned|Fig.11|||||||||
14730|Paaratte Formation|29856|5|Briefly described|p38|||||||||
14730|Paaratte Formation|30499|6|Mentioned|p92|||Stratigraphy.||||||14-APR-08
14730|Paaratte Formation|30576|5|Briefly described|Table 2|||||||||
14730|Paaratte Formation|30578|5|Briefly described|p7|||||||||
14730|Paaratte Formation|30580|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14730|Paaratte Formation|30675|5|Briefly described|p253|||Lithology and radioactivity.||||||29-JAN-07
14730|Paaratte Formation|30754|6|Mentioned|p12|||Stratigraphic table.||||||14-APR-08
14730|Paaratte Formation|30905|6|Mentioned|Table 7.3|||||||||
14730|Paaratte Formation|30932|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|Part of Wangerrip Group.||||||14-APR-08
14730|Paaratte Formation|31245|6|Mentioned|p77|||||||||
14730|Paaratte Formation|31372|6|Mentioned|p2|||See also p9.||||||29-JAN-07
14730|Paaratte Formation|31396|6|Mentioned|p1185|||||||||
14730|Paaratte Formation|31424|4|Described|p17|||Described from core.||||||
14730|Paaratte Formation|31534|6|Mentioned|p393|||See also Table 19-3.||||||29-JAN-07
14730|Paaratte Formation|31624|6|Mentioned|Table 5-1|||See also Table 5-2.||||||29-JAN-07
14730|Paaratte Formation|31625|6|Mentioned|Fig. 5.2|||||||||
14730|Paaratte Formation|31714|6|Mentioned|Fig. 8|||||||||
14730|Paaratte Formation|31920|4|Described|p51|||U.Cret. Unit of Sherbrook Group.||||||29-JAN-07
14730|Paaratte Formation|31922|6|Mentioned|p187|||||||||
14730|Paaratte Formation|32344|6|Mentioned|Fig.2|||||||||
14730|Paaratte Formation|32852|6|Mentioned|p10|||||||||
14730|Paaratte Formation|32894|6|Mentioned|p286|||U.Cret.||||||
14730|Paaratte Formation|32896|6|Mentioned|Encl.7.1.|||U.Cret.||||||
14730|Paaratte Formation|32898|6|Mentioned|Table 2-1|||||||||
14730|Paaratte Formation|32899|4|Described|p164|||See also pp165-175.||||||29-JAN-07
14730|Paaratte Formation|33155|6|Mentioned|p115|||||||||
14730|Paaratte Formation|33165|6|Mentioned|Chart|||Correlation chart only.||||||14-APR-08
14730|Paaratte Formation|33936|6|Mentioned|Fig.6|||||||||
14730|Paaratte Formation|33940|6|Mentioned|Fig.21-1|||Turonian - Maastrichtian||||||
14730|Paaratte Formation|34063|6|Mentioned|p3|||U.Cret. Table||||||
14730|Paaratte Formation|34308|6|Mentioned|Fig.85|||U.Cret. Sherbrook Group.||||||14-APR-08
14730|Paaratte Formation|34611|5|Briefly described|p164|||Upper Cretaceous||||||
14730|Paaratte Formation|34987|3|Fully described|p171|||||||||
14730|Paaratte Formation|35013|6|Mentioned|p393|||||||||
14730|Paaratte Formation|35066|6|Mentioned|p205|||||||||
14730|Paaratte Formation|35285|6|Mentioned|p414|||||||||
14730|Paaratte Formation|35722|6|Mentioned|p3|||Stratigraphy.||||||
14730|Paaratte Formation|36366|6|Mentioned|p3|||||||||
14730|Paaratte Formation|36913|6|Mentioned|p81|||||||||
14730|Paaratte Formation|38444|6|Mentioned|p302|||||||||
14730|Paaratte Formation|38625|6|Mentioned|Table 2|||||||||
14730|Paaratte Formation|40003|5|Briefly described|p43|||See also Fig.10||||||
14730|Paaratte Formation|40560|5|Briefly described|Fig.3|||||||||
14730|Paaratte Formation|40947|6|Mentioned|p4|||||||||
14730|Paaratte Formation|41016|5|Briefly described|p214|||||||||
14730|Paaratte Formation|41185|6|Mentioned|p177|||||||||
14730|Paaratte Formation|41269|5|Briefly described|p245|||||||||
14730|Paaratte Formation|41642|4|Described|p244|||||||||
14730|Paaratte Formation|41701|6|Mentioned|Map legend|Paleocene||Age spelt Palaeocene.||||||
14730|Paaratte Formation|41704|6|Mentioned|p100|||||||||
14730|Paaratte Formation|41714|6|Mentioned|p301|||||||||
14730|Paaratte Formation|41726|3|Fully described|p421|||See also p427.||||||29-JAN-07
14730|Paaratte Formation|41769|5|Briefly described|p16|||See also p17.||||||29-JAN-07
14730|Paaratte Formation|41868|4|Described|p533|||||||||
14730|Paaratte Formation|41936|6|Mentioned|p75|||||||||
14730|Paaratte Formation|42079|6|Mentioned|Fig.2 P264|||||||||
14730|Paaratte Formation|42318|6|Mentioned|p7|||||||||
14730|Paaratte Formation|42361|3|Fully described|p16|Maastrichtian|Turonian|Usage restricted to original concept of McQueen (1961).||||||
14730|Paaratte Formation|42524|5|Briefly described|Fig.3 P27|||||||||
14730|Paaratte Formation|42545|6|Mentioned|p19|||In the Otway Basin.||||||29-JAN-07
14730|Paaratte Formation|42555|6|Mentioned|p285|||||||||
14730|Paaratte Formation|42599|5|Briefly described|Fig.3 P614|||||||||
14730|Paaratte Formation|42827|4|Described|p244|||||||||
14730|Paaratte Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
14730|Paaratte Formation|43052|5|Briefly described|Table 2.1|||||||||
14730|Paaratte Formation|43171|5|Briefly described|5-8|||Of Sherbrook Formation. Age: 65-85 Ma||||||
14730|Paaratte Formation|43195|5|Briefly described|Map Legend||Late Cretaceous|See also commentary on back of map. Of Sherbrook Group.||||||
14730|Paaratte Formation|43208|5|Briefly described|map legend|Maastrichtian|Santonian|Of Sherbrook Group.||||||
14730|Paaratte Formation|43219|5|Briefly described|Fig.3,p6.|Maastrichtian|Santonian|Of Sherbrook Group.||||||29-JAN-07
14730|Paaratte Formation|43590|4|Described|p14|Maastrichtian|Santonian|||||||
14730|Paaratte Formation|43660|6|Mentioned|Fig.6,p15||Late Cretaceous|||||||
14730|Paaratte Formation|43733|6|Mentioned|Fig.2.11,p65||Late Cretaceous|||||||
14730|Paaratte Formation|43744|6|Mentioned|Fig.3,p3|||||||||
14730|Paaratte Formation|43783|6|Mentioned|Fig14, p11||Late Cretaceous|||||||
14730|Paaratte Formation|43784|6|Mentioned|Fig10, p12||Late Cretaceous|||||||
14730|Paaratte Formation|43814|6|Mentioned|Fig.3,p115|||||||||
14730|Paaratte Formation|43937|5|Briefly described|Map Legend|Santonian|Aptian|||||||
14730|Paaratte Formation|44133|4|Described|p147|Maastrichtian|Santonian|Of the Sherbrook Group. Geological Province: Otway Basin. Previously 'Paaratte Formation'. Thickness: 1836m. Underlies Timboon Sandstone and Dilwyn Formation, unconformably.||||||29-JAN-07
14730|Paaratte Formation|48581|2|Defined|p33|||See also p12,28,29,34,38,40. Fig.4,6,Pl.1,2. Underlies Wangerrip Gp; Overlies Belfast Mudstone. (J54-12/Port Campbell).||||||07-APR-09
14730|Paaratte Formation|48624|14|Not recorded|p5,7,Fig.2|||(J54-6/Benara).||||||
14730|Paaratte Formation|48625|14|Not recorded|p7|||(J54-6/Benara).||||||
14730|Paaratte Formation|48911|3|Fully described|p20|||||||||
14730|Paaratte Formation|48977|6|Mentioned|Fig.5|||||||||
14730|Paaratte Formation|49060|5|Briefly described|Fig.33|||||||||
14730|Paaratte Formation|61017|5|Briefly described|p5 Fig. 2|Campanian|Campanian|Of the Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
14730|Paaratte Formation|61182|3|Fully described|p18, p32, p84|Maastrichtian|Santonian|Of Sherbrook Gp. Incl:Timboon Sand and Skull Creek Mbrs.Conformable on Nullawarre Greensand, and Belfast Mudst.near coast.Unconformable below Pebble Point Fm.Thick: 962m. Geol.Prov: Otway Basin. Age from spore-pollen zones. older in South Australia. Prev.incl: Belfast Mudst, Nullawarre Greensand, Timboon Sand||||||20-SEP-18
14730|Paaratte Formation|61230|5|Briefly described|p319 Fig.2, p329, p341, pp344-345.    |Campanian|Santonian|Delta front to delta plain progradational depositional settings.||Unit in Sherbrook Group.||Overlies Belfast Mudstone (Formation). Is overlain by Timboon Formation.|Sandstone, mudstone; increasingly sandstone-dominated up-unit to coarse sandstone and conglomerate.|
14730|Paaratte Formation|61470|5|Briefly described|p28 Fig. 5|Campanian|Campanian|Of the Sherbrook Group. Overlies Skull Creek Mudstone (with which it also interfingers); underlies Timboon Sandstone. Geological Province: Otway Basin.||||||12-OCT-05
14730|Paaratte Formation|61547|6|Mentioned|p461 Fig.2, p462. |Maastrichtian|Santonian|||Unit in Sherbrook Group.||Overlies Belfast Mudstone. Is overlain by Pebble Point Formation.||
14730|Paaratte Formation|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
14730|Paaratte Formation|61623|6|Mentioned|p449 Fig. 4|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
14730|Paaratte Formation|61625|5|Briefly described|p475, p476 Fig. 1, p477, p480, p483|Late Creatceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin. Mediun to fine-grained sandstone with rare molluscs with bioturbated mudstones.||||||07-FEB-11
14730|Paaratte Formation|61626|5|Briefly described|p486, p486 Fig. 2|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
14730|Paaratte Formation|61627|5|Briefly described|p500 Fig. 2|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
14730|Paaratte Formation|61628|5|Briefly described|p509 Fig. 3|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
14730|Paaratte Formation|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p82|Late Cretaceous|Late Cretaceous|Past stratigraphy has included various nomenclatures for Skull Creek Member and Timboon Sand Member. Timboon now of formation status - as Timboon Sandstone; Skull Creek units are incorp.into Paaratte Formation. Max. thickness:1987m. Geol.Prov: Otway Basin||||||
14730|Paaratte Formation|63125|6|Mentioned|p121 Tb. 7.11|||Geological Province: Otway Basin.||||||14-APR-08
14730|Paaratte Formation|63129|5|Briefly described|p137|||Offshore, this unit is an interbedded shale-sand facies into which the Timboon Sandstone passes laterally. Geological Province: Otway Basin.||||||14-APR-08
14730|Paaratte Formation|63269|5|Briefly described|p605-606|Late Cretaceous|Late Cretaceous|Otway Basin. Details of oils and oil stains in named wells tabulated. Appears as Parratte Sandstone [!] on p606.||Sherbrook Group.||||
14730|Paaratte Formation|63431|5|Briefly described|p677 Fig. 2|Maastrictian|Santonian|Of the Sherbrook Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
14730|Paaratte Formation|66245|5|Briefly described|p6 Fig.5, p22 Fig.25, p63 Fig.C5.|Maastrichtian|Santonian|||Unit in Sherbrook Group.||Overlies Belfast Mudstone. Is intercalated with Nullawarre Greensand. Is overlain by Timboon Sandstone. ||
14730|Paaratte Formation|67061|6|Mentioned|p546 Fig.3.|Late Cretaceous|Late Cretaceous|||Unit in Sherbrook Group.||Is overlain by Timboon Sandstone.||15-MAR-12
14730|Paaratte Formation|67366|5|Briefly described|p103 Fig.2, p124.|Campanian|Campanian|Contains biodegraded gas.||Unit in Sherbrook Group.||Overlies Skull Creek Mudstone. Is overlain by Timboon Sandstone.|Shallow to nearshore marine sandstone and shale.|
14730|Paaratte Formation|67367|5|Briefly described|p131 Fig.2. |Campanian|Campanian|||Unit in Sherbrook Group.||||
14730|Paaratte Formation|69297|5|Briefly described|p79, p84, p98, p115|Maastrichtian|Campanian|Otway Basin. Contains good quality reservoir intervals. ||Sherbrook Group||Overlies the Belfast Mudstone or the Skull Creek Mudstone. Faulted against or overlain by the Timboon Sandstone. |Siltstones. |
14730|Paaratte Formation|69651|5|Briefly described|p10, p27, p32-34|Late Cretaceous|Late Cretaceous|Campanian-Maastrichtian age. Contains good-quality reservoirs; intraformational mudstones may form seals. Has gas shows in tilted fault blocks.||Sherbrook Group.||Overlies Belfast Mudstone. Is interbedded with Nullawarre Greensand. Is overlain by Timboon Sandstone.||
14730|Paaratte Formation|70077|5|Briefly described|Nelson: Fig.2; p2. Regional: Fig.4; p8|Campanian|Santonian|See also Regional: p10-11. Otway Basin. Distal sandstone equivalents in the Nelson Sub-basin may be important petroleum reservoirs. Also contains intraformational mudstones with good sealing capacity.||Sherbrook Group.||Overlies Mount Salt Formation, Belfast or Skull Creek Mudstones. Is overlain by Timboon Sandstone.||
14730|Paaratte Formation|70078|5|Briefly described|Northern: Fig.2; p2. Regional: Fig.4|Campanian|Santonian|Otway Basin. Sandstones equivalent to this unit in the Sorell Basin are potential hydrocarbon sources. Similarly, equivalent rocks are potential intraformational seals.||Sherbrook Group.||Overlies Mount Salt Formation. Is overlain by Timboon Sandstone.||
14730|Paaratte Formation|70193|5|Briefly described|p283, p284, p285-288|Campanian|Campanian|Geological province: Otway Basin. X. australis dinocyst zone; formation varies in thickness from 160 to 339m.||Unit of the Sherbrook Supersequence||Underlain unconformably by Skull Creek Mudstone, overlain conformably by Timboon Sandstone.|Carbonaceous, interbedded and laminated fine-grained sandstone, siltstone and mudstone with thin beds of coarse sandstone and gravel.|30-MAY-19
14730|Paaratte Formation|70880|6|Mentioned|p77|Maastrichtian|Coniacian|Otway Basin. Hydrocarbon reservoir.||||||
14730|Paaratte Formation|70942|6|Mentioned|p118|||||||||
14730|Paaratte Formation|71266|6|Mentioned|p614 Fig.3|Late Cretaceous|Late Cretaceous|Otway Basin.||||||
14730|Paaratte Formation|71437|4|Described|Fig. 1 opp 154,  p155, p157-158|Maastrichtian|Coniacian|Paralic, deltaic, lagoonal and tidal flat environment.||Of Wangerrip Group.|Includes Belfast Mudstone, Nullawarre Greensand, Timboon Sand members.|Gradational, transitional or interfingering  with Timboon Sand Mmeber. Unconformably overlain by Pebble Point Formation.|Clay-silt shale, quartz sand, silty sand, minor glauconite, coal, and ankerite-siderite. Well-bedded and laminated.|
14730|Paaratte Formation|73357|5|Briefly described|p21-24, p31, p45, p47|Campanian|Santonian|Otway Basin. Skull Creek Mudstone/Paaratte Formation boundary is diachronous, and lithostratigraphic boundary with Timboon Sandstone can be uncertain. Correlated with Nelsoniella aceras Dinocyst Zone, Xenikoon australis Dinocyst Zone, nearshore to marginal marine depositional environments. Correlated to multiple biozones including Tricolpites apoxyexinus Spore-Pollen Zone in western regions. Upper part correlated with Isabelidinium pellucidum Dinocyst Zone, and Forcipites longus Spore-Pollen Zone at uppermost part.||Of Sherbrook Group.||Overlies Skull Creek Mudstone, underlies Timboon Sandstone.|Includes shales.|
14730|Paaratte Formation|73383|5|Briefly described|p3, p10 Tb.3.7, p22-23, p247-248, p258|Maastrichtian|Campanian|Otway Basin. Approximately equivalent to chemostratigraphic package S5-P7 containing high Th/Sc and Si/Al values, low Th/K and Sm/U values. Intervals are also assigned to chemostratigraphic package S5-P5 defined by high Fe and P values. Lithologies based on geochemistry using the ChemLith classification includes sandstones, calcareous and argillaceous sandstones, calcareous limestone; and using the Herron classification (1988) includes lith-arenite, Fe-sand and Fe-shale. See also vi, p11 Tb.3.9, p67, p119, p131-132, p140, p199-200, p258-260, p267, p322, p325.||Sherbrook Group||Overlies Skull Creek Mudstone, Nullawarre Greensand, underlies Timboon Sandstone|Predominantly sand lithologies, including quartz arenites, sublith-arenites and subarkose.|
14730|Paaratte Formation|73385|5|Briefly described|p5|Maastrichtian|Campanian|Otway Basin.||Sherbrook Group||Overlies Skull Creek Mudstone, Nullawarre Greensand, underlies Timboon Sandstone.|Shallow marine and nearshore sandstones.|
14730|Paaratte Formation|73386|4|Described|p4, p6, p10-11, Attachment A1|Maastrichtian|Santonian|Otway Basin. Diachronous unit deposited across the Otway Basin, extends from Tricolporites apoxyexinus Spore-Pollen Zone to Lower Forcipites longus Spore-Pollen Subzone. Changes facies from upper delta plain to upper delta front interbedded sandstones and shales onshore and nearshore, to lower delta front and prodelta siltstones and shales further offshore. Interfingers with Skull Creek Mudstone in Port Campbell and Tyrendarra embayments.||Sherbrook Group||Overlies and interfingers with Skull Creek Mudstone, overlies Nullawarre Greensand, Belfast Mudstone, underlies Timboon Sandstone|Interbedded fine to coarse grained sandstones with mudstone and occasional coals.|
14730|Paaratte Formation|73594|5|Briefly described|p4-5, p13|Maastrichtian|Campanian|Otway Basin.||Sherbrook Group||Overlies Skull Creek Mudstone, Nullawarre Greensand, underlies Timboon Sandstone|Shallow marine and nearshore sandstones.|
14771|Padthaway Formation|10010|5|Briefly described|p14-15 Fig. 5e|Quaternary|Quaternary|Geological Province: Murray Basin.||||||13-AUG-07
14771|Padthaway Formation|29697|6|Mentioned|p23|||||||||
14771|Padthaway Formation|29892|6|Mentioned|p77|||||||||
14771|Padthaway Formation|33798|6|Mentioned|Fig.2|||||||||
14771|Padthaway Formation|38932|5|Briefly described|p99|||See also Fig.4||||||
14771|Padthaway Formation|42129|6|Mentioned|p254|||See also Fig.6||||||
14771|Padthaway Formation|42601|6|Mentioned|Fig.2 p15|||||||||
14771|Padthaway Formation|42966|3|Fully described|p227|||||||||
14771|Padthaway Formation|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Silt, dolomite and sand of lagoons and swamps.||||||25-MAY-05
14771|Padthaway Formation|43195|5|Briefly described|Map Legend|Late Pleistocene|Early Pleistocene|see also commentary on back of map.||||||
14771|Padthaway Formation|43258|5|Briefly described|Map Legend||Pleistocene|||||||
14771|Padthaway Formation|43298|5|Briefly described|Map Legend||Pleistocene|||||||
14771|Padthaway Formation|44133|5|Briefly described|p221 Fig. 11.3|Pleistocene|Pleistocene|Lagoonal and lacustrine facies.||||||
14771|Padthaway Formation|49038|5|Briefly described|p33|||||||||
14771|Padthaway Formation|50154|2|Defined|p21 Fig. 3.3, p26, p140|Recent|Pleistocene|Age: oldest dunes min. 0.69 Ma. Formation formed in the swales between dunes of the Bridgewater Formation. Consists of unconsolidated clay, sandy clay, calcareous clay, minor quartz sand and shell detritus.||||||23-MAY-13
14771|Padthaway Formation|50156|5|Briefly described|Map Legend|Pleistocene|Miocene|Lacustrine: lagoonal, swamp and locally colluvial deposits forming low-lying wetlands between stranded beach ridges: sand, silt, sandy clay, peat, marl, freshwater limestone; unconsolidated.||||||
14771|Padthaway Formation|50157|5|Briefly described|Map Legend|Recent|Pleistocene|Lacustrine: lagoonal, swamp and locally colluvial deposits forming low-lying wetlands between stranded beach ridges: sand, silt, sandy clay, peat, marl, freshwater limestone; unconsolidated.||||||
14771|Padthaway Formation|50158|5|Briefly described|Map Legend|Recent|Pleistocene|Lacustrine: lagoonal, swamp and locally colluvial deposits forming low-lying wetlands between stranded beach ridges: sand, silt, sandy clay, peat, marl, freshwater limestone; unconsolidated.||||||
14771|Padthaway Formation|50159|5|Briefly described|Map Legend|Recent|Pleistocene|Lacustrine: lagoonal, swamp and locally colluvial deposits forming low-lying wetlands between stranded beach ridges: sand, silt, sandy clay, peat, marl, freshwater limestone; unconsolidated.||||||24-JUN-04
14771|Padthaway Formation|50160|5|Briefly described|Map Legend|Recent|Pleistocene|||||||16-JUN-04
14771|Padthaway Formation|50161|5|Briefly described|Map Legend|Recent|Pleistocene|Lacustrine: lagoonal, swamp and locally colluvial deposits forming low-lying wetlands between stranded beach ridges: sand, silt, sandy clay, peat, marl, freshwater limestone; unconsolidated.||||||
14771|Padthaway Formation|50162|5|Briefly described|Map Legend|Recent|Pleistocene|Lacustrine: lagoonal, swamp and locally colluvial deposits forming low-lying wetlands between stranded beach ridges: sand, silt, sandy clay, peat, marl, freshwater limestone; unconsolidated.||||||
14771|Padthaway Formation|50163|5|Briefly described|Map Legend|Recent|Pleistocene|Lacustrine: lagoonal, swamp and locally colluvial deposits forming low-lying wetlands between stranded beach ridges: sand, silt, sandy clay, peat, marl, freshwater limestone; unconsolidated.||||||
14771|Padthaway Formation|60953|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Silt, dolomite and sand of lagoons and swamps.||||||
14771|Padthaway Formation|61108|5|Briefly described|map legend|Pleistocene|Pleistocene|Silt, dolomite and sand of lagoons and swamps.||||||
14771|Padthaway Formation|61155|5|Briefly described|p6|Pleistocene|Pleistocene|Inter-ridge estuarine/lacustrine/lagoonal sequences. Geological Province: Otway and Murray Basins/coastal margins.||||||
14771|Padthaway Formation|63124|6|Mentioned|p93|||Geological Province: Gambier Basin.||||||
14771|Padthaway Formation|65376|5|Briefly described|p9 Fig.1.2. |Pleistocene|Pleistocene||||||Silt, dolomite and sand of lagoons and swamps.|
14771|Padthaway Formation|66002|5|Briefly described|p13 Tb.9|Neogene|Neogene|Defined by Harris 1973.||||||
14771|Padthaway Formation|68116|5|Briefly described|Appendix, Maps 29, 38, 47.|Pleistocene|Pleistocene||||||Lagoonal, swamp and locally colluvial deposits forming low-lying wetlands between stranded beach ridges: sand, silt, sandy clay, peat, marl, freshwater limestone; unconsolidated.|
14771|Padthaway Formation|68131|5|Briefly described|p2 Fig.1|Pleistocene|Pleistocene|Lagoon and swamp sediments.|||||Silt, dolomite and sand.|
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.|
68522|Parmeener Supergroup, Upper|24551|6|Mentioned|p565|Late Triassic|Late Permian|||||||
68522|Parmeener Supergroup, Upper|24552|5|Briefly described|p5|Triassic|Late Permian|Non-marine rocks. Geological Province: Tasmanian Basin. Geological Province: Tasmanian Basin.||||||07-FEB-11
68522|Parmeener Supergroup, Upper|41696|6|Mentioned|Map legend|Triassic||||||||
68522|Parmeener Supergroup, Upper|42244|4|Described|p24|||||||||12-AUG-08
68522|Parmeener Supergroup, Upper|42553|6|Mentioned|Map legend|Triassic|Permian|||||||
68522|Parmeener Supergroup, Upper|43084|5|Briefly described|p12|||||||||
68522|Parmeener Supergroup, Upper|44135|4|Described|p44|Late Triassic|Late Permian|Comprises four lithological units including Cygnet Coal Measures and 3 unnamed units. Geological province: Tasmanian Basin.||||||07-DEC-09
68522|Parmeener Supergroup, Upper|63172|3|Fully described|p293, p309-334|||Informal - see Parmeener Gp. Chapt. 8 is divided into Lower Parmeener and Upper Parmeener Supergroups, herein treated as separate entities.They are separated by a hiatus spanning at least the Early Triassic. Palaeontological details (p321-323).||||||07-FEB-11
68522|Parmeener Supergroup, Upper|63263|6|Mentioned|p21|||Informal term used throughout Tasmanian literature - see Paremeener Supergroup. Non-marine succession of rocks comprising 4 lithological subunits - Cynet Coal Measures, a quartzarenite unit, a conglomerate-sandstone-lutite unit and a lithic sandstone.||||||
68522|Parmeener Supergroup, Upper|63675|5|Briefly described|p22|Triassic|Late Carboniferous|Fluvial and lacustrine sedimentary rocks, including subordinate coal measures. Tasmania Basin.||||||
68522|Parmeener Supergroup, Upper|65647|5|Briefly described|p5,App p8-9, 11 |Triassic|Triassic|Flat lying sedimentary rocks with tholeiitic intrusions. Fluviolacustrine sandstone, siltstone, mudstone; lithic sandstone with felsic volcanics; coal; basalt; quartz sandstone.||||||24-DEC-15
68522|Parmeener Supergroup, Upper|65653|6|Mentioned|p10.|||Intruded by basalt plugs, eg at North Apsley.||||||
68522|Parmeener Supergroup, Upper|65654|5|Briefly described|p4, p7 Fig. 3|Triassic|Late Permian|Freshwater/terrestrial sediments. Shows Liesegang rings.|||||Quartz arenite, up to 100m thick, coarse grained massive and cross bedded sandstone.; also clay pellets and conglomerate.|
68522|Parmeener Supergroup, Upper|65662|5|Briefly described|pp 9-12.  |Triassic|Late Permian||||Includes Cygnet and New Town Coal Measures and Knocklofty Formation.||Fluviolacustrine sequences of sandstone, siltstone, mudstone; lithic sandstone with felsic volcaniclastics; quartz sandstone, coal, basalt.|
68522|Parmeener Supergroup, Upper|67501|4|Described|p7, p18, Fig.8 p17,|Late Triassic|Late Permian|Freshwater division. Cross-bedded, carbonaceous feldspathic sandstone and siltstone, about 30 m thick, marks the base of the upper Parmeener Supergroup, with cross-bedded quartz sandstone and subordinate siltstone forming the remainder of ~300 m. includes coal measures in parts of Tasmania (Forsyth 1989).|||Kaoota Coal Measures, Cygnet Coal Measures|Correlates (partly) to Cygnet Coal Measures and Ross Formation.|Basal: cross-bedded, carbonaceous feldspathic sandstone and siltstone; remainder: cross-bedded quartz sandstone and subordinate siltstone.|
68522|Parmeener Supergroup, Upper|67655|6|Mentioned|p22|||Geol. Prov: Tasmania Basin|||||fluvial and lacustrine sedimentary rocks, subordinate coal measures|
68522|Parmeener Supergroup, Upper|69773|6|Mentioned|p32|Triassic|Permian|Comprises freshwater rocks of the Late Permian and Triassic.||||||
68522|Parmeener Supergroup, Upper|69842|6|Mentioned|p6|||Quamby Bluff map; additional subdivision along the Lake Highway.||||||
68522|Parmeener Supergroup, Upper|69856|5|Briefly described|Map legend|Triassic|Triassic|Undifferentiated fluviolacustrine sequences of sandstone, siltstone and mudstone; the five facies are mapped separately.||||Overlies Lower Parmeener Supergroup.|Dominantly lithic volcaniclastic sandstone; lithic sandstone, siltstone, mudstone and felsic tuff, some coal and basal quartz sandstone; alkali olivine basalt/hawaiite; dominantly siltstone, lithic sandstone and mudstone; dominantly quartz sandstone.|
68522|Parmeener Supergroup, Upper|69857|5|Briefly described|Map legend|Triassic|Triassic||||||Undifferentiated fluviolacustrine sequences of sandstone, siltstone and mudstone.|
68522|Parmeener Supergroup, Upper|69858|5|Briefly described|Map legend|Triassic|Triassic|Five facies are mapped separately.||||Overlies Lower Parmeener Supergroup.|Fluviolacustrine sequences of sandstone, siltstone and mudstone.|
68522|Parmeener Supergroup, Upper|69859|5|Briefly described|Map legend|Triassic|Triassic|The four facies are mapped separately.||||Overlies Lower Parmeener Supergroup.|Fluviolacustrine sequences of sandstone, siltstone and mudstone: dominantly lithic volcaniclastic sandstone; lithic sandstone, siltstone, mudstone, felsic tuff with some coal and basal quartz sandstone; dominantly quartz sandstone.|
68522|Parmeener Supergroup, Upper|69870|5|Briefly described|Map legend|Triassic|Triassic||||||Fluviolacustrine sequences of sandstone, siltstone and mudstone: coal measures, basalt, lithic sandstone with felsic volcaniclastics, quartz sandstone.|
68522|Parmeener Supergroup, Upper|69877|3|Fully described|p363, p376-384|Late Triassic|Capitanian|Non-marine rocks. The Triassic sandstones form distinctive exposures and low cliffs. Age from a tuff near the top of the unit gives an approximate (mid Norian) minimum age. The Late Triassic succession hosts all the economically important coal reserves in the State.|214 +/- 1 Ma (Bacon and Green, 1984).||Includes Cygnet Coal Measures; Jackey Shale; Clog Tom Sandstone; Ross, Ossa, Knocklofty, Cluan, Tiers, Brady Formations; Gould Conglomerate.||Carbonaceous sandstone and coal (Late Permian); quartzose sandstone (Early Triassic); lithic and quartz sandstone and basaltic volcanics (Middle Triassic); sandstone, coal and volcaniclastics (Late Triassic).|
68522|Parmeener Supergroup, Upper|69879|6|Mentioned|p446, p454, p465 Fig.9.53|||||||||
68522|Parmeener Supergroup, Upper|73319|5|Briefly described|Map legend|Triassic|Triassic|||Parmeener Supergroup|||Includes sandstone, siltstone, mudstone, coal measures, basalt, and felsic volcaniclastics.|
68522|Parmeener Supergroup, Upper|73639|5|Briefly described|p2-3|Late Triassic|Permian|Mainly continental deposition.|||Cygnet Coal Measures.|Overlies Lower Parmeener Supergroup.|Quartz sandstone, quartz and lithic sandstone, volcanic and lithic sandstone and coal measures.|
69420|Parslow Diorite|61161|5|Briefly described|p97-98, p76-77 Fig 6.1|Early Devonian|Early Devonian|Small circular pluton of diorite; grey-green speckled appearance; medium-grained, equigranular and metamorphosed. Intrudes Omeo Metamorphic Complex. I-type. GSV map code: G466.||||||
69420|Parslow Diorite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Kaersutite-augite diorite: medium-grained, equigranular; metamorphosed; contains plagioclase, kaersutite, augite, quartz, apatite; metamorphic epidote, actinolite, chlorite, sphene, probable albite; I-type intrusion. GSV map code: G466.||||||
69420|Parslow Diorite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Kaersutite-augite diorite: medium-grained, equigranular; metamorphosed; contains plagioclase, kaersutite, augite, quartz, apatite; metamorphic epidote, actinolite, chlorite, sphene, probable albite; I-type intrusion. GSV map code: G466.||||||07-FEB-11
69420|Parslow Diorite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Kaersutite-augite diorite: medium-grained, equigranular; metamorphosed; contains plagioclase, kaersutite, augite, quartz, apatite; metamorphic epidote, actinolite, chlorite, sphene, probable albite; I-type intrusion. GSV map code: G466.||||||
69420|Parslow Diorite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Kaersutite-augite diorite: medium-grained, equigranular; metamorphosed; contains plagioclase, kaersutite, augite, quartz, apatite; metamorphic epidote, actinolite, chlorite, sphene, probable albite; I-type intrusion. GSV map code: G466.||||||
69420|Parslow Diorite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Kaersutite-augite diorite: no gravity data; nonmagnetic (0 nT, k < 1 x10^-6 cgs); moderate K, moderate to high Th, U and total radioelements. GSV map code: G466.||||||
69420|Parslow Diorite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Silurian||||||Kaersutite-augite diorite: medium-grained, equigranular; metamorphosed; contains plagioclase, kaersutite, augite, quartz, apatite; metamorphic epidote, actinolite, chlorite, sphene, probable albite.|
37250|Patawilya Tonalite|24012|3|Fully described|p223 appendix 1|||||||||
37250|Patawilya Tonalite|50154|2|Defined|p90-91, p247 App.5|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex.||||||15-SEP-04
37250|Patawilya Tonalite|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Biotite-muscovite tonalite||||||
37250|Patawilya Tonalite|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite tonalite.||||||20-AUG-04
37250|Patawilya Tonalite|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite tonalite.||||||20-AUG-04
37250|Patawilya Tonalite|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite tonalite.||||||20-AUG-04
37250|Patawilya Tonalite|50159|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite tonalite.||||||20-AUG-04
37250|Patawilya Tonalite|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite tonalite.||||||20-AUG-04
37250|Patawilya Tonalite|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite tonalite.||||||20-AUG-04
37250|Patawilya Tonalite|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite tonalite.||||||20-AUG-04
37250|Patawilya Tonalite|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-muscovite tonalite.||||||20-AUG-04
37250|Patawilya Tonalite|66002|6|Mentioned|p9 Tb.5|||G443. Defined by Kemp et al. 2002||||||
37250|Patawilya Tonalite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Biotite-muscovite tonalite: massive, light grey-buff, medium to coarse grained, equigranular; accessory magnetite, epidote and chalcopyrite; common mafic biotite-rich microgranitoid enclaves; magnetic to weakly magnetic.|
83407|Patho pluton|73496|5|Briefly described|Map legend|Late Devonian|Late Devonian|G751.|||||Weakly reversely magnetised with response about 10 nT below surrounding rocks;  where subcropping gravity response about 5 micrometres/second/second below surroundings but part of a broader 70 micrometres per second squared low.|
83407|Patho pluton|73497|5|Briefly described|Map legend|Late Devonian|Late Devonian|G751.|||||Granite: nonmagnetic, moderately magnetic metamorphic aureole (20 nT); estimated depth of 600-665 m.|
14994|Pebble Point Formation|12781|6|Mentioned|p386|Paleocene|Paleocene|Otway Basin. Maximum thickness 90m.||Wangerip Group.||Overlies Paaratte Formation conformably and Timboon Sandstone unconformably. Is overlain by Pember Mudstone.||
14994|Pebble Point Formation|12796|5|Briefly described|p456 Fig. 2|Thanetian|Danian|Informally divided into Upper and Lower Pebble Point Formation. Overlies Massacre Shale; underlies Pember Mudstone. Geological Province: Otway Basin.||||||
14994|Pebble Point Formation|22587|6|Mentioned|p79 Fig.7|Middle Miocene|Late Paleocene|||||||
14994|Pebble Point Formation|22674|5|Briefly described|Fig.2 p719|Early Paleocene|Maastrichtian|||||||
14994|Pebble Point Formation|22875|5|Briefly described|p14|Late Paleocene|Late Cretaceous|Of the Wangerrip Group.||||||30-JAN-07
14994|Pebble Point Formation|22944|5|Briefly described|Fig3|Paleocene|Paleocene|||||||
14994|Pebble Point Formation|23230|4|Described|Table4-1p40, 41|Paleocene||||||||
14994|Pebble Point Formation|23307|5|Briefly described|Map Legend|Paleocene|Paleocene|Of Wangerrip Group.||||||24-JUL-08
14994|Pebble Point Formation|23322|5|Briefly described|957 Fig.2|Eocene|Paleocene|Of the Wangerrip Group. Geological Province: Gambier Basin.||||||07-SEP-09
14994|Pebble Point Formation|23671|6|Mentioned|p2|Paleocene|Paleocene|||||||
14994|Pebble Point Formation|23768|6|Mentioned|p14, p19|Paleocene|Paleocene|See also p22, and p37.||||||
14994|Pebble Point Formation|23778|6|Mentioned|p668|||Geological Province: Otway Basin.||||||
14994|Pebble Point Formation|24038|5|Briefly described|p439 Fig.2|Paleocene|Paleocene|Geological Province: Torquay Basin||||||
14994|Pebble Point Formation|24056|5|Briefly described|p85|Paleocene|Paleocene|Of Wangerrip Group. Geological Basin: Otway Basin.||||||24-JUL-08
14994|Pebble Point Formation|24202|5|Briefly described|p313 Fig. 2|Late Paleocene|Early Paleocene|Of the Wangerrip Group. Geological Province: Gambier Sub-basin.||||||24-JUL-08
14994|Pebble Point Formation|24314|5|Briefly described|p61 Fig.2|Paleocene||Geological Province: Otway Basin. Max. Thickness 90m. Of the Wangerrip Group.||||||30-NOV-04
14994|Pebble Point Formation|24455|5|Briefly described|p327|Late Paleocene|Paleocene|Contains fossil molluscs. Conformably overlain by Dilwyn Formation;  transgressively overlaps the Otway Group. Age is Middle Paleocene to Late Paleocene. Geological Province: Otway Basin. See also p321 Fig. 1.||||||24-JUL-08
14994|Pebble Point Formation|24551|5|Briefly described|p246, 292 Fig. 10.3|Paleocene|Paleocene|Of the Wangerrip Group.||||||
14994|Pebble Point Formation|24562|5|Briefly described|p8 Fig. 2|Paleocene|Paleocene|Of the Wangerrip Group. Geological Province: Otway Basin.||||||24-JUL-08
14994|Pebble Point Formation|29355|6|Mentioned|p185|||||||||
14994|Pebble Point Formation|29823|6|Mentioned|p14|||||||||
14994|Pebble Point Formation|29856|6|Mentioned|p40|||||||||
14994|Pebble Point Formation|30244|6|Mentioned|p153|||Palaeocene age||||||
14994|Pebble Point Formation|30454|6|Mentioned|Fig.1|||||||||
14994|Pebble Point Formation|30576|5|Briefly described|Table 2|||||||||
14994|Pebble Point Formation|30578|4|Described|p8|||||||||
14994|Pebble Point Formation|30675|5|Briefly described|p253|||Lithology and radioactivity.||||||24-JUL-08
14994|Pebble Point Formation|30905|6|Mentioned|p149|||||||||
14994|Pebble Point Formation|30932|6|Mentioned|Map legend|Paleocene|Paleocene|Equivalent to Bahgallah Formation. Part of Wangerrip Group.||||||
14994|Pebble Point Formation|31036|1|Redefined|p207|Tertiary|Tertiary|See also p194, Table 9-1.||||||30-JAN-07
14994|Pebble Point Formation|31245|6|Mentioned|p68|||M. Palaeocene. Fauna. Wangerrip Gp.||||||
14994|Pebble Point Formation|31246|6|Mentioned|p54|||Palaeocene||||||
14994|Pebble Point Formation|31372|6|Mentioned|p2|||See also p9.||||||30-JAN-07
14994|Pebble Point Formation|31424|4|Described|p17|||See also p7. Described from core.||||||30-JAN-07
14994|Pebble Point Formation|31514|6|Mentioned|p44|||Shown on Table. Refers McGowran (1965).||||||
14994|Pebble Point Formation|31534|6|Mentioned|p363|||See also Table 19-3||||||
14994|Pebble Point Formation|31624|6|Mentioned|p99|||M.Palaeocene. Synonymous with Bahgallah Fm.||||||
14994|Pebble Point Formation|31625|6|Mentioned|Fig. 5.2|||Palaeocene||||||
14994|Pebble Point Formation|31714|6|Mentioned|p32|||||||||
14994|Pebble Point Formation|31920|6|Mentioned|p55|||M.Palaeocene||||||
14994|Pebble Point Formation|31922|6|Mentioned|Fig.2|||||||||
14994|Pebble Point Formation|32115|4|Described|p1|||See also Fig.1||||||
14994|Pebble Point Formation|32117|6|Mentioned|p84|||||||||
14994|Pebble Point Formation|32120|6|Mentioned|p274|||Palaeocene, fauna||||||
14994|Pebble Point Formation|32344|6|Mentioned|Fig.2|||||||||
14994|Pebble Point Formation|32852|6|Mentioned|p10|||||||||
14994|Pebble Point Formation|32898|6|Mentioned|Table 2-1|||||||||
14994|Pebble Point Formation|33319|6|Mentioned|p167|||Fauna.||||||
14994|Pebble Point Formation|33321|6|Mentioned|p238|||||||||
14994|Pebble Point Formation|33412|6|Mentioned|p218|||M.Palaeocene.||||||
14994|Pebble Point Formation|33940|6|Mentioned|p414|||||||||
14994|Pebble Point Formation|34063|6|Mentioned|p2|||Paleocene. Table||||||
14994|Pebble Point Formation|34172|6|Mentioned|p55|||||||||
14994|Pebble Point Formation|34343|5|Briefly described|p96|||Middle Paleocene||||||
14994|Pebble Point Formation|34987|6|Mentioned|p170|||||||||
14994|Pebble Point Formation|34988|6|Mentioned|Table 9.4|||||||||
14994|Pebble Point Formation|35066|3|Fully described|p203|||||||||
14994|Pebble Point Formation|35285|6|Mentioned|p414|||||||||
14994|Pebble Point Formation|36305|6|Mentioned|p358|||||||||
14994|Pebble Point Formation|36366|3|Fully described|p1|||||||||
14994|Pebble Point Formation|36913|6|Mentioned|p81|||||||||
14994|Pebble Point Formation|37062|6|Mentioned|p179|||||||||
14994|Pebble Point Formation|37548|6|Mentioned|p129|||||||||
14994|Pebble Point Formation|38221|6|Mentioned|p348|||||||||
14994|Pebble Point Formation|38625|6|Mentioned|Table 2|||||||||
14994|Pebble Point Formation|38738|6|Mentioned|p263|||||||||
14994|Pebble Point Formation|40003|5|Briefly described|p44|||See also Fig.10||||||
14994|Pebble Point Formation|40560|6|Mentioned|p4|||||||||
14994|Pebble Point Formation|41016|5|Briefly described|Table 1|||||||||
14994|Pebble Point Formation|41043|6|Mentioned|p95|||||||||
14994|Pebble Point Formation|41075|6|Mentioned|p11|||||||||
14994|Pebble Point Formation|41185|6|Mentioned|p178|||||||||
14994|Pebble Point Formation|41230|6|Mentioned|p127|||||||||
14994|Pebble Point Formation|41269|5|Briefly described|p246|||||||||
14994|Pebble Point Formation|41642|6|Mentioned|p219|||||||||
14994|Pebble Point Formation|41701|6|Mentioned|Map legend|Eocene||||||||
14994|Pebble Point Formation|41704|6|Mentioned|Fig.3|||||||||
14994|Pebble Point Formation|41714|6|Mentioned|p301|||||||||
14994|Pebble Point Formation|41726|5|Briefly described|p421|||||||||
14994|Pebble Point Formation|41769|4|Described|p18|||||||||
14994|Pebble Point Formation|41868|4|Described|p534|||||||||
14994|Pebble Point Formation|42079|6|Mentioned|Fig.2 P264|||||||||
14994|Pebble Point Formation|42152|5|Briefly described|p15|||||||||
14994|Pebble Point Formation|42318|5|Briefly described|p8|||||||||
14994|Pebble Point Formation|42361|6|Mentioned|p17|||||||||
14994|Pebble Point Formation|42453|6|Mentioned|p11|||Port Campbell Embayment||||||
14994|Pebble Point Formation|42524|5|Briefly described|Fig.3 P27|||||||||
14994|Pebble Point Formation|42555|5|Briefly described|Fig.2 P285|||||||||
14994|Pebble Point Formation|42599|6|Mentioned|p618|||||||||
14994|Pebble Point Formation|42827|4|Described|p277|||see also Fig 8.7||||||
14994|Pebble Point Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
14994|Pebble Point Formation|43052|5|Briefly described|Table 2.1|||||||||
14994|Pebble Point Formation|43171|6|Mentioned|5-8|||Of Wangerrip Group. Age: 55-65Ma||||||
14994|Pebble Point Formation|43195|5|Briefly described|Map Legend|Eocene|Paleocene|See also commentary on back of map. Of Wangerrip Group.||||||
14994|Pebble Point Formation|43208|5|Briefly described|map legend|Late Paleocene|Maastrichtian|Of Maastrichtian - Late Palaeocene age. Of Wangerrip Group.||||||24-JUL-08
14994|Pebble Point Formation|43219|5|Briefly described|Fig.3,p6.|Paleocene|Maastrichtian|Of Wangerrip Group.||||||30-JAN-07
14994|Pebble Point Formation|43493|6|Mentioned|32||Tertiary|||||||
14994|Pebble Point Formation|43590|14|Not recorded|p16|Paleocene|Late Cretaceous|||||||
14994|Pebble Point Formation|43660|6|Mentioned|Fig.6,p15||Paleocene|||||||
14994|Pebble Point Formation|43733|6|Mentioned|Fig.2.11,p65||Paleocene|||||||
14994|Pebble Point Formation|43744|6|Mentioned|Fig.3,p3|||||||||
14994|Pebble Point Formation|43814|6|Mentioned|Fig.3,p115|||||||||
14994|Pebble Point Formation|43937|5|Briefly described|Map Legend|Paleocene|Santonian|||||||
14994|Pebble Point Formation|44133|4|Described|p154|Early Eocene|Late Paleocene|Of the Wangerrip Group. Geological Province: Gambier Basin. Unconformably overlies Sherbrook Group. Thickness: 40m.||||||30-JAN-07
14994|Pebble Point Formation|44677|14|Not recorded|p6|||Amosopollis.||||||
14994|Pebble Point Formation|47054|6|Mentioned|p491|||||||||
14994|Pebble Point Formation|48581|14|Not recorded|p14|||||||||
14994|Pebble Point Formation|48911|3|Fully described|p23|||Middle - Upper Palaeocene.||||||
14994|Pebble Point Formation|48977|6|Mentioned|Fig.5|||||||||
14994|Pebble Point Formation|60538|5|Briefly described|p474 Fig. 13|||Geological Province: Otway Basin.||||||
14994|Pebble Point Formation|60563|5|Briefly described|p45 Fig. 1, p46|||Estuarine channel sandstones. Overlain by the Pember Mudstone Member of the Dilwyn Formation.||||||16-JUN-05
14994|Pebble Point Formation|60599|5|Briefly described|p84|Late Cretaceous|Late Cretaceous|Of the Wangerrip Group. Geological Province:Otway  Basin.||||||
14994|Pebble Point Formation|61016|6|Mentioned|p13|||See also Pebble Point formation. Geological Province: Otway Basin.||||||20-APR-05
14994|Pebble Point Formation|61017|5|Briefly described|p5|Selandian|Danian|Of the Wangerrip Group. Geological Province: Otway Basin.||||||07-FEB-11
14994|Pebble Point Formation|61155|5|Briefly described|p2, p18|Early Paleocene|Early Paleocene|Paralic to shallow-marine iron-rich oolitic sediments.Overlain by Eastern View and Dilwyn Formations and by Pember Mudstone. Overlies Timboon Sand Member (Sherbrook Group). Max. thickness: 150m. Geological Province: Otway Basin, Torquay Basin.||||||30-JAN-07
14994|Pebble Point Formation|61182|3|Fully described|p19-20, p32, p89|Maastrichtian|Maastrichtian|Of Wangerrip Gp. Overlies Eumeralla Fm; disconform.on Timboon Sand Member (Paaratte Fm) in west. Capped by Pember Mudstone. Grades lat. into Moomowroong Sand. Max.thick:158m. Geol.Prov:Otway Basin. Moomowroong Sand, Wiridjil Gravel = lateral equivs. ||||||
14994|Pebble Point Formation|61185|5|Briefly described|p57|Tertiary|Tertiary|Of the Wangerrip Group. Contain large river-rounded lithic cobbles. Age: ~65Ma. Geol. Prov: Otway Basin.||||||07-FEB-11
14994|Pebble Point Formation|61470|5|Briefly described|p28 Fig. 5|Selandian|Danian|Of the Wangerrip Group. Overlain by and interfingered with Pember Mudstone.  Geological Province: Otway Basin.||||||12-OCT-05
14994|Pebble Point Formation|61547|6|Mentioned|p461 Fig.2. |Paleocene|Paleocene|||Unit in Wangerrip Group.||Overlies Paaratte Formation and Timboon Sandstone.||
14994|Pebble Point Formation|61622|5|Briefly described|p436 Fig. 2|Paleocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-FEB-11
14994|Pebble Point Formation|61623|6|Mentioned|p449 Fig. 4|Paleocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-APR-09
14994|Pebble Point Formation|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4|Paleocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-APR-09
14994|Pebble Point Formation|61627|5|Briefly described|p500 Fig. 2|Paleocene|Paleocene|Of Wangerrip Group. Overlian by Pember Mudstone. Geological Province: Otway Basin.||||||07-FEB-11
14994|Pebble Point Formation|61628|5|Briefly described|p509 Fig. 3|Paleocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-APR-09
14994|Pebble Point Formation|62896|5|Briefly described|p88|Late Paleocene|Late Paleocene|Geological Province: Otway Basin.||||||07-FEB-11
14994|Pebble Point Formation|63122|5|Briefly described|p17 Fig. 4.3|Late Paleocene|Early Paleocene|Of the Wangerrip Group. Max. thickness: 90m. Geological Province: Otway Basin. ||||||
14994|Pebble Point Formation|63124|3|Fully described|p49 Fig. 5.2, p87 Fig. 5.29, p88|Early Eocene|Late Paleocene|Previously referred to as Bahgallah Formation in South Australia. Of the Wangerrip Group. Unconformable on Sherbrook Group; conformably overlain by Pember Mudstone. Age: 55-51Ma. Max. thickness: 90m. Geological Province: Otway Basin.||||||
14994|Pebble Point Formation|63129|5|Briefly described|p137|Early Tertiary|Early Tertiary|Geological Province: Otway Basin. May act as a regional seal, and together with Pember Mudstone is the only seal for the condensed Sherbrook Group. ||||||
14994|Pebble Point Formation|63130|5|Briefly described|p143|||Geological Province: Otway Basin.||||||04-FEB-08
14994|Pebble Point Formation|63269|5|Briefly described|p605-607|Paleocene|Paleocene|Otway Basin. Contains a marginally-mature oil stain thought to be sourced from Sherbrook Group. Details of oils and oil stains in named wells tabulated.||Wangerrip Group.||||
14994|Pebble Point Formation|63431|5|Briefly described|p677 Fig. 2|Paleocene|Paleocene|Basal unit of the Wangerrip Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
14994|Pebble Point Formation|63740|5|Briefly described|p88, p92|Paleocene|Paleocene|Geological province: Otway Basin.||||||07-FEB-11
14994|Pebble Point Formation|66002|5|Briefly described|p10 Tb.7, p10 Tb.8|Paleogene|Paleogene|Of Wangerrip Group. Defined by Tickell et al 1992.||||||
14994|Pebble Point Formation|66245|5|Briefly described|p6 Fig.5. |Selandian|Danian|||Unit in Wangerrip Group.||Is overlain by Pember Mudstone.||
14994|Pebble Point Formation|67061|5|Briefly described|p545, p546 Fig.3.|Paleocene|Paleocene|Otway Basin. Coal measures and underlying mudstones and sandstones in this unit have sedimentological and stratigraphic affinities with similar facies in onshore Eastern View Group (Torquay Sub-basin). ||Unit in Wangerrip Group.||||
14994|Pebble Point Formation|67366|5|Briefly described|p103 Fig.2. |Paleocene|Paleocene|||Unit in Wangerrip Group.||Overlies Massacre Shale. Is overlain by Pember Mudstone.|Shallow to nearshore marine sandstone and shale.|
14994|Pebble Point Formation|67367|5|Briefly described|p131 Fig.2, pp132-133. |Late Paleocene|Early Paleocene|Contains oils derived from terrestrial, land-plant material; subjected to extensive microbial alteration and water washing.||Unit in Wangerrip Group.||||
14994|Pebble Point Formation|68116|5|Briefly described|Appendix, Maps 54-55.|Paleocene|Paleocene||||||Quartz sand, minor clay: micaceous, fine-grained, friable, generally massive; minor planar cross-bedding; minor gravel, minor volcanic and metamorphic lithic cobbles and pebbles; near shore, shallow marine deposits.|
14994|Pebble Point Formation|69297|5|Briefly described|p79|Thanetian|Maastrichtian|Otway Basin. See Pebble Point Formation, Lower and Upper. ||Wangerrip Group||Overlies the Timboon Sandstone and the Massacre Shale. Overlain by the Dilwyn Formation. ||
14994|Pebble Point Formation|69651|5|Briefly described|p10|Paleocene|Paleocene|||Wangerrip, Nirranda Groups [?].||Abuts Eastern View Formation. Is overlain by Pember Mudstone.||
14994|Pebble Point Formation|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4; p5, p7-8|Paleocene|Paleocene|Otway Basin. Shallow marine to coastal depositional environments. An Austral 2 Petroleum System oil show, in Wilson 1, was possibly sourced from Belfast Mudstone. Is sealed by Pember Mudstone.||Wangerrip Group.||Overlies Massacre Shale or Timboon Sandstone. Is overlain by Pember Mudstone.||
14994|Pebble Point Formation|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Paleocene|Paleocene|Gambier Embayment and Voluta Trough.||Wangerrip Group.||Overlies Massacre Shale. Is overlain by Pember Mudstone.||
14994|Pebble Point Formation|70193|6|Mentioned|p285 fig 3|||See also p284 Fig 2 where informally divided into upper and lower parts.||||||
14994|Pebble Point Formation|70880|6|Mentioned|p77|Paleocene|Maastrichtian|Otway Basin.||||||
14994|Pebble Point Formation|71266|6|Mentioned|p614 Fig.3|Paleocene|Late Cretaceous|Otway Basin.||||||
14994|Pebble Point Formation|71437|4|Described|Fig. 1 opp 154,  p155, p158-159|Paleocene|Paleocene|Important marker horizon heralding onset of neritic marine conditions. Compared with Flaxman Formation.||Of Wangerrip Group.||Transitional with Pember Mudstone Member of Dilwyn Formation.|Glauconitic sandy dolomite, sand and gravel, minor conglomerate and mudstone.|
14994|Pebble Point Formation|73357|5|Briefly described|p25-26, p44, p46, p48|Thanetian|Danian|Otway Basin. Correlated with multiple biozones including Lygistepollenites balmei Spore-Pollen Zone, typically marginal to nearshore marine depositional environments. Lower part coincides with Alisocysta circumtabulata Dinocyst Zone.||Of Wangerrip Group?||Overlies K/Pg Boundary Shale, underlies Pember Mudstone.||
14994|Pebble Point Formation|73383|5|Briefly described|p3, p10 Tb.3.7, p21, p24, p27, p265-266|Paleocene|Paleocene|Otway Basin. Equivalent to chemostratigraphic package S5-P8 continaing high Th/K, Fe and P values. Lithologies based on geochemistry using the ChemLith classification include argillaceous and calcareous sandstones, limestone, calcareous limestone, and mudstone; and using the Herron classification (1988) includes quartz arenite, Fe-shale, Fe-sand, sublith-arenite. See also vi, p11 Tb.3.9, p66-67, p83, p118-119, p131, p138-140, p199, p214, p247, p258.||Wangerrip Group||Overlies Sherbrook Group, underlies Pember Mudstone|Sandstones. Can be oolitic in parts and contains fossiliferous material.|
14994|Pebble Point Formation|73385|5|Briefly described|p5|Paleocene|Paleocene|Otway Basin.||Wangerrip Group||Overlies Sherbrook Group, underlies Pember Mudstone.|Shallow marine and nearshore sandstones.|
14994|Pebble Point Formation|73386|4|Described|p4, p6, p12, Attachment A1|Paleocene|Paleocene|Otway Basin. Deposited during a regression, forming a lowstand-transgressive systems tract, resulting in a blanket of marginal marine beach and inner shelf sandstones. Downlapped by a strongly prograding series of deltaic sequences dominated by the landward Dilwyn Formation facies and basinward Pember Mudstone facies. Onshore, the formation is thin with a sheet-like geometry, fines upwards into Pember Mudstone. Occurs within the Lower Lygistepollenites balmei Spore-Pollen Subzone.||Wangerrip Group||Overlies Cretaceous/Paleogene boundary shale, underlies Pember Mudstone|Consists of carbonaceous sandy claystones, granule conglomerate and fine to coarse-grained quartz sandstone.|
14994|Pebble Point Formation|73594|5|Briefly described|p4, p45 Fig.5.19|Paleocene|Paleocene|Otway Basin.||Wangerrip Group||Underlies Pember Mudstone|Shallow marine and nearshore sandstones.|
28194|Pember Mudstone Member|22587|6|Mentioned|p79 Fig.7|Early Eocene||||||||
28194|Pember Mudstone Member|22875|5|Briefly described|p26 Table1|||||||||
28194|Pember Mudstone Member|24551|5|Briefly described|p292 Fig. 10.3|||||||||
28194|Pember Mudstone Member|30576|5|Briefly described|Table 2|||||||||
28194|Pember Mudstone Member|30578|6|Mentioned|Table 1|||See also Table 2.||||||
28194|Pember Mudstone Member|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
28194|Pember Mudstone Member|30675|5|Briefly described|p253|||Lithology and radioactivity.||||||27-SEP-07
28194|Pember Mudstone Member|30932|6|Mentioned|Map legend|Eocene|Paleocene|Paleocene - Eocene||||||
28194|Pember Mudstone Member|31036|1|Redefined|p209|Tertiary|Tertiary|See also Table 9-1. Unit of Dilwyn Fm.||||||
28194|Pember Mudstone Member|31372|4|Described|p14|||See also p2, p9.||||||24-JAN-08
28194|Pember Mudstone Member|31424|4|Described|p16|||See also p7. Described from a core.||||||24-JAN-08
28194|Pember Mudstone Member|31922|6|Mentioned|Fig.2|||||||||
28194|Pember Mudstone Member|32852|6|Mentioned|p10|||||||||
28194|Pember Mudstone Member|33940|6|Mentioned|p415|||||||||
28194|Pember Mudstone Member|34360|6|Mentioned|p11|||||||||
28194|Pember Mudstone Member|34988|6|Mentioned|Table 9.4|||||||||
28194|Pember Mudstone Member|35066|6|Mentioned|p205|||||||||
28194|Pember Mudstone Member|36366|5|Briefly described|p3|||||||||
28194|Pember Mudstone Member|37548|5|Briefly described|p129|||||||||
28194|Pember Mudstone Member|41701|6|Mentioned|Map legend|Eocene||||||||
28194|Pember Mudstone Member|41714|6|Mentioned|p301|||||||||
28194|Pember Mudstone Member|41726|6|Mentioned|p421|||See also p427.||||||27-SEP-07
28194|Pember Mudstone Member|41769|4|Described|p23|||||||||
28194|Pember Mudstone Member|42318|6|Mentioned|Fig.2 P10|||||||||
28194|Pember Mudstone Member|42827|5|Briefly described|p280|||Of the Dilwyn Formation.||||||24-JAN-08
28194|Pember Mudstone Member|48911|6|Mentioned|Chart 1|||||||||
28194|Pember Mudstone Member|60563|5|Briefly described|p45 Fig.1, p47|||Of the Dilwyn Formation. Offshore marine deposits.||||||
28194|Pember Mudstone Member|61182|6|Mentioned|p22|||Of Glenie (1965) - introduced this name when he changed Dilwyn Clay to Dilwyn Formation -- for lower part of the formation. In this study Pember Mudstone stands superseded as separate formation.||||||27-SEP-07
28194|Pember Mudstone Member|62896|5|Briefly described|p90 Tb. 1|Late Paleocene|Late Paleocene|See also Pember Mudstone. Of Dilwyn Formation (Wangerrip Group).||||||07-FEB-11
28194|Pember Mudstone Member|63740|5|Briefly described|p89, p90 Tb. 1|Early Eocene|Late Paleocene|Shown as a unit of Wangerrip Group in Table 1 (p90) where it is overlain by the Dilwyn Formation. See also Pember Mudstone - names used interchangeably in study.||||||07-FEB-11
28194|Pember Mudstone Member|65715|5|Briefly described|p11 Tb.7|Paleogene|Paleogene|Of Dilwyn Formation.||||||
28194|Pember Mudstone Member|66002|5|Briefly described|p10 Tb.7,|Paleogene|Paleogene|Of Dilwyn Formation. Defined by Glenie 1971.||||||23-MAY-13
28194|Pember Mudstone Member|71437|5|Briefly described|Fig. 1 opp 154,  p155, p159|Paleocene|Paleocene|||Of Dilwyn Formation.||Transitional contact with underlying Pebble Point Formation, overlying Dilwyn Formation.|Mudstone.|
30689|Penderlea Granite|23309|6|Mentioned|p441 App1|||G83 S-Type.||||||
30689|Penderlea Granite|60503|5|Briefly described|p151,  p44 Tb. 2|Silurian|Silurian|Small granite intrusion north of Lake Omeo. Deeply weathered granite. See also p25.||||||
30689|Penderlea Granite|60504|5|Briefly described|Map Legend|Wenlock|Wenlock|Granitic intrusive of uncertain composition: S-type?; weathered granite and granitic soil.||||||
30689|Penderlea Granite|60505|5|Briefly described|Map legend|Wenlock|Wenlock|Granitic intrusive of uncertain composition: S-type?; weathered granite and granitic soil.||||||
30689|Penderlea Granite|60506|5|Briefly described|Map legend|Wenlock|Wenlock|Granitic intrusive of uncertain composition: S-type?; weathered granite and granitic soil.||||||
30689|Penderlea Granite|60507|5|Briefly described|Map Legend|Wenlock|Wenlock|Granitic intrusive of uncertain composition: S-type?; weathered granite and granitic soil.||||||
30689|Penderlea Granite|60508|5|Briefly described|Map legend|Early Silurian|Early Silurian|Granite: S-type(?); nonmagnetic (0-5 nT) with moderately magnetic (20-30 nT) dykes||||||
30689|Penderlea Granite|68116|5|Briefly described|Appendix, Map 27.|Wenlock|Llandovery||||||Granitic rock of uncertain composition: weathered granite and granitic soil.|
79641|Pental pluton|68116|5|Briefly described|Appendix|Middle Devonian|Early Devonian|GSV G624.|||||Granite: distinguished by geophysical response; very poorly subcropping|
77104|Pentland Hills Volcanic Group|65715|5|Briefly described|p11 Tb.7, p13|Paleogene|Paleogene|Formerly Older Volcanics.||||||
77104|Pentland Hills Volcanic Group|68116|5|Briefly described|Appendix, Map 41.|Eocene|Paleocene||||||Alkali olivine basalt to nephelinite, minor tuff: dark grey; fine-grained; rarely vesicular; secondary calcite and magnesite in vesicles and joints.|
30287|Percydale Granite|22968|5|Briefly described|P90, P223||Triassic|Intruded Tea Pot Creek Formation and Mount Tambo Group, moderately magnetic||||||
30287|Percydale Granite|23021|5|Briefly described|Map legend|Triassic|Triassic|Parent is Mount Leinster Igneous Complex||||||
30287|Percydale Granite|23029|5|Briefly described|Map legend|Triassic|Triassic|Parent is the Mount Leinster Igneous Complex||||||
30287|Percydale Granite|23030|5|Briefly described|Map legend|Triassic|Triassic|Parent is the Mount Leinster Igneous Complex||||||
30287|Percydale Granite|60503|3|Fully described|p185, p40 Tb. 2|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Formerly included in Sisters Granite. Quartz-feldspar porphyry with reddish coloured fine groundmass; strongly porphyritic. Intrudes the Teapot Creek Formation and Mount Tambo Group.||||||16-NOV-09
30287|Percydale Granite|60504|5|Briefly described|Map Legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Granite: A-type; grey to red, strongly porphyritic in quartz and feldspar, groundmass ranges from glassy to equigranular.||||||
30287|Percydale Granite|60505|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Granite: A-type; grey to red, strongly porphyritic in quartz and feldspar, groundmass ranges from glassy to equigranular.||||||
30287|Percydale Granite|60506|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Granite: A-type; grey to red, strongly porphyritic in quartz and feldspar, groundmass ranges from glassy to equigranular.||||||
30287|Percydale Granite|60507|5|Briefly described|Map Legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Granite: A-type; grey to red, strongly porphyritic in quartz and feldspar, groundmass ranges from glassy to equigranular.||||||13-OCT-04
30287|Percydale Granite|60508|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Granite: A-type; weakly magnetic (0-20 nT), more magnetic (50 nT) on western and northern margins; high total count, K, moderate Th, U||||||21-OCT-04
30287|Percydale Granite|68116|5|Briefly described|Appendix, Maps 27, 35.|Triassic|Triassic||||||Granite: grey to red, strongly porphyritic in quartz and feldspar, groundmass ranges from glassy to equigranular with rare biotite and fluorite.|
83406|Perricoota pluton|73496|5|Briefly described|Map legend|Late Devonian|Late Devonian|G659.|||||Nonmagnetic but with magnetic contact aureole to 40 nT;  gravity low to 200 micrometres/second/second below the regional.|
83406|Perricoota pluton|73497|5|Briefly described|Map legend|Late Devonian|Late Devonian|G659.|||||Nonmagnetic but with magnetic contact aureole to 40 nT; gravity low to 300 micrometres/second/second below the regional may be partly due to possible Permian and Cenozoic cover.|
83406|Perricoota pluton|73505|6|Mentioned|p7, p9|Devonian|Devonian|Newly named unit in Swan Hill and parts of Balranald and Deniliquin 1:250 000 map areas, (G659). Named after Pericoota State Forest. Distribution is north of the Governor Fault, largely overlain by the Numurkah Trough. Nonmagnetic but with magnetic contact metamorphic rim. Gravity response of 150 micrometres/second/second gravity low, partly from overlying Numurkah Trough. Interpreted to have intruded Devonian sediments. See also Percoota pluton, Pericoota pluton.||||||
15110|Peterborough Member|35066|5|Briefly described|p213|||||||||
15110|Peterborough Member|42827|6|Mentioned|p288|||Of Port Campbell Limestone.||||||07-MAR-07
15110|Peterborough Member|43590|6|Mentioned|p26|||||||||
15110|Peterborough Member|48911|6|Mentioned|Chart 1|||||||||
15110|Peterborough Member|61182|6|Mentioned|p29|||Of Baker (1953). Of the Port Campbell Limestone and now incorporated into it; not recognised elsewhere. Also previously referred to as Peterborough beds.||||||
15134|Pheasant Creek Granite|23309|5|Briefly described|p441, App1|||G138 I-Type.||||||
15134|Pheasant Creek Granite|42726|5|Briefly described|map legend|||586. NOT variation on Pheasant Creek Volcanics, NSW.||||||
15134|Pheasant Creek Granite|61160|6|Mentioned|p137|||Superseded by Allwood Granodiorite on the CORRYONG sheet.||||||01-FEB-07
69422|Phipps Granite|61161|5|Briefly described|p76-77 Fig 6.1, p106-107|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Nonmagnetic, homogeneous, equigranular, pink, medium to coarse-grained, massive leucogranite. Intruded Omeo Metamorphic Complex migmatite. Age: inferred Early Devonian. GSV map code: G460.||||||
69422|Phipps Granite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite leucogranite: cream to pink; equigranular medium-grained; unfoliated; contains plagioclase, orthoclase, biotite, rare muscovite; unassigned intrusion. GSV map code: G460.||||||
69422|Phipps Granite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite leucogranite: cream to pink; equigranular medium-grained; unfoliated; contains plagioclase, orthoclase, biotite, rare muscovite; unassigned intrusion. GSV map code: G460.||||||07-FEB-11
69422|Phipps Granite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite leucogranite: cream to pink; equigranular medium-grained; unfoliated; contains plagioclase, orthoclase, biotite, rare muscovite; unassigned intrusion. GSV map code: G460.||||||
69422|Phipps Granite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite. Biotite leucogranite: cream to pink; equigranular medium-grained; unfoliated; contains plagioclase, orthoclase, biotite, rare muscovite; unassigned intrusion. GSV map code: G460.||||||
69422|Phipps Granite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Boggy Plain Supersuite. Biotite leucogranite: no gravity data; nonmagnetic (k < 1 x10^-6 cgs); moderate to high K and total radioelements, moderate Th, low U. GSV map code: G460.||||||
69422|Phipps Granite|68116|5|Briefly described|Appendix, Map 35.|Devonian|Silurian||||||Biotite leucogranite: cream to pink; equigranular medium-grained; unfoliated; contains plagioclase, orthoclase, biotite, rare muscovite.|
74885|Phosphate Hill Formation|64536|5|Briefly described|Map legend|Late Ordovician|Middle Ordovician|Chert, siltstone, black shale, phosphorite: chert and phosphorite brown and grey, thinly bedded; phosphorite medium to coarse sand-sized; dark green-grey; contains Early Ordovician graptolites. Deep-marine hemipelagic deposits.||||||23-JUN-14
74885|Phosphate Hill Formation|64537|5|Briefly described|Map legend|Late Ordovician|Middle Ordovician|Chert, siltstone, black shale, phosphorite: chert and phosphorite brown and grey, thinly bedded; phosphorite medium to coarse sand-sized; dark green-grey; contains Early Ordovician graptolites. Deep-marine hemipelagic deposits.||||||23-JUN-14
74885|Phosphate Hill Formation|64538|5|Briefly described|Map legend|Late Ordovician|Middle Ordovician|Chert, siltstone, black shale, phosphorite: chert and phosphorite brown and grey, thinly bedded; phosphorite medium to coarse sand-sized; dark green-grey; contains Early Ordovician graptolites. Deep-marine hemipelagic deposits.||||||23-JUN-14
74885|Phosphate Hill Formation|64606|5|Briefly described|Map Legend|Cambrian|Cambrian|Chert, siltstone, black shale, phosphorite: deep-marine deposits. Blue-pink in RGB. Nonmagnetic. Small outcrop intersected by single flight line.||||||
74885|Phosphate Hill Formation|64616|4|Described|p66, p156 Fig.6.5, p182-184|Floian|Tremadocian|See also p197 Fig.6.34, p254, p278, p306. New name. All exposed contacts, eg against Mount Easton Shale, are faulted. Age well constrained by graptolites - Lancefieldian (~487-476 Ma). Thickness prob. < 100 m. Thinly bedded black chert, siliceous grey-green shale, siltstone and interbeds of grey phosphorite (bioclastic sandstones) which were locally mined near Mansfield. Complexly folded and faulted. Geophysical characteristics given.||||||
74885|Phosphate Hill Formation|65900|6|Mentioned|p155||Early Ordovician|Melbourne Zone. Lower Ordovician unit.||||||10-MAY-12
74885|Phosphate Hill Formation|68116|5|Briefly described|Appendix, Maps 34, 43.|Floian|Tremadocian|Age written as Lancefieldian to Bendigonian in text.|||||Chert, siltstone, black shale, phosphorite: chert and siltstone brown and grey, thinly bedded; phosphorite medium to coarse sand-sized, dark green-grey, contains rare Early Ordovician (Lancefieldian) graptolites.|
74885|Phosphate Hill Formation|70601|5|Briefly described|p44|Lancefieldian|Lancefieldian|Licola area.||||Overlies Wild Dog Chert.||
15148|Piangil Member|23560|5|Briefly described|p150|||Of Woorinen Formation.||||||
15148|Piangil Member|24551|6|Mentioned|p341|||Of the Woorinen Formation.||||||
15148|Piangil Member|35272|6|Mentioned|p286|||||||||
15148|Piangil Member|41848|5|Briefly described|p361|||Member of Woorinen Formation||||||
15148|Piangil Member|42264|6|Mentioned|Fig.5 P12|||||||||
15148|Piangil Member|42827|5|Briefly described|Table 9.1|||||||||
15148|Piangil Member|42966|2|Defined|Table 35 p237|Holocene||of Woorinen Formation||||||
15148|Piangil Member|44133|6|Mentioned|p253|Holocene|Middle Pleistocene|Of the Woorinen Formation. Geological Province: Murray Basin.||||||
15148|Piangil Member|68194|6|Mentioned|p28|||||Unit in Woorinen Formation.||||
15168|Picton Scoria|35722|6|Mentioned|Table 2|||Quaternary stratigraphic units and nature of components.||||||
37771|Pike Hill Granodiorite|23309|6|Mentioned|p441, Appendix 1|||G504, S-Type. Supersedes Pike Hill Granite.||||||
37771|Pike Hill Granodiorite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|Of the Ocean View Suite. G504. S-type. Weathered, foliated, coarse grained granodiorite.||||||
37771|Pike Hill Granodiorite|43315|5|Briefly described|Map Legend|Wenlock|Wenlock|G504. Of the Ocean View Suite.  S-type. Weathered, foliated, coarse grained granodiorite.||||||03-MAY-05
37771|Pike Hill Granodiorite|60541|5|Briefly described|p79, p18 Tb. 1|Silurian|Silurian|Intrusive within the Kuark Metamorphic Complex. Previously mapped by Dodd (1981) but not named. Very weathered, forming decomposed pavements and low crumbling tors of coarse-grained quartz and feldspar in a clay-rich matrix.  Age is Middle Silurian.||||||
37771|Pike Hill Granodiorite|68116|5|Briefly described|Appendix, Map 45.|Wenlock|Wenlock||||||Biotite granodiorite: coarse to medium-grained; foliated; weathered; S-type.|
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.||||||
75957|Pine Lodge Leucitite|68115|5|Briefly described|p10.|Cenozoic|Cenozoic|Formerly Cosgrove Leucitite; also on earlier GSV maps as Newer Volcanics. Has distinct composition and is remote from other Cenozoic volcanic rocks, hence merits its own Formation. Exposure mainly restricted to two quarries. Described as leucite-bearing lava, but left un-named, by Birch (1976); named Cosgrove Leucitite by Tickell (1989). This latter conflicts with Cosgrove Porphyry in NSW, which has precedence (Richardson, 1975); hence its new name Pine Lodge Leucitite after the parish of Pine Lodge in which it occurs.||||||
75957|Pine Lodge Leucitite|68116|5|Briefly described|Appendix, Map 18.|Messinian|Messinian||||||Dark grey olivine leucitite with phenocrysts of olivine and uncommon clinopyroxene in a groundmass of clinopyroxene, leucite, Fe-Ti oxides, interstitial nepheline and brown Ba- and Ti-rich mica.|
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.|
23907|Pinnak Sandstone|22628|6|Mentioned|fig1p108|Ordovician|Ordovician|||||||
23907|Pinnak Sandstone|22708|6|Mentioned|p212|||||||||
23907|Pinnak Sandstone|22794|5|Briefly described|p65|Early Ordovician|Early Ordovician|||||||
23907|Pinnak Sandstone|22815|6|Mentioned|p18|Ordovician|Ordovician|Equivalent to the Adaminaby Group.||||||
23907|Pinnak Sandstone|22876|5|Briefly described|p15|Ordovician|Ordovician|500-440Ma||||||
23907|Pinnak Sandstone|22877|5|Briefly described|map|Ordovician|Ordovician|||||||
23907|Pinnak Sandstone|22878|4|Described|p29|Ordovician|Ordovician|Adaminaby Group.||||||25-SEP-08
23907|Pinnak Sandstone|22879|5|Briefly described|map|Early Ordovician|Early Ordovician|Of the Adaminaby Group. Sandstone: green grey, often thick bedded quartz sandstone; turbiditic; interbedded with dark grey mudstone and rare black siliceous shale. Thinly bedded chert horizons.||||||01-OCT-04
23907|Pinnak Sandstone|22880|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Of the Adaminaby Group. Sandstone: green grey, often thick bedded quartz sandstone; turbiditic; interbedded with dark grey mudstone and rare black siliceous shale. Thinly bedded chert horizons.||||||01-OCT-04
23907|Pinnak Sandstone|22881|5|Briefly described|Map legend|Ordovician|Ordovician|||||||06-OCT-04
23907|Pinnak Sandstone|22968|3|Fully described|P21, Fig32, P30, P99|Ordovician|Early Ordovician|Pinnak Sandstone is nonmagnetic, parent is Adaminaby Group, overlying unit is Sunlight Creek Formation||||||
23907|Pinnak Sandstone|22971|4|Described|p 17|Ordovician|Ordovician|Included in the "Hotham beds" in WANGARATTA region. Consists of sandstones and mudstones.||||||19-JAN-06
23907|Pinnak Sandstone|23020|5|Briefly described|Map legend||Ordovician|Parent is Adaminaby Group.||||||25-SEP-08
23907|Pinnak Sandstone|23021|5|Briefly described|Map legend|Ordovician|Early Ordovician|Parent is Adaminaby Group.||||||25-SEP-08
23907|Pinnak Sandstone|23028|5|Briefly described|Map legend|Ordovician|Early Ordovician|Parent is Adaminaby Group, overlying unit is Bendoc Group.||||||25-SEP-08
23907|Pinnak Sandstone|23029|5|Briefly described|Map legend|Ordovician|Early Ordovician|Parent is the Adaminaby Group.||||||25-SEP-08
23907|Pinnak Sandstone|23030|5|Briefly described|Map legend|Ordovician|Ordovician|Parent is the Adaminaby Group||||||
23907|Pinnak Sandstone|23229|5|Briefly described|Table3-2p21|Gisbornian||||||||
23907|Pinnak Sandstone|23307|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
23907|Pinnak Sandstone|23309|5|Briefly described|p53-55, 58|||||||||
23907|Pinnak Sandstone|23615|3|Fully described|p64, p20 Fig.6|Early Ordovician|Early Ordovician|Extends into New South Wales as the Adaminaby Group. Geological Province: Lachlan Fold Belt. Age: Bendigonian to Darriwilian. ~||||||21-FEB-13
23907|Pinnak Sandstone|23850|5|Briefly described|p793|Early Ordovician|Early Ordovician|Of Adaminaby Group. Overlain by the Bendoc Group.||||||26-APR-06
23907|Pinnak Sandstone|23860|5|Briefly described|p944|Ordovician|Ordovician|Of Adaminaby Group. Overlying unit Warbisco Shale. Underlying unit Howqua Chert.||||||
23907|Pinnak Sandstone|23938|5|Briefly described|p11, p70 Tb. 6|Middle Ordovician|Early Ordovician|Of the Adaminaby Group. Marine: sandstone, mudstone, siltstone, minor chert. Geological Province: Lachlan Fold Belt. See also p139 Tb. 1 Appendix.||||||
23907|Pinnak Sandstone|24002|5|Briefly described|p228 Fig.2|Ordovician|Ordovician|||||||
23907|Pinnak Sandstone|24004|5|Briefly described|p278|Ordovician|Ordovician|||||||
23907|Pinnak Sandstone|24037|6|Mentioned|p423|||Geological Province: Lachlan Fold Belt||||||
23907|Pinnak Sandstone|24098|5|Briefly described|p27 Fig. 2|Middle Ordovician|Early Ordovician|Geological Province: Lachlan Fold Belt.||||||
23907|Pinnak Sandstone|24133|3|Fully described|p35|Ordovician|Ordovician|Parent: Adaminaby Group.  Geological Province: Lachlan Fold Belt.||||||
23907|Pinnak Sandstone|24142|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Adaminaby Group. Geological Province: Lachlan Fold Belt.||||||
23907|Pinnak Sandstone|24143|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Adaminaby Group. Geological Province: Lachlan Fold Belt.||||||
23907|Pinnak Sandstone|24144|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Adaminaby Group. Geological Province: Lachlan Fold Belt.||||||
23907|Pinnak Sandstone|24145|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Adaminaby Group. Geological Province: Lachlan Fold Belt||||||
23907|Pinnak Sandstone|24146|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Adaminaby Group. Geological Province: Lachlan Fold Belt.||||||
23907|Pinnak Sandstone|24551|3|Fully described|p101|Middle Ordovician|Early Ordovician|Only unit of the Adaminaby Group found in Victoria. Overlain by Warbisco Shale and Sunlight Creek Formation.||||||08-NOV-05
23907|Pinnak Sandstone|38151|6|Mentioned|Table 1|||||||||
23907|Pinnak Sandstone|40136|5|Briefly described|p36|||||||||
23907|Pinnak Sandstone|40761|6|Mentioned|p223|||||||||
23907|Pinnak Sandstone|41570|3|Fully described|p81|||See also p93||||||08-NOV-05
23907|Pinnak Sandstone|41572|6|Mentioned|p23|||||||||
23907|Pinnak Sandstone|41585|6|Mentioned|p132|||||||||
23907|Pinnak Sandstone|41868|6|Mentioned|Table 12.3|||||||||
23907|Pinnak Sandstone|42294|6|Mentioned|p24|||||||||
23907|Pinnak Sandstone|42627|5|Briefly described|Map legend|early Darriwilian|early Yapeenian|||||||
23907|Pinnak Sandstone|42647|4|Described|p18||Bendigonian|||||||
23907|Pinnak Sandstone|42827|5|Briefly described|p93|||||||||
23907|Pinnak Sandstone|43206|5|Briefly described|map legend||Early Ordovician|||||||
23907|Pinnak Sandstone|43220|6|Mentioned|p9||Early Ordovician|||||||
23907|Pinnak Sandstone|43228|5|Briefly described|p9||Early Ordovician|||||||
23907|Pinnak Sandstone|43312|5|Briefly described|Map Legend|Darriwilian|Bendigonian|of Adaminaby Group.||||||
23907|Pinnak Sandstone|43313|5|Briefly described|Map Legend|Darriwilian|Bendigonian|of Adaminaby Group||||||
23907|Pinnak Sandstone|43314|5|Briefly described|Map Legend||Early Devonian|of Adaminaby Group.||||||
23907|Pinnak Sandstone|43315|5|Briefly described|Map Legend||Ordovician|Of the Adaminaby Group. Sandstone, green-grey, often thick-bedded, moderately sorted lithic sandstone, turbiditic; interbedded massive to laminated siltstone, slaty mudstone and occasional chert beds.||||||03-MAY-05
23907|Pinnak Sandstone|44184|5|Briefly described|Map Legend||Early Ordovician|||||||
23907|Pinnak Sandstone|44185|5|Briefly described|Map legend.|Middle Ordovician|Early Ordovician|||Unit in Adaminaby Group.|||Marine: sandstone, mudstone, siltstone, minor chert.|30-OCT-14
23907|Pinnak Sandstone|44187|5|Briefly described|Map Legend||Early Ordovician|||||||
23907|Pinnak Sandstone|60503|3|Fully described|p81-84, p21 Fig. 4|Darriwilian|Early Ordovician|Of the Adaminaby Group. Previously Hotham slates and Mallacoota beds. Sandstones, with gritstones and quartzites, interbedded mudstones. Overlain by Sunlight Creek Formation and Besford Ignimbrite; unconformably overlies Tombong Beds. Min age: from Darriwilian conodonts in overlying Sunlight Creek Formation.||||||21-FEB-13
23907|Pinnak Sandstone|60504|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Of the Adaminaby Group. Sandstone; dark to mid grey; turbiditic, thick to thinly bedded, micaceous and silty to quartzitic; interbedded with thin-bedded grey siltstone and claystone, minor granule conglomerate, minor chert.||||||20-OCT-04
23907|Pinnak Sandstone|60505|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Of the Adaminaby Group. Sandstone; dark to mid grey; turbiditic, thick to thinly bedded, micaceous and silty to quartzitic; interbedded with thin-bedded grey siltstone and claystone, minor granule conglomerate and minor chert.||||||21-OCT-04
23907|Pinnak Sandstone|60506|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Of the Adaminaby Group. Sandstone; dark to mid grey; turbiditic, thick to thinly bedded, micaceous and silty to quartzitic; interbedded with thin-bedded grey siltstone and claystone, minor granule conglomerate and minor chert.||||||21-OCT-04
23907|Pinnak Sandstone|60507|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Of the Adaminaby Group. Sandstone; dark to mid grey; turbiditic, thick to thinly bedded, micaceous and silty to quartzitic; interbedded with thin-bedded grey siltstone and claystone, minor granule conglomerate, minor chert.||||||21-OCT-04
23907|Pinnak Sandstone|60508|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Adaminaby Group. Sandstone: nonmagnetic except where altered (0-20 nT); moderate, although variable, total count, K, Th, U||||||
23907|Pinnak Sandstone|60541|3|Fully described|p49, p19 Tb. 1|Darriwilian|Bendigonian|Previously  Adaminaby Beds and Mallacoota Beds. Referred to as Adaminaby Beds in NSW. Deposited as an extensive submarine fan, dominated by sandstones... Overlain by Combyingbar Fm and parts of Yalmy Gp. Age: 500-438Ma.Max. thick: >2.2km. Geol.Prov: LFB.||||||22-JUN-05
23907|Pinnak Sandstone|60542|3|Fully described|p45, p11 Fig. 2|Darriwilian|Bendigonian|Named Mallacoota beds and Hotham slates also. Of Adaminaby Group. Turbidites - interbedded sandstone, slaty mudstones and chert. Age: 500-438Ma.||||||19-DEC-07
23907|Pinnak Sandstone|61160|3|Fully described|p12, p44, p132, p17 Fig 3.5, p35 Tb 5.2.|Middle Ordovician|Early Ordovician|Of Adaminaby Gp. This parent rock becomes increasingly metamorphosed to constitute Omeo Met.Complex. Defined as the cordierite zone and higher grades, the Pinnak Sst includes chlorite and biotite zones. Conformably under Bendoc Gp and over Howqua Chert. ||||||
23907|Pinnak Sandstone|61161|5|Briefly described|pp78-82, p76-77 Fig 6.1, p6|Darriwilian|Early Ordovician|Of Adaminaby Group. Protolith of Omeo Metamorphic Complex. Intruded by Mount Baldhead Ig. Complex. Faulted against Cobbanah Group; overlies Howqua Chert; underlies Wentworth and Bendoc Groups. Deep marine turbidites: sandstone; mudstone. GSV map code: Oap||||||
23907|Pinnak Sandstone|61163|3|Fully described|p77, p10 Fig. 31|Middle Ordovician|Early Ordovician|Of the Adaminaby Group - parent rock (protolith) of the Omeo Metamorphic Complex, in the Omeo Zone. Deep marine sedimentary rocks, hosting primary gold. Geological Province: Lachlan Fold Belt (Tabberabbera Zone). See also p14 Fig. 3.2, p38 Tb. 6.2.||||||
23907|Pinnak Sandstone|61164|5|Briefly described|map legend|Middle Ordivician|Early Ordivician|Of Adaminaby Group. Sandstone, siltstone: sandstone very thick to thin-bedded, turbiditic, moderately sorted, minor feldspar and detrital mica; siltstone well-bedded, with smooth regular banding; deep marine. GSV map code: Oap||||||
23907|Pinnak Sandstone|61165|5|Briefly described|map legend|Middle Ordivician|Early Ordivician|Of Adaminaby Group. Sandstone, siltstone: sandstone very thick to thin-bedded, turbiditic, moderately sorted, minor feldspar and detrital mica; siltstone well-bedded, with smooth regular banding; deep marine. GSV map code: Oap||||||
23907|Pinnak Sandstone|61166|5|Briefly described|map legend|Middle Ordivician|Early Ordivician|Of Adaminaby Group. Sandstone, siltstone: sandstone very thick to thin-bedded, turbiditic, moderately sorted, minor feldspar and detrital mica; siltstone well-bedded, with smooth regular banding; deep marine. GSV map code: Oap||||||
23907|Pinnak Sandstone|61167|5|Briefly described|map legend|Middle Ordivician|Early Ordivician|Of Adaminaby Group. Sandstone, siltstone: sandstone very thick to thin-bedded, turbiditic, moderately sorted, minor feldspar and detrital mica; siltstone well-bedded, with smooth regular banding; deep marine. GSV map code: Oap||||||07-FEB-11
23907|Pinnak Sandstone|61168|5|Briefly described|map legend|Late Ordivician|Early Ordivician|Of Adaminaby Group. Sandstone, mudstone; turbidite; nonmagnetic, high gravity except where intruded by less dense plutons; very low radioelement and K, low Th, very low U on ridgetops, moderate total radioelement, K, Th and U in valleys. GSV map code: Oap||||||
23907|Pinnak Sandstone|61169|5|Briefly described|map legend|Middle Ordovician|Early Ordivician|Of Adaminaby Group. Sandstone, siltstone, minor granulestone, minor chert; deep-marine turbidite fan and hemipelagic deposits. GSV map code: Oap.||||||
23907|Pinnak Sandstone|61170|5|Briefly described|map legend|Middle Ordovician|Early Ordivician|Of Adaminaby Group. Sandstone, siltstone, minor granulestone, minor chert; deep-marine turbidite fan and hemipelagic deposits. GSV map code: Oap.||||||07-FEB-11
23907|Pinnak Sandstone|61171|5|Briefly described|map legend|Middle Ordovician|Early Ordivician|Of Adaminaby Group. Sandstone, siltstone, minor granulestone, minor chert; deep-marine turbidite fan and hemipelagic deposits. GSV map code: Oap.||||||
23907|Pinnak Sandstone|61172|5|Briefly described|map legend|Middle Ordovician|Early Ordivician|Of Adaminaby Group. Sandstone, siltstone, minor granulestone, minor chert; deep-marine turbidite fan and hemipelagic deposits. GSV map code: Oap.||||||
23907|Pinnak Sandstone|61173|5|Briefly described|map legend|Middle Ordovician|Early Ordivician|Of Adaminaby Group. Sandstone, siltstone, minor granulestone, minor chert; low to high gravity reponse; nonmagnetic to weakly magnetic; varying over topography, moderate-high K and total radioelements, low-high Th, low-moderate U. GSV map code: Oap.||||||
23907|Pinnak Sandstone|61174|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Of the Adaminaby Group. Sandstone, siltstone, rare chert: sandstone very thick to thin-bedded, turbiditic; siltstone well-bedded, with smooth regular banding. Deep-marine turbidite fan and hemipelagic deposits. GSV map code: Oap.||||||07-FEB-11
23907|Pinnak Sandstone|61175|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Of the Adaminaby Group. Sandstone, siltstone, rare chert: sandstone very thick to thin-bedded, turbiditic; siltstone well-bedded, with smooth regular banding. Deep-marine turbidite fan and hemipelagic deposits. GSV map code: Oap.||||||
23907|Pinnak Sandstone|61176|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Of the Adaminaby Group. Sandstone, siltstone, rare chert: sandstone very thick to thin-bedded, turbiditic; siltstone well-bedded, with smooth regular banding. Deep-marine turbidite fan and hemipelagic deposits. GSV map code: Oap.||||||
23907|Pinnak Sandstone|61177|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Of the Adaminaby Group. Sandstone, siltstone, rare chert: sandstone very thick to thin-bedded, turbiditic; siltstone well-bedded, with smooth regular banding. Deep-marine turbidite fan and hemipelagic deposits. GSV map code: Oap.||||||
23907|Pinnak Sandstone|61178|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Of Adaminaby Group. Sandstone, siltstone (turbidite): nonmagnetic, minor moderately magnetic Fe altered patches; high gravity, except in SE where moderate due to effects of topography and plutons; surrounds Nelson Creek Granite. GSV map code: Oap.||||||
23907|Pinnak Sandstone|61187|5|Briefly described|p5 Fig.3, p114, p122, p144 Fig.4.|Ordovician|Ordovician|Flysch sediments. Strikes E-W, dips steeply (45 to 80 degrees) S.||Unit in Adaminaby Group.||Overlies Feltis Farm Tonalite.|Siltstone, sandstone, greywacke.|
23907|Pinnak Sandstone|61196|5|Briefly described|p17|Ordovician|Ordovician|Age is Early Ordovician. Conformably overlain by the Bendoc Group. Quartz-turbidities.||||||25-JAN-06
23907|Pinnak Sandstone|61964|5|Briefly described|p24, p25 Fig. 8|||Of the Adamainaby Group in Victoria (not differentiated in NSW). Equivalent in age to part of Clements Formation but contains less siltstone.||||||
23907|Pinnak Sandstone|63635|6|Mentioned|p39|||Overlain by the Bendoc Group. Turbidite unit - thick bedded and poorly fossiliferous sandstone sequence. Correlate of Adaminaby Group in NSW. ||||||
23907|Pinnak Sandstone|65900|5|Briefly described|p167, p159 Table 1, p158||Ordovician|Tabberabbera Zone. Turbidite package.||||Underlies the Cobbannah Group.||10-MAY-12
23907|Pinnak Sandstone|66196|5|Briefly described|p618|Middle Ordovician||Turbidites, faulted against the Sunlight Creek Formation in Seal Creek, but conformably overlain by Sunlight Creek Formation throughout eastern Victoria.||||||
23907|Pinnak Sandstone|66769|6|Mentioned|137|Silurian|Ordovician|Tabberabbera Zone||||||
23907|Pinnak Sandstone|67322|5|Briefly described|p13, p15|Middle Ordovician|Late Cambrian|Age based on conodonts identified in thin sections of chert that occur in horizons interbedded with sandstone-dominated units.||Of the Adaminaby Group|||Includes chert layers.|22-FEB-18
23907|Pinnak Sandstone|68115|6|Mentioned|p4.|Ordovician|Ordovician|Now expanded to include the now-obsolete Broadbent River Sandstone.||||||
23907|Pinnak Sandstone|68116|5|Briefly described|Maps 18-20, 25-28, 34-37, 44-46.|Darriwilian|Tremadocian|Also occurs in the Appendix. Maximum age written as Lancefieldian in text. Thick sandstone beds are mostly massive graded (Bouma Ta) and in places with granulestone bases, thinner beds have well-formed laminated and cross-bedded intervals (Bouma Tb and Tc).|||||Sandstone, siltstone, rare chert: sandstone dark to pale grey and green, thick to thin-bedded, turbiditic, moderately sorted, quartz-rich with minor feldspar and detrital mica. Siltstone dark grey to green, well-bedded, with smooth regular banding.|
23907|Pinnak Sandstone|68592|5|Briefly described|p272, p279, p297-8, p308|Lancefieldian|Lancefieldian|VandenBerg et al. (1992). Eastern Victoria.||Unit in Adaminaby Group.||Conformably overlies Howqua Chert. Equivalent to Abercrombie Formation.||
23907|Pinnak Sandstone|68822|5|Briefly described|p324|Middle Ordovician|Lower Ordovician|Graptolite-poor.||Of the Adaminaby Group.||Overlain by the Warbisco Shale.||
23907|Pinnak Sandstone|70493|6|Mentioned|p55|||Contains moderately high K-feldspar content.||||||
23907|Pinnak Sandstone|70601|5|Briefly described|p44, p46, p48|Lancefieldian|Lancefieldian|Palaeocurrents indicate a westerly source. Lancefieldian graptolites occur in carbonaceous shale 20 m above the base.|ca 480 Ma.|Adaminaby Group||Overlies Howqua Chert.|Quartz turbidites: sandstone, carbonaceous shale.|
23907|Pinnak Sandstone|70718|5|Briefly described|p43-p44|Ordovician|Ordovician|Tabberabbera Zone, Murray Basin. Hosts numerous small orogenic gold deposits.||Adaminaby Group||||
23907|Pinnak Sandstone|70941|6|Mentioned|p15|||Omeo Metamorphic Complex, Omeo Zone||||Correlated with the Wagga Group.||
23907|Pinnak Sandstone|71069|6|Mentioned|p52,p58, p59, p63|Lancefieldian|Lancefieldian|||Adaminaby Group||Conformably overlies the Howqua Chert. Equivalent to the Willigam Sandstone Member.||
23907|Pinnak Sandstone|71700|5|Briefly described|p8, CD|Lancefieldian|Lancefieldian|Cooma Region.||Adaminaby Group||Equivalent to the Abercrombie Formation.||
23907|Pinnak Sandstone|72296|5|Briefly described|p6|||Gray et al. (2003). Comprises the Omeo Metamorphic Complex (the VIC part of the Wagga Metamorphic Belt).||Adaminaby Group.||Part-equivalent to the Clements Formation.||
23907|Pinnak Sandstone|73140|6|Mentioned|p495|||Proposed to be incorporated into, and superseded by the Abercrombie Formation.||||||
31625|Pinnak Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
26280|Pintadeen Basalt|22886|5|Briefly described|p16|Miocene|Miocene|||||||
26280|Pintadeen Basalt|42628|5|Briefly described|Map legend|Miocene||||||||
26280|Pintadeen Basalt|42826|2|Defined|p49|early Miocene||age of 22.5 +/- 0.1 Ma||||||
26280|Pintadeen Basalt|44197|5|Briefly described|Map Legend||Miocene|||||||
26280|Pintadeen Basalt|63445|5|Briefly described|Map legend.|Miocene|Miocene||||||Extrusive: olivine tholeiites.|
26280|Pintadeen Basalt|68116|5|Briefly described|Appendix, Maps 32-33.|Aquitanian|Aquitanian||||||Olivine basalt: blue-black; dense; phenocrysts of labradorite, clinopyroxene, olivine in finer matrix with interstitial devitrified glass; well developed columnar jointing.|
35518|Pipeline Volcanics|23309|4|Described|p124, 125. Table 2.48||Devonian|Supersedes: Brodribb River Volcanics.||||||22-FEB-10
35518|Pipeline Volcanics|68116|5|Briefly described|Appendix, Map 45.|Early Devonian|Early Devonian|Contains an informal porphyry phase subdivision.|||||Welded coarse ignimbrite, crystals of quartz + feldspar, lithic grains in a fine foliated matrix, flattened pumice; sandstone and shale lithics; minor quartz-feldspar porphyry: quartz phenocrysts in a fine sericitised matrix.|
83404|Pitarpunga pluton|73496|5|Briefly described|Map legend|Late Devonian|Late Devonian|G318.|||||Nonmagnetic but with magnentic contact aureole;  gravity low to 80 micrometres/second/second below the regional.|
30281|Pitfield Volcanics|23300|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||
30281|Pitfield Volcanics|23301|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||
30281|Pitfield Volcanics|23302|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||
30281|Pitfield Volcanics|23303|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||
30281|Pitfield Volcanics|23304|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||
30281|Pitfield Volcanics|23305|3|Fully described|p32||Cambrian|of Taylor et al (1996). Age inferred because of similarity with other Victorian greenstones. Geological Province: Lachlan Fold Belt.||||||
30281|Pitfield Volcanics|23309|5|Briefly described|p25-28. Tb 2.4/2.1|Cambrian|Cambrian|||||||
30281|Pitfield Volcanics|24551|4|Described|p83|Cambrian|Cambrian|||||||02-AUG-05
30281|Pitfield Volcanics|60451|5|Briefly described|p23|Cambrian|Cambrian|||||||
30281|Pitfield Volcanics|60585|4|Described|p16|Cambrian|Cambrian|Overlain by the Beaufort Formation. Consists of metavolcanic greenstones.||||||
30281|Pitfield Volcanics|68189|5|Briefly described|p14|||Along with the Magdala Volcanics, these rocks represent the oldest rocks at shallow depths on ST ARNAUD.||Of the Dja Dja Wrung Supergroup.||||
15297|Piton Scoria Member|41701|6|Mentioned|Map legend|Holocene||||||||
15297|Piton Scoria Member|41769|5|Briefly described|p39|||||||||
15297|Piton Scoria Member|66002|5|Briefly described|p13 Tb.9, p18|Neogene|Neogene|Of Tower Hill Tuff. Called Piton Scoria by Gill (1967)||||||
15297|Piton Scoria Member|68116|5|Briefly described|Appendix, Map 48.|Holocene|Pleistocene||||||Scoria, spatter, ash, nepheline basanite lava: scoria unconsolidated; basanite highly vesicular; small olivine phenocrysts in opaque groundmass.|
73169|Plains Basalts|61896|6|Mentioned|p15|||Refers to the basalts of the Plains Suite. Dominantly transitional to tholeiitic types.||||||27-FEB-09
15316|Platina Siltstone Member|35283|5|Briefly described|p54|||||||||
22664|Plumb Gully Ignimbrite|23309|4|Described|p110. Tb 2.40|||Maximum Thickness: 100m.  Of the Mount Dawson Subgroup.||||||
22664|Plumb Gully Ignimbrite|23615|3|Fully described|p106|Early Devonian|Early Devonian|Of Mount Dawson Subgroup.  Overlies Doyle Gully Ignimbrite and Bimmarn Ignimbrite.  Is overlain by Lookout Top Ignimbrite.  Maximum thickness: 100m.||||||
22664|Plumb Gully Ignimbrite|43206|5|Briefly described|map legend||Ludlow|Of Mount Dawson Subgroup.||||||
22664|Plumb Gully Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Quartz-feldspar ignimbrite with red volcanic lithic clasts and red pumice fragments.|
37588|Poddy Creek Metamorphics|23309|5|Briefly described|p317|||||||||
37588|Poddy Creek Metamorphics|43315|5|Briefly described|Map legend|||Spotted slate and biotite grade (biotite schist, phyllite). Associated with the Kuark Metamorphic Complex.||||||
37588|Poddy Creek Metamorphics|60541|5|Briefly described|p37, p91|Silurian|Silurian|Metamorphics are derived entirely from the Pinnak Sandstone. Probably unrelated to the Kuark Metamorphic Complex. Consists of two zones: spotted zone and biotite zone. See also p24.Age is Middle Silurian.||||||08-DEC-16
37588|Poddy Creek Metamorphics|68116|5|Briefly described|Appendix, Map 45.|Wenlock|Llandovery||||||Slate with spots of chlorite, muscovite and sericite; quartz sandstone; biotite phyllite and psammite; spots of retrogressed cordierite..|08-DEC-16
37589|Pohlner Conglomerate Member|23309|5|Briefly described|p83, 342, table 2.27|||Of Murray Hill Sandstone.||||||
37589|Pohlner Conglomerate Member|61183|6|Mentioned|p129|||Of Murray Hills Sandstone (Grampians Group). Possible low grade Au placer deposit. See also Pohlner Conglomerate Bed.||||||
37589|Pohlner Conglomerate Member|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Murray Hill Sandstone. Called Pohlner Conglomerate Bed by Cayley and Taylor (1997)||||||
37589|Pohlner Conglomerate Member|71593|6|Mentioned|p148|||||Grampians Group||||
15365|Point Addis Limestone|22626|6|Mentioned|446 fig 10, 447|Late Oligocene|Late Oligocene|Geol province East Otway Basin. Overlying unit Puebla Clay, underlying unit Angahook Formation||||||
15365|Point Addis Limestone|23768|5|Briefly described|p28 Fig.5|Early Miocene|Early Miocene|In the Torquay/Geelong area.  Presented as Pt Addis only in figure.  See also p7, p103.||||||30-MAR-05
15365|Point Addis Limestone|23778|6|Mentioned|p668|||||||||
15365|Point Addis Limestone|24551|5|Briefly described|p313|||Of the Torquay Group.||||||
15365|Point Addis Limestone|31245|6|Mentioned|p74|||Fauna. Oligocene.||||||
15365|Point Addis Limestone|32552|6|Mentioned|p184|||Janjukian||||||
15365|Point Addis Limestone|32601|6|Mentioned|p674|||Equinoid source material||||||
15365|Point Addis Limestone|33155|5|Briefly described|p118|||||||||
15365|Point Addis Limestone|34421|6|Mentioned|p261|||||||||
15365|Point Addis Limestone|36499|6|Mentioned|p34|||||||||
15365|Point Addis Limestone|37311|6|Mentioned|p49|||||||||
15365|Point Addis Limestone|37602|4|Described|p645|||||||||
15365|Point Addis Limestone|41043|5|Briefly described|p96|||||||||
15365|Point Addis Limestone|41519|6|Mentioned|p168|||||||||
15365|Point Addis Limestone|41547|6|Mentioned|Fig.4|||||||||
15365|Point Addis Limestone|42371|6|Mentioned|p35, p36|Janjukian||||||||
15365|Point Addis Limestone|42655|6|Mentioned|p39|||Member of Jan Juc Formation||||||
15365|Point Addis Limestone|43702|6|Mentioned|Fig.2,p398|Miocene|Late Oligocene|||||||
15365|Point Addis Limestone|60299|5|Briefly described|p228 Tb.5|Oligocene|Oligocene|Age: 26 Ma. Palaeopole position given.||||||
15365|Point Addis Limestone|60563|5|Briefly described|p47|Oligocene|Oligocene|Bioclastic calcarenites.||||||
15365|Point Addis Limestone|60785|5|Briefly described|p184 Fig.1, pp189-190.   |Chattian|Chattian|Of the Torquay/Port Phillip Basins. Has yielded a variety of fossil cetacean elements at different locations.|||||Yellow sandy bryozoal calcarenite. Ferruginous intraclastic conglomerate with abraded shelly and vertebrate skeletal components. |
15365|Point Addis Limestone|61186|6|Mentioned|p93|Miocene|Oligocene|Victorian dimension stone.||||||
15365|Point Addis Limestone|62899|6|Mentioned|p51|Early Miocene|Late Oligocene|||||||
15365|Point Addis Limestone|63739|5|Briefly described|p51|Early Miocene|Late Oligocene|Contains ostracod assembalges (Hermanites sp.).||||||01-JUL-08
15365|Point Addis Limestone|65316|4|Described|p595, p598, p597 Fig 2, p601-603|Chattian|Rupelian|Lower section age equivalent to Jan Juc Marl.  Thought correlative of Clifton Formation. Abundant shelly fossils; distinctive marine assemblage close to the contact with Angahook Formation.|24.24 +1.3 / -1.2 Ma at base.|Of Torquay Group.||Unconformably overlies Angahook Formation; conformably overlain by Puebla Clay.|Marine calcarenite and sandy marl.|23-APR-12
15365|Point Addis Limestone|67061|5|Briefly described|p546.||||24.24 Ma.|Unit in Torquay Group.||||
15365|Point Addis Limestone|69297|6|Mentioned|p98|Chattian|Chattian|||Torquay Group||Overlies the Angahook Formation. Overlain by the Jan Juc Formation. |Limestones. |
15365|Point Addis Limestone|70942|5|Briefly described|p121, 119|||||||||
15368|Point Danger Clay|34421|6|Mentioned|p261|||||||||
15369|Point Hesse Clay|42318|5|Briefly described|p8|||||||||
29713|Point Ricardo Granite|23309|6|Mentioned|p441 App1|||G511 I-Type.||||||
29713|Point Ricardo Granite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|I-type. Medium grained hornblende biotite granite.||||||22-OCT-04
29713|Point Ricardo Granite|43315|5|Briefly described|Map Legend|Wenlock|Wenlock|I-type. medium-grained hornblende biotite granite.||||||03-MAY-05
29713|Point Ricardo Granite|60541|5|Briefly described|p63-64|||Intrusive rock, highly weathered, medium-grained granite outcropping in a mass of rubbly boulders. Geological Province: Lachlan Fold Belt.||||||22-JUN-05
15380|Point Ronald Clay|48581|14|Not recorded|p14|||||||||
15380|Point Ronald Clay|48911|6|Mentioned|p49|||See also Chart 1||||||
34903|Polar Star Suite|22968|5|Briefly described|Fig89 P164, P195|Devonian|Silurian|New name||||||
34903|Polar Star Suite|23020|5|Briefly described|Map legend|Lochkovian|Pridoli|||||||
34903|Polar Star Suite|23021|5|Briefly described|Map legend|Lochkovian|Pridoli|||||||
34903|Polar Star Suite|23028|5|Briefly described|Map legend|Lochkovian|Pridoli|||||||
34903|Polar Star Suite|23029|5|Briefly described|Map legend|Lochkovian|Pridoli|||||||
34903|Polar Star Suite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
34903|Polar Star Suite|23309|5|Briefly described|p344|||||||||
34903|Polar Star Suite|24551|6|Mentioned|p230|||||||||
34903|Polar Star Suite|61160|6|Mentioned|p70|||Formerly a part of Fagan's (1979) Falls Creek Series. Now probably an obsolete name? Hornblende-bearing rock. ||||||
34903|Polar Star Suite|61161|5|Briefly described|p91|||I-type. See also Polar Star suite.||||||
34851|Polar Star Tonalite|22968|5|Briefly described|P71, Table7, P196||Late Silurian|Age of unit is 418+/-4Ma, New name, parent is the Polar Star Suite||||||
34851|Polar Star Tonalite|23029|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is the Polar Star Suite||||||
34851|Polar Star Tonalite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Polar Star Suite. Age: 418 +/- 4 Ma (U/Pb zircon)||||||14-SEP-04
34851|Polar Star Tonalite|23309|5|Briefly described|p100, 343||Devonian|G146. I-Type. Age: 418+/-4 Ma||||||
34851|Polar Star Tonalite|24551|6|Mentioned|p717 Table 2.4|Silurian|Silurian|Age: 418 +/- 4Ma.||||||02-AUG-05
34851|Polar Star Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Biotite tonalite: grey; medium-grained; equigranular; minor porphyritic fine-grained tonalite; moderately to strongly foliated.|
83418|Polisbet Granite|73505|5|Briefly described|p19-20|||Newly named unit in Swan Hill and parts of Balranald and Deniliquin 1:250 000 map areas, (G319). Named after Polisbet Parish. Of the Lalbert Batholith. Comprises a 75km long intrusion that extends from NW of Nyah West to SE of Sea Lake. Magnetic response shows strong zoning, with both nonmagnetic parts and other areas to 60 nT. Gravity response to 80 micrometres/second/second lower than surrounds in north and west, but less than 20 in the south and east.|||||Granite.|
15419|Polworth Conglomerate|42318|5|Briefly described|p7|||||||||
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.|
15449|Poowong gabbro|34843|6|Mentioned|p9|||Age date given.||||||
15462|Port Campbell Limestone|22674|5|Briefly described|Fig.2 p719|Late Miocene|Middle Miocene|||||||
15462|Port Campbell Limestone|22875|5|Briefly described|p69|Late Miocene|Middle Miocene|Of the Heytesbury Group.||||||07-MAR-07
15462|Port Campbell Limestone|22944|5|Briefly described|Fig3|||||||||
15462|Port Campbell Limestone|23228|6|Mentioned|Fig2-6p14||Miocene|||||||
15462|Port Campbell Limestone|23230|4|Described|Table4-1p40, Fig4-3p46|Miocene|Miocene|||||||
15462|Port Campbell Limestone|23238|6|Mentioned|p106|||||||||
15462|Port Campbell Limestone|23307|5|Briefly described|Map Legend|Miocene|Miocene|||||||
15462|Port Campbell Limestone|23322|5|Briefly described|957 Fig.2|Miocene|Miocene|Of the Heytesbury Group.  Geological Province: Otway Basin.||||||07-SEP-09
15462|Port Campbell Limestone|23768|5|Briefly described|p28 Fig. 5, p30 Fig.6|||Contains Rutledge Creek Member.  Geological Province: Otway Basin. See also p131 and p162.||||||30-MAR-05
15462|Port Campbell Limestone|23909|5|Briefly described|p291|Miocene|Miocene|Geological Province: Otway Basin.  See also p290 Fig. 3.||||||
15462|Port Campbell Limestone|24056|5|Briefly described|p84 Fig. 2|Pliocene|Miocene|Of Heytesbury Group.  Geological Basin: Otway Basin.||||||
15462|Port Campbell Limestone|24551|5|Briefly described|p292 Fig. 10.3, p732 Table 17.2|||Max thickness: 250m.||||||
15462|Port Campbell Limestone|24562|5|Briefly described|p8 Fig. 2|Miocene|Miocene|Of the Heytesbury Group.  Geological Province: Otway Basin.||||||
15462|Port Campbell Limestone|29425|6|Mentioned|p103|||||||||
15462|Port Campbell Limestone|29591|6|Mentioned|p98|||||||||
15462|Port Campbell Limestone|29823|6|Mentioned|p14|||||||||
15462|Port Campbell Limestone|29825|5|Briefly described|p18|||||||||
15462|Port Campbell Limestone|29856|6|Mentioned|p36|||||||||
15462|Port Campbell Limestone|30576|6|Mentioned|Table 2|||||||||
15462|Port Campbell Limestone|30578|5|Briefly described|p12|||||||||
15462|Port Campbell Limestone|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
15462|Port Campbell Limestone|30675|5|Briefly described|p253|||Lithology and radioactivity.||||||07-MAR-07
15462|Port Campbell Limestone|30728|6|Mentioned|p4|||||||||
15462|Port Campbell Limestone|30932|6|Mentioned|Map legend|Miocene|Miocene|Part of Heytesbury Gp. Equivalent Gambier Lst. (in part)||||||
15462|Port Campbell Limestone|31036|1|Redefined|p213|Tertiary|Tertiary|See also Table 9-1. Unit of Heytesbury Group.||||||07-MAR-07
15462|Port Campbell Limestone|31516|6|Mentioned|p49|||||||||
15462|Port Campbell Limestone|31534|6|Mentioned|p363|||See also Table 19-3||||||
15462|Port Campbell Limestone|31583|6|Mentioned|p18|||Section||||||
15462|Port Campbell Limestone|31625|6|Mentioned|Fig. 5.2|||Miocene||||||
15462|Port Campbell Limestone|31922|6|Mentioned|Fig.2|||||||||
15462|Port Campbell Limestone|32102|6|Mentioned|p177|||Miocene||||||
15462|Port Campbell Limestone|32120|6|Mentioned|p280|||Miocene fauna||||||
15462|Port Campbell Limestone|32233|6|Mentioned|p22|||||||||
15462|Port Campbell Limestone|32499|6|Mentioned|p107|||Miocene||||||
15462|Port Campbell Limestone|32601|6|Mentioned|p692|||||||||
15462|Port Campbell Limestone|32852|6|Mentioned|p15|||||||||
15462|Port Campbell Limestone|33135|5|Briefly described|p17|||||||||
15462|Port Campbell Limestone|33136|6|Mentioned|p17|||||||||
15462|Port Campbell Limestone|33155|5|Briefly described|p124|||||||||
15462|Port Campbell Limestone|33807|6|Mentioned|p97|||||||||
15462|Port Campbell Limestone|34360|6|Mentioned|p11|||||||||
15462|Port Campbell Limestone|34832|6|Mentioned|p23|||||||||
15462|Port Campbell Limestone|34954|6|Mentioned|Fig.35|||Analysis Fig.33.||||||
15462|Port Campbell Limestone|34988|6|Mentioned|p292|||||||||
15462|Port Campbell Limestone|34993|6|Mentioned|p300|||||||||
15462|Port Campbell Limestone|35271|6|Mentioned|Fig.2|||||||||
15462|Port Campbell Limestone|35274|6|Mentioned|Table12.18|||||||||
15462|Port Campbell Limestone|35285|5|Briefly described|p414|||||||||
15462|Port Campbell Limestone|35625|6|Mentioned|Fig.1|||||||||
15462|Port Campbell Limestone|35722|6|Mentioned|p4|||Stratigraphy.||||||
15462|Port Campbell Limestone|36119|6|Mentioned|p56|||||||||
15462|Port Campbell Limestone|36913|6|Mentioned|p79|||See also p81.||||||07-MAR-07
15462|Port Campbell Limestone|37583|6|Mentioned|p158|||||||||
15462|Port Campbell Limestone|37585|6|Mentioned|p40|||||||||
15462|Port Campbell Limestone|37587|6|Mentioned|p34|||||||||
15462|Port Campbell Limestone|38150|6|Mentioned|p23|||||||||
15462|Port Campbell Limestone|38625|6|Mentioned|Table 2|||||||||
15462|Port Campbell Limestone|41016|5|Briefly described|Table 1|||||||||
15462|Port Campbell Limestone|41043|6|Mentioned|p97|||||||||
15462|Port Campbell Limestone|41075|6|Mentioned|p18|||||||||
15462|Port Campbell Limestone|41076|6|Mentioned|p59|||||||||
15462|Port Campbell Limestone|41185|6|Mentioned|Fig.4|||||||||
15462|Port Campbell Limestone|41269|6|Mentioned|Fig.2|||||||||
15462|Port Campbell Limestone|41519|6|Mentioned|p168|||||||||
15462|Port Campbell Limestone|41538|6|Mentioned|p304|||||||||
15462|Port Campbell Limestone|41642|6|Mentioned|Fig.8.6|||||||||
15462|Port Campbell Limestone|41701|6|Mentioned|Map legend|Miocene||||||||
15462|Port Campbell Limestone|41704|6|Mentioned|Fig.3|||||||||
15462|Port Campbell Limestone|41714|6|Mentioned|p301|||||||||
15462|Port Campbell Limestone|41726|6|Mentioned|Fig.5|||||||||
15462|Port Campbell Limestone|41769|4|Described|p33|||||||||
15462|Port Campbell Limestone|41848|6|Mentioned|p367|||underlies Bridgewater Formation||||||
15462|Port Campbell Limestone|41868|5|Briefly described|p577|||Mention p548 and Fig.12.30.||||||07-MAR-07
15462|Port Campbell Limestone|42079|6|Mentioned|Fig.2 P264|||See also Fig.10, p272.||||||
15462|Port Campbell Limestone|42318|5|Briefly described|p8|||||||||
15462|Port Campbell Limestone|42473|6|Mentioned|p60|||||||||
15462|Port Campbell Limestone|42524|5|Briefly described|Fig.3 P27|||||||||
15462|Port Campbell Limestone|42635|5|Briefly described|p90|||(Gambier Limestone)||||||
15462|Port Campbell Limestone|42827|3|Fully described|p286|||See also Fig 8.7.||||||07-MAR-07
15462|Port Campbell Limestone|42863|5|Briefly described|Fig.14|||||||||
15462|Port Campbell Limestone|43171|6|Mentioned|5-8|||Of Heytesbury Group. Age: 10-20Ma||||||
15462|Port Campbell Limestone|43208|5|Briefly described|map legend|Late Miocene|Early Miocene|Of Heytesbury Group||||||
15462|Port Campbell Limestone|43219|5|Briefly described|Fig.3,p6.||Miocene|Of Heytesbury Group||||||07-MAR-07
15462|Port Campbell Limestone|43590|4|Described|p26|Late Miocene|Middle Miocene|||||||
15462|Port Campbell Limestone|43604|4|Described|p144|Pliocene|Miocene|||||||
15462|Port Campbell Limestone|43660|6|Mentioned|Fig.6,p15||Oligocene|||||||
15462|Port Campbell Limestone|43667|6|Mentioned|Fig.3,p12|Late Miocene|Middle Miocene|||||||
15462|Port Campbell Limestone|43733|6|Mentioned|Fig.2.11,p65||Miocene|||||||
15462|Port Campbell Limestone|43744|6|Mentioned|Fig.3,p3|||||||||
15462|Port Campbell Limestone|43937|5|Briefly described|Map Legend|Early Oligocene|Middle Eocene|||||||
15462|Port Campbell Limestone|45160|6|Mentioned|p6|||||||||
15462|Port Campbell Limestone|48581|14|Not recorded|p13,14|||||||||
15462|Port Campbell Limestone|48911|6|Mentioned|p27|||See also Chart 1||||||
15462|Port Campbell Limestone|48977|6|Mentioned|Fig.5|||||||||
15462|Port Campbell Limestone|50154|5|Briefly described|p135|||Of Heytesbury Group.||||||
15462|Port Campbell Limestone|60299|5|Briefly described|p228 Tb.5|Miocene|Miocene|Age: 12 Ma. Palaeopole position given.||||||
15462|Port Campbell Limestone|60538|5|Briefly described|p471 Fig. 10|||||||||
15462|Port Campbell Limestone|60563|5|Briefly described|p46|||Of the Heytesbury Group. Overlies the Gellibrand Marl. Shelfal bioclastic calcarenite facies.||||||
15462|Port Campbell Limestone|60785|5|Briefly described|p184 Fig.1, p186, p188.  |Messinian|Langhian|Of the Otway Basin. Foraminifera zones N10-N17(Holdgate and Gallagher, 2003). Has yielded  partial skeletons, and a fairly well-preserved posterior part of the mandible of a fossil cetacean, with two large conical teeth in place.|||Includes Bochara Limestone Member and Muddy Creek Marl Member.|Unconformably underlies the Rocklands Rhyolite.|Yellow fine-grained calcarenite.|
15462|Port Campbell Limestone|61136|6|Mentioned|p18, p27|Miocene|Miocene|Carbonate sediments. Lady Julia Island, which is a volcanic remnant, rests on this unit.||||||
15462|Port Campbell Limestone|61155|5|Briefly described|p18|Late Miocene|Middle Miocene|Of the Heytesbury Group. Contains the Rutledge Marl Member. Overlies Gellibrand Marl. Age: ~15-5.5Ma. Max. thickness: 550m. Geological Province: Otway Basin (Tyrendarra and Port Campbell Embayments).||||||07-MAR-07
15462|Port Campbell Limestone|61181|5|Briefly described|p134|Miocene|Miocene|Comprises limestone, clayey limestone, marl and calcareous clay. Overlies Gellibrand Marl. ||||||
15462|Port Campbell Limestone|61182|3|Fully described|p28, p29, p33, p178|Late Miocene|Middle Miocene|Of Heytesbury Group. Formerly subdivided into Rutledges Creek, Port Campbell and Peterborough beds (Baker 1950) also referred to as members. Overlies Gellibrand Marl; usually overlain disconformably by Hanson Plain Sand. Calcisiltite and calcarenite.||||||23-MAY-13
15462|Port Campbell Limestone|61623|6|Mentioned|p449 Fig. 4|Miocene|Miocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-APR-09
15462|Port Campbell Limestone|61624|5|Briefly described|p465, p466, p466 Fig. 2|Middle Miocene|Early Miocene|Of Haytesbury Group. Underlain by Clifton Formation. Geological Province: Otway Basin.||||||07-APR-09
15462|Port Campbell Limestone|61626|5|Briefly described|p487, p486 Fig. 2, p489 Fig. 5|Miocene|Miocene|Geological Province: Otway Basin.||||||07-APR-09
15462|Port Campbell Limestone|61628|5|Briefly described|p509 Fig. 3|Late Miocene|Middle Miocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-APR-09
15462|Port Campbell Limestone|61896|5|Briefly described|p57|Miocene|Miocene|Locally unconformably overlain by Moorabool Viaduct Formation.||||||19-DEC-07
15462|Port Campbell Limestone|62068|5|Briefly described|p134,135, p135 Fig.2,p136,p137,|Miocene|Miocene|Has karst topography on upper surface.||||Overlain by Whalers Bluff Formation. Unconformably overlain by Hanson Plain Sands. Same as, or equivalent to, Portland Limestone.|Pale yellow, horizontally bedded, shallow marine limestones in Childers Cove.|
15462|Port Campbell Limestone|63269|5|Briefly described|p605|Miocene|Miocene|Otway Basin.||Heytesbury Group.||||
15462|Port Campbell Limestone|66002|4|Described|p13 Tb.9, p26 Fig.7|Neogene|Neogene|Of Heytesbury Group. Modified from Port Campbell Beds of Baker (1950). Defined by Glenie 1971. Calcarenite, minor calcilutite, generally fine-grained. Minor coarse-grained calcarenite, quartz sand and clayey silt. Weakly cemented. Moderately well bedded. Some fossils||||||
15462|Port Campbell Limestone|66012|4|Described|p18|Miocene|Miocene|Of Heytesbury Group. Overlies Gellibrand Marl. Early to middle Miocene| | | | | |13-JUN-13
15462|Port Campbell Limestone|66245|5|Briefly described|p6 Fig.5. |Messinian|Serravallian|||Unit in Heytesbury Group.||Overlies Gellibrand Marl.||
15462|Port Campbell Limestone|67061|6|Mentioned|p546 Fig.3.|Miocene|Miocene|||Unit in Heytesbury Group.||||
15462|Port Campbell Limestone|67366|5|Briefly described|p103 Fig.2. |Miocene|Miocene|||Unit in Heytesbury Group.||Overlies Gellibrand Marl.|Shallow to open marine limestone.|
15462|Port Campbell Limestone|67367|5|Briefly described|p131 Fig.2. |Late Miocene|Middle Miocene|||Unit in Heytesbury Group.||||
15462|Port Campbell Limestone|68116|5|Briefly described|Appendix, Maps 47-49, 54-55.|Miocene|Miocene||||||Calcarenite, minor calcilutite: generally fine-grained; bryozoan, mollusc, echinoid and brachiopod fragments, minor coarse-grained calcarenite, quartz sand and clayey silt; weakly cemented, moderately bedded; continental shelf deposit.|
15462|Port Campbell Limestone|68991|5|Briefly described|p465, p465 Fig.2, p466|Miocene|Miocene|Cliff-forming unit with a middle to upper Miocene age. Maximum thickness: 297 m. An irregular solution surface occurs on the Port Campbell Limestone.||||Conformably underlain by the Gellibrand Marl. Disconformably overlain by the Hesse Clay. Unconformably overlain by the Hanson Plain Sand. Disconformably overlain by the Bridgewater Formation.|Comprises marine, grey to yellow calcisiltite to fine-grained calcarenite with minor interbeds of medium- to coarse-grained calcarenite.|
15462|Port Campbell Limestone|69297|5|Briefly described|p79, p98|Serravallian|Serravallian|Otway Basin. ||Heytesbury Group||Overlies the Gellibrand Marl. Unconformably overlain by the Hanson Plain Sand. |Limestones. |
15462|Port Campbell Limestone|69651|5|Briefly described|p10|Miocene|Miocene|||Heytesbury Group.||Overlies Gellibrand Marl. Is overlain unconformably by Hanson Plain Sand.||
15462|Port Campbell Limestone|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Miocene|Miocene|Otway Basin: Port Campbell Embayment.||Heytesbury Group.||Overlies Gellibrand Marl. Is overlain by Hanson Plain Sand.||
15462|Port Campbell Limestone|70880|6|Mentioned|p77|Miocene|Miocene|Otway Basin.||||||
15462|Port Campbell Limestone|70909|6|Mentioned|p63|||||||||
15462|Port Campbell Limestone|70942|4|Described|p127, 119|||See correlation table.||||||
15462|Port Campbell Limestone|71266|6|Mentioned|p614 Fig.3|Miocene|Miocene|Otway Basin.||||||
15462|Port Campbell Limestone|71419|6|Mentioned|p16 Fig 17|Miocene|Miocene|Shallow marine sediments.||||||
15462|Port Campbell Limestone|71437|4|Described|Fig. 1 opp 154, p155, p161-162|Miocene|Miocene|marine, deep neritic.||Of Heytesbury Group.||Laterally continuous with Portland Limestone Member.|Pure to marly limestone, minor chert.|
15462|Port Campbell Limestone|72445|5|Briefly described|App.1, App.2.|||App.2 is a .csv format file. Identified in Stavely 01.||Heytesbury Group||Conformably overlies Gellibrand Marl. Conformably overlain by Loxton Sand.|Includes sandy to muddy calcareous marl with some muddier sections and abundant shell fragments in Stavely 01.|
15462|Port Campbell Limestone|73357|5|Briefly described|p30, p46, p48|Tortonian|Langhian|Otway Basin. Correlated with Operculodinium Dinocyst Superzone and Triporopollenites bellus Spore-Pollen Zone, nearshore to offshore marine depositional environments.||Of Heytesbury Group.||Overlies Gellibrand Marl.||
15462|Port Campbell Limestone|73383|5|Briefly described|p2-3, p10 Tb.3.8, p25, p28, p164, p236|Miocene|Miocene|Otway Basin. Approximately equivalent to chemostratigraphic package S6-P4 which has high Ca, Cr/Nb and Sc/Rb values. Includes limestone and Fe-shale based on geochemistry. See also vi, p11 Tb.3.9, p34, p107, p130, p257.||Heytesbury Group||Overlies Gellibrand Marl|Limestones.|
15462|Port Campbell Limestone|73385|5|Briefly described|p5|Miocene|Miocene|Otway Basin.||Heytesbury Group||Overlies Gellibrand Marl, underlies Bridgewater Formation.|Shallow to open marine limestones.|
15462|Port Campbell Limestone|73386|5|Briefly described|p4, p6, p14, Attachment A1|Tortonian|Langhian|Otway Basin. Shallow to open marine depositional environments, outer shelf water depths during peak transgressions and at mid to inner shelf depths during regressions. Upper part records continuous sea level fall. Correlates with Triporopollenites bellus Spore-Pollen Zone.||Heytesbury Group||Overlies Gellibrand Marl|Limestones.|
15462|Port Campbell Limestone|73486|4|Described|p509-514, p516-523, p525-531, p533-535|Messinian|Serravallian|Otway Basin. Thickness of up to 297 m in the Port Campbell Embayment. Gradational transition with Gellibrand Marl. Contains decametre-scale cycles, and thin repetitive third-order cycles of shoaling-upward character. Oxic-suboxic to euxinic/anoxic depositional environment. Common to abundant foraminifera of middle to outer shelf species, and inner to middle shelf species in upper part. Sequence was emergent at ca 13.2 Ma. Uppermost weathered surface is a pisolitic ferricrete crust atop oxidised ferruginous carbonate sand.|15-10.5 Ma (foraminifera)|Heytesbury Group||Overlies Gellibrand Marl with gradational transition, underlies Hesse Clay|Grey fine-grained unconsolidated to semi-consolidated bioclastic muddy carbonate sands and limey marls, uniform appearance, upper weathered zone. Predominantly calcite, minor siliciclastics and glauconitic carbonate mud. Texturally variable.|
15462|Port Campbell Limestone|73594|5|Briefly described|p4|Miocene|Miocene|Otway Basin.||Heytesbury Group||Overlies Gellibrand Marl|Marine limestones.|
15469|Port Fairy Calcarenite|24551|6|Mentioned|p343|||Of the Bridgewater Group.||||||
15469|Port Fairy Calcarenite|29425|6|Mentioned|p103|||||||||
15469|Port Fairy Calcarenite|30993|6|Mentioned|p148|||See also p149-153. Radiocarbon dates.||||||13-MAR-07
15469|Port Fairy Calcarenite|31003|6|Mentioned|p41|||||||||
15469|Port Fairy Calcarenite|31004|6|Mentioned|p395|||||||||
15469|Port Fairy Calcarenite|31007|6|Mentioned|p254|||See also Fig.1. Age 125,000 years||||||
15469|Port Fairy Calcarenite|32102|6|Mentioned|p177|||||||||
15469|Port Fairy Calcarenite|34988|6|Mentioned|p295|||||||||
15469|Port Fairy Calcarenite|34993|3|Fully described|p300|||||||||
15469|Port Fairy Calcarenite|35722|6|Mentioned|Table 2|||Quaternary stratigraphic units and nature of components.||||||
15469|Port Fairy Calcarenite|37583|4|Described|p164|||||||||
15469|Port Fairy Calcarenite|41701|6|Mentioned|Map legend|Pleistocene||||||||
15469|Port Fairy Calcarenite|41769|4|Described|p53|||||||||
15469|Port Fairy Calcarenite|41848|4|Described|p375|||Age 110000 - 125000 yrs U-Th shells||||||
15469|Port Fairy Calcarenite|42827|4|Described|p375|||see also Table 9.4||||||
15469|Port Fairy Calcarenite|73386|6|Mentioned|p14|||||Bridgewater Formation||||
15470|Port Grinder beds|30570|6|Mentioned|p4|||||||||
15479|Port Melbourne Sand|23237|6|Mentioned|p103|||||||||
15479|Port Melbourne Sand|23537|6|Mentioned|Fig 7 p 449|||||||||
15479|Port Melbourne Sand|24551|5|Briefly described|p346, p734 Table 17.4|Quaternary|Quaternary|Overlies: Brighton Group.  Max thickness: 12m.||||||
15479|Port Melbourne Sand|30986|5|Briefly described|p197|||Holocene||||||
15479|Port Melbourne Sand|33604|5|Briefly described|p25|||||||||
15479|Port Melbourne Sand|35011|3|Fully described|p314|||||||||
15479|Port Melbourne Sand|41848|4|Described|p392|||Younger than Coode Island Silt||||||
15479|Port Melbourne Sand|42827|4|Described|p392|||||||||
15479|Port Melbourne Sand|60083|5|Briefly described|Map legend|Recent|Recent|Fossiliferous sand, sometimes showing cross-bedding.||||||
15479|Port Melbourne Sand|71277|4|Described|p301, p303-314, p316|Quaternary|Quaternary|Lucas (1887). A component of the Yarra Delta; mainly S of the present Yarra River. Formed sand ridges (subsequently destroyed by industrialisation). 5-28m thick (isopach map). Several 14C ages tabulated.|8075 - 2760 yrs BP (14C shells).|Yarra Delta Group.||Overlies Coode Island Silt.|Yellow-brown, fine- to medium-grained sand, sometimes shelly (more commonly in the lower beds) and carbonaceous. Rare peat beds in the upper part. Variably calcareous.|
27882|Portland Limestone|24551|6|Mentioned|p300|||Of the Heytesbury Group.||||||
27882|Portland Limestone|29591|6|Mentioned|p91|||||||||
27882|Portland Limestone|30993|6|Mentioned|p160|||Miocene||||||
27882|Portland Limestone|31372|6|Mentioned|Fig. 2|||||||||
27882|Portland Limestone|31424|4|Described|p14|||See also p7. Described from core.||||||20-FEB-18
27882|Portland Limestone|31624|6|Mentioned|p101|||||||||
27882|Portland Limestone|33160|6|Mentioned|p302|||||||||
27882|Portland Limestone|48911|6|Mentioned|Chart 1|||||||||
27882|Portland Limestone|50079|5|Briefly described|p46|||Eroded sediments from this unit make up the sediments of Nelson Bay Formation.||||||
27882|Portland Limestone|62068|5|Briefly described|p135|Miocene|Miocene|||||Same as, or equivalent to, the Port Campbell Limestone. Is overlain by the Whalers Bluff Formation||
30690|Post Office Granite|22968|6|Mentioned|P210||Late Silurian|Parent is Bingo Munjie Suite||||||
30690|Post Office Granite|23309|6|Mentioned|p441 App1|||G113 - I-Type.||||||
30690|Post Office Granite|44184|5|Briefly described|Map Legend||Early Silurian|||||||
30690|Post Office Granite|60503|3|Fully described|p165, p43 Tb. 2|Early Devonian|Early Devonian|Of the Bingo Munjie Suite. Overlain by the Eight Mile Loop Rhyolite. Also referred to as the Post Office pluton and "The Knocker". Two phase intrusion; hornblende-bearing phase; and, a felsic phase composed mostly of quartz, alkali-feldspar, plagioclase.||||||23-JUN-14
30690|Post Office Granite|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Granite, mainly granite soil: I-type; may be felsic phase of Bingo Munjie Quartz Diorite.||||||
30690|Post Office Granite|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Granite, mainly granite soil: I-type; may be felsic phase of Bingo Munjie Quartz Diorite.||||||
30690|Post Office Granite|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Granite, mainly granite soil: I-type; may be felsic phase of Bingo Munjie Quartz Diorite.||||||
30690|Post Office Granite|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Granite, mainly granite soil: I-type; may be felsic phase of Bingo Munjie Quartz Diorite.||||||
30690|Post Office Granite|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Bingo Munjie Suite. Granite: I-type; highly magnetic (300-400 nT) and moderately magnetic (50-100 nT) phases; low total count, K, Th, U||||||
30690|Post Office Granite|68116|5|Briefly described|Appendix, Map 27.|Early Devonian|Early Devonian||||||Biotite granite, hornblende-biotite diorite; mainly granite soil: may be felsic phase of Bingo Munjie Quartz Diorite.|
23919|Postman Spur Granodiorite|22876|5|Briefly described|p28|||||||||
23919|Postman Spur Granodiorite|22877|5|Briefly described|map|Silurian|Silurian|G59. Biotite granodiorite. A-Type.||||||26-OCT-04
23919|Postman Spur Granodiorite|23309|6|Mentioned|p441 App1|||G59 - S-Type.||||||
23919|Postman Spur Granodiorite|23615|3|Fully described|p158|Early Devonian|Early Silurian|See also p201 App. 1.  Small, circular body of S-type granite with cordierite and abundant schist and gneiss inclusions, and accessory zircon, apatite and opaques.||||||
23919|Postman Spur Granodiorite|24551|6|Mentioned|p234|||||||||
23919|Postman Spur Granodiorite|42627|5|Briefly described|Map legend|Wenlock|Wenlock|Probably not Variation on Postmans Creek Granodiorite, NSW.||||||
23919|Postman Spur Granodiorite|42647|4|Described|p47|||||||||
23919|Postman Spur Granodiorite|43206|5|Briefly described|map legend||Wenlock|Biotite granodiorite: grey, medium grained; rare cordierite; with abundant gneissic and schistose enclaves.||||||08-SEP-04
23919|Postman Spur Granodiorite|44185|5|Briefly described|Map legend.|Silurian|Silurian|S-type.||||||
23919|Postman Spur Granodiorite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Biotite-cordierite granodiorite: medium grained, abundant inclusions of gneiss and schist; S-type.|
34430|Powncebys Tonalite|22756|5|Briefly described|P47|||||||||
34430|Powncebys Tonalite|23309|6|Mentioned|p441 App1|||G367 - I-Type.||||||
34430|Powncebys Tonalite|43260|5|Briefly described|Map Legend||Early Devonian|of Glenlogie Suite. Biotite-hornblende tonalite: mafic; grey speckled appearance; medium grained; pronounced magmatic flow banding defined by elongate feldspar crystals.||||||27-OCT-04
34430|Powncebys Tonalite|66002|5|Briefly described|p7 Tb.5|||Of Glenlogie Suite. G367.  Defined by Cayley and McDonald 1995.||||||
34430|Powncebys Tonalite|68116|5|Briefly described|Appendix, Map 31.|Early Devonian|Early Devonian||||||Biotite-hornblende tonalite: mafic; grey speckled appearance; medium grained; pronounced magmatic flow banding defined by elongate feldspar crystals.|
15555|Pretty Hill Formation|12781|6|Mentioned|p386|Early Cretaceous|Early Cretaceous|Otway Basin. Maximum thickness 1585m.||Crayfish Group.||Unconformably overlies Casterton Formation. Is overlain by Laira Formation.||
15555|Pretty Hill Formation|22480|6|Mentioned|5||Early Cretaceous|Otway Basin||||||
15555|Pretty Hill Formation|22495|6|Mentioned|P220|||||||||
15555|Pretty Hill Formation|22674|4|Described|p718, Fig.2 p719|Barremian|Berriasian|||||||
15555|Pretty Hill Formation|22686|6|Mentioned|Fig3p745,747|Hauterivian|Portlandian|Max Age: 141 Ma; Min Age: 123 Ma.  Geological Province: Otway Basin.||||||17-JAN-06
15555|Pretty Hill Formation|22875|3|Fully described|p33|Aptian|Valanginian|Of the Crayfish Group||||||18-FEB-08
15555|Pretty Hill Formation|22924|5|Briefly described|51|||||||||
15555|Pretty Hill Formation|22930|6|Mentioned|50|||||||||
15555|Pretty Hill Formation|23356|5|Briefly described|26 Tab.2|Early Cretaceous|Late Jurassic|||||||
15555|Pretty Hill Formation|23427|5|Briefly described|Table 11.2 p418.|||||||||
15555|Pretty Hill Formation|24209|5|Briefly described|p151|Valanginian|Berriasian|Comprises interbedded litharenties and shales.  See also p158 Fig. 7.||||||
15555|Pretty Hill Formation|24314|5|Briefly described|p61 Fig.2|Early Cretaceous|Early Cretaceous|Geological Province: Otway Basin. Max. Thickness ?5000m. Of the Otway Supergroup.||||||30-NOV-04
15555|Pretty Hill Formation|24453|5|Briefly described|p809 Fig.2|Hauterivian|Berriasian|Of Crayfish Subgroup. Geological Province: Otway Basin.||||||07-FEB-11
15555|Pretty Hill Formation|24562|5|Briefly described|p8 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Crayfish Group.  Geological Province: Otway Basin.||||||
15555|Pretty Hill Formation|41269|5|Briefly described|p244|||||||||
15555|Pretty Hill Formation|41454|6|Mentioned|Fig.6|||||||||
15555|Pretty Hill Formation|41714|6|Mentioned|Fig.2|||||||||
15555|Pretty Hill Formation|42075|5|Briefly described|Fig.13 P252|||||||||
15555|Pretty Hill Formation|42150|6|Mentioned|p69|||||||||
15555|Pretty Hill Formation|42153|5|Briefly described|p352|||See also Fig.2||||||
15555|Pretty Hill Formation|43171|6|Mentioned|5-8|||Of Crayfish Group. Age: 135-145 Ma||||||
15555|Pretty Hill Formation|43195|5|Briefly described|Map Legend||Early Cretaceous|See also commentary on back of map.Of Crayfish Group.||||||
15555|Pretty Hill Formation|43219|5|Briefly described|Fig.3,p6.|Aptian|Valanginian|Of Otway Group.||||||16-DEC-08
15555|Pretty Hill Formation|43744|6|Mentioned|Fig.3,p3|||||||||
15555|Pretty Hill Formation|43937|5|Briefly described|Map Legend|Aptian|Kimmeridgian|||||||
15555|Pretty Hill Formation|44133|5|Briefly described|p144|Early Cretaceous|Early Cretaceous|Previously called 'Geltwood Beach Formation'. Thickness: 1585m.||||||
15555|Pretty Hill Formation|50154|6|Mentioned|p44|||Also known as the Crayfish Subgroup.||||||
15555|Pretty Hill Formation|60126|6|Mentioned|p4|||Basal unit overlain by Casterton Formation?||||||25-JAN-06
15555|Pretty Hill Formation|60452|6|Mentioned|p14|Late Cretaceous|Late Jurassic|Outwash fan and braided stream deposits. In the Bassian Rift.||||||
15555|Pretty Hill Formation|60599|6|Mentioned|p84|||Outwash fan and braided stream deposits. Geological Province: Otway Basin. ||||||
15555|Pretty Hill Formation|61017|5|Briefly described|p5 Fig. 2|Barremian|Bernasian|Of the Crayfish Subgroup (Otway Group). Includes shales with hydrocarbon potential as source rocks. Geological Province: Otway Basin.||||||07-FEB-11
15555|Pretty Hill Formation|61182|3|Fully described|p11-12, p72|Aptian|Valanginian|Of Otway Group.Together with Eumeralla Formation, unconformable over Casterton Formation or over palaeozoic bedrock; unconformably overlain by Eumeralla Formation. Mainly quartz sandstone (lower part) with minor mudstone (upper). Geol.Prov: Otway Basin.||||||04-FEB-08
15555|Pretty Hill Formation|61185|5|Briefly described|p56|Early Cretaceous|Late Jurassic|Deposits of scree, outwash fan and braided streams (Tickell et al. 1992). Geological Province: Otway Basin.||||||07-FEB-11
15555|Pretty Hill Formation|61470|5|Briefly described|p28 Fig. 5|Barremian|Berriasian|Of the Crayfish Subgroup (Otway Group). Underlies Laira Formation. Geological Province: Otway Basin.||||||12-OCT-05
15555|Pretty Hill Formation|61547|6|Mentioned|p461 Fig.2, p462, p465, p468, p472.|Valanginian|Berriasian|||Basal unit in Crayfish Group.|Includes Lower and Upper Sawpit Shale Members, Sawpit Sandstone Member, and Pretty Hill Sandstone Member.|Overlies Casterton Formation. Is overlain by Laira Formation.||
15555|Pretty Hill Formation|61618|6|Mentioned|p425, p433|||Laterally variable braided-fluvial deposit.||||||
15555|Pretty Hill Formation|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-FEB-11
15555|Pretty Hill Formation|61623|6|Mentioned|p447, p451, p449 Fig. 4|Early Cretaceous|Early Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-APR-09
15555|Pretty Hill Formation|61626|5|Briefly described|p486 Fig. 2|Early Cretaceous|Early Cretaceous|Of Crayfish Group. Geological Province: Otway Basin.||||||07-APR-09
15555|Pretty Hill Formation|61627|5|Briefly described|p500 Fig. 2|Early Cretaceous|Early Cretaceous|Of Crayfish Group. Overlian by Laria Formation, Underlain by Casterton Formation. Geological Province: Otway Basin.||||||07-FEB-11
15555|Pretty Hill Formation|61628|5|Briefly described|p509 Fig. 3|Early Cretaceous|Early Cretaceous|Of Crayfish Subgroup. Geological Province: Otway Basin.||||||07-APR-09
15555|Pretty Hill Formation|63122|5|Briefly described|p17 Fig. 4.3|Hauterivian|Berriasian|Of the Crayfish Group. Max. thickness: >1585m. Geological Province: Otway Basin. ||||||
15555|Pretty Hill Formation|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p58-59|Valanganian|Berriasian|Of Crayfish Gp (Otway Supergp). Unconformable on Casterton Fm; conformable below Laira Fm. Contains mineralogically complex grey-green litharenite to feldspathic litharenite with siltstone interbeds. Age:140-133Ma. Max.thick:?5000m. Geol.Prov: Otway Basin||||||
15555|Pretty Hill Formation|63125|5|Briefly described|p105, p116 Tb. 7.6|||Overlies the Casterton Formation. Geological Province: Otway Basin. Basal section predominantly more shaly and referred to as "unnamed basal shale"; remainder of formation comprises interbedded sandstone, siltstone and shale with rare coal laminae. ||||||
15555|Pretty Hill Formation|63129|5|Briefly described|p127|Early Cretaceous|Early Cretaceous|Of the Otway Supergroup. Thickness: up to 875m in Ladbroke Grove 1. Geological Province: Otway Basin. Good porosity which creates good reservoir conditions.||||||17-JUN-09
15555|Pretty Hill Formation|63130|5|Briefly described|p141|||Of the Crayfish Group. Geological Province: Otway Basin.||||||06-FEB-08
15555|Pretty Hill Formation|63267|5|Briefly described|p483-486, p491-493, p495-497|Early Cretaceous|Early Cretaceous|Main reservoir in the Penola Trough, Otway Basin; also source potential (elaborated). Low-sinuosity braided-fluvial deposits. Wireline log. Apparently regarded as interchangeable with Pretty Hill Sandstone (see references p488-490, p492-495). Also appears as Pretty Formation on p495. Significance of faults discussed.||Crayfish Group.||Unconformably overlies Casterton Formation. Is overlain transitionally by Laira Formation.|Grey-green litharenites to feldspathic litharenites.|
15555|Pretty Hill Formation|63269|5|Briefly described|p604-605, p607, p616, p618|Early Cretaceous|Early Cretaceous|Otway Basin. Most of this unit in the Penola Trough axis has remained in the gas generation window since latest Cretaceous. Details of natural gas, oils and oil stains in named wells tabulated. Oil-source correlation. Biomarker diagram. Appears as Pretty Hill Sandstone on p606.||Crayfish Subgroup.||||
15555|Pretty Hill Formation|63431|5|Briefly described|p676, p677 Fig. 2|Valanginian|Berriasian|Basal unit of the Crayfish Group. Geological Province: Penola Trough/Otway Basin. See also p680.||||||07-FEB-11
15555|Pretty Hill Formation|66245|5|Briefly described|p6 Fig.5. |Barremian|Berriasian|Also witten as Pretty Hill sst.||Unit in Crayfish Subgroup.||Is overlain by Laira Formation.|Includes porous sandstones.|
15555|Pretty Hill Formation|67367|5|Briefly described|p131 Fig.2, p132. |Barremian|Berriasian|Has fair hydrocarbon source rock potential, with an average total organic carbon content of 1.7%.||Unit in Crayfish Subgroup.||Is overlain conformably by Laira Formation.||
15555|Pretty Hill Formation|67541|6|Mentioned|p76, p76 Fig.1, p79, p85|||Of the Katnook reservoir (Otway Basin Australia).|||||Comprises chlorite/zeolite-rich sandstone.|
15555|Pretty Hill Formation|69297|5|Briefly described|p79, p98, p100, p101, p104|Hauterivian|Hauterivian|Otway Basin. ||Crayfish Subgroup||Overlies the Sawpit Shale and Sawpit Sandstone. Overlain by the Laira Formation. |Siltstone. |
15555|Pretty Hill Formation|69651|5|Briefly described|p10|Early Cretaceous|Early Cretaceous|||Crayfish Subgroup.||Unconformably overlies Casterton Formation. Is overlain by Laira Formation.||
15555|Pretty Hill Formation|69948|6|Mentioned|Fig.4.2|||Otway Basin (a rift basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Eromanga Basin (an intracratonic basin).||||Is overlain by Laira Formation.||
15555|Pretty Hill Formation|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4; p4, p8-9|Early Cretaceous|Early Cretaceous|See also Regional: p11-12. Otway Basin: Port Campbell Embayment and Robe-Penola Trough. Predominantly fluvial sediments. A major play fairway in SA part of Otway Basin; a producing unit in Katnook, Ladbroke Grove, Haselgrove and Haselgrove South gas fields. Good reservoir characteristics in Victoria. Sealed by Eumeralla Formation.||Crayfish Subgroup.||Overlies Casterton Formation or Sawpit Shale/Sawpit Sandstone. Is overlain by Eumeralla or Laira Formation.||
15555|Pretty Hill Formation|70379|5|Briefly described|p717, p719, p722-729, p731-732|Early Cretaceous|Early Cretaceous|Otway Basin. Widespread distribution across the Basin. Appears as Pretty Hill Sst in Fig.2. Isopach map. Relationship of tectonic activity to sediment accumulation discussed in detail. Late Valanginian to Hauterivian. Shown as Pretty Hill Sandstone in Fig2 p719.|c. 136-133 Ma.|Crayfish Group.||Overlies McEachern Sandstone and Sawpit Sandstone (equivalent). Is overlain by Laira Formation, but replaces it (as a lateral equivalent) in the E of the Basin.|Fluvial sediments.|16-FEB-17
15555|Pretty Hill Formation|70880|6|Mentioned|p77|Hauterivian|Berriasian|Otway Basin.||||||
15555|Pretty Hill Formation|71266|6|Mentioned|p614 Fig.3|Early Cretaceous|Early Cretaceous|Otway Basin.||||||
15555|Pretty Hill Formation|71342|6|Mentioned|Ch4 p9|||Otway Basin. ||||||
15555|Pretty Hill Formation|72050|5|Briefly described|p233 Fig.2, 234-235, 239|Hauterivian|Berriasian|Has produced gas flows.||Crayfish Group.|||Basal cross-bedded conglomerate, quartzose sandstones, and floodplain to lacustrine shales.|
15555|Pretty Hill Formation|73356|2|Defined|p. v-1, p4-7, p9-11, p13-17, p20-29|Hauterivian|Valanginian|Otway Basin. Revised unit; restricted to the sedimentary sequence between the Sawpit Formation and the Laira Formation. Basal boundary marked by an increase in volcanogenic lithics and feldspar. The top of the formation is notably more lithic-rich and the unit is overall less mineralogically mature than the Sawpit Formation. Upper boundary with Laira Formation is gradational and may be diachronous. Represents a fluvial-overbank system. Age constraint is from palynologic biostratigraphy; extends from the Upper R. australiensis to Upper F. wonthaggiensis Spore-Pollen Subzones of Partridge (2006). Previously informally named unit 'R' (Edworthy, 1964), then Pretty Hill Sandstone (Reynolds et al., 1966; etc). Assigned its current name by Yu (1988)[?]. No type section was designated; now defined by the reference section in Casterton-1 between 1309.2 m and 1711.2 m. Particularly thick in the Penola Trough where it reaches a maximum thickness of 1079.6 m (Salamander-1). Intersected in 54 wells across the basin; 28 in Victoria. Significantly sandier in some places. Corresponds to the S1-P5 and S1-P6 chemostratigraphic packages of Forbes et al. (2020). [See article for description of geophysical character].||Crayfish Subgroup, Otway Group||Underlain by Sawpit Formation (conformably) and Casterton Formation (unconformably). Overlain by Laira Formation.|Fine- to coarse-grained quartz sandstone with silty, micaceous and carbonaceous shale and mudstone interbeds and a fine- to medium-grained basal sandstone. Includes chlorite, garnet, mica, poor coal, kaolinite, abundant feldspar, and plant traces.|
15555|Pretty Hill Formation|73357|5|Briefly described|p15-17, p43, p45, p47|Barremian|Berriasian|Otway Basin. Sparse, poorly preserved palynomorph assemblages, or barren of palynomorphs. Correlated to the Foraminisporis wonthaggiensis Zone, brackish/marginal marine indicators. Lower part assigned to the Ruffordiaspora australiensis Spore-Pollen Zone, limited new data to confirm this.||Of Crayfish Subgroup.||Overlies Casterton Formation, underlies Lower Eumeralla Formation.|Contains sandy lithologies.|
15555|Pretty Hill Formation|73383|4|Described|p3, p7 Tb.3.1, p11, p15-16, p38, p42-45|Barremian|Berriasian|Otway Basin. Equivalent to chemostratigraphic packages S1-P1 to S1-P6. The tops of packages S1-P4 and S1-P5 are associated with large and abrupt chemical changes, may represent intra-formation unconformities of unknown type. Subdivided into several informal lithology-based subunits (Sawpit Sandstone, Upper and Lower Sawpit Shale, Pretty Hill Sandstone and others). Lithologies based on geochemistry using the ChemLith classification includes mudstone, siltstone, limestone, calcareous limestone, argillaceous and calcareous sandstones; and using the Herron classification (1988) includes shale, wacke, Fe-shale, Fe-sand, lith-arenite, sublith-arenite, quartz arenite, subarkose and arkose. See also vi, p49-55, p64-65, p95, p100-103, p110-112, p167, p171-175, p179-187, p195-198, p224-225, p229-233, p239-241, p282-295, p331-342.||Crayfish Subgroup|Sawpit Sandstone, Upper Sawpit Shale, Lower Sawpit Shale, Pretty Hill Sandstone|Unconformably overlies Casterton Formation, underlies Windermere Sandstone, Laira Formation|Fluvial channel sandstones. Includes lower sand unit and upper sand/shale unit.|
15555|Pretty Hill Formation|73385|5|Briefly described|p5|Barremian|Valanginian|Otway Basin.||Crayfish Subgroup||Overlies Casterton Formation, underlies Laira Formation, Windermere Sandstone.|Fluvial channel sandstones with lower sand unit and upper sand/shale unit.|
15555|Pretty Hill Formation|73386|4|Described|p4, p6, p8, Attachment A1|Hauterivian|Valanginian|Otway Basin. Extends from upper part of the Upper Ruffordiaspora australiensis Spore-Pollen Subzone to the lower part of the Upper Foraminisporis wonthaggiensis Spore-Pollen Subzone. Corresponds to the S1-P5 to S1-P6 chemostratigraphic packages (Eid et al., 2021a). Revised Pretty Hill Formation defined by a reference section in Casterton-1 from 1309.2 m to 1711.2 m.||Crayfish Subgroup||Conformably overlies Sawpit Formation, underlies Laira Formation|Characterised by a fluvial-overbank system with sandstones which are dominantly litharenites with arkose and subarkose signatures. Some fining upwards sequences and sparsely interbedded shales.|
15555|Pretty Hill Formation|73594|4|Described|p3-4, p14-16, p20, p42, p45-46, p48-51|Barremian|Valanginian|Otway Basin. Fluvial. Originally defined in VIC and is an important hydrocarbon reservoir in the SA part of the Penola Trough. Informal subdivision of lower part introduced by Lovibond et al. (1995) and largely followed in this review. Camac and Boult (2008) further subdivided the Sawpit Shale. See also p8, p53-54, p59, p64, p66.||Crayfish Subgroup|McEachern Sandstone, Sawpit Shale, Sawpit Sandstone, Pretty Hill Sandstone|Overlies Casterton Formation, underlies Katnook Sandstone, Laira Formation, Windermere Sandstone|Includes fine to medium grained sandstones, moderately sorted litharenites and feldspathic litharenites.|
69707|Pretty Valley Suite|61160|5|Briefly described|p62, p58-59 Fig. 6.8|Silurian|Silurian|Includes the Pretty Valley and Bundara Tonalites. I-types. See also p58-59 Fig. 6.8.||||||
69707|Pretty Valley Suite|61161|6|Mentioned|p152|||I-type intrusions.||||||
69707|Pretty Valley Suite|61164|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Pretty Valley Tonalite and Bundara Tonalite.||||||
69707|Pretty Valley Suite|61165|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Pretty Valley Tonalite and Bundara Tonalite.||||||
69707|Pretty Valley Suite|61166|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Pretty Valley Tonalite and Bundara Tonalite.||||||
69707|Pretty Valley Suite|61167|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Pretty Valley Tonalite and Bundara Tonalite.||||||07-FEB-11
69707|Pretty Valley Suite|61168|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Pretty Valley Tonalite and Bundara Tonalite.||||||
69706|Pretty Valley Tonalite|61160|4|Described|p33 Tb. 5.2, p58-59 Fig. 6.8|Silurian|Silurian|Of Pretty Valley Suite. Formerly P.V.Gneissic Granodiorite and P.V.Gneissic Tonalite. Equigranular, coarse-grained biotite tonalite with prominent to weak foliation defined by aligned biotite. Intruded by Niggerheads Granodiorite. Age:411 and 403Ma.||||||10-JAN-07
69706|Pretty Valley Tonalite|61164|5|Briefly described|map legend|Early Silurian|Early Silurian|Of the Pretty Valley Suite. Biotite tonalite: grey; coarse grained; equigranular with minor hornblende; numerous enclaves of migmatite and biotite-rich gneiss; cut by abundant aplite and pegmatite dykes; foliated; I-type intrusion. GSV map code: G154.||||||
69706|Pretty Valley Tonalite|61165|5|Briefly described|map legend|Early Silurian|Early Silurian|Of the Pretty Valley Suite. Biotite tonalite: grey; coarse grained; equigranular with minor hornblende; numerous enclaves of migmatite and biotite-rich gneiss; cut by abundant aplite and pegmatite dykes; foliated; I-type intrusion. GSV map code: G154.||||||
69706|Pretty Valley Tonalite|61166|5|Briefly described|map legend|Early Silurian|Early Silurian|Of the Pretty Valley Suite. Biotite tonalite: grey; coarse grained; equigranular with minor hornblende; numerous enclaves of migmatite and biotite-rich gneiss; cut by abundant aplite and pegmatite dykes; foliated; I-type intrusion. GSV map code: G154.||||||
69706|Pretty Valley Tonalite|61167|5|Briefly described|map legend|Early Silurian|Early Silurian|Of the Pretty Valley Suite. Biotite tonalite: grey; coarse grained; equigranular with minor hornblende; numerous enclaves of migmatite and biotite-rich gneiss; cut by abundant aplite and pegmatite dykes; foliated; I-type intrusion. GSV map code: G154.||||||07-FEB-11
69706|Pretty Valley Tonalite|61168|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Pretty Valley Suite. Biotite granodiorite: I-type; 409 +/- 16 Ma K/Ar biotite; nonmagnetic, with occasional magnetic patches; low gravity; low to moderate total radioelement, K, Th and U. GSV map code: G154.||||||
69706|Pretty Valley Tonalite|68116|5|Briefly described|Appendix, Map 27.|Silurian|Silurian||||||Biotite tonalite: coarse grained, equigranular with minor hornblende; gneissic; abundant aplite and pegmatite dykes and migmatite enclaves; I-type.|
15601|Princetown Member|29355|6|Mentioned|p188|||||||||
15601|Princetown Member|31036|6|Mentioned|p208|||Unit of Dilwyn Fm.||||||
15601|Princetown Member|31245|6|Mentioned|p77|||Fauna.||||||24-JUL-08
15601|Princetown Member|31246|6|Mentioned|p54|||See also P56, 57||||||
15601|Princetown Member|31247|6|Mentioned|p163|||Microplankton.||||||24-JUL-08
15601|Princetown Member|31922|6|Mentioned|p166|||||||||
15601|Princetown Member|32115|6|Mentioned|Fig.1|||||||||
15601|Princetown Member|32117|6|Mentioned|Fig.2|||||||||
15601|Princetown Member|33155|6|Mentioned|p122|||||||||
15601|Princetown Member|34343|5|Briefly described|p97|||Paleocene.||||||24-JUL-08
15601|Princetown Member|35066|5|Briefly described|p206|||||||||
15601|Princetown Member|41517|6|Mentioned|p137|||||||||
15601|Princetown Member|42827|6|Mentioned|p282, p262|||||||||
15601|Princetown Member|47054|6|Mentioned|p490|||||||||
15601|Princetown Member|48911|6|Mentioned|Chart 1|||||||||
15601|Princetown Member|61182|6|Mentioned|p22|||Of Baker (1953) - recognised within the Dilwyn Formation at the coast, but has not been unequivocally identified elsewhere. Geological Province: Otway Basin.||||||
15601|Princetown Member|62896|5|Briefly described|p88, p89, p90 Tb. 1|Early Eocene|Early Eocene|Of Dilwyn Formation (Wangerrip Group).||||||07-FEB-11
15601|Princetown Member|63740|5|Briefly described|p88, p90 Tb. 1|Early Eocene|Early Eocene|Of the Dilwyn Formation. Geological Province: Otway Basin.||||||07-FEB-11
15601|Princetown Member|70942|4|Described|p126, 119|||||Of Dilwyn Clay||||
31627|Promontory Suite|24551|5|Briefly described|p225|||||||||
31627|Promontory Suite|42726|5|Briefly described|map legend||Middle Devonian|||||||
34780|Promontory leucogranite|22942|6|Mentioned|p274|||Informal||||||
15639|Puckapunyal Formation|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
15639|Puckapunyal Formation|23309|5|Briefly described|p141, 148, 153, 270. Tb 2.51|Devonian|Silurian|||||||
15639|Puckapunyal Formation|24177|3|Fully described|p56, p50 Fig.22|Lochkovian|Pridoli|Overlain by the Waranga Formation. Overlies the Broadford Formation. Maximum Thickness: 1.5km. Interfingers laterally with Humevale Siltstone. Probably a lateral equivalent of the McIvor Sandstone.||||||01-DEC-15
15639|Puckapunyal Formation|24328|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
15639|Puckapunyal Formation|24329|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
15639|Puckapunyal Formation|31654|6|Mentioned|Map legend|Siegenian|Siegenian|||||||
15639|Puckapunyal Formation|33238|6|Mentioned|p642|||||||||
15639|Puckapunyal Formation|35283|6|Mentioned|p53|||||||||
15639|Puckapunyal Formation|39331|6|Mentioned|Table 2-1|||||||||
15639|Puckapunyal Formation|60083|5|Briefly described|Map legend|Early Devonian|Early Devonian|Interbedded siltstone and sandstone, including numerous greywacke-conglomerate intervals (turbidites).||||||
15639|Puckapunyal Formation|60529|5|Briefly described|Map Legend|Lochkovian|Pridoli|Upper fan, channel margin and channel levee turbidite deposits: fine to coarse grained quartz and quartz-lithic arenite, minor pebbly sandstone and conglomerate; thinly to thickly bedded, parallel and ripple drift cross laminations.||||||
15639|Puckapunyal Formation|60591|5|Briefly described|Map Legend|Lochkovian|Pridoli|Overlies the Broadford Formation. Overlain by the Waranga Formation. Fine- to coarse-grained quartz and quartz-lithicarenite, minor conglomerate; interbedded siltstone, silty claystone and claystone.||||||
15639|Puckapunyal Formation|60592|5|Briefly described|Map Legend|Lochkovian|Pridoli|Overlies the Broadford Formation. Overlain by the Waranga Formation. Fine- to coarse-grained quartz and quartz-lithicarenite, minor conglomerate; interbedded siltstone, silty claystone and claystone.||||||
15639|Puckapunyal Formation|60593|5|Briefly described|Map Legend|Lochkovian|Pridoli|Overlies the Broadford Formation. Overlain by the Waranga Formation. Fine- to coarse-grained quartz and quartz-lithicarenite, minor conglomerate; interbedded siltstone, silty claystone and claystone.||||||26-NOV-04
15639|Puckapunyal Formation|60595|5|Briefly described|Map Legend|Lochkovian|Pridoli|Overlies the Broadford Formation. Overlain by the Waranga Formation. Fine- to coarse-grained quartz and quartz-lithicarenite, minor conglomerate; interbedded siltstone, silty claystone and claystone.||||||
15639|Puckapunyal Formation|60596|5|Briefly described|Map Legend|Lochkovian|Pridoli|Overlies the Broadford Formation. Overlain by the Waranga Formation. Fine- to coarse-grained quartz and quartz-lithicarenite, minor conglomerate; interbedded siltstone, silty claystone and claystone.||||||
15639|Puckapunyal Formation|60597|5|Briefly described|Map Legend|Lochkovian|Pridoli|Low magnetic responses, with weak magnetic linear features; low to moderate K, variable Th and high U.||||||26-NOV-04
15639|Puckapunyal Formation|60599|3|Fully described|p14, p24 Tb. 4, p73, p107, p99|Lochkovian|Pridolian|Thinly to thickly bedded seq. of turbidite beds, upward-fining; massive, mostly coarse- to v.coarse-gr., may contain pebbly bases; sandstones mostly quartz + quartz-lithic arenites. Gradational over Broadford Fm; underlies Waranga Fm. Thickness: >1.5km. ||||||
15639|Puckapunyal Formation|61185|2|Defined|p31-33, p30, p21 Fig.6|Lochkovian|Pridolian|Of Anon 1970; King and Wilkinson 1975. Turbidite. Poorly exposed outcrop. Under Waranga Formation (arbitrary boundary). Over Broadford Formation. Thickness: ~1500m possibly overestimated. Geol.Prov: LFB, Melbourne Zone.||||||07-FEB-11
15639|Puckapunyal Formation|61701|5|Briefly described|Map Legend|Lochkovian|Pridoli|Upper fan, channel margin and channel levee turbidite deposits: fine to coarse grained quartz and quartz-lithic arenite, minor pebbly sandstone and conglomerate; thinly to thickly bedded, parallel and ripple drift cross laminations.||||||25-JUL-06
15639|Puckapunyal Formation|61702|5|Briefly described|Map Legend|Lochkovian|Pridoli|Upper fan, channel margin and channel levee turbidite deposits: fine to coarse grained quartz and quartz-lithic arenite, minor pebbly sandstone and conglomerate; thinly to thickly bedded, parallel and ripple drift cross laminations.||||||25-JUL-06
15639|Puckapunyal Formation|61703|5|Briefly described|Map Legend|Lochkovian|Pridoli|Upper fan, channel margin and channel levee turbidite deposits: fine to coarse grained quartz and quartz-lithic arenite, minor pebbly sandstone and conglomerate; thinly to thickly bedded, parallel and ripple drift cross laminations.||||||25-JUL-06
15639|Puckapunyal Formation|61704|6|Mentioned|Map legend|Devonian|Devonian|Low K and Th, with bands of high K and Th.||||||
15639|Puckapunyal Formation|62469|5|Briefly described|p5 Fig. 2, p20 Fig. 11, p15|Pragian|Lochkovian|Includes the Collins Quarry Sandstone Member. Geological Province: Darraweit Guim Province.||||||12-FEB-15
15639|Puckapunyal Formation|64612|6|Mentioned|p8|||||||||07-FEB-11
15639|Puckapunyal Formation|65969|6|Mentioned|p15, p17 Fig.7|||Sandy; correlates with the silty Humevale Formation. Mis-spelt as Puckupunyal in Fig.7.||||||
15639|Puckapunyal Formation|66769|6|Mentioned|p127 Fig.8d, Fig 13|||Melbourne Zone. Overlies Broadford Formation; is overlain by Waranga Formation.||||||
15639|Puckapunyal Formation|68116|5|Briefly described|Appendix, Maps 24-25, 33.|Lochkovian|Pridoli||||||Fine- to coarse-grained quartz and quartz-lithic arenite, minor conglomerate: parallel and ripple drift cross laminations, and interbedded siltstone and claystone; slump structures, commonly burrowed.|
15639|Puckapunyal Formation|69089|5|Briefly described|Map legend|Early Devonian|Early Devonian||||||Marine: siltstone, thin bedded sandstone.|
15639|Puckapunyal Formation|70487|6|Mentioned|p8-9, p11 Fig.5|Pragian|Pragian|Correlation with Stoddart Member suggested (Welch et al. 2011) and Sanford (2002).||||Correlative of McIvor Sandstone. Overlies Broadford Formation.|Includes sandstone.|
15639|Puckapunyal Formation|73497|5|Briefly described|Map legend|Devonian|Devonian|Marine.||Murrindindi Supergroup|||Siltstone, sandstone: low magnetic responses, weak magnetic linear features of short strike length (up to 5 km); low-moderate K, variable Th, and high U, some weak bands (particularly K) are parallel to strike.|
29714|Purgagoolah Granite|23309|6|Mentioned|p441 App1|||G503 S-Type.||||||
29714|Purgagoolah Granite|43314|5|Briefly described|Map Legend||Wenlock|of Ocean View Suite. I-type? Weathered coarse-medium grained granite.||||||22-OCT-04
29714|Purgagoolah Granite|43315|5|Briefly described|Map Legend|Wenlock|Wenlock|Of the Ocean View Suite. I-type? Weathered coarse-medium-grained granite||||||03-MAY-05
29714|Purgagoolah Granite|60541|5|Briefly described|p69, p46|Late Silurian|Late Silurian|Outcrops are generally poor consisting of decomposed friable masses of quartz and feldspar with minor chloritised biotite. Geological Province: Lachlan Fold Belt. See also p17 Tb. 1.||||||
29714|Purgagoolah Granite|68116|5|Briefly described|Appendix, Map 45.|Wenlock|Wenlock||||||Granite: coarse to medium-grained; weathered; I-type?|
15694|Pyalong Granite|22886|4|Described|Table.1|||Age: Rb/Sr 366Ma. Of Cobaw Batholith.||||||20-MAY-08
15694|Pyalong Granite|23203|6|Mentioned|Fig.1|||||||||
15694|Pyalong Granite|23309|5|Briefly described|p441 App 1||Late Devonian|G283 S-Type. Age: 359+/-7 Ma. Supersedes Pyalong Adamellite, Pipers Creek Granite.||||||
15694|Pyalong Granite|23810|5|Briefly described|Table 1, p892||Devonian|Felsic S-Type. Age: 376+/-2 Ma. (SHRIMP U-Pb age). Lachlan Fold Belt.||||||
15694|Pyalong Granite|23814|5|Briefly described|p755|Devonian|Devonian|Age: 367+/-2Ma (SHRIMP U-Pb zircon).||||||
15694|Pyalong Granite|24383|5|Briefly described|p9 Fig.1|||Parent: Cobaw Suite. Geological Province: Lachlan Fold Belt||||||
15694|Pyalong Granite|24384|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Cobaw Suite.||||||
15694|Pyalong Granite|24385|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Cobaw Suite. Biotite granite; pale grey, coarse-grained; commonly prophyritic in K-feldspar.||||||01-JUL-08
15694|Pyalong Granite|24386|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Cobaw Suite. Biotite granite: pale grey, coarse-grained; commonly porphyritic in K-feldspar.||||||
15694|Pyalong Granite|24387|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Cobaw Suite. Biotite granite; pale grey, coarse-grained; commonly porphyritic in K-feldspar.||||||
15694|Pyalong Granite|24388|5|Briefly described|Map legend|Late Devonian|Late Devonian|Parent: Cobaw Suite.  Biotite granite; reduced S-type; nonmagnetic; high K, high Th, moderate U, high in total radioelements.||||||
15694|Pyalong Granite|24551|6|Mentioned|p408|Late Devonian|Middle Devonian|Age: 376 +/- 2Ma.||||||
15694|Pyalong Granite|41570|6|Mentioned|Fig.3.8|||||||||
15694|Pyalong Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
15694|Pyalong Granite|42790|5|Briefly described|Fig.14 P189|||||||||
15694|Pyalong Granite|62897|6|Mentioned|p118|||||||||18-MAR-08
15694|Pyalong Granite|63741|6|Mentioned|p118|||||||||
15694|Pyalong Granite|64611|5|Briefly described|Map legend|Late Devonian|Late Devonian|Part of the Cobaw Batholith. Biotite granite: pale grey , fine- to coarse-grained with large phenocrysts of K-feldspar, occasional biotite microgranular enclaves and biotite clots; S-type intrusion.||||||23-JUN-14
15694|Pyalong Granite|64612|2|Defined|p18 Fig. 3.7, p20 Fig. 4.3, p41, p43-44|Devonian|Devonian|Chappell et al. (1991). Of Pyalong Suite. Age: 359+/-7Ma (K-Ar). Intrudes and contact metamorphosed Heathcote Volcanic Group, Castlemaine Group, Murrindindi Supergroup and Rainy Creek Porphyry. Intruded by Baynton Granodiorite. See p43-44.||||||23-JUN-14
15694|Pyalong Granite|64619|5|Briefly described|Map legend|Devonian|Devonian|Biotite granite; pale grey, coarse-grained, strongly porphyritic with large K-feldspar phenocrysts; usually deeply weathered; unassigned intrusion.||||||30-OCT-08
15694|Pyalong Granite|65715|5|Briefly described|p7 Tb.4|||Of Cobaw Batholith. G283. Called Granite G2 of Cobaw Granite by Stewart (1966) and Pyalong Adamellite by White and Chappell (1988).||||||23-JUN-14
15694|Pyalong Granite|66575|6|Mentioned|p963,|||Bendigo 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.||||||
15694|Pyalong Granite|67978|5|Briefly described|p496 Fig.1, p499 Tb.1|Frasnian|Frasnian|Dating by Bierlein et al. (2001).|376 +/- 2 Ma, SIMS U-Pb|||||19-SEP-14
15694|Pyalong Granite|68116|5|Briefly described|Appendix, Map 32.|Late Devonian|Late Devonian||||||Biotite granite: pale grey; coarse-grained; strongly porphyritic with large K-feldspar phenocrysts; S-type.|
15694|Pyalong Granite|75072|6|Mentioned|p237, 245|||Zircon ages indicate thermal events (age ranges given); probability density distribution graph.||||||
31628|Pyalong Suite|24551|6|Mentioned|p221|||||||||
31628|Pyalong Suite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
15707|Pyramid Hill Granite|23232|6|Mentioned|p61|||||||||
15707|Pyramid Hill Granite|23309|5|Briefly described|p209, 347-348, 350.|Devonian|Devonian|G295 S/I-Type.  Age: 372+/-6 Ma, 362+/-8 Ma, 360+/-5 Ma. Supersedes Terrick Terrick Granite.||||||
15707|Pyramid Hill Granite|24177|4|Described|p29, p63|Late Devonian|Late Devonian|||||||11-MAY-04
15707|Pyramid Hill Granite|24328|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|||||||
15707|Pyramid Hill Granite|24329|5|Briefly described|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
15707|Pyramid Hill Granite|24551|6|Mentioned|p224|||||||||
15707|Pyramid Hill Granite|31654|6|Mentioned|Map legend|Darriwilian|Darriwilian|||||||
15707|Pyramid Hill Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
15707|Pyramid Hill Granite|60005|5|Briefly described|Map legend|Late Devonian|Late Devonian|Coarse-grained, intrusive leucocratic adamellite.||||||12-JUL-04
15707|Pyramid Hill Granite|65715|5|Briefly described|p8 Tb.4|||Pyramid Hill Granite and Terrick Terrick Granite of King and Wilkinson (1975) grouped and named the pluton Pyramid Hill by White and Chappell (1988). VandenBerg et al. (2000) applied the name Pyramid Hill Granite.||||||
15707|Pyramid Hill Granite|65969|5|Briefly described|p3, p19, p30|Famennian|Frasnian|Ages range from 360+/-5 Ma (K/Ar muscovite) to 372+/-6 Ma (K/Ar biotite). Cut by Kanimblan deformation faults. Earthquakes recorded in and around this unit.||||||
15707|Pyramid Hill Granite|65974|6|Mentioned|p7, p39, p42|||Correponds with a large gravity low in Section Line 1. Appears as Pyramid Hill granite on p7.||||||07-FEB-18
15707|Pyramid Hill Granite|66934|6|Mentioned|Map legend|||Similar to the informally-named Baldon granite.||||||
15707|Pyramid Hill Granite|68116|5|Briefly described|Appendix, Maps 12, 17.|Late Devonian|Late Devonian||||||Leucocratic biotite-muscovite granite, with accessory apatite, zircon, garnet, andalusite, ilmenite and pyrite; coarse-grained, porphyritic with orthoclase phenocrysts; S-type.|
15707|Pyramid Hill Granite|69089|5|Briefly described|Map legend|Late Devonian|Late Devonian|I-type.||||||
15707|Pyramid Hill Granite|70718|4|Described|p38, p80, p128|Devonian|Devonian|Has similar geophysical characteristics as the Cunninyeuk granite suite. Author dervied numeric ages from the ASUD.|360 +/- 5 Ma and 372 +/- 8 Ma|||Intrudes the Sunbury Group.|Coarse-grained leucocratic monzogranite.|
15707|Pyramid Hill Granite|73496|5|Briefly described|Map legend|Late Devonian|Late Devonian|G295.|||||Muscovite-biotite-garnet-andalusite granite; nonmagnetic but with distinctive magnetic contact aureole to 40 nT; gravity low 60 micrometres/second/second below the regional; K, U high, Th moderate.|
15707|Pyramid Hill Granite|73497|5|Briefly described|Map legend|Late Devonian|Late Devonian|G295.|||||Granite: S-type; mostly nonmagnetic with magnetic phase to 20 nT, magnetic metamorphic aureole to 80 nT, magnetic dykes to 20 nT; high K, low Th and U, gravity low approximately 100 micrometres/second/second.|
15707|Pyramid Hill Granite|73505|5|Briefly described|p8 Tb.3.2, p9-10, p30, p35|Early Carboniferous|Late Devonian|(G295). Multiple K/Ar and Rb/Sr ages provided, preferred age of 361+/-3 Ma. Highly fractionated where outcropping. Nonmagnetic.|360+/-5 Ma K/Ar, 372+/-6 Ma K/Ar|||||
22711|Pyrenees Formation|22531|6|Mentioned|p6|Cambrian|Cambrian|of Saint Arnaud Group||||||
22711|Pyrenees Formation|22756|3|Fully described|p9, p26|Ordovician|Cambrian|||||||16-FEB-15
22711|Pyrenees Formation|23164|4|Described|p13|Cambrian|Cambrian|||||||
22711|Pyrenees Formation|23165|5|Briefly described|Map legend|Ordovician|Cambrian|||||||
22711|Pyrenees Formation|23166|5|Briefly described|Map legend|Ordovician|Cambrian|of Saint Arnaud Group.||||||
22711|Pyrenees Formation|23167|5|Briefly described|Map legend|Ordovician|Cambrian|of Saint Arnaud Group.||||||
22711|Pyrenees Formation|23168|5|Briefly described|Map legend|Ordovician|Cambrian|of Saint Arnaud Group.||||||
22711|Pyrenees Formation|23169|5|Briefly described|Map legend|Ordovician|Cambrian|of Saint Arnaud Group.||||||
22711|Pyrenees Formation|23300|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Saint Arnaud Group||||||
22711|Pyrenees Formation|23301|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Saint Arnaud Group||||||
22711|Pyrenees Formation|23302|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Saint Arnaud Group||||||
22711|Pyrenees Formation|23303|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Saint Arnaud Group||||||
22711|Pyrenees Formation|23304|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Saint Arnaud Group||||||
22711|Pyrenees Formation|23305|3|Fully described|p38||Late Cambrian|of Cayley and McDonald (1995). Of St Arnaud Group. Underlying unit Beaufort Formation. Max. thickness: 2000 m.||||||
22711|Pyrenees Formation|23307|5|Briefly described|Map Legend|Cambrian|Cambrian|Of Saint Arnaud Group||||||
22711|Pyrenees Formation|23309|5|Briefly described|p41. Tb 2.12|||Of the Saint Arnaud Group.||||||03-JUL-13
22711|Pyrenees Formation|24551|5|Briefly described|p83|Cambrian|Cambrian|Of Saint Arnaud Group. Overlies: Beaufort Formation.||||||02-AUG-05
22711|Pyrenees Formation|43260|5|Briefly described|Map Legend|Ordovician|Cambrian|of Saint Arnaud Group.||||||
22711|Pyrenees Formation|43846|5|Briefly described|10|Ordovician|Cambrian|||||||
22711|Pyrenees Formation|50352|5|Briefly described|Map Legend|Ordovician|Cambrian|Laminated silty micaceous quartz-rich arenite||||||
22711|Pyrenees Formation|60452|5|Briefly described|p22|Late Cambrian|Late Cambrian|Conformably overlies the Beaufort Formation.||||||
22711|Pyrenees Formation|60461|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Saint Arnaud Group.  Deep marine turbidites and hemipelagic sediments: interbedded fine to coarse grained sandstone, silt and minor mudstone.  Age: >490Ma.||||||28-SEP-04
22711|Pyrenees Formation|60491|4|Described|p14, p18|Early Ordovician|Cambrian|Of the Saint Arnaud Group. Intruded by Early Devonian granitoids. Unconformably overlain by Tertiary and Quaternary Murray Basin sediments. Thickness: ~2.5km||||||22-NOV-04
22711|Pyrenees Formation|60492|5|Briefly described|Map Legend|Ordovician|Cambrian|Of the Saint Arnaud Group. Overlain by the Renmark Group. Turbiditic sandstone and mudstone; coarse to fine grained quartzwacke and minor mudstone; occasional calcareous nodules.||||||
22711|Pyrenees Formation|60493|5|Briefly described|Map Legend|Ordovician|Cambrian|Of the Saint Arnaud Group. Marine turbiditic sandstone with minor mudstone; minor carbonaceous siltstone and local carbonate concretions; little magnetic character; gravity response moderate to high; high K, moderate to high Th, U||||||
22711|Pyrenees Formation|60581|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Saint Arnaud Group. Sandstone, mudstone; moderately to well sorted, variably rounded quartz with minor feldspar and lithic grained in quartz silt or clay matrix; medium to thick bedded; weathered to partly kaolinised.||||||
22711|Pyrenees Formation|60582|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Saint Arnaud Group. Sandstone, mudstone; moderately to well sorted, variably rounded quartz with minor feldspar and lithic grained in quartz silt or clay matrix; medium to thick bedded; weathered to partly kaolinised.||||||
22711|Pyrenees Formation|60583|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Saint Arnaud Group. Sandstone, mudstone; moderately to well sorted, variably rounded quartz with minor feldspar and lithic grained in quartz silt or clay matrix; medium to thick bedded; weathered to partly kaolinised.||||||
22711|Pyrenees Formation|60584|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Saint Arnaud Group. Sandstone, mudstone; moderately to well sorted, variably rounded quartz with minor feldspar and lithic grained in quartz silt or clay matrix; medium to thick bedded; weathered to partly kaolinised.||||||
22711|Pyrenees Formation|60585|4|Described|p16|Late Cambrian|Late Cambrian|Of the Saint Arnaud Group. Conformably overlies the Beaufort Formation. Minimum thickness: 2000m.||||||
22711|Pyrenees Formation|61750|5|Briefly described|p19, p21|||Of the Saint Arnaud Group west of Avoca Fault (Cayley and McDonald, 1995). Contains gold deposits.||||||
22711|Pyrenees Formation|62099|5|Briefly described|p331|Cambrian|Cambrian|Of the Saint Arnaud Group. Thickness: ~2.5km. In the Stawell Zone of the Lachlan Orogen.||||||
22711|Pyrenees Formation|62754|5|Briefly described|p863|||Of the Saint Arnaud Group. Geological Province: Stawell Zone.||||||23-JAN-07
22711|Pyrenees Formation|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Saint Arnaud Group.  Defined by Cayley and McDonald 1995.||||||
22711|Pyrenees Formation|66012|4|Described|p4-5, p8, p10 Tb.1, p11, p13-14, p25-26|Ordovician|Cambrian|Of Saint Arnaud Group. Unconformably overlain by White Hills Gravel & Newer Volcanic Group. Buff, laminated, medium-bedded silty micaceous arenite. Intruded by Mount Emu and Mount Bute granites. Deeply weathered. Exposed in railway cuttings W of Pittong| | | | | |13-JUN-13
22711|Pyrenees Formation|68116|5|Briefly described|Appendix, Maps 15-16, 22-23, 31, 40.|Early Ordovician|Middle Cambrian|Mostly nonmagnetic, but some parts are weakly to moderately magnetic. Deep marine deposits. |||||Sandstone and mudstone: sand-rich turbidite facies; moderately to well sorted, variably rounded quartz with minor feldspar and lithic grains in quartz silt or clay matrix; medium to thick bedded; unfossiliferous; weathered to partly kaolinised.|
22711|Pyrenees Formation|68189|6|Mentioned|p17 Tb.3.1|||||||||
22711|Pyrenees Formation|68194|5|Briefly described|p20-21, p31, p34 Figs.32-33, p35-36, p40|Cambrian|Cambrian|See also p42, p46-47, p57, p76. Unfossiliferous, texturally immature turbidites. Regolith and remote sensing profiles described.||Unit in Saint Arnaud Group.||Is faulted against Warrak Formation.|Sequences of thick-bedded sandstone and minor slate.|
22711|Pyrenees Formation|70268|6|Mentioned|p259|||Linton area, eastern Pyrenees province.||||||
22711|Pyrenees Formation|73118|6|Mentioned|p13-14|||Stawell Zone, Lachlan Fold Belt, Western Victoria. Weakly magnetic.|||||Sandstones.|
22711|Pyrenees Formation|73496|5|Briefly described|Map legend|Cambrian|Cambrian|||Saint Arnaud Group|||Parts are either weakly magnetised with magnetic responses typically 1 to 5 nT, or nonmagnetic with magnetic responses less than 1 nT.|
22711|Pyrenees Formation|73497|6|Mentioned|Map legend|Cambrian|Cambrian|||Saint Arnaud Group||||
31833|Quambatook granite|43846|6|Mentioned|13||Devonian|Belongs to Mount Cole Suite||||||
69143|Queen Coal Seam (VIC)|61140|5|Briefly described|p9, p11|Early Cretaceous|Early Cretaceous|Informal name. Of the Strzelecki Group. Historical perspective||||||09-JUN-05
15755|Quiamong Member|22756|6|Mentioned|P36|||||||||
15755|Quiamong Member|29898|5|Briefly described|p213|||||||||
15755|Quiamong Member|35272|5|Briefly described|p279|||||||||
15755|Quiamong Member|41848|5|Briefly described|p355|||Part of Shepparton Formation.||||||27-OCT-08
15755|Quiamong Member|42827|5|Briefly described|Table 9.1|||||||||
15755|Quiamong Member|42966|2|Defined|Table 30 p196|Late Pleistocene||Of Shepparton Formation.||||||27-OCT-08
15755|Quiamong Member|60599|5|Briefly described|p92|Quaternary|Quaternary|Informal name. Of Shepparton Formation.||||||
15755|Quiamong Member|70961|14|Not recorded|p133|||Refers to Lawrence (1966). Alluvial.||||||
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|||||||
34870|Quindalup Ignimbrite|22968|4|Described|Fig49 P92, P143||Early Devonian|Type section location given on P134, new name, parent is Avonmore Subgroup, maximum thickness is 650m, overlying unit is Buchan Caves Limestone, underlying unit is Tin Pot Ignimbrite||||||
34870|Quindalup Ignimbrite|23021|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is the Snowy River Volcanics||||||
34870|Quindalup Ignimbrite|23028|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is Avonmore Subgroup||||||
34870|Quindalup Ignimbrite|23309|4|Described|p113, 117. Tb 2.40|||Of the Avonmore Subgroup.  Maximum Thickness: 650m.||||||22-FEB-10
34870|Quindalup Ignimbrite|24551|5|Briefly described|p145, 139 Fig. 5.30|Early Devonian|Early Devonian|Of the Avonmore Subgroup.||||||02-AUG-05
34870|Quindalup Ignimbrite|68116|5|Briefly described|Appendix, Map 35.|Pragian|Lochkovian||||||Quartz ignimbrite: salmon pink; often coarse-grained with prominent quartz crystals; moderate to high phenocryst content; variably welded, commonly with obvious eutaxitic foliation; minor thin sandstone and conglomerate.|
69418|Racecourse Plain Tonalite|61161|5|Briefly described|p94, p76-77 Fig 6.1, p92 Fig. 6.11|Early Devonian|Early Devonian|Of Rileys Creek Suite. Nonconformably overlain by Older Volcanic Group basalt. Nonmagnetic to weakly magnetic, grey, medium-grained, equigranular biotite-hornblende tonalite with weak magmatic foliation. I-type. Type locality p94. GSV map code: G463.||||||
69418|Racecourse Plain Tonalite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende tonalite: medium-grained, equigranular; contains quartz, plagioclase (commonly with distinct calcic cores), biotite, hornblende, cummingtonite (within hornblende); I-type intrusion. GSV map code: G463.||||||
69418|Racecourse Plain Tonalite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende tonalite: medium-grained, equigranular; contains quartz, plagioclase (commonly with distinct calcic cores), biotite, hornblende, cummingtonite (within hornblende); I-type intrusion. GSV map code: G463.||||||07-FEB-11
69418|Racecourse Plain Tonalite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende tonalite: medium-grained, equigranular; contains quartz, plagioclase (commonly with distinct calcic cores), biotite, hornblende, cummingtonite (within hornblende); I-type intrusion. GSV map code: G463.||||||
69418|Racecourse Plain Tonalite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende tonalite: medium-grained, equigranular; contains quartz, plagioclase (commonly with distinct calcic cores), biotite, hornblende, cummingtonite (within hornblende); I-type intrusion. GSV map code: G463.||||||
69418|Racecourse Plain Tonalite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende tonalite: no gravity data; nonmagnetic to weakly magnetic (0 nT, k = 1 to 45 x10^-6 cgs); low to moderate K, Th, U and total radioelements. GSV map code: G463.||||||
69418|Racecourse Plain Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Silurian||||||Biotite-hornblende tonalite: medium-grained, equigranular; contains quartz, plagioclase (commonly with distinct calcic cores), biotite, hornblende, cummingtonite (within hornblende).|
73488|Rainy Creek Porphyry|64611|5|Briefly described|Map legend|Late Devonian|Late Devonian|Part of the Cobaw Batholith. Orthopyroxene-plagioclase-biotite porphyry, fine- to medium-grained, with phenocrysts of plagioclase and orthopyroxene set in an aphanitic groundmass. S-type intrusion.||||||01-JUL-13
73488|Rainy Creek Porphyry|64612|2|Defined|p42-43, p58, p69, p73, p78 Fig. 10.11|||Of Cobaw Batholith. Intrudes Castlemaine Group and has been intruded by Pyalong Granite. Orthopyroxene-plagioclase-biotite porphyry is fine to medium-grained and contains phenocrysts of plag and orthopyroxene. S-type.||||||01-JUL-13
73488|Rainy Creek Porphyry|65715|6|Mentioned|p7 Tb.4|||G281. Defined Cayley et al. (2008).||||||
73488|Rainy Creek Porphyry|68116|5|Briefly described|Appendix, Map 32.|Late Devonian|Late Devonian||||||Orthopyroxene-plagioclase-biotite porphyry: fine to medium grained porphyry with phenocrysts of plagioclase and orthopyroxene set in an aphanitic groundmass; magnetic S-type intrusion.|
29719|Rankin Road Ignimbrite|23309|4|Described|p108.  Tb 2.40|||Of the Little River Subgroup.||||||22-FEB-10
29719|Rankin Road Ignimbrite|24551|5|Briefly described|p145|||Of the Little River Subgroup.||||||
29719|Rankin Road Ignimbrite|43312|5|Briefly described|Map Legend||Early Devonian|||||||
29719|Rankin Road Ignimbrite|43313|5|Briefly described|Map Legend||Early Devonian|of Little River Subgroup||||||
29719|Rankin Road Ignimbrite|60542|4|Described|p65-66, p22 Tb. 2|Early Devonian|Early Devonian|Of Little River Subgroup. Consists of bluish green feldspar ignimbrite, with a variable but generally low phenocryst content in a fine vitriclastic matrix. Overlain by Castor Oil Lava and Jellung Ignimbrite.||||||23-JUN-14
29719|Rankin Road Ignimbrite|68116|5|Briefly described|Appendix, Map 45.|Pragian|Pragian||||||Vitric feldspar ignimbrite: pale coloured, massive, recrystallised, contains Ordovician-derived lithic fragments; pyroclastic deposits.|
30546|Raymond Falls Lava|23309|4|Described|p108  Tb 2.40|||Of the Little River Subgroup.||||||22-FEB-10
30546|Raymond Falls Lava|23615|4|Described|p128, p166|Early Devonian|Early Devonian|Of Little River Subgroup. Supersedes Raymond Falls Rhyolite (VandenBerg, 1988b). Quartz feldspar porphyry, flow banded and partially flowbanded rhyolitic to rhyodacitic lava; parts contain "thunder eggs" (vughs lined with chalcedony and quartz crystals).||||||23-JUN-14
30546|Raymond Falls Lava|23938|6|Mentioned|p63-65 Figs. 23-24.|||||||||
30546|Raymond Falls Lava|24551|5|Briefly described|p145|||Of the Little River Subgroup.||||||02-AUG-05
30546|Raymond Falls Lava|43206|5|Briefly described|map legend||Lochkovian|Of Little River Subgroup.||||||25-SEP-08
30546|Raymond Falls Lava|43312|5|Briefly described|Map Legend||Early Devonian|Of Little River Group.||||||25-SEP-08
30546|Raymond Falls Lava|43313|5|Briefly described|Map Legend||Early Devonian|Of Little River Group.||||||25-SEP-08
30546|Raymond Falls Lava|60542|4|Described|p62|Early Devonian|Early Devonian|Of Little River Subgroup. Rhyolite lava, porphyritic to flow-banded, autobrecciated to massive with no visible texture; contains small quartz and feldspar phenocrysts in a glassy groundmass . Overlain by Moores Ford Andesite.||||||
30546|Raymond Falls Lava|66181|6|Mentioned|p311|Devonian||||||||
30546|Raymond Falls Lava|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Rhyolite lava: small quartz and feldspar phenocrysts, in part flow banded; lava dome.|
69413|Red Hut Tonalite|61160|3|Fully described|p82, p31 Tb. 5.2|Early Devonian|Early Devonian|I-type. Grey, fine-grained, equigranular biotite-hornblende tonalite. In contact with Cobungra Granite and migmatite of Omeo Metamorphic Complex. See also p58-59 Fig. 6.8.||||||22-JAN-07
69413|Red Hut Tonalite|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende tonalite: grey; fine grained, equigranular; magnetic; I-type intrusion. GSV map code: G544.||||||
69413|Red Hut Tonalite|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende tonalite: grey; fine grained, equigranular; magnetic; I-type intrusion. GSV map code: G544.||||||
69413|Red Hut Tonalite|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende tonalite: grey; fine grained, equigranular; magnetic; I-type intrusion. GSV map code: G544.||||||
69413|Red Hut Tonalite|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende tonalite: grey; fine grained, equigranular; magnetic; I-type intrusion. GSV map code: G544.||||||07-FEB-11
69413|Red Hut Tonalite|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende tonalite (I-type): highly magnetic (200-500 nT; kv = 100-3000 x10^-6 cgs); low gravity (-435 ums^-2); low total radioelement, K, Th and U. GSV map code: G544.||||||
15951|Red Limestone|48971|6|Mentioned|p101|||||||||
30429|Red Man Bluff Subgroup|23309|5|Briefly described|p78|||Consists of the Major Mitchell Sandstone, Kalymna Falls Sandstone, Murray Hill Sandstone, Watgania Gap Sandstone, Gariwerd Sandstone, Thermopylae Conglomerate.||||||02-MAY-13
30429|Red Man Bluff Subgroup|23402|3|Fully described|p25|Silurian|Silurian|Parent: Grampians Group. Thickness: 1600m. Geological Province: Adelaide Fold Belt||||||30-JAN-07
30429|Red Man Bluff Subgroup|24551|4|Described|p120|||Of the Grampians Group. Approximately 1900m thick. Consists of 6 formations.||||||08-MAR-07
30429|Red Man Bluff Subgroup|24581|5|Briefly described|p813|||Of the Grampians Group. Overlain by the Silverband Formation. Geological Province: Kanmantoo Fold Belt.||||||
30429|Red Man Bluff Subgroup|50154|5|Briefly described|p110|||Of the Grampians Group.||||||
30429|Red Man Bluff Subgroup|60451|4|Described|p76|Early Devonian|Ordovician|Of the Grampians Group. Maximum Thickness: 1900m. Conformably underlies Silverband Formation. Consists of six formations. Quartzo-feldspathic sandstone.||||||12-NOV-08
30429|Red Man Bluff Subgroup|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Includes: Thermopylae Conglomerate, Gariwerd Sandstone, Watgania Gap Sandstone, Murray Hill Sandstone, Kalymna Falls Sandstone, Major Mitchell Sandstone.||||||
30429|Red Man Bluff Subgroup|61183|3|Fully described|p28-29, p50|||Lower part of the Grampians Group; subdivided into 6 formations. Quartzo-feldspathic to micaceous sandstone packages. Conformably overlain by Silverband Formation. Thickness: 1900m. See also p30 Tb. 2, p36.||||||
30429|Red Man Bluff Subgroup|61749|5|Briefly described|p14|||Of the Grampians Group. Quartzose-feldspathic to micaeous sandstone. Underlies Silverband Formation. Thickness: 1900m.||||||02-MAY-13
30429|Red Man Bluff Subgroup|61752|5|Briefly described|p10|||Lower unit of the Grampians Group. Quartzose to micaceous sandstone. Underlies Silverband Formation. Thickness: 1900m. Geological Province: Lachlan Fold Belt.||||||07-FEB-11
30429|Red Man Bluff Subgroup|64610|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Grampians Group. Includes Thermopylae Conglomerate, and the Gariwerd, Walgania Gap, Murray Hill, Kalymna Falls and Major Mitchell Sandstones. Mainly sandstones; some conglomerate.||||||11-NOV-08
30429|Red Man Bluff Subgroup|65313|6|Mentioned|p582 Fig.10|Silurian|Ordovician||||Includes Thermopylae Conglomerate; Gariwerd, Watgania Gap, Murray Hill, Kalymna Falls and Major Mitchell Sandstones.|||26-MAR-12
30429|Red Man Bluff Subgroup|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Grampians Group. Includes Major Mitchell Sandstone, Kalymna Falls Sandstone, Murray Hill Sandstone, Watgania Gap Sandstone, Gariwerd Sandstone and Thermopylae Conglomerate. Defined by Cayley & Taylor, 1997. Modified from Red Man Bluff Sandstones of Spencer-Jones (1965)||||||
30429|Red Man Bluff Subgroup|68116|5|Briefly described|Appendix, Map 39.|Llandovery|Late Ordovician||||||Sandstone with interbedded siltstone, conglomerate.|
35474|Red Rock volcanic complex|23215|5|Briefly described|p196-7|||||||||
35474|Red Rock volcanic complex|24551|6|Mentioned|p706|||Table 27.1, sites of international significance.||||||02-AUG-05
35474|Red Rock volcanic complex|61896|6|Mentioned|p58|||Informally refers to the Red Rock Complex.||||||19-DEC-07
34856|Reedy Flat Tonalite|22968|5|Briefly described|P74, P205|Early Devonian|Late Silurian|Parent is the Ensay Suite, highly magnetic||||||
34856|Reedy Flat Tonalite|23028|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Ensay Suite||||||
34856|Reedy Flat Tonalite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Ensay Suite||||||
34856|Reedy Flat Tonalite|23309|5|Briefly described|p103, App 1 p442|||G128, I-type. Supersedes Ensay Granite.||||||04-NOV-14
34856|Reedy Flat Tonalite|68116|5|Briefly described|Appendix, Maps 35-36.|Early Devonian|Early Devonian||||||Biotite-hornblende tonalite/granodiorite: pale grey; medium-grained; porphyritic in hornblende; weak magmatic foliation; microgranitoid enclaves.|
69032|Refrigerator Gap Dacite|23309|5|Briefly described|p175, 176, 181, 185, Table 2.67|Devonian|Devonian|Of the Wellington Volcanics/Wellington Volcanic Group. Dacitic lavas and tuffs up to 300m thick||||Bindaree Formation at same stratigraphic level.||21-FEB-13
69032|Refrigerator Gap Dacite|24551|4|Described|p173, 175|Frasnian|Frasnian|Of the Wellington Volcanic Group (age discussed p187). Maximum thickness: 300m.||||Bindaree Formation may be part lateral equivalent.|Basal sedimentary breccias and mudstones, overlain by succession of porphyritic dacites.|21-FEB-13
69032|Refrigerator Gap Dacite|66252|2|Defined|p209, p211, p212 Fig.2, p213 Fig.3, p214|Frasnian|Frasnian|See also p215-217 Figs.5-7, p220, p228-229, p231. New name. Definition data given. S Macalister Synclinorium. Unit in Avon River Group. Corresponds to Rose River Volcanics and Bindaree Formation. Discontinuous basal rhyolite/shale breccia and sandstone, grey porphyritic dacite lava, thinly interbedded grey shale and mudstone. Variable thickness; c.450m in type section. Unconformably overlies Ordovician metasediments in Jamieson River area. Is overlain by Howitt Spur Formation. Detailed stratigraphic section.||||||
69032|Refrigerator Gap Dacite|68116|5|Briefly described|Appendix, Map 34.|Late Devonian|Late Devonian||||||Thin tabular flows of massive dacitic lava and occasional hyaloclastite, with a 20 m thick unit of black laminated shale intercalated.|
41775|Reliance pluton|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: moderate gravity response (-370 ums^-2); moderately magnetic (70 -90 nT). Magnetic modelling of the shallower parts of the pluton indicate possible depth to top of approx 2 km. GSV map code: G469.||||||21-SEP-05
41775|Reliance pluton|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: moderate gravity response (-370 ums^-2); moderately magnetic (70 -90 nT). Magnetic modelling of the shallower parts of the pluton indicate possible depth to top of approx 2 km. GSV map code: G469.||||||07-FEB-11
41775|Reliance pluton|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: moderate gravity response (-370 ums^-2); moderately magnetic (70 -90 nT). Magnetic modelling of the shallower parts of the pluton indicate possible depth to top of approx 2 km. GSV map code: G469.||||||21-SEP-05
41775|Reliance pluton|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: moderate gravity response (-370 ums^-2); moderately magnetic (70 -90 nT). Magnetic modelling of the shallower parts of the pluton indicate possible depth to top of approx 2 km. GSV map code: G469.||||||21-SEP-05
41775|Reliance pluton|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Subsurface pluton: moderate gravity response (-380 to -310 ums^-2); moderately magnetic (70 to 90 nT), magnetic modelling of the shallower parts of the pluton indicate possible depth to top of approx 2 km. GSV map code: G469.||||||
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.|
16064|Rheola Gabbro|23309|5|Briefly described|p442|Devonian|Silurian|G349. Age: 411+/-8 Ma. Supersedes Rheola Diorite.||||||26-JUL-05
16064|Rheola Gabbro|42726|5|Briefly described|map legend|||||||||
16064|Rheola Gabbro|65715|5|Briefly described|p8 Tb.4|||G349. Called Rheola Diorite by Marlow and Bushell (1995).||||||
16064|Rheola Gabbro|68189|6|Mentioned|p42 App.2||||411 +/- 8 Ma (K-Ar, Richards & Singleton, 1981).|||||30-JUN-14
16064|Rheola Gabbro|73576|6|Mentioned|p803 Fig.1, p809|Devonian|Devonian|||||||
16066|Rhyll Arkose|22476|2|Defined|p958||Neocomian|Expansion of definition by Jenkins 1962.||||||08-FEB-17
16066|Rhyll Arkose|22495|6|Mentioned|P220||Late Cretaceous|||||||
16066|Rhyll Arkose|24453|4|Described|p808, p809 Fig.2|Valanginian|Berriasian|Massive or weakly cross-bedded, feldspathic granulstones and sandstones. Of Tyers River Subgroup. Geological Province: Gippsland Basin.||||||07-FEB-11
16066|Rhyll Arkose|24551|6|Mentioned|p261|||Of the Strzelecki Group.||||||
16066|Rhyll Arkose|30905|6|Mentioned|p160|||||||||
16066|Rhyll Arkose|32002|6|Mentioned|p120|||||||||
16066|Rhyll Arkose|41642|6|Mentioned|p230|||||||||
16066|Rhyll Arkose|42318|6|Mentioned|Fig.5 P12|||||||||
16066|Rhyll Arkose|42827|5|Briefly described|p230|||see also Table 7.3||||||
16066|Rhyll Arkose|61329|6|Mentioned|p123|||On Phillip Island.||||||
16066|Rhyll Arkose|63124|5|Briefly described|p61|||Of the lower Strzelecki Group. Geological Province: Gippsland Basin. Equivalent of Pretty Hill Formation sequence in Otway Basin.||||||
16066|Rhyll Arkose|64289|6|Mentioned|p17|Neocomian|Neocomian|On Mornington Peninsula, Victoria.||||||07-FEB-11
16066|Rhyll Arkose|64616|6|Mentioned|p141|||Obsolete name established in 1962 on Phillip Island. Eumeralla Formation used for these rocks since 1971.||||||
16066|Rhyll Arkose|70378|6|Mentioned|p696 Fig.1|Cretaceous|Cretaceous|||Strzelecki Group.||||
16066|Rhyll Arkose|75065|5|Briefly described|p157|Early Cretaceous|Early Cretaceous|Gippsland Basin.||Tyers River Subgroup.||Passes eastwards into Rintouls Creek Sandstone.|Arkose with minor associated mudstones and thin floodplain coals.|
41834|Rhymney Schist|60451|4|Described|p63, 71, 111, 164-165|||Of the Moornambool Metamorphic Complex. Type section in text. Upper greenschist grade metamorphism + some contact metamorphism. Magdala Volcanic and Warrak formation probably protoliths of this unit.||||||
41834|Rhymney Schist|60454|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-biotite-graphite schist; black, laminated, thin graded quartz and pelite layers are relict bedding.||||||
41834|Rhymney Schist|60457|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-biotite-graphite schist; black, laminated; thin graded quartz and pelite layers are relict bedding.||||||
41834|Rhymney Schist|60458|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Unit does not appear on this map.||||||
41834|Rhymney Schist|60459|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Moornambool Metamorphic Complex. Quartz-biotite graphitic schist. Biotite greenschist grade.||||||29-SEP-04
41834|Rhymney Schist|61187|6|Mentioned|p82, p83 Fig.1, p84 Fig.2.|||This unit may have the Magdala Metabasalt as precursor.||||||
41834|Rhymney Schist|61752|5|Briefly described|p6 Fig. 2|Cambrian|Cambrian|Volcanogenic sediments.||||||07-FEB-11
41834|Rhymney Schist|66002|5|Briefly described|p5 Tb.2|Cambrian|Cambrian|Of Moornambool Metamorphic Complex. Defined by Cayley and Taylor 2001.||||||
41834|Rhymney Schist|68116|5|Briefly described|Appendix, Map 30.|Late Cambrian|Middle Cambrian||||||Quartz-biotite-graphite schist, black, laminated: thin graded quartz and pelite layers are relict bedding; pelitic layers contain biotite and graphitic material; black, greasy texture; disseminated pyrrhotite and pyrite mineralization; nonmagnetic.|
16073|Rices Hill Sandstone Member|24249|5|Briefly described|p90 Fig.3, p93|Pridoli|Pridoli|Parent: Humevale Formation||||||
16073|Rices Hill Sandstone Member|38378|6|Mentioned|p134|||||||||
16073|Rices Hill Sandstone Member|38787|6|Mentioned|p134|||||||||
16073|Rices Hill Sandstone Member|61185|6|Mentioned|p24-25 Fig. 7|||Of Garratt (1986). Former stratigraphic subdivision of Lower Palaeozoic rocks associated with Humevale Siltstone and Walhalla Group sediments.||||||07-FEB-11
16077|Richmond Granite|23309|5|Briefly described|p442, App1|||G361 I-Type.||||||
16077|Richmond Granite|24551|6|Mentioned|p229|||Of the Charlton Province.||||||
16077|Richmond Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
16077|Richmond Granite|60491|4|Described|p46|||Of the Coonooer Suite. I-type.||||||22-NOV-04
16077|Richmond Granite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Coonooer Suite. Biotite granite: I-type, oxidised; fine grained pink to white; some small crosscutting pegmatite veinlets.||||||
16077|Richmond Granite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of the Coonooer Suite. Granite; reduced S-type: nonmagnetic; K high, Th low, U moderate.||||||30-SEP-04
16077|Richmond Granite|66002|5|Briefly described|p6 Tb.5|||Of Coonooer Suite. G361. Defined in Bibby and Moore 1998.||||||
16077|Richmond Granite|68116|5|Briefly described|Appendix, Map 16.|Middle Devonian|Early Devonian||||||Biotite granite: I-type, oxidised; fine grained pink to white; some small pegmatite veinlets.|
25442|Riddell Sandstone|22628|5|Briefly described|fig1p108|||||||||
25442|Riddell Sandstone|22885|5|Briefly described|map|Late Ordovician|Late Ordovician|||||||
25442|Riddell Sandstone|22886|4|Described|p12|Late Ordovician|Late Ordovician|Previously known as Riddell Grits.||||||14-APR-08
25442|Riddell Sandstone|23229|4|Described|Table3-2p20-1, 22|Bolindian|Darriwilian|||||||
25442|Riddell Sandstone|23272|5|Briefly described|p414, Fig14-4.1p415, 423|Bolindian|Darriwilian|Former Name: Riddell Grits.||||||14-APR-08
25442|Riddell Sandstone|23307|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
25442|Riddell Sandstone|23309|5|Briefly described|p42, 60, 80, 155.  Tb 2.18 Fig. 2.14||Ordovician|||||||
25442|Riddell Sandstone|24002|5|Briefly described|p240|Late Ordovician|Late Ordovician|||||||
25442|Riddell Sandstone|24551|4|Described|p105|Late Ordovician|Late Ordovician|Of the Sunbury Group. Total thickness probably exceeds 1000m. Includes complete Bouma sequences. Conformably overlain by Bolinda Shale.||||||
25442|Riddell Sandstone|24588|5|Briefly described|p29|Eastonian|Eastonian|Of the Sunbury Group. Geological Province: Darraweit Guim Province. Is overlain by Bolinda Shale?||||||29-NOV-13
25442|Riddell Sandstone|40761|6|Mentioned|p222|||||||||
25442|Riddell Sandstone|41570|3|Fully described|p81|||See also P87||||||
25442|Riddell Sandstone|41572|6|Mentioned|p13|||||||||
25442|Riddell Sandstone|41585|6|Mentioned|Fig.4.1|||||||||
25442|Riddell Sandstone|42628|5|Briefly described|Map legend|Bolindian|Darriwilian|||||||
25442|Riddell Sandstone|42826|2|Defined|p30|Late Ordovician||||||||
25442|Riddell Sandstone|42827|5|Briefly described|p87|||||||||
25442|Riddell Sandstone|44197|5|Briefly described|Map Legend||Late Ordovician|||||||
25442|Riddell Sandstone|61187|6|Mentioned|p5 Fig.3. |Late Ordovician|Late Ordovician|||||||
25442|Riddell Sandstone|62099|5|Briefly described|p332|Late Ordovician|Late Ordovician|Thickness: >800m. In the Bendigo Zone of the Lachlan Orogen. ||||||
25442|Riddell Sandstone|63083|6|Mentioned|p223 Fig. 4|Late Ordovician|Late Ordovician|||||||07-FEB-11
25442|Riddell Sandstone|64619|5|Briefly described|Map legend|Late Ordovician|Late Ordovician|Of the Sunbury Group. Sandstone, black shale, black and grey siltstone. Sandstone is thin to thick bedded, turbiditic. Shale is commonly graptolitic; uncommom sandstone, well sorted, x-bedded; minor conglomerate - etc.||||||
25442|Riddell Sandstone|65715|5|Briefly described|p4 Tb.2|Ordovician|Ordovician|Of Sunbury Group. Formation rank.||||||
25442|Riddell Sandstone|66769|6|Mentioned|118|Ordovician|Ordovician|Rapid sedimentation into proto-Melbourne Zone from a proximal western source.||||||
25442|Riddell Sandstone|68116|5|Briefly described|Appendix, Maps 32, 41.|Hirnantian|Sandbian|Age written as Gisbornian to Bolindian in text. Informally subdivided into two units based on age, including  Eastonian and Gisbornian.|||||Sandstone, black shale, black and grey siltstone: sandstone thin to thick-bedded, turbiditic; shale commonly graptolitic; minor pebble conglomerate with well-rounded pebbles.|
25442|Riddell Sandstone|75072|5|Briefly described|p232, 240|Late Ordovician|Late Ordovician|Melbourne Zone. Zircon age distribution.||Sunbury Group.|||Metagreywacke.|
32568|Rileys Creek Granodiorite|22968|4|Described|P15, P186|Early Devonian|Late Silurian|Age of unit is 408+/-4 Ma, moderate to highly magnetic, parent is Swifts Creek Igneous Complex||||||
32568|Rileys Creek Granodiorite|23020|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Swifts Creek Igneous Complex. Biotite-hornblendite granodiorite to quartz diorite; I-type; inhomogeneous, strongly foliated, grey to dark grey, medium-coarse grained, with abundant stretched mafic igneous enclaves||||||23-JUN-14
32568|Rileys Creek Granodiorite|23030|5|Briefly described|Map legend|Early Devonian|Late Silurian|Parent is the Swifts Creek Igneous Complex. Biotiite-hornblende granodiorite, tonalite and quartz diorite: I-type; moderately to highly magnetic (250 nT); low to moderate K, low Th, U.||||||15-SEP-04
32568|Rileys Creek Granodiorite|23309|5|Briefly described|p295, 343, 344|Devonian|Silurian|G137 I-Type. Age: 408+/-4Ma, 402+/-4 Ma.||||||
32568|Rileys Creek Granodiorite|24004|6|Mentioned|p283|||||||||
32568|Rileys Creek Granodiorite|24551|6|Mentioned|p230, 726 Table 8.9|||||||||
32568|Rileys Creek Granodiorite|61161|5|Briefly described|p93|Early Devonian|Late Silurian|Probably of Rileys Creek Suite. GSV map code: G137.||||||
32568|Rileys Creek Granodiorite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Biotite-hornblende granodiorite, tonalite: grey; medium to coarse-grained; locally porphyritic in plagioclase; strongly foliated; abundant dark stretched quartz diorite and megacrystic tonalite enclaves give rock a migmatitic appearance.|
34904|Rileys Creek Suite|22968|6|Mentioned|Fig89 P164|Devonian|Silurian|||||||
34904|Rileys Creek Suite|23020|5|Briefly described|Map legend|Lochkovian|Pridoli|||||||
34904|Rileys Creek Suite|23021|5|Briefly described|Map legend|Lochkovian|Pridoli|||||||
34904|Rileys Creek Suite|23028|5|Briefly described|Map legend|Lochkovian|Pridoli|||||||
34904|Rileys Creek Suite|23029|5|Briefly described|Map legend|Lochkovian|Pridoli|||||||
34904|Rileys Creek Suite|23030|5|Briefly described|Map legend|Early Devonian|Late Silurian|||||||
34904|Rileys Creek Suite|24551|5|Briefly described|p230|||||||||
34904|Rileys Creek Suite|61160|6|Mentioned|p70|||Formerly a part of Fagan's (1979) Falls Creek Series. Now probably an obsolete name? Hornblende-bearing rock. ||||||
34904|Rileys Creek Suite|61161|5|Briefly described|p76-77 Fig 6.1, p92-97, p92 Fig. 6.11|Early Devonian|Early Devonian|Includes Junction Plain, Racecourse Plain, Horsehair Creek, Saturday Morning and Mungobabba Tonalites; Mount Baldhead Igneous Complex, Bundara Munjie Quartz Diorite, and possibly Morris Peak pluton and Rileys Creek Granodiorite. I-type.||||||
34904|Rileys Creek Suite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Bundara Munjie Quartz Diorite - quartz diorite phase and granodiorite phase, Mount Baldhead Granodiorite, Morris Peak pluton, and Marthavale,  Horsehair Creek, Racecourse Plain, Junction Plain and Saturday Morning Tonalites.||||||
34904|Rileys Creek Suite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Bundara Munjie Quartz Diorite - quartz diorite phase and granodiorite phase, Mount Baldhead Granodiorite, Morris Peak pluton, and Marthavale,  Horsehair Creek, Racecourse Plain, Junction Plain and Saturday Morning Tonalites.||||||07-FEB-11
34904|Rileys Creek Suite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Bundara Munjie Quartz Diorite - quartz diorite phase and granodiorite phase, Mount Baldhead Granodiorite, Morris Peak pluton, and Marthavale,  Horsehair Creek, Racecourse Plain, Junction Plain and Saturday Morning Tonalites.||||||
34904|Rileys Creek Suite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Bundara Munjie Quartz Diorite - quartz diorite phase and granodiorite phase, Mount Baldhead Granodiorite, Morris Peak pluton, and Marthavale,  Horsehair Creek, Racecourse Plain, Junction Plain and Saturday Morning Tonalites.||||||
34904|Rileys Creek Suite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Bundara Munjie Quartz Diorite - quartz diorite phase and granodiorite phase, Mount Baldhead Granodiorite, Morris Peak pluton, and Marthavale, Horsehair Creek, Racecourse Plain, Junction Plain and Saturday Morning Tonalites.||||||
34021|Rintoul Creek Formation|22476|2|Defined|p934,5,6||Neocomian|Includes Locmany and Exalt Members||||||08-FEB-17
34021|Rintoul Creek Formation|24453|4|Described|p808, p809 Fig.2|Hauterivian|Valanginian|Siltstone and sandstone. Overlies Tyers Conglomerate. Of Tyers Creek Subgroup.||||||07-FEB-11
34021|Rintoul Creek Formation|24551|6|Mentioned|p263|Neocomian|Neocomian|Of the Tyers Subgroup.||||||02-AUG-05
34021|Rintoul Creek Formation|64616|5|Briefly described|p142|Early Cretaceous|Early Cretaceous|Name proposed to be dropped. The unit includes an arkosic succession at the top that is of entirely different provenance to the quartz-lithic sequence below. Overlies Tyers Conglomerate. Included Locmany and Exalt Members. Also appears as Rintouls Creek Formation in Tb.5.6 and p143.||||||
34021|Rintoul Creek Formation|70378|4|Described|p710-711|Early Cretaceous|Early Cretaceous|Originally the Rintouls Creek Sandstone (Phillip, 1958); see references (p695, p702 Fig.7, p709 Fig.12, p712 Fig.15). Renamed as Rintoul Creek Formation, it was subdivided into these two Members by Tosolini et al. (1999) and assigned to the renamed Tyers River Subgroup (formerly Tyers Group). See also references to mis-spelt Rintouls Creek Formation (p695-696, 698-700, 702-703, 707-709, 714). The type area is outcrops in Rintoul Creek. 278m thick. Source rock and reservoir target for petroleum wells: oil slicks have been observed in mudstone outcrops. Hydrocarbon characterisation diagrams, gamma and lithology log, and gamma log and TOC % diagram, from Yallourn North-1A.||Tyers River Subgroup.|Locmany and Exalt Members.|Overlies Tyers Conglomerate. Is overlain by Wonthaggi Formation.||
34021|Rintoul Creek Formation|75065|5|Briefly described|p151, 156|Valanginian|Valanginian|Gippsland Basin; onshore. Alluvial, fluvial deposits.||Tyers River Subgroup.||Overlies Tyers Conglomerate.||
35598|Riverina Granite|23275|6|Mentioned|p472|||Possibly an informal building stone name? See also Riverina Grey Granite.||||||13-MAR-07
16131|Rivernook Member|24551|6|Mentioned|p630|Eocene|Eocene|Of the Dilwyn Formation||||||
16131|Rivernook Member|24562|6|Mentioned|p76 Fig. 30|||||||||
16131|Rivernook Member|29355|6|Mentioned|p189|||||||||
16131|Rivernook Member|30454|6|Mentioned|Fig.1|||||||||
16131|Rivernook Member|31036|6|Mentioned|p196|||See also P208. Unit of Dilwyn Fm.||||||
16131|Rivernook Member|31372|6|Mentioned|Fig. 2|||||||||
16131|Rivernook Member|31624|6|Mentioned|p101|||Palaeocene. T.F. unit of Dartmoor Fm.||||||
16131|Rivernook Member|31920|6|Mentioned|p60|||Unit of Dilwyn Fm.||||||
16131|Rivernook Member|32115|5|Briefly described|p1|||Early Tertiary. See also Fig.1||||||
16131|Rivernook Member|32117|6|Mentioned|Fig.2|||||||||
16131|Rivernook Member|33155|5|Briefly described|p122|||||||||
16131|Rivernook Member|33949|6|Mentioned|p274|||||||||
16131|Rivernook Member|34343|5|Briefly described|p97|||See also p102.||||||02-OCT-07
16131|Rivernook Member|35066|5|Briefly described|p206|||||||||
16131|Rivernook Member|41043|6|Mentioned|p95|||||||||
16131|Rivernook Member|41517|6|Mentioned|p134|||See also Fig.3||||||
16131|Rivernook Member|42827|5|Briefly described|p280|||Of Dilwyn Formation.||||||02-OCT-07
16131|Rivernook Member|44232|14|Not recorded|p20||Paleocene|Of Dilwyn Clay.||||||
16131|Rivernook Member|47054|6|Mentioned|p491|||||||||
16131|Rivernook Member|48911|6|Mentioned|Chart 1|||||||||
16131|Rivernook Member|61182|6|Mentioned|p22|||Of Baker (1953) - recognised within the Dilwyn Formation at the coast, but has not been unequivocally identified elsewhere. Geological Province: Otway Basin. See also Rivernook bed.||||||
16131|Rivernook Member|62896|5|Briefly described|p89, p90 Tb. 1|Eocene|Paleocene|Of Dilwyn Formation (Wangerrip Group) near the base of of Pember Mudstone. Thickness: 6m. Glauconitic and limonitic sand and clay.||||||07-FEB-11
16131|Rivernook Member|63740|4|Described|p89, p90 Tb. 1|||Of Dilwyn Formation. Geol.prov: Otway Basin. Outcrops at coast. Thickness: 6m. Glauconitic and limonitic sand and clay with a lower bed usually concealed by beach sand and referred to as Rivernook A bed - also of glauconitic and micaceous silty clay.||||||07-FEB-11
16131|Rivernook Member|70942|4|Described|p126, 119|||||||||
34865|Roadsend Formation|22968|4|Described|Fig49 P92, P144||Early Devonian|New name, top formation of the Avonmore Subgroup, overlain by Buchan Caves Limestone, maximum thickness is 40m||||||
34865|Roadsend Formation|23021|5|Briefly described|Map legend|Pragian|Pragian|Parent is the Snowy River Volcanics||||||
34865|Roadsend Formation|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Avonmore Subgroup||||||
34865|Roadsend Formation|23309|4|Described|p113, 117  Tb 2.38|||Of the Avonmore Subgroup.  Maximum Thickness: 40m.||||||22-FEB-10
34865|Roadsend Formation|24551|5|Briefly described|p139 Fig. 5.30|Early Devonian|Early Devonian|Of the Avonmore Subgroup.||||||02-AUG-05
16160|Roaring Mag Member|23309|5|Briefly described|p104, 133  Tb 2.38|||||||||
16160|Roaring Mag Member|23710|14|Not recorded|p84|||Excursion details.||||||
16160|Roaring Mag Member|24551|5|Briefly described|p138, 620|||Of the Tabberabbera Formation.||||||
16160|Roaring Mag Member|33326|6|Mentioned|p434|||Fauna.||||||
16160|Roaring Mag Member|33393|6|Mentioned|p173|||||||||
16160|Roaring Mag Member|33732|5|Briefly described|Table III|||||||||
16160|Roaring Mag Member|34926|6|Mentioned|p120|||||||||
16160|Roaring Mag Member|34954|6|Mentioned|Fig.34|||||||||
16160|Roaring Mag Member|37330|5|Briefly described|p17|||||||||
16160|Roaring Mag Member|41585|6|Mentioned|Fig.4.9|||||||||
16160|Roaring Mag Member|42033|6|Mentioned|p653|||||||||
16160|Roaring Mag Member|42577|5|Briefly described|Fig.3, P31|||||||||
16160|Roaring Mag Member|43530|14|Not recorded|p1030|||Part of Wentworth Group||||||
16160|Roaring Mag Member|43547|14|Not recorded|Table p153,154||Eifelian|||||||
16160|Roaring Mag Member|48971|6|Mentioned|p42|||||||||
16160|Roaring Mag Member|61161|5|Briefly described|p118|||Of Tabberabbera Formation. Upper part of formation. Overlies Kilgower Member. Dominantly mudstone.||||||
29550|Robertson Creek Granodiorite|42971|5|Briefly described|p144, Fig.2 p143|||||||||
16197|Robleys Spur Volcanics|23309|5|Briefly described|p164-166, 171,  Tb 2.61|||||||||
16197|Robleys Spur Volcanics|24551|5|Briefly described|p164, p163 Fig. 6.4|Late Devonian|Late Devonian|Of Taggery Subgroup, Marysville Igneous Complex||||||
16197|Robleys Spur Volcanics|35073|5|Briefly described|Table 2|||||||||
16197|Robleys Spur Volcanics|35186|4|Described|p6|||||||||
16197|Robleys Spur Volcanics|35277|3|Fully described|p87|||||||||
16197|Robleys Spur Volcanics|39291|6|Mentioned|Table 1|||||||||
16197|Robleys Spur Volcanics|41641|4|Described|p157|||See also P160||||||
16197|Robleys Spur Volcanics|42827|4|Described|p160|||see also Fig 5.2||||||
16197|Robleys Spur Volcanics|68311|5|Briefly described|p273-274|Late Devonian|Late Devonian|Cerberean Cauldron, Central Victoria. Up to 150m thick. Pre-collapse phase.||Taggerty Subgroup.||Overlies Torbreck Spur Andesite. Is overlain by Rubicon Ignimbrite (Cerberean Subgroup).|Rhyolitic ignimbrites and lava flows.|
69145|Rock Coal Seam|61140|5|Briefly described|p9, p11|Early Cretaceous|Early Cretaceous|Informal name. Of the Strzelecki Group.  Historical perspective.||||||
39879|Rocklands Volcanic Group|24383|6|Mentioned|p56 Tb.6|||||||||
39879|Rocklands Volcanic Group|24551|6|Mentioned|p52 Fig. 2.66|||||||||
39879|Rocklands Volcanic Group|50154|2|Defined|p17, p22, p43, p113-114|Early Devonian|Early Devonian|Unconformably overlies the Grampians Group and Nargoon Group, nonconformably overlies the granite and schist of the Glenelg River Metamorphic Complex. Overlain by Newer Volcanics. Age: ca. 410 Ma. Min. thickness: 250m||||||15-SEP-04
39879|Rocklands Volcanic Group|50155|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
39879|Rocklands Volcanic Group|50156|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||24-AUG-04
39879|Rocklands Volcanic Group|50157|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
39879|Rocklands Volcanic Group|50158|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
39879|Rocklands Volcanic Group|50160|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||16-JUN-04
39879|Rocklands Volcanic Group|50161|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
39879|Rocklands Volcanic Group|50162|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
39879|Rocklands Volcanic Group|50163|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
39879|Rocklands Volcanic Group|60421|5|Briefly described|p408 Fig. 1, 409, 411, 416|Devonian|Devonian|Non-conformably underlies: Dorodong Sands. Includes: Nigretta Ignimbrite.||||||24-MAY-13
39879|Rocklands Volcanic Group|61841|5|Briefly described|p242, p244|Early Devonian|Early Devonian|Unconformably overlies a Cambrian basement and the Grampians Group.||||||
39879|Rocklands Volcanic Group|61842|5|Briefly described|p246|Early Devonian|Early Devonian|Includes ignimbrites.  Age: 410Ma.||||||
39879|Rocklands Volcanic Group|65313|6|Mentioned|p582|||See also superseded Rocklands Rhyolite (p580) and Rocklands Volcanics (p581 Fig. 9, p582). Considered comagmatic with Mafeking, Mackenzie River, Victoria Valley and Mirranatwa Granites.|U-Pb zircon age 410 +/- 3 (VandenBerg 2003).|||||26-MAR-12
39879|Rocklands Volcanic Group|66002|5|Briefly described|p6 Tb.4|Devonian|Devonian|Includes Barangaroo Ignimbrite, Cadden Rhyolite, Fern Hill Microgranite, Gatum Ignimbrite, Glendinning Ignimbrite, Mooralla Ignimbrite, Nigretta Ignimbrite, Toolondo Volcaniclastics & Yat Nat Ignimbrite. Called Rocklands Rhyolites by Spencer-Jones (1965).||||||24-MAY-13
39879|Rocklands Volcanic Group|66286|6|Mentioned|p189, p192.|||Source material in Dundas Tableland for fluvial sediments of Loddon River Group. Weathering profiles show lenticular or platy mottles providing pathways for root growth.||||||
39879|Rocklands Volcanic Group|68116|5|Briefly described|Appendix, Maps 29, 30, 38-39.|Early Devonian|Early Devonian||||||Ryholite lava: flow banded; ignimbrite; volcaniclastic sedimentary rocks; microgranite.|
39879|Rocklands Volcanic Group|70877|5|Briefly described|p10, p12-p13|Early Devonian|Early Devonian|Grampians-Stavely Zone. May be comagmatic with late Silurian to early Devonian rocks which intrude the Grampians Group. See Rocklands Volcanics.|||||Intermediate-felsic volcanic rocks.|
39879|Rocklands Volcanic Group|70967|6|Mentioned|p10|Early Devonian|Early Devonian|Mount Stavely Belt.||||||
39879|Rocklands Volcanic Group|71593|4|Described|p8, p12, p44-p45, p47-p49|Early Devonian|Early Devonian|Occupies an area of 1500 km ^2. Up to 250m thick, generally less than 100m thick. Referred to as the Rocklands Volcanics on p45 and p138. Intersected by numerous drillholes including Woohlpooer 6. Geochemically and temporally similar to the Victoria Valley Complex. See also  p59, p68, p85, p99, p102, p133, p138, p197, p203.|c. 400 Ma |||Overlies the Grampians Group. Unconformably overlain by the Newer Volcanic Group.|Flat-lying sheets of felsic ignimbrite and lava.|
39879|Rocklands Volcanic Group|72445|5|Briefly described|p9-10.|Early Devonian|Early Devonian|See also Rocklands Volcanics App.7 p6 Fig.3. Occurs west of the Grampians Ranges.||||Comagmatic with Dwyer Granite, Mirranatwa Granite, Bullawin Porphyry, Mafeking Suite and Duchembegarra Granite.||15-OCT-20
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.||||||
30541|Rocky Camp Limestone Member|23309|5|Briefly described|p114, 117, 118 Tb 2.41|||Of the Murrindal Limestone.||||||
30541|Rocky Camp Limestone Member|23615|3|Fully described|p141-142|Early Devonian|Early Devonian|Of Murrindal Limestone.  Overlies McLarty Limestone Member.  Orginally defined by Teichert and Talent (1958) and redefined by Wallace (1982) to include all the pale limestone in the Murrindal Limestone.||||||
30541|Rocky Camp Limestone Member|24551|5|Briefly described|p147|||Of the Murrindal Limestone.||||||02-AUG-05
30541|Rocky Camp Limestone Member|43206|5|Briefly described|map legend|Emsian|Emsian|Of Murrindal Limestone||||||
29715|Rocky Jack Granite|23309|6|Mentioned|p442 Appendix 1|||G509, I-Type.||||||
29715|Rocky Jack Granite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|I-type? Altered felsic granite clinozoisite / epidote, foliated||||||22-OCT-04
29715|Rocky Jack Granite|43315|5|Briefly described|Map Legend|Wenlock|Wenlock|I-type? Altered felsic granite clinozoisite/epidote, foliated.||||||03-MAY-05
29715|Rocky Jack Granite|60541|4|Described|p64|Silurian|Silurian|Small dyke-like felsic body; highly altered with ubiquitous epidote group minerals; large clinozoisite crystals occur as veins, with interstitial qtz, probably infilling vughs. Quartz dominates over plagioclase... Geol.Prov: LFB. Age is Middle Silurian.||||||23-JUN-14
29715|Rocky Jack Granite|68116|5|Briefly described|Appendix, Map 45.|Wenlock|Llandovery||||||Granite: felsic; foliated; altered, with clinozoisite/epidote; I-type?|
30585|Rocky Valley Granodiorite|23309|6|Mentioned|p442 App1|||G155 I-Type.||||||
30585|Rocky Valley Granodiorite|43220|5|Briefly described|p11||Devonian|||||||
30585|Rocky Valley Granodiorite|44184|5|Briefly described|Map Legend||Early Devonian|Shown as Rocky Valley I-type.||||||
30585|Rocky Valley Granodiorite|61160|6|Mentioned|p70|||Former name for a part of East Kiewa Granodiorite near eastern end of Rocky Valley Reservoir. ||||||
37776|Rodger River Granodiorite|23309|6|Mentioned|p442 Appendix 1|||G60, I-Type. Supersedes Rodger River Granite.||||||
37776|Rodger River Granodiorite|23615|4|Described|p202 App. 1|||Name used interchangeably with Rodger River Granite throughout publication.||||||
37776|Rodger River Granodiorite|24551|6|Mentioned|p234|||||||||
37776|Rodger River Granodiorite|44185|5|Briefly described|Map legend.|||I-type. Age uncertain: shown as SDg, ie Silurian-Devonian.||||||
37776|Rodger River Granodiorite|68116|5|Briefly described|Appendix, Map 36.|Devonian|Silurian||||||Biotite-augite granodiorite: slightly K-feldspar phyric; with igneous and sedimentary enclaves; I-type.|
38296|Romeny Diorite|24383|4|Described|p23, 48-49|||Geological Province: Lachlan Fold Belt||||||03-FEB-15
38296|Romeny Diorite|24384|5|Briefly described|Map legend|Late Devonian|Late Devonian|||||||
38296|Romeny Diorite|24385|5|Briefly described|Map legend|Late Devonian|Late Devonian|Diorite: medium-grained, equigranular, dark green and pink; magnetic.||||||
38296|Romeny Diorite|24386|5|Briefly described|Map legend|Late Devonian|Late Devonian|Diorite, medium-grained, equigranular, dark green and pink; magnetic.||||||
38296|Romeny Diorite|24387|5|Briefly described|Map legend|Late Devonian|Late Devonian|Diorite; medium-grained, equigranular, dark green and pink; magnetic||||||01-OCT-04
38296|Romeny Diorite|24388|5|Briefly described|Map legend|Late Devonian|Late Devonian|Diorite; moderately magnetic; gravity and radiometric responses not determined due to small size of pluton.||||||
38296|Romeny Diorite|65715|6|Mentioned|p8 Tb.4|||G292. Of Willman et al. (2002) p48.||||||
37591|Romsey Subgroup|23309|5|Briefly described|p51-53, 56. Table 2.16|||Of Castlemaine Group. Includes Angry Hill Sandstone, Byro Gully Shale, Split Hill Sandstone, Stauro Gully Shale and Lano Gully Sandstone.||||||23-JUN-14
37591|Romsey Subgroup|24551|5|Briefly described|p96, 99|Middle Ordovician|Early Ordovician|Of the Castlemaine Group.||||||02-AUG-05
37591|Romsey Subgroup|60452|6|Mentioned|p27|Ordovician|Ordovician|Of the Castlemaine Group.||||||
37591|Romsey Subgroup|62099|5|Briefly described|p331|Ordovician|Ordovician|Of the Castlemaine Group. In the Bendigo Zone of the Lachlan Orogen.||||||
37591|Romsey Subgroup|64611|5|Briefly described|Map legend|Bendigonian|Lancefieldian|Of the Castlemaine Group.  Includes Lano Gully Sandstone and Stauro Gully Shale and undifferentiated Romsey Group sandstone/siltstone/black shale, chert.||||||23-JUN-14
37591|Romsey Subgroup|64612|2|Defined|p8, p34, p36-37|Bendigonian|Cambrian|Of Castlemaine Group. Includes Stauro Gully Shale, Lano Gully Sandstone. Underlain conformably by Goldie Chert (sharp contact). Overlain conformably by undifferentiated Castlemaine Group. Thick: 1200m. Quartz-mica sandstone and siltstone.||||||07-FEB-11
37591|Romsey Subgroup|64619|5|Briefly described|Map legend|Middle Ordovician|Early Ordovician|Of Castlemaine Group. Sandstone, siltstone, black shale, chert: sst of various colours, thick to thin-bedded, turbiditic; siltst. is dark green when fresh, generally well-bedded; shale graptolitic in places; deep-water turbiditic fan+hemipelagic deposits.||||||10-NOV-08
37591|Romsey Subgroup|65715|5|Briefly described|p4 Tb.2|Ordovician|Ordovician|Basal portion of Castlemaine Group in the vicinity of Lancefield-Romsey.||||||
37591|Romsey Subgroup|68116|5|Briefly described|Appendix, Map 32.|Floian|Late Cambrian|Minimum age written as Bendigonian in text.|||||Sandstone, siltstone, black shale, chert: sandstone various colours, thick to thin-bedded, turbiditic; siltstone: dark green when fresh, generally well bedded; shale: in places richly graptolitic; chert: minor, well bedded.|
16326|Rose Hill Marl Member|41043|6|Mentioned|p97|||||||||
68479|Rose River Volcanics|24551|5|Briefly described|p174||Late Devonian|Maximum Thickness: 450m. Consist of the Cobbler Rhyolite and Staircase Ignimbrite. Of the Wellington Volcanic Group||||||30-NOV-11
68479|Rose River Volcanics|61163|6|Mentioned|p95|||At Mount Cobbler. Comprises two units - Cobbler Rhyolite (formerly "Mine Creek Rhyolite" of Gaul, 1982, 1995).||||||
68479|Rose River Volcanics|66252|2|Defined|p209, p211, p212 Fig.2, p214, p216-217.|Frasnian|Frasnian|See also p219 Tb.1, p224, p226, p228-231. New name. Definition given. Outcrops along NW margins of Macalister Synclinorium. Equivalent to Refrigerator Gap Dacite in the S, and Bindaree Formation in the centre, of the Synclinorium. Comprises two formal Members: Cobbler Rhyolite and Staircase Ignimbrite. Unit in Avon River Group. Thickness to 450m. Correlated with Tolmie Igneous Complex: rhyolitic ignimbrite, rhyolite, rhyolitic breccia; minor red mudstone, basalt. Is overlain by Howitt Spur Formation. Geochemistry detailed.||||||
16373|Rotten Point Sand|30576|5|Briefly described|Table 2|||||||||
16373|Rotten Point Sand|30578|6|Mentioned|Table 1|||Also mention Table2||||||
16373|Rotten Point Sand|33155|5|Briefly described|p119|||||||||
16373|Rotten Point Sand|35066|5|Briefly described|p224|||||||||
16373|Rotten Point Sand|41043|6|Mentioned|p95|||||||||
16373|Rotten Point Sand|42318|6|Mentioned|Fig.2 P10|||||||||
16373|Rotten Point Sand|42827|4|Described|p298|||||||||
16373|Rotten Point Sand|43590|6|Mentioned|p15|||Mapped in Dilwyn Formation||||||
16373|Rotten Point Sand|61155|5|Briefly described|p18|Early Paleocene|Early Paleocene|Overlain by Johanna River Sand. Age: ~66-64Ma. Thickness: 30m. Geological Province: Aire Embayment.||||||
16373|Rotten Point Sand|61182|5|Briefly described|p19|||Of Dilwyn Formation (Wangerrip Group). Isolated outcrop mapped as part of Dilwyn Formation along with Johanna River Sand. Geological Province: Otway Basin. May be equivalent to Pebble Point Formation.||||||
16373|Rotten Point Sand|70942|5|Briefly described|p122, 119|||||||||
16380|Rough Creek Conglomerate Member|22968|5|Briefly described|P51, P110||Gisbornian|Parent is Towanga Sandstone, maximum thickness is 30m||||||
16380|Rough Creek Conglomerate Member|23021|5|Briefly described|Map legend|Llandovery|Llandovery|Parent is Yalmy Group||||||
16380|Rough Creek Conglomerate Member|23309|5|Briefly described|p86, 88  Tb 2.30|||||||||
16380|Rough Creek Conglomerate Member|23615|3|Fully described|p73|Llandovery|Llandovery|Of Towanga Sandstone.  Maximum thickness: 30m.  See also Rough Creek Conglomerate.||||||
16380|Rough Creek Conglomerate Member|24551|5|Briefly described|p131|||Of the Towanga Sandstone.||||||
16380|Rough Creek Conglomerate Member|41585|6|Mentioned|p125|||||||||
16380|Rough Creek Conglomerate Member|42827|5|Briefly described|p125|||||||||
16380|Rough Creek Conglomerate Member|43206|5|Briefly described|map legend||Llandovery|of Towanga Sandstone||||||
32296|Roundhead Member|13323|5|Briefly described|p393 Fig. 2|Maastrichtian|Maastrichtian|Of the Volador Formation (Halibut Subgroup, Latrobe Group). Geological Province: Gippsland Basin.||||||
32296|Roundhead Member|24090|5|Briefly described|p8 Fig.3|Maastrichtian|Maastrichtian|Of the Volador Formation.  Geological Province: Gippsland Basin.||||||19-JAN-05
32296|Roundhead Member|24551|6|Mentioned|p268, 478 Fig. 15.8||Paleocene|Of the Halibut Subgroup. Of the Volador Formation.||||||02-AUG-05
32296|Roundhead Member|61552|5|Briefly described|p583 Fig.2, p589.|Late Maastrichtian|Late Maastrichtian|||Unit in Volador Formation.||Is overlain by Kate Shale.|Transgressive sands.|
32296|Roundhead Member|64876|5|Briefly described|p144-147, p151, p153-155|Late Cretaceous|Late Cretaceous|Gippsland Basin. Strandplain and restricted-marine deposits. Depositional environments and facies described in detail.||Volador Formation.|||Marine shale overlain by incised fluvial sediments.|
32296|Roundhead Member|65717|5|Briefly described|p9 Fig.2.2|Maastrichtian|Maastrichtian|||Volador Formation||Overlain by Kate Shale|Interbedded sandstone, siltstone, shale and coal.|05-SEP-17
32296|Roundhead Member|70076|5|Briefly described|South-Eastern: Fig.2; Regional: Fig.3|Maastrichtian|Maastrichtian|||Volador Formation.||Is overlain by Kate Shale or Grunter Member (Kingfish Formation).||
39643|Rowe's Shale|24088|6|Mentioned|p355 Fig. 4||| Geological Province: Lachlan Fold Belt.||||||
16400|Rowsley Formation|34991|6|Mentioned|p387|||||||||
16400|Rowsley Formation|37385|6|Mentioned|p15|||||||||
16400|Rowsley Formation|37547|6|Mentioned|p150|||||||||
16400|Rowsley Formation|39865|5|Briefly described|p28|||||||||
16400|Rowsley Formation|41537|6|Mentioned|p352|||||||||
16400|Rowsley Formation|41868|6|Mentioned|p509|||||||||
16400|Rowsley Formation|42827|6|Mentioned|p509|||||||||
16400|Rowsley Formation|42847|6|Mentioned|p522|||Unconformably overlies the Werribee Formation.||||||09-MAY-05
39635|Royal Albert Shale|24088|6|Mentioned|p355 Fig. 4||| Geological Province: Lachlan Fold Belt.||||||
26879|Rubicon Rhyolite|23229|6|Mentioned|p37|||||||||
26879|Rubicon Rhyolite|23235|6|Mentioned|Fig7-2p69|||||||||
26879|Rubicon Rhyolite|23309|4|Described|p164-167, Table 2.61|Early Carboniferous|Late Devonian|Of Cerberean Subgroup. Age: 359+/-15Ma, 361+/-13Ma (K/Ar biotite).  Same as Rubicon Ignimbrite.||||||
26879|Rubicon Rhyolite|29786|6|Mentioned|p75|||||||||
26879|Rubicon Rhyolite|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
26879|Rubicon Rhyolite|35073|6|Mentioned|p9|||See also Table 2.||||||
26879|Rubicon Rhyolite|35186|4|Described|p6|||||||||
26879|Rubicon Rhyolite|35277|6|Mentioned|p88|||||||||
26879|Rubicon Rhyolite|35278|6|Mentioned|p355|||||||||
26879|Rubicon Rhyolite|35283|6|Mentioned|p48|||||||||
26879|Rubicon Rhyolite|39291|6|Mentioned|p221|||See also Table 1||||||
26879|Rubicon Rhyolite|40725|6|Mentioned|Fig.1|||||||||
26879|Rubicon Rhyolite|41641|5|Briefly described|p158|||||||||
26879|Rubicon Rhyolite|41868|6|Mentioned|p486|||||||||
26879|Rubicon Rhyolite|44187|5|Briefly described|Map Legend||Late Devonian|||||||
26879|Rubicon Rhyolite|68116|5|Briefly described|Appendix, Maps 33, 42.|Late Devonian|Late Devonian||||||Rhyolite: light bluish-grey, porphyritic; phenocrysts of quartz, biotite, almandine, plagioclase and cordierite; pumiceous ignimbrite at base; base of formation contains concentration of hornfels and andesite lithic fragments.|
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|||||||||
25456|Run Boundary Granite|30906|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25456|Run Boundary Granite|30909|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25456|Run Boundary Granite|33553|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
25456|Run Boundary Granite|37029|6|Mentioned|p48|||||||||
25456|Run Boundary Granite|40328|4|Described|p210|||||||||
25456|Run Boundary Granite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
25456|Run Boundary Granite|40498|6|Mentioned|p376|||||||||
25456|Run Boundary Granite|42726|5|Briefly described|map legend|Silurian||||||||
25456|Run Boundary Granite|43383|14|Not recorded|p11||Ordovician|||||||
25456|Run Boundary Granite|44340|14|Not recorded|p.9,Table.1,p.5|||||||||
25456|Run Boundary Granite|44341|14|Not recorded|map legend||Ordovician|||||||
16454|Runnymede Formation|24551|6|Mentioned|p247|||At Killara Bluff in the Casterton area. Name proposed to be abandoned by Duddy (1983). Equivalent to Eumeralla Formation.||||||12-JAN-10
16454|Runnymede Formation|31245|6|Mentioned|p79|||L. Cretaceous||||||
16454|Runnymede Formation|31625|6|Mentioned|Fig. 5.2|||L.Cret.||||||
16454|Runnymede Formation|31920|5|Briefly described|p49|||Unit of Merino Gp.||||||
16454|Runnymede Formation|34148|6|Mentioned|p272|||||||||
16454|Runnymede Formation|41642|6|Mentioned|p218|||||||||
16454|Runnymede Formation|42827|5|Briefly described|Table 7.2|||of Otway Group||||||
16454|Runnymede Formation|48624|14|Not recorded|p5|||(J54-6/Benara).||||||
16454|Runnymede Formation|48625|14|Not recorded|p5|||(J54-6/Kennion).||||||
16454|Runnymede Formation|48911|6|Mentioned|Chart 1|||||||||
25457|Rutledge Marl Member|22875|5|Briefly described|p26 Table1|||||||||
25457|Rutledge Marl Member|31036|6|Mentioned|Table 9-1|||Unit of Port Campbell lst.||||||
25457|Rutledge Marl Member|31625|6|Mentioned|Fig. 5.2|||Miocene||||||
25457|Rutledge Marl Member|32601|6|Mentioned|p692|||||||||
25457|Rutledge Marl Member|34954|6|Mentioned|Fig.35|||||||||
25457|Rutledge Marl Member|35066|5|Briefly described|p213|||||||||
25457|Rutledge Marl Member|35271|6|Mentioned|p66|||||||||
25457|Rutledge Marl Member|36119|6|Mentioned|Fig.6|||||||||
25457|Rutledge Marl Member|41701|6|Mentioned|Map legend|Miocene||||||||
25457|Rutledge Marl Member|41769|5|Briefly described|p33|||||||||
25457|Rutledge Marl Member|42827|6|Mentioned|p287|||Supersedes Rutledges Creek Member. Of Port Campbell Limestone.||||||
25457|Rutledge Marl Member|43590|6|Mentioned|p26|||Included in Port Campbell Limestone||||||
25457|Rutledge Marl Member|48911|6|Mentioned|Chart 1|||||||||
25457|Rutledge Marl Member|61155|5|Briefly described|p18|Middle Miocene|Middle Miocene|Of the Port Campbell Limestone (Heytesbury Group). Overlies Gellibrand Marl. Age: 12.5-10.5Ma. Geological Province: Otway Basin (Tyrendarra and Port Campbell Embayments). ||||||
25457|Rutledge Marl Member|61182|5|Briefly described|p29|||Renamed by Bock and Glenie (1965) and Glenie (1971). Formerly Rutledges Creek Member or R.C.beds. Regarded as a tongue, and hence member, of Gellibrand Marl. Mallett (1977) considered it as equivalent of Glenample Clay, and not R.C.Member of Baker (1953).||||||
25457|Rutledge Marl Member|71437|4|Described|Fig. 1 opp 154, p155, p161-162|Miocene|Miocene|marine, neritic.||Top of Gellibrand Marl.||Transitional or interfingering with  Port Campbell Limestone.|Richly fossiliferous marl to limey marlstone.|
72926|Rutledges Creek beds|61182|6|Mentioned|p29|||One of three former subdivisions of Baker (1950) of Port Campbell Limestone, together with Peterborough and Port Campbell beds; also referred to as Rutledges Creek Member.||||||
35139|Ryans Creek Ignimbrite|22971|4|Described|p 24|Devonian|Devonian|Overlies Mine Creek Rhyolite. Max. thickness: 450m.  see also Ryans Creek Rhyolite - misspelling?||||||19-JAN-06
35139|Ryans Creek Ignimbrite|23309|5|Briefly described|p169, 181, 183, 185.  Table 2.64||Devonian|Age: 368 Ma. Supersedes: "Rose River Volcanics".||||||
35139|Ryans Creek Ignimbrite|24551|4|Described|p167|||Maximum Thickness: 400m. Of the Tolmie Igneous complex. Overlying unit Toombullup Rhyodacite.||||||
35139|Ryans Creek Ignimbrite|64312|5|Briefly described|p440|||Of the Wabonga Volcanic Complex. S-type granite - rich in barium.||||||
35139|Ryans Creek Ignimbrite|68116|5|Briefly described|Appendix, Maps 26, 34.|Late Devonian|Late Devonian||||||Rhyolitic quartz ignimbrite: cordierite and garnet phenocrysts, densely welded/recrystallized; shows upward zonation from a chilled dark base, to eutaxitic and partly microcrystalline, to recrystallized.|
35139|Ryans Creek Ignimbrite|69669|5|Briefly described|p951|Late Devonian|Late Devonian|Contains garnet phenocrysts with rutile inclusions, indicating earliest crystallisation at deep (c.35 km) crustal conditions. Recalculated Sr and Nd isotope data confirm that Tolmie Igneous Complex magmas were derived from metasedimentary protoliths constructed from materials not long extracted from the mantle.||||||
35139|Ryans Creek Ignimbrite|73199|6|Mentioned|p524-526|Frasnian|Frasnian|S-type. Geochron from Clemens et al. (2014).|377 Ma|Tolmie Igneous Complex||Overlain by Toombullup Ignimbrite.|Includes crystal-poor, high-Ba, strongly ferroan, low-silica rhyolite.|
37594|S Creek Granodiorite|23309|5|Briefly described|p165|||Formerly known as unnamed unit Dgk2.||||||
23952|Saint Arnaud Group|22530|6|Mentioned|p693||Cambrian|Saint actually spelt St||||||
23952|Saint Arnaud Group|22531|5|Briefly described|p6|Cambrian|Cambrian|Saint is written St. in text||||||
23952|Saint Arnaud Group|22628|6|Mentioned|fig4p114||Cambrian|||||||
23952|Saint Arnaud Group|22708|5|Briefly described|p210|Early Silurian|Early Silurian|||||||
23952|Saint Arnaud Group|22756|4|Described|P6, P20|Ordovician|Cambrian|||||||
23952|Saint Arnaud Group|22799|5|Briefly described|p15|Ordovician|Cambrian|||||||
23952|Saint Arnaud Group|22857|5|Briefly described|p89 Fig. 14.7A, p98|Cambrian|Cambrian|Saint is St. in text of figure. Geological Province: Stawell Basin. ||||||
23952|Saint Arnaud Group|22858|5|Briefly described|p75,98|Ordovician|Cambrian|||||||
23952|Saint Arnaud Group|22887|6|Mentioned|p9||Cambrian|||||||
23952|Saint Arnaud Group|22893|6|Mentioned|p11 table3|||Given as a description of an unnamed equivalent of a basement rock in the Pooncarie 1:250000 but this rock completely concealed in the area.||||||01-JUL-13
23952|Saint Arnaud Group|23164|4|Described|p12|Cambrian|Cambrian|||||||
23952|Saint Arnaud Group|23166|5|Briefly described|Map legend|Ordovician|Cambrian|||||||
23952|Saint Arnaud Group|23168|5|Briefly described|Map legend|Ordovician|Cambrian|||||||
23952|Saint Arnaud Group|23169|5|Briefly described|Map legend|Ordovician|Cambrian|||||||
23952|Saint Arnaud Group|23300|5|Briefly described|Map Legend|Ordovician|Cambrian|Saint is St. in text||||||
23952|Saint Arnaud Group|23301|5|Briefly described|Map Legend|Ordovician|Cambrian|Saint is St. in text||||||
23952|Saint Arnaud Group|23302|5|Briefly described|Map Legend|Ordovician|Cambrian|Saint is St. in text||||||
23952|Saint Arnaud Group|23303|5|Briefly described|Map Legend|Ordovician|Cambrian|Saint is St in text||||||
23952|Saint Arnaud Group|23304|5|Briefly described|Map Legend|Ordovician|Cambrian|Saint is St in text||||||
23952|Saint Arnaud Group|23305|4|Described|p37||Cambrian|Previously St Arnaud Beds of Vandenberg and Wilkinson 1982. Defined by Cayley and McDonald 1995. Age presumed due to lack of Ordovician graptolites. Lachlan Fold Belt.||||||
23952|Saint Arnaud Group|23307|5|Briefly described|Map Legend|Cambrian|Cambrian|Saint is St. in text||||||
23952|Saint Arnaud Group|23309|5|Briefly described|p41-48,218. p5 Fig. 1.3|Late Cambrian|Late Cambrian|Saint is St in text. Includes Pyrenees, Beaufort and Warrak Formations.||||||
23952|Saint Arnaud Group|23402|6|Mentioned|p35|||||||||
23952|Saint Arnaud Group|23603|4|Described|p10|Ordovician|Cambrian|Geological Province: Lachlan Fold Belt.||||||
23952|Saint Arnaud Group|23604|5|Briefly described|Map Legend|Cambrian|Cambrian|Saint is St. in text.||||||
23952|Saint Arnaud Group|23605|5|Briefly described|Map Legend|Cambrian|Cambrian|Saint is St. in text.||||||
23952|Saint Arnaud Group|23606|5|Briefly described|Map Legend|Cambrian|Cambrian|Saint is St. in text.||||||
23952|Saint Arnaud Group|23607|5|Briefly described|Map Legend|Cambrian|Cambrian|Saint is St. in text.||||||
23952|Saint Arnaud Group|23814|5|Briefly described|p744|Early Ordovician|Late Cambrian|Saint is St in text.  Geological Province: Stawell Zone.||||||
23952|Saint Arnaud Group|24134|5|Briefly described|p6 Fig. 2|Middle Ordovician|Early Ordovician|Saint is St. in the text.||||||
23952|Saint Arnaud Group|24221|5|Briefly described|p893 Fig. 2|||Saint is St. in text.   Geological Province:  Lachlan Fold Belt||||||
23952|Saint Arnaud Group|24311|5|Briefly described|p1060, p1059 Fig. 2|Cambrian|Cambrian|Saint is St. in text||||||
23952|Saint Arnaud Group|24312|5|Briefly described|p1081|Cambrian|Cambrian|Saint is St. in text.||||||
23952|Saint Arnaud Group|24439|5|Briefly described|p7 Fig. 2|Cambrian|Cambrian|Saint is St. in text of figure.||||||
23952|Saint Arnaud Group|24551|3|Fully described|p83|Cambrian|Cambrian|Saint is St in text. Conformably overlies Magdala Volcanics. Consists of three formations.||||||01-AUG-05
23952|Saint Arnaud Group|37501|6|Mentioned|p407|||||||||
23952|Saint Arnaud Group|42745|5|Briefly described|p3, p6|||Actually spelt St Arnaud Group. Formerly St Arnaud Beds.||||||
23952|Saint Arnaud Group|43033|5|Briefly described|p6|||actually spelt St Arnaud Group.||||||21-OCT-08
23952|Saint Arnaud Group|43260|5|Briefly described|Map Legend|Ordovician|Cambrian|||||||
23952|Saint Arnaud Group|43627|6|Mentioned|Map|||||||||
23952|Saint Arnaud Group|43846|5|Briefly described|10|Ordovician|Cambrian|Thickness at least 4000m.||||||21-OCT-08
23952|Saint Arnaud Group|44093|6|Mentioned|p47, p91|||See also p102 Fig. 10.3, p106. Correlated with Robertson Bay Group in Antarctica.||||||
23952|Saint Arnaud Group|44186|5|Briefly described|Map Legend||Cambrian|||||||
23952|Saint Arnaud Group|44188|6|Mentioned|Map Legend|Middle Ordovician|Late Cambrian|Geological province: Kanmantoo Fold Belt/Lachlan Fold Belt. Fine-grained black slate with thin carbonate and quartz veins parallel to and cross cutting cleavage.||||||15-MAY-08
23952|Saint Arnaud Group|44191|6|Mentioned|Map Legend|Early Ordovician|Cambrian|||||||
23952|Saint Arnaud Group|44931|5|Briefly described|Map Legend|Ordovician|Cambrian|Includes: Magdala Metabasalt, Moornambool Schist and Harrow Granite.||||||14-JUN-06
23952|Saint Arnaud Group|50154|6|Mentioned|p18 Fig 3.1|||Geological Province: Lachlan Fold Belt. Saint is St. in text.||||||
23952|Saint Arnaud Group|60451|4|Described|p21 Fig. 7, 23, 24, 57, 107, 147|Late Cambrian|Late Cambrian|Deformed quartz-rich turbidites. Includes: Warrak Formation. Discussed in the context of Moornambool Metamorphic Complex. Saint is St in text.||||||23-MAY-13
23952|Saint Arnaud Group|60452|4|Described|p21|Late Cambrian|Late Cambrian|An unfossiliferous sequence of turbidites. Includes the Warrack, Beaufort and Pyrenees Formations. Conformably overlies the Magdala Volcanics at Stawell. Saint is St in text.||||||17-JAN-07
23952|Saint Arnaud Group|60454|5|Briefly described|Map Legend|Ordovician|Cambrian|Includes: Warrak Formation, Concongella Gritstone. Saint is St in text.||||||
23952|Saint Arnaud Group|60456|5|Briefly described|Map Legend|Cambrian|Cambrian|Units do not appear on this map.||||||
23952|Saint Arnaud Group|60457|5|Briefly described|Map Legend|Ordovician|Cambrian|Includes: Warrak Formation, Concongella Gritstone.||||||
23952|Saint Arnaud Group|60458|5|Briefly described|Map Legend|Ordovician|Cambrian|Includes: Warrak Formation, Concongella Gritstone.||||||
23952|Saint Arnaud Group|60459|5|Briefly described|Map Legend|Ordovician|Cambrian|Includes: Warrak Formation.||||||
23952|Saint Arnaud Group|60461|5|Briefly described|Map legend|Cambrian|Cambrian|Includes the Pyrenees and Beaufort Formations.  Overlain by the Castlemaine Group.||||||
23952|Saint Arnaud Group|60462|5|Briefly described|Map Legend|Cambrian|Cambrian|Marine turbiditic interbedded siltstone and mudstone with minor sandstone; mudstone is thin bedded, pyritic and rich in carbonaceous matter; mostly highly deformed and contact metamorphosed.||||||01-JUL-13
23952|Saint Arnaud Group|60491|4|Described|p17|Ordovician|Cambrian|Includes the Beaufort and Pyrenees formations. Contains Delamerian aged zircons. Consists of a sequence of unfossiliferous interbedded sandstones and mudstones.||||||
23952|Saint Arnaud Group|60492|5|Briefly described|Map Legend|Ordovician|Cambrian|Includes: Pyrenees Formation, Beaufort Formation||||||
23952|Saint Arnaud Group|60493|5|Briefly described|Map Legend|Ordovician|Cambrian|Includes Beaufort Formation and Pyrenees Formation. Saint is St in legend.||||||
23952|Saint Arnaud Group|60544|5|Briefly described|Map legend|Ordovician|Cambrian|In the Stawell Zone.||||||23-DEC-09
23952|Saint Arnaud Group|60581|5|Briefly described|Map Legend|Cambrian|Cambrian|Includes: Beaufort Formation and Pyrenees Formation.||||||
23952|Saint Arnaud Group|60582|5|Briefly described|Map Legend|Cambrian|Cambrian|Includes: Beaufort Formation and Pyrenees Formation.||||||
23952|Saint Arnaud Group|60583|5|Briefly described|Map Legend|Cambrian|Cambrian|Includes: Beaufort Formation and Pyrenees Formation.||||||
23952|Saint Arnaud Group|60584|5|Briefly described|Map Legend|Cambrian|Cambrian|Includes: Beaufort Formation and Pyrenees Formation.||||||
23952|Saint Arnaud Group|60585|5|Briefly described|p4|Cambrian|Cambrian|Geological Province: Stawell Zone, Lachlan Fold Belt||||||
23952|Saint Arnaud Group|61183|5|Briefly described|p21, p119|Late Ordovician|Late Cambrian|Chevron-folded and cleaved turbidites. Geological Province: Stawell Zone/Lachlan Fold Belt. Saint is St in places.||||||
23952|Saint Arnaud Group|61187|5|Briefly described|p3, p4, p5 Fig.3, p82, p83, p84 Fig.2.|Cambrian|Cambrian|Stawell Zone, Melbourne Terrane. Weakly magnetic; most trends strike NNW. Susceptibility measures given. Tightly folded, cleaved and faulted.|||||Thick, distal deep quartz-mica turbidites.|
23952|Saint Arnaud Group|61410|5|Briefly described|p7 Fig.2, p8 |Silurian|Ordovician|Unfossiliferous.|||||Siltstone and sandstone.|
23952|Saint Arnaud Group|61749|5|Briefly described|p11|||Includes chevron folded and cleaved turbidites.||||||21-JAN-10
23952|Saint Arnaud Group|61750|5|Briefly described|p19|Early Ordovician|Cambrian|Saint is St. in text.||||||
23952|Saint Arnaud Group|61752|5|Briefly described|p3 Fig. 1|Silurian|Ordovician|Of the Castlemaine Supergroup. Saint may be St in text.||||||07-FEB-11
23952|Saint Arnaud Group|62099|5|Briefly described|p331|Cambrian|Cambrian|Includes the Warrak, Beaufort and Pyrenees Formations. Unfossiliferous turbidites. Overlies the Magdala Volcanics. Max. thickness: 6.5Km. In the Stawell Zone of the Lachlan Orogen. Saint is St in text. ||||||
23952|Saint Arnaud Group|62754|5|Briefly described|p863|||Comprises Warrak, Beaufort and Pyrenees Formations. Includes mud-rich packages and sandstone. Consists of upright folds that have been faulted. Geological Province: Stawell Zone.  Saint is St in text.||||||
23952|Saint Arnaud Group|62755|5|Briefly described|p876 Fig.1|Cambrian|Cambrian|Sandstone, siltstone. See also p885 Fig. 8. Saint is St. in text.||||||23-JAN-07
23952|Saint Arnaud Group|64312|6|Mentioned|p442, p443 Fig. 5|||||||||
23952|Saint Arnaud Group|64314|5|Briefly described|p493, p495 Fig. 2a|Cambrian|Cambrian|Includes turbidites. Saint is St in text.||||||21-OCT-08
23952|Saint Arnaud Group|64616|6|Mentioned|p343 Fig.23|||||||||
23952|Saint Arnaud Group|65665|6|Mentioned|p1160 Fig.14|||||||||
23952|Saint Arnaud Group|65715|6|Mentioned|p26 Fig.1b|||||||||
23952|Saint Arnaud Group|65974|6|Mentioned|p4|Cambrian|Cambrian|Written as St Arnaud Group.|||||Comprises a folded and faulted turbidite sequence.|
23952|Saint Arnaud Group|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Includes Warrak Formation, Beaufort Formation, Pyrenees Formation, Albion Formation and Leviathan Formation. Called St Arnaud Beds by VandenBerg and Wilkinson (1982)||||||
23952|Saint Arnaud Group|66012|4|Described|p4-6, p8, p10 Tb.1, p11-12, p15, p26|Ordovician|Cambrian|Includes Warrak Formation and Pyrenees Formation. Deep-marine quartz-rich turbidite succession. Called Saint Arnaud Beds by VandenBerg and Wilkinson (1982). Intruded by Devonian granites of the Beckworth Suite| | | | | |13-JUN-13
23952|Saint Arnaud Group|66182|6|Mentioned|p323 Fig.5|Cambrian|Cambrian|Turbidites.||||||11-MAY-12
23952|Saint Arnaud Group|66769|5|Briefly described|117-118, 128, fig 9, 130, 133, 156|Late Cambrian|Late Cambrian|Stawell Zone. Appears throughout as St Arnaud Group. Thick package of metasedimentary siliciclastic turbidites. Along the Moyston Fault, is interbedded with Cambrian volcanics to form the Moornambool Metamorphic Complex.||||||17-SEP-14
23952|Saint Arnaud Group|67847|6|Mentioned|p10 fig 2.3, p14 fig 2.9, p99|Ordovician|Ordovician|Micas in this unit record evidence of Delamerian deformation. ||||||
23952|Saint Arnaud Group|68116|5|Briefly described|Appendix, Map 15.|Late Cambrian|Late Cambrian||||||Sandstone, siltstone, biotite schist; sandstone quartzose to feldspathic; deep marine turbidite deposits.|
23952|Saint Arnaud Group|68189|6|Mentioned|p3, p14-20, p25 Fig.13, p33|Cambrian|Cambrian|Spelt as St. Arnaud Group in text. Turbidite fan deposit. Contains pyrrhotite and is therefore generally magnetic.||||||
23952|Saint Arnaud Group|68194|4|Described|p6, p9, p20-21, p35-37, p40, p43 Fig.42|Cambrian|Cambrian|See also p44, p57, p75, p78-80, p95. Cayley and McDonald (1995). Formerly Saint Arnaud Beds (VandenBerg and Wilkinson, 1982). Forms bedrock across most of Stawell Zone, and prominent ridges trending NNW. Western edge of Lachlan Fold Belt. Hosts the Kingston gold deposit. Regolith and remote sensing profiles described. Basement to Department of Natural Resources and Environment boreholes, details of which are given.|||Includes Warrak, Beaufort and Pyrenees Formations.|Conformably overlies Moornambool Metamorphic Complex.|Turbidites. Includes auriferous mesothermal quartz veins and brecciated metasediments.|
23952|Saint Arnaud Group|68823|6|Mentioned|p401|Late Cambrian|Late Cambrian|Saint written as St in text. Outcrops in Stawell Zone. Similar to Warratta Group.||||||
23952|Saint Arnaud Group|70718|5|Briefly described|p37-38|Ordovician|Late Cambrian|Deposited in a deep oceanic setting on a turbidite fan.|||||Quartz-rich sandstone and mudstone turbidites.|02-JUN-19
23952|Saint Arnaud Group|71419|6|Mentioned|p20 Fig. 21|||||||Overlain unconformably by Sandringham Sandstone at Illabrook road cut.||02-FEB-18
23952|Saint Arnaud Group|71593|4|Described|p8, p12, p19, p35, p102|||Stawell Zone. Regarded as a time-equivalent to the Glenthompson Sandstone. See also p133, p166, p169, p180, p195.||||Overlies the Magdala Basalt.|Thick, unfossiliferous, turbidite sequences of sandstone and mudstone deposited in a deep marine environment.|
23952|Saint Arnaud Group|72445|6|Mentioned|App.7 p6 Fig.3.|Cambrian|Cambrian|Spelt 'St Arnaud Group' in geological map p6 Fig.3. Shown only on the geological map covering the Stavely Project area (from Geology of Victoria 2003: 21).||||||
23952|Saint Arnaud Group|73059|5|Briefly described|p1060-1061, 1064|Late Cambrian|Late Cambrian|Stawell Zone, Lachlan Fold Belt, western Victoria. Detrital zircon age plots in the range 600-550 Ma.|||Leviathan, Albion Formations.|||
23952|Saint Arnaud Group|73118|5|Briefly described|p7-8, 14, 61, 64|Ordovician|Cambrian|Stawell Zone, Lachlan Fold Belt, Western Victoria. Deformed no earlier than 450 Ma. Drill core summary logs.||||Is overlain by Geera Clay or Olney Formation.|Largely unfossiliferous marine quartz-mica turbidites and black shales deposited on ocean floor tholeiitic basalt and then metamorphosed (mostly to low greenschist facies).|
23952|Saint Arnaud Group|73177|5|Briefly described|p1097-1098, 1112-1113, 1114, 1115-1118|Late Cambrian|Late Cambrian|Stawell Zone, western Lachlan Orogen. Has strong similarities to the Warratta Group. Deformed by the latest stages of the Delamerian Orogeny. Appears as St Arnaud Gp in Fig.16.|500-490 Ma (MDA: Squire et al., 2006).|||Probable equivalent to Warratta Group.|Turbiditic interbedded mudstone, siltstone and sandstone (the latter two yellow and grey in outcrop); dark carbonaceous pyritic mudstone.|
23952|Saint Arnaud Group|73264|5|Briefly described|p1388, p1389 Fig.11|Late Cambrian|Late Cambrian|Stawell Zone. 900-1200 Ma zircon population, and 588, 513 Ma zircon peaks. Written as St Arnaud Group in text.|500-490 Ma||||Quartz-rich sandstone.|
23952|Saint Arnaud Group|73496|5|Briefly described|Map legend|Cambrian|Cambrian||||Pyrenees Formation, Warrak Formation, Beaufort Formation||Sandstone with lesser siltstone and mudstone; deep marine turbidite deposits.|
23952|Saint Arnaud Group|73497|5|Briefly described|Map legend|Cambrian|Cambrian|Marine.|||Pyrenees Formation, Warrak Formation, Beaufort Formation|Overlies Goldie Chert|Sandstone, with lesser siltstone and mudstone, turbidite deposits: broadly corresponds with weakly magnetic parts of the Pyrenees Formation but includes parts of the Warrak and Beaufort formations; magnetic, responses typically 1 to 10 nT.|
23952|Saint Arnaud Group|73505|5|Briefly described|p2, p5-7, p14, p28, p32|Cambrian|Cambrian|||||Overlies Dja Dja Wrung Supergroup||
23952|Saint Arnaud Group|73576|6|Mentioned|p805 Tb.1, p812 Fig.8, p813|||Written as St Arnaud.||||||
23952|Saint Arnaud Group|75072|5|Briefly described|p232, 237|Late Cambrian|Late Cambrian|Stawell Zone, Central Victoria. Zircon age distribution.|||Leviathan, Albion Formations.||Metaturbidites.|
16525|Saint Clair Formation|31852|6|Mentioned|p720|||L.Silurian||||||
16525|Saint Clair Formation|32074|6|Mentioned|Table 1|||See also p180.||||||03-OCT-07
16525|Saint Clair Formation|32285|6|Mentioned|Fig. 4|||||||||
16525|Saint Clair Formation|33601|6|Mentioned|p3|||Refs Moore 1965.||||||03-OCT-07
16525|Saint Clair Formation|37727|6|Mentioned|p70|||||||||
16525|Saint Clair Formation|70933|14|Not recorded|Table 1|||Generalised east west section Silurian and Devonian,Victoria refers to Talent 1965.||||||
37601|Saint Elmo Granodiorite|23309|5|Briefly described|p335,337.|Ordovician|Ordovician|G422, I-Type.  Supersedes Wando Vale and Deep Creek Granodiorites.  Age 482+/-9Ma, 476+/-6Ma.||||||
37601|Saint Elmo Granodiorite|50154|2|Defined|p75, p79, p248 App.5|Ordovician|Cambrian|Corresponds to part of Wells (1956) 'Wando Granodiorite'. Previously referred to as 'Deep Creek Granodiorite' by Anderson (1990) but this name has already been used in Victoria. Age: 482 +/- 9 Ma & 476 +/- 6 Ma (K/Ar). Saint is St. in text.||||||15-SEP-04
37601|Saint Elmo Granodiorite|50156|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite. Saint is St in map legend.||||||20-AUG-04
37601|Saint Elmo Granodiorite|50157|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite. Saint is St in map legend.||||||20-AUG-04
37601|Saint Elmo Granodiorite|50158|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite. Saint is St in map legend.||||||20-AUG-04
37601|Saint Elmo Granodiorite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite. Saint is St in map legend.||||||20-AUG-04
37601|Saint Elmo Granodiorite|50160|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite. Saint is St in map legend.||||||20-AUG-04
37601|Saint Elmo Granodiorite|50161|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite. Saint is St in map legend.||||||20-AUG-04
37601|Saint Elmo Granodiorite|50162|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite. Saint is St in map legend.||||||20-AUG-04
37601|Saint Elmo Granodiorite|50163|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite. Saint is St in map legend.||||||20-AUG-04
37601|Saint Elmo Granodiorite|50164|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Biotite-muscovite granite. Biotite granodiorite; I-type. Saint is St in map legend.||||||
37601|Saint Elmo Granodiorite|66002|6|Mentioned|p8 Tb.5|||G422. Defined by Morand et al. 2003.||||||
37601|Saint Elmo Granodiorite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Biotite granodiorite: massive, light grey, medium grained, equigranular; accessory magnetite; rare small biotite-rich enclaves; weakly magnetic.|
16542|Saint Kilda Formation|23482|5|Briefly described|p9|Holocene|Holocene|Saint is St. in text.||||||
16542|Saint Kilda Formation|23489|5|Briefly described|p43 Table 1|Holocene|Holocene|Saint is St. in text.||||||
16542|Saint Kilda Formation|23719|4|Described|p32|Holocene|Holocene|Saint is St. in text. See also page 30 table 9. Overlain by Semaphore Sand. Underlain by Moornaba Sand. Geological Province: Gawler Craton [?unlikely].||||||04-NOV-10
16542|Saint Kilda Formation|23731|6|Mentioned|p23, p29|Holocene|Holocene|Saint is St. in text.||||||
16542|Saint Kilda Formation|23818|4|Described|p212 Fig.108, p224|Recent|Recent|Geological Province: Otway Basin. Saint is spelt St. in text. Overlying units: Fulham Sand and Semaphore Sand. Underlying unit: Pooraka Formation. Age: 1000-4000 years B.P.||||||
16542|Saint Kilda Formation|29697|6|Mentioned|Table 7|||||||||
16542|Saint Kilda Formation|30080|6|Mentioned|p2|||||||||
16542|Saint Kilda Formation|30752|6|Mentioned|Table 1|||||||||
16542|Saint Kilda Formation|30753|6|Mentioned|p15|||Recent||||||
16542|Saint Kilda Formation|30754|5|Briefly described|p22|||Stratigraphic table. Sections P28,36||||||
16542|Saint Kilda Formation|30756|6|Mentioned|p2|||||||||
16542|Saint Kilda Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
16542|Saint Kilda Formation|30922|6|Mentioned|Map legend|Holocene|Holocene|||||||
16542|Saint Kilda Formation|31655|6|Mentioned|Table 1|||Geology & hydrology||||||
16542|Saint Kilda Formation|31850|4|Described|p40|||||||||
16542|Saint Kilda Formation|31921|5|Briefly described|p6|||||||||
16542|Saint Kilda Formation|32438|6|Mentioned|p41|||||||||
16542|Saint Kilda Formation|33054|6|Mentioned|p53|||See also Fig.1||||||
16542|Saint Kilda Formation|33422|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
16542|Saint Kilda Formation|33423|6|Mentioned|p15|||Strat.||||||
16542|Saint Kilda Formation|34180|5|Briefly described|p224|||Recent. See P212||||||
16542|Saint Kilda Formation|34181|4|Described|p47|||Recent||||||
16542|Saint Kilda Formation|34295|6|Mentioned|p42|||Pleistocene. Fauna||||||
16542|Saint Kilda Formation|34536|6|Mentioned|Map legend|Recent|Recent|||||||
16542|Saint Kilda Formation|35028|6|Mentioned|p339|||||||||
16542|Saint Kilda Formation|35097|6|Mentioned|p27|||||||||
16542|Saint Kilda Formation|35159|5|Briefly described|p12|||See also Fig.2.||||||
16542|Saint Kilda Formation|35673|6|Mentioned|Fig.1|||Location plan, Para Hills quartzite quarry.||||||
16542|Saint Kilda Formation|35677|6|Mentioned|p54|||||||||
16542|Saint Kilda Formation|35772|6|Mentioned|Table 1|||||||||
16542|Saint Kilda Formation|36621|6|Mentioned|Fig.1|||||||||
16542|Saint Kilda Formation|36626|6|Mentioned|Fig.1|||||||||
16542|Saint Kilda Formation|36834|6|Mentioned|Fig.1|||||||||
16542|Saint Kilda Formation|36835|6|Mentioned|Fig.1|||||||||
16542|Saint Kilda Formation|36894|6|Mentioned|Fig.2|||||||||
16542|Saint Kilda Formation|37853|6|Mentioned|Fig.1|||||||||
16542|Saint Kilda Formation|38068|5|Briefly described|p79|||See also Fig.8.||||||
16542|Saint Kilda Formation|38107|6|Mentioned|Fig.2|||||||||
16542|Saint Kilda Formation|38699|6|Mentioned|p30|||||||||
16542|Saint Kilda Formation|38700|6|Mentioned|p42|||||||||
16542|Saint Kilda Formation|39349|6|Mentioned|Map legend|Holocene|Holocene|||||||
16542|Saint Kilda Formation|39351|6|Mentioned|Map legend|late Holocene|late Holocene|||||||
16542|Saint Kilda Formation|39835|4|Described|p281|||||||||
16542|Saint Kilda Formation|40003|5|Briefly described|Table 11|||||||||
16542|Saint Kilda Formation|40149|1|Redefined|p121|Holocene|Holocene|||||||
16542|Saint Kilda Formation|40219|6|Mentioned|p2|||||||||
16542|Saint Kilda Formation|40442|6|Mentioned|p38|||||||||
16542|Saint Kilda Formation|40448|6|Mentioned|p43|||||||||
16542|Saint Kilda Formation|40502|5|Briefly described|p83|||||||||
16542|Saint Kilda Formation|40556|6|Mentioned|p66|||||||||
16542|Saint Kilda Formation|40643|6|Mentioned|p149|||||||||
16542|Saint Kilda Formation|40941|6|Mentioned|Map legend|Holocene|Holocene|||||||
16542|Saint Kilda Formation|40942|4|Described|p23|||||||||
16542|Saint Kilda Formation|40976|5|Briefly described|p280|||||||||
16542|Saint Kilda Formation|41078|6|Mentioned|p47|||||||||
16542|Saint Kilda Formation|41151|6|Mentioned|p14|||||||||
16542|Saint Kilda Formation|41278|5|Briefly described|p110|||||||||
16542|Saint Kilda Formation|41292|6|Mentioned|Fig.1|||||||||
16542|Saint Kilda Formation|41362|5|Briefly described|p7|||||||||
16542|Saint Kilda Formation|41499|6|Mentioned|p70|||||||||
16542|Saint Kilda Formation|41506|6|Mentioned|p9|||||||||
16542|Saint Kilda Formation|41943|6|Mentioned|Fig.3 P73|||||||||
16542|Saint Kilda Formation|42498|5|Briefly described|Map legend|Holocene|Holocene|Actually spelt St Kilda Formation.||||||
16542|Saint Kilda Formation|42717|6|Mentioned|map legend|Holocene||Actually spelt St Kilda Formation||||||
16542|Saint Kilda Formation|42966|2|Defined|p286|Holocene||Actually spelt St Kilda Formation.||||||
16542|Saint Kilda Formation|43049|6|Mentioned|p28|||actually spelt St Kilda Formation||||||
16542|Saint Kilda Formation|43052|5|Briefly described|Table 2.1|||actually spelt St Kilda Formation||||||
16542|Saint Kilda Formation|43053|5|Briefly described|Map Legend|Holocene|Holocene|Spelt St Kilda Formation. Calcareous, fossiliferous sand and mud of intertidal flats, beaches and tidal marshes; organic, gypseous clay of supratidal flats.||||||25-MAY-05
16542|Saint Kilda Formation|43073|6|Mentioned|p17|||actually spelt St Kilda Formation||||||
16542|Saint Kilda Formation|43258|5|Briefly described|Map Legend||Holocene|Spelt St.Kilda Formation.||||||
16542|Saint Kilda Formation|44133|5|Briefly described|p220 Fig. 11.2|Holocene|Pleistocene|||||||
16542|Saint Kilda Formation|49038|4|Described|Table 2|||||||||
16542|Saint Kilda Formation|60953|5|Briefly described|Map Legend|Holocene|Holocene|Calcareous, fossiliferous sand and mud of intertidal sand flats, beaches and tidal marshes; organic, gypseous clay of supratidal flats.||||||
16542|Saint Kilda Formation|60958|5|Briefly described|Map Legend|Holocene|Holocene|Undifferentiated holocene coastal marine sediment. <7000 yrs to present.||||||12-MAR-09
16542|Saint Kilda Formation|61070|5|Briefly described|Map Legend|Holocene|Holocene|Coastal sediments.||||||12-JAN-10
16542|Saint Kilda Formation|61108|5|Briefly described|map legend|Holocene|Holocene|Spelt St. on map legend. Calcareous, fossiliferous sand and mud of intertidal sand flats, beaches and tidal marshes; organic, gypseous clay of supratidal flats.||||||
16542|Saint Kilda Formation|61121|5|Briefly described|Map legend|Holocene|Holocene|Comprises three members and undifferentiated Holocene coastal marine sediment. members: Le Hunte, Semaphore Sand and Gantheaume Sand Members. Saint is St in text of legend.||||||07-JUN-05
16542|Saint Kilda Formation|62893|4|Described|Map Legend, p25|Holocene|Holocene|Reflects an intertidal setting. Facies equivalent of Semaphore Sand and Yamba Formation [not necessarily a stratigraphic equivalent].|ca 0.0066 Ma||||Shelly mud and sand, and stranded beach sand.|
16542|Saint Kilda Formation|63124|6|Mentioned|p93|||Geological Province: Gambier Basin. Saint is St in text.||||||
16542|Saint Kilda Formation|64282|5|Briefly described|Map legend|Holocene|Holocene|Includes Gantheaume and Semaphore Sand Members, and le Hunte Member, plus undifferentiated coastal marine sediment.  Age <7000years to present. Saint is St in legend.||||||24-JUL-08
16542|Saint Kilda Formation|65901|6|Mentioned|p177|Holocene|Holocene|Interfingers with Waldeila Formation. Marine.||||||08-MAR-12
16542|Saint Kilda Formation|68131|6|Mentioned|p12, p31|Holocene|Holocene|SW Yorke Peninsula.||||||
16542|Saint Kilda Formation|68811|5|Briefly described|p85, p86|||Deposited in an estuarine setting. Hosts good quality water that is recharged periodically by rainwater. |||Includes the Semaphore Sands. ||Muds and silts. |
16542|Saint Kilda Formation|69048|5|Briefly described|p2|Cenozoic|Cenozoic|Southern Eyre Peninsula.|||Semaphore Sand Member.|||
16542|Saint Kilda Formation|69666|6|Mentioned|p25, p27|Cenozoic|Cenozoic|||||||
16542|Saint Kilda Formation|70334|5|Briefly described|p3,61-62,65,70-71,73,90-91,93|Holocene|Holocene|Of Spencer Gulf area. Peritidal sediments. Part of a prograding cool water carbonate platform extending along the southern margin of Australia (Gostin et al., 1984a, Gostin et al., 1988).||||Disconformably overlies the Lowly Point Formation and the Mambray Formation.|Subtidal seagrass banks, shallow channels and mega-ripple fields, intertidal sand flats, mangrove-algal and halophyte-algal marshes, supratidal sand flats, sabkhas, stranded beach ridges and coastal dunes.|14-OCT-19
16542|Saint Kilda Formation|73103|5|Briefly described|Map legend.|Holocene|Holocene||||||Undifferentiated Holocene coastal marine sediment.|
16542|Saint Kilda Formation|73107|5|Briefly described|Map legend.|Holocene|Holocene|Appears on the map as ST KILDA FORMATION.|<7000 yrs to present.||||Undifferentiated Holocene coastal marine sediment.|
16542|Saint Kilda Formation|73110|5|Briefly described|Map legend.|Holocene|Holocene||||||Undifferentiated Holocene coastal marine sediment.|
16542|Saint Kilda Formation|73188|6|Mentioned|p320|Holocene|Holocene|[Written as St Kilda Formation]. St Vincent Basin.|||Semaphore Sand Member||Muddy and sandy coastal sediments.|
16542|Saint Kilda Formation|73236|5|Briefly described|p36, p38, p44|Holocene|Holocene|Coastal sediments; beach and dune sands. Represents shoreline deposits of the Holocene transgression in South Australia.|||Semaphore Sand Member|||
16542|Saint Kilda Formation|73302|6|Mentioned|p34|Holocene|Holocene|||||||
37778|Saint Kilda Granodiorite|23309|6|Mentioned|p443 Appendix 1|||G265, S-Type. Supersedes Saint Kilda Granite.||||||
16554|Saint Patricks Creek Granite|22968|4|Described|P213, P132, Table7||Early Devonian|Age of unit is 402+/-12 Ma, parent is Mount Elizabeth Caldera Complex||||||
16554|Saint Patricks Creek Granite|23021|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is Mount Elizabeth Caldera Complex.||||||
16554|Saint Patricks Creek Granite|23028|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is Mount Elizabeth Caldera Complex.||||||
16554|Saint Patricks Creek Granite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Mount Elizabeth Caldera Compex.||||||
16554|Saint Patricks Creek Granite|23309|5|Briefly described|p14, 123, 126, 134, 165, 343, 442|||GSV code G133.||||||04-NOV-14
16554|Saint Patricks Creek Granite|23938|5|Briefly described|p71 Fig. 25|Early Devonian|Early Devonian|Saint is St. and Creek is Ck. in text of figure. See also p73 Fig. 26.||||||25-SEP-08
16554|Saint Patricks Creek Granite|24551|5|Briefly described|p148|Devonian|Devonian|||||||
16554|Saint Patricks Creek Granite|42726|5|Briefly described|map legend|Early Devonian||580. Actually spelt St Patricks Creek Granite.||||||
16554|Saint Patricks Creek Granite|43284|5|Briefly described|Map Legend||Early Devonian|||||||
16554|Saint Patricks Creek Granite|43312|5|Briefly described|Map Legend||Wenlock|G133. Biotite granite, medium to fine grained, pink, I-Type.||||||26-OCT-04
16554|Saint Patricks Creek Granite|43313|5|Briefly described|Map Legend||Wenlock|||||||
16554|Saint Patricks Creek Granite|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|I-type.||||||
16554|Saint Patricks Creek Granite|60542|5|Briefly described|p96, p19 Fig. 3|||Forms the main ring dyke around the Mount Elizabeth Caldera Complex west of ORBOST.||||||
16554|Saint Patricks Creek Granite|68116|5|Briefly described|Appendix, Maps 35, 44.|Early Devonian|Early Devonian||||||Biotite granite: pale pink; medium to fine-grained.|
16557|Sale Group|23230|5|Briefly described|Table4-1p40, 42||Pliocene|||||||
16557|Sale Group|23938|6|Mentioned|p71 Fig. 25|||||||||
16557|Sale Group|24053|4|Described|p38|Quaternary|Late Pliocene|Geological Basin: Gippsland Basin.||||||
16557|Sale Group|24551|5|Briefly described|p327 Fig. 10.33|Pliocene|Pliocene|Maximum thickness: 200m.||||||
16557|Sale Group|29355|6|Mentioned|p179|||||||||
16557|Sale Group|31352|4|Described|p133|||See also P134, Fig. 3. Miocene - Pliocene.||||||
16557|Sale Group|32679|6|Mentioned|p94|||Strat. diagram||||||
16557|Sale Group|33603|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
16557|Sale Group|34843|4|Described|p10|||||||||
16557|Sale Group|35273|3|Fully described|p262|||||||||
16557|Sale Group|37330|6|Mentioned|p22|||||||||
16557|Sale Group|37530|6|Mentioned|p5|||||||||
16557|Sale Group|38929|5|Briefly described|p43|||||||||
16557|Sale Group|42184|6|Mentioned|Fig.2 P348|||||||||
16557|Sale Group|42827|4|Described|p336|||||||||
16557|Sale Group|43145|4|Described|p12|Pleistocene|Pliocene|||||||
16557|Sale Group|43284|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
16557|Sale Group|43312|5|Briefly described|Map Legend||Miocene|||||||
16557|Sale Group|43313|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
16557|Sale Group|44185|5|Briefly described|Map legend.|Pliocene|Miocene|||||||
16557|Sale Group|44187|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
16557|Sale Group|61155|5|Briefly described|p18|Late Pliocene|Late Pliocene|Includes Boisdale Formation and Haunted Hill Gravel. Overlies the Seaspray Group. Geological Province: Gippsland Basin (SE onshore). ||||||
16557|Sale Group|61302|5|Briefly described|p12|Late Pliocene|Late Pliocene|Non-marine sands and clays. Geological Province: Gippsland Basin.||||||
16557|Sale Group|61336|5|Briefly described|p(v) Fig. 5|Pliocene|Late Miocene|Includes Jemmys Point and Boisdale Formations. Geological Province: Gippsland Basin.||||||07-FEB-11
16557|Sale Group|64616|5|Briefly described|p147|Neogene|Neogene|A succession of continental clastics deposited in the northern onshore part of the Gippsland Basin. Includes Haunted Hills Gravel.||||||
16557|Sale Group|65718|6|Mentioned|p10 Fig 3.2|Pleistocene|Pliocene|||||||
16557|Sale Group|68116|5|Briefly described|Appendix, Maps 37, 46.|Pliocene|Miocene||||||Clastics and carbonate sediments: includes gravel, claystone, sandstone, siltstone; nonmarine to marginal marine.|
16557|Sale Group|69016|5|Briefly described|p89,91|Pleistocene|Late Miocene|Of the Gippsland Basin.|||Includes Haunted Hill Formation and Boisdale Formation.|||
16557|Sale Group|70028|6|Mentioned|p79|Pleistocene|Pliocene|Gippsland Basin.||||Unconformably overlies Seaspray Group.||
16557|Sale Group|75065|6|Mentioned|p151|Quaternary|Pliocene|Gippsland Basin.||||Unconformably overlies Yallourn and Balook Formations (Latrobe Valley Group).||
36797|Salt Creek Formation|23778|2|Defined|p666, 678|Late Eocene|Late Eocene|(new name). Of Demons Bluff Group. Overlying unit Anglesea Formation. Underlying unit Boonah Formation. Torquay Basin. Max. thickness: 25 m.||||||16-APR-18
36797|Salt Creek Formation|24551|6|Mentioned|p308, 311, 515|||Of the Demons Bluff Group.||||||27-SEP-06
36797|Salt Creek Formation|69297|6|Mentioned|p98|Priabonian|Priabonian|||Demons Bluff Group||Overlies the Boonah Formation. Overlain by the Anglesea Formation. |Siltstone. |
68482|San Remo Member|24551|5|Briefly described|p473 Fig. 15.4|||||||||
68482|San Remo Member|70378|6|Mentioned|p696 Fig.1|Aptian|Barremian|||Strzelecki Group.||||08-FEB-17
68482|San Remo Member|75065|5|Briefly described|p151, 156|Aptian|Aptian|Gippsland Basin; onshore.||Korumburra Subgroup.||Unconformably overlies Tyers River Subgroup.|Non-marine conglomerate.|
16592|Sandford Limestone|23768|6|Mentioned|p71|Longfordian|Longfordian|See also p85, p125.||||||10-MAR-05
16592|Sandford Limestone|30184|6|Mentioned|p173|||||||||
16592|Sandford Limestone|30905|6|Mentioned|p149|||||||||
16592|Sandford Limestone|41642|6|Mentioned|p218|||||||||
16592|Sandford Limestone|42371|6|Mentioned|p36|||||||||
16598|Sandhurst Group|24088|5|Briefly described|p352|||||||||
16598|Sandhurst Group|42683|5|Briefly described|map legend|||Variation on Sandhurst Beds?||||||12-JAN-10
16606|Sandpatch Point Granite|23309|6|Mentioned|p442 App1|||G29 - I-Type.||||||
16606|Sandpatch Point Granite|42726|5|Briefly described|map legend|||||||||
16606|Sandpatch Point Granite|68116|5|Briefly described|Appendix, Map 46.|Early Devonian|Early Devonian||||||Granite.|
80411|Sandringham Sandstone|71419|3|Fully described|p7-22|Pliocene|Miocene|New name (VandenBerg, 2016), after Sandringham Sands of Gill (1950); Gill's type section is retained for Sandringham Sandstone. Unit description significantly revised. Entirely paralic sediments unfossiliferous towards top.  Depositional environment and extent discussed but not fully determined. Min age (4.6 Ma) based on overlying basalts, but oldest are undated. This newly redescribed unit intended to replace Hanson Plain Sand, Moorabool Viaduct Sands, Baxter Sandstone, Marina Cove Sand, Black Rock Sandstone, Red Bluff Sandstone, Beaumaris Sandstone, Brighton Group.|Base 5.8+/-0.2 Ma (Sr/Sr ratios in molluscs).|||Overlies Gellibrand Marl, Calivil Formation, and (unconformably) the Saint Arnaud Group. Is overlain locally by Newer Volcanics Group.|Sandy silt, fine sandstone, sandy conglomerate to pebbly sandstone, clayey sand, clayey gravel, carbonaceous band including plant fossils; lag deposit including variable to highly-rounded pebbles; horizontal and swaley cross-lamination; burrows.|02-FEB-18
34859|Sapper Nose Rhyolite Member|22968|5|Briefly described|P85, P111||Silurian|||||||
34859|Sapper Nose Rhyolite Member|23021|5|Briefly described|Map legend|Ludlow|Ludlow|Parent is Thorkidaan Volcanics||||||
34859|Sapper Nose Rhyolite Member|23309|5|Briefly described|p92 Table 2.31|||||||||
34859|Sapper Nose Rhyolite Member|60503|5|Briefly described|p108, p15, p28 Fig. 9|Silurian|Silurian|Of the Thorkidaan Volcanics. Dominantly fine-grained, weakly porphyritic rhyolite lavas; aphanitic to moderately quartz-feldspar phyric with minor biotite; sericite.  Recognised purely on the basis of its high potassium response in the radiometric data.||||||05-SEP-05
34859|Sapper Nose Rhyolite Member|60504|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Thorkidaan Volcanics (Enano Group). Rhyolite lava; high K response in radiometrics||||||20-OCT-04
34859|Sapper Nose Rhyolite Member|60505|5|Briefly described|Map legend|Ludlow|Ludlow|Of the Thorkidaan Volcanics (Enano Group). Rhyolite lava; high K response in radiometrics.||||||21-OCT-04
34859|Sapper Nose Rhyolite Member|60506|5|Briefly described|Map legend|Ludlow|Ludlow|Of the Thorkidaan Volcanics (Enano Group). Rhyolite lava; high K response in radiometrics.||||||21-OCT-04
34859|Sapper Nose Rhyolite Member|60507|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Thorkidaan Volcanics (Enano Group). Rhyolite lava; high K response in radiometrics.||||||21-OCT-04
30506|Sarah Allen Granodiorite|22878|4|Described|p84|||||||||06-OCT-04
30506|Sarah Allen Granodiorite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Biotite-minor hornblende granodiorite: pale grey, medium grained, massive; plagioclase rich||||||01-OCT-04
30506|Sarah Allen Granodiorite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Biotite-minor hornblende granodiorite: pale grey, medium grained, massive; plagioclase rich||||||01-OCT-04
30506|Sarah Allen Granodiorite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Biotite-minor hornblende granodiorite: Highly magnetic (400-420 nT) and moderately magnetic (~60 nT) in the centre. High K , low Th and U.||||||06-OCT-04
30506|Sarah Allen Granodiorite|23309|6|Mentioned|p422 App1|||G523 I-Type.||||||
30506|Sarah Allen Granodiorite|68116|5|Briefly described|Appendix, Map 37.|Early Devonian|Silurian||||||Biotite-minor hornblende granodiorite: pale grey, medium grained, massive; plagioclase-rich.|
16626|Sardine Conglomerate|22876|5|Briefly described|p17|Late Silurian|Late Silurian|||||||
16626|Sardine Conglomerate|22877|5|Briefly described|map|Silurian|Silurian|||||||
16626|Sardine Conglomerate|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
16626|Sardine Conglomerate|23309|5|Briefly described|p89-97,  Table 2.34|Ludlow|Late Silurian|||||||
16626|Sardine Conglomerate|23615|5|Briefly described|p82, p21|Ludlow|Ludlow|Overlain by Wibenduck Limestone.  Name used interchangably with Sardine Creek Conglomerate throughout publication. Age: in ~425-410Ma range i.e. Middle to Late Silurian.||||||16-AUG-18
16626|Sardine Conglomerate|23938|5|Briefly described|p31-32 Fig. 12|Late Silurian|Late Silurian|Marine: conglomerate, sandstone, siltstone. See also p139 Tb. 1 Appendix.||||||
16626|Sardine Conglomerate|24004|5|Briefly described|p275 Fig.2|Silurian|Silurian|||||||
16626|Sardine Conglomerate|24551|4|Described|p138, p120|Silurian|Silurian|||||||
16626|Sardine Conglomerate|41585|4|Described|p131|||||||||
16626|Sardine Conglomerate|42627|5|Briefly described|Map legend|Ludlow||||||||
16626|Sardine Conglomerate|42635|6|Mentioned|p24.|||||||||
16626|Sardine Conglomerate|42647|2|Defined|p27|Silurian||Supersedes Sardine beds, in part.||||||
16626|Sardine Conglomerate|42827|4|Described|p131|||see also Table 4.1||||||
16626|Sardine Conglomerate|43206|5|Briefly described|map legend||Wenlock|||||||
16626|Sardine Conglomerate|43228|5|Briefly described|p9||Late Silurian|||||||
16626|Sardine Conglomerate|44185|5|Briefly described|Map legend.|Late Silurian|Late Silurian||||||Marine: conglomerate, sandstone, limestone.|
16626|Sardine Conglomerate|60503|5|Briefly described|p28 Fig. 9|||Of the Wombat Creek Group?||||||
16626|Sardine Conglomerate|60541|5|Briefly described|p11 Fig. 2|Late Silurian|Late Silurian|||||||
16626|Sardine Conglomerate|60542|5|Briefly described|p11 Fig. 2|Late Silurian|Late Silurian|||||||
16626|Sardine Conglomerate|61181|6|Mentioned|p124|Silurian|Silurian|||||||
16626|Sardine Conglomerate|68116|5|Briefly described|Appendix, Map 36.|Pridoli|Llandovery||||||Pebble to cobble-conglomerate: massive; minor sandstone; matrix is a mixture of sand, small pebbles and silt; most clasts are micaceous sandstone; minor volcanigenic sandstone.|
16631|Sarsfield Granite|23309|5|Briefly described|p422 App1|Devonian|Devonian|Age: 371 +/- 11Ma.  Supersedes Clifton Creek Granite.||||||
16631|Sarsfield Granite|24551|6|Mentioned|p230|||See also Clifton Creek Granite||||||
16631|Sarsfield Granite|42726|5|Briefly described|map legend|Middle Devonian||583.||||||
16631|Sarsfield Granite|44185|5|Briefly described|Map legend.|Late Devonian|Late Devonian|S-type. G131.||||||04-NOV-14
16631|Sarsfield Granite|68116|5|Briefly described|Appendix, Map 44.|Late Devonian|Late Devonian||||||Biotite-muscovite leucogranite: fine to medium grained, cream-white; S-type.|
32562|Saturday Morning Tonalite|22968|5|Briefly described|P75, P218|Early Devonian|Late Silurian|New name, type locality location given on P218||||||
32562|Saturday Morning Tonalite|23020|5|Briefly described|Map legend||Late Silurian|||||||
32562|Saturday Morning Tonalite|23030|5|Briefly described|Map legend|Late Silurian|Late Silurian|||||||
32562|Saturday Morning Tonalite|23309|6|Mentioned|p442 App1|||G528.||||||
32562|Saturday Morning Tonalite|61161|5|Briefly described|p94-95, p76-77 Fig 6.1|Early Devonian|Late Silurian|Of Rileys Creek Suite. Porphyritic, unfoliated biotite-hornblende tonalite; tabular hornblende phenocrysts in fine-grained matrix; plagioclase, quartz, biotite, hornblende, minor K-feldspar. Type locality p94. GSV map code: G528.||||||
32562|Saturday Morning Tonalite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende tonalite: fine-grained; porphyritic with tabular hornblende phenocrysts; I-type intrusion. GSV map code: G528.||||||
32562|Saturday Morning Tonalite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende tonalite: fine-grained; porphyritic with tabular hornblende phenocrysts; I-type intrusion. GSV map code: G528.||||||07-FEB-11
32562|Saturday Morning Tonalite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende tonalite: fine-grained; porphyritic with tabular hornblende phenocrysts; I-type intrusion. GSV map code: G528.||||||
32562|Saturday Morning Tonalite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende tonalite: fine-grained; porphyritic with tabular hornblende phenocrysts; I-type intrusion. GSV map code: G528.||||||
32562|Saturday Morning Tonalite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Rileys Creek Suite. Biotite-hornblende tonalite: insufficient gravity data to determine response; highly magnetic (200 to 410 nT, k = 800 x10^-6 cgs); low to moderate K, moderate Th, U, and total radioelements. GSV map code: G528.||||||
32562|Saturday Morning Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Biotite-hornblende tonalite: fine-grained; porphyritic with tabular hornblende phenocrysts.|
83256|Sawpit Formation|73356|2|Defined|p. v-1, p4-29|Valanginian|Berriasian|Otway Basin, western and central Victoria. New unit; named after Sawpit Swamp northeast of Penola. Type section is between 1402 and 2465.8 m in Sawpit-1 where it consists of three shale units separated by two sandstone sequences. Reaches a maximum thickness of 1681.8 m in Jolly-1 ST1 in the Penola Trough. Includes stacked fluvial channels and fluvio-lacustrine shales; channel sands are not laterally extensive. Intersected in 19 wells across the Otway Basin; 8 in Victoria. Age constraint is from palynologic biostratigraphy; belongs to the latest Berriasian to Valanginian Upper Ruffordiaspora australiensis Spore-Pollen Subzone of Partridge (2006) and corresponds to the S1-P1 to S1-P4 chemostratigraphic packages (Forbes et al., 2020). Basal boundary is unconformable in many instances (cf. Warrong Trough) but is shown to be conformable in Sawpit-1 (Penola Trough). The basal portion of the type section is informally known as the C. australiensis shale of Lovibond et al. (1993) [p. 6-7, 12, 19]. Upper boundary is marked by an increase in volcanogenic lithics and feldspar. More mineralogically mature than the Pretty Hill Formation. Incorporates strata previously informally named Sawpit Sandstone, Sawpit Shale and variations thereon. [See article for description of geophysical character].||Crayfish Subgroup, Otway Group|McEachern Sandstone Member|Conformably overlain by Pretty Hill Formation. Conformably underlain by Casterton Formation.|Litharenite to sublitharenite sandstone with minor arkoses and subarkoses, and brown to grey shale with minor siltstone and sandstone interbeds.|
83256|Sawpit Formation|73386|4|Described|p4, p6, p8, Attachment A1|Valanginian|Berriasian|Otway Basin, western and central. Conformably overlies Casterton Formation in the western Otway Basin, and is unconformable in the central Otway Basin. Belongs to the latest Berriasian to Valanginian Upper Ruffordiaspora australiensis Spore-Pollen Subzone, and the S1-P1 to S1-P4 chemostratigraphic packages (Eid et al., 2021a). Newly designated type section defined between 1402 m and 2465.8 m in Sawpit-1 (Eid et al., 2021a).||Crayfish Subgroup|McEachern Member|Overlies Casterton Formation, McEachern Member, conformably underlies Pretty Hill Formation|Consists of a series of stacked fluvial channel sands, each with overlying fluvio-lacustrine shales. Includes basal unit of fluvial sandstones, quartz arenites and subarkoses, with thin interbeds of siltstone and shale.|
37595|Schofield Granite|23309|6|Mentioned|p422, App 1|||G413, S-Type. Supersedes Scholfield Adamellite.||||||
37595|Schofield Granite|50154|2|Defined|p93-94, p247 App.5|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex. Supersedes the Schofield Adamellite of Kemp & Gray (1999).||||||15-SEP-04
37595|Schofield Granite|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Muscovite-biotite granite; S-type||||||
37595|Schofield Granite|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite.||||||20-AUG-04
37595|Schofield Granite|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite.||||||20-AUG-04
37595|Schofield Granite|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite.||||||20-AUG-04
37595|Schofield Granite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite.||||||20-AUG-04
37595|Schofield Granite|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite.||||||20-AUG-04
37595|Schofield Granite|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite.||||||20-AUG-04
37595|Schofield Granite|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite.||||||20-AUG-04
37595|Schofield Granite|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex. Muscovite-biotite granite.||||||20-AUG-04
37595|Schofield Granite|66002|5|Briefly described|p8 Tb.5|||G413. Called Schofield Adamellite by Kemp and Gray (1999)||||||
37595|Schofield Granite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian|Non-magnetic. Schlieren, aligned biotite-muscovite clots and selvedges define foliation;|||||Muscovite-biotite granite: heterogeneous, foliated, light buff, medium to coarse grained, porphyritic with megacrysts of microcline; abundant schist and migmatite enclaves. Includes garnet pegmatite lenses, biotite- and plagioclase-rich horizons.|
22824|Scorpion Creek Sandstone|23309|4|Described|p112 Taable 2.40|||Of the Timbarra Subgroup.||||||
22824|Scorpion Creek Sandstone|23615|3|Fully described|p89, p25 Fig.7|Early Devonian|Early Devonian|Of Timbarra Subgroup.  Overlain by Gordon Creek Ignimbrite, underlain by Statham Ignimbrite.  Maximum thickness: 20m. Distinctive sequence of green, red and buff interbedded sandstone and siltstone.||||||
22824|Scorpion Creek Sandstone|24551|4|Described|p142|||Of the Timbarra Subgroup.||||||
22824|Scorpion Creek Sandstone|43206|5|Briefly described|map legend||Ludlow|Timbarra Subgroup||||||
22824|Scorpion Creek Sandstone|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Sandstone and siltstone, ash, conglomerate, pebbly sandstone.|
37777|Scotts Flat Granite|23309|6|Mentioned|p422 Appendix 1|||G324.||||||
37777|Scotts Flat Granite|60452|4|Described|p56|||Very weathered outcrop. Medium-grained. Minerals present are: quartz, kaolinite after feldspar, and muscovite. Intruded by Saint Arnaud Group.||||||21-OCT-04
37777|Scotts Flat Granite|60461|5|Briefly described|Map legend|Early Devonian|Early Devonian|Granite, medium-grained; highly weathered outcrops of quartz, kaolinite and muscovite.||||||
37777|Scotts Flat Granite|60462|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Granite: reduced; nonmagnetic.||||||
37777|Scotts Flat Granite|65715|6|Mentioned|p8 Tb.4|||G324. Of Edwards et al. (2001) p56.||||||
37596|Scrubby Flat Gabbro|23309|5|Briefly described|p68, 338|||G505. Supersedes Scrubby Flat Granite.  See also Scrubby Flat gabbro (informal). Of Kuark Metamorphic Complex.||||||
37596|Scrubby Flat Gabbro|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|Of the Arte River Gabbro Suite. Medium-coarse grained, pyroxene, hornblende gabbro and gabbronorite.||||||
37596|Scrubby Flat Gabbro|43315|5|Briefly described|Map Legend|Wenlock|Wenlock|Of the Arte River Gabbro Suite. Medium-coarse grained, pyroxene, hornblende gabbro and gabbronorite.||||||03-MAY-05
37596|Scrubby Flat Gabbro|60541|5|Briefly described|p82, p22|Early Silurian|Early Silurian|See also Scrubby Flat gabbro. Intrusive within the Kuark Metamorphic Complex. Large previously unmapped gabbro, poorly exposed. In type section it is very weathered, with closely spaced jointing promoting development of cubic and almond-shaped blocks.||||||
37596|Scrubby Flat Gabbro|68116|5|Briefly described|Appendix, Map 45.|Wenlock|Llandovery||||||Pyroxene-hornblende gabbro and gabbronorite: medium to coarse-grained; I-type.|
33130|Scrubby Junction Granodiorite|23309|5|Briefly described|p335|||G415 S-Type||||||
33130|Scrubby Junction Granodiorite|23319|4|Described|p408 Fig. 1,  p414|Ordovician|Cambrian|Medium- to coarse-grained and texturally heterogeneous. Interlayered with Schofield Adamellite. Intruded by Marn Mering Granodiorite in the east.||||||23-MAY-13
33130|Scrubby Junction Granodiorite|50154|2|Defined|p92, p246 App.5|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex. Crosscut by Marn Mering Granodiorite.||||||15-SEP-04
33130|Scrubby Junction Granodiorite|50155|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Biotite-muscovite granodiorite; S-type||||||
33130|Scrubby Junction Granodiorite|50156|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granodiorite.||||||20-AUG-04
33130|Scrubby Junction Granodiorite|50157|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granodiorite.||||||20-AUG-04
33130|Scrubby Junction Granodiorite|50158|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granodiorite.||||||20-AUG-04
33130|Scrubby Junction Granodiorite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granodiorite.||||||20-AUG-04
33130|Scrubby Junction Granodiorite|50160|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granodiorite.||||||20-AUG-04
33130|Scrubby Junction Granodiorite|50161|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granodiorite.||||||20-AUG-04
33130|Scrubby Junction Granodiorite|50162|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granodiorite.||||||20-AUG-04
33130|Scrubby Junction Granodiorite|50163|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-muscovite granodiorite.||||||20-AUG-04
33130|Scrubby Junction Granodiorite|66002|6|Mentioned|p8 Tb.5|||G415. Defined by Kemp and Gray 1999.||||||
33130|Scrubby Junction Granodiorite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Biotite-muscovite granodiorite: foliated, medium to coarse grained, porphyritic with microcline phenocrysts; common schlieric layering and nebulitic banding; common schist enclaves. Includes pegmatite and sheets of garnet leucogranite; non-magnetic.|
16699|Scutellina Limestone|42371|6|Mentioned|p35, p41|||||||||
16702|Seacombe Marl Member|24551|5|Briefly described|p327 Fig. 10.33|Miocene|Oligocene|||||||
16702|Seacombe Marl Member|35273|4|Described|p259|||||||||
16702|Seacombe Marl Member|42827|4|Described|p333|||of Lakes Entrance Formation||||||
16702|Seacombe Marl Member|65718|5|Briefly described|p10 Fig 3.2|Miocene|Oligocene|See also Seacombe Marl. Early Miocene minimum age.||Of the Lakes Entrance Formation.||||10-JAN-17
16702|Seacombe Marl Member|70076|5|Briefly described|Regional: Fig.3|Aquitanian|Chattian|||Lakes Entrance Formation.||Overlies Giffard Sandstone Member. Is overlain by Longford Limestone.||
16716|Sealers Cove Granite|23309|6|Mentioned|p443 App1|||G258 S-Type.||||||
16716|Sealers Cove Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
16716|Sealers Cove Granite|68116|5|Briefly described|Appendix, Map 57.|Middle Devonian|Middle Devonian||||||Cordierite-biotite granite: fine grained to porphyritic; S-type.|
16717|Seaspray Group|13323|5|Briefly described|p392, p394 Fig. 3|Recent|Early Oligocene|Includes Latrobe Valley, Angler, Albacore, Hapuku and Sale Subgroups. Geological Province: Gippsland Basin. See also p393 Fig. 2.||||||26-JUN-06
16717|Seaspray Group|13324|4|Described|p93, p94 Fig. 4, p99|Pleistocene|Oligocene|Gippsland Basin. Regional seal.|||Includes Lakes Entrance Formation, Gippsland Limestone.||(Offshore) consists of fine-grained calcareous mudstones, marls and fossiliferous limestones.|
16717|Seaspray Group|13332|5|Briefly described|p187 Fig.7|||Geological Province: Gippsland Basin||||||
16717|Seaspray Group|13350|5|Briefly described|p94||Oligocene|Comprises Lakes Entrance Formation and Gippsland Limestone. Marine deposits. Overlies the Latrobe Group. Geological Province: Gippsland Basin.  See also p100 Fig. 7.||||||
16717|Seaspray Group|22454|5|Briefly described|p3, fig. 4||Cenozoic|Gippland Basin. Overlies Latrobe Group.||||||19-NOV-08
16717|Seaspray Group|22663|6|Mentioned|V97 - G1 to G4 Fig.4|||||||||
16717|Seaspray Group|23230|5|Briefly described|p42, 44|Pliocene|Oligocene|||||||
16717|Seaspray Group|23264|6|Mentioned|p326|||||||||
16717|Seaspray Group|23309|6|Mentioned|p360|Miocene|Oligocene|||||||
16717|Seaspray Group|23625|4|Described|p54|Miocene|Miocene|Thickness: >2500m. Underlying unti: Latrobe Group. Geological Province: Gippsland Basin||||||25-SEP-08
16717|Seaspray Group|23792|5|Briefly described|p22||Oligocene|Marine carbonates. Geological Province: Gippsland Basin.||||||20-JUL-06
16717|Seaspray Group|23909|5|Briefly described|p295|Miocene|Oligocene|Geological Province: Gippsland Basin.||||||
16717|Seaspray Group|24002|5|Briefly described|p241 fig. 10|Miocene|Oligocene|Geological Province: Gippsland Basin||||||
16717|Seaspray Group|24053|4|Described|p37|Pliocene|Oligocene|Geological Basin: Gippsland Basin.||||||
16717|Seaspray Group|24090|5|Briefly described|p17||Eocene|Geological Province: Gippsland Basin. See also page 8 Fig.3.||||||
16717|Seaspray Group|24164|5|Briefly described|p15,20,27-29,34,37,39,41-44 and more|Quaternary|Oligocene|Open shallow marine, swamp. Muddy and carbonate-bearing. mid-Miocene channels. Included in Figs.8,12,17, Tb.2.|||Latrobe Valley Coal Measures, Lakes Entrance Formation, Gippsland Limestone|Interleaved with Latrobe Group|Marls and limestones|
16717|Seaspray Group|24202|5|Briefly described|p326|Recent|Oligocene|Geological Province: Gippsland Basin.||||||
16717|Seaspray Group|24211|5|Briefly described|p84|Pleistocene|Oligocene|Geological Province: Gippsland Basin.||||||
16717|Seaspray Group|24407|5|Briefly described|p13 Fig.2|Oligocene|Oligocene|Geological Province: Gippsland Basin||||||
16717|Seaspray Group|24468|5|Briefly described|p403|Holocene|Oligocene|Geological Province: Gippsland Basin||||||
16717|Seaspray Group|24495|5|Briefly described|p9|||Of Latrobe Group.  Geological Province: Gippsland Basin.||||||
16717|Seaspray Group|24551|5|Briefly described|p325,328, 477|Pliocene|Oligocene|||||||04-NOV-14
16717|Seaspray Group|24561|5|Briefly described|p44|||Geological Province: Gippsland Basin. Provides the regional seal to the hydrocarbon traps in the basin.||||||04-FEB-08
16717|Seaspray Group|29355|6|Mentioned|p179|||||||||
16717|Seaspray Group|30938|6|Mentioned|Map legend|Miocene|Miocene|||||||
16717|Seaspray Group|31202|5|Briefly described|p218|||First Late Eocene transgression of Gippsland Basin.||||||
16717|Seaspray Group|31352|4|Described|p133|eoc||See also p134,135,Fig.3. Eocene-Pleistocene.||||||20-JUL-06
16717|Seaspray Group|32162|5|Briefly described|p56|||Refers petroleum aspect||||||
16717|Seaspray Group|32679|4|Described|p94|||||||||
16717|Seaspray Group|33603|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
16717|Seaspray Group|34842|4|Described|p21|||||||||
16717|Seaspray Group|34843|6|Mentioned|p10|||||||||
16717|Seaspray Group|35013|4|Described|p396|||||||||
16717|Seaspray Group|35271|6|Mentioned|p67|||||||||
16717|Seaspray Group|35273|3|Fully described|p257|||||||||
16717|Seaspray Group|35285|6|Mentioned|p415|||||||||
16717|Seaspray Group|37330|6|Mentioned|p22|||||||||
16717|Seaspray Group|37530|6|Mentioned|p5|||||||||
16717|Seaspray Group|38928|6|Mentioned|Fig.4|||||||||
16717|Seaspray Group|38929|4|Described|p47|||||||||
16717|Seaspray Group|38931|6|Mentioned|p74|||Also mentioned Fig.5||||||
16717|Seaspray Group|39315|6|Mentioned|Fig.7|||||||||
16717|Seaspray Group|41193|5|Briefly described|p315|||||||||
16717|Seaspray Group|41282|6|Mentioned|p34|||||||||
16717|Seaspray Group|41318|6|Mentioned|Fig.1|||||||||
16717|Seaspray Group|41727|5|Briefly described|p433|||||||||
16717|Seaspray Group|41868|4|Described|p522|||||||||
16717|Seaspray Group|41999|6|Mentioned|p2|||||||||
16717|Seaspray Group|42075|5|Briefly described|Fig.15 P253|||||||||
16717|Seaspray Group|42184|6|Mentioned|p350|||||||||
16717|Seaspray Group|42649|6|Mentioned|p201|||||||||
16717|Seaspray Group|42827|4|Described|p331|||||||||
16717|Seaspray Group|42998|6|Mentioned|p61|||||||||
16717|Seaspray Group|43145|5|Briefly described|p11||Early Oligocene|||||||
16717|Seaspray Group|43312|5|Briefly described|Map Legend||Miocene|||||||
16717|Seaspray Group|43313|5|Briefly described|Map Legend||Miocene|||||||
16717|Seaspray Group|43314|5|Briefly described|Map Legend||Miocene|||||||
16717|Seaspray Group|43315|5|Briefly described|Map Legend||Miocene|Sand, calcareous, silty, sandy and silty limestone, moderately consolidated, ferruginised with patchy carbonate sediment; often richly fossiliferous.||||||03-MAY-05
16717|Seaspray Group|43667|6|Mentioned|Fig.3,p12||Miocene|||||||
16717|Seaspray Group|44185|5|Briefly described|Map legend.|Pliocene|Miocene|||||||
16717|Seaspray Group|44187|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
16717|Seaspray Group|60538|5|Briefly described|p475 Fig. 14, 480, 482 Fig. 21|Oligocene|Middle Eocene|Geological Province: Gippsland Basin. Includes: Gippsland Limestone, Lakes Entrance Formation, Gippsland Limestone Formation, Wuk Wuk Marl.||||||
16717|Seaspray Group|60541|5|Briefly described|p59-60|Early Pliocene|Oligocene|Limestones and marls; outcropping limestone is yellow and realtively soft with occasional hard bands of shelly fossils or well-preserved shells.||||||
16717|Seaspray Group|60542|5|Briefly described|p84|Tertiary|Tertiary|Includes Gippsland Limestone and Jemmys Point Formation. Limestones and marls - limestone is yellow and realtively soft, with occasional hard bands with shelly fossils or well preserved shells. ||||||
16717|Seaspray Group|61155|5|Briefly described|p18|Early Pliocene|Early Oligocene|Includes: Lakes Entrance Formation, Gippsland Limestone,Tambo River Formation and Jemmys Point Formation. Overlies Latrobe Group; underlies Sale Group. Geological Province: Gippsland Basin (onshore/offshore).||||||
16717|Seaspray Group|61212|5|Briefly described|p300, p301 Fig. 2|Holocene|Oligocene|Carbonates. Geological Province: Gippsland Basin.||||||
16717|Seaspray Group|61302|4|Described|p12|Early Miocene|Early Oligocene|Overlies the Latrobe Group. Geological Province: Gippsland Basin.||||||
16717|Seaspray Group|61328|5|Briefly described|p112 Fig. 3|Miocene|Oligocene|Overlies Latrobe or Golden Beach Groups. Geological Province: Gippsland Basin.||||||
16717|Seaspray Group|61336|5|Briefly described|p(iv) Fig. 4|||Includes Lakes Entrance Formation.  Marine deposits. Overlies Latrobe Group. Geological Province: Gippsland Basin. See als p(v) Fig. 5.||||||07-FEB-11
16717|Seaspray Group|61552|5|Briefly described|p583 Fig.2, p584, p586, p588 Fig.5. |Late Oligocene|Early Oligocene|These carbonate sediments comprise the regional seal to the top of the Latrobe play in the Gippsland basin.|||Includes Latrobe Valley Subgroup.||Fine-grained calcareous mudstones, marls, as well as richly fossiliferous limestones.|
16717|Seaspray Group|61607|6|Mentioned|p5 Fig. 2|Cenozoic|Oligocene|Geological Province: Gippsland Basin.||||||12-MAR-09
16717|Seaspray Group|61624|6|Mentioned|p465, p472|Tertiary|Tertiary|Geological Province: Gippsland Basin. Carbonates.||||||07-APR-09
16717|Seaspray Group|61846|5|Briefly described|p258|Neogene|Paleogene|Shelf carbonates.||||||07-NOV-08
16717|Seaspray Group|62370|6|Mentioned|p455|||Geological Province: Gippsland Basin.||||||
16717|Seaspray Group|63217|6|Mentioned|p102. |||||||||
16717|Seaspray Group|64876|5|Briefly described|p145 Fig.2|Oligocene|Oligocene|Gippsland Basin.|||Latrobe Valley Subgroup; Balook, Lakes Entrance, Swordfish Formations.|Overlies Cobia Subgroup (Latrobe Group) (Marshall Paraconformity and Latrobe Unconformity).||
16717|Seaspray Group|65717|5|Briefly described|p9 Fig.2.2, p10-12, p28, p38|Oligocene|Oligocene|Gippsland Basin. The regional seal to the top-Latrobe Group oil and gas accumulations.|||Latrobe Valley Subgroup.|Unconformably overlies Latrobe Group.|Calcareous sediments - marl and limestones.|05-SEP-17
16717|Seaspray Group|65718|5|Briefly described|p8, p10 Fig 3.2, p12, p14 Fig 3.3, p43|Oligocene|Oligocene|Gippsland Basin. Provides the regional seal to the top of the Latrobe Group oil and gas accumulations.|||Includes Lakes Entrance Formation (basal unit), Gippsland Limestone, Wuk Wuk Marl, Bairnsdale Limestone, Tambo River Formation, and Jemmys Point Formation.|Unconformably underlain by the Latrobe Group.|Comprises a carbonate-dominated succession.|
16717|Seaspray Group|65973|4|Described|p13, p17, p29, p33, p35, |||Gippsland Basin. Forms the regional top seal for the oil and gas accumulations of the Latrobe Group. Intersected in numerous drillholes including Leatherjacket-1, Kipper-1, Kipper-2, Judith-1, Hammerhead-1, East Pilchard-1, Longtom-1, Longtom-1/ST-1, Longtom-2/ST-1, Moby-1, Northright-1, Shark-1, Sole-1 and many more drillholes (see appendix). See also p57, p62, p65, p71, p74, p76-78, p80, p82, p85-86, p90, p93, p97, p102, p104, p108, p112, p114, p116-118, p123-144, p147-148, p151, p171, p180-183.|||Includes the Lakes Entrance Formation and the Gippsland Limestone.|Unconformably overlies the Latrobe Group.||
16717|Seaspray Group|66181|5|Briefly described|p310 Fig.5|Pleistocene|Oligocene|Includes the Sale, Hapuku, Albacore, Angler and Latrobe Valley Subgroups. Unconformably overlies the Latrobe Group.||||||
16717|Seaspray Group|67061|6|Mentioned|p554 Fig.10.|Miocene||Gippsland Basin, onshore.|||Includes Lakes Entrance, Gippsland and Tambo River Formations, Bairnsdale Limestone and Wuk Wuk Marl.|||
16717|Seaspray Group|67727|5|Briefly described|p55, p59, p62. |Holocene|Oligocene|Marine carbonate facies, up to 3 km thick, equivalent of Morwell and Yallourn Formations.|||Includes Lakes Entrance Formation.||Marls and limestones.|
16717|Seaspray Group|68116|5|Briefly described|Appendix.|Miocene|Rupelian||||||Clastic sedimentary rocks: calcareous and ferruginous sandstone, marl; nonmarine to paralic clastics, marine clastics, marine carbonates.|
16717|Seaspray Group|69016|5|Briefly described|p88-89|Early Pliocene|Early Oligocene|Of the Gippsland Basin.|||Includes Gippsland Limestone, Seaspray Sands, Bairnsdale Limestone, Lakes Entrance Formation, Tambo River Formation and Jemmy's Point Formation.||Marls and limestone.|
16717|Seaspray Group|69879|5|Briefly described|p428|Oligocene|Eocene|Gippsland Basin. Post Eocene upper megasequence. ~1km thick.||||Overlies Latrobe Group [Halibut Subgroup].|Mainly marine carbonate prograding strongly on the upper continental slope but rapidly wedging out downslope.|
16717|Seaspray Group|70028|5|Briefly described|p77-83, 86-91|Oligocene|Oligocene|Gippsland Basin. Has an extensive fault system; implications for CO2 storage analysed. Includes onshore and offshore sediments. Contains numerous, vertically stacked submarine channels.|||Lakes Entrance Formation.|Unconformably overlies Latrobe Group.||
16717|Seaspray Group|70076|5|Briefly described|South-Eastern: Fig.2; p2|Holocene|Rupelian|See also Regional: Fig.3; p3, p6.|||Angler, Albacore, Hapuku and Sale Subgroups; Sailfish Volcanics, Gippsland Limestone; Haunted Hills, Coongulmerang, Jemmys Point and Tambo River Formations.|Overlies Latrobe Group.||
16717|Seaspray Group|70331|5|Briefly described|p69-70|Oligocene|Oligocene|Gippsland Basin (western).||||Overlies Cobia Subgroup (Latrobe Group).|Onshore: paralic sandstone. Offshore: marine carbonates.|
16717|Seaspray Group|70862|6|Mentioned|p48 Fig.1|||Latrobe Valley, Gippsland Basin.|||Lakes Entrance, Tambo River Formations; Wuk Wuk Marl; Bairnsdale Limestone; Gippsland Limestone Formation.||Marine limestones and marls; marine sands at top.|
16717|Seaspray Group|73289|5|Briefly described|p764, 765 Fig.2, 767-769||||||Lakes Entrance Formation, Gippsland Limestone Formation; Wuk Wuk Marl.||Marine carbonates.|
16717|Seaspray Group|73471|5|Briefly described|p86-87, p89, p100 Fig.10, p104 Fig.14|Quaternary|Rupelian|Gippsland Basin. Mid-Miocene unconformity horizon serves as the stratigraphic boundary between the lower and upper Seaspray Group.|32 Ma||Balook Formation, Latrobe Valley subgroup, Lakes Entrance Formation, Gippsland Limestone|Overlies Cobia Subgroup|Marine carbonates.|
16717|Seaspray Group|73488|4|Described|p631-632, p633 Fig.3, p634 Fig.4, p636|Miocene|Oligocene|Gippsland Basin.|||Gippsland Limestone, Lakes Entrance Formation, Wuk Wuk Marl|Grades laterally into Balook Formation, correlates with Latrobe Valley Coal Measures|Marine carbonate sediments.|
16717|Seaspray Group|73562|5|Briefly described|p300-301, 303-305, 307, 309, 312-313|Quaternary|Oligocene|Gippsland Basin; offshore.|||Gippsland Limestone, Lakes Entrance Formation.|Overlies and transitions laterally into Latrobe Group.|Predominantly carbonate (marine) sediments.|
16717|Seaspray Group|75065|5|Briefly described|p149, 151, 154, 169|Quaternary|Oligocene|Gippsland Basin; offshore.|||Lakes Entrance Formation, Gippsland Limestone.|Unconformably overlies Cobia Subgroup (Latrobe Group).||
30566|Seldom Seen Formation|22968|6|Mentioned|P53||Early Silurian|||||||
30566|Seldom Seen Formation|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
30566|Seldom Seen Formation|23309|5|Briefly described|p63, 85, 87, 308, 351. Table 2.30.||Silurian|Parent: Yalmy Group.||||||25-SEP-08
30566|Seldom Seen Formation|23615|3|Fully described|p70, p21|Llandovery|Llandovery|Previously referred to as Seldom Seen Beds (Woodford, E.R. unpub) and Seldom Seen Group (VandenBerg et al, 1984).  Age: ~440-430Ma.  Max. thickness: >2600m. Correlated with Towanga Sandstone.||||||16-AUG-18
30566|Seldom Seen Formation|23938|5|Briefly described|p31-32 Fig. 12|Silurian|Silurian|See also p139 Tb. 1 Appendix.||||||25-SEP-08
30566|Seldom Seen Formation|24551|4|Described|p131|||||||||
30566|Seldom Seen Formation|43206|5|Briefly described|map legend||Llandovery|||||||
30566|Seldom Seen Formation|44185|5|Briefly described|Map legend.|Early Silurian|Early Silurian|Map symbol suggests may be part of Yalmy Group.|||||Marine: chert conglomerate, minor sandstone.|03-NOV-14
30566|Seldom Seen Formation|60503|5|Briefly described|p27, p28 Fig. 9|Early Silurian|Early Silurian|Of the Yalmy Group. Marine terrigenous clastics formed in submarine fan.||||||
30566|Seldom Seen Formation|60541|5|Briefly described|p11 Fig. 2|Early Silurian|Early Silurian|||||||
30566|Seldom Seen Formation|60542|5|Briefly described|p11 Fig. 2|Early Silurian|Early Silurian|||||||
30566|Seldom Seen Formation|61181|6|Mentioned|p196|Silurian|Silurian|Contains wollastonite in metamorphosed gritstone. ||||||
30566|Seldom Seen Formation|63290|6|Mentioned|p395|Late Ordovician|Late Ordovician|Contains late Ordovician conodonts in chert clasts and also black shale clasts, granite clasts also occur.||||||03-NOV-14
30566|Seldom Seen Formation|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery|||Unit in Yalmy Group.|||Quartzite, conglomerate, breccia; variably sorted, clast supported conglomerate; debris-flow breccia; pebbly and well sorted sandstone; clasts of chert, quartzite, intermediate to felsic volcanics, shale, black slate; rare mudstone.|
25470|Selma Sandstone|33601|6|Mentioned|p5|||||||||
25470|Selma Sandstone|42089|6|Mentioned|Fig.16 P27|||||||||
27564|Selwyn Granite|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
27564|Selwyn Granite|35073|6|Mentioned|p11|||||||||
27564|Selwyn Granite|61163|6|Mentioned|p39|||||||||
16748|Sentinel Rock Clay|24551|6|Mentioned|p642|||||||||
16748|Sentinel Rock Clay|30576|5|Briefly described|Table 2|||||||||
16748|Sentinel Rock Clay|30578|6|Mentioned|Table 1|||Also mention Table 2.||||||
16748|Sentinel Rock Clay|35066|6|Mentioned|p226|||In reference to Singleton 1967||||||
16748|Sentinel Rock Clay|42318|6|Mentioned|Fig.2 P10|||||||||
16748|Sentinel Rock Clay|42827|5|Briefly described|p300|||||||||
16748|Sentinel Rock Clay|70942|5|Briefly described|p124|||Non-marine.Plants.||||||
16757|Septarian Limestone|33155|6|Mentioned|p119|||||||||
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.|
30439|Serra Sandstone|23309|5|Briefly described|p78 Table 2.27|||Maximum Thickness: 350m.  Of the Mount Difficult Subgroup.||||||
30439|Serra Sandstone|24551|6|Mentioned|p122 Fig. 5.4|||Of the Red Man Bluff Formation?||||||
30439|Serra Sandstone|44929|5|Briefly described|Map Legend|Silurian|Ordovician|Of Mount Difficult Group. Includes the Teddy Bear Conglomerate Member. Quartz sandstone; intervals of poorly outcropping siltstone.||||||14-JUN-06
30439|Serra Sandstone|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Of Mount Difficult Sub-Group (Grampians Group). Includes Teddy Bear Conglomerate. Quartz sandstone, pale, medium- to coarse-grained; poorly outcropping intervals of siltstone among prominently outcropping sandstones.||||||13-JUN-06
30439|Serra Sandstone|44932|5|Briefly described|Map Legend|Silurian|Ordovician|Of Mount Difficult Group. Includes the Teddy Bear Conglomerate Member. Quartz sandstone; intervals of poorly outcropping siltstone.||||||14-JUN-06
30439|Serra Sandstone|44933|5|Briefly described|Map Legend|Silurian|Ordovician|Of Mount Difficult Group. Includes the Teddy Bear Conglomerate Member. Quartz sandstone; intervals of poorly outcropping siltstone.||||||14-JUN-06
30439|Serra Sandstone|60451|4|Described|p77 Fig. 47, 81, 137|Early Devonian|Ordovician|Of the Mount Difficult Subgroup (Grampians Group). Maximum Thickness: ~500m. Two Facies: 1. Pebbly lithofacies, fluvial in origin, 2. more sorted, finer grained, marine in origin.||||||
30439|Serra Sandstone|60456|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Mount Difficult Sub-Group.  Quartz sandstone: pale, medium to coarse grained with scattered and lag horizons of subrounded vein quartz pebbles at base.||||||
30439|Serra Sandstone|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Mount Difficult Subgroup. Quartz sandstone; pale, medium to coarse veined with scattered and lag horizons of sub-rounded vein quartz pebbles at base.||||||
30439|Serra Sandstone|61183|3|Fully described|p30 Tb. 2, p45|||Of Grampians Gp. Distinct marker horizon Teddy Bear Conglomerate, high in unit. Prominent sst outcrops, thinning southwards where interbedded poorly outcropping siltstone and marker bed occur; brecciated in places. Overlies Silverband Fm. Max.thick: 500m.||||||24-NOV-08
30439|Serra Sandstone|61186|6|Mentioned|p76|||Probably an equivalent to the Grampians or Stawell Sandstone; also thought to be equivalent of Wartook Sandstone at Rigby Rock. See also Serra Sandstone Formation. ||||||
30439|Serra Sandstone|61752|6|Mentioned|p24|||Site description - sedimentary structure of unit near Halls Gap.||||||07-FEB-11
30439|Serra Sandstone|64541|5|Briefly described|Map Legend|Silurian|Silurian|Of Mount Difficult Sub-group. Quartz sandstone: pale, medium to coarse grained with scattered and lag horizons of sub-rounded vein quartz pebbles at base; laminated, cross-laminated and trough cross-laminated.||||||07-FEB-11
30439|Serra Sandstone|64610|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Difficult (Grampians Gp). Comprises two subunits: quartz sandstone and poorly outcropping intervals of siltstone amongst the prominently outcropping sandstone - more details included.||||||11-NOV-08
30439|Serra Sandstone|65313|5|Briefly described|p582, Fig 10, p575 Fig. 4, p581 Fig. 9|Devonian|Ludlovian|Includes the basal Devonian Klonk (?isotopic) Event at ~416 Ma near the top of the unit. Includes latest Ludlovian equisetalean stem fossils near base. Grampians National Park section.||Part of Mount Difficult Subgroup.||Overlies Silverbrand Formation; underlies Moora Moora Sandstone.||26-MAR-12
30439|Serra Sandstone|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Mount Difficult Subgroup. Includes Teddy Bear Conglomerate Member.  Defined by Cayley & Taylor, 1997. ||||||
30439|Serra Sandstone|68116|5|Briefly described|Appendix, Maps 22, 30, 39.|Pridoli|Ludlow|Siltstone intervals prominent in the south of the Grampians Ranges. Skolithos horizons and ripple surfaces. Conglomerates: abundant bedrock clasts of angular dark slate and subrounded quartz-vein clasts. Sandstones: laminated to trough cross-laminated. |||||Quartz sandstone, minor siltstone and conglomerate; sandstone pale, medium to coarse grained with subrounded vein quartz pebbles, medium to thickly bedded. Conglomerate bands are pale grey, polymictic, poorly sorted with open framework. |
30439|Serra Sandstone|73118|6|Mentioned|p70-71|Ordovician|Ordovician||||||Quartz sandstone, siltstone.|
16777|Seven Creeks Basalt|22971|5|Briefly described|p 27||Tertiary|Age: +/- 6.8 Ma.||||||23-JUN-14
16777|Seven Creeks Basalt|33752|6|Mentioned|Fig.4|||||||||
16777|Seven Creeks Basalt|66244|4|Described|pp7-8.|Miocene|Miocene|Named after Seven Creeks, just south of Euroa. Description and analysis by Paul et al. (2005) shows basalt is more appropriate than limburgite (as in Euroa Limburgite). Included in the Older Volcanics on the Wangaratta 1:250 000 sheet (Vandenberg 1997); but its age (<10 Ma) makes it young enough to be included in the Newer Volcanic Group. Lying outside the geographic range of the Newer Volcanic Group, a separate Group has been established for the flows in the Euroa area: the Euroa Volcanic Group. This unit has two flows which join under the alluvium of Seven Creeks and extend north to Euroa.|6.79 +/- 0.16 Ma (Wellman 1974).|Unit in Euroa Volcanic Group.|||Two flows: one of alkali basalt, the other of basanite.|12-FEB-15
16777|Seven Creeks Basalt|68116|5|Briefly described|Appendix, Map 25.|Miocene|Miocene||||||Dark grey mafic volcanic rock containing small phenocrysts of olivine in a groundmass of augite, glass, magnetite and rare plagioclase, leucite or nepheline and red-brown biotite; ranges from alkali basalt to basanite; minor scoria and ash.|
34886|Shanahan Sandstone|22968|4|Described|P122, P127|Late Silurian|Late Silurian|New name, formalised unit, uppermost unit of the Mount Tambo Group, type section location given on P127, maximum thickness is 1200m||||||
34886|Shanahan Sandstone|23021|5|Briefly described|Map legend|Pridoli|Ludlow|Overlies Blackfellows Flat Conglomerate, parent is Mount Tambo Group||||||
34886|Shanahan Sandstone|23030|5|Briefly described|Map legend|Late Silurian|Late Silurian|Parent is the Mount Tambo Group||||||
34886|Shanahan Sandstone|23309|5|Briefly described|p103, 129 Table 2.37|||||||||
34886|Shanahan Sandstone|24551|4|Described|p140|||Of the Mount Tambo Group.||||||29-JUL-05
34886|Shanahan Sandstone|60503|5|Briefly described|p130|Early Devonian|Early Devonian|Of the Mount Tambo Group.  Also referred to as Mount Shanahan Sandstone in this study.||||||
34886|Shanahan Sandstone|68116|5|Briefly described|Appendix, Map 35.|Pragian|Ludlow||||||Sandstone and siltstone, with interbedded ignimbrite, minor lava and volcanigenic rocks at the base.|
16818|Sheehans Bluff Limestone Member|39447|6|Mentioned|p8|||Misspelling of Sheehan?||||||
16818|Sheehans Bluff Limestone Member|41585|6|Mentioned|p128|||||||||
16818|Sheehans Bluff Limestone Member|42827|5|Briefly described|p128|||of Cowombat Siltstone||||||
22836|Sheepyard Flat Boninite|23309|5|Briefly described|p28, 30-32 Table 2.4|||Of the Lickhole Volcanic Group.||||||
22836|Sheepyard Flat Boninite|24551|5|Briefly described|p90|||Of the Lickhole Volcanic Group. Overlies Mountain Chief Andesite.||||||23-JUN-14
22836|Sheepyard Flat Boninite|68116|5|Briefly described|Appendix, Map 34.|Cambrian|Cambrian||||||Ultramafic boninite lava and volcanic breccia; rare interbeds of finer volcaniclastics and two thin flows of tholeiitic basalt. Includes zones of melange: blocks of boninite, metabasalt, serpentinite and chlorite slate in a dark schistose matrix.|
37598|Sheevers Spur Ignimbrite|23309|5|Briefly described|p122, 133, Table 2.45|||Of Dartella Volcanics.||||||
37598|Sheevers Spur Ignimbrite|24551|5|Briefly described|p149|Devonian|Devonian|Of the Dartella Volcanics.||||||29-JUL-05
37598|Sheevers Spur Ignimbrite|60503|4|Described|p124, p41 Tb. 2|Early Devonian|Early Devonian|Of the Dartella Volcanics. Excludes the Larsen Creek Ignimbrite. Green, medium-grained ignimbrite with moderate-high phenocrysts, low quartz; pyroxene (chloritised); minor pumice, moderate welding. Conformably overlies the Larsen Creek Ignimbrite.||||||
37598|Sheevers Spur Ignimbrite|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Ignimbrite: dacitic pyroxene-feldspar ignimbrite, grey-green, densely welded||||||
37598|Sheevers Spur Ignimbrite|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Ignimbrite: dacitic pyroxene-feldspar ignimbrite, grey-green, densely welded||||||
37598|Sheevers Spur Ignimbrite|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Ignimbrite: dacitic pyroxene-feldspar ignimbrite, grey-green, densely welded||||||
37598|Sheevers Spur Ignimbrite|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Ignimbrite: dacitic pyroxene-feldspar ignimbrite, grey-green, densely welded||||||
37598|Sheevers Spur Ignimbrite|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Dartella Volcanic Group. Ignimbrite: flat lying moderately magnetic (20-150 nT); very low total count, K, Th, U||||||
37598|Sheevers Spur Ignimbrite|68116|5|Briefly described|Appendix, Map 27.|Early Devonian|Early Devonian||||||Dacitic pyroxene-feldspar ignimbrite: grey-green; medium-grained; moderate to high phenocryst content; densely welded.|
30463|Sheoak Gully Boninite|23309|5|Briefly described|p28, 30 Table 2.40|||Of the Heathcote Volcanics.||||||10-NOV-08
30463|Sheoak Gully Boninite|24177|4|Described|p35, p19 Tb.1|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Overlain by Lazy Bar Andesite. Intruded by Colbinabbin Diorite Sill||||||
30463|Sheoak Gully Boninite|24328|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics.||||||10-NOV-08
30463|Sheoak Gully Boninite|24329|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics.||||||10-NOV-08
30463|Sheoak Gully Boninite|24551|4|Described|p85|Cambrian|Cambrian|Of the Heathcote Volcanics. Overlain by Lazy Bar Andesite.||||||29-JUL-05
30463|Sheoak Gully Boninite|60591|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Deep marine boninite: phenocrysts of pyroxene, chromite, plagioclase; sperulites: minor rhyolite lava, volcanic sandstone, ash, hyaloclastite breccia.||||||27-OCT-08
30463|Sheoak Gully Boninite|60592|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Deep marine boninite: phenocrysts of pyroxene, chromite, plagioclase; sperulites: minor rhyolite lava, volcanic sandstone, ash, hyaloclastite breccia||||||25-NOV-04
30463|Sheoak Gully Boninite|60593|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Deep marine boninite: phenocrysts of pyroxene, chromite, plagioclase; sperulites: minor rhyolite lava, volcanic sandstone, ash, hyaloclastite breccia||||||
30463|Sheoak Gully Boninite|60595|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Deep marine boninite: phenocrysts of pyroxene, chromite, plagioclase; sperulites: minor rhyolite lava, volcanic sandstone, ash, hyaloclastite breccia||||||
30463|Sheoak Gully Boninite|60596|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Heathcote Volcanics. Deep marine boninite: phenocrysts of pyroxene, chromite, plagioclase; sperulites: minor rhyolite lava, volcanic sandstone, ash, hyaloclastite breccia||||||
30463|Sheoak Gully Boninite|60597|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Intensely magnetic boninite (>500 nT), nonmagnetic boninite (<1 nT), minor weakly magnetic and non-magnetic volcanic sandstone; low K, Th and U.||||||29-NOV-04
30463|Sheoak Gully Boninite|60599|2|Defined|p7, p32-33|Early Cambrian|Early Cambrian|Of Heathcote Volcanics (formerly an unnamed section of Heathcote Greenstone). Boninite lava and minor boninitic sediments and rhyolite lava. Overlain by Mount William Metabasalt. Geological Province: Lachlan Fold Belt. See also p24 Tb. 4, p32 Fig. 10.||||||
30463|Sheoak Gully Boninite|61187|5|Briefly described|p103, p104, p109 Fig.7, p110 Fig.8.|Cambrian|Cambrian|Hosts copper mineralisation at the Mount Camel Copper Show. Nonmagnetic to intensely magnetic responses. Thin bands of Ordovician black shale occur as fault slices in the boninite.||Unit in Mount William Volcanics.|||Boninitic lava with associated hyaloclastite breccia and sandstone; minor flow banded rhyolite with associated rhyolite hyaloclastite and breccia.|
30463|Sheoak Gully Boninite|65715|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Heathcote Volcanic Group. Formation rank.||||||
30463|Sheoak Gully Boninite|65969|6|Mentioned|p11, p17 Fig.7, p21 Fig.10|Cambrian|Cambrian|Of Heathcote Volcanic Group.||||||
30463|Sheoak Gully Boninite|68116|5|Briefly described|Appendix, Map 24.|Middle Cambrian|Early Cambrian||||||Boninite: phenocrysts of pyroxene, chromite, plagioclase; spherulites; massive with minor pillow lava; minor rhyolite lava, volcanic sandstone, ash, hyaloclastite breccia; deep-marine deposit.|
30463|Sheoak Gully Boninite|73497|5|Briefly described|Map legend|Cambrian|Cambrian|||Heathcote Volcanic Group||Underlies Lazy Bar Andesite|Boninite, volcanic sediment: intensely magnetic (>500 nT) boninite bands with minor weakly magnetic volcanic sandstone, nonmagnetic (<1 nT) boninite bands with minor nonmagnetic volcanic sandstone; low K, Th and U.|
25474|Shepparton Formation|2967|5|Briefly described|p14, p15 Fig.2.2, p18, p20 Fig.2.8, p22|Pliocene|Pliocene|Lawrence (1966). Eastern Murray Basin. Shallow aquifers. See also p28, 30-31, 33-35, 40-41, p47 Fig.2.25, p79, p83 Fig.4.5, p88, 96, 105, 128, 140, 143, 151.||Wunghnu Group.|Yando Clay Member.|Overlies Calivil Formation, Yando Clay or (in the Loddon Plain) the Parilla Sand..|Fluviolacustrine sediments: a suite of finer-grained sediments consisting of clays with interbedded shoestring sand lenses.|
25474|Shepparton Formation|10010|5|Briefly described|p12 Fig. 3|Late Pleistocene|Early Pliocene|Of the Wunghnu Group. Grades downwards into Calivil Formation. Geological Province: Murray Basin.||||||13-AUG-07
25474|Shepparton Formation|22487|6|Mentioned|p211, p212 Fig. 13|Quaternary|Tertiary|||||||11-SEP-08
25474|Shepparton Formation|22531|6|Mentioned|p6|||||||||
25474|Shepparton Formation|22756|3|Fully described|P13, P36|Pleistocene|Pliocene|||||||
25474|Shepparton Formation|22773|5|Briefly described|Fig24.8p352,354|||||||||
25474|Shepparton Formation|22782|4|Described|p16|||||||||
25474|Shepparton Formation|22799|5|Briefly described|p23 Fig.9|Late Pliocene|Late Pliocene|||||||
25474|Shepparton Formation|22857|5|Briefly described|p352-3 Figs.24.8 and 24.9, p354|Pleistocene|Late Pliocene|Of the Wunghnu Group. Fluvial and lacustrine deposits. Geological Province: Murray Basin.||||||
25474|Shepparton Formation|22886|6|Mentioned|p36|||||||||
25474|Shepparton Formation|22887|2|Defined|p45, Fig.6 p13|Pleistocene|Pleistocene|||||||
25474|Shepparton Formation|22893|3|Fully described|p61,62 table3 fig9|Pleistocene|Pleistocene|||||||
25474|Shepparton Formation|22971|4|Described|p 27||Tertiary|Max Thickness: 120m.||||||
25474|Shepparton Formation|23089|5|Briefly described|p649||Early Pliocene|||||||
25474|Shepparton Formation|23164|4|Described|p16|Pleistocene|Late Pliocene|||||||
25474|Shepparton Formation|23166|5|Briefly described|Map legend||Pliocene|||||||
25474|Shepparton Formation|23167|5|Briefly described|Map legend||Pliocene|||||||
25474|Shepparton Formation|23168|5|Briefly described|Map legend||Pliocene|||||||
25474|Shepparton Formation|23169|5|Briefly described|Map legend||Pliocene|||||||
25474|Shepparton Formation|23252|5|Briefly described|Map Legend||Pleistocene|Is subdivided into additional unnamed units.||||||
25474|Shepparton Formation|23300|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
25474|Shepparton Formation|23302|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
25474|Shepparton Formation|23303|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
25474|Shepparton Formation|23304|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
25474|Shepparton Formation|23305|6|Mentioned|p58|||Alluvium of Creswick similar to Shepparton Formation @ Kialla.||||||
25474|Shepparton Formation|23603|5|Briefly described|p12|Pleistocene|Late Pliocene|||||||
25474|Shepparton Formation|23604|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
25474|Shepparton Formation|23605|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
25474|Shepparton Formation|23606|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
25474|Shepparton Formation|23607|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
25474|Shepparton Formation|23884|5|Briefly described|p153, p155 Fig. 13.2|Pliocene|Pliocene|Geological Province: Murray Basin. Of the Wunghnu Group.||||||21-SEP-09
25474|Shepparton Formation|23921|5|Briefly described|p1109 Table 1|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
25474|Shepparton Formation|24043|5|Briefly described|p525|Holocene|Pleistocene|||||||
25474|Shepparton Formation|24103|5|Briefly described|p139 Fig.3, p141|Recent|Pliocene|||||||
25474|Shepparton Formation|24106|6|Mentioned|p185|||||||||
25474|Shepparton Formation|24107|5|Briefly described|p224|Quaternary|Tertiary|||||||
25474|Shepparton Formation|24108|5|Briefly described|p241|Recent|Pliocene|Geological Province: Murray Basin. Underlying Unit: Calivil Formation.||||||29-NOV-04
25474|Shepparton Formation|24133|6|Mentioned|p51|||Geological Province: Murray Basin.||||||
25474|Shepparton Formation|24177|3|Fully described|p75, p104|Quaternary|Neogene|Overlain by the Coonambidgal Formation. Disconformably overlies the Calivil and Wild Duck Formations, White Hills Gravel and Newer Volcanics. Age: <5 Ma. Geological Province: Murray Basin.||||||11-MAY-04
25474|Shepparton Formation|24178|6|Mentioned|p18|Devonian|Ordovician|||||||
25474|Shepparton Formation|24232|5|Briefly described|p226 Fig.2, p227|||||||||
25474|Shepparton Formation|24326|5|Briefly described|Map legend|Pleistocene|Miocene|||||||
25474|Shepparton Formation|24328|5|Briefly described|Map legend|Neogene|Neogene|||||||
25474|Shepparton Formation|24329|5|Briefly described|Map legend|Neogene|Neogene|||||||
25474|Shepparton Formation|24383|5|Briefly described|p31, p40 Fig.17|Recent|Pliocene|Max Thickness: 33m. Geological Province: Lachlan Fold Belt||||||
25474|Shepparton Formation|24384|5|Briefly described|Map legend|Pliocene|Pliocene|||||||
25474|Shepparton Formation|24385|5|Briefly described|Map legend|Pliocene|Pliocene|Sandy clay and sand; fine to coarse, includes leticular gravel channel beds; red to pale cream, mottled; well to poorly sorted, unconsolidated; dissected flood plains.||||||
25474|Shepparton Formation|24386|5|Briefly described|Map legend|Pliocene|Pliocene|Sandy clay and sand: fine to coarse, includes lenticular gravel channel beds.||||||
25474|Shepparton Formation|24387|5|Briefly described|Map legend|Pliocene|Pliocene|Sandy clay and sand; fine to coarse, includes lenticular gravel channel beds.||||||
25474|Shepparton Formation|24388|5|Briefly described|Map legend|Pliocene|Pliocene|Sandy clay and sand; nonmagnetic to weakly magnetic; variable, generally low-moderate total radioelements, K, Th and U.||||||13-JUN-06
25474|Shepparton Formation|24439|5|Briefly described|p8, p37, p38|Quaternary|Cenozoic|Geological Province: Murray Basin.  see also p47 Fig. 22 Appendix 2; p60 Appendix 3.||||||19-NOV-08
25474|Shepparton Formation|24440|5|Briefly described|Map legend|||||||||
25474|Shepparton Formation|24551|5|Briefly described|p322 Fig. 10.29, p324, p731|||Of the Wunghnu Group. Maximum Thickness: 125m.||||||29-JUL-05
25474|Shepparton Formation|29591|6|Mentioned|Table 20|||||||||
25474|Shepparton Formation|29860|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25474|Shepparton Formation|29898|4|Described|p213|||||||||
25474|Shepparton Formation|30581|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
25474|Shepparton Formation|30906|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
25474|Shepparton Formation|30934|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25474|Shepparton Formation|30935|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25474|Shepparton Formation|30936|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
25474|Shepparton Formation|31654|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
25474|Shepparton Formation|31713|6|Mentioned|p4|||Also P16||||||
25474|Shepparton Formation|31742|5|Briefly described|p6|||Upper Cainozoic||||||
25474|Shepparton Formation|31746|6|Mentioned|p197|||||||||
25474|Shepparton Formation|31747|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
25474|Shepparton Formation|32232|6|Mentioned|p19|||||||||
25474|Shepparton Formation|34312|5|Briefly described|p46|||Quaternary||||||
25474|Shepparton Formation|34735|4|Described|p39|||Also mention p8||||||
25474|Shepparton Formation|34757|6|Mentioned|Fig.3|||||||||
25474|Shepparton Formation|34813|6|Mentioned|p63|||||||||
25474|Shepparton Formation|34986|6|Mentioned|p339|||||||||
25474|Shepparton Formation|35091|4|Described|p11|||Also P17.||||||
25474|Shepparton Formation|35094|6|Mentioned|p12|||||||||
25474|Shepparton Formation|35111|6|Mentioned|p2|||||||||
25474|Shepparton Formation|35187|6|Mentioned|Table1|||||||||
25474|Shepparton Formation|35234|6|Mentioned|p9|||||||||
25474|Shepparton Formation|35242|6|Mentioned|p95|||||||||
25474|Shepparton Formation|35272|3|Fully described|p276|||||||||
25474|Shepparton Formation|37809|6|Mentioned|p5|||||||||
25474|Shepparton Formation|37871|4|Described|p12|||||||||
25474|Shepparton Formation|37873|6|Mentioned|p3|||||||||
25474|Shepparton Formation|37881|6|Mentioned|p16|||||||||
25474|Shepparton Formation|37882|4|Described|p6|||||||||
25474|Shepparton Formation|37883|6|Mentioned|p11|||||||||
25474|Shepparton Formation|37884|6|Mentioned|p15|||||||||
25474|Shepparton Formation|37885|5|Briefly described|p6|||||||||
25474|Shepparton Formation|38293|4|Described|p23|||||||||
25474|Shepparton Formation|39329|6|Mentioned|Fig.1|||||||||
25474|Shepparton Formation|39858|6|Mentioned|Map legend|Pleistocene|Pliocene|Pliocene - Pleistocene||||||
25474|Shepparton Formation|39860|5|Briefly described|p33|||||||||
25474|Shepparton Formation|40498|6|Mentioned|p433|||||||||
25474|Shepparton Formation|40520|6|Mentioned|Fig.5|||||||||
25474|Shepparton Formation|40522|6|Mentioned|Fig.2|||||||||
25474|Shepparton Formation|40599|5|Briefly described|p19|||||||||
25474|Shepparton Formation|40795|6|Mentioned|p80|||||||||
25474|Shepparton Formation|40820|6|Mentioned|p147|||||||||
25474|Shepparton Formation|41068|5|Briefly described|p67|||||||||
25474|Shepparton Formation|41136|5|Briefly described|p215|||||||||
25474|Shepparton Formation|41765|4|Described|p39|||||||||
25474|Shepparton Formation|41848|3|Fully described|p352||Quaternary|age ranges from approx 1 million years to 25 thousand years BP||||||
25474|Shepparton Formation|41849|6|Mentioned|p409|||Age Pleistocene||||||
25474|Shepparton Formation|41868|5|Briefly described|p551|||||||||
25474|Shepparton Formation|42125|5|Briefly described|p139|||||||||
25474|Shepparton Formation|42126|6|Mentioned|p149|||||||||
25474|Shepparton Formation|42130|6|Mentioned|Fig.3 P265|||||||||
25474|Shepparton Formation|42133|6|Mentioned|p302|||||||||
25474|Shepparton Formation|42134|4|Described|p339|||||||||
25474|Shepparton Formation|42137|5|Briefly described|p367|||See also Fig.2||||||
25474|Shepparton Formation|42138|6|Mentioned|Fig.2 P390|||||||||
25474|Shepparton Formation|42184|6|Mentioned|Fig.2 P348|||||||||
25474|Shepparton Formation|42454|4|Described|p12|Recent|Pliocene|Pliocene to 20 000BP.||||||
25474|Shepparton Formation|42455|5|Briefly described|Map legend|Recent|Pliocene|||||||
25474|Shepparton Formation|42683|5|Briefly described|map legend|||||||||
25474|Shepparton Formation|42827|3|Fully described|p352|||Of Wunghnu Group||||||13-JUN-06
25474|Shepparton Formation|42881|4|Described|Fig.3, P84|||||||||
25474|Shepparton Formation|42966|2|Defined|p187|Recent|Pliocene|Of Wunghnu Group. First published definition, but supersedes definition card.||||||13-JUN-06
25474|Shepparton Formation|43198|5|Briefly described|Map Legend|Recent|Pliocene|||||||
25474|Shepparton Formation|43199|5|Briefly described|Map Legend|Recent|Pliocene|||||||
25474|Shepparton Formation|43211|4|Described|p29||Quaternary|||||||
25474|Shepparton Formation|43218|4|Described|Fig.3,p22|Quaternary|Tertiary|||||||
25474|Shepparton Formation|43260|5|Briefly described|Map Legend|Pleistocene|Miocene|||||||
25474|Shepparton Formation|43261|5|Briefly described|Map Legend|Pleistocene|Pliocene|||||||
25474|Shepparton Formation|43493|5|Briefly described|32-36|Recent|Pleistocene|Radiocarbon dates to 30 000 years BP||||||
25474|Shepparton Formation|43578|6|Mentioned|p337|Pleistocene|Pliocene|||||||
25474|Shepparton Formation|43601|6|Mentioned|p225|||||||||
25474|Shepparton Formation|43627|6|Mentioned|p6||Quaternary|||||||
25474|Shepparton Formation|43655|5|Briefly described|p40-846|||||||||
25474|Shepparton Formation|43780|6|Mentioned|p6|||||||||
25474|Shepparton Formation|43791|6|Mentioned|p372, Fig1|||||||||
25474|Shepparton Formation|43804|6|Mentioned|Fig.2,p49|||||||||
25474|Shepparton Formation|43841|5|Briefly described|8||Tertiary|||||||
25474|Shepparton Formation|43846|5|Briefly described|14|Recent|Pleistocene|||||||
25474|Shepparton Formation|44184|5|Briefly described|Map Legend||Pleistocene|||||||
25474|Shepparton Formation|44186|5|Briefly described|Map Legend||Pleistocene|||||||
25474|Shepparton Formation|44188|5|Briefly described|Map Legend|Holocene|Pliocene|Geological province: Murray Basin. Poorly consolidated to unconsolidated mottled, variegated clay, silty clay with lenses of polymictic coarse to fine sand and gravel.||||||15-MAY-08
25474|Shepparton Formation|44197|5|Briefly described|Map Legend||Pleistocene|||||||
25474|Shepparton Formation|45168|6|Mentioned|p14|||||||||
25474|Shepparton Formation|49038|4|Described|Table 2|||Briefly described p31 and p40||||||13-JUN-06
25474|Shepparton Formation|49040|6|Mentioned|p12|||||||||
25474|Shepparton Formation|50154|2|Defined|p26, p139-140|Recent|Pliocene|Geological Province: Murray Basin. Conformably overlies the Calivil Formation. Partly equivalent to the Parilla Sand.||||||24-JUN-14
25474|Shepparton Formation|50156|5|Briefly described|Map Legend|Pleistocene|Miocene|Fluvial: prior stream, valley-backfill and floodplain deposits; clay, sand, silt, gravel.||||||
25474|Shepparton Formation|50157|5|Briefly described|Map Legend|Pleistocene|Miocene|Fluvial: prior stream, valley-backfill and floodplain deposits; clay, sand, silt, gravel.||||||
25474|Shepparton Formation|50158|5|Briefly described|Map Legend|Pleistocene|Miocene|Of Wunghnu Group. Fluvial: prior stream, valley-backfill and floodplain deposits; clay, sand, silt, gravel.||||||
25474|Shepparton Formation|50159|5|Briefly described|Map Legend|Pleistocene|Miocene|Of Wunghnu Group. Fluvial: prior stream, valley-backfill and floodplain deposits; clay, sand, silt, gravel.||||||
25474|Shepparton Formation|50160|5|Briefly described|Map Legend|Pleistocene|Miocene|Of Wunghnu Group.||||||
25474|Shepparton Formation|50161|5|Briefly described|Map Legend|Pleistocene|Miocene|Of Wunghnu Group. Fluvial: prior stream, valley-backfill and floodplain deposits; clay, sand, silt, gravel.||||||
25474|Shepparton Formation|50162|5|Briefly described|Map Legend|Pleistocene|Miocene|Of Wunghnu Formation. Fluvial: prior stream, valley-backfill and floodplain deposits; clay, sand, silt, gravel.||||||22-JUN-04
25474|Shepparton Formation|50163|5|Briefly described|Map Legend|Pleistocene|Miocene|Of Wunghnu Group. Overlies Duddo Limestone. Overlain by Lowan Sand. Fluvial: prior stream, valley-backfill and floodplain deposits; clay, sand, silt, gravel.||||||25-JUN-04
25474|Shepparton Formation|60005|5|Briefly described|Map legend|Pleistocene|Pleistocene|Fluvial: silt, sand, minor gravel.||||||11-JAN-10
25474|Shepparton Formation|60451|4|Described|p102|Holocene|Pliocene|Type section in text. Maximum Thickness: >30m. Overlies: Parilla Sand, Calivil Formation, rarely White Hills Gravel.||||||27-OCT-04
25474|Shepparton Formation|60452|4|Described|p40|Quaternary|Quaternary|Forms the flat riverine plain. Includes the Katandra, Quiamong, and Mayrung members (which probably represent only the upper part of the formation). Interfingers with Parilla Sand; disconformably overlies the Calivil Formation.||||||23-MAY-13
25474|Shepparton Formation|60454|5|Briefly described|Map Legend|Quaternary|Neogene|Dissected flood plain alluvium, terraces 1-10m above present river channels; sandy clay; fine to coarse sand; poorly sorted lenticular gravel.||||||
25474|Shepparton Formation|60456|5|Briefly described|Map Legend|Quaternary|Neogene|dissected flood plain alluvium: terraces 1-10m above present river channels; sandy clay; fine to coarse sand; poorly sorted lenticular gravel.||||||
25474|Shepparton Formation|60457|5|Briefly described|Map Legend|Quaternary|Neogene|Dissected flood plain alluvium; terraces 1-10m above present river channels; sandy clay; fine to coarse sand; poorly sorted lenticular gravel; well developed soil 2-3m thick.||||||13-JUN-06
25474|Shepparton Formation|60458|5|Briefly described|Map Legend|Quaternary|Neogene|Dissected flood plain alluvium.||||||
25474|Shepparton Formation|60461|5|Briefly described|Map legend|Recent|Miocene|Of the Murray Group.  Clay, silt, fine to coarse-grained sand of quartz, mica, feldspar and ironstone; quartz gravel.||||||06-OCT-04
25474|Shepparton Formation|60491|4|Described|p23|Quaternary|Pliocene|Overlies all units in the Charlton 1: 100K map area, except the Coonambidgal Formation, lunettes and source bordering dunes. Locally overlain by the Parilla Sand.||||||
25474|Shepparton Formation|60492|5|Briefly described|Map Legend|Pleistocene|Pliocene|Overlies the Parill Sand. Of the Wunghnu Group. Alluvium: incised floodplain deposits, prior streams and minor lake deposits; coarse grained sand, silt, clay.||||||30-SEP-04
25474|Shepparton Formation|60529|5|Briefly described|Map Legend|Recent|Pliocene|Prior stream deposits, valley backfill deposits and alluvial flood plain and swamp deposits.||||||
25474|Shepparton Formation|60591|5|Briefly described|Map Legend|Recent|Pliocene|Unconformably overlies the Mount Ida Formation, Sheoak Gully Boninite, Broadford Formation, Puckapunyal Formation and Waranga Formation.||||||
25474|Shepparton Formation|60592|5|Briefly described|Map Legend|Recent|Pliocene|Unconformably overlies the Mount Ida Formation, Sheoak Gully Boninite, Broadford Formation, Puckapunyal Formation and Waranga Formation.||||||25-NOV-04
25474|Shepparton Formation|60593|5|Briefly described|Map Legend|Recent|Pliocene|Unconformably overlies the Mount Ida Formation, Sheoak Gully Boninite, Broadford Formation, Puckapunyal Formation and Waranga Formation.||||||
25474|Shepparton Formation|60595|5|Briefly described|Map Legend|Recent|Pliocene|Unconformably overlies the Mount Ida Formation, Sheoak Gully Boninite, Broadford Formation, Puckapunyal Formation and Waranga Formation.||||||
25474|Shepparton Formation|60596|5|Briefly described|Map Legend|Recent|Pliocene|Unconformably overlies the Mount Ida Formation, Sheoak Gully Boninite, Broadford Formation, Puckapunyal Formation and Waranga Formation.||||||
25474|Shepparton Formation|60597|5|Briefly described|Map Legend|Recent|Pliocene|Nonmagnetic with dendritic, moderately magnetic responses (10-20 nT) coinciding with present and prior streams; moderate K, variable Th, and U.||||||
25474|Shepparton Formation|60599|2|Defined|p16, p24 Tb. 4, p92, p85|Recent|Pliocene|Of Wunghnu Gp. Comprises Kialla, Katandra, Quiamong + Mayrung Members, capped by Widgelli Pedoderm. Fluvial /lacustrine seds. Disconformable on Calivil + Wild Duck Fms, White Hills Gravel + Newer Volcs;overlain by Coonambidgal Formation. Murray Basin.||||||10-NOV-08
25474|Shepparton Formation|61155|5|Briefly described|p5, p18|Pleistocene|Early Pliocene|Clastics. Overlies the Calvil Formation; overlies and interfingers with Loxton-Parilla Sands. Age: <4.5Ma. Thickness: 20m. Geological Province: Murray Basin.||||||
25474|Shepparton Formation|61163|4|Described|p104-105, p36 Tb. 6.2, p177|Pleistocene|Pleistocene|Of Wunghnu Group. Overlain by Calivil Fm (also Wunghnu Gp). Geol Prov: LFB. Well-compacted channel fill conglomerate, gravel and sand, intercalated with point bar gravel and sand and finer overbank deposits - forming terrace remnants above alluvial flats.||||||06-JUL-07
25474|Shepparton Formation|61174|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Clay, sand, silt, gravel: generally well sorted, well rounded; friable; polymictic; friable, deep red to pale colours. GSV map code: Nws.||||||07-FEB-11
25474|Shepparton Formation|61175|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Clay, sand, silt, gravel: generally well sorted, well rounded; friable; polymictic; friable, deep red to pale colours. GSV map code: Nws.||||||
25474|Shepparton Formation|61176|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Clay, sand, silt, gravel: generally well sorted, well rounded; friable; polymictic; friable, deep red to pale colours. GSV map code: Nws.||||||
25474|Shepparton Formation|61177|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Clay, sand, silt, gravel: generally well sorted, well rounded; friable; polymictic; friable, deep red to pale colours. GSV map code: Nws.||||||
25474|Shepparton Formation|61178|5|Briefly described|map legend|Quaternary |Quaternary |Of Wunghnu Group. Clay, sand, silt, gravel (prior stream, valley-backfill and floodplain deposits): nonmagnetic; no discernible gravity response; low total radioelements, K moderate Th and U; low Th and high U in upper Buffalo R. GSV map code: Nws.||||||
25474|Shepparton Formation|61183|5|Briefly described|p18 Fig. 9, p68|Recent|Pliocene|Consists mostly of clay, which is mottled and contains pisolitic nodules. Geological Province: Murray Basin. See also p133. ||||||
25474|Shepparton Formation|61185|2|Defined|p63-69, p49, p53, p57|Recent|Pliocene|Incl: Kialla, Katandra, Quiamong, Mayrung Members and Widgelli Pedoderm of Wunghnu Group (Lawrence 1966). Incl: Torrumbarry Clay (Tickell 1977). Fluvial and lacustrine sediments. Overlies Strathbogie Granite and Hilldene Basalt. Underlies Coonambidgal Fm.||||||07-FEB-11
25474|Shepparton Formation|61314|5|Briefly described|p129|Quaternary|Late Pliocene|Fine-grained clastics and polymictic sands and gravels. Geological Province: eastern Murray Basin.||||||
25474|Shepparton Formation|61701|5|Briefly described|Map Legend|Recent|Pliocene|Prior stream deposits, valley backfill deposits and alluvial flood plain and swamp deposits.||||||
25474|Shepparton Formation|61702|5|Briefly described|Map Legend|Recent|Pliocene|Prior stream deposits, valley backfill deposits and alluvial flood plain and swamp deposits.||||||
25474|Shepparton Formation|61703|5|Briefly described|Map Legend|Recent|Pliocene|Prior stream deposits, valley backfill deposits and alluvial flood plain and swamp deposits.||||||
25474|Shepparton Formation|61704|6|Mentioned|Map legend|Quaternary|Quaternary|Variable radiometric respone; non-magnetic.||||||12-FEB-15
25474|Shepparton Formation|61964|3|Fully described|p14 Fig. 4, p143-144|Pleistocene|Late Pliocene|Of Wunghnu Group. Associated with Coonambidgal Fm, mapped as a Quaternary alluvial suite. Unit presents as extensive flat alluvial floodplains, traversed by traces of meandering palaeochannels. Conformably overlies Calivil Fm. Geol.Prov: Murray Basin||||||
25474|Shepparton Formation|62370|5|Briefly described|p449, p452 Fig.4|Holocene|Pliocene|Fluviolaucstrine unit which includes channel sand, levee banks of fine sandy clay and floodplain clay. Unconformably overlies Calivil Formation. Geological Province: Murray Basin. See also p464 Fig.12.||||||
25474|Shepparton Formation|62405|5|Briefly described|Map legend|Tertiary|Tertiary|Unconsolidated brown silty to sandy clay, mottled variegated clay, silty clay with sporadic lenses of polymictic fine- to coarse-gr. sand and gravel. Partly modified by pedogenesis; intercalated red-brown palaeosols.||||||25-MAR-08
25474|Shepparton Formation|63446|5|Briefly described|Map legend|Pleistocene|Pleistocene||||||Fluvial: silt, sand, minor gravel.|
25474|Shepparton Formation|63777|5|Briefly described|p1104 Fig. 1, p1105 -1108, p1110-1113|||Underlian by Calival Formation. Geological Province: Murray Basin. Series of fluvio-lacustrine clays, sands and silts.||||||
25474|Shepparton Formation|63893|5|Briefly described|p191|||Lowest units overlie Loxton-Parilla Sands and Blanchetwon Clay. Fluvial sequence generally deposited onto the erosional surface formed after the Loxton-Parilla depositional cycle.||||||
25474|Shepparton Formation|64823|5|Briefly described|p1012 Fig. 2b|Cenozoic|Cenozoic|Overlies Calivil Formation and Parilla Formation.||||||
25474|Shepparton Formation|65552|5|Briefly described|p2, p4-7, p19; p24-27 App.3-6|Holocene|Early Pliocene|Of Wanghnu Group. Hosts saline groundwater from which salt is extracted. With Coonambidgal Formation, overlies Calivil Formation and is the upper sequence in the Murray Basin. Fluvial with sporadic aeolian parna deposits and overflow lake sediments.||||||
25474|Shepparton Formation|65715|5|Briefly described|p15 Tb.8, p17|Neogene|Neogene|Of Wunghnu Group. Essentially alluvial sediments of the Murray Basin. Said to be older than Coonambidgal Formation by Lawrence (1966), but this unit no longer used by GSV.||||||
25474|Shepparton Formation|65969|5|Briefly described|p27 Tb.3.3, p30|Pliocene|Miocene|Fluvial mud and shoestring sand and gravel. Onshore sequence equivalent to Parilla Sand. Occurs in dendritic river channels draining north; fills broad topographic lows. Pliocene to Late Miocene. Streams close to basin margin have magnetic responses to 20 nT; low radiometric response.||||||
25474|Shepparton Formation|66002|5|Briefly described|p13 Tb.9, p18|Neogene|Neogene|Of Wunghnu Group. Defined by Lawrence 1966. Essentially alluvial sediments. In Murray Basin||||||
25474|Shepparton Formation|66244|6|Mentioned|p8.|||||||Overlies the Balmattum Basalt at its downstream end.||12-FEB-15
25474|Shepparton Formation|66286|5|Briefly described|p182, pp185-187, p190.|||Regarded as the source of much of the infiltrated clays and possible silts in Lithofacies D and E of Loxton-Parilla sands. 3 - 5 m thick sandy muds and sandy clays. Lacustrine and fluvial overbank sediments with channel fills.||||Overlies Loxton-Parilla sands.|Sandy clays, sandy muds, gravelly lenses with ferruginous pisoliths set in lenticular mottled clay.|
25474|Shepparton Formation|67179|4|Described|p580-85, Fig.1b, Fig.3, Fig.4|Holocene|Pliocene|May fill the the swales between Loxton Sand strandlines.||||Overlies the Loxton Sand (locally the Wandella Sandstone Member) in eastern Murray Basin, underlies the Coonambidgal Formation (conformably).|Unconsolidated to poorly consolidated clay, silt and silty clay deposited as floodplain muds, intercalated with lenses of fine to coarse sand and gravel.|
25474|Shepparton Formation|68116|5|Briefly described|Appendix, Maps 7-8, 10-26, 29-33, 42.|Holocene|Pliocene||||||Clay, sand, silt, poorly-sorted lenticular gravel. Dissected flood plain alluvium: terraces 1-10 metres above present river channels; well developed soil 2-3 m thick.|
25474|Shepparton Formation|68140|5|Briefly described|p1699, p1702, p1703 Fig.4, pp1706-1708|||Uppermost unit. Heterogeneous and laterally discontinuous. Groundwater in this unit is susceptible to contamination from human activities on the surface.||||Underlain by the Loxton-Parilla Sands. Underlain by the Calivil-Renmark Formation.|Comprises fluvio-lacustrine clays, sands and silts; laterally discontinuous.|09-FEB-18
25474|Shepparton Formation|68189|5|Briefly described|p4, p27 Tb.3.2, p29, p30, p31 Fig.16|Quaternary|Miocene|Flood plain and prior stream deposits; the flood plain deposits interfinger and overlap with the Parilla Sand.||||Conformably underlain and interfingers with the Parilla Sand.  Possibly underlain by the Blanchetown Clay.|Comprises mud and shoestring sand.|
25474|Shepparton Formation|68194|5|Briefly described|p6, p9, p11, p17, p21, p24-27, p35-36|Pleistocene|Pliocene|See also p40, p44, p56-57, p66. Lawrence (1966). Fluvio-lacustrine sediments forming flat clay plains. Regolith and remote sensing profiles described.||Unit in Wunghnu Group.||Disconformably overlies Parilla Sand.|Sands and gravels.|
25474|Shepparton Formation|69089|5|Briefly described|Map legend|Pleistocene|Pleistocene||||||Fluvial: silt, sand, minor gravel.|
25474|Shepparton Formation|69162|5|Briefly described|Map legend|Tertiary|Tertiary|Murray Basin.|||||Unconsolidated brown silty to sandy clay, mottled variegated clay, silty clay with sporadic lenses of polymictic fine- to coarse-grained sand and gravel; partly modified by pedogenesis; intercalated red-brown palaeosols.|
25474|Shepparton Formation|69163|5|Briefly described|Map legend|Tertiary|Tertiary|Murray Basin.|||||Unconsolidated brown silty to sandy clay, mottled variegated clay, silty clay with sporadic lenses of polymictic fine- to coarse-grained sand and gravel; partly modified by pedogenesis; intercalated red-brown palaeosols.|
25474|Shepparton Formation|69798|5|Briefly described|p4 Fig.2|Pliocene|Pliocene|Murray Basin.||Wunghnu Group.||||
25474|Shepparton Formation|70718|4|Described|p17, p23, p25, p104|Pliocene|Pliocene|Deposited in a fluvio-lacustrine environment with floodplain, channel and levee components and minor aeolian influences. Is one of the primary aquifers in the Hay map sheet area. Shallow aquifers in this formation have a  higher salinity in the east and pockets of lower salinity in the west; this is attributed to fresh water influx frfom the Murrumbidgee alluvial fan.||Wunghnu Group||Transitionally overlies the Calivil Formation. Overlain by the Coonambidgal Formation. Equivalent to the Parilla Sand.|Unconsolidated to poorly consolidated, mottled, variegated clay, silty clay with lenses of polymictic, coarse to fine-grained sand and gravel; partly modified by pedogenesis, includes intercalated red-brown palaeosols.|
25474|Shepparton Formation|70961|14|Not recorded|p133|||Refers to Lawrence (1966).||||||
25474|Shepparton Formation|71593|4|Described|p53-p54, p56||Pliocene|Deposited by fluvial systems. Generally less than 10-20m thick. ||||Overlies the Loxton Sand.|Laterally extensive clayey overband sediments.|
25474|Shepparton Formation|72445|5|Briefly described|App 1; App.2; App.7 p7, p7 Fig.4.|Quaternary|Pliocene|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991). Described, along with Loxton-Parilla Sands, Shepparton Formation, as fluvio lacustrine. Identified in Stavely 09,10, 12, 16.||Wunghnu Group||Overlies Loxton Sand (sharp contact). Shown as overlying Calivil Formation (sharp contact) and Torrumbarry Clay partially equivalent to Wandella Limestone Member and Blanchetown Clay.|Includes mottled sandy silt; silty mud and fine sand; silty to sandy mud; muddy sand (soil horizon).|
25474|Shepparton Formation|73118|5|Briefly described|p17, 30, 34, 42, 48, 81|Quaternary|Pliocene|Murray Basin. 100m thick; generally <70m. Forms extensive flat alluvial floodplains. Drill core summary logs. Fluvio-lacustrine, flood-plain, channel and levee deposits; minor aeolian.||Wunghnu Group||Overlies Loxton-Parilla Sands, Duddo Limestone, Grampians Group.|Un- to poorly-consolidated, mottled to variegated clay, silty clay with lenses of coarse to fine polymictic sand and gravel. Forms red-brown palaeosols.|
25474|Shepparton Formation|73228|6|Mentioned|p57, p62|Quaternary|Pliocene|Underlain by an erosion or non-depositional horizon.||||Overlain by Coomandook Formation[?]. Equivalent to Bookpurnong Formation[?].||
25474|Shepparton Formation|73229|6|Mentioned|p67|||Murray Basin. Shown in Fig.1 as Miocene to Pliocene.||||||31-OCT-22
25474|Shepparton Formation|73496|5|Briefly described|Map legend|Pleistocene|Miocene|||Wunghnu Group|||Prior stream deposits and minor alluvium; mostly nonmagnetic but with dendritic, moderately magnetic responses (to 10-20 nT) coinciding with present and prior streams; high K, low Th, U radiometric highs.|
25474|Shepparton Formation|73497|5|Briefly described|Map legend|Pleistocene|Miocene|||Wunghnu Group|||Prior stream, valley-backfill and floodplain deposits: nonmagnetic with moderately magnetic responses (10-20 nT) with a dendritic pattern coinciding with drainage; low-high K, Th and U.|
25474|Shepparton Formation|73505|4|Described|p2, p11, p13|Pliocene|Late Miocene|Murray Basin. Topography of dendritic river channels draining north, fills broad lows. Low radiometric response.||Wunghnu Group||Onshore sequence equivalent of Parilla Sand, sequence/time equivalent of Bookpurnong beds and Parilla Sand|Fluvial mud and shoestring sand.|
25474|Shepparton Formation|73576|5|Briefly described|p802|Paleogene|Paleogene|Partially covers Tarnagulla Granodiorite.|||||Alluvium.|
16826|Sherbrook Group|12781|5|Briefly described|p386, 391-392|Late Cretaceous|Late Cretaceous|Otway Basin. A very rapid increase in thickness occurs south of the Tartwaup Hingeline.|||Copa, Waarre, Paaratte, Flaxman Formations; Timboon Sandstone; Belfast Mudstone.|Overlies Otway Supergroup. Is overlain by Wangerrip Group.||
16826|Sherbrook Group|12796|5|Briefly described|p456 Fig. 2|||Geological Province: Otway Basin.||||||
16826|Sherbrook Group|22470|5|Briefly described|p13 Fig. 17|Maastrichtian|Turonian|Otway Basin.||||||
16826|Sherbrook Group|22674|5|Briefly described|p718, Fig.2 p719|Maastrichtian|Cenomanian|See also Fig.8 p725||||||
16826|Sherbrook Group|22875|3|Fully described|p37|Late Cretaceous|Late Cretaceous|~65-95Ma.||||||27-AUG-18
16826|Sherbrook Group|22914|6|Mentioned|17|||||||||
16826|Sherbrook Group|22944|6|Mentioned|p2||Cenomanian|||||||
16826|Sherbrook Group|23230|5|Briefly described|Table4-1p40, 40||Late Cretaceous|||||||
16826|Sherbrook Group|23792|5|Briefly described|p26|Maastrichtian|Turonian|Geological Province: Otway Basin.||||||21-OCT-08
16826|Sherbrook Group|23818|5|Briefly described|p162, 175|Late Cretaceous|Late Cretaceous|Of the Knight Group. Underlying unit: Otway Group. Overlying unit: Bahgallah Formation.||||||
16826|Sherbrook Group|23939|6|Mentioned|Fig.5|||May be Late Cretaceous in age. ||||||
16826|Sherbrook Group|24056|4|Described|p85|Late Cretaceous|Late Cretaceous|Geological Basin: Otway Basin.||||||
16826|Sherbrook Group|24200|5|Briefly described|p408|Maastrichtian|Maastrichtian|Geological Province: Otway basin.  See also p423 Figs. 15 & 16, p 428 Fig. 18.  Sherbrook Group Equivalents discussed throughout text.||||||
16826|Sherbrook Group|24323|5|Briefly described|p136|Late Cretaceous|Late Cretaceous|Geological Province: Otway Basin. Overlain by the Wangerrip Group.||||||
16826|Sherbrook Group|24453|5|Briefly described|p809 Fig.2|Maastrichtian|Cenomian|Geological Province: Otway Basin.||||||07-FEB-11
16826|Sherbrook Group|24551|5|Briefly described|p240, Fig. 9.2|Late Cretaceous|Late Cretaceous|||||||
16826|Sherbrook Group|24562|4|Described|p6, 8, 37 Fig. 2|Late Cretaceous|Late Cretaceous|Maximum Thickness: 5000m+.  Includes: Waarre Sandstone, Flaxmans Formation, Belfast Mudstone, Nullawarre Greensand, Paaratte Formation, Timboon Sandstone.  Geological Province: Otway Basin.||||||
16826|Sherbrook Group|29697|6|Mentioned|Fig.11|||||||||
16826|Sherbrook Group|29856|5|Briefly described|p38|||||||||
16826|Sherbrook Group|30499|6|Mentioned|p92|||Stratigraphy||||||
16826|Sherbrook Group|30576|6|Mentioned|Fig.1|||||||||
16826|Sherbrook Group|30578|6|Mentioned|p6|||||||||
16826|Sherbrook Group|30905|6|Mentioned|p149|||||||||
16826|Sherbrook Group|30928|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|||||||
16826|Sherbrook Group|31202|5|Briefly described|p218|||Unconformity with Otway Gp. & rift formation||||||
16826|Sherbrook Group|31372|6|Mentioned|p9|||||||||
16826|Sherbrook Group|31624|6|Mentioned|p98|||U.Cret. Contains Curdies Fm. & Paaratte Fm.||||||
16826|Sherbrook Group|31625|6|Mentioned|Fig. 5.2|||U.Cret.||||||
16826|Sherbrook Group|31920|3|Fully described|p50|||U.Cret. See also Fig.3-2||||||
16826|Sherbrook Group|31922|6|Mentioned|p187|||||||||
16826|Sherbrook Group|31923|6|Mentioned|p16|||||||||
16826|Sherbrook Group|32162|6|Mentioned|p58|||See also Fig. 5||||||
16826|Sherbrook Group|32344|6|Mentioned|Fig.2|||||||||
16826|Sherbrook Group|32852|6|Mentioned|P110|||||||||
16826|Sherbrook Group|32894|6|Mentioned|Table 2-1|||||||||
16826|Sherbrook Group|32897|4|Described|p177|||U.Cret.||||||
16826|Sherbrook Group|32898|6|Mentioned|Table 2-1|||||||||
16826|Sherbrook Group|33165|6|Mentioned|Chart|||Correlation chart only||||||
16826|Sherbrook Group|33320|5|Briefly described|p57|||Palynology & Strat.||||||
16826|Sherbrook Group|33940|6|Mentioned|p393|||U.Cret.||||||
16826|Sherbrook Group|34063|6|Mentioned|p3|||Table. U.Cret.||||||
16826|Sherbrook Group|34308|6|Mentioned|p175|||U.Cret.||||||
16826|Sherbrook Group|34611|6|Mentioned|p162|||Marine||||||
16826|Sherbrook Group|34987|5|Briefly described|p170|||||||||
16826|Sherbrook Group|35013|6|Mentioned|p393|||||||||
16826|Sherbrook Group|35066|6|Mentioned|p201|||||||||
16826|Sherbrook Group|35285|5|Briefly described|p414|||||||||
16826|Sherbrook Group|36913|6|Mentioned|Fig.4|||||||||
16826|Sherbrook Group|37065|6|Mentioned|p42|||||||||
16826|Sherbrook Group|37783|6|Mentioned|Fig.10|||||||||
16826|Sherbrook Group|38221|6|Mentioned|Fig.4|||Otway Basin||||||
16826|Sherbrook Group|38625|6|Mentioned|p271|||||||||
16826|Sherbrook Group|38717|5|Briefly described|p20|||||||||
16826|Sherbrook Group|39077|6|Mentioned|Table 2|||||||||
16826|Sherbrook Group|39211|6|Mentioned|Fig.45|||||||||
16826|Sherbrook Group|39315|6|Mentioned|Fig.7|||||||||
16826|Sherbrook Group|40003|5|Briefly described|p43|||See also Fig.10||||||
16826|Sherbrook Group|40560|6|Mentioned|p4|||||||||
16826|Sherbrook Group|40947|6|Mentioned|p3|||||||||
16826|Sherbrook Group|41016|5|Briefly described|Mention|||||||||
16826|Sherbrook Group|41171|6|Mentioned|p168|||||||||
16826|Sherbrook Group|41185|5|Briefly described|p175|||See also Fig.7a||||||
16826|Sherbrook Group|41269|5|Briefly described|p245|||||||||
16826|Sherbrook Group|41318|6|Mentioned|p191|||||||||
16826|Sherbrook Group|41487|5|Briefly described|p625|||||||||
16826|Sherbrook Group|41552|6|Mentioned|p459|||||||||
16826|Sherbrook Group|41642|6|Mentioned|p219|||||||||
16826|Sherbrook Group|41701|6|Mentioned|Map legend|late Campanian||||||||
16826|Sherbrook Group|41704|6|Mentioned|p100|||||||||
16826|Sherbrook Group|41706|5|Briefly described|p145|||||||||
16826|Sherbrook Group|41714|6|Mentioned|p301|||||||||
16826|Sherbrook Group|41726|5|Briefly described|p420|||||||||
16826|Sherbrook Group|41769|5|Briefly described|p12|||||||||
16826|Sherbrook Group|41797|5|Briefly described|p224|||||||||
16826|Sherbrook Group|41868|4|Described|p533|||||||||
16826|Sherbrook Group|41936|6|Mentioned|p75|||||||||
16826|Sherbrook Group|42075|5|Briefly described|Fig.13 P252|||||||||
16826|Sherbrook Group|42079|6|Mentioned|Fig.10 P272|||||||||
16826|Sherbrook Group|42152|6|Mentioned|p15|||||||||
16826|Sherbrook Group|42184|6|Mentioned|Fig.2 P348|||||||||
16826|Sherbrook Group|42318|6|Mentioned|p7|||||||||
16826|Sherbrook Group|42361|4|Described|p12, p18|||||||||
16826|Sherbrook Group|42524|5|Briefly described|Fig.3 P27|||||||||
16826|Sherbrook Group|42545|6|Mentioned|p4|||Otway Basin||||||
16826|Sherbrook Group|42555|5|Briefly described|284|||||||||
16826|Sherbrook Group|42599|5|Briefly described|Fig.3 P614|||||||||
16826|Sherbrook Group|42827|3|Fully described|p243|||see also Table 7.12||||||
16826|Sherbrook Group|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
16826|Sherbrook Group|43052|5|Briefly described|Fig.2.16|||||||||
16826|Sherbrook Group|43171|4|Described|2-8|Maastrichtian|Cenomanian|Of Otway Supergroup.||||||21-OCT-08
16826|Sherbrook Group|43195|5|Briefly described|Map Legend||Late Cretaceous|See also commentary on back of map.||||||
16826|Sherbrook Group|43208|5|Briefly described|map legend|Maastrichtian|Cenomanian|||||||
16826|Sherbrook Group|43219|5|Briefly described|Fig.3,p6.|Maastrichtian|Cenomanian|||||||
16826|Sherbrook Group|43590|4|Described|p12||Late Cretaceous|||||||
16826|Sherbrook Group|43660|6|Mentioned|Fig.6,p15||Late Cretaceous|||||||
16826|Sherbrook Group|43733|5|Briefly described|p9||Late Cretaceous|||||||
16826|Sherbrook Group|43744|6|Mentioned|Fig.3,p3|||||||||
16826|Sherbrook Group|43747|6|Mentioned|p5||Cenomanian|||||||
16826|Sherbrook Group|43783|6|Mentioned|Fig14, p11||Late Cretaceous|||||||
16826|Sherbrook Group|43784|4|Described|Fig10, p12, p29||Late Cretaceous|||||||
16826|Sherbrook Group|43814|6|Mentioned|Fig.3,p115|||||||||
16826|Sherbrook Group|43937|5|Briefly described|Map Legend|Santonian|Aptian|||||||
16826|Sherbrook Group|44133|5|Briefly described|p142, 94 Fig. 9.2, 146|Mesozoic|Cretaceous|Geological Province: Otway Basin. ||||||
16826|Sherbrook Group|44135|6|Mentioned|p49|||Geological province: Otway Basin. Mentioned in the context of correlates.||||||07-DEC-09
16826|Sherbrook Group|46802|6|Mentioned|Table 1|||||||||
16826|Sherbrook Group|46970|6|Mentioned|Fig.17|||||||||
16826|Sherbrook Group|48911|4|Described|p17|||Cret. Formations in group||||||
16826|Sherbrook Group|48977|5|Briefly described|p26|||See also p2 & Fig.5. Upper Cret.||||||27-AUG-18
16826|Sherbrook Group|49060|6|Mentioned|Fig.32|||||||||
16826|Sherbrook Group|60451|5|Briefly described|p95 Fig. 61|||||||||
16826|Sherbrook Group|60538|5|Briefly described|p474 Fig. 13|||Geological Province: Otway Basin.||||||
16826|Sherbrook Group|61017|5|Briefly described|p5|Maastrichtian|Turonian|Geological Province: Otway Basin.||||||07-FEB-11
16826|Sherbrook Group|61045|6|Mentioned|p93|Late Cretaceous|Late Cretaceous|||||||
16826|Sherbrook Group|61155|5|Briefly described|p18|||Includes the Timboon Sand Member. Unconformably overlain in part by Pebble Point Formation. Age is pre-Cainozoic. Geological Province: Otway Basin.||||||
16826|Sherbrook Group|61182|3|Fully described|p14, p35|Late Cretaceous|Late Cretaceous|Comprises Waarre and Flaxman Fms, Belfast Mudstone, Nullawarre Greensand and Paarratte Fm. Unconformable over Otway Group; unconformable beneath Wangerrip Gp. Max. thickness: 1790m. Age: 97-65Ma. Geol.Prov:Otway Basin. Included by some in Wangerrip Group.||||||
16826|Sherbrook Group|61230|5|Briefly described|p319, p329, p333, p337, p344.     |Late Cretaceous|Late Cretaceous|Of the Otway Delta. Hosts gas reserves. Deposition occurred in a variety of environments, from flood plain to upper slope.|||Includes Waarre, Flaxman, Belfast Mudstone and Paaratte Formations; Nullawarre Greensand; Skull Creek Mudstone and Timboon Sandstone.|||
16826|Sherbrook Group|61470|5|Briefly described|p28 Fig. 5|Maastrichtian|Turonian|Includes Flaxman Fm., Belfast Mudstone, Nullawarre Greensand, Skull Creek Mudstone, Paaratte Fm., Timboon Sandstone and Massacre Shale. Geological Province: Otway Basin.||||||12-OCT-05
16826|Sherbrook Group|61547|5|Briefly described|p461 Fig.2, p462. |Late Cretaceous|Late Cretaceous|Fluvio-deltaic deposition.|||Includes Timboon Sandstone, Paaratte Formation, Belfast Mudstone, Flaxman Formation and Shipwreck Subgroup.|Overlies Otway Supergroup. Is unconformably overlain by Wangerrip Group.|Frequent mudstone and massive sandstone units.|
16826|Sherbrook Group|61607|6|Mentioned|p5 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Otway Basin.||||||12-MAR-09
16826|Sherbrook Group|61608|6|Mentioned|p41 Fig. 5|||Refers to equivalent unit.||||||
16826|Sherbrook Group|61622|5|Briefly described|p436 Fig. 2, p438 Fig. 4|Cretaceous|Cretaceous|Includes; Copa, Flaxman and Paaratte Formations, Timboon and Waarre Sandstone and Belfast Mudstone. Geological Province: Otway Basin.||||||07-FEB-11
16826|Sherbrook Group|61623|5|Briefly described|p447, p452, p449 Fig. 4|Late Cretaceous|Late Cretaceous|Includes; Flaxman, Waarre and Paaratte Formations, Timboon Sandstone and Belfast Mudstone.Geological Province: Otway Basin.||||||
16826|Sherbrook Group|61624|6|Mentioned|p465|Cretaceous|Cretaceous|Geological Province: Otway Basin.||||||07-APR-09
16826|Sherbrook Group|61625|5|Briefly described|p475|Late Creatceous|Late Cretaceous|Includes Waarre Formation, Belfast Mudstone, Nullawarre Greensand, Paaratte Formation, Flaxman Formaion and Timboon Sandstone. Geological Province: Otway Basin.||||||07-FEB-11
16826|Sherbrook Group|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4, p488|Late Cretaceous|Late Cretaceous|Includes; Waarre, Flaxman and Paaratte Formations, Belfast Mudstone and Timboon Sandstone. Geological Province: Otway Basin.||||||
16826|Sherbrook Group|61627|5|Briefly described|p499, p500 Fig. 2|Late Cretaceous|Late Cretaceous|Includes Shipwreck Subgroup. Includes Paaratte Formation and Timboon Sandstone. Geological Province: Otway Basin.||||||07-FEB-11
16826|Sherbrook Group|61628|5|Briefly described|p507, p509 Fig. 3, p511, p512, p515|Late Cretaceous|Late Cretaceous|Includes; Waarre, flaxman and Paaratte Formations, Belfast Mudstone, Nullawarre Greensand and Timboon Sandstone. Geological Province: Otway Basin.||||||
16826|Sherbrook Group|62896|6|Mentioned|p88|Mesozoic|Mesozoic|||||||07-FEB-11
16826|Sherbrook Group|63122|5|Briefly described|p17 Fig. 4.3, p21, p41|Maastrichtian|Cenomanian|Includes the Copa, Flaxman and Paaratte Formations, Waarre and Timboon Sandstones and Belfast Mudstone. Geological Province: Otway Basin. ||||||
16826|Sherbrook Group|63124|3|Fully described|p47, p49 Fig. 5.2, p74-77|Late Cretaceous|Late Cretaceous|Includes Shipwreck Subgroup and Copa, Flaxman and Paaratte Formations, Waarre and Timboon Sandstones and Belfast Mudstone. Unconformable over Eumeralla Formation. Max. age: 97Ma. Max. thickness: 5000m. Geological Province: Otway Basin.||||||31-JAN-08
16826|Sherbrook Group|63125|5|Briefly described|p111|Early Paleocene|Late Cretaceous |Min. age: ~65Ma. Geological Province: Otway Basin||||||
16826|Sherbrook Group|63129|6|Mentioned|p137|||Geological Province: Otway Basin.||||||30-JAN-08
16826|Sherbrook Group|63130|5|Briefly described|p143|||Geological Province: Otway Basin. North of Tartwaup Hingeline this is a thin, condensed sandy sequence with poor hydrocarbon trapping potential. ||||||
16826|Sherbrook Group|63150|5|Briefly described|p96|Late Cretaceous|Late Cretaceous|Geological province: Otway Basin. Plant microfossils are abundant and diverse in claystone sections of this group and are only absent from sandstone lithologies.||||||
16826|Sherbrook Group|63173|5|Briefly described|p342 Fig. 9.2|Late Cretaceous|Late Cretaceous|Geological Province: Otway Basin, offshore.||||||07-FEB-11
16826|Sherbrook Group|63269|5|Briefly described|p603-605, p607, p609|Late Cretaceous|Late Cretaceous|Otway Basin. A thick, syn-rift siliciclastic succession.|||Waarre, Flaxman, Paaratte Formations; Belfast Mudstone; Nullawarre Greensand; Timboon Sandstone.|Unconformably overlies Otway Group. Is overlain unconformably by Wangerrip Group.||
16826|Sherbrook Group|63431|5|Briefly described|p677 Fig. 2|Maastrictian|Cenomanian|Includes the Shipwreck Subgroup, Flaxman Formation and Belfast Mudstone, Paaratte Formation and Timboon Sandstone. Overlain by Wangerrip Group. Geological Province: Penola Trough/Otway Basin.See also p680.||||||07-FEB-11
16826|Sherbrook Group|63740|6|Mentioned|p88|Mesozoic|Mesozoic|||||||07-FEB-11
16826|Sherbrook Group|64314|5|Briefly described|p504|Late Cretaceous|Late Cretaceous|Unconformably overlain by Wangerrip Group.||||||21-OCT-08
16826|Sherbrook Group|66245|5|Briefly described|p5, p6 Fig.5, p15, p30. |Late Cretaceous|Late Cretaceous|The authors call for subdivision of this unit; they split it into six depositional sequences. Deposited as the Otway Basin continued to widen. Provided necessary overburden to mature source intervals near the base of the Eumeralla Formation.|||Includes Waarre, Flaxman and Paaratte Formations, Belfast Mudstone, Nullawarre Greensand and Timboon Sandstone.|||
16826|Sherbrook Group|67061|5|Briefly described|p545, p546 Fig.3.|Maastrichtian|Turonian|Otway Basin. Equivalent to lower parts of Eastern View Group (Torquay Sub-basin).|||Includes Copa, Waarre, Flaxman and Paaratte Formations; Belfast and Skull Creek Mudstones; and Nullawarre Greensand.|||
16826|Sherbrook Group|67366|5|Briefly described|p101. |Late Cretaceous|Late Cretaceous|The primary reservoir unit in onshore gas fields of northeast Otway Basin.|||Includes Waarre, Flaxman, Belfast, Nullawarre and Paaratte Formations, Skull Creek Mudstone and Timboon Sandstone.|Unconformably overlies Otway Group. Is overlain unconformably by Wangerrip Group.||
16826|Sherbrook Group|67367|5|Briefly described|p130, p131 Fig.2, p133. |Late Cretaceous|Late Cretaceous|Non-marine to marine siliciclastics. Stratigraphic equivalent to Latrobe Group, offshore Gippsland Basin. Overall, the hydrocarbon source rock quality of this Group is fairly poor.|||Includes Waarre, Flaxman and Paaratte Formations, Belfast and Skull Creek Mudstones, Nullawarre Greensand, Timboon Sandstone and Wiridjil Gravels.|||
16826|Sherbrook Group|67541|6|Mentioned|p76 Fig.1|||||||||
16826|Sherbrook Group|69297|6|Mentioned|p79, p84, p98, p112, p116, p117|Maastrichtian|Cenomanian|Otway Basin. Is the primary reservoir facies in the offshore Otway Basin.  |||Includes the Copa Formation, Waarre Formation, Flaxman Formation, Belfast Mudstone, Paaratte Formation and the Timboon Sandstone. |Unconformably overlies the Otway Group. Overlain by the Wangerrip Group. ||
16826|Sherbrook Group|69651|5|Briefly described|p6, p10, p12, p26, p31-34, p38|Late Cretaceous|Late Cretaceous|Otway and Sorell Basins. Up to 5km of coastal plain, deltaic and inner shelf sediments. Minor amounts of free oil recorded in Cape Sorell 1 is evidence for an active Cretaceous petroleum system in the Strahan Sub-basin. Contains the primary reservoir facies in offshore Otway Basin. Modelling diagrams.|||Waarre, Flaxman, Paaratte Formations; Belfast Mudstone, Nullawarre Greensand, Timboon Sandstone.|Unconformably overlies Otway Group. Is overlain unconformably by Wangerrip Group.|Interbedded conglomeratic sandstone, sandstone, siltstone and claystone; the latter two dominating at depth.|17-JUN-20
16826|Sherbrook Group|69879|5|Briefly described|p418, p424|Maastrichtian|Maastrichtian|Strahan Sub-basin. Shown as Sherbrook Group equivalent. Offshore exploration well Cape Sorell 1.||||Underlies Wangerrip Group.|Quartzitic sandstone with basal conglomerate. Oil show. Mainly sandstone and shale with some coaly beds deposited in a paralic to coastal plain environment.|
16826|Sherbrook Group|70077|5|Briefly described|Nelson:Fig.2; p2.Regional:Fig.4;p7-8,p10|Late Cretaceous|Late Cretaceous|Otway Basin: Gambier Embayment and Voluta Trough. Distal equivalents in the Nelson Sub-basin may be petroleum sources of the Austral 3 Petroleum System.|||Copa, Waarre, Flaxman, Mount Salt, Paaratte Formations; Skull Creek and Belfast Mudstones; Nullawarre Greensand and Timboon Sandstone.|Overlies Otway Group. Is overlain by Wangerrip Group.||
16826|Sherbrook Group|70078|5|Briefly described|Northern: Fig.2; p2. Regional: Fig.4; p6|Late Cretaceous|Late Cretaceous|Gambier Embayment and Voluta Trough. Fluvio-deltaic to marine sediments equivalent to this unit in the Sorell Basin are potential oil and gas sources in the Basin. Contains potential structural traps (high-side fault traps and faulted anticlines).|||Copa, Waarre, Flaxman, Mount Salt, Paaratte Formations; Belfast Mudstone; Timboon Sandstone.|Overlies Otway Group. Is overlain by Wangerrip Group.||
16826|Sherbrook Group|70379|6|Mentioned|p723-727, p732|||Otway Basin.||||Overlies Eumeralla Formation. Is overlain by Wangerrip Group.||
16826|Sherbrook Group|71593|5|Briefly described|p51|Eocene|Cretaceous|||||||
16826|Sherbrook Group|72050|6|Mentioned|p237, 240 Fig.9, 242 Fig.13|Maastrichtian|Cenomanian|||||||
16826|Sherbrook Group|73356|6|Mentioned|p2, p15-16||||||||Fluvial, deltaic and shallow marine sediments.|
16826|Sherbrook Group|73357|6|Mentioned|p43, p45, p47|Maastrichtian|Turonian|Otway Basin.||||||
16826|Sherbrook Group|73383|4|Described|p2-4, p7 Tb.3.1, p10, p21, p27, p214|Maastrichtian|Cenomanian|Otway Basin. Equivalent to chemostratigraphic Sequence S5 containing generally lower Ti/Th values than other sequences in Otway Basin. Contains several occurrences of high Fe and P intervals, likely related to berthierine 'greensands'. See also p83.|||Waarre Formation, Flaxman Formation, Belfast Mudstone, Nullawarre Greensand, Skull Creek Mudstone, Paaratte Formation, Timboon Sandstone|Overlies Otway Group, Eumeralla Formation, underlies Wangerrip Group|Contains clastic units of sandstones, mudstones, siltstones and marine shales. Includes sandstone, quartz arenite based on geochemistry.|
16826|Sherbrook Group|73385|5|Briefly described|p3-6, p19, p20 Fig.5.4, p21-24|Maastrichtian|Cenomanian|Otway Basin. Deposited in a series of half-grabens and embayments. Sedimentary package of the Sherbrook group is much thinner in the Tyrendarra Embayment than in the Port Campbell Embayment. Sedimentary package thins significantly across the Mussel Platform, Prawn Platform and Bridgewater High, and thickens in the Shipwreck Trough.|||Waarre Formation, Flaxman Formation, Belfast Mudstone, Nullawarre Greensand, Skull Creek Mudstone, Paaratte Formation, Timboon Sandstone|Overlies Otway Group, Eumeralla Formation, underlies Wangerrip Group, Pebble Point Formation.|Sequence of fluvial, deltaic and shallow marine sediments.|
16826|Sherbrook Group|73386|4|Described|p1-2, p4-7, p10-12, iii, Attachment A1|Maastrichtian|Turonian|Otway Basin. Absent from northern margin of the basin, increases in thickness towards the south. Represents a shift from fluvial to marginal marine and lower coastal plain sandstones, mudstones and coals, deposited due to renewed extension. Contact with Otway Group is conformable or mildly disconformable in Late Cretaceous depocentres, unconformable where the Sherbrook Group wedges out against inversion structures. Top of the group is a major flooding surface, upper boundary marked by regional intra-Maastrichtian unconformity. Contains Phyllocladidites mawsonii to Lower Forcipites longes spore-pollen zones, and chemostratigraphic sequence S5 of Forbes et al. (2020).|||Timboon Sandstone, Paaratte Formation, Skull Creek Mudstone, Nullawarre Greensand, Belfast Mudstone, Flaxman Formation, Waarre Formation|Overlies Otway Group, Eumeralla Formation, unconformably underlies Wangerrip Group|Sandstones, mudstones and coals.|
16826|Sherbrook Group|73594|5|Briefly described|p2-5|Maastrichtian|Cenomanian|Otway Basin. Sedimentary fill of second phase of rifting. Reflects increasing marine influence. Angular unconformity with Eumeralla Formation in places of Cenomanian uplift such as the Otway Ranges.|||Waarre Formation, Flaxman Formation, Belfast Mudstone, Nullawarre Greensand, Skull Creek Mudstone, Paaratte Formation, Timboon Sandstone|Conformably overlies Eumeralla Formation, Otway Group. Underlies Wangerrip Group.|Includes a basal transgressive sequence of sandstones, mudstones and coals, overlain by silty mudstones and glauconitic sandstones.|
73297|Sherbrook Supersequence|63134|2|Defined|108-110|||||||||
73297|Sherbrook Supersequence|63269|5|Briefly described|p605, p607, p609|Late Cretaceous|Late Cretaceous|Otway Basin.||||Overlies Shipwreck Supersequence. Is overlain by Wangerrip Supersequence.||
73297|Sherbrook Supersequence|69297|5|Briefly described|p78, p80, p81, p83, p98, p110, p114-p116|Late Cretaceous|Late Cretaceous|Otway Basin. Coastal plain, deltaic and marine sediments up to 5km thick. ||||||
73297|Sherbrook Supersequence|69651|5|Briefly described|p2, p10, p12, p15, p17-21, p23, p27|Late Cretaceous|Late Cretaceous|See also p31-33, p36-40, p42-43, p45-47, p49-50. Otway Basin. Campanian to Maastrichtian age. Marginal marine to fluvial deltaic (regional regression) sediments. About 900m thick. Good oil and gas potential in the Strahan Sub-basin. An excellent offshore regional seal.||||Overlies Shipwreck Supersequence. Is overlain by Wangerrip Supersequence.|Coarse-grained sandstone, breccia-conglomerate sandy shale, sandy claystone and clayey sandstone.|
73297|Sherbrook Supersequence|70077|5|Briefly described|Nelson: p1. Regional: Fig.4; p4-7, p9|Late Cretaceous|Late Cretaceous|Otway Basin. Up to 5km thick, basinward-thickening progradational succession of coastal plain, deltaic and marine sediments.||||||
73297|Sherbrook Supersequence|70078|5|Briefly described|Regional: Fig.4; p3-4, p6|Late Cretaceous|Late Cretaceous|Hosts part of Austral 3 petroleum system. Fluvio-deltaic to marine environments.||||Overlies Shipwreck Supersequence. Is overlain by Wangerrip Supersequence.||
73297|Sherbrook Supersequence|70193|5|Briefly described|p283, p284 Fig 2|Thanetian|Albian|Geological province: Otway Basin. See also Sherbrook Group.|||Includes the Paaratte Formation.|||
73297|Sherbrook Supersequence|70880|5|Briefly described|p77, 83, 85|Maastrichtian|Campanian|Otway Basin.||||Overlies Shipwreck Supersequence. Is overlain by Wangerrip Supersequence.|Major deltaic deposition.|
73297|Sherbrook Supersequence|71266|5|Briefly described|p614 Fig.3, p615|Late Cretaceous|Late Cretaceous|Otway Basin. Deltaic deposits thicken southwards.||||Overlies Shipwreck Supersequence. Is overlain by Wangerrip Supersequence.||
37522|Shippen Gully Porphyry|61163|4|Described|p124, p37 Tb. 6.2|Late Devonian|Late Devonian|Small, nonmagnetic stock of garnet-bearing quartz-feldspar porphyry of granodiorite composition. Strongly porphyritic with phenocrysts of quartz, plagioclase, perthite orthoclase, biotite and garnet in a fine-grained granoblastic groundmass.||||||
37522|Shippen Gully Porphyry|61174|5|Briefly described|map legend|Late Devonian|Late Devonian|Quartz-feldspar porphyry: strongly porphyritic; phenocrysts of quartz, plagioclase, perthitic orthoclase, biotite and garnet in a fine-grained granoblastic groundmass of quartz, plagioclase and orthoclase; occasional cordierite. GSV map code: G192.||||||07-FEB-11
37522|Shippen Gully Porphyry|61175|5|Briefly described|map legend|Late Devonian|Late Devonian|Quartz-feldspar porphyry: strongly porphyritic; phenocrysts of quartz, plagioclase, perthitic orthoclase, biotite and garnet in a fine-grained granoblastic groundmass of quartz, plagioclase and orthoclase; occasional cordierite. GSV map code: G192.||||||
37522|Shippen Gully Porphyry|61176|5|Briefly described|map legend|Late Devonian|Late Devonian|Quartz-feldspar porphyry: strongly porphyritic; phenocrysts of quartz, plagioclase, perthitic orthoclase, biotite and garnet in a fine-grained granoblastic groundmass of quartz, plagioclase and orthoclase; occasional cordierite. GSV map code: G192.||||||
37522|Shippen Gully Porphyry|61177|5|Briefly described|map legend|Late Devonian|Late Devonian|Quartz-feldspar porphyry: strongly porphyritic; phenocrysts of quartz, plagioclase, perthitic orthoclase, biotite and garnet in a fine-grained granoblastic groundmass of quartz, plagioclase and orthoclase; occasional cordierite. GSV map code: G192.||||||
37522|Shippen Gully Porphyry|61178|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Tolmie Igneous Complex. Quartz-feldspar porphyry (S-type): nonmagnetic; no discernible gravity response; moderate total radioelement, K, Th and U. GSV map code: G192.||||||
37522|Shippen Gully Porphyry|68116|5|Briefly described|Appendix, Map 26.|Devonian|Devonian||||||Quartz-feldspar porphyry: strongly porphyritic; phenocrysts of quartz, plagioclase, perthitic orthoclase, biotite and garnet in a fine-grained granoblastic groundmass of quartz, plagioclase and orthoclase; occasional cordierite.|
73296|Shipwreck Supersequence|63134|2|Defined|104-108|||||||||
73296|Shipwreck Supersequence|63269|5|Briefly described|p605, p607, p609|Late Cretaceous|Late Cretaceous|Otway Basin.||||Overlies Eumeralla Supersequence. Is overlain by Sherbrook Supersequence.||
73296|Shipwreck Supersequence|69297|6|Mentioned|p78, p81, p83, p98, p110, p114-p116|Late Cretaceous|Late Cretaceous|Otway Basin. Fluvio-lacustrine, deltaic and marine sediments. |||Includes the Waarre and Flaxman Formations. |||
73296|Shipwreck Supersequence|69651|5|Briefly described|p2, p10, p12-19, p23, p26, p31-34,p36-40|Late Cretaceous|Late Cretaceous|See also p42-47, p49-50. Otway Basin. Turonian to Santonian age. Includes the economically important reservoirs of the Waarre and Flaxman Formations, and Thylacine Member (Belfast Mudstone). Over 1300m thick (at least locally). Fluvial to deltaic and marginal marine facies. An excellent offshore regional seal. Modelling diagrams.||||Overlies Eumeralla Supersequence. Is overlain by Sherbrook Supersequence.|Basal conglomerate; interbedded sandstone, siltstone and claystone.|
73296|Shipwreck Supersequence|70077|5|Briefly described|Nelson: p1. Regional: Fig.4; p4-7, p9-10|Late Cretaceous|Late Cretaceous|Otway Basin. Includes Sherbrook Group (Waarre and Flaxman Formations). Fluvio-lacustrine, deltaic and marine sediments. Sealed by Belfast Mudstone.||||||
73296|Shipwreck Supersequence|70078|5|Briefly described|Regional: Fig.4; p3-4, p6|Late Cretaceous|Late Cretaceous|Hosts part of Austral 3 petroleum system. Fluvio-deltaic to marine environments.||||Overlies Eumeralla Supersequence. Is overlain by Sherbrook Supersequence.||
73296|Shipwreck Supersequence|70880|5|Briefly described|p76-78, 81-82|Santonian|Turonian|Otway Basin. Comprises three seismically-defined stratal units (described).||||Unconformably overlies Eumeralla Supersequence. Is overlain by Sherbrook Supersequence.||
73296|Shipwreck Supersequence|71266|5|Briefly described|p614 Fig.3|Late Cretaceous|Late Cretaceous|Otway Basin. Thickens southwards.||||Unconformably overlies Eumeralla Supersequence. Is overlain by Sherbrook Supersequence.||
27895|Silvan Granodiorite|22885|5|Briefly described|map|||||||||
27895|Silvan Granodiorite|23269|5|Briefly described|p402, Fig14-3.3p405||Late Devonian|||||||
27895|Silvan Granodiorite|23309|5|Briefly described|p167|||G240 I-Type. Supersedes Silvan Granite||||||
27895|Silvan Granodiorite|33157|6|Mentioned|p42|||||||||
27895|Silvan Granodiorite|33598|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27895|Silvan Granodiorite|33599|4|Described|p10|||U.Dev.||||||
27895|Silvan Granodiorite|35277|5|Briefly described|p95|||||||||
27895|Silvan Granodiorite|41641|5|Briefly described|p165|||||||||
27895|Silvan Granodiorite|42827|5|Briefly described|p165|||||||||
27895|Silvan Granodiorite|44197|5|Briefly described|Map Legend||Late Devonian|G240 I-type.||||||
27895|Silvan Granodiorite|68116|5|Briefly described|Appendix, Map 42.|Late Devonian|Late Devonian||||||Biotite granodiorite porphyry.|
27895|Silvan Granodiorite|71180|4|Described|p185|||||||||
30344|Silver Flat Porphyries|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
30344|Silver Flat Porphyries|23309|5|Briefly described|p89, 100, 351|||||||||
30344|Silver Flat Porphyries|60503|4|Described|p170, p27|||Originally part of Mitta Mitta Rhyolite, probably related to Dartella Volcanics. Intrude the Mitta Mitta Rhyolite. The Lower Tableland Granite possible part of this group. Phenocrysts and glomerocrysts of feldspar and quartz in groundmass.||||||
30344|Silver Flat Porphyries|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Intrusive stocks: brown, red, grey, porphyritic with variable amounts of quartz and feldspar, fine recrystallised groundmass, commonly displays well developed columnar jointing.||||||
30344|Silver Flat Porphyries|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Intrusive stocks: brown, red, grey, porphyritic with variable amounts of quartz and feldspar, fine recrystallised groundmass, commonly displays well developed columnar jointing.||||||
30344|Silver Flat Porphyries|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Intrusive stocks: brown, red, grey, porphyritic with variable amounts of quartz and feldspar, fine recrystallised groundmass, commonly displays well developed columnar jointing.||||||
30344|Silver Flat Porphyries|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Intrusive stocks: brown, red, grey, porphyritic with variable amounts of quartz and feldspar, fine recrystallised groundmass, commonly displays well developed columnar jointing.||||||
30344|Silver Flat Porphyries|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Stocks: 438+/-6 Ma (U/Pb zircon); nonmagnetic to weakly magnetic; high K, moderate total count, low to moderate Th, U||||||
30344|Silver Flat Porphyries|68116|5|Briefly described|Appendix, Map 27.|Early Devonian|Ludlow||||||Feldspar-quartz porphyry: brown, red, grey; variable amounts of quartz and feldspar; fine recrystallised groundmass; commonly displays well developed columnar jointing.|
16896|Silverband Formation|13996|6|Mentioned|p149|Late Silurian|Late Silurian|Grampians. Contains turiniid thelodonts: biogeographic affinities mentioned.||||||
16896|Silverband Formation|23229|6|Mentioned|p25|||||||||
16896|Silverband Formation|23247|5|Briefly described|Fig12-1.1p182, 186, 188|Devonian||||||||
16896|Silverband Formation|23307|5|Briefly described|Map Legend|Silurian|Silurian|Of Grampians Group||||||
16896|Silverband Formation|23309|5|Briefly described|p79-83, 204-206, 382, Table 2.27|||Maximum Thickness: 750m.||||||
16896|Silverband Formation|23402|4|Described|p28, p25|Silurian|Silurian|Thickness: 300m.  Overlies the Red Man Bluff Subgroup. Geological Province: Adelaide Fold Belt.||||||24-NOV-08
16896|Silverband Formation|23522|5|Briefly described|p246|Middle Devonian|Early Devonian|Of Grampians Group.||||||
16896|Silverband Formation|24551|4|Described|p120, p122|||Of the Grampians Group. Appoximately 750m thick.||||||
16896|Silverband Formation|24581|5|Briefly described|p811|Late Silurian|Late Silurian|Of the Grampians Group. Overlies the Red Bluff Subgroup. Overlain by the Mount Difficult Subgroup. Geological Province: Kanmantoo Fold Belt.||||||
16896|Silverband Formation|32865|4|Described|p486|||Dev.-Carb.||||||
16896|Silverband Formation|33232|3|Fully described|p72|||||||||
16896|Silverband Formation|33238|6|Mentioned|p640|||||||||
16896|Silverband Formation|33732|5|Briefly described|Table III|||L.Carb.||||||
16896|Silverband Formation|39967|6|Mentioned|p33|||||||||
16896|Silverband Formation|41002|5|Briefly described|p183|||||||||
16896|Silverband Formation|41585|4|Described|p142|||||||||
16896|Silverband Formation|42745|5|Briefly described|p9|||||||||
16896|Silverband Formation|42827|4|Described|p142|||Of Grampians Group.||||||24-NOV-08
16896|Silverband Formation|43461|14|Not recorded|Table p625|Early Carboniferous|Late Devonian|||||||
16896|Silverband Formation|43547|14|Not recorded|Table p153,155||Frasnian|Part of Grampians Group||||||
16896|Silverband Formation|43846|5|Briefly described|11|Early Devonian|Late Silurian|Thickness about 900m||||||
16896|Silverband Formation|44929|5|Briefly described|Map Legend|Silurian|Ordovician|Between the Mount Difficulty Sub-Group and the Red Man Bluff Sub-Group.  Includes Wannon Sandstone and Glen Hills Sandstone Members.  Micaceous mudstone.||||||14-JUN-06
16896|Silverband Formation|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Includes the Wannon Sandstone and Glen Hills Sandstone Members. Micaceous mudstone, red with thin interbands of yellowish quartzo-micaceous sandstone.||||||13-JUN-06
16896|Silverband Formation|44932|5|Briefly described|Map Legend|Silurian|Ordovician|Between the Mount Difficulty Sub-Group and the Red Man Bluff Sub-Group.  Includes Wannon Sandstone and Glen Hills Sandstone Members.  Micaceous mudstone.||||||14-JUN-06
16896|Silverband Formation|44933|5|Briefly described|Map Legend|Silurian|Ordovician|Between the Mount Difficulty Sub-Group and the Red Man Bluff Sub-Group.  Includes Wannon Sandstone and Glen Hills Sandstone Members.  Micaceous mudstone.||||||14-JUN-06
16896|Silverband Formation|46053|14|Not recorded|p.445|||||||||
16896|Silverband Formation|48971|6|Mentioned|p41|||||||||
16896|Silverband Formation|50154|5|Briefly described|p112|Early Devonian|Late Silurian|Of the Grampians Group. Contains fossil fish assemblage of Late Silurian to Early Devonian age.||||||02-MAY-13
16896|Silverband Formation|60451|4|Described|p76, 80|Early Devonian|Ordovician|Of the Grampians Group. Maximum Thickness: 750m. Overlies: Red Man Bluff Subgroup. Underlies Mount Difficult Subgroup. Type section in text. Includes the Glen Hills & Wannon Sandstone Members. Overlies: Major Mitchell Sandstone. Underlies: Serra Sandstone||||||
16896|Silverband Formation|60456|5|Briefly described|Map Legend|Silurian|Ordovician|Micaceous mudstone: red, with thin interbeds of yellowish quartzo-micaceous sandstone; planar laminated; rippled surfaces, mudcracks and bioturbation.||||||
16896|Silverband Formation|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Micaceous mudstone: red, with thin interbeds of yellowish quartzo-micaceous sandstone; planar laminated; rippled surfaces, mudcracks and bioturbation.||||||
16896|Silverband Formation|60459|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Grampians Group. Marginal marine micaceous mudstone and lesser quartzo-micaceous sandstone.||||||29-SEP-04
16896|Silverband Formation|61183|3|Fully described|p28-29, p42, p30 Tb.2, p55|||Middle of Grampians Group. Includes members: Glen Hills and Wannon Sandstones. An intervening micaceous, red-bed mudstone package. Overlain by Serra Sandstone (Mt Difficult Subgroup) and Major Mitchell Sandstone. Max. thickness: 750m.||||||
16896|Silverband Formation|61749|5|Briefly described|p14|||Micaeous mudstone-dominated package. Overlies Red Man Bluff Subgroup, underlies Mount Difficult Subgroup. Thickness: 750m.||||||21-JAN-10
16896|Silverband Formation|61752|5|Briefly described|p10|||Separates Red Man Bluff Subgroup units from the Mount Difficult Subgroup units above. Thickness: 750m. Geological Province: Lachlan Fold Belt.||||||07-FEB-11
16896|Silverband Formation|64541|5|Briefly described|Map Legend|Silurian|Ordovician|Micaceous mudstone: red; with thin interbede of yellowish quartzo-micaceous sandstone; laminated; rippled surfaces, mudcracks and bioturbation; poorly outcropping.||||||07-FEB-11
16896|Silverband Formation|64610|5|Briefly described|Map legend|Silurian|Ordovician|Of the Grampians Gp.  Contains the Wannon Sandstone and Glen Hills Sandstone Members. Micaceous mudstone: red, with interbeds of yellowish quartz-micaceous sandstone; laminated, rippled surfaces, mudcracks and biotrubation; poorly outcropping.||||||12-NOV-08
16896|Silverband Formation|65313|5|Briefly described|p582, 580, p575 Fig. 4, p581 Fig. 9|Ludlovian|Wenlockian|Age based on fish denticles, spines, scales, paleosols. Lithology includes siltstone. Grampians National Park section.|ca. 427 Ma - 419 Ma.|||Overlies Major Mitchell Sandstone; underlies Serra Sandstone.||26-MAR-12
16896|Silverband Formation|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Grampians Group. Includes Glen Hills Sandstone Member and Wannon Sandstone Member. Defined by  Spencer-Jones, 1965. See also Cayley & Taylor, 1997. ||||||
16896|Silverband Formation|66498|6|Mentioned|p39, 41, 43|Ludlow|Ludlow|The dominant Silurian vertebrate is the endemic thelodont 'Turinia fuscina'.||||||
16896|Silverband Formation|68116|5|Briefly described|Appendix, Maps 22, 30, 39.|Ludlow|Ludlow||||||Micaceous mudstone: red, with thin interbeds of yellowish quartzo-micaceous sandstone; laminated; rippled surfaces, mudcracks and bioturbation; poorly outcropping; sparse fossil fauna of ostracods, brachiopods, and fish spines, teeth and scales.|
16896|Silverband Formation|68297|5|Briefly described|p175|Early Devonian|Late Silurian|Grampians, Vic. Includes turiniid agnathan scales (Turner 1986) previously identified by Talent (1963) as elasmobranch denticles. See also Silverband fauna discussion p181|Min age 400 Ma?|||Rocklands Rhyolite intrudes equivalent sediments in Black Range||
16896|Silverband Formation|70901|14|Not recorded|p7|||Refers to Talent and spencer-Jones, 1963.||||||
16896|Silverband Formation|71593|5|Briefly described|p47|||Marginal marine to fluvial depositional setting.|||||Mudstones.|
16918|Simmonds Gap Granite|23309|6|Mentioned|p433|||G150.||||||
16918|Simmonds Gap Granite|42791|5|Briefly described|p217|||see also Fig.3 p207.||||||10-JAN-07
16918|Simmonds Gap Granite|61160|3|Fully described|p86, p32 Tb. 5.2|Early Devonian|Early Devonian|I-type.Fine- to medium-grained, massive, pale grey leucocratic biotite granite varying from equigranular to porphyritic with phenocrysts of pink orthoclase.  Intrudes the Pinnak Sandstone. See also p20, p58-59 Fig. 6.8.||||||
16918|Simmonds Gap Granite|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite granite: grey to pinkish-grey; leucocratic; medium to fine grained; varies from equigranular to porphyritic with phenocrysts of pink orthoclase; I-type intrusion. GSV map code: G150.||||||
16918|Simmonds Gap Granite|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite granite: grey to pinkish-grey; leucocratic; medium to fine grained; varies from equigranular to porphyritic with phenocrysts of pink orthoclase; I-type intrusion. GSV map code: G150.||||||
16918|Simmonds Gap Granite|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite granite: grey to pinkish-grey; leucocratic; medium to fine grained; varies from equigranular to porphyritic with phenocrysts of pink orthoclase; I-type intrusion. GSV map code: G150.||||||
16918|Simmonds Gap Granite|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite granite: grey to pinkish-grey; leucocratic; medium to fine grained; varies from equigranular to porphyritic with phenocrysts of pink orthoclase; I-type intrusion. GSV map code: G150.||||||07-FEB-11
16918|Simmonds Gap Granite|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite granite: I-type; moderately magnetic (30 nT; kv = 0-40 x10^-6 cgs); low gravity (-510 to -450 ums ^-2); high total radioelement and K, low to moderate Th and U. GSV map code: G150.||||||
16918|Simmonds Gap Granite|68116|5|Briefly described|Appendix, Map 27.|Early Devonian|Early Devonian||||||Biotite granite: grey to pinkish-grey, leucocratic, medium- to fine-grained, varies from equigranular to porphyritic with phenocrysts of pink orthoclase; I-type.|
16928|Sinclair Valley Sandstone|22971|6|Mentioned|p 22|||Jordan River Group.||||||22-DEC-08
16928|Sinclair Valley Sandstone|23229|4|Described|Table3-3p27, 32|Ludlow|Ludlow|||||||
16928|Sinclair Valley Sandstone|23265|6|Mentioned|p341|||||||||
16928|Sinclair Valley Sandstone|23309|4|Described|p143,151, 152, 153, 155, Table 2.54|Ludlow|Ludlow|Of Jordan River Group.||||||
16928|Sinclair Valley Sandstone|24177|5|Briefly described|p50 Fig.22|Late Silurian|Late Silurian|Geological Province: Mount Easton Province.||||||
16928|Sinclair Valley Sandstone|24551|5|Briefly described|p128|Ludlow|Ludlow|||||||
16928|Sinclair Valley Sandstone|24588|5|Briefly described|p19-21, p12 Fig.3|Ludlow|Ludlow|Geological Province: Mount Easton Province. Of the Jordan River Group. See also p17, 26, 27, 28.||||||29-NOV-13
16928|Sinclair Valley Sandstone|33601|2|Defined|p8|Late Silurian|Late Silurian|||||||
16928|Sinclair Valley Sandstone|33607|6|Mentioned|Map legend|Silurian|Silurian|||||||
16928|Sinclair Valley Sandstone|35073|5|Briefly described|Table 1.|||See also P6.||||||
16928|Sinclair Valley Sandstone|35283|4|Described|p51|||||||||
16928|Sinclair Valley Sandstone|36389|6|Mentioned|p41|||||||||
16928|Sinclair Valley Sandstone|38787|6|Mentioned|Fig.2|||||||||
16928|Sinclair Valley Sandstone|39551|6|Mentioned|Map legend|Pridolian|Ludlovian|Pridolian to Ludlovian||||||
16928|Sinclair Valley Sandstone|39555|6|Mentioned|Map legend|Pridolian|Ludlovian|Pridolian to Ludlovian.||||||22-DEC-08
16928|Sinclair Valley Sandstone|41585|4|Described|p112|||||||||
16928|Sinclair Valley Sandstone|42827|5|Briefly described|p112|||Of Jordan River Group.||||||27-OCT-08
16928|Sinclair Valley Sandstone|44187|5|Briefly described|Map Legend||Late Silurian|||||||
16928|Sinclair Valley Sandstone|60599|5|Briefly described|p47 Fig. 19|Pridolian|Ludlow|Geological Province: Mount Easton Province, Melbourne Zone, Lachlan Fold Belt.||||||
16928|Sinclair Valley Sandstone|61185|5|Briefly described|p37, p21 Fig. 6|Pridolian|Ludlow|Of Jordan River Group (VandenBerg, 1975). Overlies Bullung Siltstone; underlies Whitelaw Siltstone. Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
16928|Sinclair Valley Sandstone|62099|5|Briefly described|p331|Late Silurian|Late Silurian|In eastern Melbourne Zone of the Lachlan Orogen. ||||||
16928|Sinclair Valley Sandstone|64535|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp.Sst+siltst.in variable proportion: thick to thin bedded sst;Tbc,Tabc,Tc turbidites, qtz-rich to micaceous, med.- to fine-gr; dk grey siltst., laminated/bioturbated, rare shale with Ludlow graptolites; deep marine turbidite fan deposits.||||||22-DEC-08
16928|Sinclair Valley Sandstone|64536|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp.Sst+siltst.in variable proportion: thick to thin bedded sst;Tbc,Tabc,Tc turbidites, qtz-rich to micaceous, med.- to fine-gr; dk grey siltst., laminated/bioturbated, rare shale with Ludlow graptolites; deep marine turbidite fan deposits.||||||07-FEB-11
16928|Sinclair Valley Sandstone|64537|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp.Sst+siltst.in variable proportion: thick to thin bedded sst;Tbc,Tabc,Tc turbidites, qtz-rich to micaceous, med.- to fine-gr; dk grey siltst., laminated/bioturbated, rare shale with Ludlow graptolites; deep marine turbidite fan deposits.||||||07-FEB-11
16928|Sinclair Valley Sandstone|64538|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp.Sst+siltst.in variable proportion: thick to thin bedded sst;Tbc,Tabc,Tc turbidites, qtz-rich to micaceous, med.- to fine-gr; dk grey siltst., laminated/bioturbated, rare shale with Ludlow graptolites; deep marine turbidite fan deposits.||||||07-FEB-11
16928|Sinclair Valley Sandstone|64539|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp.Sst+siltst.in variable proportion: thick to thin bedded sst;Tbc,Tabc,Tc turbidites, qtz-rich to micaceous, med.- to fine-gr; dk grey siltst., laminated/bioturbated, rare shale with Ludlow graptolites; deep marine turbidite fan deposits.||||||22-DEC-08
16928|Sinclair Valley Sandstone|64540|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Gp.Sst+siltst.in variable proportion: thick to thin bedded sst;Tbc,Tabc,Tc turbidites, qtz-rich to micaceous, med.- to fine-gr; dk grey siltst., laminated/bioturbated, rare shale with Ludlow graptolites; deep marine turbidite fan deposits.||||||22-DEC-08
16928|Sinclair Valley Sandstone|64605|5|Briefly described|Map legend|Silurian|Silurian|Of the Jordan River Group. Sandstone, siltstone; deep-marine deposits. Black to dark blueand light blue in RGB. Nonmagnetic.||||||17-NOV-08
16928|Sinclair Valley Sandstone|64606|5|Briefly described|Map Legend|Silurian|Silurian|Of Jordan River Group. Sandstone, siltstone: deep-marine deposits. Black to dark blue and light blue in RGB. Nonmagnetic.||||||11-NOV-08
16928|Sinclair Valley Sandstone|64616|3|Fully described|p85, p159, p163 Fig.6.9, p165, p173|Ludlow|Ludlow|See also p183 Fig.6.29, p197 Fig.6.34, p204, p247, p282-287, p293, p305. Of Jordan River Group. Conformably between underlying Bullung Siltstone and overlying Whitelaw Siltstone. Grey, medium- to fine-grained quartzose sandstone, locally with abundant small pyrite cubes; dark grey siltstone interbeds. 200-1300m thick (250m in type area). Age from graptolites in rare black shale beds. Hosts Golden Mountain gold deposit in the hornfels aureole of Strathbogie Granite. Geophysical characteristics given.||||||
16928|Sinclair Valley Sandstone|68116|5|Briefly described|Appendix, Maps 25, 33-34, 43, 52.|Gorstian|Homerian||||||Sandstone, siltstone in variable proportion: sandstone mid- to pale grey, thick to thin-bedded, turbidites, quartz-rich to micaceous, medium to fine-grained; siltstone generally dark grey, laminated and bioturbated; Ludlow graptolites in rare shale.|
34821|Sisters Granite|22968|5|Briefly described|P21, P222||Triassic|New name, intruded the Grand View Syenite and Percydale Granite, type locality location given of P222, highly magnetic||||||
34821|Sisters Granite|23029|5|Briefly described|Map legend|Triassic|Triassic|Parent is the Mount Leinster Igneous Complex||||||
34821|Sisters Granite|23030|5|Briefly described|Map legend|Triassic|Triassic|Parent is the Mount Leinster Igneous Complex||||||
34821|Sisters Granite|60503|6|Mentioned|p129|||Does not extend into BENAMBRA.||||||
34821|Sisters Granite|68116|5|Briefly described|Appendix, Map 35.|Triassic|Triassic|Informally subdivided into a syenite phase.|||||Biotite alkali granite, quartz syenite: cream; fine to medium-grained; rare small K-feldspar phenocrysts. Syenite: biotite-hornblende-quartz syenite: fine-grained; equigranular .|
26899|Skerries Granite|23309|6|Mentioned|p443 App1|||G10 I-Type.||||||
26899|Skerries Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
26899|Skerries Granite|68115|5|Briefly described|p6.|||On the geophysical interpretation map of Oranskaia (1997a), this magnetic unit is surrounded by the non-magnetic Wingan Granite pluton. The eponymous Skerries islands are non-magnetic, so the names of the plutons have been swapped.||||||
26899|Skerries Granite|68116|5|Briefly described|Appendix, Map 46.|Early Devonian|Early Devonian||||||Biotite granite, felsic: pink to grey; hornfels enclaves locally abundant; mostly non-magnetic.|
16984|Skull Creek Mudstone|12796|4|Described|p460, p456 Fig. 2|Maastrichtian|Campanian|Of Sherbrook Group. Originally member of Paarratte Fm. Now incorporates some younger mudstones. Interfingers with and overlain by Paarratte Fm. Geological Province: Otway Basin/Port Campbell Embayment.||||||
16984|Skull Creek Mudstone|22470|5|Briefly described|p13 Fig. 17|Campanian|Campanian|Of Sherbrook Group.||||||
16984|Skull Creek Mudstone|24551|6|Mentioned|p257 Fig. 9.25|||Of the Sherbrook Group.||||||14-APR-08
16984|Skull Creek Mudstone|41714|6|Mentioned|Fig.2|||||||||
16984|Skull Creek Mudstone|61017|5|Briefly described|p5 Fig. 2|Campanian|Campanian|Of the Sherbrook Group. Geological Province: Otway Basin. See also p6 Fig. 3.||||||07-FEB-11
16984|Skull Creek Mudstone|61182|6|Mentioned|p18|Late Cretaceous|Late Cretaceous|Of Buffin (1989). Superseded by Skull Creek Member. Geological Province: Otway Basin.||||||
16984|Skull Creek Mudstone|61230|6|Mentioned|p319 Fig.2, p344.|Campanian|Santonian|||Unit in Sherbrook Group.||||
16984|Skull Creek Mudstone|61470|5|Briefly described|p28 Fig. 5|Campanian|Campanian|Of the Sherbrook Group. Overlies Belfast Mudstone and Nullawarre Greensand; underlies Paaratte Formation (with which it also interfingers) and Timboon Sandstone. Geological Province: Otway Basin.||||||12-OCT-05
16984|Skull Creek Mudstone|67061|6|Mentioned|p546 Fig.3.|Late Cretaceous|Late Cretaceous|||Unit in Sherbrook Group.||||
16984|Skull Creek Mudstone|67366|5|Briefly described|p103 Fig.2. |Campanian|Campanian|||Unit in Sherbrook Group.||Overlies Belfast and Nullawarre Formations. Is overlain by Paaratte Formation and Timboon Sandstone.|Shelf to open marine shale.|
16984|Skull Creek Mudstone|67367|5|Briefly described|p131 Fig.2. |Campanian|Campanian|||Unit in Sherbrook Group.||||
16984|Skull Creek Mudstone|69297|5|Briefly described|p79, p98|Santonian|Santonian|Otway Basin. ||Sherbrook Group||Overlies the Nullawarre Greensand. Overlain by the Paaratte Formation. |Mudstone. |
16984|Skull Creek Mudstone|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Campanian|Campanian|Otway Basin: Port Campbell Embayment.||Sherbrook Group.||Overlies Nullawarre Greensand. Is overlain by Paaratte Formation and Timboon Sandstone.||
16984|Skull Creek Mudstone|70193|5|Briefly described|p284, p285 fig 3|Maastrichtian|Campanian|Geological province: Otway Basin. N. aceras dinocyst zone.  Part of the Sherbrook Supersequence.||||Overlain unconformably by Paaratte Formation.||
16984|Skull Creek Mudstone|73357|5|Briefly described|p21-22, p31, p45|Campanian|Santonian|Otway Basin. Skull Creek Mudstone/Paaratte Formation boundary is diachronous across central region. Lower part of unit correlated with Tricolpites apoxyexinus Spore-Pollen Zone, basal part correlated with the Isabelidinium cretaceum Dinocyst Zone. Upper part correlated with the nearshore marine Nelsoniella aceras Dinocyst Zone and Nothofagidites senectus Spore-Pollen Zone. Uppermost part correlated with the marginal to very nearshore marine Xenikoon australis Dinocyst Zone, early Campanian.||Of Sherbrook Group.||Overlies Belfast Mudstone, Nullawarre Greensand.|Includes fine-grained lithologies in uppermost part.|
16984|Skull Creek Mudstone|73383|5|Briefly described|p3, p11 Tb.3.9, p21-23, p27, p260-261|Campanian|Campanian|Otway Basin. Equivalent to chemostratigraphic package S5-P6 identified only in Penryn-1, characterised by intermediate Sm/U, Th/K and Th/Sc values between the overlying and underlying packages. Intervals are also included in package S5-P5 defined by high Fe and P values. Lithologies based on geochemistry using the ChemLith classification includes argillaceous sandstone, sandstone, limestone, mudstone; and using the Herron classification (1988) includes Fe-sand, wacke, sublith-arenite, Fe-shale. See also vi, p132-133.||Sherbrook Group||Overlies Nullawarre Greensand, underlies Paaratte Formation|Shelfal siltstones and marine shales, clay-rich.|
16984|Skull Creek Mudstone|73385|5|Briefly described|p5|Campanian|Campanian|Otway Basin.||Sherbrook Group||Overlies Nullawarre Greensand, underlies Paaratte Formation.|Shelfal siltstones and marine shales.|
16984|Skull Creek Mudstone|73386|4|Described|p4, p6, p10-11, Attachment A1|Campanian|Santonian|Otway Basin. Top of unit is diachronous across the central Otway Basin. Belongs to the Tricolporites apoxyexinus to Nothofagidites senectus spore-pollen zones, latest Santonian maximum age. Shallow marine shelf, prodeltaic depositional environment. Restricted to the Port Campbell and Tyrendarra embayments onshore, where it is relatively thin, interfingering with the Paaratte Formation.||Sherbrook Group||Conformably overlies Nullawarre Greensand, underlies and interfingers with Paaratte Formation|Pale grey to grey silty mudstone.|
16984|Skull Creek Mudstone|73594|5|Briefly described|p4-5, p27-28, p32, p35|Campanian|Campanian|Otway Basin. Unconformably overlies Eumeralla Formation at the crest of the Mussel Platform over an intra-Santonian unconformity.||Sherbrook Group||Unconformably overlies Belfast Mudstone and Waarre Formation locally on the Mussel Platform, underlies Paaratte Formation|Shelfal siltstones and marine shales.|
29836|Slater Ignimbrite|22968|4|Described|P66, P132, P133||Early Devonian|Several fault truncated lenses, parent is Mount Elizabeth Caldera Complex.||||||25-SEP-08
29836|Slater Ignimbrite|23021|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is Mount Elizabeth Caldera Complex.||||||25-SEP-08
29836|Slater Ignimbrite|23028|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is Mount Elizabeth Caldera Complex.||||||25-SEP-08
29836|Slater Ignimbrite|23309|5|Briefly described|p123 Table 2.46|||||||||
29836|Slater Ignimbrite|23938|6|Mentioned|p73 Fig. 26|||||||||
29836|Slater Ignimbrite|24551|5|Briefly described|p149|||Part of the Mount Elizabeth Cauldron Complex.||||||
29836|Slater Ignimbrite|43284|5|Briefly described|Map Legend||Early Devonian|Of Tara Range Subgroup.||||||25-SEP-08
29836|Slater Ignimbrite|60542|6|Mentioned|p67, p14|||Thin intercalation of red quartz ignimbrite in Mount Elizabeth caldera. Considered that perhaps this should be assigned to Tara Range Subgroup due to its composition which suggests it originated from the Waiwera Graben.||||||30-SEP-10
29836|Slater Ignimbrite|68116|5|Briefly described|Appendix, Maps 35, 44.|Early Devonian|Early Devonian||||||Quartz ignimbrite: purple-red with pink pumice, coarse-grained with up to 40% crystal content; contains biotite; densely welded throughout.|
75777|Sloan Knob Microgranite|68115|5|Briefly described|p7.|||Omeo Zone. New name, after Sloan Knob, where it crops out. The ring dyke for the Garden Creek Igneous Complex.|||||quartz-feldspar porphyry|20-FEB-13
75777|Sloan Knob Microgranite|68116|5|Briefly described|Appendix, Map 27.|Early Devonian|Early Devonian||||||Ring dyke: coarse quartz-feldspar porphyry with large euhedral crystals of quartz and feldspar and some biotite in a finer groundmass of the same minerals; glassy rhyolite with rare quartz phenocrysts.|
69402|Smokers Creek Volcanic Subgroup|64588|5|Briefly described|p25|||Alkalic rocks around Mount Macedon - distinct from tholeiitic basalts in the area, where use of 'igneous provinces'  nomenclature for naming volcanic rocks is considered. VandenBerg considers this unit would be eligible for elevation to full group status.||||||13-OCT-08
69402|Smokers Creek Volcanic Subgroup|64619|5|Briefly described|Map legend|Pliocene|Miocene|Of the Newer Volcanic Group. Comprises Yungaburra Formation and unnamed lavas - basanite, hawaiite, benmoreite, mugearite, and trachyte lavas.||||||
69402|Smokers Creek Volcanic Subgroup|65715|2|Defined|p18, p18 Tb.9, p103-108|Miocene|Miocene|Newly defined here. Of Newer Volcanic Group. Includes Yungabulla Formation. Alkaline and intermediate lavas and minor pyroclastic rocks of the region around the Macedon Ranges. Name derived from Smokers Creek. Includes trachyte, mugearite, icelandite, benmoreite, hawaiite and minor basanite. Erupted as domes that form prominent landscape features. Unconformably overlies Ordovician-Devonian bedrock, or disconformably on fluvial gravels. Overlain by Newer Volcanic Group.||||||10-FEB-15
69402|Smokers Creek Volcanic Subgroup|68116|5|Briefly described|Appendix, Maps 32, 41.|Pliocene|Miocene|Informally subdivided into benmorite lava, basanite lava, hawaiite lave, mugearite lava, and trachyte lava. See text for a detailed lithological description of these phases.||||||01-JUL-13
37241|Snake River Tonalite|24012|3|Fully described|p222 appendix 1|Ordovician|Cambrian|Intrudes Wando Tonalite.||||||
37241|Snake River Tonalite|50154|2|Defined|p75, p77, p248 App.5|Cambrian|Cambrian|Corresponds to part of Wells' (1956) Wando Granodiorite gneiss. Intruded by Brimboal Granodiorite.||||||15-SEP-04
37241|Snake River Tonalite|50156|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex. Hornblende-biotite tonalite||||||23-MAY-13
37241|Snake River Tonalite|50157|5|Briefly described|Map Legend|Late Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex. Hornblende-biotite tonalite||||||23-MAY-13
37241|Snake River Tonalite|50158|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex. Hornblende-biotite tonalite||||||23-MAY-13
37241|Snake River Tonalite|50159|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex. Hornblende-biotite tonalite||||||23-MAY-13
37241|Snake River Tonalite|50160|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex. Hornblende-biotite tonalite||||||23-MAY-13
37241|Snake River Tonalite|50161|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex. Hornblende-biotite tonalite||||||23-MAY-13
37241|Snake River Tonalite|50162|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex. Hornblende-biotite tonalite||||||23-MAY-13
37241|Snake River Tonalite|50163|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex. Hornblende-biotite tonalite||||||23-MAY-13
37241|Snake River Tonalite|50164|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Hornblende-biotite tonalite||||||
37241|Snake River Tonalite|66002|6|Mentioned|p9 Tb.5|||G437.  Defined by Kemp et al. 2002||||||
37241|Snake River Tonalite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Hornblende-biotite tonalite: foliated, grey, medium grained; porphyritic in hornblende; accessory magnetite, epidote, sphene and allanite. Numerous hornblende-rich mafic microgranitoid enclaves; magnetic.|
22856|Snake-Edwards Sandstone Member|23309|5|Briefly described|p151 Table 2.54||Ludlow|||||||
22856|Snake-Edwards Sandstone Member|24551|5|Briefly described|p128|||Of the Murderers Hill Sandstone.||||||
22856|Snake-Edwards Sandstone Member|64536|5|Briefly described|Map legend|Silurian|Silurian|Of Murderers Hill Siltstone (Jordan River Gp). Well bedded, thinly lam'inated siltstone; thinly bedded sst, med.- to coarse-gr., quartzose to lithic; rare black shale, thick bedded +rich Ludlow graptolite fauna. Deep-marine hemipelagic+trubidite deposits.||||||07-FEB-11
22856|Snake-Edwards Sandstone Member|64537|5|Briefly described|Map legend|Silurian|Silurian|Of Murderers Hill Siltstone (Jordan River Gp). Well bedded, thinly lam'inated siltstone; thinly bedded sst, med.- to coarse-gr., quartzose to lithic; rare black shale, thick bedded +rich Ludlow graptolite fauna. Deep-marine hemipelagic+trubidite deposits.||||||07-FEB-11
22856|Snake-Edwards Sandstone Member|64538|5|Briefly described|Map legend|Silurian|Silurian|Of Murderers Hill Siltstone (Jordan River Gp). Well bedded, thinly lam'inated siltstone; thinly bedded sst, med.- to coarse-gr., quartzose to lithic; rare black shale, thick bedded +rich Ludlow graptolite fauna. Deep-marine hemipelagic+trubidite deposits.||||||07-FEB-11
22856|Snake-Edwards Sandstone Member|64606|5|Briefly described|Map Legend|Silurian|Silurian|Of Murderers Hill Siltstone (Jordan River Group). Siltstone, sandstone, rare black shale: deep-marine deposits. Speckled green-blue-pink in RGB. Nonmagnetic.||||||12-NOV-08
22856|Snake-Edwards Sandstone Member|64616|4|Described|p79, p306|Ludlow|Ludlow|Of Murderers Hill Siltstone. ~220m thick. Graptolite fauna indicates Ludlow age. Siltstone interbedded with thin lithic sandstone and fine-grained quartz sandstone beds; black shale. Geophysical characteristics given.||||||
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.||||||
38819|Snowy Bluff Group|24053|5|Briefly described|p36|Early Carboniferous|Late Devonian|Geological Basin: Gippsland Basin.||||||
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
17054|Snowy Plains Formation|23309|5|Briefly described|p171-179|||||||||
17054|Snowy Plains Formation|23329|6|Mentioned|1048|||||||||
17054|Snowy Plains Formation|23710|14|Not recorded|p84|||Excursion.||||||
17054|Snowy Plains Formation|24551|5|Briefly described|p88 Fig. 3.15, 178, 635|Late Devonian|Late Devonian|Of Mansfield Group.  Maximum Thickness: >2400m.  ||||||
17054|Snowy Plains Formation|31706|6|Mentioned|p645|||Devonian correlation chart||||||
17054|Snowy Plains Formation|32865|4|Described|p485|Late Devonian|Early Carboniferous|See also p486.||||||28-FEB-08
17054|Snowy Plains Formation|33238|5|Briefly described|p644|||||||||
17054|Snowy Plains Formation|33602|6|Mentioned|p21|||||||||
17054|Snowy Plains Formation|33603|6|Mentioned|Map legend|Devonian|Devonian|||||||
17054|Snowy Plains Formation|33607|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
17054|Snowy Plains Formation|35073|6|Mentioned|p12|||See also Table 5.||||||
17054|Snowy Plains Formation|35112|6|Mentioned|p280|||||||||
17054|Snowy Plains Formation|35277|5|Briefly described|p102|||||||||
17054|Snowy Plains Formation|35281|6|Mentioned|p23|||||||||
17054|Snowy Plains Formation|37330|4|Described|p20|||||||||
17054|Snowy Plains Formation|38367|6|Mentioned|Table 3|||||||||
17054|Snowy Plains Formation|40761|5|Briefly described|p237|||||||||
17054|Snowy Plains Formation|40995|6|Mentioned|Fig.31|||||||||
17054|Snowy Plains Formation|41571|5|Briefly described|Fig.2.6|||||||||
17054|Snowy Plains Formation|41572|6|Mentioned|p13|||||||||
17054|Snowy Plains Formation|41641|4|Described|p172|||||||||
17054|Snowy Plains Formation|42089|5|Briefly described|p31|||||||||
17054|Snowy Plains Formation|42547|5|Briefly described|p58|||||||||
17054|Snowy Plains Formation|42797|5|Briefly described|Fig.3 P40|||||||||
17054|Snowy Plains Formation|42827|4|Described|p172|||Of the Avon River Group.||||||28-FEB-08
17054|Snowy Plains Formation|43461|14|Not recorded|Table p625|Early Carboniferous|Late Devonian|||||||
17054|Snowy Plains Formation|43547|14|Not recorded|Table p153||Famennian|||||||
17054|Snowy Plains Formation|44185|5|Briefly described|Map legend.|Late Devonian|Late Devonian|||Unit in Avon River Group.|||Fluvial: red mudstone, sandstone, conglomerate.|
17054|Snowy Plains Formation|44187|5|Briefly described|Map Legend||Late Devonian|||||||
17054|Snowy Plains Formation|61163|3|Fully described|p99, p36 Tb. 6.2|Late Devonian|Late Devonian|Of the Mansfield Group (Avon Supergroup). Floodplain fluvial sandstone and mudstone. Transitionally overlies Mount Kent Conglomerate. Thickness: >400m. Geological Province: Lachlan Fold Belt.||||||
17054|Snowy Plains Formation|61174|5|Briefly described|map legend|Late Devonian|Late Devonian|Of the Mansfield Group. Mudstone, sandstone: red mudstone generally poorly bedded, sandstone pale-coloured, quartz-rich; upward-fining with  minor conglomerate near base. GSV map code: Dams.||||||07-FEB-11
17054|Snowy Plains Formation|61175|5|Briefly described|map legend|Late Devonian|Late Devonian|Of the Mansfield Group. Mudstone, sandstone: red mudstone generally poorly bedded, sandstone pale-coloured, quartz-rich; upward-fining with  minor conglomerate near base. GSV map code: Dams.||||||
17054|Snowy Plains Formation|61176|5|Briefly described|map legend|Late Devonian|Late Devonian|Of the Mansfield Group. Mudstone, sandstone: red mudstone generally poorly bedded, sandstone pale-coloured, quartz-rich; upward-fining with  minor conglomerate near base. GSV map code: Dams.||||||
17054|Snowy Plains Formation|61177|5|Briefly described|map legend|Late Devonian|Late Devonian|Of the Mansfield Group. Mudstone, sandstone: red mudstone generally poorly bedded, sandstone pale-coloured, quartz-rich; upward-fining with  minor conglomerate near base. GSV map code: Dams.||||||
17054|Snowy Plains Formation|61178|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Mansfield Group. Mudstone, sandstone, conglomerate (fluvial): nonmagnetic, with moderately magnetic (~10 nT) strike parallel magnetic trends (probably dykes); low gravity (-530 ms^-2); very low total radioelement, K, Th and U. GSV map code: Dams.||||||
17054|Snowy Plains Formation|63738|5|Briefly described|p3|Early Carboniferous|Early Carboniferous|Of the Mansfield Group. Contains the Home Station Sandstone Member. Geological Province: Mansfield Basin.||||||11-MAR-08
17054|Snowy Plains Formation|64010|5|Briefly described|p257-273.     |Tournaisian|Tournaisian|||Of the Mansfield Group.|Includes Dungeon Gully, Home Station, Buttercup and Lanky Creek, Sandstone Members; Ashwin and Devil's Plain, Siltstone Members; Hearns Mudstone Member.|Overlies Mount Kent Conglomerate.||
17054|Snowy Plains Formation|64536|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Mansfield Group. Contains 7 named members, including 3 that are sandstone, 2 siltstone and 2 mudstone.||||||07-FEB-11
17054|Snowy Plains Formation|64537|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Mansfield Group. Contains 7 named members, including 3 that are sandstone, 2 siltstone and 2 mudstone.||||||07-FEB-11
17054|Snowy Plains Formation|64538|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of Mansfield Group. Contains 7 named members, including 3 that are sandstone, 2 siltstone and 2 mudstone.||||||07-FEB-11
17054|Snowy Plains Formation|64606|5|Briefly described|Map Legend|Quaternary|Early Carboniferous|Of Mansfield Group. Includes Devils Plain Siltstone Member, Hearns Mudstone Member, Lanky Creek Sandstone Member, Buttercup Mudstone Member, Horne Station Sandstone Member, Ashwin Siltstone Member and Dungeon Gully Sandstone Member.||||||12-NOV-08
17054|Snowy Plains Formation|64616|4|Described|p138, p253, p279, p299-300, p434-435|Early Carboniferous|Early Carboniferous|Of Mansfield Group. Overlies Mount Kent Conglomerate. Subdivided into 7 new Members: Devils Plain Siltstone (at top), then Hearns Mudstone, Lanky Creek Sandstone, Buttercup Mudstone, Home Station Sandstone, Ashwin Sandstone, Dungeon Gully Sandstone, Members. FT dating at 272 +/- 35 Ma. Hosts many small occurrences of low-grade Cu-U-V-Ag deposits, especially the Buttercup Mudstone Member. Geophysical characteristics given.||||||
17054|Snowy Plains Formation|66244|5|Briefly described|p6.|Late Devonian|Late Devonian|||||Is overlain unconformably by the Bryce Plain Basalt.||
17054|Snowy Plains Formation|66252|5|Briefly described|p211 Fig.1, p213 Fig.3, p214.|Early Carboniferous|Frasnian|See also p215-216 Figs.5-6, p222 Fig.8, p226-230. Thick (greater than 2.4km), widespread succession of purple sandstones and mudstones, the latter >75%. Meandering fluvial depositional environment. Gradationally overlies Mount Kent Conglomerate. Equivalent to Devils Plain Formation (Mansfield Basin). Youngest unit of the Macalister Synclinorium.||||||
17054|Snowy Plains Formation|66498|6|Mentioned|p46|||Spans the Devonian-Carboniferous boundary.|||Home Station Sandstone Member.|||
17054|Snowy Plains Formation|68116|5|Briefly described|Maps 25-26, 33-34, 43-44.||||||||Mudstone, sandstone; red mudstone generally poorly bedded; sandstone pale-coloured, quartz-rich, upward-fining with minor conglomerate near base.|
28138|Snowy River Volcanic Group|22487|6|Mentioned|p201|Early Devonian|Early Devonian|||||||
28138|Snowy River Volcanic Group|24551|3|Fully described|p140|Devonian|Devonian|Name used interchangeably with Snowy River Volcanics.||||||24-JUN-14
28138|Snowy River Volcanic Group|38145|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
28138|Snowy River Volcanic Group|39447|4|Described|p12|||||||||
28138|Snowy River Volcanic Group|40761|6|Mentioned|Fig.6|||||||||
28138|Snowy River Volcanic Group|68115|5|Briefly described|p4.|Devonian|Devonian||||Includes Deddick Rhyodacite, Wulgulmerang Volcaniclastics, Castor Oil Lava, Tara Range Subgroup and Ballantyne Megabreccia.|||
28138|Snowy River Volcanic Group|68116|5|Briefly described|Appendix, Maps 28, 35-36, 45.|Early Devonian|Early Devonian|Informally subdivided into porphyry and rhyolite phases. Feldspar-hornblende porphyry contains pyroxene and/or small amounts of quartz phenocrysts.|||||Volcanic lava, pyroclastics and epiclastics. Feldspar-hornblende porphyry, coarse-grained, dark bluish green (fresh). Rhyolite: vitric with sparse feldspar and/or quartz phenocrysts, in places flow-banded, spherulitic.|
28138|Snowy River Volcanic Group|71040|5|Briefly described|p8 Fig.5|||Wagga/Omeo and Buchan Zones. U-Pb zircon age for the base of the unit.|411 +/- 3 Ma (Morand and Fanning, 2009).|||||
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.|
83405|Social Bend pluton|73496|5|Briefly described|Map legend|Late Devonian|Late Devonian|G658.|||||Nonmagnetic but with magnetic contact aureole to 200 nT where interpreted to include mafic volcanic rocks, elsewhere to 20 nT;  gravity low to 30 micrometres/second/second below the regional.|
83405|Social Bend pluton|73497|5|Briefly described|Map legend|Late Devonian|Late Devonian|G658.|||||Nonmagnetic but with magnetic contact aureole to 200 nT where interpreted to include mafic volcanic rocks, elsewhere to 20 nT: gravity low to 30 micrometres/second/second below the regional.|
83405|Social Bend pluton|73505|5|Briefly described|p9, p19, p22, p30|Late Devonian|Devonian|Newly named unit in Swan Hill and parts of Balranald and Deniliquin 1:250 000 map areas, (G658). Named after Social Bend, locality on the Murray River. Situated in hangingwall of the Governor Fault system, appears to postdate the fault, and stitches the Governor Fault west of the Pericoota pluton. Intrudes the Pericoota pluton. Nonmagnetic, has contact metamorphosed mafic volcanic rocks. Gravity response of a 20 micrometres/second/second low. Intersected in Murrabit West 1.|||||Granite.|
17096|Somerton granite|34992|6|Mentioned|p406|||||||||
78972|Speculation Ignimbrite|66252|6|Mentioned|p216 Fig.6.|||Overlies Cobbler Rhyolite and is overlain by Snowy Plains Formation and Bindaree Formation.||||||
29013|Speewa Member|24551|6|Mentioned|p341|||||||||
29013|Speewa Member|29898|6|Mentioned|p218|||||||||
29013|Speewa Member|35272|6|Mentioned|p286|||||||||
29013|Speewa Member|41848|5|Briefly described|p361|||Member of Woorinen Formation. Age 24000 +- 900 yrs||||||
29013|Speewa Member|42264|6|Mentioned|Fig.5 P12|||||||||
29013|Speewa Member|42827|5|Briefly described|Table 9.1|||of Woorinen Formation||||||
29013|Speewa Member|42966|2|Defined|Table 35 p236|Late Pleistocene||of Woorinen Formation||||||
29013|Speewa Member|44133|6|Mentioned|p253|Holocene|Middle Pleistocene|Of the Woorinen Formation. Geological Province: Murray Basin.||||||
29013|Speewa Member|70961|6|Mentioned|p138|||Stratigraphic sequence.||||||
30589|Spion Kopje Quartz Diorite|23309|5|Briefly described|p433 App1|Devonian|Silurian|G151 I-Type. Age: 403+/-16Ma, 406+/-16Ma, 398+/-16Ma. Supersedes Spion Kopje Granodiorite.||||||
30589|Spion Kopje Quartz Diorite|43220|5|Briefly described|p11||Devonian|||||||
30589|Spion Kopje Quartz Diorite|44184|5|Briefly described|Map Legend||Early Devonian|Shown as Spion Kopje I-type.||||||
24499|Split Hill Sandstone|23309|5|Briefly described|p42 Fig. 2.14|||||||||
24499|Split Hill Sandstone|40136|5|Briefly described|p40|||||||||
24499|Split Hill Sandstone|41050|6|Mentioned|p51|||||||||
24499|Split Hill Sandstone|41570|4|Described|p85|||||||||
24499|Split Hill Sandstone|42560|6|Mentioned|p51|||||||||
24499|Split Hill Sandstone|42628|5|Briefly described|Map legend|Lancefieldian||||||||
24499|Split Hill Sandstone|42790|5|Briefly described|Fig.14 P189|||||||||
24499|Split Hill Sandstone|42826|2|Defined|p27|Early Ordovician||Of Romsey Group.||||||03-FEB-09
24499|Split Hill Sandstone|42827|5|Briefly described|p85|||Of Romsey Group.||||||03-FEB-09
24499|Split Hill Sandstone|64612|6|Mentioned|p37|||Overlies Stauro Gully Shale.||||||07-FEB-11
24499|Split Hill Sandstone|65715|5|Briefly described|p4 Tb.2|Ordovician|Ordovician|Of Romsey Subgroup. Formation rank.||||||
24499|Split Hill Sandstone|68116|5|Briefly described|Appendix.|Floian|Tremadocian|Age written as Lancefieldian in text.|||||Sandstone, siltstone, shale, chert.|
30543|Spring Creek Sandstone Member|23615|4|Described|p215 App.1, p221 App.1|||See also Spring Creek Member.||||||
30543|Spring Creek Sandstone Member|23938|5|Briefly described|p37|||Of the Buchan Caves Limestone. See also Spring Creek Member - names used interchangeably.||||||25-SEP-08
30543|Spring Creek Sandstone Member|43206|5|Briefly described|map legend|Pragian|Pragian|Of Buchan Caves Limestone.||||||25-SEP-08
30543|Spring Creek Sandstone Member|60542|6|Mentioned|p40, p41|||Of the Buchan Group. ||||||
73175|Spring Hill Complex|61896|5|Briefly described|p68-69|Pliocene|Pliocene|Age: ~4.35Ma.||||||19-DEC-07
26146|Springfield Sandstone|22511|4|Described|p659, p661||Silurian|||||||
26146|Springfield Sandstone|22684|4|Described|p748, Fig.2 p746|Llandovery|Llandovery|See also Fig.5 p749, p754||||||
26146|Springfield Sandstone|22886|4|Described|p12|Wenlock|Llandovery|||||||
26146|Springfield Sandstone|23229|4|Described|Table3-2p21, 27|Llandovery|Llandovery|Various names including: Wapentake Formation at Heathcote; lowest part in Andersons Creek Formation at Warrandyte.||||||
26146|Springfield Sandstone|23272|5|Briefly described|p414, Fig14-4.1p415, 427-9||Early Silurian|||||||
26146|Springfield Sandstone|23309|5|Briefly described|p134, 137-139, 150-155, 382, Table 2.50||Telychian|Parent: Murrundindi Supergroup.||||||27-OCT-08
26146|Springfield Sandstone|24177|5|Briefly described|p50 Fig.22|Llandovery|Llandovery|Geological Province: Darraweit Guim Province.||||||
26146|Springfield Sandstone|24551|5|Briefly described|p123|||||||||
26146|Springfield Sandstone|24588|5|Briefly described|p18-19, p12 Fig.3|Wenlock|Llandovery|Geological Province: Darraweit Guim Province.  Described as Late Llandovery p13, shown as Wenlock Fig. 3. Age constrained by graptolites. End-Aeronian sedgwickii Biozone. Absolute age uncertain. Overlies Deep Creek Siltstone.See also p13, 15, 21, 27, 28, 29||||||29-NOV-13
26146|Springfield Sandstone|41570|6|Mentioned|p83|||||||||
26146|Springfield Sandstone|41585|6|Mentioned|p105|||||||||
26146|Springfield Sandstone|42628|5|Briefly described|Map legend|Wenlock||||||||
26146|Springfield Sandstone|42790|5|Briefly described|Fig.14 P189|||||||||
26146|Springfield Sandstone|42826|2|Defined|p38|Early Silurian||||||||
26146|Springfield Sandstone|42827|5|Briefly described|Table 4.1|||||||||
26146|Springfield Sandstone|44197|6|Mentioned|Map Legend||Early Silurian|||||||
26146|Springfield Sandstone|60599|5|Briefly described|p13, p47 Fig. 19|Llandovery|Llandovery|Geological Province: Darraweit Guim Province, Melbourne Zone, Lachlan Fold Belt.||||||
26146|Springfield Sandstone|61185|5|Briefly described|p13, p21 Fig. 6|Ludlow|Llandovery|Turbidites. Overlies Deep Creek Siltstone; underlies Chintin Formation. Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
26146|Springfield Sandstone|62469|5|Briefly described|p5 Fig. 2, p45, p20|Llandovery|Llandovery|Underlies Chintin Formation. Contains biozone graptolites. Geological Province: Darraweit Guim Province. See also p20 Fig. 11.||||||12-FEB-15
26146|Springfield Sandstone|64611|5|Briefly described|Map legend|Llandovery|Llandovery|Of Murrindindi Supergroup. Sandstone, siltstone and conglomerate: medium to thick bedded, lithic quartz sandstone alternating with grey-green shaly siltstone+thin bedded sst; variably bioturbated; occasional graptolites. Deep-marine turbidite fan deposits||||||
26146|Springfield Sandstone|64612|2|Defined|p37-38|Late Landovery|Late Llandovery|Of Murrindindi Supergroup. Underlain conformably by Deep Creek Siltstone, overlain conformably by Chintin Formation. Equivalent to Wapentake Formation. Thickness: 980m. Packages of medium to thick-bedded lithic quartz sandstone interbedded with siltstone.||||||24-JUN-14
26146|Springfield Sandstone|66769|6|Mentioned|118|Silurian|Silurian|Sedimentation into Melbourne Zone from a proximal western source.||||||
26146|Springfield Sandstone|68116|5|Briefly described|Appendix, Maps 32, 41.|Telychian|Rhuddanian||||||Sandstone, siltstone and conglomerate: medium to thick bedded, lithic quartz sandstone alternating with grey-green shaly siltstone and thin-bedded sandstone; variably bioturbated, occasional graptolites; deep-marine turbidite fan deposits.|
17238|Staggs Creek Granite|23309|6|Mentioned|p448 App1|||Obsolete granite name.||||||
17238|Staggs Creek Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
68447|Staircase Ignimbrite|24551|4|Described|p174|||Of the Rose River Volcanics. Overlies Cobbler Rhyolite. Maximum Thickness: 250m.||||||25-JAN-07
68447|Staircase Ignimbrite|66252|2|Defined|p211 Fig.1, p215 Fig.5, p219, p228, p231|Frasnian|Frasnian|Definition data given. Upper Member of Rose River Volcanics, along NW margins of Macalister Synclinorium. Irregularly columnar jointed rhyolitic and minor rhyodacitic ignimbrites, tuff, red mudstone. Thickness to 250m. Conformably overlies Cobbler Rhyolite. Detailed stratigraphic section. Geochemistry detailed.||||||
17266|Stanley Granite|30906|6|Mentioned|Map legend|Devonian|Devonian|||||||
17266|Stanley Granite|31800|6|Mentioned|p206|||||||||
17266|Stanley Granite|70910|14|Not recorded|p44|||Geological map on opposite page.||||||
22890|Statham Ignimbrite|23309|4|Described|p110 Table 2.40|||Maximum Thickness: 1700m.  Of the Marroo Subgroup.||||||
22890|Statham Ignimbrite|23615|3|Fully described|p98-99, p23. 41, 86, 88, 89, 93, 94|Early Devonian|Early Devonian|Of Marroo Subgp.  Overlain by Scorpion Cr. Sst. and Glen Shiel Ignim; overlies Wombargo Subgp. in the north; in the west rests on Nunniong Granodiorite.  Interfingers with Timbarra Gp. in SW.  Thickness in type section: 1600-1700m (est.).  Age: 410-395Ma. Shown as Mount Statham Ignimbrite p62.||||||10-SEP-18
22890|Statham Ignimbrite|43206|5|Briefly described|map legend||Ludlow|Of Marroo Subgroup||||||
22890|Statham Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Quartz-feldspar ignimbrite with large phenocrysts and red pumice fragments: abundant lithic clasts near the base; minor sandstone, siltstone, breccia, feldspar ignimbrite.|
24504|Stauro Gully Shale|23309|5|Briefly described|p42, 55, Table 2.16, Fig. 2.14|Early Ordovician|Early Ordovician|Of Romsey Subgroup.||||||
24504|Stauro Gully Shale|24551|5|Briefly described|p108|||||||||
24504|Stauro Gully Shale|40136|5|Briefly described|p40|||Mention P68||||||
24504|Stauro Gully Shale|41050|6|Mentioned|p51|||||||||
24504|Stauro Gully Shale|41570|4|Described|p85|||||||||
24504|Stauro Gully Shale|42560|6|Mentioned|p51|||||||||
24504|Stauro Gully Shale|42628|5|Briefly described|Map legend|Lancefieldian||||||||
24504|Stauro Gully Shale|42790|5|Briefly described|Fig.14 P189|||||||||
24504|Stauro Gully Shale|42826|2|Defined|p27|Early Ordovician||Of Romsey Group.||||||03-FEB-09
24504|Stauro Gully Shale|42827|5|Briefly described|p85|||of Romsey Group||||||
24504|Stauro Gully Shale|64611|5|Briefly described|Map legend|Lancefieldian|Lancefieldian|Of the Romsey Subgroup (Castlemaine Group). Shale and siltstone; black, siliceous cherty shale, often with visible pyrite; contains graptolites, phyllocarid crustacea and arthropods; deep marine hemipelagic deposits.||||||16-DEC-08
24504|Stauro Gully Shale|64612|2|Defined|p33, p37, p73|Ordovician|Lancefieldian|Of Romsey Subgroup. Overlies Goldie Chert and Lano Gully Sandstone (conformably). Overlain by Castlemaine Group and Split Hill Sandstone (conformably). Thickness: 35m. Consists of black siliceous to cherty shale. Graptolites.||||||07-FEB-11
24504|Stauro Gully Shale|65715|5|Briefly described|p4 Tb.2|Ordovician|Ordovician|Of Romsey Subgroup. Formation rank.||||||
24504|Stauro Gully Shale|68116|5|Briefly described|Appendix, Map 32.|Floian|Tremadocian|Age written as Lancefieldian in text.|||||Sandstone, siltstone, shale, chert.|
17308|Stawell Granite|22710|6|Mentioned|p183|||||||||
17308|Stawell Granite|23105|5|Briefly described|p537|||||||||
17308|Stawell Granite|23110|5|Briefly described|p498|||Age:~395Ma.||||||
17308|Stawell Granite|23203|6|Mentioned|Fig.1|||||||||
17308|Stawell Granite|23309|5|Briefly described|p64, 65, 229-231, 238, 239, 341|Early Devonian|Early Devonian|G379. I-Type  Age: 396+/-5Ma, 399+/-3Ma. Supersedes Stawell Granodiorite and Sisters Rocks Adamellite.||||||
17308|Stawell Granite|23810|5|Briefly described|p888||Devonian|400+/-2 Ma emplacement age. Lachlan Fold Belt.||||||
17308|Stawell Granite|23814|5|Briefly described|p744|Early Devonian|Early Devonian|Geological Province: Stawell Zone.||||||
17308|Stawell Granite|23857|5|Briefly described|p903 Fig 2a.|||||||||
17308|Stawell Granite|24087|5|Briefly described|p329|Devonian|Devonian|Age: 399 +/- 4Ma (Ar/Ar).   Geological Province: Lachlan Fold Belt.||||||
17308|Stawell Granite|24100|6|Mentioned|p95|||Geological Province: Lachlan Fold Belt.||||||19-APR-05
17308|Stawell Granite|24551|6|Mentioned|p58, 717 Table 2.4|Early Devonian|Early Devonian|Age: 402 +/- 2Ma, 407 +/- 2Ma.||||||
17308|Stawell Granite|34990|6|Mentioned|p438|||||||||
17308|Stawell Granite|40761|6|Mentioned|p245|||||||||
17308|Stawell Granite|41572|6|Mentioned|p7|||||||||
17308|Stawell Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
17308|Stawell Granite|42745|5|Briefly described|p18|||||||||
17308|Stawell Granite|42827|5|Briefly described|p7|||||||||
17308|Stawell Granite|43627|6|Mentioned|p12|||||||||
17308|Stawell Granite|50546|5|Briefly described|p1232 Fig.1c, p1234 Fig. 2b|||Of Stawell Pluton||||||
17308|Stawell Granite|60451|4|Described|p52, 59, 90, 147|||Of the Stawell Pluton. Type section in text. Medium to coarse grained, pale cream coloured. Some xenoliths, areas of weak foliation.||||||
17308|Stawell Granite|60457|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Ararat Suite. Hornblende-biotite granite: pale; medium to coarse grained; occasional diorite, granodiorite and hornfels xenoliths; weekly foliated, oxidised, I-type.||||||
17308|Stawell Granite|60458|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Hornblende-biotite granite; pale, medium to coarse grained, occasional diorite, granodiorite and hornfels xenoliths; weakly foliated; oxidised.||||||
17308|Stawell Granite|60459|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Ararat Suite. Hornblende-biotite granite: oxidised, I-Type.||||||
17308|Stawell Granite|61146|5|Briefly described|p387 Fig.2, p394. |Early Devonian|Early Devonian|Its contact aureole hosts the Wonga gold deposit.|c.400 Ma.|||||
17308|Stawell Granite|61187|5|Briefly described|p82, p83 Fig.1.|||High-K radiometric response.||||Intrudes and contact metamorphoses Carrolls Amphibolite.||
17308|Stawell Granite|61410|5|Briefly described|p9, p11, p13, p15-17, p35-37    |Early Devonian|Early Devonian|Also appears as Stawell granite. Associated with the Wonga (gold) lode. Numerous other age determinations given.|413 +/- 3 Ma SHRIMP U-Pb (Arne et al., 1996).|||Intrudes the Wonga Schist.|Composite granite body composed of a central portion of granodiorite and a marginal diorite phase. Considered to be a high-level I-type granite.|
17308|Stawell Granite|61750|5|Briefly described|p20|||Classified by Chappell et al (1991) as an unfractionated, felsic I-type.||||||
17308|Stawell Granite|62751|6|Mentioned|p759|||Emplaced at ca 401Ma.||||||22-JAN-07
17308|Stawell Granite|62752|5|Briefly described|p759|||Emplaced at ca 401 Ma. At Stawell.||||||
17308|Stawell Granite|63599|6|Mentioned|p976 Fig. 1|||Geological Province: Stawell Zone.||||||10-DEC-07
17308|Stawell Granite|66002|5|Briefly described|p7 Tb.5|||Of Ararat Suite in Stawell Pluton area. G379. Defined by Cayley and Taylor 2001.||||||
17308|Stawell Granite|67806|6|Mentioned|pp110-111|Devonian|Devonian|Associated with gold mineralisation at Fosterville and the Wonga deposit. Weakly- to non-magnetic. Mis-spelt as Stawall Granite on p110.||||||
17308|Stawell Granite|67978|5|Briefly described|p496 Fig.1|Eifelian|Emsian|Geochronology by Black (unpublished data); Geoscience Australia database.|399 +/- 6 Ma, U-Pb|||||
17308|Stawell Granite|68116|5|Briefly described|Appendix, Map 30.|Early Devonian|Early Devonian||||||Hornblende-biotite granite: pale; medium to coarse grained; occasional diorite, granodiorite and hornfels xenoliths; weakly foliated; oxidised, I-type, moderately magnetic.|
17308|Stawell Granite|68194|6|Mentioned|p11, p15, p25|||Erosion has produced feldspathic quartzose sediments which give K-rich radiometric images.||||||
17308|Stawell Granite|70268|6|Mentioned|p256|||K-Ar age determination by Richards and Singleton (1981).|396 +/- 5 Ma (K-Ar biotite).|||||
17308|Stawell Granite|71040|6|Mentioned|p15|Early Devonian|Early Devonian|Pre-dates the Tabberabberan Orogeny.||||||
17308|Stawell Granite|71593|5|Briefly described|p148|Early Devonian|Early Devonian|Hosts the Wonga gold deposit.||||||
41181|Steep Bank Greywacke Member|50154|2|Defined|p52, p63, p249 App.5|Cambrian|Cambrian|Of the Nangeela Formation. Geological Province: Delamerian Fold Belt.||||||15-SEP-04
41181|Steep Bank Greywacke Member|50156|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Nangeela Formation. Greywacke and sandstone; quartzose, feldspar-lithic and quartz-feldspar-lithic types.||||||
41181|Steep Bank Greywacke Member|50157|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Nangeela Formation. Greywacke and sandstone; quartzose, feldspar-lithic and quartz-feldspar-lithic types; graded beds up to 30 cm thick.||||||24-JUN-04
41181|Steep Bank Greywacke Member|50158|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Nangeela Formation. Greywacke and sandstone; quartzose, feldspar-lithic and quartz-feldspar-lithic types.||||||
41181|Steep Bank Greywacke Member|50159|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Nangeela Formation. Greywacke and sandstone; quartzose, feldspar-lithic and quartz-feldspar-lithic types.||||||22-JUN-04
41181|Steep Bank Greywacke Member|50160|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Nangeela Formation. Greywacke and sandstone||||||
41181|Steep Bank Greywacke Member|50161|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Nangeela Formation. Greywacke and sandstone; quartzose, feldspar-lithic and quartz-feldspar-lithic types.||||||
41181|Steep Bank Greywacke Member|50162|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Nangeela Formation. Greywacke and sandstone||||||
41181|Steep Bank Greywacke Member|50163|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Nangeela Formation. Greywacke and sandstone; quartzose, feldspar-lithic and quartz-feldspar-lithic types.||||||
41181|Steep Bank Greywacke Member|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Nangeela Formation. Defined  by Morand et al. 2003||||||
41181|Steep Bank Greywacke Member|71593|6|Mentioned|p20, p150|||Glenelg Zone. May correlate with the lower Kanmantoo Group.||Nangeela Formation||||
23993|Stockdale Conglomerate Member|22684|5|Briefly described|Fig.2 p746|Llandovery|Llandovery|See also Fig.5 p749||||||
23993|Stockdale Conglomerate Member|23309|5|Briefly described|p138, 139. Table 2.50|||||||||
23993|Stockdale Conglomerate Member|24551|6|Mentioned|p126 Fig. 5.10|||Of the Springfield Sandstone?||||||
23993|Stockdale Conglomerate Member|41585|5|Briefly described|p105|||||||||
23993|Stockdale Conglomerate Member|42628|5|Briefly described|Map legend|Llandovery||||||||
23993|Stockdale Conglomerate Member|42826|2|Defined|p41|Early Silurian||of Springfield Sandstone||||||
23993|Stockdale Conglomerate Member|42827|5|Briefly described|p105|||of Springfield Formation||||||
30576|Stoddart Member|23309|5|Briefly described|p139 Table 2.49|Devonian|Silurian|||||||
30576|Stoddart Member|24177|4|Described|p54|Lochkovian|Lochkovian|Of the Mount Ida Formation. Overlies the Dealba Member. Geological Province: Darraweit Guim Province.||||||
30576|Stoddart Member|24329|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent: Mount Ida Formation.||||||27-OCT-08
30576|Stoddart Member|60591|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Mount Ida Formation. Overlies the Dealba Formation. Consists of interbedded laminated mudstone, shale, fine-grained sandstone and conglomerate; shelly fossils.||||||
30576|Stoddart Member|60592|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Mount Ida Formation. Overlies the Dealba Formation. Consists of interbedded laminated mudstone, shale, fine-grained sandstone and conglomerate; shelly fossils.||||||25-NOV-04
30576|Stoddart Member|60593|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Mount Ida Formation. Overlies the Dealba Formation. Consists of interbedded laminated mudstone, shale, fine-grained sandstone and conglomerate; shelly fossils.||||||
30576|Stoddart Member|60595|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Mount Ida Formation. Overlies the Dealba Formation. Consists of interbedded laminated mudstone, shale, fine-grained sandstone and conglomerate; shelly fossils.||||||
30576|Stoddart Member|60596|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Mount Ida Formation. Overlies the Dealba Formation. Consists of interbedded laminated mudstone, shale, fine-grained sandstone and conglomerate; shelly fossils.||||||
30576|Stoddart Member|60599|2|Defined|p31 Fig. 9, p65|Early Devonian|Early Devonian|Of Mount Ida Formation. Correlates with the upper 2 units of Mount Ida Beds of Thomas (1937) - the mudstone-shale-conglomerates section, and the Pleurodictyum Beds. Max. thickness: ~1100m. Conformably overlies Dealba Sandstone Member. ||||||
30576|Stoddart Member|61185|5|Briefly described|p21 Fig. 6|Pragian|Lochkovian|Of Mount Ida Formation. Overlies Dealba Member. Geological Province: Melbourne Zone.||||||07-FEB-11
30576|Stoddart Member|62469|5|Briefly described|p5 Fig. 2, p25, p15|Lochkovian|Lochkovian|Of the Mount Ida Formation. Geological Province: Darraweit Guim Province.See also p43.||||||12-FEB-15
30576|Stoddart Member|70487|6|Mentioned|p9-10|Lochkovian|Lochkovian|Maximum andd minimum ages inferred by supporting palaeontology (Wright and Garratt). Boucotia australis biozone: Edwards et al. 1998).||Mount Ida Formation||Correlated with Broadford Formation by Sandford (2002).|Fossiliferous strata.|
39337|Stonefish Sandstone Member|13323|5|Briefly described|p393 Fig. 2|Late Paleocene|Late Paleocene|Of the Kingfish Formation (Halibut Subgroup, Latrobe Group). Geological Province: Gippsland Basin.||||||
39337|Stonefish Sandstone Member|24090|5|Briefly described|p8 Fig.3|Paleocene|Paleocene|Of the Kingfish Formation.  Geological Province: Gippsland Basin.||||||19-JAN-05
39337|Stonefish Sandstone Member|24551|6|Mentioned|p478 Fig. 15.8||Paleocene|Of the Halibut Subgroup.||||||29-JUL-05
39337|Stonefish Sandstone Member|61552|6|Mentioned|p583 Fig.2. |Paleocene|Paleocene|||Unit in Barracouta Formation.||||
39337|Stonefish Sandstone Member|65717|5|Briefly described|p9 Fig.2.2|Paleocene|Paleocene|||Barracouta Formation||Interbedded with Kingfish Formation|Interbedded sandstone, siltstone and shale.|05-SEP-17
29694|Stonehenge Ignimbrite|23309|4|Described|p109, 131 Table 2.40|||Overlies: Johnson Mudstone and Yellow Waterholes Ignimbrite.  Maximum Thickness: 300m.  Of the Little River Subgroup.||||||22-FEB-10
29694|Stonehenge Ignimbrite|24551|5|Briefly described|p144|||Of the Little River Subgroup.||||||29-JUL-05
29694|Stonehenge Ignimbrite|43312|5|Briefly described|Map Legend||Early Devonian|of Little River Group.||||||
29694|Stonehenge Ignimbrite|43313|5|Briefly described|Map Legend||Early Devonian|of Little River Subgroup||||||
29694|Stonehenge Ignimbrite|60542|3|Fully described|p63, p51|Early Devonian|Early Devonian|Of Little River Subgroup. Formerly mapped with Mount Johnson Mbr. Fine-grained vitric feldspar ignimbrite. Overlies Yellow Waterholes Ignimbrite; overlies Johnson Mudstone. Overlain by Holloways Fm. Max. thick: >300m.||||||
29694|Stonehenge Ignimbrite|68116|5|Briefly described|Appendix, Map 45.|Pragian|Pragian||||||Feldspar and vitric feldspar ignimbrite: variably welded and in parts pumiceous, green to pale grey; vitriclastic pumiceous sandstone; pyroclastic and marine mass-flow deposits.|
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.||||||
17410|Strathbogie Igneous Complex|23269|6|Mentioned|Fig14-3.1p403|||||||||
17410|Strathbogie Igneous Complex|24099|5|Briefly described|p45, p47|||Also referred to as "Strathbogie Igneous Complex".||||||
17410|Strathbogie Igneous Complex|24551|4|Described|p161|||||||||
17410|Strathbogie Igneous Complex|29786|6|Mentioned|p77|||||||||
17410|Strathbogie Igneous Complex|31713|5|Briefly described|p7|||||||||
17410|Strathbogie Igneous Complex|32001|6|Mentioned|p78|||||||||
17410|Strathbogie Igneous Complex|41641|4|Described|p166|||||||||
17410|Strathbogie Igneous Complex|41868|6|Mentioned|p485|||||||||
17410|Strathbogie Igneous Complex|42547|5|Briefly described|Fig.15 P57|||||||||
17410|Strathbogie Igneous Complex|42827|5|Briefly described|p485|||||||||
17410|Strathbogie Igneous Complex|64616|5|Briefly described|p127|||Of White (1954). Consisting of Violet Town Volcanics and Strathbogie Granite.||||||
17410|Strathbogie Igneous Complex|70933|14|Not recorded|p102|||Geological map.||||||
25496|Strathbogie Suite|24099|6|Mentioned|p45|||See also Strathbogie supersuite. Geological Province: Lachlan Fold Belt.||||||18-APR-05
25496|Strathbogie Suite|24551|5|Briefly described|p222|||Of the Strathbogie Province.||||||
25496|Strathbogie Suite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
25496|Strathbogie Suite|42827|5|Briefly described|p434|||||||||
25496|Strathbogie Suite|61185|5|Briefly described|p47|Late Devonian|Late Devonian|Includes Strathbogie Granite, Trawool and Barjang adamellites (White & Chappell 1988; Chappell et al 1991).||||||07-FEB-11
25496|Strathbogie Suite|64616|5|Briefly described|p127|||Of White and Chappell (1988). Characterised by cordierite, a very low oxidation state and high Ba.||||||
25496|Strathbogie Suite|69876|5|Briefly described|p316|||Lachlan Fold Belt. Discussed in relation to source rock.|||||S-type granite.|
17440|Strzelecki Group|13323|5|Briefly described|p391, p393 Fig. 2|Early Cretaceous|Early Cretaceous|Includes Korumburra and Tyers River Subgroups. Characterised by fluvial deposition of dominantly volcaniclastic sediments. Overlain by Emperor Subgroup. Age is Albian. Geological Province: Gippsland Basin.||||||
17440|Strzelecki Group|13324|4|Described|p93, p94 Fig. 4, Fig.5, p98|Cenomanian|Albian|Gippsland Basin. Total thickness likely to exceed 3000 m.||||Unconformably overlies igneous and folded sedimentary Palaeozoic rocks. Unconformably overlain by (offshore) Latrobe Group.|Non-marine, volcaniclastic-rich greywackes, mudstones and minor coals.|
17440|Strzelecki Group|13332|5|Briefly described|p184 Fig.2|Early Cretaceous|Early Cretaceous|Geological Province: Gippsland Basin||||||
17440|Strzelecki Group|13350|5|Briefly described|p94, p96|Early Cretaceous|Late Jurassic|Basin basement deposits. Overlain by Golden Beach Group. Geological Province: Gippsland Basin. Otway Group equivalents.  See also p100 Fig. 7.||||||
17440|Strzelecki Group|22454|5|Briefly described|p3, fig. 4|Early Cretaceous||Maximum age ?Lower Cretaceous. Gippsland Basin||||||22-AUG-18
17440|Strzelecki Group|22476|4|Described|p951|Aptian|Berriasian|||||||
17440|Strzelecki Group|22487|6|Mentioned|p212||Cretaceous|Geological province: Gippsland Basin. See also Fig. 13.||||||11-SEP-08
17440|Strzelecki Group|22495|6|Mentioned|P220, Fig4 P221||Early Cretaceous|||||||
17440|Strzelecki Group|22663|5|Briefly described|V97 - G1 to G4 Fig.2|Early Cretaceous|Early Cretaceous|||||||01-MAR-10
17440|Strzelecki Group|23041|6|Mentioned|p116||Cretaceous|||||||
17440|Strzelecki Group|23230|5|Briefly described|p39, Table4-1p40|Early Cretaceous||||||||
17440|Strzelecki Group|23234|6|Mentioned|p88||Early Cretaceous|||||||
17440|Strzelecki Group|23262|6|Mentioned|Fig13-1.1p290||Early Cretaceous|||||||
17440|Strzelecki Group|23263|5|Briefly described|p313, 315||Early Cretaceous|||||||
17440|Strzelecki Group|23264|5|Briefly described|Table13-3.1p324, 325||Early Cretaceous|||||||
17440|Strzelecki Group|23266|5|Briefly described|Fig13-5.1p354||Aptian|||||||
17440|Strzelecki Group|23372|4|Described|p251, Fig.3|Albian|Barremian|Equivalent to Otway Group. In the Gippsland Basin.||||||17-NOV-08
17440|Strzelecki Group|23427|5|Briefly described|Table 11.2 p418.|||Divided into upper and lower.||||||
17440|Strzelecki Group|23792|5|Briefly described|p22|Early Cretaceous|Late Jurassic|Non-marine syn-rift sediments. Geological Province: Gippsland Basin.||||||
17440|Strzelecki Group|23885|6|Mentioned|p163 Fig. 14.3|||Geological Province: Gippsland Basin.||||||
17440|Strzelecki Group|23909|5|Briefly described|p298|Early Cretaceous|Early Cretaceous|||||||
17440|Strzelecki Group|24053|4|Described|p36|Early Cretaceous|Jurassic|Geological Basin: Gippsland Basin.||||||
17440|Strzelecki Group|24054|4|Described|p46|Early Cretaceous|Early Cretaceous|Geological Basin: Gippsland Basin.||||||
17440|Strzelecki Group|24055|5|Briefly described|p70|||Geological Basin: Gippsland Basin.||||||
17440|Strzelecki Group|24085|5|Briefly described|p42 Tb.2|Early Cretaceous|Early Cretaceous|||||||
17440|Strzelecki Group|24090|5|Briefly described|p8 Fig.3|Early Cretaceous|Early Cretaceous|Geological Province: Gippsland Basin.||||||
17440|Strzelecki Group|24164|5|Briefly described|p3,7,11,15,17-20,22-26,28,30,32-34, more|Campanian|Campanian|Horizon top of this unit was mapped from seismic data. Earliest sedimentary rocks in Gippsland Basin. Initial syn-rift fill. In Bass Canyon. Detrital pollen spores present. Included on p36-37,39-40,42 and in Figs. 8,10,12,14,15,16,18,19,22,24,26.|||Tyers River Subgroup|Is unconformably overlain by Latrobe Group|Fluvial, volcaniclastic sediments|
17440|Strzelecki Group|24211|5|Briefly described|p86 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Gippsland Basin.  See also p85 Fig. 2 and p87 Fig. 4.||||||
17440|Strzelecki Group|24224|5|Briefly described|p264|Early Cretaceous|Early Cretaceous|||||||
17440|Strzelecki Group|24238|5|Briefly described|p8|Early Cretaceous|Jurassic|Geological Province: Gippsland Basin.||||||16-MAR-05
17440|Strzelecki Group|24403|6|Mentioned|p4|||||||||
17440|Strzelecki Group|24407|5|Briefly described|p13 Fig.2|Albian||||||||
17440|Strzelecki Group|24495|5|Briefly described|p9|||Overlain by Latrobe Group.  Geological Province: Gippsland Basin.||||||
17440|Strzelecki Group|24551|5|Briefly described|p240, Fig. 9.2, 475|Cretaceous|Late Jurassic|||||||
17440|Strzelecki Group|24561|5|Briefly described|p27|||Geological Province: Gippsland Basin. Includes volcanogenic sediments.||||||04-FEB-08
17440|Strzelecki Group|29650|6|Mentioned|p111|||||||||
17440|Strzelecki Group|29721|6|Mentioned|p192|||||||||
17440|Strzelecki Group|29736|6|Mentioned|p192|||||||||
17440|Strzelecki Group|29821|6|Mentioned|p2|||||||||
17440|Strzelecki Group|29974|6|Mentioned|p48|||||||||
17440|Strzelecki Group|30084|6|Mentioned|p3|||||||||
17440|Strzelecki Group|30365|6|Mentioned|Fig.5|||||||||
17440|Strzelecki Group|30499|6|Mentioned|p95|||Stratigraphy||||||
17440|Strzelecki Group|30569|6|Mentioned|p189|||Flora||||||
17440|Strzelecki Group|30570|5|Briefly described|p6|||||||||
17440|Strzelecki Group|30836|4|Described|p1264|||Early Cretaceous.||||||
17440|Strzelecki Group|30905|3|Fully described|p158|||||||||
17440|Strzelecki Group|30929|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17440|Strzelecki Group|30930|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17440|Strzelecki Group|30933|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17440|Strzelecki Group|31159|6|Mentioned|p85|||Lower Cretaceous||||||
17440|Strzelecki Group|31160|6|Mentioned|p78|||||||||
17440|Strzelecki Group|31202|6|Mentioned|p217|||||||||
17440|Strzelecki Group|31254|3|Fully described|p139|||See also p140.||||||17-NOV-08
17440|Strzelecki Group|31352|4|Described|p133|||See also p134, Fig. 3. Lower Cretaceous.||||||17-NOV-08
17440|Strzelecki Group|31480|4|Described|Fig.3|||Lower Cretaceous. Non-marine greywacke.||||||17-NOV-08
17440|Strzelecki Group|31508|6|Mentioned|Table 1|||L. Cretaceous||||||
17440|Strzelecki Group|31510|6|Mentioned|p12|||See also Table 1.||||||
17440|Strzelecki Group|31616|6|Mentioned|p202|||L.Cret.||||||
17440|Strzelecki Group|32162|5|Briefly described|p56|||Refers petroleum aspect||||||
17440|Strzelecki Group|32679|4|Described|p94|||Refers Gippsland Basin.||||||17-NOV-08
17440|Strzelecki Group|32995|6|Mentioned|Fig.10|||||||||
17440|Strzelecki Group|33156|6|Mentioned|p134|||||||||
17440|Strzelecki Group|33165|6|Mentioned|Chart|||Correlation chart only||||||
17440|Strzelecki Group|33267|5|Briefly described|p70|||See also Fig.8||||||
17440|Strzelecki Group|33320|6|Mentioned|p57|||L.Cret.||||||
17440|Strzelecki Group|33348|6|Mentioned|p136|||Ref. Hocking (1972).||||||
17440|Strzelecki Group|33354|6|Mentioned|p187|||U.Jur.-L.Cret.||||||
17440|Strzelecki Group|33362|6|Mentioned|Fig.2|||||||||
17440|Strzelecki Group|33459|6|Mentioned|Table 1|||||||||
17440|Strzelecki Group|33462|6|Mentioned|p10|||Strat. table.||||||
17440|Strzelecki Group|33602|6|Mentioned|Table 1|||||||||
17440|Strzelecki Group|33627|6|Mentioned|p595|||||||||
17440|Strzelecki Group|34148|6|Mentioned|p10|||Lower Cretaceous. See also PP11,12,43,263.||||||
17440|Strzelecki Group|34558|4|Described|p19|||||||||
17440|Strzelecki Group|34815|6|Mentioned|p16|||||||||
17440|Strzelecki Group|34842|6|Mentioned|Table 3|||||||||
17440|Strzelecki Group|34843|4|Described|p9|||||||||
17440|Strzelecki Group|35013|4|Described|p396|||||||||
17440|Strzelecki Group|35067|6|Mentioned|p1151|||||||||
17440|Strzelecki Group|35112|6|Mentioned|Table 1|||||||||
17440|Strzelecki Group|35151|6|Mentioned|p153|||||||||
17440|Strzelecki Group|35273|6|Mentioned|p251|||||||||
17440|Strzelecki Group|35290|6|Mentioned|p23|||||||||
17440|Strzelecki Group|35537|6|Mentioned|p23|||||||||
17440|Strzelecki Group|35573|6|Mentioned|Fig.3|||Chronostratigraphic section - Gippsland Basin||||||
17440|Strzelecki Group|36197|4|Described|Table 1|||Lithology.||||||
17440|Strzelecki Group|36327|6|Mentioned|p7|||||||||
17440|Strzelecki Group|36643|6|Mentioned|Fig.7|||||||||
17440|Strzelecki Group|36749|6|Mentioned|p141|||||||||
17440|Strzelecki Group|37136|4|Described|p353|||||||||
17440|Strzelecki Group|37330|6|Mentioned|p21|||||||||
17440|Strzelecki Group|37530|3|Fully described|p3|||||||||
17440|Strzelecki Group|38422|6|Mentioned|p150|||||||||
17440|Strzelecki Group|38717|5|Briefly described|p21|||||||||
17440|Strzelecki Group|38738|5|Briefly described|p262|||||||||
17440|Strzelecki Group|38928|4|Described|p9|||||||||
17440|Strzelecki Group|38931|4|Described|p75|||||||||
17440|Strzelecki Group|39211|6|Mentioned|Fig.45|||||||||
17440|Strzelecki Group|39315|6|Mentioned|Fig.7|||||||||
17440|Strzelecki Group|39551|6|Mentioned|Map legend|Aptian|Neocomian|Aptian to Neocomian||||||
17440|Strzelecki Group|39555|6|Mentioned|Map legend|Aptian|Neocomian|Aptian to Neocomian||||||
17440|Strzelecki Group|39858|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17440|Strzelecki Group|40114|6|Mentioned|p4|||||||||
17440|Strzelecki Group|40523|6|Mentioned|Table 1|||||||||
17440|Strzelecki Group|40527|6|Mentioned|Table 1|||||||||
17440|Strzelecki Group|40716|6|Mentioned|p67|||||||||
17440|Strzelecki Group|41057|6|Mentioned|p60|||||||||
17440|Strzelecki Group|41171|5|Briefly described|p166|||||||||
17440|Strzelecki Group|41193|6|Mentioned|Fig.10|||||||||
17440|Strzelecki Group|41213|5|Briefly described|p143|||||||||
17440|Strzelecki Group|41227|5|Briefly described|p3|||||||||
17440|Strzelecki Group|41282|6|Mentioned|Fig.4|||||||||
17440|Strzelecki Group|41318|5|Briefly described|p181|||||||||
17440|Strzelecki Group|41426|6|Mentioned|p1|||||||||
17440|Strzelecki Group|41427|6|Mentioned|p79|||||||||
17440|Strzelecki Group|41454|6|Mentioned|Fig.5|||||||||
17440|Strzelecki Group|41534|5|Briefly described|p135|||||||||
17440|Strzelecki Group|41552|6|Mentioned|p459|||||||||
17440|Strzelecki Group|41642|4|Described|p224|||Selwyn (1856) used Paterson Beds.||||||
17440|Strzelecki Group|41727|5|Briefly described|p433|||||||||
17440|Strzelecki Group|41812|6|Mentioned|Table 4|||||||||
17440|Strzelecki Group|41868|4|Described|p515|||||||||
17440|Strzelecki Group|42075|5|Briefly described|Fig.15 P253|||||||||
17440|Strzelecki Group|42083|6|Mentioned|Fig.9 P346|||||||||
17440|Strzelecki Group|42184|5|Briefly described|p349|||||||||
17440|Strzelecki Group|42311|5|Briefly described|Fig.2 P526|||||||||
17440|Strzelecki Group|42415|5|Briefly described|p177|||Gippsland Basin||||||
17440|Strzelecki Group|42423|5|Briefly described|p327|Early Cretaceous||||||||
17440|Strzelecki Group|42555|5|Briefly described|p285|||||||||
17440|Strzelecki Group|42648|6|Mentioned|p43|||||||||
17440|Strzelecki Group|42827|4|Described|p230|||see also Table 7.3||||||
17440|Strzelecki Group|42998|6|Mentioned|p60|||||||||
17440|Strzelecki Group|43078|6|Mentioned|p180|||||||||
17440|Strzelecki Group|43145|4|Described|p8||Cretaceous|Age is Lower to Middle Cretaceous.||||||17-NOV-08
17440|Strzelecki Group|44029|14|Not recorded|p157,158||Early Cretaceous|||||||
17440|Strzelecki Group|48631|5|Briefly described|p1,4-7,pl.1,sh 2-5||Early Cretaceous|Lower Cretaceous - ? Jurassic. (J/55-11).||||||
17440|Strzelecki Group|48636|14|Not recorded|p.1,13,17,19|||(J55-11/Sale).||||||
17440|Strzelecki Group|49004|6|Mentioned|p18|||||||||
17440|Strzelecki Group|50043|6|Mentioned|p2, p6, 8, 12|Aptian|Aptian||||Includes Wonthaggi Formation.|||27-MAR-12
17440|Strzelecki Group|60538|6|Mentioned|p472 Fig. 11, 488 Fig. 27|||||||||
17440|Strzelecki Group|60638|5|Briefly described|p235|||Includes lava flows.  Geological Province: Gippsland Basin.||||||
17440|Strzelecki Group|61140|5|Briefly described|p9, p10|Early Cretaceous|Early Cretaceous|An historical perspective of the Harmers Haven coal site Cape Paterson on the South Gippsland coast.||||||16-JUN-05
17440|Strzelecki Group|61180|6|Mentioned|p36|||Contains black coal (East Gippsland).||||||
17440|Strzelecki Group|61212|6|Mentioned|p300 |||Fluvial and lacustrine sediments. Geological Province: Gippsland Basin (basement).||||||
17440|Strzelecki Group|61302|4|Described|p9, p11 Fig.4|Cretaceous|Jurassic|First sediments to accumulate in Gippsland rift basin. Interbedded non-marine greywackes, mudstones, sandstones, conglomerates, minor coals and volcanics. Overlain by Golden Beach and Latrobe Gps. Max. thickness: 3km. Geol. Prov: Gippsland Basin.||||||01-JUL-08
17440|Strzelecki Group|61323|5|Briefly described|p3 Fig. 3|Cretaceous|Cretaceous|Volcaniclastics; non-marine sediments. Geological Province: Gippsland Basin.||||||12-FEB-08
17440|Strzelecki Group|61328|5|Briefly described|p111, p112 Fig. 2|Early Cretaceous|Early Cretaceous|Overlain by Golden Beach Group. Age: >120 - 98Ma. Geological Province: Gippsland Basin.||||||17-NOV-08
17440|Strzelecki Group|61329|5|Briefly described|p121|Cretaceous|Early Cretaceous|Overlain by Latrobe Group. Geological Province: Gippsland Basin. Non marine deposits.||||||17-NOV-08
17440|Strzelecki Group|61336|5|Briefly described|p(v) Fig. 5|Early Cretaceous|Early Cretaceous|See also Strzelecki Formation. Overlain by Latrobe Group.||||||07-FEB-11
17440|Strzelecki Group|61469|6|Mentioned|p33|||Unit acts as a seal for reservoirs. Underlies Gurnard Formation and Halibut Subgroup in places. Geological Province: Gippsland Basin.||||||23-MAY-06
17440|Strzelecki Group|61552|5|Briefly described|pp582-584.|Early Cretaceous|Early Cretaceous|Represents early synrift sedimentation. Eastern rift equivalent to the Otway Group in the Otway Basin. 2503m thick.|||Includes Korumburra Subgroup.||Interbedded lithic and volcaniclastic sandstones as well as mudstones and minor coals. |
17440|Strzelecki Group|61553|6|Mentioned|p606.|||Chronostratigraphic equivalent of the Otway Megasequence (Bass Basin).||||||
17440|Strzelecki Group|61607|6|Mentioned|p5 Fig. 2|Early Cretaceous|Early Cretaceous|Refers to both the upper and lower parts of the Strzelcki Group. Geological Province: Gippsland Basin.||||||12-MAR-09
17440|Strzelecki Group|61608|6|Mentioned|p37|||||||||
17440|Strzelecki Group|61846|5|Briefly described|p258|Early Cretaceous|Late Jurassic|Volcaniclastic sediments.||||||03-JUL-06
17440|Strzelecki Group|63173|5|Briefly described|p342 Fig. 9.2|Early Cretaceous|Early Cretaceous|Geological Province: Gippsland Basin, offshore.||||||07-FEB-11
17440|Strzelecki Group|63217|6|Mentioned|p97 Fig.2.|||Gippsland Basin.||||Is overlain unconformably by the Traralgon Formation.||
17440|Strzelecki Group|63263|6|Mentioned|p36|||Mentioned as Late Jurassic-mid-Cretaceous correlates.||||||07-FEB-11
17440|Strzelecki Group|63445|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous||||Wonthaggi Formation.|||
17440|Strzelecki Group|64616|5|Briefly described|p141-142, p144|Early Cretaceous|Early Cretaceous|Name proposed to be dropped. It has been used in eastern Victoria for the same rift basin sediments that the name, with "much better heritage", Otway Group is used for, to the west.||||||
17440|Strzelecki Group|64876|5|Briefly described|p145 Fig.2|Albian||Gippsland Basin.|||Korumburra Subgroup.|Is overlain by Latrobe Group (Otway Unconformity).||
17440|Strzelecki Group|65316|5|Briefly described|p596|||Called the Otway Group in the Otway Basin.||||||23-APR-12
17440|Strzelecki Group|65715|5|Briefly described|p10|||Considered to be a junior synonym of Otway Group by VandenBerg et al. (2006) and herein.||||||
17440|Strzelecki Group|65717|5|Briefly described|p7-8, p9 Fig.2.2, p10, p34|Albian|Albian|Gippsland Basin. Unconformably overlies unnamed Palaeozoic igneous and folded sedimentary rocks. Sediments accumulated under a fluvial deposition regime. Contains oil and gas accumulations. Thickness likely exceeds 1500m. Has strong affinities with the Otway Group.|||Includes Korumburra Subgroup|Unconformably overlain by Emperor Subgroup|Interbedded lithic, volcaniclastic sandstones and mudstones with several coal-rich horizons.|05-SEP-17
17440|Strzelecki Group|65718|5|Briefly described|p5, p10 Fig 3.2, p11, p38, pp44-47, p50.|Cretaceous|Cretaceous|Seaspray Depression. Gippsland Basin. Represents non-marine sedimentation. Ill-defined total thickness, but likely to exceed 1500 m, and may be up to 3000 m in places. Lower Cretaceous age.|||Includes the Tyers River Subgroup.|Unconformably overlain by the Emperor Subgroup.|Comprises a thick sequence of non-marine, volcaniclastic rich sediments.|
17440|Strzelecki Group|65973|4|Described|p13-14, p19-23, p25, p27-30, p32, p35,|Aptian|Albian|Gippsland Basin. Non-marine, volcaniclastic rich sediments. Deposited during low-strain, syn-rift extension. Unconformably overlies palaeozoic sedimentary and igneous rocks. This group has very strong affinities with the Eumeralla Formation of the Otway Group. Total thickness is poorly known but expected to exceed 1500m. Proven source of gas in the onshore fields of the Gippsland Basin. Faulted against the Admiral Formation. Intersected in Leatherjacket-1, Northright-1, Sweep-1  and many more drillholes (see appendix). See also  p37, p38, p44-46, p57-58, p61, p81, p86, p89, p96-98, p102, p104, p112, p114, p116-117, p132-133, p136-137, p141-143, p171, p180-p184.||||Unconformably overlain by the Emperor Subgroup. Unconformably overlain by the Seaspray Group. Faulted against the Admiral Formation.|Interbedded lithic, volcaniclastic sandstones and mudstones and several coal horizons. Claystone, siltstone and argillaceous sandstone.|
17440|Strzelecki Group|66244|5|Briefly described|p4.|Early Cretaceous|Early Cretaceous|Name replaced by Otway Group (VandenBerg et al. 2006 and VandenBerg 2008) for all the Early Cretaceous clastic sedimentary rocks in the Otway, Bass and Gippsland Basins. Because of its entrenched nature in the petroleum industry, the name (Strzelecki Group) is retained for the Early Cretaceous equivalent of the Otway Group in the Gippsland Basin. This makes the Tyers River Subgroup a daughter unit.|||Includes Tyers River Subgroup.|||
17440|Strzelecki Group|67727|6|Mentioned|p56 Fig.1, p74 Fig.9, p80 Fig.10.|||||||||11-JUL-12
17440|Strzelecki Group|68206|6|Mentioned|p27||||||||Contains carbonate concretions.|
17440|Strzelecki Group|69016|5|Briefly described|p88-89,91,93-97|Late Cretaceous|Late Cretaceous|Of the Gippsland Basin. Forms an aquitard to adjacent sedimentary aquifers.|||||Consolidated sandstones and shales.|
17440|Strzelecki Group|69297|6|Mentioned|p370, p400, p402, p418, p434|Lower Cretaceous|Lower Cretaceous|Gippsland Basin. Gas-prone source rocks. Deposited in fluvio-lacustrine environments. |||||Coal and mudstones. |
17440|Strzelecki Group|69750|6|Mentioned|p66|Mesozoic|Mesozoic|Part of the basement to the Gippsland Basin.||||||
17440|Strzelecki Group|69879|4|Described|p411, p417, p428, p436, p462|Early Cretaceous|Early Cretaceous|Deposited during the second phase of rifting in the (Otway and) Gippsland Basins. Possibly faulted and folded. Volcanogenic material may have come from Cape Portland shoshonite complex and/or Cygnet Alkaline Complex.||||Is overlain by Halibut Subgroup.|Non-marine sediments with some volcanics.|
17440|Strzelecki Group|70028|6|Mentioned|p79-82|Albian||Gippsland Basin.||||Is overlain unconformably by Latrobe Group.|Syn-rift, mainly fluvial-lacustrine sediments.|
17440|Strzelecki Group|70076|5|Briefly described|South-Eastern: Fig.3; p2-3|Albian|Barremian|See also Regional: p2-5, p7. Hydrocarbon source rocks (unproven in release area); most likely source of gas in onshore (Gangell, Seaspray and Wombat) fields. Deposition occurred in a complex system of graben and half-graben.|||Korumburra Subgroup.|Is overlain by Latrobe Group. Time-equivalent to Eumeralla Formation.||
17440|Strzelecki Group|70331|5|Briefly described|p68-70, 73, 75-76|Early Cretaceous|Late Jurassic|Gippsland Basin. Holds potential for shale gas. Up to at least 3000m thick.|150-~100 Ma.|||Is overlain unconformably by Latrobe Group.|A thick sequence of carbon-rich fluvial sediments (overbank and lacustrine shales), and volcaniclastic sandstone, conglomerate, mudstone and coal.|
17440|Strzelecki Group|70378|5|Briefly described|p695-714|Early Cretaceous|Early Cretaceous|Gippsland Highlands, Latrobe Valley. Over 108m thick. Oil and gas shows.|||Tyers River Subgroup, Wonthaggi Formation.|Is overlain by Latrobe Valley coal measures.|Volcanigenic sediments.|
17440|Strzelecki Group|71601|6|Mentioned|p123|||In Victoria. Includes described ankylosaurian osteoderms.||||||
17440|Strzelecki Group|73153|6|Mentioned|p284-285, p292|Albian|Barremian|Fossil material for an astragalocalcaneum (NMV P221202) and an astragalus (NMV P150070) were recovered from the upper portion of this unit.||||||
17440|Strzelecki Group|73289|5|Briefly described|p764-765 Figs.1-2, 766-767, 770-772, 778|Early Cretaceous|Early Cretaceous|Basement to onshore Gippsland Basin. There is evidence for reversed and block faulting and folding||||Is overlain by Traralgon Formation, Carrajung Volcanics.||
17440|Strzelecki Group|73471|4|Described|p85-87, p89, p98-99, p104-105, p108-109|Early Cretaceous|Late Jurassic|Defined as the main syn-rift mega-sequence of the Gippsland Basin. Coarse clastic and volcanic material associated with an extensive westward-draining braided river system, fine-grained flood plain deposits contain interbedded coal horizons towards the top of the succession. Underlies Otway breakup unconformity. Preserved thickness in basin centre is likely over 7000 m, may include Late Jurassic successions at base. See also Strzelecki Formation p108.|ca 145-103 Ma||Lower Strzelecki Group, Upper Strzelecki Group|Unconformably underlies Latrobe Group, Emperor Subgroup|Non-marine arkose and volcanoclastics.|
17440|Strzelecki Group|73488|5|Briefly described|p631 Fig.1, p634 Fig.4, p640 Fig.8|Lower Cretaceous|Lower Cretaceous|||||Underlies Honeysuckle Hill Formation|Includes arkose.|
17440|Strzelecki Group|73562|5|Briefly described|p301, 305|Late Cretaceous|Late Cretaceous|Basal Gippsland Basin.||||Is overlain by Latrobe Group.|Non-marine, mostly volcaniclastic sediments.|
17440|Strzelecki Group|75065|5|Briefly described|p149, 151-152, 154, 156-160, 170-172|Albian|Valanginian|Gippsland Basin. Entirely non-marine. Contains reservoirs and potential petroleum source rocks. Chronostratigraphy diagram.|||Tyers River, Korumburra Subgroups.|Is overlain unconformably by Emperor Subgroup (Latrobe Group).||
34699|Sturgess Point Member|22875|5|Briefly described|p26 Table1|||Mepunga Formation||||||
34699|Sturgess Point Member|24397|5|Briefly described|p245|Middle Eocene|Middle Eocene|Overlies Dilwyn Formation.  Geological Province: Otway Basin.||||||
34699|Sturgess Point Member|24551|5|Briefly described|p292 Fig. 10.3|||||||||
34699|Sturgess Point Member|60538|6|Mentioned|p470 Fig. 10, 471 Fig. 10|||||||||
34699|Sturgess Point Member|61182|4|Described|p25, p26, p171|Middle Eocene|Middle Eocene|Basal mudstone unit within the Mepunga Formation, with two informally named units, the upper and lower Mepunga sands, above and below it. Dark brown, carbonaceous clayey silt to silty clay, often burrowed. Max. thickness: 23m in Callista.||||||
34699|Sturgess Point Member|65891|5|Briefly described|p221 Fig.5, p227 Fig.10.|Paleogene|Paleogene|Otway Basin. Unit in Mepunga Formation. Sands, dark, carbonaceous, pyritic, silty. Lutetian-Bartonian age.||||||
78584|Sturgess Sand|68991|5|Briefly described|p465 Fig.2, pp467-469|Holocene|Pleistocene|Gill (1965); Shoemaker and Uhlherr (1999). Upper Pleistocene maximum age, radiocarbon dating. ~ 0.5 to 1 m thick.|17.3-5.55 ka (Fairbanks et al. 2005).|||Disconformably underlain by the Dog Trap Bay Sand.|Comprises a mostly fine-grained eolian deposit. Displays a humus podsol soil profile with scattered ferruginous pisolites and fragments of ironstone (ferruginous sand), and a weakly cemented clayey sand at the base forms a hardpan when dry.|16-JAN-14
78584|Sturgess Sand|73486|6|Mentioned|p522 Fig.12|||||||||
17505|Suggan Buggan Granodiorite|23309|5|Briefly described|p115, 338|||G74 S-Type||||||
17505|Suggan Buggan Granodiorite|23615|3|Fully described|p155, p32|Early Devonian|Early Silurian|Of the Bullenbalong Suite.  Intrudes the Bendoc and Yalmy Groups.  Non-conformably overlain by Snowy River Volcanics.  Part of the Suggan Buggan Pluton on MURRINDAL - partly surrounds the Chilpin Granodiorite.  See also p205 App. 1.||||||
17505|Suggan Buggan Granodiorite|24551|6|Mentioned|p58|||||||||
17505|Suggan Buggan Granodiorite|41850|6|Mentioned|p431|||||||||
17505|Suggan Buggan Granodiorite|42827|6|Mentioned|p431|||||||||
17505|Suggan Buggan Granodiorite|43206|5|Briefly described|map legend||Wenlock|Of Bullenbalong Suite. Biotite-cordierite granodiorite: grey, medium and coarse grained; massive.||||||24-JUN-14
17505|Suggan Buggan Granodiorite|44185|5|Briefly described|Map legend.|Silurian|Silurian|S-type.||||||
17505|Suggan Buggan Granodiorite|61181|6|Mentioned|p195|||Wollastonite occurs in the aureole. ||||||
17505|Suggan Buggan Granodiorite|68115|5|Briefly described|p7.|||Deddick Zone. Non-magnetic. Continues to the NSW border, across which it is called Ingebyrah Granodiorite. Probably the same pluton.|||||Biotite-cordierite granodiorite.|
17505|Suggan Buggan Granodiorite|68116|5|Briefly described|Appendix, Maps 28, 36.|Wenlock|Llandovery||||||Biotite-cordierite granodiorite: coarse grained, quartz phyric; S-type.|
33256|Sunbury Group|12100|5|Briefly described|p819|Late Ordovician|Late Ordovician|West of Melbourne; upward fining succession with an upward decrease in lithic content.||||||08-MAY-12
33256|Sunbury Group|23309|5|Briefly described|p58-61, 241, 258 Table 2.18|Ordovician|Ordovician|||||||
33256|Sunbury Group|24002|5|Briefly described|p237|Late Ordovician|Late Ordovician|||||||
33256|Sunbury Group|24098|6|Mentioned|p27 Fig. 2|Late Ordovician|Late Ordovician|Geological Province: Bendigo/Melbourne Zones, Lachlan Fold Belt.||||||19-APR-05
33256|Sunbury Group|24134|5|Briefly described|p6 Fig. 2|Late Ordovician|Late Ordovician|||||||
33256|Sunbury Group|24178|5|Briefly described|p15 Fig.2|Late Ordovician|Late Ordovician|Geological Province: Bendigo Zone.||||||21-OCT-08
33256|Sunbury Group|24312|6|Mentioned|p1083|||||||||
33256|Sunbury Group|24551|3|Fully described|p105, 606|Late Ordovician|Middle Ordovician|Overlain by the Murrindindi Supergroup.||||||
33256|Sunbury Group|24588|5|Briefly described|p29|Late Ordovician|Late Ordovician|Geological Province: Darraweit Guim Province. Underlies: Murrindindi Supergroup. The onset of Sunbury Group sedimentation may match the oldest deformation ages (ca 457-453 Ma) obtained from the Bendigo and Stawell Zones by Ar/Ar method (Foster et al., 1996, 1998; Gray et al., 1997; VandenBerg, 1999b).||||||29-NOV-13
33256|Sunbury Group|24600|5|Briefly described|p479,|Late Ordovician|Late Ordovician|Quartz-rich turbidites and black shale.  Geological Province: Lachlan Fold Belt.||||||
33256|Sunbury Group|61187|5|Briefly described|p4.|Late Ordovician|Late Ordovician|Western Melbourne Zone.||||Conformably overlies Castlemaine Group.|Turbidites.|
33256|Sunbury Group|62099|5|Briefly described|p331|Late Ordovician|Middle ordovician|Dominated by quartz sandstone, mudstone and black shale. In the Bendigo Zone of the Lachlan Orogen.||||||01-JUL-13
33256|Sunbury Group|64312|5|Briefly described|p442|Late Ordovician|Late Ordovician|Sedimentary deposits at western edge of the Melbourne Tectonic Zone. Rich in sandstone in lower section, and contains some conglomerate. ||||||
33256|Sunbury Group|64612|4|Described|p27|Late Silurian|Late Silurian|Overlies Castlemaine Group. Thickness: 1300m. Sediments similar to Castlemaine Group and show upward fining.||||||07-FEB-11
33256|Sunbury Group|64619|5|Briefly described|Map legend|Late Ordovician|Late Ordovician|Includes the Riddell Sandstone.||||||03-NOV-08
33256|Sunbury Group|65715|5|Briefly described|p4 Tb.2, p5|Ordovician|Ordovician|Mapped by Thomas (1932) as unconformably overlain by Kerrie Group rocks. Includes Riddell Sandstone, Bolinda Shale, Darraweit Guim Mudstone and Mount Easton Shale.||||||
33256|Sunbury Group|67322|6|Mentioned|p13|Late Ordovician|Late Ordovician|Lachlan Orogen.||||||
33256|Sunbury Group|67802|6|Mentioned|p28|Late Ordovician||Eastern margin of Bendigo Zone.||||||
33256|Sunbury Group|67847|6|Mentioned|p10 fig 2.3|Ordovician|Ordovician|||||||
33256|Sunbury Group|68116|5|Briefly described|Appendix, Maps 32, 41.|Hirnantian|Sandbian|Age written as Gisbornian to Bolindian in text.|||||Shale, sandy shale, minor sandstone and mudstone.|
33256|Sunbury Group|68592|5|Briefly described|p12|Late Ordovician|Late Ordovician|Melbourne Terrane.|||||Sand-rich turbidites.|
33256|Sunbury Group|68823|6|Mentioned|p401, p406|Late Ordovician|Late Ordovician|Sourced from deformed Castlemaine Group.|||||Turbidites.|
33256|Sunbury Group|69002|6|Mentioned|p13|Late Ordovician|Late Ordovician|Of the Melbourne Zone.||||||
33256|Sunbury Group|69541|6|Mentioned|p652-653|Late Ordovician|Late Ordovician|Central Victoria.||||Overlies Castlemaine Group.||
33256|Sunbury Group|70125|5|Briefly described|p394|Late Ordovician|Late Ordovician|Probability density plot of U-Pb ages of detrital zircons is compared with that of other units.|450 Ma (Squire et al., 2006).|||||
33256|Sunbury Group|70601|5|Briefly described|p48|Ordovician|Ordovician|Deposited on the eastern flank of the Bendigo Zone.|ca 450 Ma.||||Sandstones.|
33256|Sunbury Group|70629|6|Mentioned|p986|Late Ordovician|Late Ordovician|Melbourne Zone.||||||
33256|Sunbury Group|70684|6|Mentioned|p7 Fig.1|||||||||
33256|Sunbury Group|70718|4|Described|p38|Late Ordovician|Late Ordovician|Marine turbidite deposits. Deformed and metamorphosed during the Benambran Orogeny. Source of date is not provided.|372 +/- 2 Ma |||Intruded by the Pyramid Hill Granite and Lake Boga Granite.|Dominantly quartz sandstone, mudstone and black shale.|
33256|Sunbury Group|71069|5|Briefly described|p22|Late Ordovician|Late Ordovician|Melbourne Zone.|||||Sand rich turbidite sequences.|
33256|Sunbury Group|71700|5|Briefly described|p9|||||||||
33256|Sunbury Group|73175|6|Mentioned|p1051|Late Ordovician|Late Ordovician|Melbourne Zone.|||||Quartz-rich turbidites.|
33256|Sunbury Group|75072|6|Mentioned|p232|Late Ordovician|Late Ordovician|Melbourne Zone.|||Riddell Sandstone.|||
24002|Sunlight Creek Formation|5258|5|Briefly described|164|Darriwilian|Darriwilian|Basal unit of Bendoc Group. At this conodont and graptolite fossil site on the Bungonia-Goulburn road NSW, consists of thin-bedded turbidites and light honey-coloured, thin bedded chert (with conodonts), overlain by black shale with abundant graptolites||||||22-JAN-10
24002|Sunlight Creek Formation|22577|6|Mentioned|p120||Darriwilian|||||||
24002|Sunlight Creek Formation|22624|6|Mentioned|p678|||||||||
24002|Sunlight Creek Formation|22876|6|Mentioned|p16|||Of the Bendoc Group.||||||17-JAN-07
24002|Sunlight Creek Formation|22878|5|Briefly described|p29|Ordovician|Ordovician|||||||
24002|Sunlight Creek Formation|22968|5|Briefly described|P30, P103||Ordovician|Grades up into Warbisco Shale, parent is Bendoc Group||||||
24002|Sunlight Creek Formation|23307|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
24002|Sunlight Creek Formation|23309|5|Briefly described|p57-61 Table 2.19|Ordovician|Ordovician|||||||
24002|Sunlight Creek Formation|23615|3|Fully described|p67, p20 Fig.6|Gisbornian|Gisbornian|Of the Bendoc Gp.  Overlain by Warbisco Shale, overlies Broadbent River Sst..  Originally included in Warbisco Shale by Cas and VandenBerg (1988). Age within the 'deep marine Ordovician sedimentation' period: 500-438Ma.  Geological Province: Lachlan Fold Belt.||||||16-AUG-18
24002|Sunlight Creek Formation|23938|6|Mentioned|p54 Tb. 4|||See also p59-61 Figs. 21-22.||||||25-SEP-08
24002|Sunlight Creek Formation|24004|5|Briefly described|p275 Fig.2|Ordovician|Ordovician|||||||
24002|Sunlight Creek Formation|24037|4|Described|p424|Gisbornian|Darriwilian|Of Bendoc Group. Geological Province: Lachlan Fold Belt||||||
24002|Sunlight Creek Formation|24133|3|Fully described|p37|Ordovician|Ordovician|Of the Bendoc Group.  Max. thickness: ~250m.  Geological Province: Lachlan Fold Belt.||||||17-JAN-07
24002|Sunlight Creek Formation|24142|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Bendoc Group. Geological Province: Lachlan Fold Belt.||||||
24002|Sunlight Creek Formation|24143|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Bendoc Group. Geological Province: Lachlan Fold Belt.||||||
24002|Sunlight Creek Formation|24144|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Bendoc Group. Geological Province: Lachlan Fold Belt.||||||
24002|Sunlight Creek Formation|24145|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Bendoc Group. Geological Province: Lachlan Fold Belt||||||
24002|Sunlight Creek Formation|24551|4|Described|p105|Gisbornian|Darriwilian|Of the Bendoc Group. Overlain by the Warbisco Shale. Overlies the Pinnak Sandstone.||||||
24002|Sunlight Creek Formation|41933|5|Briefly described|Map legend|Late Ordovician|Early Ordovician|||||||
24002|Sunlight Creek Formation|42294|5|Briefly described|p22|||Reserved March 1989||||||
24002|Sunlight Creek Formation|42560|6|Mentioned|p54|||||||||
24002|Sunlight Creek Formation|42627|5|Briefly described|Map legend|late Gisbornian||||||||
24002|Sunlight Creek Formation|42647|5|Briefly described|p19|||Equivalent to Sunlight Creek Mudstone Member. Used on Bendoc map.||||||
24002|Sunlight Creek Formation|43206|5|Briefly described|map legend||Eastonian|Of the Bendoc Group.||||||17-JAN-07
24002|Sunlight Creek Formation|43228|5|Briefly described|p9||Late Ordovician|of the Bendoc Group.||||||17-JAN-07
24002|Sunlight Creek Formation|43312|5|Briefly described|Map Legend|Gisbornian|Darriwilian|Of the Bendoc Group.||||||17-JAN-07
24002|Sunlight Creek Formation|43313|5|Briefly described|Map Legend|Gisbornian|Darriwilian|Of the Bendoc Group.||||||17-JAN-07
24002|Sunlight Creek Formation|43314|5|Briefly described|Map Legend||Gisbornian|Of the Bendoc Group.||||||17-JAN-07
24002|Sunlight Creek Formation|43315|5|Briefly described|Map Legend|Eastonian|Gisbornian|Of the Bendoc Group. Sandstone and mudstone, rhythmically alternating (stripey) thin bedded pale grey fine grained sandstone and dark grey green mudstone, siliceous mudstone, chert.||||||03-MAY-05
24002|Sunlight Creek Formation|60503|4|Described|p84-85, p29|Late Ordovician|Late Ordovician|Lower part of Bendoc Group. Characterised by thin bedded black mudstone and thin bedded chert, thin bedded quartzitic sandstone beds which grade up into the black shales of the Warbisco Shale; in places thick bedded quartzitic sandstone.||||||
24002|Sunlight Creek Formation|60504|5|Briefly described|Map Legend|Gisbornian|Darriwilian|Of the Bendoc Group. Sandstone and mudstone; alternating thin bedded pale grey fine grained sandstone and dark grey green mudstone, siliceous mudstone.||||||13-OCT-04
24002|Sunlight Creek Formation|60505|5|Briefly described|Map legend|Gisbornian|Darriwilian|Of the Bendoc Group. Sandstone and mudstone; alternating thin bedded pale grey fine grained sandstone and dark grey green mudstone, siliceous mudstone.||||||
24002|Sunlight Creek Formation|60506|5|Briefly described|Map legend|Gisbornian|Darriwilian|Of the Bendoc Group. Sandstone and mudstone; alternating thin bedded pale grey fine grained sandstone and dark grey green mudstone, siliceous mudstone.||||||
24002|Sunlight Creek Formation|60507|5|Briefly described|Map Legend|Gisbornian|Darriwilian|Of the Bendoc Group. Sandstone and mudstone; alternating thin bedded pale grey fine grained sandstone and dark grey green mudstone, siliceous mudstone.||||||20-OCT-04
24002|Sunlight Creek Formation|60541|3|Fully described|p51-52, p12, p27. p35|Gisbornian|Darriwilian|Of Bendoc Gp. Supersedes S.C.Mudstone Mbr.  Rhythmically alternating dark green to pale grey to almost black siliceous sltst and white thin-bedded, fine-gr.quartzitic sst beds giving stripey appearance. Grades up into Warbisco Shale; conf.over Pinnak Sst||||||12-JAN-06
24002|Sunlight Creek Formation|60542|3|Fully described|p47, p12|Gisbornian|Darriwilian|Basal unit of Bendoc Group. Comprises siliceous, dark to light grey, thin bedded siliceous siltstones and shales interbedded with quartzitic thin bedded sandstones; contains graptolites. Overlain by Warbisco Shale.||||||
24002|Sunlight Creek Formation|60904|5|Briefly described|p782|||Mudstone dominant turbidites. ||||||
24002|Sunlight Creek Formation|61160|5|Briefly described|p48|Late Ordovician|Late Ordovician|Basal unit of the Bendoc Group. Geological Province: Lachlan Fold Belt.||||||
24002|Sunlight Creek Formation|61161|5|Briefly described|p31, p82|||Lower part of Bendoc Group. Thin quartz sandstone beds that appear to be distal turbidites. Grade up into Warbisco Shale.||||||
24002|Sunlight Creek Formation|61163|4|Described|p81, p14 Fig. 3.2|Late Ordovician|Late Ordovician|Of the Bendoc Group. Grades up into Warbisco Shale. Geological Province: Lachlan Fold Belt (Tabberabbera Zone). See also p38 Tb. 6.2.||||||
24002|Sunlight Creek Formation|61174|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Black shale, cherty shale, stripy thin-bedded cross-bedded sandstone and siltstone: sparse Gisbornian graptolites. Deep-marine turbidite fan and hemipelagic deposits. GSV map code: Obs.||||||07-FEB-11
24002|Sunlight Creek Formation|61175|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Black shale, cherty shale, stripy thin-bedded cross-bedded sandstone and siltstone: sparse Gisbornian graptolites. Deep-marine turbidite fan and hemipelagic deposits. GSV map code: Obs.||||||
24002|Sunlight Creek Formation|61176|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Black shale, cherty shale, stripy thin-bedded cross-bedded sandstone and siltstone: sparse Gisbornian graptolites. Deep-marine turbidite fan and hemipelagic deposits. GSV map code: Obs.||||||
24002|Sunlight Creek Formation|61177|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Black shale, cherty shale, stripy thin-bedded cross-bedded sandstone and siltstone: sparse Gisbornian graptolites. Deep-marine turbidite fan and hemipelagic deposits. GSV map code: Obs.||||||
24002|Sunlight Creek Formation|61178|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of Bendoc Group. Medium- to thick- bedded sandstone, black shale, cherty shale, stripy thin-bedded cross-bedded sandstone and siltstone (turbidite): nonmagnetic (5 nT); slight gravity high (-453 ms^-2); moderate radioelements. GSV map code: Obs.||||||
24002|Sunlight Creek Formation|61964|5|Briefly described|p25 Fig. 8|Gisbornian|Darriwilian|Of the Bendoc Group in Victoria. ||||||
24002|Sunlight Creek Formation|63290|5|Briefly described|p396 Fig. 3|Gisbornian|Gisbornian|Of Bendoc Group. Underlain by Adaminaby Group, overlain by Warbisco Shale.||||||
24002|Sunlight Creek Formation|66196|5|Briefly described|p618|||Interbedded chert-shale succession and thin-bedded turbidites and chert. Overlies the Pinnak Sandstone, conformably underlies the Warbiso Shale. Pelagic deep-sea environment.||||||
24002|Sunlight Creek Formation|67322|4|Described|p15, p16, p17; Fig.5|Sandbian|Sandbian|Formerly Sunlight Creek Member of the Warbisco Shale; VandenBerg et al. (1991) after Glen et al. (1990). The Formation is Gisbornian in age, determined by the presence of graptolite bearing shales. Occurs in the Cooma-Mallacoota region.||Of the Bendoc Group.||Overlain by the Warbisco Shale. Overlies the Chakola Formation. Correlative of Pinnak Sandstone.|Well-laminated black shales, siltstones and thin beds of sandstone. Includes chert layers.|22-FEB-18
24002|Sunlight Creek Formation|68116|5|Briefly described|Appendix, Maps 20, 26-27, 36, 45.|Sandbian|Dariwilian|Minimum age written as Gisbornian in text.|||||Black shale, cherty shale, stripy thin-bedded cross-bedded sandstone and siltstone: medium- to thick-bedded turbiditic grey sandstone, minor mica; siltstone massive to bioturbated; sparse Gisbornian graptolites.|
24002|Sunlight Creek Formation|68592|5|Briefly described|p318, p320-2, p326, p1862|Gisbornian|Darriwilian|Also in E. Victoria. Probably equivalent to a combination of Nattery Chert Member and Bumballa Formation. Contains Pygodus serra conodonts.||Unit in Bendoc Group.||||
24002|Sunlight Creek Formation|70493|6|Mentioned|p63|Late Ordovician|Late Ordovician|Eastern Victoria, Lachlan Orogen. Zircons may have been derived from an area between the Bunger Hills and Transantarctic Mountains, East Antarctica.||||||
24002|Sunlight Creek Formation|70601|5|Briefly described|p43|Gisbornian|Gisbornian|Albury-Bega Basin: Inland Zone.||Bendoc Group.||||
24002|Sunlight Creek Formation|70661|6|Mentioned|p19, p22|||In Eastern Victoria.||Bendoc Group||Equivalent to the Bumballa Formation||
24002|Sunlight Creek Formation|71069|5|Briefly described|p68, p72, p74, p75, p77|Early Silurian|Gisbornian|Contains fossils of phosphatic brachiopods, burrows, conodonts and Gisbornian aged graptolites.||Bendoc Group||May be equivalent to the Nattery Chert Member and is equivalent to the Bumballa Formation.|Thin, rhythmic interbeds of dark grey to black siltstone and pale grey to white fine-grained sandstone that is characteristically 'stripy'. Occasional thick-bedded or lenses of quartzose sandstone.|
24002|Sunlight Creek Formation|71656|6|Mentioned|p14|||Now included in Nattery Chert Member.||||||
24002|Sunlight Creek Formation|71700|6|Mentioned|CD|||||Bendoc Group||||
24002|Sunlight Creek Formation|73140|5|Briefly described|p495 Fig.1, Fig.6|Gisbornian|Gisbornian|Age based on conodonts and graptolites.||Bendoc Group||Overlies Abercrombie Formation, Numeralla Chert Member, underlies Warbisco Shale||
29031|Sunnyside Sand|24551|6|Mentioned|p343|||Of the Bridgewater Group.||||||
29031|Sunnyside Sand|31003|6|Mentioned|p41|||||||||
29031|Sunnyside Sand|34993|5|Briefly described|p299|||||||||
29031|Sunnyside Sand|35722|6|Mentioned|Table 2|||Quaternary stratigraphic units and nature of components.||||||
29031|Sunnyside Sand|37583|6|Mentioned|Fig.2|||||||||
29031|Sunnyside Sand|41769|4|Described|p51|||||||||
29031|Sunnyside Sand|41848|5|Briefly described|p374|||Age circa 400000 yrs U-Th shells||||||
29031|Sunnyside Sand|42827|5|Briefly described|p374|||||||||
29031|Sunnyside Sand|73386|6|Mentioned|p14|||||Bridgewater Formation||||
37872|Surveyors Creek Suite|24133|3|Fully described|p71|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37872|Surveyors Creek Suite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37872|Surveyors Creek Suite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37872|Surveyors Creek Suite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37872|Surveyors Creek Suite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt||||||
37872|Surveyors Creek Suite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
17559|Sutherland Creek Sand|23239|5|Briefly described|Table1p109|Oligocene||||||||
17559|Sutherland Creek Sand|37385|6|Mentioned|p10|||See also P13||||||
17559|Sutherland Creek Sand|65715|6|Mentioned|p53,55|||Marine.||||||
34974|Swifts Creek Igneous Complex|22968|5|Briefly described|P15, Table7, P186||Early Devonian|Ages of unit are 408+/-4 and 402+/-4 Ma, parent is Rileys Creek Suite||||||
34974|Swifts Creek Igneous Complex|23020|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Rileys Creek Suite||||||
34974|Swifts Creek Igneous Complex|23030|5|Briefly described|Map legend|Early Devonian|Late Silurian|Parent is the Rileys Creek Suite||||||
34974|Swifts Creek Igneous Complex|23309|5|Briefly described|p100, 102, 284, 294-296, 344.|||||||||
34974|Swifts Creek Igneous Complex|24004|6|Mentioned|p279|||||||||
34974|Swifts Creek Igneous Complex|24551|5|Briefly described|p44 Fig. 2.51, p408|Early Devonian|Late Silurian|Age: 408 +/- 4Ma, 402 +/- 4Ma.||||||
34974|Swifts Creek Igneous Complex|61161|6|Mentioned|p150, p64|||Contact metamorphism - cordierite isograd follows shape of this unit. In OMEO.||||||
39334|Swordfish Formation|13323|5|Briefly described|p393 Fig. 2|Late Oligocene|Early Oligocene|Of the Latrobe Valley Subgroup (Seaspray Group). Marine carbonates. Geological Province: Gippsland Basin.||||||
39334|Swordfish Formation|24090|5|Briefly described|p8 Fig.3|Oligocene|Eocene|Geological Province: Gippsland Basin.||||||
39334|Swordfish Formation|24407|5|Briefly described|p13 Fig.2|Oligocene|Oligocene|Geological Province: Gippsland Basin||||||
39334|Swordfish Formation|61552|6|Mentioned|p583 Fig.2. |Late Oligocene|Early Oligocene|||Unit in Latrobe Valley Subgroup.||||
39334|Swordfish Formation|64876|5|Briefly described|p145 Fig.2|Oligocene|Oligocene|Gippsland Basin.||Seaspray Group.||||
39334|Swordfish Formation|65717|5|Briefly described|p9 Fig.2.2, p12|Oligocene|Oligocene|Partridge (1999); formerly "Unit 1" (Bernecker et al., 1997) of the offshore Seaspray Group.
||Latrobe Valley Subgroup.||Unconformably overlies Gurnard Formation. Equivalent to the onshore Lakes Entrance Formation.|Interbedded marl and glauconite; hemipelagic fossiliferous mudstone..|05-SEP-17
39334|Swordfish Formation|65973|6|Mentioned|p171|||Gippsland Basin.||||||
39334|Swordfish Formation|70028|6|Mentioned|p79|Oligocene|Oligocene|Offshore Gippsland Basin.||||||
39334|Swordfish Formation|70076|5|Briefly described|South-Eastern:Fig.2;p2.Regional:Fig.3;p6|Miocene|Oligocene|Regional seal.||Angler Subgroup.||Is overlain by Conger Formation. Lateral equivalent of Lakes Entrance Formation.||
37603|Sykes Tuff|23309|4|Described|p109 Table 2.40|||Of Little River Subgroup (Snowy River Volcanics).  Maximum Thickness: 300m.||||||
37603|Sykes Tuff|24551|5|Briefly described|p144|||Of the Little River Subgroup.||||||
37603|Sykes Tuff|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Breccia, thinly bedded vitric ash, fine sandstone, with accretionary lapilli.|
17618|Tabberabbera Formation|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
17618|Tabberabbera Formation|23309|6|Mentioned|p104|||||||||
17618|Tabberabbera Formation|24551|4|Described|p138|||Of the Wentworth Group.||||||
17618|Tabberabbera Formation|30790|6|Mentioned|p3|||||||||
17618|Tabberabbera Formation|31161|5|Briefly described|PA11|||||||||
17618|Tabberabbera Formation|32399|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
17618|Tabberabbera Formation|33481|6|Mentioned|p16|||||||||
17618|Tabberabbera Formation|33601|6|Mentioned|p39|||||||||
17618|Tabberabbera Formation|33602|6|Mentioned|p26|||||||||
17618|Tabberabbera Formation|33603|6|Mentioned|Map legend|Devonian|Devonian|||||||
17618|Tabberabbera Formation|33606|3|Fully described|p57|||||||||
17618|Tabberabbera Formation|33732|6|Mentioned|Table III|||||||||
17618|Tabberabbera Formation|34250|5|Briefly described|p19|||||||||
17618|Tabberabbera Formation|34954|6|Mentioned|Fig.34|||Analysis Fig.33.||||||
17618|Tabberabbera Formation|35274|6|Mentioned|p421|||||||||
17618|Tabberabbera Formation|35283|6|Mentioned|p49|||||||||
17618|Tabberabbera Formation|37330|4|Described|p17|||||||||
17618|Tabberabbera Formation|38787|6|Mentioned|p143|||||||||
17618|Tabberabbera Formation|41000|6|Mentioned|p279|||||||||
17618|Tabberabbera Formation|41585|4|Described|p132|||||||||
17618|Tabberabbera Formation|42015|6|Mentioned|p316|||||||||
17618|Tabberabbera Formation|42577|5|Briefly described|Fig.3 P31|||||||||
17618|Tabberabbera Formation|42635|5|Briefly described|p27|||||||||
17618|Tabberabbera Formation|42827|4|Described|p132|||Of Wentworth Group.||||||30-JUN-08
17618|Tabberabbera Formation|43461|14|Not recorded|p628|||||||||
17618|Tabberabbera Formation|43547|14|Not recorded|p150,Tb p153,154|Eifelian|Emsian|||||||
17618|Tabberabbera Formation|43871|14|Not recorded|p12-55||Early Devonian|||||||
17618|Tabberabbera Formation|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Unit in Wentworth Group.|||Marine: siltstone, sandstone, minor limestone.|
17618|Tabberabbera Formation|47037|6|Mentioned|p114|||||||||
17618|Tabberabbera Formation|48971|6|Mentioned|p10|||See also P40, P42.||||||
17618|Tabberabbera Formation|61161|5|Briefly described|p118-119, p76-77 Fig 6.1|||Of Wentworth Group.  Includes: Dead Bull Member underlying Kilgower Member, which underlies Roaring Mag Member. Overlies Wentworth Group - transitional boundary. Dominantly fine to medium-grained sandstone. Very poor outcrop. GSV map code: Dwt.||||||29-MAY-13
17618|Tabberabbera Formation|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Wentworth Group. Sandstone: arkosic to quartz arenite; medium to fine-grained; thin to thick-bedded; mudstone: well bedded; generally crumbly due to anastomosing cleavage. Shallow-marine deposits. GSV map code: Dwt.||||||14-SEP-05
17618|Tabberabbera Formation|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Wentworth Group. Sandstone: arkosic to quartz arenite; medium to fine-grained; thin to thick-bedded; mudstone: well bedded; generally crumbly due to anastomosing cleavage. Shallow-marine deposits. GSV map code: Dwt.||||||07-FEB-11
17618|Tabberabbera Formation|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Wentworth Group. Sandstone: arkosic to quartz arenite; medium to fine-grained; thin to thick-bedded; mudstone: well bedded; generally crumbly due to anastomosing cleavage. Shallow-marine deposits. GSV map code: Dwt.||||||14-SEP-05
17618|Tabberabbera Formation|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Wentworth Group. Sandstone: arkosic to quartz arenite; medium to fine-grained; thin to thick-bedded; mudstone: well bedded; generally crumbly due to anastomosing cleavage. Shallow-marine deposits. GSV map code: Dwt.||||||14-SEP-05
17618|Tabberabbera Formation|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Wentworth Group. Sandstone: moderate gravity response (-330 to -300 ums^-2); weakly magnetic (50 to 60 nT, k up to 650 x10^-6 cgs); low to moderate K, moderate Th, U and total radioelements. GSV map code: Dwt.||||||
17618|Tabberabbera Formation|61181|5|Briefly described|p127|Early Devonian|Early Devonian|Contains thin limestone beds associated with marine siltstone and sandstone. ||||||
17618|Tabberabbera Formation|61859|6|Mentioned|p26, p40|latest Pragian|early Emsian|Brachiopod species contrasted with that in Garra Limestone.||||||
17618|Tabberabbera Formation|63170|5|Briefly described|p229|||Of the Wentworth Group. In eastern Victoria. Conodonts.||||||07-FEB-11
17618|Tabberabbera Formation|68116|5|Briefly described|Appendix, Maps 35, 44.|Early Devonian|Early Devonian||||||Siltstone, sandstone, minor carbonate.|
17618|Tabberabbera Formation|69875|5|Briefly described|p262|||Eastern Victoria. Contains faunal elements in common with the Point Hibbs Formation in southwest Tasmania.||Wentworth Group.||||
37604|Tabor Volcanics|23309|5|Briefly described|p122,133, Table 2.45|||Of Dartella Volcanics.||||||
37604|Tabor Volcanics|24133|4|Described|p46|Devonian|Devonian|Parent: Dartella Volcanic Group.  Geological Province: Lachlan Fold Belt.||||||
37604|Tabor Volcanics|24142|5|Briefly described|Map Legend|Devonian|Devonian|Of Dartella Volcanic Group. Geological Province: Lachlan Fold Belt.||||||
37604|Tabor Volcanics|24143|5|Briefly described|Map Legend|Devonian|Devonian|Of Dartella Volcanic Group. Geological Province: Lachlan Fold Belt.||||||
37604|Tabor Volcanics|24144|5|Briefly described|Map Legend|Devonian|Devonian|Of Dartella Volcanic Group. Geological Province: Lachlan Fold Belt.||||||
37604|Tabor Volcanics|24145|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of Dartella Volcanic Group. Geological Province: Lachlan Fold Belt||||||
37604|Tabor Volcanics|24146|5|Briefly described|Map Legend|Devonian|Devonian|Of Dartella Volcanic Group. Geological Province: Lachlan Fold Belt.||||||
37604|Tabor Volcanics|24551|5|Briefly described|p149|Devonian|Devonian|Of the Dartella Volcanics.||||||
37604|Tabor Volcanics|60503|4|Described|p114, p41 Tb. 2|Early Devonian|Early Devonian|Of the Dartella Volcanics. Not recognised originally. Conformably underlying Murtagh Creek Ignimbrite. Crystal-rich vitric ignimbrite-dark with eutaxitic foliation. Thickness: 200m. Mag. suggest Tabor Volcanics may partly be Murtagh Creek Ignimbrite.||||||01-SEP-05
37604|Tabor Volcanics|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Dartella Volcanic Group. Lava and volcanogenic sediments: basaltic andesite, dark blue-green, minor unwelded felsic ignimbrite and tuff||||||
37604|Tabor Volcanics|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Lava and volcanogenic sediments: basaltic andesite, dark blue-green, minor unwelded felsic ignimbrite and tuff||||||
37604|Tabor Volcanics|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Dartella Volcanic Group. Lava and volcanogenic sediments: basaltic andesite, dark blue-green, minor unwelded felsic ignimbrite and tuff||||||
37604|Tabor Volcanics|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Dartella Volcanic Group. Lava and volcanogenic sediments: basaltic andesite, dark blue-green, minor unwelded felsic ignimbrite and tuff||||||07-OCT-04
37604|Tabor Volcanics|60508|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Dartella Volcanic Group. Basaltic andesite lava: highly magnetic (100-350 nT) flat lying; moderate total count, low K, Th, U especially in the east.||||||21-OCT-04
37604|Tabor Volcanics|68116|5|Briefly described|Appendix, Maps 20, 27.|Middle Devonian|Early Devonian||||||Lava and volcanigenic sediments: basaltic andesite, dark blue-green, minor unwelded felsic ignimbrite and ashstone.|
17652|Taggerty Subgroup|23229|6|Mentioned|p37|||||||||
17652|Taggerty Subgroup|23309|5|Briefly described|p162-166 Table 2.61|||||||||
17652|Taggerty Subgroup|24551|4|Described|p164|||Of Marysville Igneous Complex||||||
17652|Taggerty Subgroup|33602|6|Mentioned|p19|||||||||
17652|Taggerty Subgroup|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
17652|Taggerty Subgroup|35073|5|Briefly described|p8|||||||||
17652|Taggerty Subgroup|35112|6|Mentioned|p276|||||||||
17652|Taggerty Subgroup|35186|6|Mentioned|p3|||||||||
17652|Taggerty Subgroup|35277|5|Briefly described|p83|||||||||
17652|Taggerty Subgroup|38327|6|Mentioned|p564|||||||||
17652|Taggerty Subgroup|39291|6|Mentioned|Fig.14|||See also Table 1||||||
17652|Taggerty Subgroup|40725|6|Mentioned|Fig.1|||||||||
17652|Taggerty Subgroup|41641|5|Briefly described|p162|||||||||
17652|Taggerty Subgroup|44187|5|Briefly described|Map Legend||Late Devonian|||||||
17652|Taggerty Subgroup|65900|5|Briefly described|p161|||Includes thin magnetic volcanic unit of basalt and andesite near the base.  Cerberean Cauldron area. ||||||
17652|Taggerty Subgroup|68116|5|Briefly described|Appendix, Maps 33, 42.|Late Devonian|Late Devonian||||||Felsic ignimbrites, basalt and andesite lavas, conglomerate, sandstone.|
17652|Taggerty Subgroup|68311|6|Mentioned|p273-274, 279|Late Devonian|Late Devonian|Cerberean Cauldron, Central Victoria. Pre-collapse phase.|||Wightmans Hill Conglomerate; Snobs Creek, Robleys Spur, Volcanics; Blue Range Formation; Torbreck Range Andesite.|||
17652|Taggerty Subgroup|70742|5|Briefly described|p163|Late Devonian|Late Devonian|Cerberean Cauldron, S of Lake Eildon.||Marysville Igneous Complex.||||
22936|Tailor Creek Tonalite|22756|5|Briefly described|P46|||||||||
22936|Tailor Creek Tonalite|23309|6|Mentioned|p443, App1|||G365 I-Type.||||||
22936|Tailor Creek Tonalite|43260|5|Briefly described|Map Legend||Early Devonian|Of the Glenlogie Suite. Hornblende tonalite: mafic, medium to coarse grained; light green to dark greenish grey; speckled appearance; some parts very rich in hornblende.||||||24-JUN-14
22936|Tailor Creek Tonalite|44186|5|Briefly described|Map Legend||Early Devonian|G365 I-type.||||||
22936|Tailor Creek Tonalite|66002|5|Briefly described|p7 Tb.5|||Of Glenlogie Suite. G365.  Defined by Cayley and McDonald 1995.||||||
22936|Tailor Creek Tonalite|68116|5|Briefly described|Appendix, Map 31.|Early Devonian|Early Devonian||||||Hornblende tonalite: mafic; medium to coarse grained: light green to dark greenish grey; speckled appearance; some parts very rich in hornblende.|
39634|Tait Sandstone|24088|6|Mentioned|p355 Fig. 4||| Geological Province: Lachlan Fold Belt.||||||
17667|Talbot Drive Granodiorite|24551|6|Mentioned|p223|||See also Mount Stinton Granodiorite.||||||
17667|Talbot Drive Granodiorite|42154|6|Mentioned|Table 1 P334|||||||||
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||||||
72967|Tallangatta Porphyry|61186|5|Briefly described|p66|||Dimension stone. Occurs as acid dykes. Rock from red-brown to green, with classic porphyritic texture with large cream to white rhombic-shaped feldspars, often zoned with white cores, and corroded quartz set in a finer grained matrix.||||||
17710|Tally Ho Quartz Diorite|33598|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
17710|Tally Ho Quartz Diorite|33599|6|Mentioned|p10|||U.Dev.||||||
34811|Tambo Crossing Tonalite|22968|5|Briefly described|P15, Table7, P207||Early Devonian|Age of unit is 402+/-12 Ma, parent is Ensay Suite||||||
34811|Tambo Crossing Tonalite|23028|5|Briefly described|Map legend|Lochkovian|Pridoli|Parent is Ensay Suite.||||||25-SEP-08
34811|Tambo Crossing Tonalite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent is the Ensay Suite.||||||25-SEP-08
34811|Tambo Crossing Tonalite|23309|6|Mentioned|p443 App 1|||Supersedes the Tambo Crossing Granodiorite.||||||
34811|Tambo Crossing Tonalite|23938|6|Mentioned|p73 Fig. 26|||||||||
34811|Tambo Crossing Tonalite|24551|5|Briefly described|p152 Fig. 5.42|Devonian|Silurian|||||||
34811|Tambo Crossing Tonalite|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|I-type.||||||
34811|Tambo Crossing Tonalite|68116|5|Briefly described|Appendix, Maps 35, 44.|Early Devonian|Ludlow||||||Biotite-hornblende tonalite: grey; medium to coarse-grained; porphyritic in hornblende; weakly to moderately foliated.|
26924|Tambo River Formation|23230|5|Briefly described|Table4-1p40|||||||||
26924|Tambo River Formation|23768|5|Briefly described|p28 Fig.5|Middle Miocene|Middle Miocene|Overlain by Jemmys Point Formation.  Geological Province: Gippsland Basin.  See also p34,93,137,141.||||||29-MAR-05
26924|Tambo River Formation|23909|5|Briefly described|p298|Miocene|Miocene|Of Seaspray Group.  Geological Province: Gippsland Basin.  See also p290 Fig. 3.||||||
26924|Tambo River Formation|24053|4|Described|p38|Late Miocene|Late Miocene|Formerly Tambo Formation. Of Seaspray Group. Geological Basin: Gippsland Basin.||||||01-JUL-08
26924|Tambo River Formation|24164|6|Mentioned|p22 Fig.14|||Drill hole cross-section along Ninety Mile Beach.||||Is overlain by Jemmy's Point Formation; overlies Gippsland Limestone Formation||
26924|Tambo River Formation|24468|5|Briefly described|p405 Fig.2|Miocene|Miocene|Geological Province: Gippsland Basin. Of the Albacore Subgroup. Max Thickness: 33m||||||
26924|Tambo River Formation|24551|5|Briefly described|p327 Fig. 10.33, p328|Miocene|Miocene|Of the Seaspray Group.||||||
26924|Tambo River Formation|29355|6|Mentioned|p185|||||||||
26924|Tambo River Formation|30093|6|Mentioned|p19|||||||||
26924|Tambo River Formation|31351|6|Mentioned|Table 1|||||||||
26924|Tambo River Formation|31352|6|Mentioned|p134|||Refers Carter (1964)||||||
26924|Tambo River Formation|31509|6|Mentioned|p155|||||||||
26924|Tambo River Formation|31627|6|Mentioned|p12|||||||||
26924|Tambo River Formation|32157|6|Mentioned|Fig. 9.8|||||||||
26924|Tambo River Formation|33238|5|Briefly described|p644|||||||||
26924|Tambo River Formation|33459|6|Mentioned|Table 1|||||||||
26924|Tambo River Formation|33689|5|Briefly described|p13|||||||||
26924|Tambo River Formation|33929|6|Mentioned|p71|||||||||
26924|Tambo River Formation|34519|6|Mentioned|p47|||||||||
26924|Tambo River Formation|34558|5|Briefly described|p19|||||||||
26924|Tambo River Formation|34842|6|Mentioned|p11|||||||||
26924|Tambo River Formation|34843|6|Mentioned|p10|||||||||
26924|Tambo River Formation|34954|6|Mentioned|Fig.35|||||||||
26924|Tambo River Formation|35271|6|Mentioned|Fig.2|||||||||
26924|Tambo River Formation|35273|3|Fully described|p261|||||||||
26924|Tambo River Formation|35720|6|Mentioned|p131|||See also Fig.2, stratigraphic column.||||||
26924|Tambo River Formation|37330|5|Briefly described|Table 4|||||||||
26924|Tambo River Formation|38070|6|Mentioned|Fig.12|||Gippsland Basin||||||
26924|Tambo River Formation|38929|4|Described|p48|||See also Fig.6||||||
26924|Tambo River Formation|41043|5|Briefly described|p97|||||||||
26924|Tambo River Formation|41075|6|Mentioned|p24|||||||||
26924|Tambo River Formation|41511|4|Described|p14|||||||||
26924|Tambo River Formation|41537|6|Mentioned|Fig.2|||||||||
26924|Tambo River Formation|41868|6|Mentioned|Fig.12.14|||||||||
26924|Tambo River Formation|42371|6|Mentioned|p38|late Miocene||||||||
26924|Tambo River Formation|42824|6|Mentioned|p267|||||||||
26924|Tambo River Formation|42827|3|Fully described|p335|||see also Fig 8.21||||||
26924|Tambo River Formation|43667|6|Mentioned|Fig.3,p12||Late Miocene|||||||
26924|Tambo River Formation|45128|6|Mentioned|Fig.42|||Correlation table of sediments containing Dromornithidae in Australia.||||||
26924|Tambo River Formation|48631|5|Briefly described|p4,5,Pl.1,sh1||Late Miocene|(J/55-11). Upper Miocene.||||||
26924|Tambo River Formation|60538|5|Briefly described|p482 Fig. 21, 483 Fig. 22|||Geological Province: Gippsland Basin.||||||
26924|Tambo River Formation|60785|5|Briefly described|p184 Fig.1, p193 .|Messinian|Tortonian|Of the Gippsland Basin. Planktonic foraminifera zone N16-N17. Sr/Sr dates average 6.0 Ma for the top of the type section at Swan Reach (Dickinson, 2002). Has yielded fossil cetacean elements.|||||Uniform marl and marly limestone, and glauconitic sandy coquinas.|
26924|Tambo River Formation|61155|5|Briefly described|p5, p18|Late Miocene|Late Miocene|Of the Seaspray Group. Marginal-marine glauconitic marls. Overlain by Jemmys Point Formation. Max. thickness: 300m. Geological Province: Gippsland  Basin SE onshore). ||||||
26924|Tambo River Formation|61207|5|Briefly described|p280 Fig. 2, p288-|Late Miocene|Late Miocene|Strandplain sediments consisting of glauconitic and phosphatic marls. Underlies Jemmys Point Formation. Age: N17-18 from foraminifera, 6.6-5.3 Ma from Sr isotopes at Swan Reach. Geological Province: onshore Gippsland Basin. See also p289.||||||23-SEP-18
26924|Tambo River Formation|61302|5|Briefly described|p11 Fig.4|Miocene|Miocene|Of the Seaspray Group. Geological Province: Gippsland Basin. See also p90 Figs. 37b and 37c Appendix 1.||||||
26924|Tambo River Formation|61336|5|Briefly described|p(v) Fig. 5|Middle Miocene|Early Miocene|Geological Province: Gippsland Basin.||||||07-FEB-11
26924|Tambo River Formation|62899|5|Briefly described|p37 Fig. 2|||Geological province: Lakes Entrance Platform.||||||
26924|Tambo River Formation|63217|5|Briefly described|p97 Fig.2, p102 Fig.6.|||Lateral equivalent to Boisdale Formation.||||Overlies Wuk Wuk Marl Formation. Is overlain by Haunted Hills Formation. Is unconformably overlain by Jemmys Point Formation.||
26924|Tambo River Formation|63739|5|Briefly described|p37 Fig. 2|||Geological province: Gippsland Basin.||||||01-JUL-08
26924|Tambo River Formation|65717|6|Mentioned|p12|Pliocene|Miocene|Part of unnamed marine sequence (p12)||||||
26924|Tambo River Formation|65718|5|Briefly described|p10 Fig 3.2, p12, p17 Fig 3.6|Pliocene|Miocene|Middle Miocene minimum age.||Of the Seaspray Group.||||
26924|Tambo River Formation|67061|6|Mentioned|p554 Fig.10.|Miocene|Miocene|Gippsland Basin, onshore.||Unit in Seaspray Group.||Overlies Bairnsdale Limestone.||
26924|Tambo River Formation|69016|5|Briefly described|p88-89|||Of the Gippsland Basin. Thickness: ~110m. Marine deposit restricted to the eastern part of the basin. Aquitard.||Unit of Seaspray Group.|||Glauconite marls and marly limestones.|
26924|Tambo River Formation|70028|6|Mentioned|p79|Miocene|Miocene|Onshore Gippsland Basin.||||||
26924|Tambo River Formation|70076|5|Briefly described|Regional: Fig.3|Messinian|Tortonian|||Seaspray Group.||Overlies Bairnsdale Limestone. Is overlain by Jemmys Point Formation.||
26924|Tambo River Formation|70862|6|Mentioned|p48 Fig.1|||Latrobe Valley, Gippsland Basin.||Seaspray Group.||Overlies Bairndsale Limestone.||
26924|Tambo River Formation|70995|14|Not recorded|p156||Late Miocene|||||||
26924|Tambo River Formation|73289|6|Mentioned|p765 Fig.2|||||||Overlies Wuk Wuk Marl. Is overlain by Jemmys Point Formation.||16-MAY-23
26924|Tambo River Formation|73488|6|Mentioned|p634 Fig.4|||||||||
77280|Tamboon Road Granite|68115|5|Briefly described|p6.|||Originally Tamboon Granite (VandenBerg, 1999). Name changed to Tamboon Road Granite to avoid confusion: Tamboon township lies within Everard Granite, but the unit in question is crossed by the Tamboon Road, after which it is thus named.||||||
77280|Tamboon Road Granite|68116|5|Briefly described|Appendix, Map 46.|Early Devonian|Early Devonian||||||Biotite granite: pinkish, equigranular, felsic; I-type.|
17743|Tamboon Suite|24551|6|Mentioned|p235|||||||||
17743|Tamboon Suite|42726|5|Briefly described|map legend||Early Devonian|of the Bemboka Supersuite.  Contains the Tamboon Granite.||||||08-FEB-05
17743|Tamboon Suite|42827|6|Mentioned|p430|||||||||
17751|Taminick Gap Granite|22971|5|Briefly described|p 34|||||||||
17751|Taminick Gap Granite|23309|5|Briefly described|p444 App1|||G204 S-Type.||||||27-AUG-04
17751|Taminick Gap Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
17751|Taminick Gap Granite|68116|5|Briefly described|Appendix, Map 19.|Late Devonian|Late Devonian||||||Biotite granite: very coarse grained, pale grey; S-type.|
37783|Tan-Y-Bryn Granite|23309|6|Mentioned|p444 App1|||G393, I-Type.   See also Tan-Y-Byrn granite.||||||
37782|Tanjil Granodiorite|23309|6|Mentioned|p441 Appendix 1|||G237, I-Type. Supersededs Tanjil Granite.||||||
37782|Tanjil Granodiorite|44187|5|Briefly described|Map Legend|Late Devonian|Late Devonian|G237 I-type||||||
37782|Tanjil Granodiorite|68116|5|Briefly described|Appendix, Map 43.|Late Devonian|Late Devonian||||||Granodiorite: medium grained, equigranular, hornblende-bearing.|
27581|Taparoo Sandstone|22773|5|Briefly described|Fig24.5p350|Early Cretaceous|Early Cretaceous|||||||
27581|Taparoo Sandstone|22887|3|Fully described|Fig.5 p12, p31|Early Cretaceous|Early Cretaceous|Proposed equivalent to sedimentary units in Booligal. Renmark Trough.||||||
27581|Taparoo Sandstone|22893|5|Briefly described|p22,23||Early Cretaceous|Reffering to equivalents to this unit.||||||
27581|Taparoo Sandstone|24551|5|Briefly described|p270|||Of the Millewa Group. Underlies: Morkalla Formation.||||||
27581|Taparoo Sandstone|30905|5|Briefly described|p147|||||||||
27581|Taparoo Sandstone|31745|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
27581|Taparoo Sandstone|37873|6|Mentioned|p1|||||||||
27581|Taparoo Sandstone|39211|6|Mentioned|p38|||See Fig.23||||||
27581|Taparoo Sandstone|41642|5|Briefly described|p217|||||||||
27581|Taparoo Sandstone|42318|6|Mentioned|Fig.5 P12|||Murray Basin||||||
27581|Taparoo Sandstone|42827|5|Briefly described|Table 7.3|||of Millewa Group||||||
27581|Taparoo Sandstone|42966|2|Defined|Table 9 p70|Aptian||of Millewa Group||||||
27581|Taparoo Sandstone|43218|4|Described|Fig.3 p22, p27|Aptian|Aptian|Of Millewa Group.||||||
27581|Taparoo Sandstone|44188|5|Briefly described|Map legend|Cretaceous|Cretaceous|Of the Millewa Group.  Mentioned in the context of equivalents. Sandy brown clay, fine-grained mature quartzose sandstone, fine- to medium-grained bimodal poorly sorted sand with traces of pyrite, blue-grey clay with gypsum. Siltstone, carbonaceous.......||||||
27581|Taparoo Sandstone|61314|5|Briefly described|p129|Cretaceous|Cretaceous|Fluvial deposits. Overlain by Morkalla Formation. Geological Province: eastern part of Murray Basin.||||||
30050|Tara Range Subgroup|22968|6|Mentioned|P132|||Parent is Snowy River Volcanics.||||||25-SEP-08
30050|Tara Range Subgroup|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Snowy River Volcanics.||||||25-SEP-08
30050|Tara Range Subgroup|23309|4|Described|p111 Table 2.40|||Of the Snowy River Volcanics.||||||22-FEB-10
30050|Tara Range Subgroup|23938|5|Briefly described|p102 Fig. 42|Devonian|Devonian|||||||
30050|Tara Range Subgroup|24551|4|Described|p143, 141 Fig. 5.32|||Of the Snowy River Volcanics.||||||28-JUL-05
30050|Tara Range Subgroup|43284|5|Briefly described|Map Legend||Early Devonian|Of Snowy River Volcanics||||||
30050|Tara Range Subgroup|43312|5|Briefly described|Map Legend||Early Devonian|||||||
30050|Tara Range Subgroup|43313|5|Briefly described|Map Legend||Early Devonian|Of Snowy River Volcanics.||||||25-SEP-08
30050|Tara Range Subgroup|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Unit in Snowy River Volcanics.|||Extrusive: ignimbrite, main flow deposits.|
30050|Tara Range Subgroup|60542|4|Described|p67, p14|Early Devonian|Early Devonian|Same as Mount Tara Sgp? Two previously mapped ignimbrites perhaps should be assigned to this subgroup are: Moonkan McRaes Ignimbrite and Slater Ignimbrite. Ignimbrites. Overlies Crohn Granite. Thickness: >900m. Geo. Prov: Waiwera Graben. ||||||
30050|Tara Range Subgroup|61187|5|Briefly described|p157. |||Sediments and volcanics in-filling the Wairewa Graben, east of the main Buchan Rift. Hosts the Three Mile iron-copper prospect. See also reference to Tara Subgroup p150.||Unit in Snowy River Volcanics.|||Quartz ignimbrites and volcanic derived sediments.|
30050|Tara Range Subgroup|68115|5|Briefly described|p4.|Devonian|Devonian|The Yellow Waterholes Ignimbrite was included in this unit by VandenBerg et al. (2000); previously of the Little River Subgroup (Orth et al. 1995).||Unit in Snowy River Volcanic Group.|Includes Yellow Waterholes Ignimbrite.|||
30050|Tara Range Subgroup|68116|5|Briefly described|Appendix, Map 45.|Pragian|Pragian|Contains minor basalt lava and flows.|||||Quartz ignimbrite: crystal rich, medium to coarse-grained, red, densely welded; minor volcanigenic sediments including mudstone and sandstone with accretionary lapilli, tabular cross-bedded sandstone; pyroclastic and epiclastic rocks.|
30542|Taravale Marlstone|22968|4|Described|P15, Fig49, P153|Devonian|Devonian|Nonmagnetic, maximum thickness of 3000m, conformably overlies Buchan Caves Limestone.||||||25-SEP-08
30542|Taravale Marlstone|23309|4|Described|p117-132 Table 2.41|||Of the Buchan Group.||||||22-FEB-10
30542|Taravale Marlstone|23615|3|Fully described|p140|Middle Devonian|Middle Devonian|Of Buchan Group.  Formerly Taravale Formation. Overlain by Murrindal Limestone, overlies Buchan Caves Limestone.  Maximum thickness: 600m.  See also p216 App.1.||||||
30542|Taravale Marlstone|23938|5|Briefly described|p102 Fig. 42|Devonian|Devonian|||||||
30542|Taravale Marlstone|24551|4|Described|p147, 139 Fig. 5.30, p547|Early Devonian|Early Devonian|Of the Buchan Group.||||||
30542|Taravale Marlstone|43206|5|Briefly described|map legend|Emsian|Emsian|Of Buchan Group.||||||25-SEP-08
30542|Taravale Marlstone|43228|5|Briefly described|p10||Early Devonian|||||||
30542|Taravale Marlstone|43312|5|Briefly described|Map Legend||Emsian|Of Buchan Group.||||||25-SEP-08
30542|Taravale Marlstone|43313|5|Briefly described|Map Legend||Pragian|Of Buchan Group.||||||25-SEP-08
30542|Taravale Marlstone|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Unit in Buchan Group.|||Marine: dark grey-green marlstone.|
30542|Taravale Marlstone|60542|5|Briefly described|p82, p15|Emsian|Emsian|Of Buchan Group. Relationship with name Taravale Formation isnt clear. Impure limestones, mudstone and nodular limestone. Transitional with Buchan Caves Limestone below. Max. thickness: 780m.||||||
30542|Taravale Marlstone|66197|5|Briefly described|p635 Fig.5c|Emsian|Emsian|Buchan Basin. Shallow marine marlstone. Overlies the Buchan Caves Limestone.||||||13-MAR-12
30542|Taravale Marlstone|68116|5|Briefly described|Appendix, Maps 35, 45.|Emsian|Emsian||||||Marlstone, mudstone, nodular limestone, calcareous siltstone and minor dolomite; blue-grey, green grey to pale brown and white with dark limestone nodules, poorly to well bedded.|
17856|Tarlton Granite|23309|6|Mentioned|p444 App1|||G41 I-Type.||||||
17856|Tarlton Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
17856|Tarlton Granite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|I-type. Medium to coarse grained hornblende, biotite / muscovite, biotite granite, high internal variability.||||||22-OCT-04
17856|Tarlton Granite|43315|5|Briefly described|Map Legend|Wenlock|Wenlock|I-type granite. medium- to coarse-grained hornblende, biotite/muscovite, biotite granite, high internal variability.||||||03-MAY-05
17856|Tarlton Granite|60541|4|Described|p70, p73|||Intrusive within the Kuark Metamorphic Complex. I-type granite. Small part of this unit was previously known as "Tarlton Granodiorite" (Dodd 1981).||||||
17856|Tarlton Granite|68116|5|Briefly described|Appendix.|Devonian|Silurian||||||Granite, composition variable: hornblende, biotite and muscovite; medium to coarse-grained; I-type.|
17856|Tarlton Granite|72711|6|Mentioned|p3 Fig.2.|Paleoproterozoic|Paleoproterozoic|Shown only on p3 Fig.2. From the interpretive geology map of the Jervois Range Special (modified from Weisheit et al 2019). Shown as part of the Aileron Province.|||||Includes granite.|
31647|Tarlton Suite|42726|5|Briefly described|Map Legend||Early Devonian|||||||
35567|Tarnagulla Granodiorite|23260|5|Briefly described|Fig12-6.4p261||Early Devonian|||||||
35567|Tarnagulla Granodiorite|23603|4|Described|p17|Early Devonian|Early Devonian|||||||
35567|Tarnagulla Granodiorite|23604|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
35567|Tarnagulla Granodiorite|23605|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
35567|Tarnagulla Granodiorite|23606|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
35567|Tarnagulla Granodiorite|23607|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Granodiorite: medium, even grained; composite pluton; minor pegmatites developed and fine grained sills.||||||12-NOV-04
35567|Tarnagulla Granodiorite|23810|5|Briefly described|Fig 3. p889||Devonian|Lachlan Fold Belt.||||||
35567|Tarnagulla Granodiorite|24178|4|Described|p19, 68, 69|||Divided into three separate units: Bullabul, Kangdegaar and Tarnagulla Granodiorites (White and Chappell, 1988)||||||03-FEB-15
35567|Tarnagulla Granodiorite|24326|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
35567|Tarnagulla Granodiorite|61369|5|Briefly described|p383|Early Devonian|Early Devonian|Part of the oxidised I-type Tarnagulla pluton (White and Chappell 1988). Medium- to coarse-grained, non-foliated granodiorite.  Age: 391+/-5My (K-Ar: Richards and Singleton 1981).||||||28-SEP-05
35567|Tarnagulla Granodiorite|65715|5|Briefly described|p8 Tb.4|||Superseded name for Tarnagulla Granite used by Marlow and Bushell (1995).||||||
35567|Tarnagulla Granodiorite|67804|5|Briefly described|p67|Middle Devonian|Middle Devonian|Contact metamorphoses auriferous quartz veins at Tarnagulla and Rheola.|396 +/- 4 Ma (U-Pb SHRIMP, Bierlein et al. 2001b)|||||
35567|Tarnagulla Granodiorite|68116|5|Briefly described|Appendix, Map 23.|Early Devonian|Early Devonian||||||Hornblende-biotite granodiorite: medium grained; minor pegmatite and aplite; variably magnetic.|
35567|Tarnagulla Granodiorite|73576|4|Described|p801-805, p807-810, p811-812, p814-822|Early Devonian|Early Devonian|Lachlan Fold Belt, Bendigo Zone. I-type. Poorly exposed, shows high magnetic response. Distinctive U-shape with internal pattern of nested concentric magnetic and non-magnetic phases in aeromagnetic data. Additional CA-ID-TIMS U-Pb zircon age of 401.28+/-0.11 Ma. Previously published SHRIMP U-Pb ages of 393+/-4 Ma and 396+/-4 Ma are younger and may reflect Pb loss. Includes Bullabul Phase in SW part.|406.08+/-0.17 Ma CA-ID-TIMS U-Pb zircon, 393+/-4Ma|||Hosted by Castlemaine Group|Medium- to coarse-grained, equigranular, massive granodiorite, with mafic enclaves in parts, includes an aplite phase.|
24012|Tarra River Formation|38929|4|Described|p53|||See also Fig.6||||||
24515|Tarrangatta Schist|37871|4|Described|p7|||||||||
24515|Tarrangatta Schist|39858|6|Mentioned|Map legend|Silurian|Ordovician|Silurian - Ordovician||||||
24014|Tarraville Member|38929|6|Mentioned|Fig.6|||||||||
17872|Tarringo Sandstone|34449|6|Mentioned|Table 2-1|||Invalid||||||
17893|Tatong Chert|32074|6|Mentioned|p178|||||||||
17893|Tatong Chert|70933|5|Briefly described|p89|||||||||
17904|Tawonga Gravels|24551|5|Briefly described|p338 Fig. 11.2, 340|Middle Pleistocene|Late Pliocene|||||||15-MAY-07
17904|Tawonga Gravels|31800|6|Mentioned|p210|||||||||
17904|Tawonga Gravels|37882|6|Mentioned|p6|||||||||
17904|Tawonga Gravels|41848|5|Briefly described|p357|||Late Pleistocene to Recent allavium. Spelt Tawonga Gravel diagram p353||||||
17904|Tawonga Gravels|42827|5|Briefly described|p357|||||||||
17904|Tawonga Gravels|42966|4|Described|p214|||||||||
17904|Tawonga Gravels|70910|14|Not recorded|p50|||Geological map.||||||
30587|Taylors Crossing Tonalite|43220|6|Mentioned|p11||Devonian|||||||
30587|Taylors Crossing Tonalite|44184|5|Briefly described|Map Legend||Early Devonian|||||||
30587|Taylors Crossing Tonalite|68116|5|Briefly described|Appendix, Map 27.|Silurian|Silurian||||||Biotite tonalite: grey; medium-grained; weakly foliated; occasional metasedimentary enclaves.|
83412|Tchum pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G606.||Of Glenloth Suite|||Granite, oxidised I-type; moderately magnetic (to 70 nT); gravity low to 80 micrometres/second/second below adjacent metasediments.|
34827|Teapot Creek Formation|22968|6|Mentioned|P33|||||||||
34827|Teapot Creek Formation|23021|5|Briefly described|Map legend|Triassic|Triassic|Parent is Mount Leinster Igneous Complex||||||
34827|Teapot Creek Formation|23030|5|Briefly described|Map legend|Triassic|Triassic|Parent is the Mount Leinster Igneous Complex||||||
34827|Teapot Creek Formation|23307|5|Briefly described|Map Legend|Triassic|Triassic|Of Mount Leinster Igneous Complex||||||
34827|Teapot Creek Formation|60503|3|Fully described|p131|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Volcaniclastic and volcanogenic sediments with trachyte lava. Metamorphosed. Unconformably on Omeo Metamorphic Complex and inferred to overlie Pinnak Sandstone. Intruded by Mole Hill Syenite. Max. thickness: ~100m.||||||24-JUN-14
34827|Teapot Creek Formation|60504|5|Briefly described|Map Legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Includes: Little Mount Tambo Trachyte Member. Fluvial and colluvial deposits: volcanogenic sandstone,conglomerate, breccia; with minor trachyte lava.||||||20-OCT-04
34827|Teapot Creek Formation|60505|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Includes: Little Mount Tambo Trachyte Member. Fluvial colluvial deposits: volcanogenic sandstone, conglomerate, breccia with minor trachyte lava.||||||21-OCT-04
34827|Teapot Creek Formation|60506|5|Briefly described|Map legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Includes: Little Mount Tambo Trachyte Member.  Fluvial colluvial deposits: volcanogenic sandstone, conglomerate, breccia with minor trachyte lava.||||||24-JUN-14
34827|Teapot Creek Formation|60507|5|Briefly described|Map Legend|Triassic|Triassic|Of the Mount Leinster Igneous Complex. Includes: Little Mount Tambo Trachyte Member. Fluvial colluvial deposits; volcanogenic sandstone, conglomerate, breccia, with minor trachyte lava.||||||21-OCT-04
34827|Teapot Creek Formation|60508|5|Briefly described|Map legend|Triassic|Triassic|Includes the Little Mount Tambo Trachyte Member. Fluvial and colluvial deposits: nonmagnetic sediments with highly magnetic (300 nT) trachyte; high total count, K, moderate Th, moderate to high U.||||||
34827|Teapot Creek Formation|68116|5|Briefly described|Appendix, Maps 27, 35.|Triassic|Triassic||||||Volcanigenic sandstone, conglomerate, breccia: marked variation from place to place; minor trachyte lava.|
30440|Teddy Bear Conglomerate Member|23309|5|Briefly described|p78|||Maximum Thickness: 15m.  Of the Serra Sandstone.||||||
30440|Teddy Bear Conglomerate Member|24551|5|Briefly described|p122|||Of the Mount Difficult Subgroup.||||||
30440|Teddy Bear Conglomerate Member|44929|5|Briefly described|Map Legend|Silurian|Ordovician|Of Serra Sandstone (Mount Difficult Sub-Group). Polymictic conglomerate, pale grey, poorly sorted.||||||14-JUN-06
30440|Teddy Bear Conglomerate Member|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Of Serra Sandstone (Mount Difficult Sub-Group, Grampians Group). Polymictic conglomerate, pale grey, poorly sorted.||||||13-JUN-06
30440|Teddy Bear Conglomerate Member|44932|5|Briefly described|Map Legend|Silurian|Ordovician|Of Serra Sandstone (Mount Difficult Sub-Group). Polymictic conglomerate, pale grey, poorly sorted.||||||14-JUN-06
30440|Teddy Bear Conglomerate Member|44933|5|Briefly described|Map Legend|Silurian|Ordovician|Of Serra Sandstone (Mount Difficult Sub-Group). Polymictic conglomerate.||||||14-JUN-06
30440|Teddy Bear Conglomerate Member|60456|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Mount Difficult Sub-Group. Polymictic conglomerate: pale grey, poorly sorted with open framework, abundant bedrock clasts.||||||
30440|Teddy Bear Conglomerate Member|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Mount Difficult Subgroup. Unit does not appear on this map.||||||
30440|Teddy Bear Conglomerate Member|61183|4|Described|p46, p47 Fig. 29|||Of Serra Sandstone (Grampians Gp). Distinctive marker horizon high, continuous, conformable within the unit. Polymictic conglomerate with angular dark mudstone clasts and lesser sub-rounded vein quartz clasts. Also referred to as Teddy Bear Conglomerate.||||||
30440|Teddy Bear Conglomerate Member|64541|5|Briefly described|Map Legend|Silurian|Silurian|Of Serra Sandstone, Mount Difficult Sub-group. Polymictic conglomerate: pale grey, poorly sorted with open framework with abundant bedrock clasts of angular dark slate and sub-rounded vein quartz and minor sub-rounded, cleaved and veined, sandstone.||||||07-FEB-11
30440|Teddy Bear Conglomerate Member|64610|5|Briefly described|Map legend|Silurian|Silurian|Of Serra Sandstone (Mount Difficult Subgp., Grampians Gp). Polymictic conglom: pale grey, poorly sorted + open framework with abundant bedrock clasts of angular dark slate and sub-rounded vein qtz+minor sub-rounded, cleaved/veined, med-gr. qtz.sst, etc.||||||11-NOV-08
30440|Teddy Bear Conglomerate Member|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Serra Sandstone.  Defined by Cayley & Taylor, 1997. ||||||
17920|Teddywaddy Granite|23309|5|Briefly described|p339|Early Devonian|Early Devonian|G335 S-Type. Age: 390+/-6Ma,  398+/-6 Ma||||||
17920|Teddywaddy Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
17920|Teddywaddy Granite|60491|4|Described|p40|Devonian|Devonian|Age: 390+/-6 Ma (K/Ar biotite). S-type. Intruded by basaltic? dykes.||||||
17920|Teddywaddy Granite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Glenloth Suite. Biotite cordierite granite: S-type, reduced; medium grained, weakly porphyritic; small rounded mafic enclaves up to 1cm in diameter.||||||
17920|Teddywaddy Granite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of the Glenloth Suite. Age: 390 +/- 6 Ma (K/Ar). Granite; reduced S-type; non-magnetic; gravity response lower than the host metasediments; K is relatively high over outcrop, Th lower and U similar to surrounds.||||||30-SEP-04
17920|Teddywaddy Granite|66002|5|Briefly described|p6 Tb.5|||Of Glenloth Suite. G335. Defined in Bibby and Moore 1998.||||||
17920|Teddywaddy Granite|68116|5|Briefly described|Appendix, Map 16.|Middle Devonian|Early Devonian||||||Biotite-muscovite granite: coarse to medium porphyritic; contains small mafic enclaves; S-type; nonmagnetic.|
17920|Teddywaddy Granite|68189|6|Mentioned|p42 App.2|||K-Ar ages from Richards & Singleton (1981).|398 +/- 6 and 390 +/- 6 Ma.|||||30-JUN-14
17927|Telbit Sandstone Member|35283|5|Briefly described|p54|||||||||
18035|The Bluff member|33156|6|Mentioned|p132|||||||||
25526|The Sisters Granite Porphyry|23710|14|Not recorded|p75|||Intrudes Mount Tambo Group.||||||
25526|The Sisters Granite Porphyry|33393|6|Mentioned|p164|||||||||
25526|The Sisters Granite Porphyry|34519|6|Mentioned|p46|||||||||
30430|Thermopylae Conglomerate|23309|5|Briefly described|p78 Table 2.27|||Maximum Thickness: 300m.  Of the Red Man Bluff Subgroup.||||||
30430|Thermopylae Conglomerate|24551|5|Briefly described|p122|||Basal unit of the Red Man Bluff Subgroup.||||||
30430|Thermopylae Conglomerate|44929|5|Briefly described|Map Legend|Silurian|Ordovician|Basal unit of Red Man Bluff Sub-Group (Grampians Group). Polymictic conglomerate; pale grey, poorly sorted.||||||14-JUN-06
30430|Thermopylae Conglomerate|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Man Bluff Sub-Group (Grampians Group). Polymictic conglomerate, pale grey, poorly sorted and variably rounded.||||||13-JUN-06
30430|Thermopylae Conglomerate|44932|5|Briefly described|Map Legend|Silurian|Ordovician|Basal unit of Red Man Bluff Sub-Group (Grampians Group). Polymictic conglomerate; pale grey, poorly sorted.||||||14-JUN-06
30430|Thermopylae Conglomerate|44933|5|Briefly described|Map Legend|Silurian|Ordovician|Basal unit of Red Man Bluff Sub-Group (Grampians Group).||||||14-JUN-06
30430|Thermopylae Conglomerate|60451|4|Described|p76, 79|Early Devonian|Ordovician|Of the Red Man Bluff Subgroup (Grampians Group). Type section in text. Maximum Thickness: ~300m. Poorly sorted polymictic conglomerate.||||||
30430|Thermopylae Conglomerate|60456|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Man Bluff Sub-Group. Polymictic conglomerate: pale grey, poorly sorted and variably rounded with an open framework of bedrock clasts of vein quartz and veined sandstone.||||||30-SEP-04
30430|Thermopylae Conglomerate|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Man Bluff Subgroup. Unit does not appear on this map.||||||
30430|Thermopylae Conglomerate|61183|4|Described|p28, p30 Tb. 2, p33, p106|||Lowest exposed unit of Red Man Bluff Subgroup (Grampians Gp). Med. to thick, massive, laminated or cross-bedded with pebbly lag horizons; poorly sorted polymictic conglomerate with bedrock clasts. Underlies Gariwerd Sandstone. Thickness: ~300m.||||||
30430|Thermopylae Conglomerate|64541|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Red Man Bluff Sub-group. Polymictic conglomerate: pale grey, poorly sorted and variably rounded with an open framework of bedrock clasts of vein quartz, quartz sandstone.||||||07-FEB-11
30430|Thermopylae Conglomerate|64610|5|Briefly described|Map legend|Ordovician|Ordovician|Of Red Man Bluff Subgroup (Grampians Gp). Polymictic conglom; pale grey, poorly sorted + variably rounded with open framework of bedrock clasts of vein quartz and veined, quartz sandstone; coarse-grained qtz-feldsp.sst matrix - more lithol. detail.||||||17-NOV-08
30430|Thermopylae Conglomerate|65313|6|Mentioned|p582 Fig.10|Ordovician|Ordovician|Grampians National Park sections. See also mis-spelling on  Fig.9.||Of  Red Man Bluff Subgroup.||Is overlain by Gariwerd Sandstone.||26-MAR-12
30430|Thermopylae Conglomerate|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Red Man Bluff Subgroup. Defined by Cayley & Taylor, 1997.||||||
30430|Thermopylae Conglomerate|68116|5|Briefly described|Appendix, Map 30.|Ludlow|Late Ordovician||||||Polymictic conglomerate: pale grey; massive; poorly sorted, open framework, variably rounded clasts: vein quartz and veined sandstone; matrix and interbeds of coarse-grained quartzofeldspathic sandstone; planar, cross laminated, thin to thick-bedded.|
37274|Thiele Igneous Complex|23309|5|Briefly described|p24-26, 282 Table 2.1|Cambrian|Cambrian|||||||
37274|Thiele Igneous Complex|24002|6|Mentioned|p242|||||||||
37274|Thiele Igneous Complex|24004|5|Briefly described|p275 Fig.2|Cambrian|Cambrian|||||||
37274|Thiele Igneous Complex|24551|4|Described|p91|Silurian|Middle Cambrian|||||||
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||
18076|Thomson Siltstone|37727|4|Described|p88|||||||||
18076|Thomson Siltstone|38787|6|Mentioned|p139|||||||||
18076|Thomson Siltstone|39331|6|Mentioned|Table 2-1|||||||||
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.|
76919|Thorpdale Volcanic Group|66244|4|Described|p5, p6.|Miocene|Eocene|First shown on Warragul 1:250 000 Geological map (Geological Survey of Victoria, 1971) as Thorpdale Volcanics. Covers a large area around the Strzelecki Ranges. Apparently continuous in outcrop and magnetic data with Carrajung Volcanic Group to the east; their boundary is arbitrary.|49 - 22 Ma (Wellman 1974).|||Overlies unconformably the Wonthaggi Formation. Is interbedded with the La Trobe Valley Group.|Tholeiitic and alkali basalt, minor nephelinite, basanite, nepheline hawaiite, hawaiite, nepheline mugearite, mugearite, tuff and interbedded sandstone and silcrete.|11-FEB-15
76919|Thorpdale Volcanic Group|68116|5|Briefly described|Appendix, Maps 42, 51-52, 56-57.|Miocene|Paleocene||||||Tholeiitic and alkalic basalt; minor nephelinite, basanite, nepheline hawaiite, hawaiite, mugearite, nepheline mugearite, tuff, interbedded sandstone and silcrete.|
37785|Thowgla Creek Granite|23309|6|Mentioned|p444, Appendix 1|||G569, S-Type.||||||
37785|Thowgla Creek Granite|24133|3|Fully described|p62|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37785|Thowgla Creek Granite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37785|Thowgla Creek Granite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37785|Thowgla Creek Granite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37785|Thowgla Creek Granite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Biotite-corderite granite: brownish grey, medium to coarse grained; mostly porphyritic in K-feldspar; S-type; nonmagnetic.||||||09-SEP-04
37785|Thowgla Creek Granite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Biotite-corderite granite:S-type; nonmagnetic; high K, high Th, moderate to low U.||||||09-SEP-04
37785|Thowgla Creek Granite|68116|5|Briefly described|Appendix, Map 20.|Pridoli|Wenlock||||||Biotite cordierite granite: brownish grey, medium to coarse grained; mostly porphyritic in K-feldspar; S-type; nonmagnetic.|26-JUN-14
18109|Thurra Granodiorite|41850|6|Mentioned|p430|||||||||
79581|Thylacine Member|69651|5|Briefly described|p32-33|Late Cretaceous|Late Cretaceous|Cliff et al. (2004). Economically important reservoir. Appears on p15 as Thylacine Sandstone Member.||Belfast Mudstone.||||17-JUN-20
79581|Thylacine Member|69879|5|Briefly described|p424|Santonian|Santonian|Otway Basin. Major hydrocarbon reservoir for Thylacine gas-condensate field.||Belfast Formation|||Fluvio-deltaic sandstone.|
79581|Thylacine Member|73594|5|Briefly described|p16, p24-25, p27, p67|Santonian|Santonian|Otway Basin. Marine and marginal marine. Appears to be locally restricted to the eastern flank of the Shipwreck Trough. Important reservoir in the offshore Geographe and Thylacine gas fields. Not intersected in onshore parts. The Coniacian stage is absent between the Flaxman Formation and Thylacine Member. Extent interpreted to be controlled by the Sorell Fault Zone. Prograded westwards during the late Santonian (O. porifera microplankton zone) into the Shipwreck Trough.||Belfast Mudstone||Unconformably overlies Flaxman Formation|Fine to medium grained sandstones, well sorted litharenites and sub-litharenites. Base marked by a mass-flow deposit comprising upwards-fining argillaceous sandstones, passes upwards into one or more coarsening upwards cycles.|
18118|Tiac Granite|23309|6|Mentioned|p444 App1|||G307 I-Type.||||||
18118|Tiac Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
18118|Tiac Granite|66002|5|Briefly described|p6 Tb.5|||Of Beckworth Suite.G307. Includes the Warrawidgee and Mount Emu (Barralin) granites of White and Chappell (1988). Part of Tiac Granite of White and Chappell (1988) incorporated into Illoura Granodiorite.||||||
18118|Tiac Granite|68116|5|Briefly described|Appendix, Map 40.|Late Devonian|Late Devonian||||||Coarse-grained equigranular biotite granite; cream coloured.|
18150|Tildesley Sandstone|41511|4|Described|p14|||Mention Fig.2||||||
30554|Timbarra Subgroup|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Snowy River Volcanics||||||
30554|Timbarra Subgroup|23309|4|Described|p112. Table 2.40|||Of the Snowy River Volcanics.  Interfingers with the Tara Range Subgroup.  Statham Ignimbrite is Intercalated in places.||||||22-FEB-10
30554|Timbarra Subgroup|23615|3|Fully described|p87, p22|Early Devonian|Early Devonian|Of Snowy River Volcanics.  Upgrade of Timbarra Fm. recognising Wilkinson Cr. Conglomerate, Windarra Fm., Scorpion Creek Sandstone, Johnson Mudstone, Dicks Cr. Ignimbrite and Dinner Hill Gap Lava. Overlain by Yellow Waterholes Ignimbrite.  Age:  Early Devonian ~410-395Ma.||||||16-AUG-18
30554|Timbarra Subgroup|23938|5|Briefly described|p105 Fig. 45|Devonian|Devonian|Extrusive, fluvial, marine. ||||||
30554|Timbarra Subgroup|24551|4|Described|p142, 141 Fig. 5.32|||Of the Snowy River Volcanics||||||
30554|Timbarra Subgroup|43206|5|Briefly described|map legend||Ludlow|Of Snowy River Volcanics.||||||
30554|Timbarra Subgroup|43312|5|Briefly described|Map Legend||Early Devonian|Of Snowy River Volcanics.||||||25-SEP-08
30554|Timbarra Subgroup|43313|5|Briefly described|Map Legend||Early Devonian|of Snowy River Volcanics.||||||25-SEP-08
30554|Timbarra Subgroup|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Unit in Snowy River Volcanics.|||Extrusive, fluvial, marine: ignimbrite, lava, conglomerate, sandstone, polymictite.|
30554|Timbarra Subgroup|60542|3|Fully described|p50, p18|Devonian|Devonian|Of Snowy River Volcanics. Includes: Windarra, Mount Johnson and Davidsons Lane formations. Shows a strong lateral facies change, from a large fan delta in Mount Johnson area in north, to deeper water sediments in south. ||||||
30554|Timbarra Subgroup|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Breccia, conglomerate, sandstone, siltstone, ash, ignimbrite.|
26944|Timboon Sandstone|12781|6|Mentioned|p386|Late Cretaceous|Late Cretaceous|Otway Basin. Maximum thickness 1590m.||Sherbrook Group.||Unconformably overlies Waarre Formation. Abuts Flaxman and Paaratte Formations. Is overlain unconformably by Pebble Point Formation.||
26944|Timboon Sandstone|12796|5|Briefly described|p460, p456 Fig. 2|Maastrichtian|Campanian|Of the Sherbrook Group. Overlies Paarratte Formation; interfingers with and overlain partially by Wiridjil Gravels; also overlain by Massacre Shale. Geological Province: Otway Basin. ||||||
26944|Timboon Sandstone|22470|5|Briefly described|p13 Fig. 17|Maastrichtian|Campanian|Of Sherbrook Group.||||||
26944|Timboon Sandstone|24314|5|Briefly described|p61 Fig.2||Turonian|Geological Province: Otway Basin. Max. Thickness 1590m. Of the Sherbrook Subgroup.||||||30-NOV-04
26944|Timboon Sandstone|24551|6|Mentioned|p245|||Of the Sherbrook Group.||||||
26944|Timboon Sandstone|24562|5|Briefly described|p3, 8|Late Cretaceous|Late Cretaceous|Of the Sherbrook Group.  Geological Province: Otway Basin.||||||
26944|Timboon Sandstone|42361|3|Fully described|p17|Turonian||||||||
26944|Timboon Sandstone|42545|6|Mentioned|p19|||Otway Basin||||||
26944|Timboon Sandstone|43195|5|Briefly described|Map Legend||Late Cretaceous|See also commentary on back of map. Of Sherbrook Group.||||||
26944|Timboon Sandstone|43219|5|Briefly described|Fig.3,p6.|Maastrichtian|Campanian|Of Sherbrook Group.||||||14-APR-08
26944|Timboon Sandstone|43733|6|Mentioned|Fig.2.11,p65||Late Cretaceous|||||||
26944|Timboon Sandstone|43814|6|Mentioned|Fig.3,p115|||||||||
26944|Timboon Sandstone|44133|4|Described|p147|Maastrichtian|Santonian|Of the Sherbrook Group. Geological Province: Otway Basin. Unconformably overlain by Dilwyn Formation. Thickness: 1590m. ||||||
26944|Timboon Sandstone|61017|5|Briefly described|p5 Fig. 2|Maastrichtian|Campanian|Of the Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
26944|Timboon Sandstone|61230|5|Briefly described|p319 Fig.2, p329. |Maastrichtian|Campanian|Delta front to delta plain progradational depositional settings.||Unit in Sherbrook Group.||Overlies Paaratte Formation.|Sandstone, mudstone; increasingly sandstone-dominated up-unit to coarse sandstone and conglomerate.|
26944|Timboon Sandstone|61470|5|Briefly described|p28 Fig. 5|Maastrichtian|Campanian|Of the Sherbrook Group. Overlies Skull Creek Formation; underlies Massacre Shale. Geological Province: Otway Basin.||||||12-OCT-05
26944|Timboon Sandstone|61547|6|Mentioned|p461 Fig.2, p462. |Maastrichtian|Turonian|||Unit in Sherbrook Group.||Overlies Waarre Sandstone. Is overlain by Pebble Point Formation.||
26944|Timboon Sandstone|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
26944|Timboon Sandstone|61623|6|Mentioned|p449 Fig. 4|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
26944|Timboon Sandstone|61625|5|Briefly described|p475, p476 Fig. 1, p477, p480, p483|Late Creatceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin. Fine to very corase-grained sandstones, lacks bioturbated horizons and contains leaf fossils.||||||07-FEB-11
26944|Timboon Sandstone|61626|5|Briefly described|p486, p486 Fig. 2|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
26944|Timboon Sandstone|61627|5|Briefly described|p500 Fig. 2|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
26944|Timboon Sandstone|61628|5|Briefly described|p509 Fig. 3|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
26944|Timboon Sandstone|63122|5|Briefly described|p17 Fig. 4.3|Maastrichtian|Turonian|Of the Sherbrook Group. Max. thickness: 1590m. Geological Province: Otway Basin. ||||||
26944|Timboon Sandstone|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p82-84|Maastrichtian|Santonian|Supersedes all former Timboon nomenclature, incl: T.Sst Mbr, T.Sand, Curdies Fm and C. Beds, T. Sand and T.Sand Member. Unconform.below Wangerrip Group. Max.thick:1590m. Geol.Prov: Otway Basin. Of Sherbrook Gp in SA; in VIC is upper member of Paaratte Fm.||||||
26944|Timboon Sandstone|63129|5|Briefly described|p137|||Geological Province: Otway Basin. Offshore, this unit passes laterally into the interbedded shale-sand facies of Paaratte Formation. ||||||
26944|Timboon Sandstone|63269|5|Briefly described|p605|Late Cretaceous|Late Cretaceous|Otway Basin.||Sherbrook Group.||||
26944|Timboon Sandstone|63431|5|Briefly described|p677 Fig. 2|Maastrictian|Turonian|Of the Sherbrook Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
26944|Timboon Sandstone|66245|5|Briefly described|p6 Fig.5, p64 Fig.C6.|Maastrichtian|Campanian|The top of this unit is used to correlate well logs in this study.||Unit in Sherbrook Group.||Overlies Paaratte Formation.|Fluvial sandstones and floodplain claystones and some coals.|
26944|Timboon Sandstone|67061|6|Mentioned|p546 Fig.3.|Maastrichtian|Campanian|||Unit in Sherbrook Group.||Overlies Paaratte Formation.||15-MAR-12
26944|Timboon Sandstone|67366|5|Briefly described|p103 Fig.2. |Maastrichtian|Campanian|||Topmost unit in Sherbrook Group.||Overlies Paaratte Formation and Skull Creek Mudstone. Is unconformably overlain by Massacre Shale.|Marginal marine and lower coastal plain sandstone and mudstone.|
26944|Timboon Sandstone|67367|5|Briefly described|p131 Fig.2. |Maastrichtian|Campanian|||Unit in Sherbrook Group.||||
26944|Timboon Sandstone|69297|5|Briefly described|p79, p98|Maastrichtian|Campanian|Otway Basin. ||Sherbrook Group||Faulted against or overlies the Paaratte Formation. Overlain by the Massacre Shale, Wiridjil Gravel or the Pebble Point Formation. |Sandstone. |
26944|Timboon Sandstone|69651|5|Briefly described|p10, p33-34|Late Cretaceous|Late Cretaceous|Otway Basin. Intraformational mudstones may form seals.||Sherbrook Group.||Overlies Paaratte Formation. Is overlain unconformably by Eastern View Formation.|Sandstone, shale.|
26944|Timboon Sandstone|70077|5|Briefly described|Nelson: Fig.2; p2. Regional: Fig.4; p8|Maastrichtian|Campanian|Otway Basin. Mudstones within distal equivalents in the Nelson Sub-basin provide intraformational seals.||Sherbrook Group.||Overlies Paaratte Formation or Skull Creek Mudstone. Is overlain by Massacre Shale and Wiridjil Gravel.||
26944|Timboon Sandstone|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Maastrichtian|Campanian|Gambier Embayment and Voluta Trough.||Sherbrook Group.||Overlies Paaratte Formation. Is overlain by Massacre Shale.||
26944|Timboon Sandstone|70193|5|Briefly described|p284 Fig 2, p285 fig 3|Maastrichtian|Maastrichtian|Geological province: Otway Basin. I. korojonense dinocyst zone. Part of the Sherbrook Supersequence.||||Underlain conformably by the Paaratte Formation.||
26944|Timboon Sandstone|70880|6|Mentioned|p77|Maastrichtian|Campanian|Otway Basin.||||||
26944|Timboon Sandstone|71266|6|Mentioned|p614 Fig.3|Late Cretaceous|Late Cretaceous|Otway Basin.||||||
26944|Timboon Sandstone|73357|5|Briefly described|p23-24, p43, p45, p47|Maastrichtian|Campanian|Otway Basin. Lithostratigraphic boundary with Paaratte Formation can be uncertain. Correlated with Isabelidinium korojonense Dinocyst Zone, Forcipites longus Spore-Pollen Zone, and I. pellucidum Dinocyst Zone, marginal to nearshore marine setting. Upper part correlates with Manumiella druggii Dinocyst Zone, marginal to shelfal marine depositional environment.||Of Sherbrook Group.||Overlies Paaratte Formation, underlies K/Pg Boundary Shale|Predominantly sandy unit.|
26944|Timboon Sandstone|73383|4|Described|p3, p23, p119, p140, p247, p266-267|Maastrichtian|Campanian|Otway Basin. Lithologies based on geochemistry using the ChemLith classification also includes calcareous sandstone, limestone; and using the Herron classification (1988) includes quartz arenite, sublith-arenite, lith-arenite, Fe-sand, Fe-shale. See also p322.||Sherbrook Group||Overlies Paaratte Formation, underlies Wangerrip Group|Sandstones, mudstones.|
26944|Timboon Sandstone|73385|5|Briefly described|p5|Maastrichtian|Campanian|Otway Basin.||Sherbrook Group||Overlies Paaratte Formation, underlies Wangerrip Group.|Marginal marine and lower coastal plain sandstones, mudstones.|
26944|Timboon Sandstone|73386|4|Described|p4, p6, p10-12, Attachment A1|Maastrichtian|Campanian|Otway Basin. Changes facies from fluvial-upper delta plain onshore and nearshore, to lower delta plain, interdistributary sandstone and shale mid-shelf, and marine shale in the outer shelf. Occurs within the Lower Forcipites longus Spore-Pollen Subzone, late Campanian to Maastrichtian in age. Sharp boundary with overlying Cretaceous/Paleogene boundary shale.||Sherbrook Group||Overlies Paaratte Formation, underlies Wangerrip Group, Cretaceous/Paleogene boundary shale|Characterised by mainly white fine to very coarse sandstones with siltstone/mudstone interbeds.|
26944|Timboon Sandstone|73594|6|Mentioned|p4|Maastrichtian|Campanian|Otway Basin.||Sherbrook Group||Overlies Paaratte Formation||
69415|Timms Spur Leucogranite|61160|3|Fully described|p84, p31 Tb. 5.2|Early Devonian|Early Devonian|S-type, small pluton. Medium-grained, equigranular muscovite-biotite leucogranite; no foliation observed.  Intrudes the migmatite of Omeo Metamorphic Complex and the Cobungra Granite. See also p58-59 Fig. 6.8.||||||
69415|Timms Spur Leucogranite|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Muscovite-biotite leucogranite: medium grained; equigranular; non-magnetic; S-type intrusion. GSV map code: G156.||||||
69415|Timms Spur Leucogranite|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Muscovite-biotite leucogranite: medium grained; equigranular; non-magnetic; S-type intrusion. GSV map code: G156.||||||
69415|Timms Spur Leucogranite|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Muscovite-biotite leucogranite: medium grained; equigranular; non-magnetic; S-type intrusion. GSV map code: G156.||||||
69415|Timms Spur Leucogranite|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Muscovite-biotite leucogranite: medium grained; equigranular; non-magnetic; S-type intrusion. GSV map code: G156.||||||07-FEB-11
69415|Timms Spur Leucogranite|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Muscovite-biotite leucogranite (S-type): non-magnetic (kv = 0-10 x10^-6 cgs); gravity low (?); high total radioelement and K, low to moderate Th and U. GSV map code: G156.||||||
69415|Timms Spur Leucogranite|68116|5|Briefly described|Appendix, Map 27.|Silurian|Silurian||||||Muscovite-biotite leucogranite: medium grained; equigranular; non-magnetic; S-type.|
34871|Tin Pot Ignimbrite|22968|4|Described|Fig49 P92, P141||Early Devonian|New name. Of the parent is Avonmore Subgroup. Max. thickness: 120m. Overlain by Quindalup Ignimbrite; underlain by Carriage Range Ignimbrite.||||||11-DEC-06
34871|Tin Pot Ignimbrite|23021|5|Briefly described|Map legend|Lochkovian|Lochkovian|Parent is the Snowy River Volcanics||||||
34871|Tin Pot Ignimbrite|23309|4|Described|p113 Table 2.40|||Of the Avonmore Subgroup.  Maximum Thickness: 120m.||||||22-FEB-10
34871|Tin Pot Ignimbrite|24551|5|Briefly described|p145, 139 Fig 5.30|Early Devonian|Early Devonian|Of Avonmore Subgroup. Crystal-rich felsdspar ignimbrite. Overlies Carriage Range Ignimbrite.  Max. thickness: ~120m.||||||11-DEC-06
34871|Tin Pot Ignimbrite|68116|5|Briefly described|Appendix, Map 35.|Pragian|Pragian||||||Feldspar and quartz ignimbrite: commonly with very low quartz content; generally weathered and poorly exposed.|
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|||||||
23015|Tobacco Creek Andesite|23309|5|Briefly described|p36 Table 2.7||Cambrian|Of the Licola Volcanics.||||||
23015|Tobacco Creek Andesite|24551|6|Mentioned|p59|||||||||
23015|Tobacco Creek Andesite|24576|5|Briefly described|p729|Late Cambrian|Middle Cambrian|Age: 500 +/- 8 Ma (U-Pb). Geological Province: Lachlan Fold Belt.||||||22-DEC-08
23015|Tobacco Creek Andesite|64535|5|Briefly described|Map legend|Cambrian|Cambrian|Of Licola Volcanic Group. Andesite lava, andesite breccia, volcanogenic sandstone, limestone; marine lavas and mass-flow deposits. ||||||
23015|Tobacco Creek Andesite|64539|5|Briefly described|Map legend|Cambrian|Cambrian|Of Licola Volcanic Group. Andesite lava, andesite breccia, volcanogenic sandstone, limestone; marine lavas and mass-flow deposits. ||||||
23015|Tobacco Creek Andesite|64540|5|Briefly described|Map legend|Cambrian|Cambrian|Of Licola Volcanic Group. Andesite lava, andesite breccia, volcanogenic sandstone, limestone; marine lavas and mass-flow deposits. ||||||
23015|Tobacco Creek Andesite|64605|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Licola Volcanic Group. Andesite lava, andesite breccia, volcanogenic sandstone, limestone; marine lavas and volcaniclastics. Red-black in RGB. Non-magnetic.||||||17-NOV-08
23015|Tobacco Creek Andesite|64616|4|Described|p60, p184, p307|Late Cambrian|Middle Cambrian|Of Licola Volcanic Group. Conformably underlies Cobbs Spur Andesite Breccia. In faulted contact with Whisky Knob Rhyolite. Dated by TIMS U-Pb 500 +/-8 Ma. Porphyritic andesite lavas, andesitic breccia, volcanogenic sandstone, limestone. Geophysical characteristics given.||||||
23015|Tobacco Creek Andesite|66244|5|Briefly described|p2.|Cambrian|Cambrian|Formerly a unit in Licola Volcanic Group (VandenBerg et al. 1995) which has been made redundant.||Unit in Jamieson Volcanic Group.||||
23015|Tobacco Creek Andesite|68116|5|Briefly described|Appendix, Map 43.|Cambrian|Cambrian||||||Andesite lava, andesite breccia, volcanigenic sandstone, limestone.|
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.||||||
26950|Tolmie Igneous Complex|22971|5|Briefly described|p 23|||||||||
26950|Tolmie Igneous Complex|23269|6|Mentioned|Fig14-3.1p403|||||||||
26950|Tolmie Igneous Complex|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
26950|Tolmie Igneous Complex|23309|5|Briefly described|p160, 169, 170, 175, 176.|||||||||
26950|Tolmie Igneous Complex|24004|5|Briefly described|p275 Fig.2|Devonian|Devonian|||||||
26950|Tolmie Igneous Complex|24551|6|Mentioned|p157, 160, 166|Devonian|Devonian|||||||
26950|Tolmie Igneous Complex|31713|6|Mentioned|p6|||||||||
26950|Tolmie Igneous Complex|32001|6|Mentioned|p78|||||||||
26950|Tolmie Igneous Complex|33602|6|Mentioned|p23|||||||||
26950|Tolmie Igneous Complex|35111|6|Mentioned|p1|||See also P2.||||||
26950|Tolmie Igneous Complex|35112|6|Mentioned|p281|||||||||
26950|Tolmie Igneous Complex|35278|6|Mentioned|Fig.11.1|||||||||
26950|Tolmie Igneous Complex|40761|6|Mentioned|Fig.11|||||||||
26950|Tolmie Igneous Complex|41571|6|Mentioned|p50|||||||||
26950|Tolmie Igneous Complex|41641|4|Described|p166|||||||||
26950|Tolmie Igneous Complex|41868|6|Mentioned|p486|||||||||
26950|Tolmie Igneous Complex|42547|5|Briefly described|Fig.15 P57|||||||||
26950|Tolmie Igneous Complex|42726|5|Briefly described|map legend|Middle Devonian||||||||
26950|Tolmie Igneous Complex|44187|5|Briefly described|Map Legend||Late Devonian|||||||
26950|Tolmie Igneous Complex|61163|3|Fully described|p7, p88-89|Late Devonian|Middle Devonian|See p89 Tb. 8.1 for straigraphical detail. Includes rhyolite lavas and ignimbrites. Overlain by Avon Supergroup. Geological Province: Lachlan Fold Belt (Tabberabbera Zone). In the Wabonga Cauldron. See also p14 Fig. 3.2.||||||
26950|Tolmie Igneous Complex|61174|5|Briefly described|map legend|Late Devonian|Late Devonian|Includes undifferentiated unit, Mount Warrick Rhyolite and Bennies Formation. Ignimbrite: undifferentiated volcanic and possible fluvial rocks (subsurface only). GSV map code: Dt.||||||07-FEB-11
26950|Tolmie Igneous Complex|61175|5|Briefly described|map legend|Late Devonian|Late Devonian|Includes undifferentiated unit, Mount Warrick Rhyolite and Bennies Formation. Ignimbrite: undifferentiated volcanic and possible fluvial rocks (subsurface only). GSV map code: Dt.||||||14-SEP-05
26950|Tolmie Igneous Complex|61176|5|Briefly described|map legend|Late Devonian|Late Devonian|Includes undifferentiated unit, Mount Warrick Rhyolite and Bennies Formation. Ignimbrite: undifferentiated volcanic and possible fluvial rocks (subsurface only). GSV map code: Dt.||||||14-SEP-05
26950|Tolmie Igneous Complex|61177|5|Briefly described|map legend|Late Devonian|Late Devonian|Includes undifferentiated unit, Mount Warrick Rhyolite and Bennies Formation. Ignimbrite: undifferentiated volcanic and possible fluvial rocks (subsurface only). GSV map code: Dt.||||||14-SEP-05
26950|Tolmie Igneous Complex|61178|5|Briefly described|map legend|Late Devonian|Late Devonian|Includes Shippen Gully Porphyry, Mount Warrick Rhyolite and Bennies Formation.||||||
26950|Tolmie Igneous Complex|64616|6|Mentioned|p156-157, p189|Middle Devonian|Middle Devonian|Underlies Mansfield Basin. Includes Lewis Farm Conglomerate.||||||
26950|Tolmie Igneous Complex|66252|5|Briefly described|p211, p219 Table 1, p220, p228-230.|||Intra-caldera felsic volcanic succession in north of Macalister Synclinorium. Correlated with Staircase Ignimbrite, an outflow facies equivalent. Includes Ryans Creek Rhyolite.||||||
26950|Tolmie Igneous Complex|67804|6|Mentioned|p65|Late Devonian|Late Devonian|Hosts the Tatong mineralisation.||||||
26950|Tolmie Igneous Complex|68311|6|Mentioned|p275, 286|||||||||
26950|Tolmie Igneous Complex|69669|5|Briefly described|p951-957|Late Devonian|Late Devonian|Forms part of the Central Victorian Magmatic Province. Recalculated Sr and Nd isotope data confirm that Tolmie Igneous Complex magmas were derived from metasedimentary protoliths constructed from materials not long extracted from the mantle, possibly as arc-related volcanic and volcaniclastic rocks. The Selwyn Block was probably the protolith for the Tolmie Igneous Complex magmas.|||Includes Toombullup Ignimbrite.||Several S-type rhyolitic ignimbrite sheets with a number of small hypabyssal stocks of porphyritic microgranodiorite.|
26950|Tolmie Igneous Complex|73199|6|Mentioned|p521-522, p524, p526|Frasnian|Frasnian|S-type. Inferred to have similar deep-crustal sources to plutonic granitic magmas.|377 Ma||Ryans Creek Ignimbrite||May include silicic ignimbrite deposits.|
26950|Tolmie Igneous Complex|75062|5|Briefly described|p74 Fig.2, p87|Devonian|Devonian|Clemens et al. (2100). Crops out astride the Melbourne and Tabberabbera Zones boundary. Harker-type plots. Has some compositional and isotopic similarities with the Wilsons Promontory batholith.|||||Strongly peraluminous A-type rocks. Includes volcanics.|
26950|Tolmie Igneous Complex|75072|5|Briefly described|p230, 233, 256|Late Devonian|Late Devonian|Eastern margin of the Melbourne Zone.|||Hollands Creek Ignimbrite.||Includes a peraluminous A-type rhyolite with distinct, rounded-core zircon antecrysts.|
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.|
30581|Tom Groggin Tonalite|23309|6|Mentioned|p444 App1|||G89 S-Type.||||||
30581|Tom Groggin Tonalite|43220|6|Mentioned|p10||Silurian|||||||
30581|Tom Groggin Tonalite|44184|5|Briefly described|Map Legend||Early Silurian|Shown as Tom Groggin S-type.||||||
37607|Tomato Creek Ignimbrite|23309|4|Described|p111 Tb: 2.40.|||Of Tara Range Subgroup.  Maximum Thickness: 100m.||||||
37607|Tomato Creek Ignimbrite|24551|5|Briefly described|p143|||Of Tara Range Subgroup.||||||
37607|Tomato Creek Ignimbrite|60542|3|Fully described|p68, p54|Early Devonian|Early Devonian|Ignimbrite with minor interbedded volcanic breccia and conglomerate. Conformably overlies Kanni Ignimbrite; conformably overlain by Boggy Creek Sandstone, and perhaps Nowa Nowa Conglomerate, and Castor Oil Lava. Thickness >100m.||||||
37607|Tomato Creek Ignimbrite|68116|5|Briefly described|Appendix, Map 45.|Pragian|Pragian||||||Quartz ignimbrite: crystal rich, medium to coarse-grained, red, generally densely welded and with well developed eutaxitic foliation, rheomorphic at base; contains Ordovician-derived lithic fragments; pyroclastic deposits.|
33677|Tombong Formation|22815|2|Defined|p33|Llandovery|Llandovery|Originally called Tombong beds.||||||
33677|Tombong Formation|22857|4|Described|p420 App. 1 Tb. A1.5|Early Silurian|Early Silurian|Of the Yalmy Group. Quartz-rich grey to buff arenite and siltstone, interbedded shales and very minor conglomerate horizons. Unconformably overlain by Merriangaah Siltstone. Max. thickness: 400m. Geological Province: Yalmy Basin. ||||||
33677|Tombong Formation|22968|6|Mentioned|P108|||Parent is Yalmy Group||||||
33677|Tombong Formation|23329|5|Briefly described|1042|Silurian|Silurian|||||||
33677|Tombong Formation|43233|5|Briefly described|Map Legend|Llandovery||of Yalmy Group.||||||
33677|Tombong Formation|60988|5|Briefly described|p144-146  |Early Silurian|Early Silurian|Tombong Block. c.400m thick. Possibly derived from the Adaminaby Group. Unfossiliferous.||||Is overlain by the Merriangaah Siltstone conformably, or by Quidong Limestone disconformably.|Quartz-rich sandstones and siltstones and interbedded shales; includes chert and slate pebbles.|
18327|Tommy Roundhead Granodiorite|22876|4|Described|p26|||||||||
18327|Tommy Roundhead Granodiorite|22877|5|Briefly described|map|Silurian|Silurian|G35. Hornblende granodiorite. I-Type.||||||26-OCT-04
18327|Tommy Roundhead Granodiorite|23309|6|Mentioned|p444, App1|||G35 I-Type||||||
18327|Tommy Roundhead Granodiorite|41572|6|Mentioned|Fig.1.10|||Reserved as Tommy Roundhead Granitoid||||||
18327|Tommy Roundhead Granodiorite|42627|5|Briefly described|Map legend|Wenlock||||||||
18327|Tommy Roundhead Granodiorite|42647|3|Fully described|p44|||Supersedes invalid name Errinundra Granodiorite||||||
18327|Tommy Roundhead Granodiorite|42827|6|Mentioned|Fig 1.10|||||||||
18327|Tommy Roundhead Granodiorite|68116|5|Briefly described|Appendix, Maps 36-37.|Wenlock|Llandovery||||||Biotite granodiorite and tonalite: medium grained, porphyritic, grey, variably foliated; contains abundant biotite schist enclaves as well as enclaves of hornblende-biotite diorite; I-type.|
34874|Tongaro Formation|22968|6|Mentioned|P108|Llandovery|Llandovery|||||||
34874|Tongaro Formation|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
34874|Tongaro Formation|23309|5|Briefly described|p85-90, 294. Table 2.30|||||||||
34874|Tongaro Formation|24551|4|Described|p133|||Formerly included in the Wombat Creek Group, now included in the Yalmy Group.||||||28-JUL-05
34874|Tongaro Formation|60503|3|Fully described|p101-102|Late  Silurian|Late Silurian|Of the Wombat Creek Group. Supersedes Tongaro Sandstone. In type section is separated from other members of the Wombat Group by Newlands Fault. Lithology in type section: alternating packages of sandstone and mudstone; plus a series of limestone lenses.||||||16-NOV-09
34874|Tongaro Formation|60504|5|Briefly described|Map Legend|Pridoli|Pridoli|Of the Wombat Creek Group. Quartzitic turbidites interbedded with mudstone; quartzites medium to fine grained, green and brown, cleaved||||||20-OCT-04
34874|Tongaro Formation|60505|5|Briefly described|Map legend|Pridoli|Pridoli|Of the Wombat Creek Group. Quartzic turbidites interbedded with mudstone; quartzites medium to fine grained, green and brown, cleaved||||||21-OCT-04
34874|Tongaro Formation|60506|5|Briefly described|Map legend|Pridoli|Pridoli|Of the Wombat Creek Group. Quartzic turbidites interbedded with mudstone; quartzites medium to fine grained, green and brown, cleaved||||||21-OCT-04
34874|Tongaro Formation|60507|5|Briefly described|Map Legend|Pridoli|Pridoli|Of the Wombat Creek Group. Quartzic turbidites interbedded with mudstone; quartzites medium to fine grained, green and brown, cleaved||||||21-OCT-04
34874|Tongaro Formation|60508|5|Briefly described|Map legend|Late Silurian|Late Silurian|Of the Wombat Creek Group. Sandstone: weakly magnetic (0-20nT) in south, low total count, K, Th, U||||||08-NOV-04
34874|Tongaro Formation|68116|5|Briefly described|Appendix, Map 27.|Wenlock|Llandovery||||||Sandstone, minor mudstone: sandstone pale grey; quartzitic, medium to fine grained; thin to thick-bedded; mudstone green and brown, cleaved; rare conglomerate and massive limestone lenses.|
34874|Tongaro Formation|71040|6|Mentioned|p10 Fig.6|Silurian|Silurian|||||||
18335|Tonghi Granodiorite|22878|4|Described|p76|||||||||
18335|Tonghi Granodiorite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Of the Tonghi Supersuite. Biotite-hornblende granodiorite: pale grey, medium to coarse grained; massive; slightly porphyritic in quartz; hornblende bearing western half and hornblende-poor eastern half.||||||01-OCT-04
18335|Tonghi Granodiorite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Tonghi Supersuite. Biotite-hornblende granodiorite: pale grey, medium to coarse grained; massive; slightly porphyritic in quartz; hornblende bearing western half and hornblende-poor eastern half.||||||01-OCT-04
18335|Tonghi Granodiorite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Tonghi Supersuite. Biotite-hornblende granodiorite: highly magnetic (175-250 nT). High potassium response over outcrop and low K and U where the granodiorite is weathered.||||||06-OCT-04
18335|Tonghi Granodiorite|23309|6|Mentioned|p444 App1|||G12 - I-Type. Supersedes Tonghi Granite.||||||
18335|Tonghi Granodiorite|41850|6|Mentioned|p427|||||||||
18335|Tonghi Granodiorite|42827|5|Briefly described|p427|||||||||
18335|Tonghi Granodiorite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|of Bega Batholith. I-type. Coarse-grained hornblende biotite granodiorite.||||||22-OCT-04
18335|Tonghi Granodiorite|43315|5|Briefly described|Map Legend|Wenlock|Wenlock|Of Bega Batholith. I-type granite. Coarse-grained hornblende biotite granite.||||||03-MAY-05
18335|Tonghi Granodiorite|60541|4|Described|p64-65, p39|Devonian|Late Silurian|Part of Tonghi Suite. Intrusive large rounded tors. Grey weathering to green coarse-grained and moderately mafic rock; slightly porphyritic with large grains of qtz, plagioclase and hornblende set in finer grained groundmass. LFB. See also p16, p17, p93.||||||23-JUN-05
18335|Tonghi Granodiorite|68116|5|Briefly described|Appendix, Maps 37, 45-46.|Early Devonian|Early Devonian||||||Biotite-hornblende granodiorite: pale grey, medium to coarse grained; massive; slightly porphyritic in quartz; hornblende-bearing western half and hornblende-poor eastern half; I-type.|
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|||||||
34897|Tongio Munjie Volcanics|22968|5|Briefly described|P134||Early Devonian|New name, only a few meters thick||||||
34897|Tongio Munjie Volcanics|23309|5|Briefly described|p123, 125, 290.  Table 2.48|||||||||
34897|Tongio Munjie Volcanics|24551|5|Briefly described|p151|||||||||
77889|Tongio Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Early Devonian||||||Tonalite: mid- to dark grey; fine-grained equigranular; massive; minor quartz diorite and hornblende-rich gabbro.|
37608|Toole-be-wong Granodiorite|23309|5|Briefly described|p165,347|Devonian|Devonian|G226, S-type.  Supersedes Mount Toole-be-wong Granite. Age:371+/-13Ma.||||||
37608|Toole-be-wong Granodiorite|24551|6|Mentioned|p223, 720 Table 8.3|||||||||
37608|Toole-be-wong Granodiorite|44187|5|Briefly described|Map Legend|Late Devonian|Late Devonian|G226 S-type.||||||01-OCT-08
40706|Toolondo Volcaniclastics|23309|5|Briefly described|p81|||Of the Rocklands Volcanics.||||||
40706|Toolondo Volcaniclastics|50154|2|Defined|p119, p244 App.5|Devonian|Devonian|Of the Rocklands Volcanic Group.||||||15-SEP-04
40706|Toolondo Volcaniclastics|50155|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Feldspar-phyric ignimbrite||||||
40706|Toolondo Volcaniclastics|50156|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Feldspar-phyric ignimbrite: pumice-rich, non-welded; bedded pyroclastic surge deposits; alternating pumice-crystal-rich layers and finer grained accretionary lapilli rich layers, planar and low angle cross-stratification.||||||
40706|Toolondo Volcaniclastics|50157|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Feldspar-phyric ignimbrite: pumice-rich, non-welded; bedded pyroclastic surge deposits; alternating pumice-crystal-rich layers and finer grained accretionary lapilli rich layers, planar and low angle cross-stratification.||||||
40706|Toolondo Volcaniclastics|50158|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Feldspar-phyric ignimbrite: pumice-rich, non-welded; bedded pyroclastic surge deposits; alternating pumice-crystal-rich layers and finer grained accretionary lapilli rich layers, planar and low angle cross-stratification.||||||
40706|Toolondo Volcaniclastics|50159|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Feldspar-phyric ignimbrite: pumice-rich, non-welded; bedded pyroclastic surge deposits; alternating pumice-crystal-rich layers and finer grained accretionary lapilli rich layers, planar and low angle cross-stratification.||||||
40706|Toolondo Volcaniclastics|50160|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Feldspar-phyric ignimbrite||||||16-JUN-04
40706|Toolondo Volcaniclastics|50161|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Feldspar-phyric ignimbrite: pumice-rich, non-welded; bedded pyroclastic surge deposits; alternating pumice-crystal-rich layers and finer grained accretionary lapilli rich layers, planar and low angle cross-stratification.||||||24-JUN-04
40706|Toolondo Volcaniclastics|50162|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Feldspar-phyric ignimbrite: pumice-rich, non-welded; bedded pyroclastic surge deposits; alternating pumice-crystal-rich layers and finer grained accretionary lapilli rich layers, planar and low angle cross-stratification.||||||
40706|Toolondo Volcaniclastics|50163|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Feldspar-phyric ignimbrite: pumice-rich, non-welded; bedded pyroclastic surge deposits; alternating pumice-crystal-rich layers and finer grained accretionary lapilli rich layers, planar and low angle cross-stratification.||||||
40706|Toolondo Volcaniclastics|66002|5|Briefly described|p6 Tb.4|Devonian|Devonian|Of Rocklands Volcanic Group. Defined by Simpson in Morand et al. 2003.||||||
40706|Toolondo Volcaniclastics|71593|6|Mentioned|p48|||||||||
18400|Tooloonook Gravel Formation|38929|4|Described|p51|||||||||
35141|Toombullup Ignimbrite|22971|4|Described|p 24|||||||||
35141|Toombullup Ignimbrite|23309|5|Briefly described|p169 Table 2.64|||||||||
35141|Toombullup Ignimbrite|24551|5|Briefly described|p167|||Overlies Ryans Creek Rhyodacite/Ignimbrite. Maximum Thickness: 700m.||||||
35141|Toombullup Ignimbrite|61163|5|Briefly described|p89 Tb. 8.1|||Grouped within Mount Warrick Rhyolite subdivision of Tolmie Igneous Complex. Recrystallised rhyolitic/rhyodacitic ignimbrite with biotite and garnet; coarse-grained, abundant phenocrysts of quartz, feldspar, biotite, garnet. Thickness: >700m.||||||21-AUG-07
35141|Toombullup Ignimbrite|64312|5|Briefly described|p440|||Of the Wabonga Volcanic Complex. S-type granite - rich in barium.||||||
35141|Toombullup Ignimbrite|68116|5|Briefly described|Appendix, Map 26.|Late Devonian|Late Devonian||||||Recrystallized rhyolitic/rhyodacitic ignimbrite: coarse; abundant phenocrysts of quartz, feldspar, biotite, garnet and, locally, enstatite; schlieren of granodiorite porphyry occur; contains lithic fragments of hornblende granodiorite.|
35141|Toombullup Ignimbrite|69669|5|Briefly described|p951-957|Late Devonian|Late Devonian|SHRIMP U-Pb zircon age. Intruded by the Lima pluton dated at 366 +/- 7 Ma (Rb-Sr; Richards and Singleton, 1981).|377 +/- 2 Ma; Clemens et al. (2014).|Unit in Tolmie Igneous Complex.||Overlies Ryans Creek Ignimbrite.|Contains two suites of phenocrysts formed in different P/T conditions and from different sources.|
35141|Toombullup Ignimbrite|73199|6|Mentioned|p526|||||||Underlain by Ryans Creek Ignimbrite.|Low-silica rhyolite formation.|
35141|Toombullup Ignimbrite|75072|5|Briefly described|p230 Fig.2, 233, 243, 249|Late Devonian|Late Devonian|Tabberabbera Zone. Zircons crystals discussed; probability density distribution graph.|377 +/- 2 Ma (Clemens et al., 2014).||||Peraluminous rhyolite. A-type.|
18407|Toongabbie Limestone|24551|6|Mentioned|p622|||||||||
18407|Toongabbie Limestone|33408|6|Mentioned|p231|||||||||
18407|Toongabbie Limestone|35193|6|Mentioned|p20|||||||||
33956|Toora gravels|22495|6|Mentioned|Fig4 P221||Tertiary|||||||
27588|Toorongo Granodiorite|23309|5|Briefly described|p350|||G238. Supersedes Toorongo Granite. I-Type.||||||
27588|Toorongo Granodiorite|33602|6|Mentioned|p19|||||||||
27588|Toorongo Granodiorite|33607|6|Mentioned|Map legend|Devonian|Devonian|Granodiorite, medium, even-grained, hornblende-bearing.||||||29-NOV-04
27588|Toorongo Granodiorite|35073|5|Briefly described|p11|||See also Table 4.||||||
27588|Toorongo Granodiorite|44187|5|Briefly described|Map Legend||Late Devonian|G238 I-type.||||||
27588|Toorongo Granodiorite|64616|6|Mentioned|p131|Late Devonian|Late Devonian|Age determined by Richards and Singleton, 1981.||||||
27588|Toorongo Granodiorite|66181|6|Mentioned|p297|||Has a hornfels aureole.||||||
83438|Toort pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G662.||Of Glenloth Suite|||Weakly to moderately magnetic core (responses mostly less than 30 nT) surrounded by strongly magnetic rim (responses to 200 nT); gravity response about 20 micrometres/second/second higher than surrounding plutons.|
83438|Toort pluton|73505|5|Briefly described|p19, p22|||Newly named unit in Swan Hill and parts of Balranald and Deniliquin 1:250 000 map areas, (G662). Named after Toort parish. Near the east edge of Lalbert Batholith. Crudely elliptical 24 by 15 km intrusion 25 km NW of Quambatook. Weakly to moderately magnetic core (mostly less than 30 nT) surrounded by strongly magnetic rim (to 200 nT). Gravity response of 20 micrometres/second/second higher than surrounding plutons.|||||Granite.|
29547|Torah Granodiorite|23309|5|Briefly described|p335|||G427 I-Type||||||
29547|Torah Granodiorite|24012|5|Briefly described|p202 Fig. 1|Ordovician|Cambrian|||||||
29547|Torah Granodiorite|24551|5|Briefly described|p76|||Of the Glenelg River Complex.||||||
29547|Torah Granodiorite|42971|5|Briefly described|p144, Fig.2 p143|||||||||
29547|Torah Granodiorite|50154|2|Defined|p30, p75, p78, p248 App.5|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex. Corresponds to part of the Wando Granodiorite of Wells (1956)||||||15-SEP-04
29547|Torah Granodiorite|50156|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite||||||20-AUG-04
29547|Torah Granodiorite|50157|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite||||||20-AUG-04
29547|Torah Granodiorite|50158|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite||||||20-AUG-04
29547|Torah Granodiorite|50159|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite||||||20-AUG-04
29547|Torah Granodiorite|50160|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite||||||20-AUG-04
29547|Torah Granodiorite|50161|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite||||||20-AUG-04
29547|Torah Granodiorite|50162|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite||||||20-AUG-04
29547|Torah Granodiorite|50163|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite||||||20-AUG-04
29547|Torah Granodiorite|50164|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Biotite granodiorite; I-type||||||
29547|Torah Granodiorite|66002|6|Mentioned|p9 Tb.5|||G427. Defined by Morand et al. 2003.||||||
29547|Torah Granodiorite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Biotite granodiorite: foliated, fine to medium grained, light grey, equigranular; accessory magnetite and epidote; weakly magnetic.|
18428|Torbreck Range Andesite|23229|6|Mentioned|p37|||||||||
18428|Torbreck Range Andesite|23309|5|Briefly described|p164, 166, 171. Table 2.61|||||||||
18428|Torbreck Range Andesite|24551|5|Briefly described|p164, p163 Fig. 6.4|Late Devonian|Late Devonian|Of Taggery Subgroup, Marysville Igneous Complex||||||
18428|Torbreck Range Andesite|35073|5|Briefly described|Table 2|||||||||
18428|Torbreck Range Andesite|35277|4|Described|p87|||||||||
18428|Torbreck Range Andesite|39291|6|Mentioned|Table 1|||||||||
18428|Torbreck Range Andesite|41641|4|Described|p157|||||||||
18428|Torbreck Range Andesite|42827|5|Briefly described|Table 5.1|||||||||
18428|Torbreck Range Andesite|68311|5|Briefly described|p273-274, 279, 281|Late Devonian|Late Devonian|Cerberean Cauldron, Central Victoria. Up to 360m thick. Pre-collapse phase.||Taggerty Subgroup.||Overlies Blue Range Formation. Is overlain by Robleys Spur Volcanics.|Andesite and basaltic andesite lava flows, tuffs and agglomerates.|
18441|Torquay Group|22944|5|Briefly described|Fig3|||||||||
18441|Torquay Group|23230|5|Briefly described|Table4-1p40, 42, 44|Miocene||Present in the Torquay Basin.||||||
18441|Torquay Group|23240|5|Briefly described|p120-1|Miocene|Oligocene|||||||
18441|Torquay Group|23267|5|Briefly described|p377, Fig14-1.4p385||Middle Miocene|||||||
18441|Torquay Group|23357|5|Briefly described|53|Recent|Oligocene|||||||
18441|Torquay Group|23372|4|Described|p251 Fig3,p250|Pliocene|Oligocene|In the Bass Basin.||||||09-OCT-07
18441|Torquay Group|23472|4|Described|p326|Miocene|Oligocene|Geological Province: Torquay Basin.||||||
18441|Torquay Group|23537|5|Briefly described|p 440|||||||||
18441|Torquay Group|23778|5|Briefly described|p660|Miocene|Oligocene|Geological Province: Torquay Basin.||||||
18441|Torquay Group|23909|5|Briefly described|p294|Miocene|Miocene|Geological Province: Torquay Sub-basin.||||||
18441|Torquay Group|24055|4|Described|p76|Miocene|Oligocene|Geological Basin: Bass Basin.||||||
18441|Torquay Group|24551|6|Mentioned|p308|||||||||
18441|Torquay Group|24562|6|Mentioned|p132|Miocene|Oligocene|||||||
18441|Torquay Group|29355|6|Mentioned|p179|||||||||
18441|Torquay Group|30576|4|Described|Table 1|||||||||
18441|Torquay Group|30929|6|Mentioned|Map legend|Miocene|Miocene|||||||
18441|Torquay Group|32162|6|Mentioned|p57|||Refers petroleum aspect||||||
18441|Torquay Group|33155|6|Mentioned|p118|||||||||
18441|Torquay Group|33228|6|Mentioned|p2|||||||||
18441|Torquay Group|33240|6|Mentioned|p2|||||||||
18441|Torquay Group|33458|6|Mentioned|p18|||||||||
18441|Torquay Group|34063|6|Mentioned|p10|||Table. U.Eocene-L.Miocene||||||
18441|Torquay Group|34954|5|Briefly described|p198|||||||||
18441|Torquay Group|35013|6|Mentioned|p395|||||||||
18441|Torquay Group|35066|6|Mentioned|p215|||||||||
18441|Torquay Group|35151|6|Mentioned|p150|||||||||
18441|Torquay Group|35262|6|Mentioned|p4|||||||||
18441|Torquay Group|35274|6|Mentioned|p424|||||||||
18441|Torquay Group|35276|3|Fully described|p233|||p238.||||||09-OCT-07
18441|Torquay Group|35290|5|Briefly described|p33|||See also P25.||||||
18441|Torquay Group|35712|4|Described|p18|||See also p33 re aquifers.||||||09-OCT-07
18441|Torquay Group|35854|5|Briefly described|p159|||Stratigraphy discussed.||||||
18441|Torquay Group|36499|3|Fully described|p43|||See also p20.||||||09-OCT-07
18441|Torquay Group|37035|6|Mentioned|p142|||||||||
18441|Torquay Group|37129|6|Mentioned|p359|||||||||
18441|Torquay Group|37385|4|Described|p9|||See also p13.||||||09-OCT-07
18441|Torquay Group|37546|6|Mentioned|p157|||||||||
18441|Torquay Group|38147|6|Mentioned|Map legend|Miocene|Miocene|||||||
18441|Torquay Group|38159|6|Mentioned|Map legend|Oligocene|Eocene|Eocene to Miocene||||||
18441|Torquay Group|39967|6|Mentioned|p43|||||||||
18441|Torquay Group|40524|6|Mentioned|Table 1|||||||||
18441|Torquay Group|41124|4|Described|p255|||||||||
18441|Torquay Group|41201|5|Briefly described|p2|||||||||
18441|Torquay Group|41521|6|Mentioned|p236|||||||||
18441|Torquay Group|41704|6|Mentioned|Fig.3|||||||||
18441|Torquay Group|41715|6|Mentioned|p312|||||||||
18441|Torquay Group|41868|5|Briefly described|p545|||See also P578||||||
18441|Torquay Group|42152|6|Mentioned|Fig.2 P4|||||||||
18441|Torquay Group|42184|6|Mentioned|Fig.2 P348|||||||||
18441|Torquay Group|42318|6|Mentioned|p5|||||||||
18441|Torquay Group|42524|5|Briefly described|Fig.3 P27|||||||||
18441|Torquay Group|42635|5|Briefly described|p91|||||||||
18441|Torquay Group|42827|4|Described|p307|||see also p312.||||||09-OCT-07
18441|Torquay Group|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
18441|Torquay Group|43660|6|Mentioned|Fig.6,p15||Oligocene|||||||
18441|Torquay Group|43702|6|Mentioned|Fig.2,p398|Miocene|Oligocene|||||||
18441|Torquay Group|44135|5|Briefly described|p47|Holocene|Oligocene|Overlies Demons Bluff Formation. Thickness: 540m. Geological province: Durroon Basin. Sandstone, shale, then shallow-marine calcarenite.||||||07-DEC-09
18441|Torquay Group|46988|6|Mentioned|p204|||||||||
18441|Torquay Group|48911|6|Mentioned|Chart 1|||||||||
18441|Torquay Group|61155|5|Briefly described|p3, p18|Middle Miocene|Late Oligocene|Comprises: Jan Juc Formation, Port Addis Limestone, Puebla Formation and Zeally Limestone. Overlies Demons Bluff Formation. Marine marls and clastics. Max. thickness: 1650m in Bass Basin. Geological Province: Torquay Basin.||||||
18441|Torquay Group|61181|5|Briefly described|p135|Middle Miocene|Oligocene|Comprises limestone, clayey limestone, marl and calcareous clay. Overlies Gellibrand Marl. Max. thickness locally: >200m. ||||||
18441|Torquay Group|63173|5|Briefly described|p342 Fig. 9.2|Recent|Late Oligocene|Includes Jan Juc Formation (marl/limestone) and Puebla Formation (claystone/marl). Thickness: at least 1650m. Geological Province: Bass Basin. Claystone, marl and limestone.||||||07-FEB-11
18441|Torquay Group|65316|4|Described|p595, p597 Fig 2, 598|Miocene|Oligocene|Torquay Basin. See also previously included unit: Jan Juc Formation (p598, p603).|||Includes Jan Juc Marl, Point Addis Limestone, Puebla Formation and Newer Volcanics.||Marine carbonate.|23-APR-12
18441|Torquay Group|65687|6|Mentioned|p189|Tertiary|Tertiary|Torquay Basin. Contains echinoid fossils. Includes Puebla Formation which includes Zeally Limestone Member.||||||
18441|Torquay Group|65715|5|Briefly described|p14 Tb.8, p16|Miocene|Oligocene|Includes Batesford Limestone and Gellibrand Marl. Marine. In Torquay and Port Phillip Basins. Formerly included Fyansford Clay instead of Gellibrand Marl.||||||
18441|Torquay Group|67061|5|Briefly described|p546, p551. |Miocene|Oligocene|Maximum thickness of c.700 m in the Basin Deep. A widespread, low-angle unconformity, c.10-5 Ma, separates this unit's variably-folded sediments from overlying Pliocene-Holocene sediments. An estimated 400m (offshore) to 950m (at the coast) of Miocene section has been removed from this Group in the Torquay Sub-basin.|||Includes Jan Juc Marl, Puebla Formation and Point Addis Limestone.|Unconformably overlies Demons Bluff Group. Is unconformably overlain by Brighton Group.|Marine carbonates.|
18441|Torquay Group|68116|5|Briefly described|Appendix, Map 50.|Miocene|Oligocene||||||Marlstone, limestone, mudstone, sandstone, minor lignite.|
18441|Torquay Group|69297|6|Mentioned|p97, p98, p99 fig 2.32|Upper Miocene|Oligocene|Torquay Sub-basin of the Otway Basin. Deposited in a shallow marine environment. |||Includes the Point Addis Limestone, Jan Juc Formation and the Puebla Formation. |Overlies the Demons Bluff Group. |Carbonate rocks. |
18441|Torquay Group|69879|6|Mentioned|p436|||May be confused with Torquay Sequence? (references p431-432, p435).|||Includes Angahook Formation|||
18441|Torquay Group|70077|5|Briefly described|Regional: p5|Miocene|Oligocene|Bass Basin and Torquay Sub-basin.||||Overlies Demons Bluff Group.|Shallow marine carbonates.|
18441|Torquay Group|70942|6|Mentioned|p125|||Map and section.||||||
18441|Torquay Group|73217|5|Briefly described|p1008 Fig.1, 1009, 1022|||Eastern Otway Basin.|c.24-15 Ma.|||Overlies Demons Bluff Group (Angahook and Anglesea Formations).|Marine limestone.|
18441|Torquay Group|73488|6|Mentioned|p632|||Torquay Basin.||||||
18451|Torrent Gravels|31345|6|Mentioned|p326|||||||||
18451|Torrent Gravels|37127|6|Mentioned|p349|||||||||
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.|
37786|Touzells Granodiorite|23309|6|Mentioned|p445, Appendix 1|||G573, I-Type.||||||
37786|Touzells Granodiorite|24133|3|Fully described|p66|Silurian|Silurian|I-type granodiorite.  Intrudes Corryong Granite.  Geological Province: Lachlan Fold Belt.||||||
37786|Touzells Granodiorite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37786|Touzells Granodiorite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37786|Touzells Granodiorite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37786|Touzells Granodiorite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt||||||
37786|Touzells Granodiorite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37786|Touzells Granodiorite|68116|5|Briefly described|Appendix, Map 20.|Pridoli|Wenlock||||||Biotite granodiorite: dark grey, medium grained, minor amphibole; equigranular interior and porphyritic margin; I-type; moderately magnetic.|
27245|Towanga Sandstone|22968|3|Fully described|p19, Fig49,p108|Early Silurian|Early Silurian|Parent is Yalmy Group. Lower contact not exposed. Disconformably overlain by Enano Group, and Thorkidaan Volcanics, with angular unconformity.||||||31-OCT-14
27245|Towanga Sandstone|23021|5|Briefly described|Map legend|Llandovery|Llandovery|Parent is Yalmy Group||||||
27245|Towanga Sandstone|23029|5|Briefly described|Map legend|Llandovery|Llandovery|Parent is Yalmy Group||||||
27245|Towanga Sandstone|23030|5|Briefly described|Map legend|Silurian|Silurian|Parent is the Yalmy Group.||||||25-SEP-08
27245|Towanga Sandstone|23309|5|Briefly described|p85-88. Table 2.30||Telychian|||||||
27245|Towanga Sandstone|23615|3|Fully described|p72, p20 Fig.6, p78|Llandovery|Llandovery|Previously referred to as Towanga Formation (Talent, 1964, 1965).  Formerly classified with Enano Group (VandenBerg et al 1981, 1984) as overlying Thorkidaan Volcanics; now considered to underlie Thorkidaan Volcanics (Allen, 1987).  Age within the `Early Silurian deep marine sedimentation¿ period: 440-430Ma.||||||16-AUG-18
27245|Towanga Sandstone|23938|5|Briefly described|p14 Tb. 1, p139 Tb.1 App.|Early Silurian|Early Silurian|Characterised by abundant fine-grained mica poor, quartz sst interbedded with planar-laminated siltst and shale; chert pebble conglom occur towards top. Overlain by Enano Group. See also p31-32Fig. 12, p38-39 Tb. 2, p77.||||||
27245|Towanga Sandstone|24004|5|Briefly described|p280|Early Silurian|Early Silurian|Of Yalmy Group.||||||
27245|Towanga Sandstone|24275|4|Described|p1695|Early Silurian|Early Silurian|Quartz-sandstone turbidites and siltstones, chert pebble conglomerates and minor rhyolites. Unconformably overlies Blueys Creek Formation.  Geological Province: Lachlan Fold Belt.||||||
27245|Towanga Sandstone|24551|4|Described|p131|||Of the Yalmy Group?||||||
27245|Towanga Sandstone|38145|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
27245|Towanga Sandstone|38151|6|Mentioned|Table 1|||||||||
27245|Towanga Sandstone|38367|6|Mentioned|Fig.9.|||||||||
27245|Towanga Sandstone|39447|2|Defined|p9|late Wenlockian|late Wenlockian|See also P4||||||
27245|Towanga Sandstone|39860|6|Mentioned|p10|||||||||
27245|Towanga Sandstone|40761|6|Mentioned|p226|||||||||
27245|Towanga Sandstone|41570|6|Mentioned|p84|||||||||
27245|Towanga Sandstone|41572|5|Briefly described|p21|||||||||
27245|Towanga Sandstone|41585|4|Described|p125|||||||||
27245|Towanga Sandstone|42827|5|Briefly described|p125|||see also Table 4.1||||||
27245|Towanga Sandstone|43128|5|Briefly described|Fig.6,p476|||Of Early to Middle Silurian age.||||||25-SEP-08
27245|Towanga Sandstone|43206|5|Briefly described|map legend||Llandovery|||||||
27245|Towanga Sandstone|43220|5|Briefly described|p9||Silurian|||||||
27245|Towanga Sandstone|43770|5|Briefly described|p829|Late Silurian|Early Silurian|(E.Sil.-M.Sil.)||||||
27245|Towanga Sandstone|44092|5|Briefly described|map legend|Early Silurian|Early Silurian|Smf4||||||
27245|Towanga Sandstone|44184|5|Briefly described|Map Legend||Early Silurian|||||||
27245|Towanga Sandstone|44185|5|Briefly described|Map legend.|Early Silurian|Early Silurian||||||Marine: sandstone, thick- to thin-bedded, siltstone, minor conglomerate.|
27245|Towanga Sandstone|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
27245|Towanga Sandstone|60503|5|Briefly described|p27, p28 Fig. 9|Early Silurian|Early Silurian|Of the Yalmy Group. Marine terrigenous clastics formed in submarine fan. Conformably/disconformably overlies Blueys Creek Formation. Geological Province: Limestone Creek Graben. ||||||
27245|Towanga Sandstone|61187|5|Briefly described|p24.|Silurian||Limestone Creek Graben. Non-volcanic, marine sediments deposited in a submarine fan.||||Conformably overlies Blueys Creek Formation. Is conformably overlain by, and interfingers with, Thorkidaan Volcanics.|Mainly thick quartz sandstone turbidites and siltstone; chert pebble conglomerates amd minor rhyolitic volcanics near the top.|
27245|Towanga Sandstone|63290|5|Briefly described|p391, p394 Tb. 1|Llandovery|Llandovery|Of Yalmy Group. In East Gippsland. Sandstones are matrix-poor and contain well-sorted and rounded vein and plutonic quartz grains.||||||
27245|Towanga Sandstone|66197|5|Briefly described|p634, p635 Fig.5c|Early Silurian|Early Silurian|Buchan Basin. Deep marine shale and sandstone. Overlies the Seldom Seen Conglomerate. Age inferred.||||||14-MAR-12
27245|Towanga Sandstone|68116|5|Briefly described|Appendix, Maps 28, 35-36.|Telychian|Telychian|||Unit in Yalmy Group.|||Sandstone, siltstone, minor conglomerate: sandstone: thick to thin bedded; quartzarenite; interbedded with siltstone.|
24532|Towanway Tuff|23229|5|Briefly described|Table3-1p16, 16|Middle Cambrian|Cambrian|||||||
24532|Towanway Tuff|23309|5|Briefly described|p35, 44. Table 2.6/2.14|Cambrian|Cambrian|Age: 495+/-5Ma, 509+/-9 Ma.  Of the Mount Stavely Volcanics.||||||
24532|Towanway Tuff|23402|3|Fully described|p11, p8 Tb. 1|Late Cambrian|Late Cambrian|Parent:  Mount Stavely Volcanic Complex.   Age: 501+/-9Ma (U-Pb zircon).   Overlies Nanapundah Tuff and Fairview Andesite Breccia.   Geological Province: Adelaide Fold Belt||||||
24532|Towanway Tuff|24551|5|Briefly described|p79|||Of the Mount Stavely Volcanic Complex.||||||
24532|Towanway Tuff|38436|4|Described|p425|||See also Fig.2.||||||
24532|Towanway Tuff|40172|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
24532|Towanway Tuff|40761|5|Briefly described|Table 1|||||||||
24532|Towanway Tuff|40887|2|Defined|p17|Cambrian|Cambrian|Prob. Cambrian||||||
24532|Towanway Tuff|41571|6|Mentioned|Table 2.2|||||||||
24532|Towanway Tuff|42827|6|Mentioned|Table 2.2|||of Mount Stavely Volcanic Complex||||||
24532|Towanway Tuff|50371|5|Briefly described|Map Legend|Cambrian|Cambrian|Of Mount Stavely Volcanic Complex. Dacitic crystal lithic volcanic sandstone.||||||
24532|Towanway Tuff|61187|5|Briefly described|p67, p75 Table 4, pp75-76, p80.|||Hosts disseminated and stringer sulphide mineralisation and alteration at Wickliffe Prospect. North Ltd. regard the boundary with Glenthompson Sandstone as the prospective copper VHMS horizon. Nonmagnetic to weakly magnetic. Magnetic susceptibility and S.G. are given.||||Is overlain conformably by Glenthompson Sandstone.||
24532|Towanway Tuff|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Mount Stavely Volcanic Complex. Includes Narrapumelap Road Dacite Member. Defined by Buckland 1986.||||||
24532|Towanway Tuff|68116|5|Briefly described|Appendix, Map 39.|Late Cambrian|Early Cambrian||||||Dacitic crystal lithic volcanic sandstone; minor laminated chert and volcanic siltstone.|
24532|Towanway Tuff|68314|5|Briefly described|p755 Fig.6|Late Cambrian|Middle Cambrian|Age inferred from Fig.6.|500 +/- 5 Ma (Stuart-Smith and Black, 1999).|Unit in Stavely Volcanics.|||Includes dacite.|
24532|Towanway Tuff|70211|5|Briefly described|p3, p5, p45-46|||Stavely region.|501.0 +/- 9.0 Ma (Stuart-Smith and Black, 1999).|Mount Stavely Volcanic Complex.||||
24532|Towanway Tuff|70877|4|Described|p2, p49, p54, p61-p67|Cambrian|Cambrian|See also p80, p167-p168, p172-p173, p192. Grampians-Stavely Zone. Ballarat 1:250k and Willaura 1:100k map sheets.  SHRIMP ages derived from this study and represent a maximum age of deposition. Also dated as 501 +/- 9 Ma (Stuart Smith and Black, 1999). Petrography, zircon morphology and SHRIMP U-Pb results are discussed in detail for a sample of this unit.|503.9 +/- 4.2 Ma (SHRIMP U-Pb)|Mount Stavely Volcanic Complex||Structurally overlies the Nanapundah Tuff and Fairview Andesite Breccia. Structurally underlies and is faulted against the Glenthompson Sandstone.||
24532|Towanway Tuff|70967|6|Mentioned|p28|||Stavely Belt.||||||
24532|Towanway Tuff|71593|4|Described|p9, p29-p30, p39-p40, p135, p137, p163|||The type locality for this unit occurs in the Stavely Belt segment. Together with the Glenthompson Sandstone hosts the Thursdays Gossan Prospect. The upper portion of the Towanway Tuff hosts the Wickcliffe Prospect.|501 +/- 9 Ma (SHRIMP U-Pb)|Mount Stavely Volcanic Complex||||
18502|Tower Hill Tuff|29825|5|Briefly described|p18|||||||||
18502|Tower Hill Tuff|30989|5|Briefly described|p188|||See also P190. Radiocarbon date.||||||
18502|Tower Hill Tuff|31007|6|Mentioned|Fig. 1|||See also P255||||||
18502|Tower Hill Tuff|34993|4|Described|p302|||||||||
18502|Tower Hill Tuff|35625|6|Mentioned|Fig.1|||||||||
18502|Tower Hill Tuff|35722|6|Mentioned|Table 2|||Quaternary stratigraphic units and nature of components.||||||
18502|Tower Hill Tuff|38150|4|Described|p26|||||||||
18502|Tower Hill Tuff|41769|6|Mentioned|p39|||||||||
18502|Tower Hill Tuff|41848|4|Described|p377|||Age 7300 yrs C-14 midden||||||
18502|Tower Hill Tuff|42827|4|Described|p377|||||||||
18502|Tower Hill Tuff|64569|6|Mentioned|p904|||||||||
18502|Tower Hill Tuff|66002|5|Briefly described|p13 Tb.9, p18|Neogene|Neogene|Of Newer Volcanic Group. Includes Piton Scoria Member.Defined by Gill 1967, although name much older. Also referred to as Tower Hill series and Tower Hill Volcanic Formation. In Tower Hill area near Warrnambool||||||
18502|Tower Hill Tuff|68116|5|Briefly described|Appendix, Map 48.|Holocene|Pleistocene||||||Pyroclastic rocks with basaltic and sedimentary clasts; ash and lapilli with scattered blocks and bombs; well layered with planar to diffuse bedding; common cross-bedding and climbing ripples.|
83441|Towma pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G654.|||||Largely nonmagnetic but with outer rim to 100 nT; gravity response 100 micrometres/second/second lower than surrounds.|
83441|Towma pluton|73505|5|Briefly described|p19, p21|||Newly named unit in Swan Hill and parts of Balranald and Deniliquin 1:250 000 map areas, (G654). Named after Towma Parish. Comprises a 6 by 17 km intrusion about 15 km north of Birchip. Largely nonmagnetic but with outer rim to 100 nT. Gravity response of 100 micrometres/second/second lower than surrounds.|||||Granite.|
18524|Towzer Creek Granite|23309|5|Briefly described|p338||Early Silurian|G58 S-Type||||||
18524|Towzer Creek Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
18524|Towzer Creek Granite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|S-type. Foliated, medium grained biotite, muscovite, andalusite granodiorite with numerous schistose enclaves.||||||22-OCT-04
18524|Towzer Creek Granite|43315|5|Briefly described|Map Legend|Wenlock|Wenlock|Of the Bete Bolong Suite. S-type granite. Foliated, medium-grained biotite, muscovite, andalusite granodiorite with numerous schistose enclaves.||||||03-MAY-05
18524|Towzer Creek Granite|68116|5|Briefly described|Appendix.|Devonian|Silurian||||||Biotite-muscovite-andalusite granodiorite: medium-grained; foliated with numerous schistose enclaves; S-type.|
31642|Towzer Creek Suite|42726|5|Briefly described|Map Legend||Early Devonian|||||||
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.|
83096|Traralgon 0 coal seam|73289|5|Briefly described|p763-779|Rupelian|Rupelian|"Holdgate et al. (2000). Abbreviated to T0 in the text and diagrams. Variably referred to as T0 seam, T0 coal seam, T0 coal. Youngest seam in the Traralgon Formation; it straddles the Eocene ""greenhouse"" and the Oligocene ""icehouse"". Has an Upper Nothofagitides asperus Zone age (early Oligocene). Up to 90m thick. Extends westwards only to the Morwell Monocline.". See App3 for explanation of age range.||Traralgon Formation.||Overlies the Dutson Sand Member. Is overlain disconformably by the Morwell Formation and locally the Lakes Entrance Formation.||16-MAY-23
83173|Traralgon 1 coal seam|73289|5|Briefly described|p763-779|Priabonian|Priabonian|George (1965). Abbreviated to T1 in the text and diagrams. Variably referred to as T1 seam, T1 coal seam, T1 coal. Has a Middle Nothofagitides asperus Zone age (late Eocene). See App 3 for further explanation on age range.||Traralgon Formation.||Is overlain by the Dutson Sand Member.||04-APR-22
83097|Traralgon 2 coal seam|73289|5|Briefly described|p763-764, 766-774, 778|Bartonian|Lutetian|George (1965). Abbreviated to T2 in the text and diagrams. Variably referred to as T2 seam, T2 coal seam, T2 coal. Has an Lower Nothofagitides asperus Zone age (middle Eocene). Splits into two seams <5m thick in the Loy Yang area. See appendix 3 for explanation of age range.||Traralgon Formation.||||04-APR-22
18553|Traralgon Formation|23230|5|Briefly described|Table4-1p40|Oligocene|Eocene|||||||
18553|Traralgon Formation|23264|5|Briefly described|Table13-3.1p325|Oligocene||||||||
18553|Traralgon Formation|23885|5|Briefly described|p163|Tertiary|Late Cretaceous|Min age: Middle Tertiary.||||||
18553|Traralgon Formation|24053|5|Briefly described|p37|Miocene|Eocene|Of Latrobe Group.  Geological Basin: Gippsland Basin.||||||
18553|Traralgon Formation|24551|5|Briefly described|p498 Fig. 16.8, p327 Fig. 10.33|Oligocene|Paleocene|||||||07-NOV-08
18553|Traralgon Formation|31352|6|Mentioned|Fig. 3|||Eocene- Oligocene. See also P133.||||||
18553|Traralgon Formation|32679|6|Mentioned|p94|||Strat. diagram||||||
18553|Traralgon Formation|34815|6|Mentioned|p15|||||||||
18553|Traralgon Formation|34991|6|Mentioned|p383|||||||||
18553|Traralgon Formation|35273|3|Fully described|p256|||See also p264.||||||04-APR-22
18553|Traralgon Formation|37330|5|Briefly described|Table 4|||||||||
18553|Traralgon Formation|37530|4|Described|p9|||||||||
18553|Traralgon Formation|38417|6|Mentioned|p87|||||||||
18553|Traralgon Formation|38928|6|Mentioned|Fig.14|||||||||
18553|Traralgon Formation|38929|6|Mentioned|Fig.6|||||||||
18553|Traralgon Formation|38930|5|Briefly described|p58|||||||||
18553|Traralgon Formation|38931|6|Mentioned|p80|||||||||
18553|Traralgon Formation|38973|6|Mentioned|p563|||||||||
18553|Traralgon Formation|40117|6|Mentioned|p53|||||||||
18553|Traralgon Formation|41227|4|Described|p4|||||||||
18553|Traralgon Formation|41868|5|Briefly described|p520|||||||||
18553|Traralgon Formation|42184|6|Mentioned|p350|||||||||
18553|Traralgon Formation|42648|5|Briefly described|p45|||||||||
18553|Traralgon Formation|42649|4|Described|p196|middle Oligocene|Eocene middle|||||||
18553|Traralgon Formation|42827|4|Described|p330|||see also Fig 8.21||||||
18553|Traralgon Formation|43145|5|Briefly described|p10|Early Oligocene|Middle Eocene|Pass laterally into Latrobe Group.||||||
18553|Traralgon Formation|60538|5|Briefly described|p472 Fig. 11|Late Eocene|Middle Eocene|||||||
18553|Traralgon Formation|61155|5|Briefly described|p3, p18|Early Oligocene|Middle Eocene|Of the Latrobe Group. Includes sands, gravels and coal seams. Overlain in part by Childers Formation. Max. thickness: 1100m in Gippsland Basin (onshore). Geological Province: Gippsland Basin.||||||
18553|Traralgon Formation|61302|5|Briefly described|p9|Miocene|Oligocene|Overlies the Thorpdale Volcanics. Geological Province: Gippsland Basin.||||||
18553|Traralgon Formation|61328|5|Briefly described|p112 Fig. 2|Oligocene|Eocene|Geological Province: Gippsland Basin.||||||12-FEB-08
18553|Traralgon Formation|61336|4|Described|p(v) Fig. 5, p(xi)|Early Oligocene|Middle Eocene|Comrpises interbedded gravels, sands, clays and major coal seams with thin coarser grained sands and gravels predominating at base. Angular unconformity with Alberton Coal Measures. See also Traralgon Fm. Geol Prov: Gippsland Basin.||||||07-FEB-11
18553|Traralgon Formation|63217|5|Briefly described|p97 Fig.2.|Oligocene|Eocene|Gippsland Basin.|55.0 - 33.0 Ma.||Includes Carrajung Volcanics, Honeysuckle Hill Sequence, Traralgon 0 Sequence, Traralgon 1 Sequence and Traralgon 2 Sequence.|Unconformably overlies Strzelecki Group. Is unconformably overlain by Morwell Formation.||
18553|Traralgon Formation|65316|6|Mentioned|p597|||In the Gippsland Basin; thought to correlate with the Demons Bluff Group.||||||23-APR-12
18553|Traralgon Formation|65718|5|Briefly described|p10 Fig 3.2, p12, p42|Oligocene|Eocene|||Of the Latrobe Valley Group.||Underlain by the Carrajung Volcanics.||
18553|Traralgon Formation|67727|3|Fully described|pp55-84.|Early Oligocene|Middle Eocene|Gippsland Basin. Contains two of the five major brown coal seams in the onshore part of this Basin. Seam thicknesses often exceed 100 m. Subcrops beneath 30 - 500 m overburden, with a total resource of 345 Gt. Coal seam isopachs and correlations, coal properties and lithotypes, ash and sulfur contents are detailed. Fossil dinoflagellates occur in interseam sediments and are discussed.||Unit in Latrobe Valley Group.|Includes Honeysuckle Hill Gravels and Dutson Sand Member.|Is overlain by Morwell and Yallourn Formations and Alberton Coal Measures.|Coarser-grained sandstones and conglomerates at the base; coals and shales in the middle; sandstones, shales and minor coals near the top.|
18553|Traralgon Formation|69016|5|Briefly described|p88-89|||Of the Gippsland Basin. Widespread unit. Contains coal seams up to 100m thick that fucntion as aquitards, but are also jointed and may act as conduits for groundwater flow.||Unit of Latrobe Valley Group.|Includes Carrajung Volcanics.||Thick coal seams, sand, gravel, and clay, with minor coal and olivine basalts.|
18553|Traralgon Formation|69750|6|Mentioned|p68|Oligocene|Eocene|On-shore Gippsland Basin.||Latrobe Valley Group.||Is overlain by Morwell Formation.||
18553|Traralgon Formation|70076|5|Briefly described|Regional: Fig.3|Rupelian|Lutetian|Includes subunits marked (Clays), (Seam 0), (Seam 1) and (Seam 2).||Latrobe Group.||Overlies Honeysuckle Hill Gravels. Is overlain by Morwell Formation.||
18553|Traralgon Formation|70862|6|Mentioned|p48 Fig.1, p49-50|Oligocene|Eocene|Latrobe Valley, Gippsland Basin. Middle Eocene to Early Oligocene.|41.5-28.4 Ma (Partridge, 2006).|Latrobe Valley Group.||Is overlain by Morwell Formation or Lakes Entrance Formation.||
18553|Traralgon Formation|73289|5|Briefly described|p763-764, 765 Fig.2, 766-769, 774-775|Oligocene|Eocene|Gloe (1960). Gippsland Basin (onshore). Referred to as Burong Formation in offshore Gippsland Basin. Seam ages in this unit are younger (Upper Nothofagidites asperus Zone) in the Latrobe Valley than in the Seaspray Depression (Lower-Middle Nothofagidites Zone); implying this Formation straddles the Eocene-Oligocene boundary. See also pp777-778.|||Traralgon 0, 1, 2 Seams; Dutson Sand Member.|Overlies Carrajung Volcanics and (unconformably) the Strzelecki Group. Is overlain disconformably by Morwell, Balook, Lakes Entrance, Childers Formations.|Includes coal seams.|
18553|Traralgon Formation|73488|4|Described|p631-632, p635, p637, p642, p646|Rupelian|Lutetian|Gippsland Basin. Middle-upper Eocene to lowermost Oligocene in age. Coal seams are given varying names in text and diagrams, includes the T3, Traralgon 2 (T2), Traralgon 1 (T1), Traralgon 0 (T0) coal seams, and subdivisions of them. Also referred to as Traralgon coals p634, 636, Traralgon coal seams p631, 640, 647.|||Dutson Sand Member, Traralgon 0 Seam, Traralgon 1 Seam , Traralgon 2 Seam|Overlies Burong Formation, Carrajung Volcanics, underlies Morwell Formation, Seaspray Group, Balook Formation, Alberton Coal Measures. Correlated with Gurnard Formation.|Non-marine claystones and sandstones, brown coal seams.|
18553|Traralgon Formation|73562|6|Mentioned|p300, 302-303, 305-306, 313, 316|Oligocene|Late Cretaceous|Gippsland Basin. Marginal marine and tidal facies are intercalated within the coal facies.||Latrobe Group.||||
18553|Traralgon Formation|73640|5|Briefly described|p1, p3 Fig.2|Eocene|Eocene|Gippsland Basin. Comprises several distinct stacked sedimentary units, described in great detail. Contains brown coals up to 100m thick.||Latrobe Group||||
18553|Traralgon Formation|75065|5|Briefly described|p151, 166, 168|Oligocene|Eocene|Gippsland Basin; mostly onshore. Alluvial sediments, with interseam deposits by marginal marine incursions.||Cobia Subgroup.||Unconformably overlies Bream Volcanics and Barracouta Formation (Halibut Subgroup). Is overlain by Childers Formation.|Coal.|
18555|Traralgon Seam|23264|6|Mentioned|Fig13-3.5p330, 326, 332|||||||||
18555|Traralgon Seam|31045|6|Mentioned|p139|||||||||
18555|Traralgon Seam|35273|6|Mentioned|p264|||||||||
18555|Traralgon Seam|38935|6|Mentioned|Fig.1|||||||||
18555|Traralgon Seam|61336|5|Briefly described|p(xi) Fig. 11|||Brown coal seam in Traralgon Formation.||||||20-APR-12
18555|Traralgon Seam|75065|6|Mentioned|p154|||Gippsland Basin.||||||
23042|Trawalla Granite|22756|5|Briefly described|P50||Middle Devonian|||||||
23042|Trawalla Granite|23309|6|Mentioned|p448 App1|||Obsolete granite name.||||||
23042|Trawalla Granite|43260|5|Briefly described|Map Legend||Middle Devonian|of Beckworth Suite. Biotite granite: cream to pink, felsic, porphyritic; dominated by mildly perthitic K-feldspar crystals up to 25mm.||||||27-OCT-04
23042|Trawalla Granite|44186|5|Briefly described|Map Legend||Early Devonian|G311 Unassigned.||||||
23042|Trawalla Granite|66012|5|Briefly described|p13|||Included in Mount Emu Granodiorite in this report. Described by Cayley and McDonald (1995) as a pink, coarse-grained, porphyritic biotite granite| | | | | |13-JUN-13
23042|Trawalla Granite|68116|5|Briefly described|Appendix, Map 31.|Late Devonian|Middle Devonian||||||Biotite granite: cream to pink, felsic, porphyritic; dominated by mildly perthitic K-feldspar crystals up to 25mm.|
23045|Trendale Formation|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Snowy River Volcanics||||||
23045|Trendale Formation|23309|4|Described|p109. Table 2.40|||Maximum Thickness: 900m.||||||
23045|Trendale Formation|23615|3|Fully described|p111, p23|Early Devonian|Early Devonian|Of Snowy River Volcanics.  Overlain by Gelantipy Ignimbrite (unconformable), overlies Devils Den Conglomerate.  Age: Early Devonian ~410-395Ma.  Max. thickness: ~200m.||||||16-AUG-18
23045|Trendale Formation|24551|5|Briefly described|p141 Fig. 5.32|||Of Snowy River Volcanics.||||||
23045|Trendale Formation|43206|5|Briefly described|map legend||Ludlow|Of Snowy River Volcanics||||||
23045|Trendale Formation|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Unit in Snowy River Volcanics.|||Extrusive, fluvial: ignimbrite, ashstone, sandstone, mudstone.|
23045|Trendale Formation|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Quartz-feldspar ignimbrite, ashstone, sandstone, siltstone, mudstone.|
18571|Trentham basalt|30271|6|Mentioned|p159|||||||||
18571|Trentham basalt|35293|6|Mentioned|p159|||||||||
24042|Trident Arm Formation|41511|6|Mentioned|p14|||||||||
68431|Trochocyathus bed|24551|6|Mentioned|p294|||Of the Wangerrip Group.||||||
26184|Truro Volcanics|14019|5|Briefly described|p20|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Correlative of the Antrim Plateau Volcanics.||||||
26184|Truro Volcanics|22581|6|Mentioned|Fig.2,p37|||Normanville Group, Kanmantoo Basin. Overlies Heatherdale Shale. Overlain by Carrickalinga Head Formation||||||
26184|Truro Volcanics|22643|5|Briefly described|p186, fig3,6|Early Cambrian|Early Cambrian|||||||
26184|Truro Volcanics|22671|6|Mentioned|p847-48|||Generally equated with the top of Normanville Group. Geological Province: Kanmantoo Belt (eastern South Australia).||||||18-JAN-06
26184|Truro Volcanics|22766|4|Described|Fig.2 p561, p562|Early Cambrian|Early Cambrian|See also Fig.1 p561.||||||26-FEB-07
26184|Truro Volcanics|22830|6|Mentioned|P25|||Interbedded with Heatherdale Shale||||||
26184|Truro Volcanics|22857|5|Briefly described|p88 Fig. 14.7A, p93-94|Early Cambrian|Early Cambrian|Of the Normanville Group. Max. thickness: 300m. ||||||
26184|Truro Volcanics|22858|5|Briefly described|p93|||||||||
26184|Truro Volcanics|23023|6|Mentioned|p1800|||||||||
26184|Truro Volcanics|23309|5|Briefly described|p25-27, Table 2.1, 2.3|Cambrian|Cambrian|of the Normanville Group||||||05-NOV-07
26184|Truro Volcanics|23818|4|Described|p98|Cambrian|Cambrian|Max. thickness: 2000 ft. Overlain by Hawker Group. Underlain by Umberatana Group (unconformable).||||||26-FEB-07
26184|Truro Volcanics|23854|5|Briefly described|p863|Early Cambrian|Early Cambrian|||||||
26184|Truro Volcanics|23869|5|Briefly described|p15 Fig. 3|Cambrian|Cambrian|||||||
26184|Truro Volcanics|23914|6|Mentioned|p158 Fig. 12|||||||||
26184|Truro Volcanics|23932|5|Briefly described|p665 Table 1|Early Cambrian|Early Cambrian|Geological Province: Adelaide Fold Belt.  Age: 525 Ma.||||||
26184|Truro Volcanics|23981|5|Briefly described|p8-9 Fig. 4, p22|Early Cambrian|Early Cambrian|Overlies Fork Tree Limestone. Interfingers with Heatherdale Shale. Geological Province: Stansbury Basin (Fleurieu Peninsula). See also p50.||||||
26184|Truro Volcanics|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Of the Normanville Group.  Geological Province: Stansbury Basin.||||||19-JAN-05
26184|Truro Volcanics|24509|5|Briefly described|p42, p39 Fig. 1|Early Cambrian|Early Cambrian|Alkaline volcanics. Age: 525Ma. 300+m of altered vesicular and amygdaloidal andesite, trachyte and metabasalt. Geological Province: Adelaide Geosyncline.||||||04-MAY-05
26184|Truro Volcanics|24551|5|Briefly described|p74|||Of Normanville Group.||||||
26184|Truro Volcanics|30801|6|Mentioned|p5|||Lower Cambrian. Table P5-6||||||
26184|Truro Volcanics|30805|2|Defined|p1|Early Cambrian|Early Cambrian|See also p2-5.||||||26-FEB-07
26184|Truro Volcanics|30807|6|Mentioned|p102|||Suggested map symbol||||||
26184|Truro Volcanics|33471|5|Briefly described|p555|||||||||
26184|Truro Volcanics|34536|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
26184|Truro Volcanics|34612|6|Mentioned|p98|||Cambrian||||||
26184|Truro Volcanics|36534|6|Mentioned|p221|||||||||
26184|Truro Volcanics|39352|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
26184|Truro Volcanics|39489|4|Described|p8|||||||||
26184|Truro Volcanics|40442|6|Mentioned|p13|||||||||
26184|Truro Volcanics|40856|6|Mentioned|Fig.23.6|||||||||
26184|Truro Volcanics|41526|6|Mentioned|p61|||||||||
26184|Truro Volcanics|42222|5|Briefly described|p21|||||||||
26184|Truro Volcanics|42246|6|Mentioned|p17|||||||||
26184|Truro Volcanics|42266|6|Mentioned|Fig.2 P292|||||||||
26184|Truro Volcanics|42272|5|Briefly described|p404|||||||||
26184|Truro Volcanics|42274|6|Mentioned|p458|||||||||
26184|Truro Volcanics|42275|5|Briefly described|p468|||||||||
26184|Truro Volcanics|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Mafic to intermediate.||||||25-MAY-05
26184|Truro Volcanics|43195|5|Briefly described|Map Legend||Cambrian|See also commentary on back of map.||||||
26184|Truro Volcanics|43258|5|Briefly described|Map Legend||Cambrian|||||||
26184|Truro Volcanics|43298|5|Briefly described|Map Legend||Cambrian|||||||
26184|Truro Volcanics|43560|6|Mentioned|p235|||Maybe Truro tuff||||||
26184|Truro Volcanics|43781|6|Mentioned|p3||Botoman|SHRIMP Zircon age: 526+/-4 Ma||||||
26184|Truro Volcanics|44093|6|Mentioned|p108|||Intraplate basalt.||||||
26184|Truro Volcanics|44133|4|Described|p4 Fig. 7.2, 6, 13, 51 Fig. 7.18|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Normanville Group. Maximum Thickness: 300m+.||||||
26184|Truro Volcanics|50154|2|Defined|p23, p52, p159|Early Cambrian|Early Cambrian|Of the Moralana Supergroup. Interlayered with the Nangeela Formation. Intruded by the Dergholm Granite. Geological Province: Glenelg Zone, Delamerian Fold Belt.||||||15-SEP-04
26184|Truro Volcanics|50156|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup||||||
26184|Truro Volcanics|50157|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|||||||
26184|Truro Volcanics|50158|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup||||||
26184|Truro Volcanics|50159|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|||||||22-JUN-04
26184|Truro Volcanics|50160|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup||||||
26184|Truro Volcanics|50161|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup.||||||
26184|Truro Volcanics|50162|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup||||||
26184|Truro Volcanics|50163|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Moralana Supergroup||||||
26184|Truro Volcanics|50164|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Glenelg River Metamorphic Complex (Moralana Supergroup).||||||
26184|Truro Volcanics|60567|5|Briefly described|p39|Cambrian|Cambrian|Age: 526+/-4Ma (Cooper et al, 1992).||||||
26184|Truro Volcanics|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Mafic to intermediate volcanics.||||||
26184|Truro Volcanics|61046|5|Briefly described|p7 Fig. 1, p8 Fig. 2|||Of Normanville Group. Basic.||||||
26184|Truro Volcanics|61108|5|Briefly described|map legend|Cambrian|Cambrian|Mafic to intermediate volcanic rock.||||||
26184|Truro Volcanics|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Of the Normanville Group. Interfingers with Heatherdale Shale. Geological Province: Karinya Syncline/Adelaide Fold Belt. See also p14 Fig. 6||||||
26184|Truro Volcanics|62744|6|Mentioned|p708|||Of the Normanville Group. In western Victoria.||||||
26184|Truro Volcanics|63848|6|Mentioned|p532,  p534 Fig.4.|||||Unit in Normanville Group.||||
26184|Truro Volcanics|65337|5|Briefly described|p95.|Early Cambrian|Early Cambrian|Stansbury Basin. Correlative with Kalkarindji Volcanic Group.||Unit in Gnalta Group.||||
26184|Truro Volcanics|65489|6|Mentioned|p119|||Stansbury Basin.||||Correlates with Mooracoochie Volcanics (Warburton Basin).||
26184|Truro Volcanics|65716|4|Described|p3-9|Cryogenian|Cryogenian|From Chetwynd and part of Casterton 1:50k sheets. Sample dated is metagabbro. SHRIMP zircon U-Pb magmatic age of 642.5 +/- 3.9 Ma. Age conflicts with younger age of enclosing Moralana Supergroup sediments.||||||
26184|Truro Volcanics|65892|5|Briefly described|p9 Fig.4, p17. |Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Unit in Normanville Group.||Overlies Fork Tree Limestone. Is unconformably overlain by Carrickalinga Head Formation.||
26184|Truro Volcanics|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Moralana Supergroup. Defined by Forbes (1972). See also Morand et al. 2003.||||||
26184|Truro Volcanics|66623|6|Mentioned|p14, p427.|Middle Cambrian|Middle Cambrian|Strong geochemical correlation with Mount Arrowsmith Volcanics of Koonenberry Belt, although the authors point to problems involving location and age of the samples examined.||||||
26184|Truro Volcanics|67536|5|Briefly described|Map Legend|||Kanmantoo Province; basement to Murray Basin.||||Intercalated with Normanville and/or Kanmantoo Group metasediments.|Mafic to intermediate volcanic rocks. |
26184|Truro Volcanics|68116|5|Briefly described|Appendix, Map 29.|Early Cambrian|Early Cambrian|Contains  thin interbeds of slate and greywacke. Low regional metamorphic grade, commonly cleaved.|||||Mafic to felsic lavas and intrusives: basalt, andesite dark green, fine-grained; rhyolite cream, quartz-phyric; dolerite and gabbro: dark green; diorite dykes and sills: grey-green; mafic volcaniclastic sandstone and granulestone: dark grey-green.|
26184|Truro Volcanics|68735|6|Mentioned|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin.||Normanville Group.||||10-APR-17
26184|Truro Volcanics|68822|5|Briefly described|p324|Stage 2|Stage 2||ca. 522 Ma|Of the Normanville Group.|||Alkalic volcanics.|
26184|Truro Volcanics|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Normanville Group.||||
26184|Truro Volcanics|69445|6|Mentioned|p30:17|Early Cambrian|Early Cambrian|Stansbury Basin.||||||12-JUL-16
26184|Truro 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.||||||
26184|Truro Volcanics|71139|6|Mentioned|p153-155, 157, 161|||Adelaide Geosyncline. Pb, Th, U concentrations and Pb isotope data tabulated.||||Interbedded with Kanmantoo Group sediments.|Alkali volcanics.|
26184|Truro Volcanics|71322|5|Briefly described|p51, p52 Fig.1, p53, p57, p60, p66, p73|Early Cambrian|Early Cambrian|Tentatively correlated with a volcano-sedimentary sequence in drillhole DEL 10ACD001 in the Haylands Cu-Au prospect near Morgan. This c.511 Ma age is of a tuffaceous siltstone from DEL 10ACD001. Other ages given with interpretations.|511 +/- 5 Ma (maximum depositional age).|Normanville Group.||Intercalated with Normanville and/or Kanmantoo Group. Provisionally correlated with Marne River Volcanics.|Mafic volcanics.|14-DEC-21
26184|Truro Volcanics|71593|4|Described|p8, p12, p19-p22, p102||Early Cambrian|Glenelg Zone. Early Cambrian age for this unit derived from SHRIMP U/Pb dates of correlatives which yielded ages of 521 +/- 4 Ma and 522 +/- 2 Ma (Cooper et al, 1992; Burtt et al, 2000; Jenkins et al, 2002). See also p121-p122, p133, p166, p169-p172, p177, p180, p195, p198, p202.|c. 525 Ma|||Overlain by the Kanmantoo Group.|Basaltic dykes, mafic to felsic igneous rocks and associated volcanics.|
26184|Truro Volcanics|72445|6|Mentioned|App.7 p6 Fig.3.|Cambrian|Cambrian|Shown only on the geological map covering the Stavely Project area (from Geology of Victoria 2003: 21).||||||
26184|Truro Volcanics|73118|6|Mentioned|p73|||Probably related to early Delamerian Orogeny.|526 Ma; Cooper et al., 1992).|||||
26184|Truro Volcanics|73188|6|Mentioned|p353|||Evidence of extensional tectonism.|||||Mafic intraplate lavas.|
26184|Truro Volcanics|73430|5|Briefly described|p492, p497-498, p508 Fig.8|Early Cambrian|Early Cambrian|Mostly outcrops on the flanks of the Karinya syncline to the north and northeast of Adelaide. MgO-rich and high compatible elements suggest the alkali basalts are near-primary unfractionated melts. High eNd values of +5 to +7.8. Equated with a deformed alkaline mafic suite hosted in the Harvester's Creek greywacke by Gibson et al., (2015). See also Turo alkali basalt lavas p493, Truro volcanics p493, p508, p517, Truro basalts p503 Fig.6, Truro suite p498, p516.|522+/-2 Ma|Normanville Group|||Suite of undersaturated anorogenic style alkali basalts. Highly alkaline basaltic lava flows, variably deformed, metamorphosed and altered.|
75955|Tubbut Basalt|68115|5|Briefly described|p10.|Eocene|Eocene|New name, after the town of Tubbut. Formerly Older Volcanic Group basalts near Tubbut and Bonang, and outliers 30 km to the SW near Serpentine and Riddle Creeks. May be different flows, being 200 m apart in elevation. Wellman (1974) included the basalt at Tubbut in the Gelantipy province, and that at Bonang in the Bonang Province.|||||Olivine tholeiite, olivine nephelinite and hawaiite.|
75955|Tubbut Basalt|68116|5|Briefly described|Appendix, Map 36.|Priabonian|Lutetian||||||Basalt flows: olivine tholeiite, olivine nephelinite and hawaiite.|
69421|Tucker Creek Tonalite|61161|5|Briefly described|p103, p105, p76-77 Fig 6.1|Early Devonian|Early Devonian|Strongly altered, nonmagnetic, grey to pale green, medium-grained, equigranular, unfoliated, biotite-hornblende tonalite. Age: inferred Early Devonian. GSV map code: G465.||||||
69421|Tucker Creek Tonalite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende tonalite: medium-grained; contains quartz, plagioclase, biotite (replaced by chlorite and sphene) and relics of brown hornblende; alteration minerals include sericite, carbonate, epidote; I-type intrusion. GSV map code: G465.||||||
69421|Tucker Creek Tonalite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende tonalite: medium-grained; contains quartz, plagioclase, biotite (replaced by chlorite and sphene) and relics of brown hornblende; alteration minerals include sericite, carbonate, epidote; I-type intrusion. GSV map code: G465.||||||07-FEB-11
69421|Tucker Creek Tonalite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende tonalite: medium-grained; contains quartz, plagioclase, biotite (replaced by chlorite and sphene) and relics of brown hornblende; alteration minerals include sericite, carbonate, epidote; I-type intrusion. GSV map code: G465.||||||
69421|Tucker Creek Tonalite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende tonalite: medium-grained; contains quartz, plagioclase, biotite (replaced by chlorite and sphene) and relics of brown hornblende; alteration minerals include sericite, carbonate, epidote; I-type intrusion. GSV map code: G465.||||||
69421|Tucker Creek Tonalite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite-hornblende tonalite: no gravity data; nonmagnetic (k < 1 x10^-6 cgs), intruded by moderate magnetic dykes (80 to 100 nT); low to moderate K, low Th and total radioelements, moderate U. GSV map code: G465.||||||26-JUN-14
69421|Tucker Creek Tonalite|68116|5|Briefly described|Appendix, Map 35.|Early Devonian|Silurian||||||Biotite-hornblende tonalite: medium-grained; contains quartz, plagioclase, biotite (replaced by chlorite and sphene) and relics of brown hornblende; alteration minerals include sericite, carbonate, epidote.|
18657|Tullamarine Basalt|33604|6|Mentioned|p21|||Stratigraphic diagram||||||
18657|Tullamarine Basalt|66244|5|Briefly described|p7.|Miocene|Miocene|Unconformably overlies Paleozoic rocks between Bulla and the lower reaches of the Maribyrnong River. Was included in the Melbourne Province of Wellman (1974) and the Melbourne Subprovince of Price et al. (2003).|20.5 Ma (Bowen 1975).|||Is overlain by Brighton Group and Newer Volcanics.||14-SEP-12
18657|Tullamarine Basalt|68116|5|Briefly described|Appendix, Map 41.|Burdigalian|Aquitanian||||||Lava flows: alkali olivine basalt.|
18657|Tullamarine Basalt|71419|6|Mentioned|p8 Fig 2|Miocene|Miocene|||||||
25558|Tullaroop Granodiorite|23300|5|Briefly described|Map Legend|Devonian|Devonian|Of Harcourt Suite||||||
25558|Tullaroop Granodiorite|23301|5|Briefly described|Map Legend|Devonian|Devonian|Of Harcourt Suite||||||
25558|Tullaroop Granodiorite|23302|5|Briefly described|Map Legend|Devonian|Devonian|Of Harcourt Suite||||||
25558|Tullaroop Granodiorite|23303|5|Briefly described|Map Legend|Devonian|Devonian|Of Harcourt Suite||||||
25558|Tullaroop Granodiorite|23304|5|Briefly described|Map Legend|Devonian|Devonian|Of Harcourt Suite||||||
25558|Tullaroop Granodiorite|23305|4|Described|p44 Table 6, 7||Late Devonian|Now formally defined after White & Chappell (1988). Of Harcourt Suite. Central Victorian Magmatic Province.||||||02-JUL-13
25558|Tullaroop Granodiorite|23309|6|Mentioned|p445 App1|||G315 I-Type. Supersedes Tullaroop Granite.||||||
25558|Tullaroop Granodiorite|23810|5|Briefly described|Table 1, p890, Fig 4||Devonian|Mafic I-Type. Age: 378+/-2 Ma (SHRIMP U-Pb age). Lachlan Fold Belt.||||||
25558|Tullaroop Granodiorite|24551|6|Mentioned|p221, 718 Table 8.1|||||||||
25558|Tullaroop Granodiorite|30579|6|Mentioned|Map legend|Devonian|Devonian|||||||
25558|Tullaroop Granodiorite|42154|6|Mentioned|Table 1 P334|||||||||
25558|Tullaroop Granodiorite|65715|5|Briefly described|p8 Tb.4|||G315. Of Harcourt Suite.||||||
25558|Tullaroop Granodiorite|67978|5|Briefly described|p496 Fig.1, p499 Tb.1|Frasnian|Frasnian|Dating by Bierlein et al. (2001).|378 +/- 2 Ma, SIMS U-Pb|||||19-SEP-14
25558|Tullaroop Granodiorite|68116|5|Briefly described|Appendix, Map 31.|Late Devonian|Late Devonian||||||Biotite +/- hornblende granodiorite: medium grained; equigranular to weakly porphyritic in plagioclase, quartz and K-feldspar; nonmagnetic phase at surface intruded by a magnetic phase at depth; nonmagnetic phase reduced to oxidised; I-type.|
25558|Tullaroop Granodiorite|75072|5|Briefly described|p230 Fig.2, 241-242, 248-249|Late Devonian|Late Devonian|Bendigo Zone. Zircon age spectra discussed, graphed.|378 +/- 2 Ma (Bierlein et al., 2001).||||I-type.|
18661|Tulloch Ard Ignimbrite|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Snowy River Volcanics.||||||25-SEP-08
18661|Tulloch Ard Ignimbrite|23309|4|Described|p106-109. Table 2.40|||Maximum Thickness: 900m.||||||
18661|Tulloch Ard Ignimbrite|23615|3|Fully described|p107, p23|Early Devonian|Early Devonian|Of Snowy River Volcanics. Formerly inc.in Gelantipy Rhyodacite (Ringwood, 1955b). Max. thick: 900m. Overlain in different areas by Moonkan Ignimbrite, Statham Ignimbrite, Dingo Hill Lava and Devils Den Conglomerate.  Age: Early Devonian ~410-395Ma. See also p233 App.1.||||||16-AUG-18
18661|Tulloch Ard Ignimbrite|23938|6|Mentioned|p53|||Of the Snowy River Volcanics. See also p54-55 Tb. 4 and p59-65 Figs. 21-24.||||||25-SEP-08
18661|Tulloch Ard Ignimbrite|24551|5|Briefly described|p144, 141 Fig. 5.32|||Of Snowy River Volcanics. Not included in any of the subgroups.||||||
18661|Tulloch Ard Ignimbrite|41585|6|Mentioned|p135|||Misspelling of reserved name Tulach Ard?||||||
18661|Tulloch Ard Ignimbrite|42827|5|Briefly described|p136|||||||||
18661|Tulloch Ard Ignimbrite|43206|5|Briefly described|map legend||Ludlow|Of Snowy River Volcanics||||||
18661|Tulloch Ard Ignimbrite|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Unit in Snowy River Volcanics.|||Extrusive: felsic ignimbrite, mostly densely welded.|
18661|Tulloch Ard Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Quartz-feldspar ignimbrite with lithic clasts of black shale and other older sediment: mostly densely welded.|
33132|Tuloona Granodiorite|23309|5|Briefly described|p337|||G425 I-Type||||||
33132|Tuloona Granodiorite|23319|4|Described|p408 Fig. 1,  p415|Ordovician|Cambrian|Intrudes Kout Norien Granodiorite. Comprises a mafic phase grading into marginal felsic phase; mafic part is unique for swarms of igneous-textured porphyritic microgranular enclaves; felsic part becomes more leucocratic , muscovite-rich with phenocrysts||||||07-FEB-07
33132|Tuloona Granodiorite|24012|5|Briefly described|p215 Table 6|||||||||
33132|Tuloona Granodiorite|24551|5|Briefly described|p77 Fig. 3.7|||||||||
33132|Tuloona Granodiorite|50154|2|Defined|p36, p85, p248 App.5|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex. Includes the Coojar Granodiorite of Kemp et al. (2002). Intrudes the Kout Norien Granodiorite and Awaiti Granite. Overlain by a thin sheet of Glendara Granite.||||||15-SEP-04
33132|Tuloona Granodiorite|50155|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Biotite granodiorite; I-type||||||
33132|Tuloona Granodiorite|50156|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite.||||||20-AUG-04
33132|Tuloona Granodiorite|50157|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite.||||||20-AUG-04
33132|Tuloona Granodiorite|50158|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite.||||||20-AUG-04
33132|Tuloona Granodiorite|50159|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite.||||||20-AUG-04
33132|Tuloona Granodiorite|50160|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite.||||||20-AUG-04
33132|Tuloona Granodiorite|50161|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite.||||||20-AUG-04
33132|Tuloona Granodiorite|50162|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite.||||||20-AUG-04
33132|Tuloona Granodiorite|50163|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Glenelg River Metamorphic Complex? Biotite granodiorite.||||||20-AUG-04
33132|Tuloona Granodiorite|50164|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Biotite granodiorite; I-type.||||||16-JUN-04
33132|Tuloona Granodiorite|66002|6|Mentioned|p8-9 Tb.5|||G425. Defined by Kemp and Gray 1999. Their 'felsic' phase of this unit was renamed Awaiti Granite (Morand et al. 2003).||||||24-MAY-13
33132|Tuloona Granodiorite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian|Common mafic biotite-rich microgranitoid enclaves; also enclaves of migmatite and schist.|||||Biotite granodiorite: massive to weakly foliated, light grey, medium to coarse grained, porphyritic with phenocrysts of quartz and microcline; accessory muscovite and magnetite;  biotite-rich schlieren locally common; magnetic.|
33132|Tuloona Granodiorite|72313|6|Mentioned|p459 Table 2|||Delamerian Orogen. I-S-type. Hf isotope data included.|500 Ma|||||
24049|Tumberluck Diorite|22876|4|Described|p25|||Ellery Suite||||||
24049|Tumberluck Diorite|22877|5|Briefly described|map|Silurian|Silurian|Of the Ellery Suite. G28. Hornblende diorite.||||||26-OCT-04
24049|Tumberluck Diorite|23309|6|Mentioned|p445 App1|||G28 - I-Type.||||||
24049|Tumberluck Diorite|42627|5|Briefly described|Map legend|Wenlock|Wenlock|Reserved. See also Timberluck ...||||||
24049|Tumberluck Diorite|42647|4|Described|p41|||||||||
24049|Tumberluck Diorite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Hornblende diorite: coarse to medium grained, dark green-grey; foliated; I-type.|
83439|Tungie pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G663.||Of Glenloth Suite|||Confused magnetic response, but generally high in the west and nonmagnetic in the east; gravity response about 60 micrometres/second/second higher in the east than the west.|
83439|Tungie pluton|73505|5|Briefly described|p19, p22|||Newly named unit in Swan Hill and parts of Balranald and Deniliquin 1:250 000 map areas, (G663). Irregularly shaped intrusion about 25 km SE of Sea Lake. Near the western edge of the Lalbert Batholith. Confused magnetic response, but generally high in the west and nonmagnetic in the east. Gravity repsonse of 60 micrometres/second/second higher in the east than the west.|||||Granite.|
83435|Tunstalls pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G631.||Of Glenloth Suite|||Possibly granodiorite; I-type, oxidised; magnetic response to 130 nT; gravity response about 10 micrometres/second/second lower than metasediments, but partly obscured by adjacent plutons.|
18726|Turritable Falls Trachyte|35215|6|Mentioned|Table 4|||Variation of Turritable?||||||
18729|Turrum Formation|13332|5|Briefly described|p184 Fig.2|Eocene|Eocene|Geological Province: Gippsland Basin.||||||
18729|Turrum Formation|23230|4|Described|Table4-1p40, 44||Eocene|||||||
18729|Turrum Formation|24054|5|Briefly described|p46|Eocene|Eocene|Of Latrobe Group. Geological Basin: Gippsland Basin.||||||12-FEB-08
18729|Turrum Formation|24551|6|Mentioned|p477, 334 Fig. 10.42||Middle Eocene|Of the Cobia Subgroup.||||||
18729|Turrum Formation|29355|6|Mentioned|p190|||||||||
18729|Turrum Formation|29721|6|Mentioned|p192|||||||||
18729|Turrum Formation|29736|6|Mentioned|Fig.2|||||||||
18729|Turrum Formation|29974|6|Mentioned|Fig.1|||||||||
18729|Turrum Formation|31352|6|Mentioned|p134|||Late Eocene||||||
18729|Turrum Formation|31480|3|Fully described|p71|||See also P72, 73. Non-marine. Latrobe Gp.||||||
18729|Turrum Formation|32162|6|Mentioned|Fig.3|||||||||
18729|Turrum Formation|32574|6|Mentioned|p73|||See also P75||||||
18729|Turrum Formation|33320|6|Mentioned|p57|||Eocene.||||||
18729|Turrum Formation|33362|6|Mentioned|p111|||||||||
18729|Turrum Formation|35013|6|Mentioned|p396|||||||||
18729|Turrum Formation|35067|6|Mentioned|Fig.3|||||||||
18729|Turrum Formation|35273|4|Described|p269|||||||||
18729|Turrum Formation|35573|6|Mentioned|Fig.3|||Chronostratigraphic section - Gippsland Basin||||||
18729|Turrum Formation|36643|6|Mentioned|Fig.7|||||||||
18729|Turrum Formation|38929|6|Mentioned|p45|||||||||
18729|Turrum Formation|41282|6|Mentioned|Fig.4|||||||||
18729|Turrum Formation|41534|6|Mentioned|Fig.3|||||||||
18729|Turrum Formation|41727|6|Mentioned|p433|||||||||
18729|Turrum Formation|41868|6|Mentioned|p521|||||||||
18729|Turrum Formation|42827|4|Described|p343|||||||||
18729|Turrum Formation|43145|5|Briefly described|p10||Late Eocene|Of Latrobe Group.||||||
18729|Turrum Formation|60538|5|Briefly described|p475 Fig. 14|Middle Eocene|Middle Eocene|Geological Province: Gippsland Basin.||||||
18729|Turrum Formation|61155|5|Briefly described|p3, p18|Middle Eocene|Middle Eocene|Fine marine clastics. Geological Province: Gippsland Basin (offshore channel sequences). ||||||
18729|Turrum Formation|61212|5|Briefly described|p301 Fig. 2|Early Oligocene|Middle Eocene|Geological Province: Gippsland Basin.||||||
18729|Turrum Formation|61323|6|Mentioned|p3 Fig. 3|||Geological Province: Gippsland Basin.||||||
18729|Turrum Formation|61328|5|Briefly described|p112 Fig. 3|Oligocene|Eocene|Geological Province: Gippsland Basin.||||||
18729|Turrum Formation|61336|5|Briefly described|p(iv) Fig. 4|Late Eocene|Late Eocene|Of Cobia Group. Geological Province: Gippsland Basin. See also p(v) Fig. 5.||||||07-FEB-11
18729|Turrum Formation|61552|6|Mentioned|p583 Fig.2. |Eocene|Eocene|Marine sediments partly infilling major channels which were eroded, during the Early Eocene, into the shelf, shoreface and coaly coastal plain successions.||Unit in Cobia Subgroup.||||
18729|Turrum Formation|64876|5|Briefly described|p145 Fig.2|Eocene|Eocene|Gippsland Basin.||Cobia Subgroup.||||
18729|Turrum Formation|65717|6|Mentioned|p9 Fig.2.2, p11-13|Oligocene|Eocene|James and Evans (1971). Marine channel-fill sediments. One of the Latrobe Group's top seals. Appears also as Turum Formation on p12.||Cobia Subgroup||||05-SEP-17
18729|Turrum Formation|67727|5|Briefly described|p58 Fig.2.|Middle Eocene|Middle Eocene|Offshore Gippsland Basin. Marginal marine infill of the Tuna, Marlin and Opah Channels.||||Overlies Latrobe Group and Flounder Formation.||
18729|Turrum Formation|70076|5|Briefly described|South-Eastern: Fig.2; Regional: Fig.3|Priabonian|Bartonian|||Cobia Subgroup||Overlies Opah or Flounder Formation.||
18729|Turrum Formation|73562|5|Briefly described|p303-304, 312|Eocene|Eocene|James and Evans (1971). Gippsland Basin; offshore. Filled in the Marlin Channel (a submarine canyon) that incised into the Flounder Formation and underlying sediments of the Latrobe Group.||Latrobe Group.|||A marine silty shale.|
18729|Turrum Formation|73640|6|Mentioned|p3 Fig.2|Eocene|Eocene|Gippsland Basin; offshore.||Latrobe Group||||
18729|Turrum Formation|75065|5|Briefly described|p151, 168|Eocene|Eocene|Gippsland Basin; offshore. Sediments deposited in incised river valleys which became submarine canyons during transgressive phases.||Cobia Subgroup.||Unconformably overlies Flounder Formation.|Dark grey marine mudstones and glauconitic sandstones.|
37787|Two Eyed Creek Granodiorite|23309|6|Mentioned|p445, Appendix 1|||G387.||||||
37787|Two Eyed Creek Granodiorite|24551|6|Mentioned|p717 Table 2.4, 722 Table 8.5|Early Devonian|Early Devonian|Age: 401 +/- 2Ma.||||||
37787|Two Eyed Creek Granodiorite|60451|4|Described|p90, 220|Early Devonian|Early Devonian|Of the Stawell Pluton. Type section in text. Cover in many areas consists of White Hills Gravel as well as alluvium. Medium to coarse grained, grey, predominantly quartz & plagioclase feldspar, minor K-feldspar, hornblende & biotite. Age: 396-400 +/- 5Ma.||||||19-OCT-04
37787|Two Eyed Creek Granodiorite|60457|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Ararat Suite. Hornblende-biotite granodiorite: grey; medium to coarse grained; numerous quartz diorite, biotite granodiorite and country rock xenoliths; strongly foliated in part; I-Type.||||||
37787|Two Eyed Creek Granodiorite|60459|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Ararat Suite. Hornblende-biotite granodiorite: reduced, I-Type.||||||
37787|Two Eyed Creek Granodiorite|66002|5|Briefly described|p7 Tb.5|||Of Ararat Suite in Stawell Pluton area. G387. Defined by Cayley and Taylor 2001.||||||
37787|Two Eyed Creek Granodiorite|68116|5|Briefly described|Appendix, Map 30.|Early Devonian|Early Devonian||||||Hornblende-biotite granodiorite: grey; medium to coarse grained; numerous quartz diorite, biotite granodiorite and country rock xenoliths; strongly foliated in part; occasional small miarolitic cavities; reduced; I-type, nonmagnetic.|
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.||
29084|Tyers Conglomerate|22476|2|Defined|p954,5,6||Berriasian|Within the Strzelecki Group,  of Tyers River Subgroup.||||||22-DEC-08
29084|Tyers Conglomerate|24453|4|Described|p808, p809 Fig.2|Valanginian|Berriasian|Fluvial. Overlain by Rintoul Creek Formation. Of Tyers River Subgroup. Thickness: Up to 122 m. Geological Province: Gippsland Basin.||||||07-FEB-11
29084|Tyers Conglomerate|24551|5|Briefly described|p262 Fig. 9.29|Early Cretaceous|Early Cretaceous|Of the Strzelecki Group.||||||
29084|Tyers Conglomerate|30905|5|Briefly described|p160|||||||||
29084|Tyers Conglomerate|31352|6|Mentioned|p133|||||||||
29084|Tyers Conglomerate|41642|5|Briefly described|p230|||||||||
29084|Tyers Conglomerate|41868|6|Mentioned|p516|||||||||
29084|Tyers Conglomerate|42827|5|Briefly described|p230|||||||||
29084|Tyers Conglomerate|60452|6|Mentioned|p14|||In the Bassian Rift.||||||
29084|Tyers Conglomerate|60599|6|Mentioned|p84|||Outwash fan and braided stream deposits. Geological Province: Gippsland Basin. ||||||
29084|Tyers Conglomerate|61185|5|Briefly described|p56|Early Cretaceous|Late Jurassic|Deposits of scree, outwash fan and braided streams (Philip 1958). Geological Province: Gippsland Basin.||||||07-FEB-11
29084|Tyers Conglomerate|61302|5|Briefly described|p9|Early Cretaceous|Early Cretaceous|Same as Tyers Subgroup? Wedge of coarse clastics. Overlain by Wonthaggi Formation (Strzelecki Group). Geological Province: Gippsland Basin.||||||
29084|Tyers Conglomerate|61329|5|Briefly described|p124|Early Cretaceous|Early Cretaceous|Of Strzelecki Group. Max. thickness: 100m. Consists of well rounded and flattened pebbles of basement sandstone and subordinate vein quartz, quartzites, mudstones and shales, matrix of course angular vein quartz and sandstone.||||||12-FEB-08
29084|Tyers Conglomerate|63124|5|Briefly described|p61|||Of the lower Strzelecki Group. Geological Province: Gippsland Basin. Equivalent of Pretty Hill Formation sequence in Otway Basin.||||||
29084|Tyers Conglomerate|64535|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of Tyers River Subgroup (Otway Group). Conglomerate, pebbly sandstone, rare siltstone, shale; cobble, minor pebble and occasional boulder conglomerate massive to cross-bedded, polymictic; sandstone, coarse- to fine-grained, bedded; fluvial deposits.||||||22-DEC-08
29084|Tyers Conglomerate|64539|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of Tyers River Subgroup (Otway Group). Conglomerate, pebbly sandstone, rare siltstone, shale; cobble, minor pebble and occasional boulder conglomerate massive to cross-bedded, polymictic; sandstone, coarse- to fine-grained, bedded; fluvial deposits.||||||22-DEC-08
29084|Tyers Conglomerate|64540|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of Tyers River Subgroup (Otway Group). Conglomerate, pebbly sandstone, rare siltstone, shale; cobble, minor pebble and occasional boulder conglomerate massive to cross-bedded, polymictic; sandstone, coarse- to fine-grained, bedded; fluvial deposits.||||||22-DEC-08
29084|Tyers Conglomerate|64605|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Tyers River Subgroup (Otway Group). Conglomerate, pebbly sandstone, rare siltstone, shale; alluvial deposits. Speckled blue-green-pink in RGB. Nonmagnetic.||||||17-NOV-08
29084|Tyers Conglomerate|64616|3|Fully described|p141-143, p299|Early Cretaceous|Early Cretaceous|Of Bolger and Carey (1983). They used this name and the overlying unit which they named Rintouls Creek Sandstone, instead of Tyers Group, which was introduced by Philip (1958). Now the lower unit in Tyers River Subgroup; overlain conformably by Locmany Formation. Type section given. Thickness to 122m. Unconformably overlies Jordan River and Walhalla Groups. Conglomerates interbedded with lenses of sandstone; rare siltstone and shale. Geophysical characteristics given.||||||
29084|Tyers Conglomerate|65718|5|Briefly described|p11|Hauterivian|Berriasian|Derived from the Paleozoic basement present around the northern margin of the Gippsland Basin. Age constrained by the Tyers River Subgroup.||Of the Tyers River Subgroup.||Overlain by the Rintoul's Creek Sandstone.|Comprises a quartz-rich fluvial conglomerate.|10-JAN-17
29084|Tyers Conglomerate|68116|5|Briefly described|Appendix, Map 52.|Valanginian|Berriasian||||||Conglomerate, pebbly sandstone, rare siltstone, shale: cobble, minor pebble and occasional boulder conglomerate massive to cross-bedded, variable rounding, low sphericity, polymictic; sandstone very coarse to fine-grained, bedded.|
29084|Tyers Conglomerate|70378|5|Briefly described|p695-696, 698, 700, 702, p707, p709|Early Cretaceous|Early Cretaceous|Latrobe Valley. Also appears as Tyers conglomerate in Fig.2. Over 40m thick. Reservoir target for petroleum wells.||Tyers River Subgroup.||Is overlain by Locmany Member (Rintoul Creek Formation).|Polymict pebble conglomerate; numerous Paleozoic pebbles 1 to 3 cm in size in a mudstone matrix.|
29084|Tyers Conglomerate|75065|5|Briefly described|p151, 156-157|Valanginian|Valanginian|Gippsland Basin; onshore.||Tyers River Subgroup.||Is overlain by Rintoul Creek Formation.|Non-marine, basement metasediments-derived, conglomerate.|
33942|Tyers River Subgroup|13323|5|Briefly described|p394 Fig. 3|Valanginian|Berriasian|Of the Strzelecki Group. Non-marine to paralic clastics. Overlain by Korumburra Subgroup. Geological Province: Gippsland Basin.||||||26-JUN-06
33942|Tyers River Subgroup|22476|4|Described|p953-4|||Incorporates Tyers Conglomerate and Rintoul Creek Formation.||||||22-DEC-08
33942|Tyers River Subgroup|24164|5|Briefly described|p19, p21, p23, p41 Tb.2|Hauterivian|Valanginian|Deposition began by Valanginian and continued until Hauterivian (Dettman and Douglas, 1988 and Holdgate and McNichol, 1992). Age: ?Neocomian. Lithological descriptions imply sediments were locally derived from Palaeozoic rocks (Tosolini et al. 1999).||Strzelecki Group||Is overlain by Wonthaggi Formation|Generally quartzose fluvial; probably paludal and/or lacustrine|
33942|Tyers River Subgroup|24453|5|Briefly described|p808, p809 Fig.2|Hauterivian|Berriasian|Of Strzelecki Group. Geological Province: Gippsland Basin.||||||07-FEB-11
33942|Tyers River Subgroup|24551|6|Mentioned|p261||Neocomian|Of the Strzelecki Group.||||||
33942|Tyers River Subgroup|64535|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Otway Group. Contains Tyers Conglomerate and Locmany Formation.||||||16-DEC-08
33942|Tyers River Subgroup|64539|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Otway Group. Contains Tyers Conglomerate and Locmany Formation.||||||16-DEC-08
33942|Tyers River Subgroup|64540|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Otway Group. Contains Tyers Conglomerate and Locmany Formation.||||||16-DEC-08
33942|Tyers River Subgroup|64605|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Otway Group. Includes Tyers Conglomerate and Locmany Formation.||||||
33942|Tyers River Subgroup|64616|5|Briefly described|p142-144, p298-299|Early Cretaceous|Early Cretaceous|Of Tosolini et al. (1999), replacing Tyers Subgroup of Holdgate and McNicol (1992) and Chupka (1996). Now a unit in Otway Group. Includes Tyers Conglomerate and Locmany Formation. Includes all quartz-lithic rocks in the succession. Geophysical characteristics given.||||||
33942|Tyers River Subgroup|65718|5|Briefly described|p5, p10 Fig 3.2, p11, p44, p50, p54, p60|Hauterivian|Berriasian|Gippsland Basin. Neocomian age. Identified as a potential hydrocarbon and CO2 storage.||Basal unit of the Strzelecki Group.|Includes the Tyers Conglomerate and Rintoul's Creek Sandstone. ||Comprises alluvial fan conglomerates and fluvial coarse quartzose sandstones.|
33942|Tyers River Subgroup|66181|5|Briefly described|p310 Fig.5|Valanginian|Berriasian|Underlies the Eumeralla Formation, in the Otway Group.||||||
33942|Tyers River Subgroup|66244|5|Briefly described|p4.|Early Cretaceous|Early Cretaceous|The Strzelecki Group name is retained for the Early Cretaceous clastic sedimentary rocks of the Gippsland Basin, but not for the Otway and Bass Basins where such rocks fall under the Otway Group.||Unit in Strzelecki Group.||||
33942|Tyers River Subgroup|70378|5|Briefly described|p695-714|Barremian|Barremian|Tosolini et al. (1999). Previously the Tyers Group (Phillip, 1958). Latrobe Valley. In Yallourn North, these outcrops represent an uplifted separate sub-basin herein named the Monash trough. May not have been intersected in drilling south of the Princes Highway. Appears as Tyers River subgroup on p713.||Strzelecki Group.|Rintoul Creek Formation, Tyers Conglomerate.|Is overlain by Wonthaggi Formation.||
33942|Tyers River Subgroup|75065|5|Briefly described|p151, 156-157, 159, 172|Barremian|Valanginian|Tosolini et al. (1999). Gippsland Basin. Fossiliferous (species listed). Good hydrocarbon potential reservoir.||Strzelecki Group.|Tyers Conglomerate, Rintoul Creek Formation, Locmany Member.|Is overlain unconformably (onshore ) and conformably (offshore) by Korumburra Subgroup. Correlates with Crayfish Subgroup.|Sandstone, shale, coal, non-marine arkose and volcaniclastics.|
18759|Tynong Granite|23269|6|Mentioned|Fig14-3.1p403|||||||||
18759|Tynong Granite|23309|5|Briefly described|p347, 350||Late Devonian|G239 I-Type. Supersedes Tynong Adamellite.||||||
18759|Tynong Granite|24551|5|Briefly described|p225, 717 Table 2.4|Late Devonian|Late Devonian|Age: 368 +/- 2Ma.||||||
18759|Tynong Granite|31510|5|Briefly described|p9|||See also Table 1.||||||
18759|Tynong Granite|32001|6|Mentioned|p78|||||||||
18759|Tynong Granite|33607|6|Mentioned|Map legend|Devonian|Devonian|Granite, porphyritic, coarse-grained||||||29-NOV-04
18759|Tynong Granite|34843|6|Mentioned|p6|||||||||
18759|Tynong Granite|34956|6|Mentioned|p82|||||||||
18759|Tynong Granite|35073|6|Mentioned|p11|||See also Table 4.||||||
18759|Tynong Granite|35290|5|Briefly described|p22|||See also P20.||||||
18759|Tynong Granite|35712|6|Mentioned|p15|||||||||
18759|Tynong Granite|39291|6|Mentioned|Fig.13|||See also Fig.14||||||
18759|Tynong Granite|39331|6|Mentioned|Fig.1-1|||||||||
18759|Tynong Granite|41641|6|Mentioned|Fig.5.1|||||||||
18759|Tynong Granite|41868|6|Mentioned|p568|||See also P589||||||
18759|Tynong Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
18759|Tynong Granite|42827|5|Briefly described|p568|||see also Fig 5.1||||||
18759|Tynong Granite|44187|5|Briefly described|Map Legend||Late Devonian|G239 I-type.||||||
18759|Tynong Granite|61186|5|Briefly described|p45 Fig. 14|||Victorian dimension stone - coarse-grained, pale grey rock containing large white potassium feldspars. From the Tyong pluton. See also p67 and p68 Fig. 32.||||||02-JUL-13
18759|Tynong Granite|61328|6|Mentioned|p114|Paleozoic|Paleozoic|Age: 257.3+/-12.6Ma.||||||07-NOV-08
18759|Tynong Granite|63445|5|Briefly described|Map legend.|Late Devonian|Late Devonian||||||I-type granite.|
18759|Tynong Granite|64616|6|Mentioned|p316-318, p332, p335-336, p344|||Strathbogie Domain. Gravity readings suggest it is a steeply dipping structure. Geophysical modelling discussed.||||||
18759|Tynong Granite|65900|5|Briefly described|p156, p157, p160 Fig. 4, p161, 162, 169||Late Devonian|Intrudes Melbourne Zone folded rocks. Granite is non-magnetic, and shows as gravity low. Includes magnetic dykes.||||||
18759|Tynong Granite|66244|6|Mentioned|p6.|||||||||
18759|Tynong Granite|68116|5|Briefly described|Appendix, Maps 42-43, 51.|Late Devonian|Late Devonian||||||Biotite granite: medium grained, porphyritic; pale grey.|
18759|Tynong Granite|75072|6|Mentioned|p250|||Has the least proportion of zircon inheritance of the samples analysed in this study.||||||
18760|Tynong Suite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
18760|Tynong Suite|42827|6|Mentioned|p433|||||||||
18760|Tynong Suite|64616|5|Briefly described|p129|||Of Tynong Supersuite of White and Chappell (1988). Suite characterised by hornblende-ilmenite granites. ||||||
18760|Tynong Suite|65715|5|Briefly described|p7 Tb.4|||Tynong Supersuite in White and Chappell (1988). Demoted to Suite status by Rossiter (2003). Includes You Yangs Granite.||||||02-JUL-13
18764|Tyrrell beds|42510|5|Briefly described|p35|||Variation of Tyrrell Beds.||||||
18764|Tyrrell beds|42518|6|Mentioned|p185|||||||||
18764|Tyrrell beds|42966|2|Defined|Table 37 p261|Holocene|Late Pleistocene|||||||
30282|Undowah Siltstone|23309|5|Briefly described|p90, 95, 97. Table 2.32|||||||||
30282|Undowah Siltstone|24551|4|Described|p136, 137|||Of the Wombat Creek Group.||||||
30282|Undowah Siltstone|60503|3|Fully described|p96-98|Silurian|Silurian|Originally included in Toaks Creek Conglomerate. Thin unit of siltstone and volcanolithic sandstone. Contains a thin limestone lens ("Hairpin"). Conformably overlain by Toaks Creek Conglomerate; nonconformably overlies Mitta Mitta Rhyolite.||||||16-NOV-09
30282|Undowah Siltstone|60504|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Wombat Creek Group. Mudstone; grey-green and red, with basal graded volcanogenic sandstone and conglomerate consisting of reworked rhyolite lava clasts||||||
30282|Undowah Siltstone|60505|5|Briefly described|Map legend|Pridoli|Ludlow|Of the Wombat Creek Group. Mudstone; grey-green and red, with basal graded volcanogenic sandstone and conglomerate consisting of reworked rhyolite lava clasts||||||20-OCT-04
30282|Undowah Siltstone|60506|5|Briefly described|Map legend|Pridoli|Ludlow|Of the Wombat Creek Group. Mudstone; grey-green and red, with basal graded volcanogenic sandstone and conglomerate consisting of reworked rhyolite lava clasts||||||
30282|Undowah Siltstone|60507|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Wombat Creek Group. Mudstone; grey-green and red, with basal graded volcanogenic sandstone and conglomerate consisting of reworked rhyolite lava clasts||||||
30282|Undowah Siltstone|60508|5|Briefly described|Map legend|Late Silurian|Late Silurian|Of the Wombat Creek Group. Mudstone: nonmagnetic (0-5 nT); low total count, K, Th, U||||||08-NOV-04
30282|Undowah Siltstone|68116|5|Briefly described|Appendix, Map 27|Pridoli|Ludlow||||||Siltstone: grey-green and red, with basal graded volcanigenic sandstone and conglomerate of reworked rhyolite lava clasts.|
30282|Undowah Siltstone|71040|6|Mentioned|p10 Fig.6|Silurian|Silurian|||||||
39644|United Sandstone|24088|6|Mentioned|p355 Fig. 4|||Geological Province: Lachlan Fold Belt.||||||18-JAN-16
69609|Uplands Province Volcanics|61155|5|Briefly described|p19|Late Pliocene|Late Pliocene| Age: ~3.0-<2.0Ma. In the Ovens, Buchan Valleys, Victoria.||||||
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.|
26974|Vereker Granite|23309|6|Mentioned|p445 App1|||G259. S-Type.||||||
26974|Vereker Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
26974|Vereker Granite|68116|5|Briefly described|Appendix, Map 57.|Middle Devonian|Middle Devonian||||||Leucocratic granite: medium to coarse grained; with garnet and cordierite; S-type.|
82046|Victor Porphyry|70967|6|Mentioned|p10|Cambrian|Cambrian|Mount Stavely Belt. Mineralised.|c.500 Ma (Lewis et al., 2015).|||||
82046|Victor Porphyry|72445|6|Mentioned|p9.|Cambrian|Cambrian|A mineralised porphyry intrusion within Mount Stavely Belt. Igneous crystallisation age determined by Lewis et al., 2015.|c. 500 Ma igneous crystallisation|||||
19099|Victoria River Complex|40811|6|Mentioned|p321|||||||||
74001|Victoria Valley Complex|63599|5|Briefly described|p975|Early Devonian|Early Devonian|Included in the Mafeking Suite. Age: 396Ma.||||||02-OCT-09
74001|Victoria Valley Complex|71593|4|Described|p47, p81, p85|Devonian|Devonian|Geochemically and temporally similar to the Rocklands Volcanic Group.|c. 400 Ma|||||
76920|Violet Town Volcanic Group|66244|5|Briefly described|p3.|||Rocks described previously as Baddaginnie Granite are now recognised as ignimbrites of the Violet Town Volcanic Group.|||||Ignimbrites; coarse-grained with recrystallised groundmass; enstatite common.|
76920|Violet Town Volcanic Group|68116|5|Briefly described|Appendix, Map 25.|Late Devonian|Late Devonian|Informally subdivided into rhyodacite and rhyolite phases. Rhyodacite: recrystallization commonly obliterates eutaxitic fabric; cordierite and garnet in a microgranular groundmass of quartz and feldspar. Contains sedimentary xenoliths at its base.|||||Rhyodacite: ignimbrite, orthoclase phenocrysts, euhedral quartz, plagioclase, biotite and uncommon enstatite. Rhyolite: ignimbrite, orthoclase and euhedral quartz phenocrysts in a cordierite, garnet and biotite groundmass.|
19126|Violet Town Volcanics|22602|6|Mentioned|p434|||||||||
19126|Violet Town Volcanics|22779|5|Briefly described|p 172|||||||||
19126|Violet Town Volcanics|23232|6|Mentioned|p64|||||||||
19126|Violet Town Volcanics|23235|6|Mentioned|Fig7-1p68, 68|||||||||
19126|Violet Town Volcanics|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
19126|Violet Town Volcanics|24096|5|Briefly described|p6|||Consist of thick ash flow sheets overlying a thin discontinuous rhyolite at tha base.||||||18-APR-05
19126|Violet Town Volcanics|24108|6|Mentioned|p235|||||||||
19126|Violet Town Volcanics|24109|5|Briefly described|p282|Devonian|Devonian|Geological Province: Murray Basin. Maximum thickness: >6 m. Age: ca. 370 Ma.||||||
19126|Violet Town Volcanics|24551|4|Described|p161|||Part of the Strathbogie Igneous Complex.||||||
19126|Violet Town Volcanics|29786|6|Mentioned|p77|||||||||
19126|Violet Town Volcanics|30906|6|Mentioned|Map legend|Devonian|Devonian|||||||
19126|Violet Town Volcanics|31713|5|Briefly described|p7|||||||||
19126|Violet Town Volcanics|32074|6|Mentioned|p182|||||||||
19126|Violet Town Volcanics|35277|5|Briefly described|p96|||||||||
19126|Violet Town Volcanics|35278|6|Mentioned|p353|||||||||
19126|Violet Town Volcanics|36389|5|Briefly described|p39|||||||||
19126|Violet Town Volcanics|39291|4|Described|p214|||See also Fig.1||||||
19126|Violet Town Volcanics|39331|6|Mentioned|Fig.0-3|||||||||
19126|Violet Town Volcanics|39861|4|Described|p354|||||||||
19126|Violet Town Volcanics|41133|4|Described|p1118|||||||||
19126|Violet Town Volcanics|41553|6|Mentioned|p446|||||||||
19126|Violet Town Volcanics|41563|6|Mentioned|p506|||||||||
19126|Violet Town Volcanics|41641|6|Mentioned|p166|||||||||
19126|Violet Town Volcanics|42154|6|Mentioned|Table 1 P334|||||||||
19126|Violet Town Volcanics|42726|5|Briefly described|map legend|Middle Devonian||||||||
19126|Violet Town Volcanics|42827|5|Briefly described|p166|||||||||
19126|Violet Town Volcanics|43202|5|Briefly described|p20,22.||Middle Devonian|||||||
19126|Violet Town Volcanics|43850|6|Mentioned|p270|||||||||
19126|Violet Town Volcanics|61185|5|Briefly described|p47|Late Devonian|Late Devonian|Of Strathbogie igneous complex (White 1954; Laing et al 1977).||||||07-FEB-11
19126|Violet Town Volcanics|61210|5|Briefly described|p246 Fig. 2|Devonian|Devonian|Overlain by Violet Town quarry lava flow.||||||17-JAN-06
19126|Violet Town Volcanics|64312|6|Mentioned|p433|||||||||
19126|Violet Town Volcanics|64616|5|Briefly described|p127|||Of White (1954). Felsic volcanics. Of Strathbogie Igneous Complex. Coeval with Strathbogie Granite.||||||
19126|Violet Town Volcanics|65900|5|Briefly described|p155, p156 Fig. 2, p156, Fig.3||Late Devonian|Upper Devonian. Contains phenocrysts formed at 500-600 MPa,and gneiss and granulite xenoliths. S-type magma.||||||10-MAY-12
19126|Violet Town Volcanics|67978|6|Mentioned|p496 Fig.1, p500 Table 1, p519|Late Devonian|Late Devonian|Zircon from rhyodacite (Kemp et al. 2008).|373 +/- 6 Ma, SIMS U-Pb|||||13-SEP-18
19126|Violet Town Volcanics|68311|6|Mentioned|p286|||Magma composition results from internally heterogeneous protoliths, not magmatic differentiation.|||||Rhyodacites and high-SiO2 rhyolites.|
19126|Violet Town Volcanics|70933|14|Not recorded|p102||Late Devonian|Map.||||||
19126|Violet Town Volcanics|73199|6|Mentioned|p521-522, p524-526|Frasnian|Frasnian|S-type. Inferred to have similar deep-crustal sources to plutonic granitic magmas.|373 Ma||||Relatively crystal-rich low-silica rhyolitic ignimbrites.|
19126|Violet Town Volcanics|75061|6|Mentioned|p68||||||||Rhyolitic to rhyodacitic ignimbrites.|
19126|Violet Town Volcanics|75062|6|Mentioned|p74 Fig.2, p87 Fig.14|Devonian|Devonian|Melbourne Zone. Harker-type plots.|||||S-type.|
39641|Vital Shale|24088|6|Mentioned|p355 Fig. 4||| Geological Province: Lachlan Fold Belt.||||||
34893|Vitric Ignimbrite Member|22968|4|Described|p125-126, 128-129|Late Silurian|Late Silurian|Informal name, type section location given on p125. Age of unit is 416+/-5 Ma (U/Pb zircon age [probably SHRIMP]. Parent is Blackfellows Flat Formation, maximum thickness is 250m||||||10-SEP-18
34893|Vitric Ignimbrite Member|23021|5|Briefly described|Map legend|Ludlow|Ludlow|Parent is Blackfellows Flat Conglomerate, underlying unit is Berrawan Conglomerate||||||
34893|Vitric Ignimbrite Member|23309|5|Briefly described|p126|Silurian|Silurian|Age: 416+/-5 Ma.||||||
34893|Vitric Ignimbrite Member|24551|6|Mentioned|p140|||Informal name. Of the Blackfellows Flat Formation.||||||
34893|Vitric Ignimbrite Member|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Blackfellows Flat Conglomerate (Mount Tambo Group). Pyroclastics: vitric ignimbrite; fluvial conglomerate, pebbly sandstone||||||20-OCT-04
34893|Vitric Ignimbrite Member|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Blackfellows Flat Conglomerate (Mount Tambo Group). Pyroclastics: vitric ignimbrite; fluvial conglomerate, pebbly sandstone||||||21-OCT-04
34893|Vitric Ignimbrite Member|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Blackfellows Flat Conglomerate (Mount Tambo Group). Pyroclastics: vitric ignimbrite; fluvial conglomerate, pebbly sandstone||||||21-OCT-04
34893|Vitric Ignimbrite Member|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Blackfellows Flat Conglomerate (Mount Tambo Group). Pyroclastics: vitric ignimbrite; fluvial conglomerate, pebbly sandstone||||||21-OCT-04
32295|Volador Formation|13323|5|Briefly described|p393 Fig. 2|Maastrichtian|Maastrichtian|Of the Halibut Subgroup (Latrobe Group). Includes the Roundhead and Bonita Sandstone Member. Fluvial-deltaic and paralic deposits - shales, sands and minor coal. Geological Province: Gippsland Basin. ||||||
32295|Volador Formation|24090|5|Briefly described|p8 Fig.3|Maastrichtian|Maastrichtian|Contains the Roundhead Member and Bonita Sandstone Member.  Geological Province: Gippsland Basin.||||||19-JAN-05
32295|Volador Formation|24407|5|Briefly described|p13 Fig.2|||Geological Province: Gippsland Basin||||||
32295|Volador Formation|24551|5|Briefly described|p262 Fig. 9.29, 267|Paleocene|Late Cretaceous|Of the Halibut Subgroup.||||||
32295|Volador Formation|61552|4|Described|p581, pp583-590, p592.  |Maastrichtian|Maastrichtian|Deposited in lower coastal plain environments. This unit is the lateral, seaward equivalent of the Barracouta Formation. Type section is in Volador-1 well.||Of the Halibut Subgroup. |Includes Roundhead Member.|Is overlain by Kingfish Formation and, to the east, by Kate Shale. Interfingers with the Barracouta Formation to the west.|Includes coal.|
32295|Volador Formation|64876|5|Briefly described|p144-149, p151, p153-155|Late Cretaceous|Late Cretaceous|Gippsland Basin. Transgressive barrier-island deposits. Depositional environments and facies described in detail.||Latrobe Group.|Roundhead Member.||Fine- to medium-grained, highly bioturbated sandstone, lagoonal and ofshore marine shales.|
32295|Volador Formation|65717|5|Briefly described|p9 Fig.2.2, p11, p13|Paleocene|Maastrichtian|Comprises typical lower coastal plain coal-rich sediments.||Halibut Subgroup|Includes Roundhead Member|Interbedded with Bonita Sandstone Member. Is overlain by Kate Shale.|Interbedded sandstone, siltstone, shale and coal.|05-SEP-17
32295|Volador Formation|65973|4|Described|p16, 29, 31, 35, 40-41, 43, 57, 62, 65|Maastrichtian|Maastrichtian|Gippsland Basin. Comprises typical lower coastal plain coal-rich sediments. Deposited in a fluvial/alluvial environment with the shales being of lacustrine/paludal origin. Intersected in Manta-1, Kipper-1, Kipper-2, Leatherjacket-1, Judith-1, Hammerhead-1, East Pilchard-1, Longtom-1, Longtom-1/ST-1, Longtom-2/ST-1, Shark-1, Sole-1, Sweep-1 and many more drillholes (see appendix). Petroleum system characteristics are discussed. See also p71, p76, p78, p80, p82, p86, p90, p93, p97, p100, p106, p108, p110, p112, p114, p118, p123-135, p138-141, p144, p171.||Halibut Subgroup||Overlain by the Kate Shale.|Sandstones interbedded with shales.|
32295|Volador Formation|70028|6|Mentioned|p79|Maastrichtian|Maastrichtian|Offshore Gippsland Basin.||||||
32295|Volador Formation|70076|5|Briefly described|South-Eastern:Fig.2;p2.Regional:Fig.3;p3|Maastrichtian|Campanian|Hydrocarbon reservoir. Lower coastal plain, coal-rich sediments.||Halibut Subgroup.|Roundhead and Manta Members.|Overlies Anemone or Chimaera Formation. Is overlain by Kate Shale or Kingfish Formation.||
32295|Volador Formation|73471|5|Briefly described|p86|||Gippsland Basin.||Halibut Subgroup||Underlies Kate Shale, Kingfish Formation|Fluvial-deltaic and paralic sandstones and siltstones with interbedded coal layers.|
32295|Volador Formation|75065|5|Briefly described|p151|Maastrichtian|Maastrichtian|Gippsland Basin; offshore. Fluvial-deltaic and paralic sediments.||Halibut Subgroup.||Unconformably overlies Chimaera Formation (Golden Beach Subgroup). Is overlain by Kingfish Formation and Kate Shale.|Sandstone, siltstone, shale, coal.|
19156|Waaia Member|35091|6|Mentioned|Table 1|||||||||
19156|Waaia Member|42966|5|Briefly described|p409, p210|||of Shepparton Formation. Variation on Waaia Sand Member.||||||
33675|Waalima Granodiorite|22815|4|Described|p88|||||||||
33675|Waalima Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Unassigned pluton, Bega Batholith.||||||
19163|Waarre Formation|12781|6|Mentioned|p386|Late Cretaceous|Late Cretaceous|Otway Basin. Maximum thickness 204m.||Sherbrook Group.||Overlies and abuts Copa Formation. Unconformably overlies Eumeralla Formation. Is overlain unconformably by Timboon Sandstone and Flaxman Formation.||
19163|Waarre Formation|12796|5|Briefly described|p457, p456 Fig. 2|Turonian|Turonian|Of the Sherbrook Group. Geological Province: Otway Basin.||||||
19163|Waarre Formation|22470|5|Briefly described|p13 Fig. 17|Turonian|Turonian|Of Sherbrook Group.||||||
19163|Waarre Formation|22674|5|Briefly described|Fig.2 p719|Turonian|Cenomanian|||||||
19163|Waarre Formation|23818|5|Briefly described|p166, Fig.80|||Overlying unit: Flaxman Formation.||||||
19163|Waarre Formation|23916|6|Mentioned|p534|Cretaceous|Cretaceous|||||||
19163|Waarre Formation|24284|6|Mentioned|p15 Fig.2|||Otway Basin.||||||
19163|Waarre Formation|24551|6|Mentioned|p252||Late Cretaceous|Overlies the Eumeralla Formation. Maximum Thickness: 636m.||||||
19163|Waarre Formation|29856|5|Briefly described|p38|||||||||
19163|Waarre Formation|30499|6|Mentioned|p92|||Stratigraphy||||||
19163|Waarre Formation|30578|6|Mentioned|p7|||||||||
19163|Waarre Formation|30905|6|Mentioned|Table 7.4|||||||||
19163|Waarre Formation|31424|6|Mentioned|p32|||Sedimentology||||||
19163|Waarre Formation|31714|6|Mentioned|Fig. 8|||||||||
19163|Waarre Formation|32344|6|Mentioned|Fig.2|||||||||
19163|Waarre Formation|32896|6|Mentioned|Encl.7.1.|||U.Cret.||||||
19163|Waarre Formation|33936|6|Mentioned|Fig.6|||U.Cret.||||||
19163|Waarre Formation|33943|6|Mentioned|p379|||See also P383 & Fig. 20-2.||||||
19163|Waarre Formation|34063|6|Mentioned|p3|||Table. U.Cret.||||||
19163|Waarre Formation|34148|6|Mentioned|p285|||Lower Cretaceous.||||||
19163|Waarre Formation|34611|6|Mentioned|Fig.80|||Upper Cretaceous||||||
19163|Waarre Formation|36499|6|Mentioned|p36|||||||||
19163|Waarre Formation|38155|6|Mentioned|p14|||||||||
19163|Waarre Formation|40947|6|Mentioned|p4|||||||||
19163|Waarre Formation|41269|5|Briefly described|p245|||||||||
19163|Waarre Formation|41642|6|Mentioned|Table 7.12|||||||||
19163|Waarre Formation|41714|4|Described|p303|||||||||
19163|Waarre Formation|41726|5|Briefly described|p420|||See also P425||||||
19163|Waarre Formation|41769|6|Mentioned|p69|||||||||
19163|Waarre Formation|41868|4|Described|p533|||||||||
19163|Waarre Formation|41994|5|Briefly described|p6|||||||||
19163|Waarre Formation|42152|4|Described|p13|||See also P31||||||
19163|Waarre Formation|42153|5|Briefly described|p352|||See also Fig. 15||||||
19163|Waarre Formation|42599|5|Briefly described|Fig.3 P614|||||||||
19163|Waarre Formation|42827|5|Briefly described|p533|||Of Sherbrook Group.||||||14-APR-08
19163|Waarre Formation|43171|6|Mentioned|5|||||||||
19163|Waarre Formation|43208|5|Briefly described|map legend|Turonian|Cenomanian|Of Sherbrook Group.||||||
19163|Waarre Formation|43219|5|Briefly described|Fig.3,p6.||Cenomanian|Of Sherbrook Group.||||||14-APR-08
19163|Waarre Formation|43590|4|Described|p13|Turonian|Cenomanian|||||||
19163|Waarre Formation|43744|6|Mentioned|Fig.3,p3|||||||||
19163|Waarre Formation|43783|6|Mentioned|Fig14, p11||Late Cretaceous|||||||
19163|Waarre Formation|43784|6|Mentioned|Fig10, p12||Late Cretaceous|||||||
19163|Waarre Formation|43937|5|Briefly described|Map Legend|Santonian|Aptian|||||||
19163|Waarre Formation|48581|2|Defined|p35|||See also p1,12,16,28-31,34,39,40,Fig.4,Pl.1,2. (J54-12/Port Campbell).||||||
19163|Waarre Formation|48624|14|Not recorded|p1,5,7,Fig.2|||(J54-6/Benara).||||||
19163|Waarre Formation|48631|14|Not recorded|p5,7||Cretaceous|Otway Basin.||||||
19163|Waarre Formation|48911|3|Fully described|p16|||Lower - Upper Cretaceous||||||
19163|Waarre Formation|48977|6|Mentioned|Fig.5|||||||||
19163|Waarre Formation|49060|5|Briefly described|Fig.33|||||||||
19163|Waarre Formation|61016|6|Mentioned|p13|||See also Waarre formation.  Geological Province: Otway Basin.||||||20-APR-05
19163|Waarre Formation|61017|5|Briefly described|p5, p6|Turonian|Turonian|Geological Province: Otway Basin.||||||07-FEB-11
19163|Waarre Formation|61182|3|Fully described|p15-16, p31, p87-88|Turonian|Cenomanian|Of Sherbrook Gp (originally incl. in Otway Gp). Formerly known as Waarre Sandstone also. Unconformably overlies Eumeralla Fm; conformably overlain by Flaxman Fm and Belfast Mudstone. Max. thick: 180m. Geol.Province: Otway Basin. Mainly quartz sandstone.||||||
19163|Waarre Formation|61230|5|Briefly described|p319 Fig.2, pp325-326, pp337-338.    |Turonian|Turonian|Of the Otway Delta. Delta plain to shallow marine delta front conditions. TOC values vary from high to very high. Dinoflagellate diversity increases upwards.||Unit in Sherbrook Group.||Overlain by the Flaxman Formation.|Dominantly fine-medium quartz sandstone, with carbonaceous siltstone; minor coal.|
19163|Waarre Formation|61470|5|Briefly described|p27, p28 Fig. 5|Turonian|Cenomanian|Represents the main hydrocarbon play in the Port Campbell Embayment.||||||12-OCT-05
19163|Waarre Formation|61471|6|Mentioned|p34|||See also Waarre formation.  Geological Province: Otway Basin.||||||12-OCT-05
19163|Waarre Formation|61623|6|Mentioned|p449 Fig. 4|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
19163|Waarre Formation|61625|5|Briefly described|p475, p476 Fig. 1, p477|Late Santonian|Late Cenomanian|Of Sherbrook Group. Geological Province: Otway Basin. Heavily burrowed carbonaceous coarse-grained sandstone. Has common microplankton.||||||07-FEB-11
19163|Waarre Formation|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4, p492|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Underlain by Eumeralla Formation.  Geological Province: Otway Basin.||||||07-APR-09
19163|Waarre Formation|61628|5|Briefly described|p507, p509 Fig. 3, p510, p511|Late Cretaceous|Late Cretaceous|Of Sherbrook Group. Geological Province: Otway Basin.||||||07-APR-09
19163|Waarre Formation|63124|5|Briefly described|p48 Fig. 5.1|||Introd.by McQueen (1961).Variously Waarre Fm and Waarre Sst. Here, authors revert to Waarre Sst and Copa Fm. Conformable over Copa Fm; unconformable below Flaxman Fm. Geol.Prov:Otway Basin. May correlate with Wombat Sst Mbr (Wigunda Fm) in Duntroon Basin.||||||31-JAN-08
19163|Waarre Formation|63130|5|Briefly described|p143|Late Cretaceous|Late Cretaceous|Overlies Eumeralla Formation. Geological Province: Otway Basin.||||||06-FEB-08
19163|Waarre Formation|63269|5|Briefly described|p605|Late Cretaceous|Late Cretaceous|Otway Basin. See also Waarre Sandstone (p606-607).||Sherbrook Group.||||
19163|Waarre Formation|66245|5|Briefly described|p6 Fig.5, pp61-62 Fig.C1-C2, p68 Fig.D4.|Turonian|Turonian|Shipwreck Trough. Extensive shallow marine reservoirs and coaly source rocks combine to produce an effective petroleum system, with the right burial history.||Unit in Sherbrook Group.||Is overlain by Flaxman Formation.||
19163|Waarre Formation|67061|6|Mentioned|p546 Fig.3.|Turonian|Turonian|||Unit in Sherbrook Group.||||
19163|Waarre Formation|67366|5|Briefly described|p101, pp104-109. |Turonian|Turonian|Marginal marine and lower coastal plain sandstone and mudstone. Hosts gas reserves in Halladale and Black Watch gas fields, which were discovered by amplitude versus offset (AVO) anomalies seismic interpretation.||Basal unit in Sherbrook Group.||Is overlain by Flaxman Formation.|3 units: A is a sequence of interbedded shale and lithic sandstones; B has carbonaceous siltstone and claystone with occasional thin beds of sand; C is a fine- to coarse-grained quartz-rich sandstone with excellent porosity and permeability.|
19163|Waarre Formation|67367|5|Briefly described|p131 Fig.2. |Turonian|Turonian|Hydrocarbon reservoir. Assigned to the Austral 2 petroleum sub-system. A viable source rock.||Basal unit in Sherbrook Group.||||
19163|Waarre Formation|69297|5|Briefly described|p78, p79, p83, p84, p86, p98, p115-p117|Turonian|Cenomanian|Otway and Sorell Basins. Deposited in marine, marginal marine or coastal plain environments. Major potential reservoir unit in both the Otway and Sorell Basins. ||Shipwreck Supersequence||Overlies the Copa Formation. Unconformably overlies the Eumeralla Formation. Overlain by the Flaxman Formation. |Sandstones. |
19163|Waarre Formation|69651|5|Briefly described|p10, p15, p30-34, p37-39, p43-44, p50|Late Cretaceous|Late Cretaceous|Otway Basin. Turonian. Marine, marginal marine and coastal plain sediments. First hydrocarbon column intersected in the Basin (1959). The main regional reservoir in the Basin in Victoria. Sealed by Belfast Mudstone. Modelling diagrams.||Sherbrook Group.||Unconformably overlies Eumeralla Formation (Otway Group). Is overlain by Flaxman Formation.|Includes sandstones.|
19163|Waarre Formation|69879|5|Briefly described|p424|Turonian|Turonian|Otway Basin. Hydrocarbon reservoir in the Thylacine gas-condensate field. More deeply buried sediments are possibly hydrocarbon source.||||Underlies Flaxman Formation.|Fluvio-deltaic sandstone.|
19163|Waarre Formation|70077|5|Briefly described|Nelson: Fig.2; p1-2. Regional: Fig.4|Turonian|Turonian|See also Regional: p5, p7-8, p10-12. Otway Basin. Possible viable source rock. The major regional reservoir in Victorian part of the Basin. Has produced gas in 16 inshore fields in the Port Campbell area. Distal equivalents in the Nelson Sub-basin may be important petroleum reservoirs.||Sherbrook Group.||Overlies Copa or Eumeralla Formations. Is overlain by Flaxman Formation.||
19163|Waarre Formation|70078|5|Briefly described|Northern:Fig.2; p2. Regional:Fig.4; p4-6|Turonian|Turonian|Otway Basin. Equivalent sandstones in the Sorell Basin are potential reservoirs. Contains potential structural traps (high-side fault traps and faulted anticlines).||Sherbrook Group.||Overlies Copa Formation. Is overlain by Flaxman Formation.||
19163|Waarre Formation|70193|6|Mentioned|p284 Fig 2, p285 fig 3|Turonian|Turonian|Geological province: Otway Basin. Part of the Sherbrook Supersequence.||||Unconformably overlies Eumeralla Formation.||
19163|Waarre Formation|70880|6|Mentioned|p77|Turonian|Turonian|Otway Basin.||||||
19163|Waarre Formation|71266|6|Mentioned|p614 Fig.3|Late Cretaceous|Late Cretaceous|Otway Basin.||||||
19163|Waarre Formation|73357|5|Briefly described|p20, p31, p45, p47|Turonian|Turonian|Otway Basin. Correlated with Phyllocladidites mawsonii Spore-Pollen Zone, and Palaeohystrichophora infusorioides Dinocyst Zone marking a marine transgression with marginal to shallow marine facies.||Of Sherbrook Group.||Underlies Flaxman Formation.||
19163|Waarre Formation|73383|5|Briefly described|p3, p10 Tb.3.7, p11 Tb.3.9, p21-22, p68|Turonian|Cenomanian|Otway Basin. Approximately equivalent to the S5-P1 chemostratigraphic package in lower part and S5-P2 package in upper part. Higher Fe and P values and lower Si/Al values in lower part, more quartz-rich in upper part. Mudstone-dominated Package S5-P3 is only identified in Penryn-1, interpreted as uppermost part of formation. Lithologies based on geochemistry using the ChemLith classification includes argillaceous sandstone and limestone, and using the Herron classification (1988) includes quartz arenite, Fe-sand, Fe-shale, shale, wacke and lith-arenite. See also vi, p135-136, p200-201, p262-263. Waarre Formation Unit C and Waarre Formation Unit B are used on p135 and p262, and Waarre Formation Unit A on p135-136, p262-263.||Sherbrook Group||Unconformably overlies Eumeralla Formation, Otway Group, underlies Flaxman Formation|Sandstones, mudstones. Mature quartz-rich sandstone in upper part. Mudstone-dominated package in uppermost part.|
19163|Waarre Formation|73385|5|Briefly described|p5|Turonian|Cenomanian|Otway Basin.||Sherbrook Group||Overlies Eumeralla Formation, underlies Flaxman Formation.|Marginal marine and lower coastal plain sandstones, mudstones.|
19163|Waarre Formation|73386|4|Described|p4, p6, p10, Attachment A1|Turonian|Turonian|Otway Basin. First described in Bain and McQueen (1960), and Wood and Bain (1961). Type section is defined between 2494.5 m and 2675.3 m in Port Campbell-2 (Morton et al., 1994). Four sub-units previously identified, unit D originally termed Flaxman Beds and now referred to as the Flaxman Formation. Waarre Formation unit C is the primary hydrocarbon reservoir interval in the Otway Basin. Lies within the Phyllocladidites mawsonii Spore-Pollen Zone. Formation intersected primarily in the Port Campbell Embayment, Shipwreck Trough and Mussel Platform, sediments of similar age interpreted in the central and western Otway Basin are interpreted here as Warre Formation equivalent. Waarre Formation Eq. appears in multiple boreholes, Attachment A1.||Sherbrook Group||Overlies Eumeralla Formation, Otway Group, conformably underlies Flaxman Formation|Characterised by clean quartzose sandstones, conglomerates and minor siltstones and shales.|
19163|Waarre Formation|73594|5|Briefly described|p4-5, p13-16, p24-25, p27-35, p38, p66|Turonian|Cenomanian|Principal gas-bearing reservoir in the Otway Basin. Subdivided into units A, B and C (includes Ca and Cb) in the Port Campbell Embayment, not always possible to recognise these units in other places. Thickens substantially in the Shipwreck Trough. Fluvial to marginal marine environments. Diverse assemblage of marine microplankton at base interpreted to reflect flooding over a short time period (Partridge, 1997).||Sherbrook Group||Overlies Eumeralla Formation. Underlies Flaxman Formation|Transgressive sequence of sandstones, mudstones and coals. Includes a basal fine-grained lithic sandstone interbedded with mudstones and coals, overlain by carbonaceous siltstones and mudstones, fine to coarse grained quartz sandstones.|
37788|Wabba Granite|23309|6|Mentioned|p446, Appendix 1|||G95, S-Type. Supersedes Wabba Granodiorite.||||||
37788|Wabba Granite|24133|3|Fully described|p61|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37788|Wabba Granite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37788|Wabba Granite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37788|Wabba Granite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
37788|Wabba Granite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Two-mica granite: grey, medium to coarse grained; includes both fine grained and coarse grained porphyritic areas; S-type; nonmagnetic||||||09-SEP-04
37788|Wabba Granite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Biotite-muscovite granite: S-type; nonmagnetic; moderate to high K, moderate to low Th, moderate U||||||09-SEP-04
37788|Wabba Granite|24551|6|Mentioned|p233|||||||||
37788|Wabba Granite|68116|5|Briefly described|Appendix, Map 20.|Pridoli|Wenlock||||||Biotite-muscovite granite: grey, medium to coarse grained; includes both fine grained and coarse grained porphyritic areas; S-type; nonmagnetic.|
68436|Wabonga Volcanic Complex|24551|6|Mentioned|p218|||||||||
68436|Wabonga Volcanic Complex|64312|5|Briefly described|p435 Fig. 2|Late Devonian|Late Devonian|Includes the Toombullup, Ryans Creek and Hollands Creek Ignimbrites. Rich in barium. ||||||
68436|Wabonga Volcanic Complex|66769|6|Mentioned|142|||Tabberabbera Zone. Ba-rich||||||
74884|Wahroonga Breccia|64536|5|Briefly described|Map legend|Cambrian|Cambrian|Sandstone, breccia: green-grey; massive to well bedded; medium to very thick bedded; phosphatic; abundant lithic clasts; contains brachiopod and phyllocarid fossils. Deep-marine mass flow deposits.||||||07-FEB-11
74884|Wahroonga Breccia|64537|5|Briefly described|Map legend|Cambrian|Cambrian|Sandstone, breccia: green-grey; massive to well bedded; medium to very thick bedded; phosphatic; abundant lithic clasts; contains brachiopod and phyllocarid fossils. Deep-marine mass flow deposits.||||||07-FEB-11
74884|Wahroonga Breccia|64538|5|Briefly described|Map legend|Cambrian|Cambrian|Sandstone, breccia: green-grey; massive to well bedded; medium to very thick bedded; phosphatic; abundant lithic clasts; contains brachiopod and phyllocarid fossils. Deep-marine mass flow deposits.||||||07-FEB-11
74884|Wahroonga Breccia|64606|5|Briefly described|Map Legend|Cambrian|Cambrian|Sandstone, breccia: marine deposits. Light blue, pink and yellow in RGB (low total count). Nonmagnetic to moderately magnetic.||||||
74884|Wahroonga Breccia|64616|3|Fully described|p61, p178, p179, p182-183, p192|Late Cambrian|Middle Cambrian|See also p197 Fig.6.34, p203-204, p255, p281, p306. New name. Appears to overlie Licola Volcanic Group; contact not exposed. Overlain gradationally by Wild Dog Chert. Overlain ?disconformably by Mount Easton Shale. In faulted contact with Walhalla Group rocks. The type locality also contains phosphatic volcano-sedimentary breccia containing apatite and turquoise. Age inferred. At least 200 m thick. A range of contact metamorphosed mineral assemblages is developed due to Strathbogie Granite. Geophysical characteristics given.||||||
74884|Wahroonga Breccia|67104|6|Mentioned|p635|||Correlates with the Bear Gully Gritstone in Victoria and the Owen Conglomerate in western Tasmania.||||||
74884|Wahroonga Breccia|68116|5|Briefly described|Appendix, Map 25.|Late Cambrian|Middle Cambrian||||||Sandstone, breccia: green-grey; massive to well-bedded; medium to very thick-bedded; phosphatic; abundant lithic clasts; contains brachiopod and phyllocarid fossils.|
74884|Wahroonga Breccia|70601|5|Briefly described|p44|Idamean|Mindyallan|Licola area.||||Underlies Wild Dog Chert. Overlies Jamieson Volcanics.||
30516|Wakefield Granite|22878|4|Described|p86|||||||||
30516|Wakefield Granite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Biotite granite: pink, coarse grained, massive; slightly porphyritic in K-feldspar; numerous microgranite and mafic dykes.||||||01-OCT-04
30516|Wakefield Granite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Biotite granite: pink, coarse grained, massive; slightly porphyritic in K-feldspar; numerous microgranite and mafic dykes.||||||01-OCT-04
30516|Wakefield Granite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Biotite granite: Highly magnetic (400-420 nT), subsurface (180-200 nT). High K, low Th and U||||||06-OCT-04
30516|Wakefield Granite|23309|6|Mentioned|p446 App1|||G520 - I-Type.||||||
30516|Wakefield Granite|68116|5|Briefly described|Appendix, Map 37.|Early Devonian|Early Devonian||||||Biotite granite: pink, coarse grained, massive; slightly porphyritic in K-feldspar; numerous microgranite and mafic dykes.|
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|||
37609|Walkerville Member|23309|5|Briefly described|p149, Table 2.57|Devonian|Devonian|Of Waratah Limestone||||||
37609|Walkerville Member|24551|5|Briefly described|p130|||Of Waratah Limestone||||||
30568|Wallaby Granite|23309|6|Mentioned|p446 App1|||G107 S-Type.||||||
30568|Wallaby Granite|24551|5|Briefly described|p149|||||||||
30568|Wallaby Granite|60503|3|Fully described|p146, p45 Tb. 2|Silurian|Silurian|Name used interchangeably with Wallaby Creek Granite and Wallaby granite. Unconformably overlain by Larsen Creek Ignimbrite. Also forms dykes (p174). See also Wallaby Creek Granite and Wallaby granite. See also p121.||||||16-NOV-09
30568|Wallaby Granite|60504|5|Briefly described|Map Legend|Wenlock|Wenlock|Biotite granite, S-type, mostly weathered granite with some small corestones of grey to dark grey fresh granite||||||
30568|Wallaby Granite|60505|5|Briefly described|Map legend|Wenlock|Wenlock|Biotite granite, S-type, mostly weathered granite with some small corestones of grey to dark grey fresh granite||||||
30568|Wallaby Granite|60506|5|Briefly described|Map legend|Wenlock|Wenlock|Biotite granite, S-type, mostly weathered granite with some small corestones of grey to dark grey fresh granite||||||
30568|Wallaby Granite|60507|5|Briefly described|Map Legend|Wenlock|Wenlock|Biotite granite, S-type, mostly weathered granite with some small corestones of grey to dark grey fresh granite||||||
30568|Wallaby Granite|60508|5|Briefly described|Map legend|Early Silurian|Early Silurian|Biotite granite: S-type; nonmagnetic (0-5 nT) with moderately magnetic (25 nT) dykes in southwest; radiometric response often masked by Lake Dartmouth, low total count, K, Th, moderate U in the west, high K, U, low total count, Th in the east.||||||
30568|Wallaby Granite|61160|5|Briefly described|p60, p32 Tb. 5.2|Silurian|Silurian|S-type biotite granite. Intruded by the Banimboola Quartz Monzodiorite. ||||||
30568|Wallaby Granite|65396|6|Mentioned|p85, p366 table 1||||||||Two-mica granite.|
30568|Wallaby Granite|68116|5|Briefly described|Appendix, Map 27.|Wenlock|Llandovery||||||Biotite granite: leucocratic; medium-grained; with muscovite, tourmaline and minor garnet; mostly weathered with some small corestones of fresh granite.|
19255|Wallace Basalt|30370|6|Mentioned|p25|||||||||
25586|Wallagaraugh Suite|22815|5|Briefly described|p70|||||||||
25586|Wallagaraugh Suite|22878|6|Mentioned|p83|||||||||
25586|Wallagaraugh Suite|24551|6|Mentioned|p235|||||||||
25586|Wallagaraugh Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
25586|Wallagaraugh Suite|42827|5|Briefly described|p430|||||||||
25586|Wallagaraugh Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Bega Batholith.||||||
25586|Wallagaraugh Suite|69801|6|Mentioned|p3, p129, p138|Devonian|Devonian|Eastern Lachlan Orogen.||Kameruka Supersuite|Includes the Mount Poole Monzogranite.|||
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|||||||||
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.|
29549|Wando Tonalite|23309|5|Briefly described|p335|||G421 I-Type. Supersedes Wando River Tonalite and Meissen Granodiorite.||||||
29549|Wando Tonalite|24012|3|Fully described|p222 appendix 1|Ordovician|Cambrian|Previously referred to as "Wando Granodiorite gneiss", "Wando Granodiorite" and "Wando Tonalite gneiss".||||||
29549|Wando Tonalite|24551|5|Briefly described|p76|||||||||
29549|Wando Tonalite|42971|5|Briefly described|p144, Fig.2 p143|||Variation on Wando Tonalite Gneiss||||||
29549|Wando Tonalite|50154|2|Defined|p75, p76, p248 App.5|Cambrian|Cambrian|Of the Glenelg river Metamorphic Complex. Corresponds to part of Wells' (1956) Wando Granodiorite gneiss. Age: 493 +/- 8 Ma (U/Pb; Ireland et al., 2002). Geological Province: Delamerian Fold Belt.||||||15-SEP-04
29549|Wando Tonalite|50156|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-hornblende tonalite||||||20-AUG-04
29549|Wando Tonalite|50157|5|Briefly described|Map Legend|Late Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-hornblende tonalite||||||20-AUG-04
29549|Wando Tonalite|50158|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-hornblende tonalite||||||20-AUG-04
29549|Wando Tonalite|50159|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-hornblende tonalite||||||20-AUG-04
29549|Wando Tonalite|50160|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-hornblende tonalite||||||20-AUG-04
29549|Wando Tonalite|50161|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-hornblende tonalite||||||20-AUG-04
29549|Wando Tonalite|50162|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-hornblende tonalite||||||20-AUG-04
29549|Wando Tonalite|50163|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Glenelg River Metamorphic Complex. Biotite-hornblende tonalite||||||20-AUG-04
29549|Wando Tonalite|50164|5|Briefly described|Map Legend|Cambrian|Cambrian|Biotite-hornblende tonalite: I-type. Age: 493+/-8 Ma (U-Pb)||||||16-JUN-04
29549|Wando Tonalite|66002|5|Briefly described|p8 Tb.5|||G421. Called Wando Granodiorite by Wells (1956). Redefined in Kemp et al.2002, Morand et al. 2003.||||||27-MAY-13
29549|Wando Tonalite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Biotite-hornblende tonalite: foliated, grey, fine to medium grained, equigranular; accessory magnetite, epidote, sphene and allanite; enclaves are hornblende-biotite microgranitoid types; magnetic.|
29549|Wando Tonalite|72313|6|Mentioned|p459 Table 2|||Delamerian Orogen. I-type. Hf and O18 isotope data included.|515 Ma|||||
29549|Wando Tonalite|73430|6|Mentioned|p517-518|Cambrian|Cambrian|Glenelg Terrane.|493+/-8 Ma|||||
19390|Wangarabell Granodiorite|22878|6|Mentioned|p83|||||||||
19390|Wangarabell Granodiorite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Of the Cobargo Supersuite. Hornblende-biotite granodiorite: grey, medium grained, massive to foliated with thin mylonite zones; slightly porphyritic in abundant plagioclase.||||||01-OCT-04
19390|Wangarabell Granodiorite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Cobargo Supersuite. Hornblende-biotite granodiorite: grey, medium grained, massive to foliated with thin mylonite zones; slightly porphyritic in abundant plagioclase.||||||01-OCT-04
19390|Wangarabell Granodiorite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Cobargo Supersuite. Hornblende-biotite granite: Strongly magnetic (320-350 nT). High K, low Th and U.||||||06-OCT-04
19390|Wangarabell Granodiorite|23309|5|Briefly described|p346||Early Devonian|G6 - I-Type. Supersedes Wangarabell Granite.||||||
19390|Wangarabell Granodiorite|24551|6|Mentioned|p236, 730 Table 8.13|||||||||
19390|Wangarabell Granodiorite|41850|6|Mentioned|p430|||||||||
19390|Wangarabell Granodiorite|42827|5|Briefly described|p430|||of Cobargo Supersuite||||||
19390|Wangarabell Granodiorite|68116|5|Briefly described|Appendix, Maps 37, 46.|Early Devonian|Early Devonian||||||Hornblende-biotite granodiorite: grey, medium grained, massive to foliated with thin mylonite zones; slightly porphyritic in abundant plagioclase; accessory sphene and magnetite; I-type.|
31571|Wangarabell Suite|22878|6|Mentioned|p83|||||||||
31571|Wangarabell Suite|24551|6|Mentioned|p236|||||||||
31571|Wangarabell Suite|42726|5|Briefly described|map legend||Silurian|||||||
31571|Wangarabell Suite|44093|5|Briefly described|p182 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
19406|Wangerrip Group|12796|6|Mentioned|p461|||Includes Massacre Shale.  Geological Province: Otway Basin||||||
19406|Wangerrip Group|22587|6|Mentioned|p79 Fig.7|Early Eocene|Late Paleocene|||||||
19406|Wangerrip Group|22674|5|Briefly described|p718, Fig.2 p719|Early Eocene|Maastrichtian|See also Fig.8 p725.||||||10-OCT-07
19406|Wangerrip Group|22875|4|Described|p13|Middle Eocene|Paleocene|In the Otway Basin.||||||10-OCT-07
19406|Wangerrip Group|22944|5|Briefly described|Fig3|Eocene|Paleocene|||||||
19406|Wangerrip Group|23230|4|Described|Table4-1p40, 41-3|Eocene|Paleocene|||||||
19406|Wangerrip Group|23307|5|Briefly described|Map Legend|Paleocene|Paleocene|||||||
19406|Wangerrip Group|23322|5|Briefly described|957 Fig.2|Eocene|Paleocene|Geological Province: Gambier Basin (SA) and Otway Basin (VIC).||||||07-SEP-09
19406|Wangerrip Group|23402|5|Briefly described|p31|Tertiary|Tertiary|Geological Province: Otway Basin.||||||21-OCT-08
19406|Wangerrip Group|23778|5|Briefly described|p660|||Geological Province: Otway Basin.||||||
19406|Wangerrip Group|23792|5|Briefly described|p26|Middle Eocene|Maastrichtian|Transgressive/regressive clastic cysles. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|23939|6|Mentioned|Fig.5|||May be Paleocene to Early Eocene in age.||||||
19406|Wangerrip Group|24056|4|Described|p85|Paleocene|Paleocene|Geological Basin: Otway Basin.||||||
19406|Wangerrip Group|24200|5|Briefly described|p421, 422||Early Eocene|See also p423 Figs. 15 & 16, p428 Fig. 18.  Wangerrip Group Equivalents discussed throughout text.||||||
19406|Wangerrip Group|24202|5|Briefly described|p313 Fig. 2|Eocene|Paleocene|Geological Province: Gambier Sub-basin.  See also p312.||||||
19406|Wangerrip Group|24314|5|Briefly described|p61 Fig.2|Middle Eocene|Paleocene|Geological Province: Otway Basin. Max. Thickness 90m.||||||30-NOV-04
19406|Wangerrip Group|24323|5|Briefly described|p136 Fig. 3|Eocene|Paleocene|Overlies the Sherbrook Group. Overlain by the Nirranda Group. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|24344|5|Briefly described|p69, 79|Paleocene|Paleocene|||||||
19406|Wangerrip Group|24470|6|Mentioned|p473|||||||||
19406|Wangerrip Group|24551|5|Briefly described|p246, 292 Fig. 10.3|Eocene|Late Cretaceous|Consists of: Pebble Point Formation, Pember Mudstone, Dilwyn Formation.||||||
19406|Wangerrip Group|24562|5|Briefly described|p7, 8, 35|Eocene|Paleocene|Overlies: Sherbrook Group (u). Geological Province: Otway Basin.||||||
19406|Wangerrip Group|29355|6|Mentioned|p179|||||||||
19406|Wangerrip Group|29823|5|Briefly described|p14|||||||||
19406|Wangerrip Group|29856|6|Mentioned|p40|||||||||
19406|Wangerrip Group|29889|6|Mentioned|p139|||||||||
19406|Wangerrip Group|30499|6|Mentioned|p92|||Stratigraphy||||||
19406|Wangerrip Group|30522|6|Mentioned|Map legend|Eocene|Paleocene|Eocene-Palaeocene||||||
19406|Wangerrip Group|30576|6|Mentioned|p23|||||||||
19406|Wangerrip Group|30578|4|Described|p8|||||||||
19406|Wangerrip Group|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19406|Wangerrip Group|30905|6|Mentioned|Table 7.4|||||||||
19406|Wangerrip Group|30928|6|Mentioned|Map legend|Paleocene|Paleocene|||||||
19406|Wangerrip Group|30932|6|Mentioned|Map legend|late Eocene|Paleocene|Equivalent Knight Group.U.Cret.? to Eocene?||||||
19406|Wangerrip Group|31036|1|Redefined|p195|early Tertiary|Late Cretaceous|See also p196-199, 215, Table 9-1. Late Cretaceous to Early Tertiary.||||||10-OCT-07
19406|Wangerrip Group|31245|5|Briefly described|p81|||Palaeocene. Formations listed.||||||10-OCT-07
19406|Wangerrip Group|31372|6|Mentioned|p9|||||||||
19406|Wangerrip Group|31424|6|Mentioned|Table 2|||Lithostratigraphy||||||
19406|Wangerrip Group|31534|6|Mentioned|p363|||See also Table 19-3||||||
19406|Wangerrip Group|31583|6|Mentioned|p18|||Section||||||
19406|Wangerrip Group|31624|6|Mentioned|p106|||U.Palaeocene flora||||||
19406|Wangerrip Group|31625|6|Mentioned|Fig. 5.2|||Palaeocene||||||
19406|Wangerrip Group|31920|5|Briefly described|p53|||See also p60. Palaeocene. Partly equivalent to Knight Group.||||||12-SEP-18
19406|Wangerrip Group|31922|6|Mentioned|p177|||||||||
19406|Wangerrip Group|32115|6|Mentioned|p1|||||||||
19406|Wangerrip Group|32117|6|Mentioned|Fig.2|||||||||
19406|Wangerrip Group|32162|6|Mentioned|p58|||See also Fig.5||||||
19406|Wangerrip Group|32898|6|Mentioned|Table 2-1|||||||||
19406|Wangerrip Group|33135|5|Briefly described|p17|||||||||
19406|Wangerrip Group|33949|6|Mentioned|p274|||||||||
19406|Wangerrip Group|34063|6|Mentioned|p2|||Paleocene. Table||||||
19406|Wangerrip Group|34164|6|Mentioned|p33|||Table.||||||
19406|Wangerrip Group|34343|5|Briefly described|p102|||||||||
19406|Wangerrip Group|34987|5|Briefly described|p170|||||||||
19406|Wangerrip Group|35013|6|Mentioned|p393|||||||||
19406|Wangerrip Group|35066|3|Fully described|p201|||||||||
19406|Wangerrip Group|35147|6|Mentioned|p127|||||||||
19406|Wangerrip Group|35285|5|Briefly described|p414|||||||||
19406|Wangerrip Group|36366|6|Mentioned|p1|||||||||
19406|Wangerrip Group|36913|6|Mentioned|Fig.4|||||||||
19406|Wangerrip Group|37548|6|Mentioned|p129|||||||||
19406|Wangerrip Group|38070|6|Mentioned|Fig.12|||Otway Basin||||||
19406|Wangerrip Group|38221|6|Mentioned|Fig.4|||Otway Basin||||||
19406|Wangerrip Group|38625|6|Mentioned|p271|||||||||
19406|Wangerrip Group|39315|6|Mentioned|Fig.7|||||||||
19406|Wangerrip Group|40003|5|Briefly described|p44|||See also Table 10.||||||10-OCT-07
19406|Wangerrip Group|40230|6|Mentioned|Fig.7|||||||||
19406|Wangerrip Group|40560|6|Mentioned|p4|||||||||
19406|Wangerrip Group|41016|5|Briefly described|Mention|||||||||
19406|Wangerrip Group|41185|5|Briefly described|p175|||||||||
19406|Wangerrip Group|41269|5|Briefly described|p246|||||||||
19406|Wangerrip Group|41487|5|Briefly described|p625|||||||||
19406|Wangerrip Group|41642|4|Described|p243|||See also Table 7.4||||||
19406|Wangerrip Group|41701|6|Mentioned|Map legend|early Eocene||||||||
19406|Wangerrip Group|41704|6|Mentioned|p100|||||||||
19406|Wangerrip Group|41714|6|Mentioned|p301|||||||||
19406|Wangerrip Group|41726|5|Briefly described|p421|||||||||
19406|Wangerrip Group|41769|4|Described|p18|||||||||
19406|Wangerrip Group|41868|5|Briefly described|p534|||||||||
19406|Wangerrip Group|42075|5|Briefly described|Fig.13 P252|||||||||
19406|Wangerrip Group|42318|6|Mentioned|p7|||||||||
19406|Wangerrip Group|42361|5|Briefly described|p18|||||||||
19406|Wangerrip Group|42453|6|Mentioned|p11|||||||||
19406|Wangerrip Group|42524|5|Briefly described|Fig.3 p27|||||||||12-SEP-18
19406|Wangerrip Group|42555|5|Briefly described|p285|||||||||
19406|Wangerrip Group|42599|5|Briefly described|Fig.3 P614|||||||||
19406|Wangerrip Group|42827|3|Fully described|p275|||see also Fig 8.10||||||
19406|Wangerrip Group|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
19406|Wangerrip Group|43171|5|Briefly described|2-8|Middle Eocene|Paleogene|Within the Otway Supergroup.||||||07-NOV-08
19406|Wangerrip Group|43195|5|Briefly described|Map Legend|Eocene|Paleocene|See also commentary on back of map.||||||
19406|Wangerrip Group|43208|5|Briefly described|map legend||Maastrichtian|Of Maastrichian-Late Palaeocene age.||||||
19406|Wangerrip Group|43219|5|Briefly described|Fig.3,p6.|Eocene|Maastrichtian|||||||
19406|Wangerrip Group|43590|4|Described|p15|Tertiary|Late Cretaceous|||||||
19406|Wangerrip Group|43604|6|Mentioned|p144,Fig.1|Eocene|Paleocene|||||||
19406|Wangerrip Group|43660|6|Mentioned|Fig.6,p15||Tertiary|||||||
19406|Wangerrip Group|43733|6|Mentioned|Fig.2.11,p65||Tertiary|||||||
19406|Wangerrip Group|43744|6|Mentioned|Fig.3,p3|||||||||
19406|Wangerrip Group|43783|6|Mentioned|Fig14, p11|Middle Eocene|Paleocene|||||||
19406|Wangerrip Group|43784|6|Mentioned|Fig10, p12|Middle Eocene|Paleocene|||||||
19406|Wangerrip Group|43937|5|Briefly described|Map Legend|Paleocene|Santonian|||||||
19406|Wangerrip Group|44133|5|Briefly described|p154|Middle Eocene|Late Paleocene|Includes: Pebble Point Formation, Pember Mudstone, Dilwyn Formation. Geological Province: Gambier Basin.||||||
19406|Wangerrip Group|44135|6|Mentioned|p49|Early Eocene|Late Cretaceous|Mentioned in the context of correlates.||||||07-DEC-09
19406|Wangerrip Group|45159|6|Mentioned|p15|||||||||
19406|Wangerrip Group|45168|6|Mentioned|p6|||||||||
19406|Wangerrip Group|46802|6|Mentioned|Table 1|||||||||
19406|Wangerrip Group|48581|4|Described|p31|||See also p12,28,29,33,37,40, Fig.4,Pl.1,2. (J54-12/Port Cambell).||||||
19406|Wangerrip Group|48911|4|Described|p23|||Palaeocene - Middle Eocene.||||||21-OCT-08
19406|Wangerrip Group|48977|6|Mentioned|p2|||See also Table 3 & Fig.5||||||
19406|Wangerrip Group|49060|5|Briefly described|Fig.33 P53|||||||||
19406|Wangerrip Group|60421|5|Briefly described|p408 Fig. 1, 409|Eocene|Paleocene|Includes: Eastern View Formation.||||||07-NOV-08
19406|Wangerrip Group|60451|5|Briefly described|p95 Fig. 61|||||||||
19406|Wangerrip Group|60452|5|Briefly described|p14|Cenozoic|Cenozoic|Geological Province: Otway Basin.||||||19-NOV-08
19406|Wangerrip Group|60538|5|Briefly described|p470 Fig. 10, 473 Fig. 12|Early Eocene|Late Cretaceous|Mudstones, litoral deposits, sands and shales.||||||
19406|Wangerrip Group|60563|5|Briefly described|p45|Eocene|Paleocene|Overlain by the Nirranda Group. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|60599|5|Briefly described|p84|Late Cretaceous|Late Cretaceous|Includes the Eastern View, Pebble Point and Wiridgil formations. Geological Province: Otway  Basin.||||||02-FEB-09
19406|Wangerrip Group|61017|5|Briefly described|p5 Fig. 2|Lutetian|Danian|Geological Province: Otway Basin.||||||07-FEB-11
19406|Wangerrip Group|61180|5|Briefly described|p33|Tertiary|Tertiary|Contains phosphate deposits.  Age is Early Tertiary. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|61182|3|Fully described|p19, p35|Early Eocene|Paleocene|Incl: Pebble Point and Dilwyn Fms; some include Sherbrook Gp rocks. Moomowroong Sand and Wiridjil Gravel have been added as they grade into Pebble Point Fm and each other. Unconformable on Sherbrook Gp. Overlain by Nirranda Gp. Otway Basin. Age: 65-45Ma.||||||06-JAN-10
19406|Wangerrip Group|61185|5|Briefly described|p57|Tertiary|Tertiary|Includes Pebble Point Formation, Wiridgil Formation and Eastern View Formation (Edwards et al. 1996). Equivalent to White Hills Gravel and Warina Sand. Age: ~65Ma. Geol. Prov: Otway Basin.||||||07-FEB-11
19406|Wangerrip Group|61470|5|Briefly described|p28 Fig. 5|Lutetian|Danian|Includes Pebble Point formation, Pember Mudstone and Dilwyn Formation. Geological Province: Otway Basin.||||||12-OCT-05
19406|Wangerrip Group|61528|6|Mentioned|p827|||||||||
19406|Wangerrip Group|61547|5|Briefly described|p461 Fig.2, p462. |Eocene|Paleocene||||Includes basal Pebble Point Formation, Pember Mudstone and Dilwyn Formation.|Unconformably overlies Sherbrook Group. Is overlain by Nirranda Group.||05-FEB-15
19406|Wangerrip Group|61607|6|Mentioned|p5 Fig. 2|Eocene|Paleocene|Geological Province: Otway Basin.||||||12-MAR-09
19406|Wangerrip Group|61608|6|Mentioned|p41 Fig. 5|||Refers to equivalent unit.||||||
19406|Wangerrip Group|61622|4|Described|p436, p437, p436 Fig. 2|Early Tertiary|Late Cretaceous|Includes Pebble Point Fm, Pember Mudst and Dilwyn Fm. Thickness: 200m. Geological Province: Otway Basin. Thin oolitic deposits and a range of mudstones and sandstones.||||||07-FEB-11
19406|Wangerrip Group|61623|5|Briefly described|p447, p449 Fig. 4|Tertiary|Tertiary|Includes Pebble Point Formation, Pember Mudstone and Dilwyn Formation. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|61624|6|Mentioned|p465|Tertiary|Tertiary|Geological Province: Otway Basin.||||||07-APR-09
19406|Wangerrip Group|61626|5|Briefly described|p486, p487, p486 Fig. 2, p488, p493|Eocene|Paleocene|Includes; Pebble Point and Dilwyn Fomations and Pember Mudstone. Geological Province: Otway Basin.||||||07-APR-09
19406|Wangerrip Group|61627|5|Briefly described|p500 Fig. 2|Eocene|Paleocene|Includes Dilwyn and Pebble Point Formations, Pember Mudstone. Geological Province: Otway Basin.||||||07-FEB-11
19406|Wangerrip Group|61628|5|Briefly described|p509 Fig. 3|Middle Eocene|Late Cretaceous|Includes; Pebble Point and Dilwyn Formations, Pember Mudstone. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|61841|5|Briefly described|p242|Eocene|Paleocene|Shallow marine to continental deposits.   Geological Province: Otway Basin.||||||03-JUL-06
19406|Wangerrip Group|62370|6|Mentioned|p455, p461|||Siliclastic sediments. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|62896|5|Briefly described|p87|||Geological Province: Otway Basin.||||||07-FEB-11
19406|Wangerrip Group|63122|5|Briefly described|p17 Fig. 4.3, p21|Eocene|Early Paleocene|Includes Pebble Point Formation, Pember Mudstone and Dilwyn Formation. Geological Province: Otway Basin. ||||||
19406|Wangerrip Group|63124|5|Briefly described|p49 Fig. 5.2, p87 Fig. 5.29, p84|Middle Eocene|Early Paleocene|Includes Pebble Point and Dilwyn Formations, and Pember Mudstone. Geological Province: Otway Basin.||||||
19406|Wangerrip Group|63125|6|Mentioned|p115|||Geological Province: Otway Basin||||||
19406|Wangerrip Group|63173|5|Briefly described|p342 Fig. 9.2|Middle Eocene|Early Paleocene|Geological Province: Otway Basin, offshore.||||||07-FEB-11
19406|Wangerrip Group|63269|5|Briefly described|p604-605|Eocene|Late Cretaceous|Otway Basin.|||Eastern View, Pebble Point, Dilwyn Formations; Pember Mudstone.|Unconformably overlies Sherbrook Group. Is overlain unconformably by Nirranda Group.||
19406|Wangerrip Group|63431|5|Briefly described|p677 Fig. 2|Eocene|Paleocene|Includes the Pebble point Formation, Pember Mudstone and Dilwyn Formation. Overlies the Sherbrook Group; Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
19406|Wangerrip Group|63446|5|Briefly described|Map legend|Paleocene|Paleocene||||||Marine, fluvial: sandstone, minor conglomerate.|
19406|Wangerrip Group|63740|5|Briefly described|p88|Early Eocene|Late Paleocene|Includes Dilwyn Formation. Geological province: Otway Basin.||||||07-FEB-11
19406|Wangerrip Group|64314|5|Briefly described|p504|Early Eocene|Paleocene|Unconformably overlies Sherbrook Group.||||||21-OCT-08
19406|Wangerrip Group|65715|5|Briefly described|p11 Tb.7|Paleogene|Paleogene|Includes Dilwyn Formation, Moomowroong Sand and Wiridjil Gravel.||||||
19406|Wangerrip Group|66002|4|Described|p3, p10 Tb.7, p10 Tb.8, p11|Paleogene|Paleogene|Includes Dilwyn Formation, Moomowroong Sand, Wiridjil Gravel and Pebble Point Formation. Outcrops extensively in the Port Campbell Embayment. Overlies Eumeralla Formation. Newly subdivided in this paper||||||
19406|Wangerrip Group|66012|5|Briefly described|p17|||In Otway Basin. Carbonaceous-rich. Correlated with Dilwyn Formation? or includes Dilwyn Formation.| | | | | |16-FEB-15
19406|Wangerrip Group|66181|6|Mentioned|p312|Eocene||Gippsland Basin||||||
19406|Wangerrip Group|66245|5|Briefly described|p6 Fig.5, p8, p27 Fig.32. |Lutetian|Maastrichtian|Coastal and shallow marine, progradational sequence of clastic sediments.|||Includes Pebble Point, Dilwyn and ?Eastern View Formations and Pember Mudstone.|||
19406|Wangerrip Group|67061|6|Mentioned|p545, p546 Fig.3.|Eocene|Paleocene|Equivalent to upper parts of Eastern View Group (Torquay Sub-basin).|||Includes Pebble Point Formation, Pember Mudstone and Dilwyn Formation.|||
19406|Wangerrip Group|67366|5|Briefly described|p103 Fig.2. |Eocene|Paleocene||||Includes basal Massacre Shale; Pebble Point Formation; Pember Mudstone, and Dilwyn Formation at the top.|Unconformably overlies Sherbrook Group. Is unconformably overlain by Nirranda Group.||05-FEB-15
19406|Wangerrip Group|67367|5|Briefly described|p130, p131 Fig.2. |Lutetian|Maastrichtian|Siliciclastics. Stratigraphic equivalent to Latrobe Group, offshore Gippsland Basin.|||Includes Massacre Shale, Pebble Point and Dilwyn Formations, and Pember Mudstone.|||
19406|Wangerrip Group|68116|5|Briefly described|Appendix, Map 38.|Eocene|Paleocene||||||Silty clay, clayey silt, fine quartz sand: carbonaceous, micaceous, pyritic, burrowed, with abundant arenaceous foraminifers, minor calcareous foraminifers and shelly fossils; shallow marine (below and close to storm wave base) deposits.|
19406|Wangerrip Group|69297|6|Mentioned|p78, p79, p98, p112, p115, p116|Lutetian|Maastrichtian|Otway and Sorell Basins. Coastal plain to open marine siliciclastic and carbonate sediments. Potential reservoir in the Sorell Basin. May contain intraformational shale seals. |||Includes the Wiridjil Gravel, Massacre Shale, Pebble Point Formation, Pember Mudstone and the Dilwyn Formation. |Overlies the Sherbrook Group. Unconformably overlain by the Nirranda Group. ||
19406|Wangerrip Group|69651|5|Briefly described|p6, p10, p12, p28, p32-35, p38|Eocene|Paleocene|Otway Basin. Coastal plain, deltaic and inner shelf deposits. Has fault/stratigraphic traps and stratigraphic reservoirs. Very high (30%+) porosity values. Modelling diagrams.|||Eastern View, Pebble Point, Dilwyn Formations; Pember Mudstone.|Unconformably overlies Sherbrook Group. Is overlain unconformably by Nirranda Group.|Includes interbedded sandstones.|
19406|Wangerrip Group|69879|5|Briefly described|p418, p424|Eocene|Maastrichtian|Strahan Sub-basin. Shown as Wangerrip Group equivalent. Offshore exploration well Cape Sorell 1.||||Overlies Sherbrook Group. Underlies Nirranda Group.|Alternating beds of silty claystone/clayey siltstone (with organic content and terrestrial input) with clastics, and quartzitic sandstone. Shallow marine quartz sandstone, siltstone and mudstone.|
19406|Wangerrip Group|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4; p5, p7|Eocene|Maastrichtian|Otway Basin: Gambier Embayment and Voluta Trough. May be petroleum sources of the Austral 3 Petroleum System.|||Massacre Shale; Pebble Point and Dilwyn Formations; Pember Mudstone; Wiridjil Gravel.|Overlies Sherbrook Group. Is overlain by Nirranda Group.||
19406|Wangerrip Group|70078|5|Briefly described|Northern:Fig.2; p2. Regional:Fig.4; p5-6|Eocene|Late Cretaceous|Otway Basin. Sandstones equivalent to this unit in the Sorell Basin are potential hydrocarbon sources; sealed by Heytesbury Group marls and fine-grained carbonates.|||Massacre Shale; Pebble Point and Dilwyn Formations; Pember Mudstone.|Overlies Sherbrook Group. Is overlain by Nirranda Group.||
19406|Wangerrip Group|70379|5|Briefly described|p723-727, p732|Eocene|Eocene|Otway Basin.||||Overlies Sherbrook Group or (locally) Eumeralla Formation. Is overlain by Nirranda Group.||
19406|Wangerrip Group|71419|6|Mentioned|p16 Fig 17|Eocene|Paleocene|Fluvial sediments.||||||
19406|Wangerrip Group|71437|4|Described|Fig. 1 opp p154, p153, p159|Eocene|Albian|Here redefined to embrace Upper Cretaceous as well as lower Tertiary sediments (Cycles 1 and 2).|||Includes Waarre Sandstone, Flaxman Formation, Paaratte Formation, Pebble Point Formation, Dilwyn Formation.|Overlain by Nirranda Group.|Sands, shales, siltstones, and mudstones with minor dolomites, siderite-ankerite, coal, gravels, and greensands.|
19406|Wangerrip Group|71593|5|Briefly described|p51|Eocene|Cretaceous|||||||
19406|Wangerrip Group|73356|6|Mentioned|p3, p15-16|||Transgressive siliciclastics. Reaches a maximum thickness of more than 1200 m in the Portland Trough.||||||
19406|Wangerrip Group|73357|6|Mentioned|p44, p46, p48|Bartonian|Danian|Otway Basin.|||Includes K/Pg Boundary Shale, Pebble Point Formation, Pember Mudstone, Dilwyn Formation.|Underlies Nirranda Group.||
19406|Wangerrip Group|73383|4|Described|p3, p7 Tb.3.1, p10, p21, p27|Eocene|Maastrichtian|Otway Basin. Paleocene to mid Eocene. Equivalent to chemostratigraphic Sequence S5 which has generally lower Ti/Th values than other sequences in Otway Basin. Includes high Fe and P intervals, likely related to berthierine 'greensands'.|||Pebble Point Formation, Pember Mudstone, Dilwyn Formation|Overlies Sherbrook Group, underlies Nirranda Group|Clastic units including sandstones and mudstones.|
19406|Wangerrip Group|73385|5|Briefly described|p3-5, p23-24|Eocene|Maastrichtian|Otway Basin. Maximum thickness of more than 1200 m in the Portland Trough, thins across the Bridgewater High. Deposited in basin margin subsidence event.|||Pebble Point Formation, Pember Mudstone, Dilwyn Formation|Overlies Sherbrook Group, unconformably underlies Nirranda Group.|Transgressive siliciclastic group.|
19406|Wangerrip Group|73386|4|Described|p1-2, p4-7, p10, p12-13, Attachment A1|Eocene|Maastrichtian|Otway Basin. Represents transition from active rifting to post-rifting subsidence. Progradational, overlies a regional intra-Maastrichtian unconformity and onlaps the top of the Otway Group, underlies intra-Lutetian unconformity. Thickest offshore, maximum thickness of over 1200 m in the Portland Trough, thins to the northeast. Latest Cretaceous to mid Eocene age, Upper Forcipites longus to Lower Nothofagidites asperus spore-pollen zones, chemostratigraphic sequence S5 of Forbes et al. (2020). Location in text includes iii.|||Dilwyn Formation, Pember Mudstone, Pebble Point Formation, Cretaceous/Paleogene boundary shale|Unconformably overlies Sherbrook Group, unconformably underlies Nirranda Group|Siliciclastic sandstones, mudstones, siltstone and shale.|
19406|Wangerrip Group|73594|5|Briefly described|p4-5|Eocene|Paleocene|Otway Basin. Characterised by a series of propagating delta systems, maximum thickness of 2200m in the Portland Trough.|||Pebble Point Formation, Pember Mudstone, Dilwyn Formation|Overlies Sherbrook Group, underlies Nirranda Group||
73298|Wangerrip Supersequence|63134|2|Defined|110-111|||||||||
73298|Wangerrip Supersequence|63269|5|Briefly described|p605|Eocene|Late Cretaceous|Otway Basin.||||Overlies Sherbrook Supersequence. Is overlain by Nirranda Supersequence.||
73298|Wangerrip Supersequence|69297|6|Mentioned|p79, p80, p110, p115|||||||||
73298|Wangerrip Supersequence|69651|5|Briefly described|p6,p10, p12-15, p17-23, p28, p33, p39-40|Eocene|Late Cretaceous|See also p42-47, p49-50. Maastrichtian to early Eocene age. Forms the base of the Australia-Antarctica post-breakup succession. Shallow-marine, marginal marine and deltaic deposits. Generally less than 500m thick; locally up to 1,534m. Modelling diagrams.||||Overlies Sherbrook Supersequence. Is overlain by Nirranda Supersequence.|Sandstone and siltstone.|17-JUN-20
73298|Wangerrip Supersequence|70077|6|Mentioned|Regional: p4-5|Cenozoic|Cenozoic|Otway Basin.||||||
73298|Wangerrip Supersequence|70078|5|Briefly described|Regional: Fig.4; p3-4|Eocene|Paleocene|Sandstones of this unit are likely reservoirs in the Sorell Basin.||||Overlies Sherbrook Supersequence. Is overlain by Nirranda Supersequence.||
73298|Wangerrip Supersequence|70880|6|Mentioned|p77|Eocene|Paleocene|Otway Basin. Post-rift sedimentation; coastal plain, deltaic and inner-shelf settings.||||Overlies Sherbrook Supersequence. Is overlain by Nirranda Supersequence.||
73298|Wangerrip Supersequence|71266|5|Briefly described|p614 Fig.3, p615|Eocene|Paleocene|Otway Basin. Latest Maastrichtian to midddle Eocene.||||Overlies Sherbrook Supersequence. Is overlain by Nirranda Supersequence.||
35834|Wangoom Sand|23322|5|Briefly described|957 Fig.2|Early Oligocene|Early Oligocene|Of the Nirranda Group.  Geological Province: Otway Basin.||||||07-SEP-09
35834|Wangoom Sand|24551|5|Briefly described|p292 Fig. 10.3|||||||||
35834|Wangoom Sand|65891|5|Briefly described|p221 Fig.5. |Paleogene|Paleogene|Otway Basin. Rupelian age. Underlies Narrawaturk Formation.||||||
35834|Wangoom Sand|69297|5|Briefly described|p79, p98|Rupelian|Rupelian|Otway Basin. ||Nirranda Group||Overlies the Narrawaturk Marl, Lower. Overlain by the Narrawaturk Marl, Upper. |Sandstone. |
35834|Wangoom Sand|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Oligocene|Oligocene|Otway Basin: Port Campbell Embayment.||Nirranda Group.||Is interbedded with Narrawaturk Marl.||
19417|Wannaeue Formation|23537|5|Briefly described|p 453|||||||||
19417|Wannaeue Formation|23909|5|Briefly described|p294|Pliocene|Pliocene|||||||
19417|Wannaeue Formation|24038|5|Briefly described|p439 Fig.2|Pliocene|Pliocene|Geological Province: Torquay Basin||||||
19417|Wannaeue Formation|24551|6|Mentioned|p310 Fig. 10.18|||||||||
19417|Wannaeue Formation|35290|6|Mentioned|p45|||||||||
19417|Wannaeue Formation|35712|4|Described|p24|||||||||
19417|Wannaeue Formation|41511|5|Briefly described|p18|||||||||
19417|Wannaeue Formation|41521|3|Fully described|p239|||||||||
19417|Wannaeue Formation|61155|5|Briefly described|p5||Early Pliocene|See also the misspelt Wannacue Formation. Marine calcarenites and clays in the Melbourne area. Max. thickness: 80m. Overlies the Brighton Group; underlies Bridgewater Formation and partly under Newer Volcanics also. ||||||
19417|Wannaeue Formation|68811|5|Briefly described|p67, p69, p170 tbl 31|Quaternary|Quaternary|||||Overlies the Brighton Group and the Fyansford Formation. |Sandy sediments. |
19417|Wannaeue Formation|69297|6|Mentioned|p98|Pleistocene|Pleistocene|||||Unconformably overlies the Moorabool Viaduct Sand. Unconformably overlain by the Newer Volcanics. ||
30437|Wannon Sandstone Member|23309|5|Briefly described|p78. Table 2.27|||Maximum Thickness: 30m.||||||
30437|Wannon Sandstone Member|44929|5|Briefly described|Map Legend|Silurian|Ordovician|Of Silverband Formation. Pale, fine- to medium-grained quartzo-micaceous sandstone.||||||14-JUN-06
30437|Wannon Sandstone Member|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Silverband Formation (Grampians Group). Sandstone, pale, fine- to medium-grained, quartzo-micaceous.||||||13-JUN-06
30437|Wannon Sandstone Member|44932|5|Briefly described|Map Legend|Silurian|Ordovician|Of Silverband Formation. Pale, fine- to medium-grained quartzo-micaceous sandstone.||||||14-JUN-06
30437|Wannon Sandstone Member|44933|5|Briefly described|Map Legend|Silurian|Ordovician|Pale, fine- to medium-grained quartzo-micaceous sandstone.||||||14-JUN-06
30437|Wannon Sandstone Member|60451|4|Described|p75, 77 Fig. 47, 81, 137|Early Devonian|Ordovician|Of the Silverband Formation (Grampians Group). Type section in text. Maximum Thickness: ~30m.||||||
30437|Wannon Sandstone Member|60456|5|Briefly described|Map Legend|Silurian|Ordovician|Sandstone: pale, fine to medium grained, quartzo-micaceous; planar and cross laminated, thin to thickly bedded; minor thin interbeds of micaceous mudstone.||||||
30437|Wannon Sandstone Member|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Sandstone, pale, fine to medium grained, quartzo-micaceous, planar and cross laminated, thin to thickly bedded.||||||
30437|Wannon Sandstone Member|61183|4|Described|p42-44, p56|||Thin sheet-like band enclosed high within Silverband Formation mudstone. Thickness: ~30m. Name used interchangeably with Wannon Sandstone.||||||
30437|Wannon Sandstone Member|64541|5|Briefly described|Map Legend|Silurian|Ordovician|Sandstone: pale, fine to medium grained, quartzo-micaceous; laminated and croos-laminated, thin to thickly bedded; minor thin interbeds of micaceous mudstone.||||||07-FEB-11
30437|Wannon Sandstone Member|64610|5|Briefly described|Map legend|Silurian|Ordovician|Of Silverband Formation (Grampians Gp). Sandstone: pale, fine- to medium-gr., quartzo-micaceous; laminated and x-laminated; thin to thickly bedded; minor interbeds of micaceous mudstone.||||||11-NOV-08
30437|Wannon Sandstone Member|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Silverband Formation. Defined by Cayley & Taylor, 1997. ||||||
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.|
30544|Waranga Formation|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
30544|Waranga Formation|23309|5|Briefly described|p141, 153. Table 2.51|||||||||
30544|Waranga Formation|24177|3|Fully described|p56, p50 Fig.22|Middle Devonian|Early Devonian|Overlies the Puckapunyal Formation. Maximum Thickness: 750m. Possibly correlates with Wilson Creek Shale and Walhalla Group.||||||
30544|Waranga Formation|24328|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
30544|Waranga Formation|24329|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
30544|Waranga Formation|60529|5|Briefly described|Map Legend|Emsian|Lochkovian|Lower fan turbidite deposits: Claystone; pale grey, extensively burrowed, with interbedded siltstone and turbiditic fine to medium grained sandstone; thinly bedded, commonly burrowed.||||||
30544|Waranga Formation|60591|5|Briefly described|Map Legend|Emsian|Pridoli|Overlies the Puckapunyal Formation. Claystone, pale grey, extensively burrowed: interbedded siltstone and turbiditic fine- to medium-grained sandstone; thinly bedded, commonly burrowed.||||||27-OCT-08
30544|Waranga Formation|60592|5|Briefly described|Map Legend|Emsian|Pridoli|Overlies the Puckapunyal Formation. Claystone, pale grey, extensively burrowed: interbedded siltstone and turbiditic fine- to medium-grained sandstone; thinly bedded, commonly burrowed.||||||27-OCT-08
30544|Waranga Formation|60593|5|Briefly described|Map Legend|Emsian|Pridoli|Overlies the Puckapunyal Formation. Claystone, pale grey, extensively burrowed: interbedded siltstone and turbiditic fine- to medium-grained sandstone; thinly bedded, commonly burrowed.||||||27-OCT-08
30544|Waranga Formation|60595|5|Briefly described|Map Legend|Emsian|Pridoli|Overlies the Puckapunyal Formation. Claystone, pale grey, extensively burrowed: interbedded siltstone and turbiditic fine- to medium-grained sandstone; thinly bedded, commonly burrowed||||||
30544|Waranga Formation|60596|5|Briefly described|Map Legend|Emsian|Pridoli|Overlies the Puckapunyal Formation. Claystone, pale grey, extensively burrowed: interbedded siltstone and turbiditic fine- to medium-grained sandstone; thinly bedded, commonly burrowed||||||26-NOV-04
30544|Waranga Formation|60597|5|Briefly described|Map Legend|Emsian|Pridoli|Low magnetic responses, with thin, weak magnetic linear features; high K and Th.||||||27-OCT-08
30544|Waranga Formation|60599|3|Fully described|p14, p74, p99|Middle Devonian|Early Devonian|Part of the upward-fining succession of Broadford, Puckapunyal and Waranga Formations. Turbidite sandstone beds interbedded with bioturbated siltstones. Hosts auriferous reefs of the Rushworth goldfield. Overlies Puckapunyal Formation. See also p24 Tb. 4.||||||
30544|Waranga Formation|61185|2|Defined|p33-34, p30, p56, p21 Fig 6.|Middle Devonian|Early Devonian|Under White Hills Gravel (ang. unconformity). Over Puckapunyal Formation (gradational boundary); nature of upper boundary not known. Thick: >500m. Geol.Prov: Lachlan Fold Belt, Melbourne Zone. Turbidite -conglomerates, sandstones, claystones.||||||07-FEB-11
30544|Waranga Formation|61701|5|Briefly described|Map Legend|Emsian|Lochkovian|Lower fan turbidite deposits: Claystone; pale grey, extensively burrowed, with interbedded siltstone and turbiditic fine to medium grained sandstone; thinly bedded, commonly burrowed.||||||
30544|Waranga Formation|61702|5|Briefly described|Map Legend|Emsian|Lochkovian|Lower fan turbidite deposits: Claystone; pale grey, extensively burrowed, with interbedded siltstone and turbiditic fine to medium grained sandstone; thinly bedded, commonly burrowed.||||||
30544|Waranga Formation|61703|5|Briefly described|Map Legend|Emsian|Lochkovian|Lower fan turbidite deposits: Claystone; pale grey, extensively burrowed, with interbedded siltstone and turbiditic fine to medium grained sandstone; thinly bedded, commonly burrowed.||||||
30544|Waranga Formation|61704|6|Mentioned|Map legend|Devonian|Devonian|Variable radiometric response.||||||
30544|Waranga Formation|65969|6|Mentioned|p17 Fig.7|||||||||
30544|Waranga Formation|66769|6|Mentioned|p127 Fig.8d, Fig 13|||Melbourne Zone. Overlies Puckapunyal Formation.||||||
30544|Waranga Formation|68116|5|Briefly described|Appendix, Maps 17-18, 24-25.|Early Devonian|Early Devonian||||||Claystone: pale grey, extensively burrowed; interbedded siltstone and turbiditic fine- to medium-grained sandstone; thinly bedded, commonly burrowed; with parallel, convolute and ripple drift cross laminations; lower-fan turbidite deposits.|
30544|Waranga Formation|69089|5|Briefly described|Map legend|Early Devonian|Early Devonian||||||Marine: siltstone, minor sandstone.|
30544|Waranga Formation|70487|6|Mentioned|p11 Fig.5|Pragian|Emsian|Of VandenBerg et al. (2000). Shown as overlying Puckapunyal Formation, and being overlain by Wilson Creek Shale. Appearing only in the correlation and age range charts (Fig.5).||||Shown below Wilson Creek Shale (VandenBerg et al. 2000).||
30544|Waranga Formation|73497|5|Briefly described|Map legend|Devonian|Devonian|Marine.||Murrindindi Supergroup|||Siltstone, minor sandstone: low magnetic repsonses with thin, weak magnetic linear features of variable length (~1 km); variable radiometric responses.|
31134|Waratah Bay Ultramafics|43489|6|Mentioned|5|||||||||
19434|Waratah Flat Granite|22876|5|Briefly described|p28|||||||||
19434|Waratah Flat Granite|22877|5|Briefly described|map|Silurian|Silurian|G61. Hornblende granite, I-Type.||||||26-OCT-04
19434|Waratah Flat Granite|23309|6|Mentioned|p446 App1|||G61 I-Type.||||||
19434|Waratah Flat Granite|24551|6|Mentioned|p234|||||||||
19434|Waratah Flat Granite|42627|5|Briefly described|Map legend|Wenlock|Wenlock|Reserved as Waratah Flat Adamellite.||||||
19434|Waratah Flat Granite|42647|5|Briefly described|p48|||||||||
19434|Waratah Flat Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
19434|Waratah Flat Granite|68116|5|Briefly described|Appendix, Map 36.|Devonian|Silurian||||||Hornblende granite: coarse grained; green.|
19435|Waratah Limestone|22885|5|Briefly described|map|Early Devonian|Early Devonian|||||||
19435|Waratah Limestone|23229|4|Described|p28, 35||Early Devonian|||||||
19435|Waratah Limestone|23266|5|Briefly described|Fig13-5.1p354|||||||||
19435|Waratah Limestone|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
19435|Waratah Limestone|23309|5|Briefly described|p54, 115, 147-154, 274 Table 2.57||Devonian|||||||
19435|Waratah Limestone|23522|5|Briefly described|p247 Fig 3|Early Devonian|Early Devonian|||||||
19435|Waratah Limestone|23710|14|Not recorded|p74|||||||||
19435|Waratah Limestone|24002|5|Briefly described|p234|Lochkovian|Lochkovian|||||||
19435|Waratah Limestone|24098|6|Mentioned|p27 Fig. 2|Pragian|Pragian|Geological Province: Melbourne Zone, Lachlan Fold Belt (Waratah Bay Platform).||||||19-APR-05
19435|Waratah Limestone|24551|4|Described|p130|Devonian|Devonian|Previously included rocks now included in the Bird Rock Member of the Digger Island Marlstone.||||||
19435|Waratah Limestone|30570|5|Briefly described|p4|||||||||
19435|Waratah Limestone|30930|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
19435|Waratah Limestone|31508|6|Mentioned|Table 1|||Devonian||||||
19435|Waratah Limestone|32583|6|Mentioned|p379|||NSW??[CEBJul95]||||||
19435|Waratah Limestone|32984|6|Mentioned|p343|||NSW??[CEBJul95]||||||
19435|Waratah Limestone|33156|4|Described|p130|||L.Dev.||||||
19435|Waratah Limestone|33159|6|Mentioned|p15||Early Devonian|||||||
19435|Waratah Limestone|33238|5|Briefly described|p642|||||||||
19435|Waratah Limestone|33393|6|Mentioned|p163|||||||||
19435|Waratah Limestone|33601|6|Mentioned|Fig.6|||||||||
19435|Waratah Limestone|33602|6|Mentioned|Fig.2|||||||||
19435|Waratah Limestone|33604|6|Mentioned|p17|||L.Dev. Correlation chart||||||
19435|Waratah Limestone|33732|6|Mentioned|p106|||||||||
19435|Waratah Limestone|34815|6|Mentioned|p18|||||||||
19435|Waratah Limestone|34843|5|Briefly described|p8|||||||||
19435|Waratah Limestone|34954|6|Mentioned|Fig.34|||Analysis Fig.33.||||||
19435|Waratah Limestone|35193|6|Mentioned|p19|||||||||
19435|Waratah Limestone|35274|5|Briefly described|p421|||||||||
19435|Waratah Limestone|35283|3|Fully described|p57|||||||||
19435|Waratah Limestone|37501|6|Mentioned|p405|||||||||
19435|Waratah Limestone|38787|6|Mentioned|p125|||||||||
19435|Waratah Limestone|39858|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
19435|Waratah Limestone|41571|6|Mentioned|p55|||||||||
19435|Waratah Limestone|41585|4|Described|p116|||||||||
19435|Waratah Limestone|41868|6|Mentioned|p575|||||||||
19435|Waratah Limestone|42032|5|Briefly described|p496|||||||||
19435|Waratah Limestone|42577|5|Briefly described|p31|||||||||
19435|Waratah Limestone|42635|5|Briefly described|p24, 26|||||||||
19435|Waratah Limestone|42938|5|Briefly described|p578|||||||||
19435|Waratah Limestone|43461|14|Not recorded|p627,628|||||||||
19435|Waratah Limestone|43525|14|Not recorded|p130,Table p132||Siegenian|Equivalent to Coopers Creek Formation||||||
19435|Waratah Limestone|43537|14|Not recorded|p7|||Includes Kiln and Bird Rock Members||||||
19435|Waratah Limestone|43547|14|Not recorded|p151,Tb 153-4,161||Emsian|(L.Emsian)||||||
19435|Waratah Limestone|44197|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
19435|Waratah Limestone|61181|5|Briefly described|p69, 127-128|Early Devonian|Early Devonian|Includes Bird Rock Member and the uppermost Kiln and Bluff Members. Overlain by Bell Point Limestone. See also p129 Tb. 32.||||||
19435|Waratah Limestone|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Waratah Bay. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
19435|Waratah Limestone|68116|5|Briefly described|Appendix, Maps 56-57.|Pragian|Lochkovian||||||Limestone: massive, mid-grey; recrystallized.|
19435|Waratah Limestone|73143|6|Mentioned|p18|Pragian|Lochkovian|Contains Aphyllum murrayi rugose coral (Etheridge, 1899).||||||
19435|Waratah Limestone|73489|6|Mentioned|p651|Early Devonian|Early Devonian|||||Overlies Bear Gully Chert||
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||
25597|Warburton Granodiorite|22602|6|Mentioned|p434|||||||||
25597|Warburton Granodiorite|22933|6|Mentioned|p21|||||||||
25597|Warburton Granodiorite|23269|6|Mentioned|Fig14-3.1p403|||||||||
25597|Warburton Granodiorite|23309|5|Briefly described|p446 App1||Late Devonian|G235 I-Type. Age: 369+/-13Ma. Supersedes Warburton Granite.||||||
25597|Warburton Granodiorite|24551|6|Mentioned|p223, 720 Table 8.3|||s Type.||||||
25597|Warburton Granodiorite|33607|6|Mentioned|Map legend|Devonian|Devonian|Granodiorite, fine, even-grained||||||29-NOV-04
25597|Warburton Granodiorite|35073|6|Mentioned|p11|||See also Table 4.||||||
25597|Warburton Granodiorite|35277|6|Mentioned|p89|||||||||
25597|Warburton Granodiorite|35278|6|Mentioned|p353|||||||||
25597|Warburton Granodiorite|39291|6|Mentioned|Fig.14|||||||||
25597|Warburton Granodiorite|41641|5|Briefly described|p159|||||||||
25597|Warburton Granodiorite|41868|6|Mentioned|p590|||||||||
25597|Warburton Granodiorite|42827|6|Mentioned|p159|||||||||
25597|Warburton Granodiorite|44187|5|Briefly described|Map Legend||Late Devonian|G235 S-type.||||||
25597|Warburton Granodiorite|64616|6|Mentioned|p131|Late Devonian|Late Devonian|Age determined by Richards and Singleton, 1981.||||||
25597|Warburton Granodiorite|68116|5|Briefly described|Appendix, Map 42.|Late Devonian|Late Devonian||||||Biotite granodiorite: fine grained, equigranular; medium grey.|
31662|Warburton Suite|24551|5|Briefly described|p222|||Of the Strathbogie Province.||||||
31662|Warburton Suite|42726|5|Briefly described|Map Legend||Middle Devonian|||||||
31662|Warburton Suite|44093|5|Briefly described|p203 App. 1|Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||
25598|Warby Springs Granite|22971|5|Briefly described|p 34|Devonian|Devonian|||||||
25598|Warby Springs Granite|23309|5|Briefly described|p446 App1|Late Devonian|Middle Devonian|G203 S-Type. Age: 368+/-15Ma, 375+/-6Ma.||||||
25598|Warby Springs Granite|24551|6|Mentioned|p218|||Age: 370Ma.||||||
25598|Warby Springs Granite|42154|6|Mentioned|Table 1 P334|||||||||
25598|Warby Springs Granite|66769|6|Mentioned|142|||Tabberabbera Zone. Ba-rich||||||
25598|Warby Springs Granite|68116|5|Briefly described|Appendix, Map 19.|Late Devonian|Late Devonian||||||Biotite-cordierite granite: grey, medium grained; slightly porphyritic in K-feldspar, has minor garnet; S-type; nonmagnetic.|
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||||
19469|Warm Corner Aplite|42726|5|Briefly described|map legend|Early Devonian||||||||
19475|Warneet Sands|42824|5|Briefly described|p264|||||||||
37244|Warradale Tonalite|24012|3|Fully described|p223 appendix 1|Ordovician|Cambrian|||||||
37244|Warradale Tonalite|50154|2|Defined|p84, p248 App.5|Cambrian|Cambrian|Of the Glenelg River Metamorphic Complex. Overlain by the Coleraine Volcanic Group.||||||15-SEP-04
37244|Warradale Tonalite|50155|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Biotite-hornblende tonalite; I-type||||||25-JUN-04
37244|Warradale Tonalite|50156|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-hornblende tonalite||||||20-AUG-04
37244|Warradale Tonalite|50157|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-hornblende tonalite||||||20-AUG-04
37244|Warradale Tonalite|50158|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-hornblende tonalite||||||20-AUG-04
37244|Warradale Tonalite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-hornblende tonalite||||||20-AUG-04
37244|Warradale Tonalite|50160|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-hornblende tonalite||||||20-AUG-04
37244|Warradale Tonalite|50161|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-hornblende tonalite||||||20-AUG-04
37244|Warradale Tonalite|50162|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-hornblende tonalite||||||20-AUG-04
37244|Warradale Tonalite|50163|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite-hornblende tonalite||||||20-AUG-04
37244|Warradale Tonalite|66002|6|Mentioned|p9 Tb.5|||G431. Defined by Morand et al. 2003.||||||
37244|Warradale Tonalite|72313|6|Mentioned|p459 Table 2|||Delamerian Orogen. I-type. Hf and O18 isotope data included.|510 Ma|||||
19487|Warragul basalts|39446|6|Mentioned|p44|||||||||
23141|Warrak Formation|22531|6|Mentioned|p6|Cambrian|Cambrian|of Saint Arnaud Group||||||
23141|Warrak Formation|22756|3|Fully described|P9, P20|Ordovician|Cambrian|||||||
23141|Warrak Formation|23164|4|Described|p12|Cambrian|Cambrian|||||||
23141|Warrak Formation|23166|5|Briefly described|Map legend|Ordovician|Cambrian|of Saint Arnaud Group.||||||
23141|Warrak Formation|23167|5|Briefly described|Map legend|Ordovician|Cambrian|of Saint Arnaud Group.||||||
23141|Warrak Formation|23168|5|Briefly described|Map legend|Ordovician|Cambrian|of Saint Arnaud Group.||||||
23141|Warrak Formation|23169|5|Briefly described|Map legend|Ordovician|Cambrian|of Saint Arnaud Group.||||||
23141|Warrak Formation|23307|5|Briefly described|Map Legend|Cambrian|Cambrian|Of Saint Arnaud Group||||||
23141|Warrak Formation|23309|5|Briefly described|p41-43. Table 2.12|||Of the Saint Arnaud Group.||||||03-JUL-13
23141|Warrak Formation|24551|4|Described|p82|Late Cambrian|Late Cambrian|Oldest unit of Saint Arnaud Group. Minimum thickness: 2-2.5km.||||||
23141|Warrak Formation|43260|5|Briefly described|Map Legend|Ordovician|Cambrian|of Saint Arnaud Group.||||||
23141|Warrak Formation|43846|5|Briefly described|10|Ordovician|Cambrian|||||||
23141|Warrak Formation|50352|5|Briefly described|Map Legend|Ordovician|Cambrian|Phyllite, micaceous quartz-rich arenite||||||
23141|Warrak Formation|60451|4|Described|p57, 152|Late Cambrian|Late Cambrian|Of/underlies the Saint Arnaud Group. Includes: Concongella Gritstone. Thickness: 1.5km+. Overlies: Magdala Volcanics.||||||
23141|Warrak Formation|60454|5|Briefly described|Map Legend|Ordovician|Cambrian|Geological Province: Delamerian Fold Belt. Of the Saint Arnaud Group. Turbiditic sandstone, siltstone, mudstone; laminated siltstone predominant.||||||03-JUL-13
23141|Warrak Formation|60457|5|Briefly described|Map Legend|Ordovician|Cambrian|Of the Saint Arnaud Group. Turbiditic sandstone, siltstone, mudstone.||||||03-JUL-13
23141|Warrak Formation|60458|5|Briefly described|Map Legend|Ordovician|Cambrian|Of the Saint Arnaud Group. Turbiditic sandstone, siltstone and mudstone.||||||
23141|Warrak Formation|60459|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Saint Arnaud Group. Turbiditic quartz-rich sandstone, mudstone; laminated siltstone predominant. Chlorite to biotite greenschist grade.||||||03-JUL-13
23141|Warrak Formation|61750|5|Briefly described|p19|||Of the Saint Arnaud Group west of Avoca Fault (Cayley and McDonald, 1995). Contains varied rock types - including turbiditic sandstone, siltstone and carbonaceous mudstone.||||||
23141|Warrak Formation|61752|5|Briefly described|p6 Fig. 2|Cambrian|Cambrian|||||||07-FEB-11
23141|Warrak Formation|62099|5|Briefly described|p331|Cambrian|Cambrian|Of the Saint Arnaud Group. Thickness: >2.5km. In the Stawell Zone of the Lachlan Orogen.||||||
23141|Warrak Formation|62754|5|Briefly described|p863|||Of the Saint Arnaud Group. Geological Province: Stawell Zone.||||||
23141|Warrak Formation|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Saint Arnaud Group. Includes Concongella Gritstone Member. Defined by Cayley and McDonald 1995.||||||
23141|Warrak Formation|66012|4|Described|p4-5, p8, p10 Tb.1, p11, p25-26|Ordovician|Cambrian|Of Saint Arnaud Group. Interbedded medium- to thickly-bedded phyllite and fine-grained, micaceous, quartzose arenite. Forms inliers surrounded by Newer Volcanic Group. Interpreted as deposited below wave base, possibly as overbank turbidite deposits| | | | | |13-JUN-13
23141|Warrak Formation|68116|5|Briefly described|Appendix, Maps 22-23, 30-31, 40.|Late Cambrian|Late Cambrian|Deep water; unfossiliferous. Thin, interbedded sandstone and siltstone beds form packages up to 15m thick.  Fine grained sandstone beds contain cross-laminations, sedimentary slump folds, and carbonate concretions.|||||Sandstone, interbedded siltstone and shale: immature quartz wacke to feldspathic greywacke sandstones; mostly grade up into green to brown siltstone; common thick blue to black carbonaceous mudstone beds.|
23141|Warrak Formation|68189|6|Mentioned|p17 Tb.3.1|||||||||
23141|Warrak Formation|68194|5|Briefly described|p10, p20-21, p31, p32-33 Figs.29,31|Cambrian|Cambrian|See also p35-37, p40, p42, p46-47, p57, p79. Regolith and remote sensing profiles described.||Basal unit in Saint Arnaud Group.||Is faulted against Pyrenees Formation.|Interbedded turbiditic sandstone, siltstone and lesser black shale.|
23141|Warrak Formation|73118|6|Mentioned|p14|||Stawell Zone, Lachlan Fold Belt, Western Victoria.||||||
23141|Warrak Formation|73496|5|Briefly described|Map legend|Cambrian|Cambrian|||Saint Arnaud Group|||Parts either have magnetic responses typically of 10 to 30 nT, or are weakly magnetised with magnetic responses typically 1 to 5 nT, or nonmagnetic with magnetic responses less than 1 nT.|
23141|Warrak Formation|73497|6|Mentioned|Map legend|Cambrian|Cambrian|||Saint Arnaud Group||||
23142|Warrambat Andesite Breccia|23309|5|Briefly described|p36 Table 2.7|||Of the Jamieson Volcanics.||||||
23142|Warrambat Andesite Breccia|24551|5|Briefly described|p87|||Of Jamieson Volcanics (fig. 3.15)||||||
23142|Warrambat Andesite Breccia|24576|6|Mentioned|p731|||Geological Province: Lachlan Fold Belt||||||
23142|Warrambat Andesite Breccia|61187|5|Briefly described|p50.|Early Cambrian|Early Cambrian|||Unit in Jamieson Volcanics.||Is faulted against Brissces Hut Andesite and Wrens Flat Andesite.||
23142|Warrambat Andesite Breccia|68116|5|Briefly described|Appendix, Map 34.|Cambrian|Cambrian||||||Andesite breccia, massive, vesicular andesite lava.|
19496|Warrandyte Conglomerate Member|22684|5|Briefly described|p751, Fig.2 p746|Wenlock|Wenlock|||||||
19496|Warrandyte Conglomerate Member|33599|6|Mentioned|p2|||||||||
19496|Warrandyte Conglomerate Member|37727|6|Mentioned|p9|||||||||
19496|Warrandyte Conglomerate Member|38787|6|Mentioned|p124|||||||||
19496|Warrandyte Conglomerate Member|62469|5|Briefly described|p5 Fig. 2|Wenlock|Wenlock|Of the Anderson Creek Formation. Geological Province: Darraweit Guim Province.||||||07-FEB-11
73177|Warrion Hill lavas|61896|6|Mentioned|p57|||Informal name for basalts in the Red Rock Complex area. Mainly olivine tholeiites to hawaiites.||||||19-DEC-07
19535|Warrnambool Aeolianite|24551|6|Mentioned|p343|||Of the Bridgewater Group.||||||
19535|Warrnambool Aeolianite|30993|6|Mentioned|p160|||Pleistocene||||||
19535|Warrnambool Aeolianite|31003|6|Mentioned|p41|||||||||
19535|Warrnambool Aeolianite|32102|6|Mentioned|p177|||||||||
19535|Warrnambool Aeolianite|34993|4|Described|p299|||||||||
19535|Warrnambool Aeolianite|35722|6|Mentioned|Table 2|||Quaternary stratigraphic units and nature of components.||||||
19535|Warrnambool Aeolianite|37583|4|Described|p163|||||||||
19535|Warrnambool Aeolianite|41769|4|Described|p52|||||||||
19535|Warrnambool Aeolianite|41848|4|Described|p374|||||||||
19535|Warrnambool Aeolianite|42827|4|Described|p374|||||||||
19535|Warrnambool Aeolianite|73386|6|Mentioned|p14|||||Bridgewater Formation||||
41180|Warrock Limestone Member|50154|2|Defined|p52, p63, p249 App.5|Cambrian|Cambrian|Of the Nangeela Formation.||||||15-SEP-04
41180|Warrock Limestone Member|50156|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Nangeela Formation. Calcite marble: fine grained, laminated||||||
41180|Warrock Limestone Member|50157|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Nangeela Formation. Calcite marble: fine grained, laminated||||||
41180|Warrock Limestone Member|50158|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Nangeela Formation.  Laminated, fine-grained clacite marble.||||||
41180|Warrock Limestone Member|50159|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Nangeela Formtion. Calcite marble: fine grained, laminated.||||||22-JUN-04
41180|Warrock Limestone Member|50160|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Nangeela Formation. Calcite marble: fine grained, laminated||||||
41180|Warrock Limestone Member|50161|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Nangeela Formation. Calcite marble: fine grained, laminated||||||
41180|Warrock Limestone Member|50162|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Nangeela Formation. Calcite marble: fine grained, laminated||||||24-JUN-04
41180|Warrock Limestone Member|50163|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Nangeela Formation.  Laminated, fine-grained calcite marble.||||||27-MAY-13
41180|Warrock Limestone Member|66002|5|Briefly described|p4 Tb.1|Cambrian|Cambrian|Of Nangeela Formation. Defined  by Morand et al. 2003||||||
41180|Warrock Limestone Member|71593|6|Mentioned|p20|||Glenelg Zone.|||||Limestone.|
30442|Wartook Sandstone|23309|5|Briefly described|p78-79, 204.|||Maximum Thickness: 250m.  Of the Mount Difficult Subgroup.||||||
30442|Wartook Sandstone|44929|5|Briefly described|Map Legend|Silurian|Ordovician|Of Mount Difficult Group. Includes the Daahl Sandstone Member. Pale, fine- to medium-grained quartz to quartzo-feldspathic sandstone.||||||26-JUN-14
30442|Wartook Sandstone|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Of Mount Difficult Sub-Group (Grampians Group). Includes Daahl Sandstone Member. Pale, fine- to coarse-grained quartz to quartzo-feldspathic sandstone.||||||13-JUN-06
30442|Wartook Sandstone|44932|5|Briefly described|Map Legend|Silurian|Ordovician|Of Mount Difficult Group. Includes the Daahl Sandstone Member. Pale, fine- to medium-grained quartz to quartzo-feldspathic sandstone.||||||26-JUN-14
30442|Wartook Sandstone|44933|5|Briefly described|Map Legend|Silurian|Ordovician|Of Mount Difficult Group. Includes the Daahl Sandstone Member. Pale, fine- to medium-grained quartz to quartzo-feldspathic sandstone.||||||26-JUN-14
30442|Wartook Sandstone|60451|4|Described|p77 Fig. 47, 82, 142|Early Devonian|Ordovician|Of the Mount Difficult Subgroup (Grampians Group). Maximum Thickness: 250m+. Quartz to quartzo-feldspathic sandstone with minor mica.||||||
30442|Wartook Sandstone|60456|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Mount Difficult Sub-Group.  Sandstone: pale, fine to coarse grained quartz to quartzo-feldspathic with scattered and lag horizons of subrounded vein quartz pebbles towards base.||||||
30442|Wartook Sandstone|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Mount Difficult Subgroup. Sandstone: pale, fine to coarse grained quartz to quartzo-feldspathic with scattered and lag horizons of sub-rounded vein quartz pebbles towards base.||||||
30442|Wartook Sandstone|61183|4|Described|p30 Tb. 2, p49|||Of Mount Difficult Subgroup (Grampians Gp). Incl: Daahl Sandstone Member. Thick-bedded, fine- to coarse-grained quartz to quartzo-feldspathic sandstone with minor mica; parts bioturbated. Conformably overlies Moora Moora Sandstone. Thickness: >250m.||||||26-JUN-14
30442|Wartook Sandstone|61186|5|Briefly described|p76, p77|||Top unit in Mount Difficult Subgroup (Grampians Group). Possible equivalent to Serra Sandstone.||||||26-JUN-14
30442|Wartook Sandstone|64541|5|Briefly described|Map Legend|Silurian|Silurian|Of Mount Difficult Sub-group. Sandstone: pale, fine to coarse-grained quartz to quartzo-feldspathic with scattered and lag horizons of sub-rounded vein quartz pebbles towards base.||||||07-FEB-11
30442|Wartook Sandstone|64610|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Difficult Subgroup (Grampians Gp). Sandstone: pale, fine- to coarse-grained quartz to quartzo-feldspathic with scattered and lag horizons of sub-rounded vein quartz pebbles towards base; laminated, x-lam'd and rarely trough x-lam'd; more details.||||||17-NOV-08
30442|Wartook Sandstone|65313|6|Mentioned|p582-3, p575 Fig. 4, p581 Fig. 9|Emsian|Pragian|Includes the basal Emsian (?isotopic) Event at 406.2 Ma towards the top of the unit. Grampians National Park section.||Part of Mount Difficult Subgroup.||Overlies Moora Moora Sandstone.||26-MAR-12
30442|Wartook Sandstone|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Mount Difficult Subgroup. Includes Daahl Sandstone Member. Defined by Cayley & Taylor, 1997. ||||||
30442|Wartook Sandstone|68116|5|Briefly described|Appendix, Maps 22, 30, 39.|Early Devonian|Ludlow|Contains minor quartz siltstone interbeds.|||||Pale, fine to coarse-grained quartz to quartzo-feldspathic sandstone with scattered and lag horizons of subrounded vein quartz pebbles (base): laminated, cross-laminated and rarely trough cross-laminated, medium to thickly-bedded.|
30442|Wartook Sandstone|73118|6|Mentioned|p64, 70|Silurian|Silurian|||Grampians Group.||||
19556|Wataepoolan Limestone|24551|6|Mentioned|p300|||Of the Heytesbury Group.||||||
19556|Wataepoolan Limestone|30828|6|Mentioned|p113|||||||||
19556|Wataepoolan Limestone|31624|6|Mentioned|p121|||See also Table 5-3||||||
19556|Wataepoolan Limestone|31625|6|Mentioned|Fig. 5.2|||Miocene||||||
37790|Watchmaker Granodiorite|23309|6|Mentioned|p446, Appendix 1|||G502, I-Type.  Supersedes Watchmaker Granite.||||||
37790|Watchmaker Granodiorite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|I-type. Medium to coarse grained biotite K-feldspar rich granodiorite.||||||
37790|Watchmaker Granodiorite|60541|5|Briefly described|p68, p22, p18 Tb. 1|Silurian|Silurian|Consists of large equidimensional quartz, large oscillatory zoned and twinned plagioclase, in an interdigitating groundmass of quartz, K-feldspar and plagioclase. May be associated with Glenbog Supersuite. Type locality given. Intrudes Pinnak Sst.||||||12-JAN-06
37790|Watchmaker Granodiorite|68116|5|Briefly described|Appendix, Map 45.|Devonian|Silurian||||||Biotite granodiorite: medium to coarse-grained; K-feldspar rich; I-type.|
30431|Watgania Gap Sandstone|23309|5|Briefly described|p78|||Maximum thickness: 200m.  Of the Red Man Bluff Subgroup.||||||
30431|Watgania Gap Sandstone|44929|5|Briefly described|Map Legend|Silurian|Ordovician|Of Red Man Bluff Sub-Group (Grampians Group). Pale yellow quartzo-feldspathic, sandstone; massive, laminated and trough cross-laminated.||||||26-JUN-14
30431|Watgania Gap Sandstone|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Of Red Man Bluff Sub-Group (Grampians Group). Pale yellow quartzo-feldspathic, sandstone; massive, laminated and trough cross-laminated.||||||25-JUL-06
30431|Watgania Gap Sandstone|44932|5|Briefly described|Map Legend|Silurian|Ordovician|Of Red Man BLuff Sub-Group (Grampians Group). Pale yellow quartzo-feldspathic, sandstone; massive, laminated and trough cross-laminated.||||||14-JUN-06
30431|Watgania Gap Sandstone|44933|5|Briefly described|Map Legend|Silurian|Ordovician|Of Red Man Bluff Sub-Group.||||||14-JUN-06
30431|Watgania Gap Sandstone|60451|4|Described|p76, 79|Early Devonian|Ordovician|Of the Red Man Bluff Subgroup (Grampians Group). Type section in text. Maximum Thickness: ~200m. Laminate siltstone interbedded with quartzo-feldspathic sandstone.||||||24-NOV-08
30431|Watgania Gap Sandstone|60456|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Man Bluff Sub-Group. Sandstone: pale yellow, quartzo-feldspathic; massive, planar and trough cross laminated, thin to thickly bedded.||||||30-SEP-04
30431|Watgania Gap Sandstone|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Red Man Bluff Subgroup. Sandstone, pale yellow, quartzo-feldspathic; massive; planar and trough cross laminated, thin to thickly bedded.||||||
30431|Watgania Gap Sandstone|61183|4|Described|p30 Tb. 2, p37-38|||Of Red Man Bluff Subgp (Grampians Gp). Laminated siltstone (<10cm thick) interbedded with massive, laminated or trough x-bedded, coarse-gr. quartzo-feldspathic sst (<1m thick). Overlies Gariwerd Sandstone; underlies Murray Hill Sandstone. Thickness: ~200m||||||
30431|Watgania Gap Sandstone|64541|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Red Man Bluff Sub-group. Sandstone: pale yellow, quartzo-feldspathic; massive, laminated and trough cross-laminated, thin to thickly bedded; outcrops poorly; minor thin interbeds of laminated siltstone.||||||07-FEB-11
30431|Watgania Gap Sandstone|64610|5|Briefly described|Map legend|Ordovician|Ordovician|Of Red Man Bluff Subgroup (Grampians Gp). Sandstone pale yellow, quartzo-feldspathic; massive, laminated and trough-laminated, thin to thickly bedded; outcrops poorly; minor thin interbeds of laminated siltstone.||||||
30431|Watgania Gap Sandstone|65313|6|Mentioned|p581 Fig. 9,p582 Fig. 10|Ordovician|Ordovician|Grampians National Park sections.||Of Red Man Bluff Subgroup.||Overlies Gariwerd Sandstone; underlies Murray Hill Sandstone.||26-MAR-12
30431|Watgania Gap Sandstone|66002|5|Briefly described|p5 Tb.3|Silurian|Silurian|Of Red Man Bluff Subgroup. Defined by Cayley & Taylor, 1997.||||||
30431|Watgania Gap Sandstone|68116|5|Briefly described|Appendix, Maps 22, 30.|Ludlow|Late Ordovician||||||Sandstone and siltstone: sandstone coarse, quartzo-feldspathic, massive to planar laminated or troughcross bedded; siltstone laminated, occurs as thin beds.|
30692|Wattle Grove Granite|23309|6|Mentioned|p446 App1|||G84. S-Type||||||
30692|Wattle Grove Granite|60503|5|Briefly described|p154, p44 Tb.2|Silurian|Silurian|Consists of medium-grained quartz, feldspar, muscovite and biotite; strongly foliated and contains abundant schist inclusions along margins. Intrudes the Omeo Metamorphic Complex and is itself intruded by Triassic Beloka Gap Granite.||||||26-JUN-14
30692|Wattle Grove Granite|60504|5|Briefly described|Map Legend|Wenlock|Wenlock|Muscovite granite: S-type, foliated, medium grained, grey: margins rich in metasedimentary enclaves||||||
30692|Wattle Grove Granite|60505|5|Briefly described|Map legend|Wenlock|Wenlock|Muscovite granite: S-type, foliated, medium grained, grey: margins rich in metasedimentary enclaves||||||
30692|Wattle Grove Granite|60506|5|Briefly described|Map legend|Wenlock|Wenlock|Muscovite granite: S-type, foliated, medium grained, grey: margins rich in metasedimentary enclaves||||||
30692|Wattle Grove Granite|60507|5|Briefly described|Map Legend|Wenlock|Wenlock|Muscovite granite: S-type, foliated, medium grained, grey: margins rich in metasedimentary enclaves||||||
30692|Wattle Grove Granite|60508|5|Briefly described|Map legend|Early Silurian|Early Silurian|Muscovite-biotite granite: S-type; nonmagnetic (0-5 nT) with weakly magnetic (10 nT) north-northwest trending dykes; high total count, K, Th, moderate U.||||||08-NOV-04
30692|Wattle Grove Granite|68116|5|Briefly described|Appendix, Map 27a.|Wenlock|Llandovery||||||Muscovite-biotite granite: grey; medium-grained; foliated, margins rich in metasedimentary enclaves.|
37612|Wedderburn Granodiorite|23309|5|Briefly described|p339, 342|Early Devonian|Early Devonian|G345, I-Type.  Age:393+/-5Ma, 394+/-5Ma, 386+/-5Ma. Supersedes Wedderburn Granite.||||||
37612|Wedderburn Granodiorite|60452|4|Described|p52|||The magnetic portion was known as Inglewood Granite. Non-magnetic portion formerly called Korong Granite. See also p7, p16-17, p47. The colluvial fan around this granodiorite was previously named "Korong Bahada".||||||
37612|Wedderburn Granodiorite|60461|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Mount Cole Suite.  Biotite and biotite-hornblende granodiorite: porphyritic.||||||
37612|Wedderburn Granodiorite|60462|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Mount Cole Suite. Granodiorite: I-type, oxidised, strongly zoned, with only the inner weakly to nonmagnetic zones having significant outcrop; radiometric response variable, outcrop areas high K, U and moderate Th, laterite covered areas Th dominant||||||
37612|Wedderburn Granodiorite|65715|5|Briefly described|p8 Tb.4|||Of Mount Cole Suite. G345. Called Wedderburn pluton by King (1977). Revised by Edwards et al. (2001) to include junior synonym Inglewood Granite of Marlow and Bushell (1995).||||||
37612|Wedderburn Granodiorite|66769|6|Mentioned|130|||Bendigo Zone. Appears as Wedderburn Granite in Fig.8. Seismically bland, poorly reflective, near surface body.||||||
37612|Wedderburn Granodiorite|68116|5|Briefly described|Appendix, Maps 16, 23.|Early Devonian|Early Devonian||||||Biotite and biotite-hornblende granodiorite; porphyritic; marginal outcrops contain enclaves of feldspar-hornblende porphyry; nonmagnetic inner phase surrounded by magnetic phase.|
37612|Wedderburn Granodiorite|68189|6|Mentioned|p42 App.2|||Ages from McKenzie et al. (K-Ar, 1984) and Gleadow & Lovering (F-T, 1978) respectively. Four intermediate ages are also given.|397 +/- 4 to 282 +/- 11 Ma.|||||30-JUN-14
19682|Weeragua Granodiorite|22878|4|Described|p69|||||||||
19682|Weeragua Granodiorite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Biotite-hornblende granodiorite: greenish grey, coarse grained, massive to mylonitic; compositionally variable; prominant quartz; abundant mafic inclusions.||||||06-OCT-04
19682|Weeragua Granodiorite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Biotite-hornblende granodiorite: greenish grey, coarse grained, massive to mylonitic; compositionally variable; prominant quartz; abundant mafic inclusions.||||||01-OCT-04
19682|Weeragua Granodiorite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Biotite-hornblende granodiorite: Moderately magnetic (40-100 nT) to non-magnetic. High K, low Th and U.||||||06-OCT-04
19682|Weeragua Granodiorite|23309|5|Briefly described|p320-324.|||G24 - I-Type.||||||
19682|Weeragua Granodiorite|40889|5|Briefly described|p97|||||||||
19682|Weeragua Granodiorite|41850|6|Mentioned|p428|||||||||
19682|Weeragua Granodiorite|68116|5|Briefly described|Appendix, Map 37.|Early Devonian|Llandovery||||||Biotite-hornblende granodiorite: medium grained, slightly porphyritic; I-type.|
37613|Wellington Volcanic Group|23309|5|Briefly described|p160, 171-175, Table2.07|Devonian|Devonian|See also Wellington Volcanics.||||||
37613|Wellington Volcanic Group|24551|5|Briefly described|p88 Fig. 3.15|Late Devonian|Late Devonian|Max. Thickness: 900m.||||||
37613|Wellington Volcanic Group|61161|5|Briefly described|p126-131, p76-77 Fig 6.1, p185|||Of Avon Supergroup. Overlies Moroka Glen Formation; underlies Mansfield Group. Mainly felsic volcanic (pyroclastics; minor epiclastic sediments); non-volcanic fluvial sedimentary rocks. Thickness varies. Age estimate Givetian. GSV map code: Daw.||||||
37613|Wellington Volcanic Group|61169|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Pyroclastic and fluvial deposits: rhyolitic ignimbrite, minor non-volcanic sedimentary rocks, including siliciclastic sandstone and red mudstone; minor epiclastic rocks; GSV map code: Daw.||||||
37613|Wellington Volcanic Group|61170|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Pyroclastic and fluvial deposits: rhyolitic ignimbrite, minor non-volcanic sedimentary rocks, including siliciclastic sandstone and red mudstone; minor epiclastic rocks; GSV map code: Daw.||||||07-FEB-11
37613|Wellington Volcanic Group|61171|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Pyroclastic and fluvial deposits: rhyolitic ignimbrite, minor non-volcanic sedimentary rocks, including siliciclastic sandstone and red mudstone; minor epiclastic rocks; GSV map code: Daw.||||||
37613|Wellington Volcanic Group|61172|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Pyroclastic and fluvial deposits: rhyolitic ignimbrite, minor non-volcanic sedimentary rocks, including siliciclastic sandstone and red mudstone; minor epiclastic rocks; GSV map code: Daw.||||||
37613|Wellington Volcanic Group|61173|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Avon Supergroup. Ignimbrite, minor non-volcanic sedimentary rocks: moderate gravity response (-350 to -320 ums^-2); generally nonmagnetic (0 nT, k < 1 x10^-6 cgs), with some weakly magnetic units (40 nT, k up to 440 x10^-6 cgs); GSV map code: Daw.||||||
37613|Wellington Volcanic Group|64010|5|Briefly described|p258 Fig.1, p259. |||||Of the Avon Supergroup.|Includes the Highton Volcanics.|Overlies Delatite Group. Is overlain by Mansfield Group.||
37613|Wellington Volcanic Group|64536|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Avon Supergroup. Includes the Highton Volcanics with 3 unnamed members of conglomerate, andesite and rhyodacite. More lithological detail included in map legend.||||||07-FEB-11
37613|Wellington Volcanic Group|64537|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Avon Supergroup. Includes the Highton Volcanics with 3 unnamed members of conglomerate, andesite and rhyodacite. More lithological detail included in map legend.||||||07-FEB-11
37613|Wellington Volcanic Group|64538|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Avon Supergroup. Includes the Highton Volcanics with 3 unnamed members of conglomerate, andesite and rhyodacite. More lithological detail included in map legend.||||||07-FEB-11
37613|Wellington Volcanic Group|64606|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Avon Supergroup. Includes Highton Volcanics.||||||11-NOV-08
37613|Wellington Volcanic Group|64616|5|Briefly described|p131-132, p136, p157, p187, p300|Frasnian|Givetian|VandenBerg et al., (2000). Formerly Wellington Rhyolite. Of Avon Supergroup. Unconformably overlies Delatite Group and overlain by Mansfield Group. Appears as Wellington Group on p131 and as Mount Wellington Volcanics on p132. Includes Highton Volcanics in project area. Geophysical characteristics given.||||||
37613|Wellington Volcanic Group|68116|5|Briefly described|Appendix, Maps 34, 43-44.|Frasnian|Givetian||||||Rhyolite and rhyodacite ignimbrite, sedimentary units.|
37243|Wennicott Tonalite|23309|6|Mentioned|p446, Appendix 1|||G429, S-Type.||||||
37243|Wennicott Tonalite|24012|3|Fully described|p222 appendix 1|Ordovician|Cambrian|||||||
37243|Wennicott Tonalite|24551|5|Briefly described|p76|||Of the Glenelg River Complex.||||||
37243|Wennicott Tonalite|50154|2|Defined|p83, p248 App.5|Cambrian|Cambrian|Of the Glenelg River Metamophic Complex. Overlain by the Coleraine Volcanic Group.||||||15-SEP-04
37243|Wennicott Tonalite|50155|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Biotite tonalite; S-type||||||
37243|Wennicott Tonalite|50156|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite tonalite||||||20-AUG-04
37243|Wennicott Tonalite|50157|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite tonalite||||||20-AUG-04
37243|Wennicott Tonalite|50158|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite tonalite||||||20-AUG-04
37243|Wennicott Tonalite|50159|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite tonalite||||||20-AUG-04
37243|Wennicott Tonalite|50160|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite tonalite||||||20-AUG-04
37243|Wennicott Tonalite|50161|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite tonalite||||||20-AUG-04
37243|Wennicott Tonalite|50162|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite tonalite||||||20-AUG-04
37243|Wennicott Tonalite|50163|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Glenelg River Metamorphic Complex? Biotite tonalite||||||20-AUG-04
37243|Wennicott Tonalite|66002|6|Mentioned|p9 Tb.5|||G429. Defined by Morand et al. 2003.||||||
37243|Wennicott Tonalite|68116|5|Briefly described|Appendix, Map 29.|Early Ordovician|Middle Cambrian||||||Biotite tonalite: foliated, bluish-grey, medium grained, equigranular; accessory magnetite and epidote; rare hornblende-rich microgranitoid enclaves; migmatite enclaves common near western boundary; nonmagnetic.|
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.||
29131|Werribee Formation|22886|4|Described|p16|Early Miocene|Paleocene|||||||
29131|Werribee Formation|23230|4|Described|Table4-1p40, 41-2, 44|Oligocene|Eocene|Present in the Port Phillip Basin.||||||
29131|Werribee Formation|23234|6|Mentioned|p88, 91|||||||||
29131|Werribee Formation|23237|6|Mentioned|p104||Tertiary|||||||
29131|Werribee Formation|23238|6|Mentioned|p107|||Geol. Province: Port Phillip Basin||||||
29131|Werribee Formation|23258|5|Briefly described|Fig12-3.1p214, 215-6||Miocene|||||||
29131|Werribee Formation|23259|5|Briefly described|Fig12-4.3p228, 231|Miocene|Paleocene|||||||
29131|Werribee Formation|23267|5|Briefly described|Fig14-1.4p385||Silurian|||||||
29131|Werribee Formation|23307|5|Briefly described|Map Legend|Eocene|Eocene|||||||
29131|Werribee Formation|23537|5|Briefly described|p 440|||||||||
29131|Werribee Formation|24038|4|Described|p441|Miocene|Oligocene|Geological Province: Port Phillip Basin.||||||12-JAN-10
29131|Werribee Formation|24551|6|Mentioned|p734 Table 17.4, p310 Fig. 10.18|||Maximum Thickness: 250m.||||||
29131|Werribee Formation|29355|6|Mentioned|p179|||||||||
29131|Werribee Formation|29591|6|Mentioned|p98|||||||||
29131|Werribee Formation|29982|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
29131|Werribee Formation|29983|6|Mentioned|p1|||||||||
29131|Werribee Formation|30929|6|Mentioned|Map legend|Paleocene|Paleocene|||||||
29131|Werribee Formation|30931|6|Mentioned|Map legend|Eocene|Eocene|Sub-Older Volcanic||||||
29131|Werribee Formation|31242|5|Briefly described|p9|||Refers hydrogeology||||||
29131|Werribee Formation|31243|4|Described|p6|||Re hydrology.||||||
29131|Werribee Formation|32222|6|Mentioned|p6|||Drilling of aquifers||||||
29131|Werribee Formation|33458|6|Mentioned|p13|||||||||
29131|Werribee Formation|33464|6|Mentioned|Fig.2|||||||||
29131|Werribee Formation|33598|6|Mentioned|Map legend|Oligocene|Eocene|Eoc.-Oligo.||||||
29131|Werribee Formation|33604|4|Described|p20|||||||||
29131|Werribee Formation|33752|6|Mentioned|p367|||||||||
29131|Werribee Formation|34991|6|Mentioned|p387|||||||||
29131|Werribee Formation|35011|6|Mentioned|p314|||||||||
29131|Werribee Formation|35276|3|Fully described|p237|||||||||
29131|Werribee Formation|35285|5|Briefly described|p415|||||||||
29131|Werribee Formation|35290|6|Mentioned|p28|||||||||
29131|Werribee Formation|35712|4|Described|p17|||See P29 re aquifers.||||||
29131|Werribee Formation|35943|4|Described|p9|||||||||
29131|Werribee Formation|36499|6|Mentioned|p42|||||||||
29131|Werribee Formation|37035|6|Mentioned|p116|||||||||
29131|Werribee Formation|37128|5|Briefly described|p357|||||||||
29131|Werribee Formation|37385|4|Described|p8|||||||||
29131|Werribee Formation|38144|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene to Miocene||||||
29131|Werribee Formation|38146|6|Mentioned|Map legend|Eocene|Eocene|||||||
29131|Werribee Formation|38147|6|Mentioned|Map legend|Eocene|Eocene|||||||
29131|Werribee Formation|39446|6|Mentioned|p35|||||||||
29131|Werribee Formation|39865|4|Described|p28|||||||||
29131|Werribee Formation|40171|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
29131|Werribee Formation|40524|6|Mentioned|Fig.3|||||||||
29131|Werribee Formation|41537|6|Mentioned|p352|||||||||
29131|Werribee Formation|41848|6|Mentioned|p392|||Age Tertiary||||||
29131|Werribee Formation|41868|6|Mentioned|p508|||See also P554, P560, P576 and P582||||||
29131|Werribee Formation|42184|6|Mentioned|p350|||||||||
29131|Werribee Formation|42648|5|Briefly described|p45|||||||||
29131|Werribee Formation|42827|3|Fully described|p310, p316|||See also Fig 8.14||||||20-MAY-08
29131|Werribee Formation|42847|5|Briefly described|p523, Fig.1 p522|Tertiary|Tertiary|Contains the Maddingley Coal Seam, also referred to as Maddingley Seam brown coals. Unconformably overlain by Rowsley Formation.||||||09-MAY-05
29131|Werribee Formation|43282|5|Briefly described|p5,p61.||Eocene|Age given p61.||||||
29131|Werribee Formation|44197|5|Briefly described|Map Legend||Eocene|||||||
29131|Werribee Formation|60083|5|Briefly described|Map legend|Oligocene|Oligocene|Stated to be synonymous with Yaloak Formation.  Sand, sandy and silty clay, with pyritic and lignitic bands.||||||19-JUL-04
29131|Werribee Formation|60585|6|Mentioned|p32|Middle Miocene|Middle Miocene|||||||
29131|Werribee Formation|61155|5|Briefly described|p3, p18|Late Oligocene|Middle Eocene|Overlain by Fyansford Formation. Age: ~50-27Ma. Max. thickness: 40m. Geological Province: Melbourne area.||||||
29131|Werribee Formation|61180|6|Mentioned|p35|||Includes highly siliceous sand and silt favoured for glass and ceramics manufacture.||||||
29131|Werribee Formation|61181|5|Briefly described|p70, p109|||Two seams of kaolinitic clay are interbedded with sands and gravels in this unit. See also mention on p183. ||||||
29131|Werribee Formation|62897|5|Briefly described|p114, p115 Fig. 1|Miocene|Oligocene|Overlies Council Trench Formation.||||||15-MAY-08
29131|Werribee Formation|63741|5|Briefly described|p114, p115 Fig. 1|Miocene|Oligocene|Overlies Council Trench Formation.  Includes ferruginous coarse sandstones. ||||||
29131|Werribee Formation|64532|6|Mentioned|p374, p375 fig 1|Tertiary|Tertiary|Bacchus Marsh area.||||Overlies Pentland Hills Volcanics.|Fluvial sands and gravels, with coal seams.|
29131|Werribee Formation|65715|5|Briefly described|p11 Tb.7, p13, p11, 12, 14, p27, p42|Paleogene|Paleogene|Overlies Ballark Conglomerate and Castlemaine Group rocks. Overlain by Calivil Formation. Includes Altona Coal Seam, Lerderderg Gravel Member and Merrimu Gravel Member.||||||
29131|Werribee Formation|68116|5|Briefly described|Appendix, Map 41.|Miocene|Eocene||||||Sand, silt, clay, gravel in variable proportions: generally white to pale grey; in part carbonaceous, pyritic; ferruginous bands common; contains Cinnamomum flora.|
29131|Werribee Formation|68811|5|Briefly described|p116|Tertiary|Tertiary||||||Alluvial and marginal marine clay, silt and fine sands. |
29131|Werribee Formation|71277|5|Briefly described|p303 Tb.1, p305, p308, p309 Fig.8|Cenozoic|Cenozoic|More widespread unit. Middle Cenozoic.||||Unconformably overlies Melbourne Formation. Unconformably underlies the Yarra Delta Group.|Clean hard sandstones, siltstones, grey-white to dark grey carbonaceous mudstones.|
29131|Werribee Formation|71419|5|Briefly described|p8 Fig 2, p18 Fig 19|Oligocene|Oligocene|Fluvial sediments in Bungal Graben.||||||
19759|Werrikoo Member|31624|6|Mentioned|p129|||Unit of Whalers Bluff Fm.||||||
19759|Werrikoo Member|32767|6|Mentioned|p66|||||||||
19759|Werrikoo Member|33160|4|Described|p305|||||||||
19759|Werrikoo Member|35066|6|Mentioned|p217|||||||||
19759|Werrikoo Member|35097|6|Mentioned|Fig.34|||||||||
19759|Werrikoo Member|42827|5|Briefly described|p291|||of Whalers Bluff Formation||||||
19759|Werrikoo Member|48911|6|Mentioned|Chart 1|||||||||
37791|Wescotts Granite|23309|6|Mentioned|p446, Appendix 1|||G338, S-Type.||||||
37791|Wescotts Granite|60491|4|Described|p47|||Of the Coonooer Suite. Intruded by the Yeungroon Granite. S-type.||||||
37791|Wescotts Granite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Glenloth Suite. Leucocratic granite: medium to coarse grained; very poorly exposed.||||||
37791|Wescotts Granite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of the Glenloth Suite. Granite; reduced S-type; possibly weakly magnetic (to 5nT), response overprinted by magnetic palaeodrainage; gravity response part of eastern edge regional low; radiometric responses subdued, K higher than Th and U.||||||15-OCT-04
37791|Wescotts Granite|66002|5|Briefly described|p6 Tb.5|||Of Glenloth Suite. G338. Defined in Bibby and Moore 1998.||||||
37791|Wescotts Granite|68116|5|Briefly described|Appendix, Map 16.|Middle Devonian|Early Devonian||||||Leucocratic granite: medium to coarse grained; very poorly exposed.|
37791|Wescotts Granite|68189|6|Mentioned|p15 Fig.6, p17|||||||||
19816|Western Port Group|23238|6|Mentioned|p107|||Geol. Province: Western Port Basin||||||
19816|Western Port Group|24551|5|Briefly described|p735 Table 17.5|||Maximum Thickness: 175m. Consists of Baxter, Sherwood and Yallock formations.||||||
19816|Western Port Group|36197|4|Described|p10|||See also Table 1.||||||
19816|Western Port Group|37366|4|Described|p3|||||||||
19816|Western Port Group|40523|6|Mentioned|p210|||||||||
19816|Western Port Group|41868|5|Briefly described|p553|||||||||
19816|Western Port Group|42827|5|Briefly described|p553|||||||||
19858|Whalers Bluff Formation|22944|5|Briefly described|Fig3|Pleistocene|Miocene|||||||
19858|Whalers Bluff Formation|23768|5|Briefly described|p27, p30 Fig.6, p185|Early Pleistocene|Late Pliocene|Overlies Werrikoo Limestone.  Age: <4.35Ma. Geological Province: Otway Basin.||||||
19858|Whalers Bluff Formation|23909|5|Briefly described|p291|Pliocene|Pliocene|Geological Province: Otway Basin.||||||
19858|Whalers Bluff Formation|24551|5|Briefly described|p338 Fig. 11.2, 342, 306|Early Pleistocene|Late Pliocene|Overlies: Heytesbury Group.||||||
19858|Whalers Bluff Formation|24562|6|Mentioned|p69 Fig. 27|||Geological Province: Otway Basin.||||||
19858|Whalers Bluff Formation|29355|6|Mentioned|p185|||||||||
19858|Whalers Bluff Formation|30393|6|Mentioned|p309|||||||||
19858|Whalers Bluff Formation|30865|6|Mentioned|p306|||Upper Pliocene-Lower Pleistocene||||||
19858|Whalers Bluff Formation|30928|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
19858|Whalers Bluff Formation|30932|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
19858|Whalers Bluff Formation|31036|6|Mentioned|Table 9-1|||Pliocene||||||
19858|Whalers Bluff Formation|31345|6|Mentioned|FigXIII-47|||||||||
19858|Whalers Bluff Formation|31372|4|Described|p10|||||||||
19858|Whalers Bluff Formation|31424|6|Mentioned|p13|||||||||
19858|Whalers Bluff Formation|31624|4|Described|p98|||See also p127, 128. L.Pleistocene.||||||11-AUG-15
19858|Whalers Bluff Formation|31625|6|Mentioned|Fig. 5.2|||Pleistocene||||||
19858|Whalers Bluff Formation|31628|6|Mentioned|Map legend|Pleistocene|Pleistocene|Enclosure 5-4||||||
19858|Whalers Bluff Formation|31629|6|Mentioned|Fig. 5.1|||L.Pleistocene||||||
19858|Whalers Bluff Formation|32767|6|Mentioned|p66|||||||||
19858|Whalers Bluff Formation|33160|4|Described|p302|||||||||
19858|Whalers Bluff Formation|34832|6|Mentioned|p23|||||||||
19858|Whalers Bluff Formation|34954|5|Briefly described|p198|||||||||
19858|Whalers Bluff Formation|34988|6|Mentioned|p290|||||||||
19858|Whalers Bluff Formation|35066|3|Fully described|p217|||||||||
19858|Whalers Bluff Formation|35097|6|Mentioned|p30|||||||||
19858|Whalers Bluff Formation|35271|6|Mentioned|Fig.2|||||||||
19858|Whalers Bluff Formation|35274|6|Mentioned|p424|||||||||
19858|Whalers Bluff Formation|35722|6|Mentioned|p4|||Stratigraphy.||||||
19858|Whalers Bluff Formation|36366|6|Mentioned|p5|||||||||
19858|Whalers Bluff Formation|37399|6|Mentioned|Fig.1|||||||||
19858|Whalers Bluff Formation|37548|6|Mentioned|p131|||||||||
19858|Whalers Bluff Formation|38070|6|Mentioned|Fig.12|||Otway Basin||||||
19858|Whalers Bluff Formation|39077|6|Mentioned|p25|||||||||
19858|Whalers Bluff Formation|40230|6|Mentioned|Fig.1|||||||||
19858|Whalers Bluff Formation|40643|6|Mentioned|p155|||||||||
19858|Whalers Bluff Formation|41043|6|Mentioned|p98|||||||||
19858|Whalers Bluff Formation|41185|6|Mentioned|Fig.4|||||||||
19858|Whalers Bluff Formation|41521|6|Mentioned|p240|||||||||
19858|Whalers Bluff Formation|41599|6|Mentioned|p192|||||||||
19858|Whalers Bluff Formation|41642|6|Mentioned|Fig.8.6|||||||||
19858|Whalers Bluff Formation|41704|6|Mentioned|Fig.3|||||||||
19858|Whalers Bluff Formation|41769|6|Mentioned|p50|||||||||
19858|Whalers Bluff Formation|41848|5|Briefly described|p365|||see Ch8 p291 for description Age Plio-Pleistocene||||||
19858|Whalers Bluff Formation|41868|5|Briefly described|p578|||||||||
19858|Whalers Bluff Formation|42524|5|Briefly described|Fig.3 P27|||||||||
19858|Whalers Bluff Formation|42635|5|Briefly described|p91|||||||||
19858|Whalers Bluff Formation|42827|2|Defined|p291|early Pleistocene|late Pliocene|see also Fig 8.9||||||
19858|Whalers Bluff Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
19858|Whalers Bluff Formation|43660|6|Mentioned|Fig.6,p15|Pleistocene|Miocene|||||||
19858|Whalers Bluff Formation|46802|6|Mentioned|Table 1|||||||||
19858|Whalers Bluff Formation|48911|6|Mentioned|p29|||See also Chart 1||||||
19858|Whalers Bluff Formation|48925|6|Mentioned|p13|||Upper Pliocene age. Fauna. P25 etc.||||||
19858|Whalers Bluff Formation|50154|2|Defined|p26, p139|Pliocene|Pliocene|Considered to be offshore equivalent of Parilla Sand. Predominantly of Pliocene age. Max. thickness: 35m. Disconformably overlies the Murray Group and Otway Group.||||||15-SEP-04
19858|Whalers Bluff Formation|50155|5|Briefly described|Map Legend|Pleistocene|Miocene|Limestone, marl||||||
19858|Whalers Bluff Formation|50156|5|Briefly described|Map Legend|Pleistocene|Miocene|Coastal: sandy limestone, calcarenite, shell beds, marl||||||
19858|Whalers Bluff Formation|50157|5|Briefly described|Map Legend|Pleistocene|Miocene|Overlain by Bridgewater Formation and Lowan Sand Coastal: sandy limestone, calcarenite, shell beds, marl.||||||07-APR-09
19858|Whalers Bluff Formation|50158|5|Briefly described|Map Legend|Pleistocene|Miocene|Coastal: sandy limestone, calcarenite, shell beds, marl.||||||07-APR-09
19858|Whalers Bluff Formation|50159|5|Briefly described|Map Legend|Pleistocene|Miocene|Coastal: sandy limestone, calcarenite, shell beds, marl||||||
19858|Whalers Bluff Formation|50160|5|Briefly described|Map Legend|Pleistocene|Miocene|Sandy limestone, calcarenite, shell beds.||||||07-APR-09
19858|Whalers Bluff Formation|50161|5|Briefly described|Map Legend|Pleistocene|Miocene|Coastal: sandy limestone, calcarenite, shell beds, marl||||||
19858|Whalers Bluff Formation|50162|5|Briefly described|Map Legend|Pleistocene|Miocene|Coastal: sandy limestone, calcarenite, shell beds, marl||||||
19858|Whalers Bluff Formation|50163|5|Briefly described|Map Legend|Pleistocene|Miocene|Coastal: sandy limestone, calcarenite, shell beds, marl||||||
19858|Whalers Bluff Formation|50164|5|Briefly described|Map Legend|Quaternary|Miocene|Limestone, marl.||||||
19858|Whalers Bluff Formation|60421|5|Briefly described|p417|Middle Pliocene|Early Pliocene|||||||
19858|Whalers Bluff Formation|60538|5|Briefly described|p471 Fig. 10|Pliocene|Pliocene|||||||
19858|Whalers Bluff Formation|60785|5|Briefly described|p184 Fig.1, p186, pp207-208.  |Zanclean|Zanclean|Of the Otway Basin. The nodule layer has yielded worn, isolated fossil cetacean elements. Written as Whaler's Bluff Formation in Fig.1.|||||Includes a basal phosphatic nodule bed, fossiliferous clays, oyster beds and sandy limestones.|
19858|Whalers Bluff Formation|61155|5|Briefly described|p18|Pleistocene|Late Pliocene|Relatively thin limestones, marls and clays. Thickness: 130m. Geological Province: Otway Basin. See also p5, p6.||||||
19858|Whalers Bluff Formation|61181|5|Briefly described|p135|Pleistocene|Pliocene|Sandy limestone and lime sand of shallow marine origin, containing oyster beds. Age of the limestone: probably Miocene-Pliocene. Thickness: up to 20m. ||||||
19858|Whalers Bluff Formation|61624|5|Briefly described|p465, p466, p466 Fig. 2|Quaternary|Pliocene|Geological Province: Otway Basin. Equivalents of Hanson Plain Sand, Moorabool Viaduct Formation and Grangeburn Formation. Mixed clastic/carbonate sediments.||||||
19858|Whalers Bluff Formation|62068|5|Briefly described|p135, Fig.2|Pliocene|Pliocene|||||Overlies the Port Campbell and Portland Limestones. Overlain by the Werrikoo Limestone||
19858|Whalers Bluff Formation|62899|6|Mentioned|p42|Pleistocene|Late Pliocene|At Myaring Bridge in south west Victoria.||||||
19858|Whalers Bluff Formation|63446|5|Briefly described|Map legend|Pleistocene|Pleistocene||||||Coastal: sandy limestone, calcarenite, shell beds, marl.|
19858|Whalers Bluff Formation|63739|5|Briefly described|p42|Pleistocene|Late Pliocene|Contains ostracod specimens eg. Rotundracythere sp. at Myaring Bridge in south west Victoria.||||||01-JUL-08
19858|Whalers Bluff Formation|66002|6|Mentioned|p13 Tb.9|||Defined by Boutakoff and Sprigg 1953.||||||
19858|Whalers Bluff Formation|67061|6|Mentioned|p554 Fig.10.|Pliocene|Pliocene|Otway Basin.||||Is overlain by Werriko Limestone.||
19858|Whalers Bluff Formation|68116|5|Briefly described|Appendix, Maps 38, 47.|Pliocene|Pliocene||||||Bioclastic calcarenite with lenses of foraminiferal clay, shelly clay and marl; quartz sand near the base.|
19858|Whalers Bluff Formation|73357|6|Mentioned|p48|Pliocene|Pliocene|Otway Basin.||Of Whalers Bluff Group?||||
73301|Whalers Bluff Supersequence|63134|2|Defined|112|||||||||
73301|Whalers Bluff Supersequence|63269|5|Briefly described|p605|Pleistocene|Pliocene|Otway Basin.||||Overlies Heytesbury Supersequence.||
73301|Whalers Bluff Supersequence|69297|6|Mentioned|p80, p98, p110, p111|||||||||
73301|Whalers Bluff Supersequence|69651|5|Briefly described|p10, p12-15, p17-19, p22, p29, p49-50|Pleistocene|Pliocene|Open marine deposits. Possible seals.||||Overlies Heytesbury Supersequence.|Calcareous claystone overlain by marls, calcarenite and calcilutite; shaly limestone overlain by calcarenite and calcilutite; quartz sandstone overlain by silty mudstone, and limestone.|
73301|Whalers Bluff Supersequence|70077|5|Briefly described|Regional: Fig.4; p4|Holocene|Miocene|Otway Basin.||||Overlies Heytesbury Supersequence.||
73301|Whalers Bluff Supersequence|70078|5|Briefly described|Regional: Fig.4; p3|Holocene|Neogene|||||Overlies Heytesbury Supersequence.|Shelfal marls and limestones.|
73301|Whalers Bluff Supersequence|70880|6|Mentioned|p77|Pleistocene|Pliocene|Otway Basin.||||Overlies Heytesbury Supersequence.||
73301|Whalers Bluff Supersequence|71266|5|Briefly described|p614 Fig.3, p615|Pleistocene|Pliocene|Otway Basin.||||Overlies Heytesbury Supersequence.||
19879|Whisky Creek Granite|34031|6|Mentioned|p277|||||||||
23184|Whisky Knob Rhyolite|23309|5|Briefly described|p36 Table 2.7|||Of the Licola Volcanics.||||||
23184|Whisky Knob Rhyolite|24551|5|Briefly described|p88 Fig. 3.15|||Of  Licola Volcanics (Fig. 3.15).||||||22-DEC-08
23184|Whisky Knob Rhyolite|64535|5|Briefly described|Map legend|Cambrian|Cambrian|Of Licola Volcanic Group.Rhyolite lava, minor rhyolitic volcaniclastics; lava pale green-grey; quartz-phyric; with intercalated crystal-rich sandstone; marine lava flows. ||||||
23184|Whisky Knob Rhyolite|64539|5|Briefly described|Map legend|Cambrian|Cambrian|Of Licola Volcanic Group.Rhyolite lava, minor rhyolitic volcaniclastics; lava pale green-grey; quartz-phyric; with intercalated crystal-rich sandstone; marine lava flows. ||||||
23184|Whisky Knob Rhyolite|64540|5|Briefly described|Map legend|Cambrian|Cambrian|Of Licola Volcanic Group.Rhyolite lava, minor rhyolitic volcaniclastics; lava pale green-grey; quartz-phyric; with intercalated crystal-rich sandstone; marine lava flows. ||||||
23184|Whisky Knob Rhyolite|64605|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Licola Volcanic Group. Rhyolite lava, minor rhyolitic volcaniclastics; marine lavas and volcaniclastics. Red-black in RGB. Non-magnetic to weakly magnetic.||||||17-NOV-08
23184|Whisky Knob Rhyolite|64616|5|Briefly described|p61, p184, p307|Late Cambrian|Middle Cambrian|Of Licola Volcanic Group. Abuts both Tobacco Creek Andesite and Cobbs Spur Andesite Breccia. Contacts probably faulted. Pale green-grey, quartz-phyric rhyolite lava intercalated with minor rhyolitic crystal-rich sandstone. Geophysical characteristics given.||||||
23184|Whisky Knob Rhyolite|66244|5|Briefly described|p2.|Cambrian|Cambrian|Formerly a unit in Licola Volcanic Group (VandenBerg et al. 1995) which has been made redundant.||Unit in Jamieson Volcanic Group.||||
23184|Whisky Knob Rhyolite|68116|5|Briefly described|Appendix, Maps 34, 43.|Cambrian|Cambrian||||||Rhyolite lava, minor rhyolitic volcaniclastics: lava pale green-grey; quartz-phyric; with intercalated crystal-rich sandstone.|
19893|White Hills Gravel|22693|6|Mentioned|P323|||||||||
19893|White Hills Gravel|22756|3|Fully described|P12, P28|Tertiary|Cretaceous|||||||
19893|White Hills Gravel|22886|5|Briefly described|p36|Paleocene|Paleocene|||||||
19893|White Hills Gravel|22971|5|Briefly described|p19, p26|||||||||19-JAN-06
19893|White Hills Gravel|23164|4|Described|p14|Tertiary|Tertiary|||||||
19893|White Hills Gravel|23166|5|Briefly described|Map legend||Oligocene|||||||
19893|White Hills Gravel|23167|5|Briefly described|Map legend||Oligocene|||||||
19893|White Hills Gravel|23168|5|Briefly described|Map legend||Oligocene|||||||
19893|White Hills Gravel|23169|5|Briefly described|Map legend||Oligocene|||||||
19893|White Hills Gravel|23300|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
19893|White Hills Gravel|23302|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
19893|White Hills Gravel|23303|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
19893|White Hills Gravel|23304|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
19893|White Hills Gravel|23305|4|Described|p51|Cenozoic|Late Cretaceous|Of Cherry and Wilkinson (1994). Geological Province: Lachlan Fold Belt.||||||19-NOV-08
19893|White Hills Gravel|23307|5|Briefly described|Map Legend|Paleogene|Paleogene|||||||07-NOV-08
19893|White Hills Gravel|23402|4|Described|p30, p7 Tb. 1|Tertiary|Tertiary|Thickness: 5m. Overlies Glenthompson Sandstone. Geological Province: Adelaide Fold Belt.||||||21-OCT-08
19893|White Hills Gravel|23603|4|Described|p11|Tertiary|Tertiary|||||||
19893|White Hills Gravel|23604|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
19893|White Hills Gravel|23605|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
19893|White Hills Gravel|23606|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
19893|White Hills Gravel|23607|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
19893|White Hills Gravel|24096|6|Mentioned|p4|Mesozoic|Mesozoic|||||||22-APR-05
19893|White Hills Gravel|24103|5|Briefly described|p139 Fig.3, p142|Tertiary|Tertiary|Eary Tertiary.||||||
19893|White Hills Gravel|24104|5|Briefly described|p148, 151|||Underlying unit: Castlemaine Group.||||||09-MAR-05
19893|White Hills Gravel|24105|5|Briefly described|p155|Miocene|Miocene|||||||
19893|White Hills Gravel|24177|4|Described|p69 -71, 61|Paleogene|Paleogene|Overlies the Commissioners Flat Granodiorite. Age: <65 Ma. Maximum Thickness: 20m. Correlate with Wangerrip Group of Otway Basin and Warina Sand (Renmark Group). Geological Province: Murray Basin.||||||06-FEB-15
19893|White Hills Gravel|24178|5|Briefly described|p18|Paleocene|Paleocene|||||||
19893|White Hills Gravel|24219|5|Briefly described|p870|Cenozoic|Cenozoic|||||||19-NOV-08
19893|White Hills Gravel|24326|5|Briefly described|Map legend|Eocene|Late Paleocene|||||||
19893|White Hills Gravel|24328|5|Briefly described|Map legend|Paleogene|Paleogene|||||||07-NOV-08
19893|White Hills Gravel|24329|5|Briefly described|Map legend|Paleogene|Paleogene|||||||07-NOV-08
19893|White Hills Gravel|24383|5|Briefly described|p18|Eocene|Cretaceous|Age: 100 - 50Ma. Geological Province: Lachlan Fold Belt||||||
19893|White Hills Gravel|24384|5|Briefly described|Map legend|Paleocene|Paleocene|Quartz cobble conglomerate.||||||
19893|White Hills Gravel|24385|5|Briefly described|Map legend|Paleocene|Paleocene|Quartz cobble conglomerate.||||||
19893|White Hills Gravel|24386|5|Briefly described|Map legend|Paleocene|Paleocene|Quartz cobble conglomerate.||||||
19893|White Hills Gravel|24387|5|Briefly described|Map legend|Paleocene|Paleocene|Quartz cobble conglomerate.||||||
19893|White Hills Gravel|24388|5|Briefly described|Map legend|Paleocene|Paleocene|Quartz cobble conglomerate; nonmagnetic||||||
19893|White Hills Gravel|24438|5|Briefly described|p34, p35|Cenozoic|Late Cretaceous|Occupies highest terraces adjacent to current stream system, and contains no fossils. Has not been dated, but regional stratigraphic relationships indicate most likely Late Cretaceous to early Cainozoic. Eroded by subsequent streams which formed deep leads which host gold mineralisation.||||Overlain by Newer Volcanic Group lava flows.|Vein quartz conglomerate.|10-MAY-17
19893|White Hills Gravel|24439|4|Described|p8, p15, p36-37|Cenozoic|Cenozoic|Deposited by the earliest recognizable drainage system in the BENDIGO region - possibly Paleocene-Eocene in age? (Hughes and Carey, 2002).  See also p47 Fig. 22 Appendix 2; p60 Appendix 3.||||||19-NOV-08
19893|White Hills Gravel|24440|5|Briefly described|Map legend|||||||||
19893|White Hills Gravel|24470|6|Mentioned|p472|||||||||
19893|White Hills Gravel|24551|5|Briefly described|p415, 417, 418|||||||||
19893|White Hills Gravel|42682|3|Fully described|p23|||Variation on White Hills Gravels.||||||
19893|White Hills Gravel|42683|5|Briefly described|Map legend|Oligocene|Paleocene|||||||
19893|White Hills Gravel|42684|5|Briefly described|Map legend|Eocene|Paleocene|||||||
19893|White Hills Gravel|42685|5|Briefly described|Map legend|Eocene|Paleocene|||||||
19893|White Hills Gravel|43199|5|Briefly described|Map Legend||Paleocene|||||||
19893|White Hills Gravel|43211|4|Described|p4,Fig.5 p15,27-8||Tertiary|||||||
19893|White Hills Gravel|43260|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
19893|White Hills Gravel|43261|5|Briefly described|Map Legend|Paleocene|Cretaceous|||||||
19893|White Hills Gravel|43493|4|Described|28-68|Early Pliocene|Miocene|||||||
19893|White Hills Gravel|43846|5|Briefly described|14||Paleocene|||||||
19893|White Hills Gravel|50080|5|Briefly described|p69 Fig. 1, p70-71|Paleogene|Paleogene|||||||07-NOV-08
19893|White Hills Gravel|50154|5|Briefly described|p133|Eocene|Paleocene|Of the Renmark Group.||||||
19893|White Hills Gravel|50352|5|Briefly described|Map Legend|Tertiary|Tertiary|Of Moorabool Viaduct Formation. Ferruginous quartz sandstone and consolidated gravel.||||||02-JUL-13
19893|White Hills Gravel|60451|5|Briefly described|p30, 95 Fig. 61, 96, 196|Eocene|Cretaceous|Age: 100-50Ma. Maximum Thickness: 30m. Disconformably overlain by: Parilla Sand, Newer Volcanics.||||||02-JUL-13
19893|White Hills Gravel|60452|4|Described|p34|Late Eocene|Early Paleocene|Fluvial deposits. Maximum Age: 65Ma. Maximum Thickness: <10m in WEDDERBURN area. Geological Province: Murray Basin.||||||
19893|White Hills Gravel|60454|5|Briefly described|Map Legend|Paleogene|Paleogene|Fluvial braid plain, outwash fan and colluvial deposits; moderately to well sorted, massive to crudely stratified, cross bedded and channelled.||||||02-JUL-13
19893|White Hills Gravel|60456|5|Briefly described|Map Legend|Paleogene|Paleogene|Fluvial braid plain, outwash fan and colluvial deposits: typically compositionally mature, with ubiquitous well rounded pebbles and cobbles of reef quartz.||||||07-NOV-08
19893|White Hills Gravel|60457|5|Briefly described|Map Legend|Paleogene|Paleogene|Fluvial braid plain, outwash fan and colluvial deposits; typically compositionally mature, with well rounded pebbles and cobbles of reef quartz, lesser vein quartz and bedrock clasts.||||||07-NOV-08
19893|White Hills Gravel|60458|5|Briefly described|Map Legend|Paleogene|Paleogene|Fluvial braid plain, outwash fan and colluvial deposits.||||||07-NOV-08
19893|White Hills Gravel|60459|5|Briefly described|Map Legend|Paleogene|Paleogene|Scattered thin cover unit not depicted on this map.||||||07-NOV-08
19893|White Hills Gravel|60461|5|Briefly described|Map legend|Eocene|Paleocene|River valley deposits and colluvium: subrounded reef quartz and metasediment pebbles and cobbles, grit, coarse-grained sand, clay; commonly kaolinised and ferruginised.||||||02-JUL-13
19893|White Hills Gravel|60491|4|Described|p15, p20|Paleocene|Late Cretaceous|Max. Thickness: 42m. Consists of white, well-rounded vein quartz pebbles, cobbles and boulders with a kaolinitic clay matrix that varies from white to strongly ferruginised.||||||02-JUL-13
19893|White Hills Gravel|60492|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvial: coarse-grained quartz gravel; strongly ferruginised, micaceous, with clayey matrix.||||||27-OCT-08
19893|White Hills Gravel|60493|5|Briefly described|Map Legend|Neogene|Paleogene|Palaeochannels: dendritic magnetic features up to 15 nT.||||||07-NOV-08
19893|White Hills Gravel|60529|5|Briefly described|Map Legend|Eocene|Paleocene|River valley deposits and colluvium: sub-rounded reef quartz and metasediment pebbles and cobbles, minor granite cobbles, grit, coarse grained sand, clay; commonly kaolinised and/or ferruginised.||||||
19893|White Hills Gravel|60581|5|Briefly described|Map Legend|Eocene|Paleocene|Alluvial braid-plain, outwash fan and scree deposits.||||||
19893|White Hills Gravel|60582|5|Briefly described|Map Legend|Eocene|Paleocene|Alluvial braid-plain, outwash fan and scree deposits.||||||23-NOV-04
19893|White Hills Gravel|60583|5|Briefly described|Map Legend|Eocene|Paleocene|Alluvial braid-plain, outwash fan and scree deposits.||||||23-NOV-04
19893|White Hills Gravel|60584|5|Briefly described|Map Legend|Eocene|Paleocene|Alluvial braid-plain, outwash fan and scree deposits.||||||
19893|White Hills Gravel|60585|4|Described|p8, p27|Tertiary|Tertiary|Max thickness: about 30m. Ferruginised, coarse grained, quartz pebble conglomerate.||||||24-NOV-04
19893|White Hills Gravel|60591|5|Briefly described|Map Legend|Paleocene|Paleocene|Unconformably overlies the Castlemaine Supergroup. Rounded to subrounded vein quartz and metasediment pebbles and cobbles, minor granite.||||||
19893|White Hills Gravel|60592|5|Briefly described|Map Legend|Paleocene|Paleocene|Unconformably overlies the Castlemaine Supergroup. Rounded to subrounded vein quartz and metasediment pebbles and cobbles, minor granite.||||||
19893|White Hills Gravel|60593|5|Briefly described|Map Legend|Paleocene|Paleocene|Unconformably overlies the Castlemaine Supergroup. Rounded to subrounded vein quartz and metasediment pebbles and cobbles, minor granite.||||||
19893|White Hills Gravel|60595|5|Briefly described|Map Legend|Paleocene|Paleocene|Unconformably overlies the Castlemaine Supergroup. Rounded to subrounded vein quartz and metasediment pebbles and cobbles, minor granite.||||||
19893|White Hills Gravel|60596|5|Briefly described|Map Legend|Paleocene|Paleocene|Unconformably overlies the Castlemaine Supergroup. Rounded to subrounded vein quartz and metasediment pebbles and cobbles, minor granite.||||||
19893|White Hills Gravel|60597|5|Briefly described|Map Legend|Eocene|Paleocene|River valley deposits and colluvium: nonmagnetic; low K, Th and U||||||
19893|White Hills Gravel|60599|2|Defined|p15, p24 Tb. 4, p83|Early Paleocene|Early Paleocene|Colluvial + fluvial sediments - fine- to med.-gr., well-moderately sorted qtz gravel+sand with intervals of coarse to very coarse quartz conglom.+clay. Unconformable on Wild Duck Fm;disconformable below Newer Volcanics. Thickness details given. Age:~65Ma.||||||10-NOV-08
19893|White Hills Gravel|61160|6|Mentioned|p91|||Fringes the southern margins of Murray Basin. ||||||
19893|White Hills Gravel|61183|6|Mentioned|p13|||||||||
19893|White Hills Gravel|61185|2|Defined|p53, p56-57, p15|Middle Eocene|Early Paleocene|Parts previously referred to as "Mangalore Gravel" (south of Mangalore Airport). Outcrops poorly. Over Wilson Creek Shale and Waranga Fm (ang. unconformity). Max age: ~65 Ma. Thick: ~10m. Geol.Prov: LFB. Colluvial and fluvial palaeovalley sediments.||||||07-FEB-11
19893|White Hills Gravel|61701|5|Briefly described|Map Legend|Eocene|Paleocene|River valley deposits and colluvium: sub-rounded reef quartz and metasediment pebbles and cobbles, minor granite cobbles, grit, coarse grained sand, clay; commonly kaolinised and/or ferruginised.||||||25-JUL-06
19893|White Hills Gravel|61702|5|Briefly described|Map Legend|Eocene|Paleocene|River valley deposits and colluvium: sub-rounded reef quartz and metasediment pebbles and cobbles, minor granite cobbles, grit, coarse grained sand, clay; commonly kaolinised and/or ferruginised.||||||25-JUL-06
19893|White Hills Gravel|61703|5|Briefly described|Map Legend|Eocene|Paleocene|River valley deposits and colluvium: sub-rounded reef quartz and metasediment pebbles and cobbles, minor granite cobbles, grit, coarse grained sand, clay; commonly kaolinised and/or ferruginised.||||||25-JUL-06
19893|White Hills Gravel|61704|6|Mentioned|Map legend|Neogene|Paleogene|Low K and Th.||||||12-FEB-15
19893|White Hills Gravel|62370|5|Briefly described|p447, p455|Eocene|Paleocene|Comprise ferruginised, silicified, coarse-grained quartz conglomerate with a framework of moderately to well-sorted, well-rounded, vein quartz grains up to cobble size, with minor angular vein quartz; rare bedrock clasts that are typically kaolinised.||||||
19893|White Hills Gravel|64314|5|Briefly described|p494, p502|Late Cretaceous||Coded as WHG in Figure 7. See also p496.||||||21-OCT-08
19893|White Hills Gravel|64612|4|Described|p28|Cainozoic|Cainozoic|Described as uphill extension of Renmark Group. Unclear if White Hills Gravel intended to be included in Renmark Group or considered a lateral/time equivalent. Quartz-rich gravel. Deposited by braided rivers. Underlain by Paleozoic bedrock. Geological Province: Murray Basin.||||||06-FEB-15
19893|White Hills Gravel|65715|4|Described|p11-12, p11 Tb.7, p26, 27, p38|Paleogene|Paleogene|Ferruginised gravel. Type locality at White Hills, N of Bendigo (MGA ref given). ~10 m thick in type area. Unconformably overlies Paleozoic bedrock in the Bendigo district. Overlies Castlemaine Group. May be older than Werribee Formation. May be laterally continuous with Yaloak Formation and possibly as old as Maastrichtian. Older than Calivil Formation.||||||
19893|White Hills Gravel|65969|5|Briefly described|p27 Tb.3.3, p30-1|Oligocene|Eocene|Murray Basin. Quartz and lithic gravel, sand and silt. Unconformable on Paleozoic basement. Found in the bases of valleys and along ridge crests where silicified. No magnetic response; low radiometric response in all channels. Source of much gold won from deep leads.||||||
19893|White Hills Gravel|66002|5|Briefly described|p10 Tb.7, p12|Paleogene|Paleogene|Defined by Cherry and Wilkinson 1994.See also VandenBerg 2009.Some outcrops previously assigned to 'Eastern Viewer [sic] Formation' in Willaura 1:100k area. Extent exaggerated in St Arnaud region. ||||||
19893|White Hills Gravel|66012|4|Described|p4-5, p10 Tb.1, p11, p13-14, p16-17, p19|Paleogene|Cretaceous|Unconformably overlies Pyrenees Formation & Mount Bute Granite. Disconformably overlies Lismore Granodiorite. Massive quartz-gravel beds with boulders up to 1m & thickly bedded & cross-bedded brown, ferruginous sandstone. 5m thick. Fluvial| | | | | |13-JUN-13
19893|White Hills Gravel|68116|5|Briefly described|Appendix, Maps 16, 22-25, 30-33, 39-41.|Oligocene|Paleocene|Outwash fan and colluvial deposits. Crossbedded and channelled; richly auriferous in places; variably ferruginised, silicified or kaolinised.|||||Vein quartz conglomerate, sand, silt, clay (fluvial braid plain); compositionally mature, well-rounded pebbles and cobbles of reef quartz, lesser angular vein quartz and bedrock clasts; moderately to well sorted, massive to crudely stratified. |
19893|White Hills Gravel|68189|5|Briefly described|p26, p27 Tb.3.2, p28 Fig.14, p29, p33|Oligocene|Eocene|Birch and Barron (1997) recorded a single 0.5 carat diamond found in the White Hills Gravel. An upstream time equivalent of the Olney Formation in ST ARNAUD. Younger parts are magnetic, whilst older parts have distinctly low radiometeric responses. Braided river channel deposits.||||Non-conformably overlain by the Calivil Formation.|Comprises pebbles, cobbles and coarse sand of quartz and metasedimentary rock; often silcrete.|
19893|White Hills Gravel|68194|5|Briefly described|p26, p31, p36, p55|Cretaceous|Cretaceous|Cayley and Taylor (2001). Deposition by braided rivers.|||||Quartz-rich sediment.|
19893|White Hills Gravel|71408|6|Mentioned|p1027|Paleocene|Eocene|Bendigo region. Fluvial gravels are quartz-dominated unlike the catchment geology.||||||
19893|White Hills Gravel|71593|6|Mentioned|p44|Cenozoic|Cenozoic|||||||
19893|White Hills Gravel|73497|5|Briefly described|Map legend|Paleogene|Paleogene||||||Alluvium: nonmagnetic; low K, Th and U.|
19893|White Hills Gravel|73576|5|Briefly described|p802|Paleogene|Paleogene|Partially covers Tarnagulla Granodiorite.|||||Alluvium.|
68411|White Monkey Volcanic Group|24551|5|Briefly described|p141 Fig. 5.32|||||||||
68411|White Monkey Volcanic Group|68115|6|Mentioned|p5.|Devonian|Devonian|Formerly given Group status as White Monkey Volcanics (VandenBerg et al. (2000); now formally named White Monkey Volcanic Group.||||||
68411|White Monkey Volcanic Group|68116|5|Briefly described|Appendix, Map 36,|Early Devonian|Early Devonian||||||Felsic ignimbrite, minor conglomerate, sandstone.|
37614|White Rabbit Diorite|23309|5|Briefly described|p227|||G389||||||
37614|White Rabbit Diorite|24221|5|Briefly described|p907|Devonian|Devonian|||||||
37614|White Rabbit Diorite|60451|4|Described|p45, 46, 92, 195|Early Devonian|Early Devonian|Of the Stawell Pluton. Type section in text. Intrudes the Lexington Schist & Good Morning Bill Schist. Ranges in composition from diorite to granite.||||||
37614|White Rabbit Diorite|60458|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Biotite-hornblende-quartz diorite; pale grey; medium grained; contains pyroxene; oxidised.||||||
37614|White Rabbit Diorite|60459|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Ararat Suite. Biotite-hornblende-quartz diorite: oxidised.||||||
37614|White Rabbit Diorite|66002|5|Briefly described|p7 Tb.5|||Of Ararat Suite in Stawell Pluton area. G389. Defined by Cayley and Taylor 2001.||||||
37614|White Rabbit Diorite|68116|5|Briefly described|Appendix, Map 30.|Early Devonian|Early Devonian||||||Biotite-hornblende-quartz diorite: pale grey; medium grained; contains pyroxene; oxidised, highly magnetic.|
37614|White Rabbit Diorite|71593|6|Mentioned|p139, p148|Early Devonian|Early Devonian|||||||
69399|White Star Sandstone|64535|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Pale grey sandstone, thick to thin bedded; Tabc, Tbc and Tc turbidites; quartz-rich, medium- to fine-grained; dark grey to black siltstone, thin bedded, well laminated to shaly; deep-marine turbidite fan deposits. ||||||
69399|White Star Sandstone|64539|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Pale grey sandstone, thick to thin bedded; Tabc, Tbc and Tc turbidites; quartz-rich, medium- to fine-grained; dark grey to black siltstone, thin bedded, well laminated to shaly; deep-marine turbidite fan deposits. ||||||
69399|White Star Sandstone|64540|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Pale grey sandstone, thick to thin bedded; Tabc, Tbc and Tc turbidites; quartz-rich, medium- to fine-grained; dark grey to black siltstone, thin bedded, well laminated to shaly; deep-marine turbidite fan deposits. ||||||
69399|White Star Sandstone|64605|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Walhalla Group. Sandstone, siltstone; deep-marine deposits. Speckled blue-pink in RGB. Nonmagnetic.||||||
69399|White Star Sandstone|64616|4|Described|p14 Table 1.1, p105, p295, p303|Early Devonian|Early Devonian|Unit in Walhalla Group. See also White Star Formation (p107).  Also used on maps. Type section details given. Quartz-rich to quartzitic, well-bedded and turbiditic; interbedded with dark grey laminated siltstone. Geophysical characteristics given.||||||
30511|Whitegum Tonalite|22878|4|Described|p77|||||||||
30511|Whitegum Tonalite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Biotite-minor hornblende tonalite: grey, medium grained, massive; conspicious quartz grains, mafic inclusions and porphyritic dykes.||||||01-OCT-04
30511|Whitegum Tonalite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Biotite-minor hornblende tonalite: grey, medium grained, massive; conspicuous quartz grains, mafic inclusions and porphyritic dykes.||||||26-JUN-14
30511|Whitegum Tonalite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Glenbog Supersuite. Biotite-minor hornblende tonalite: Moderately magnetic (120-125 nT). High K, low Th and U.||||||06-OCT-04
30511|Whitegum Tonalite|23309|6|Mentioned|p447 App1|||G530.||||||
30511|Whitegum Tonalite|68116|5|Briefly described|Appendix, Map 37.|Early Devonian|Early Devonian||||||Biotite - minor hornblende tonalite: grey, medium grained, massive; conspicuous quartz grains; mafic inclusions and porphyritic dykes; I-type.|
30511|Whitegum Tonalite|68592|6|Mentioned|p1674|Early Devonian|Early Devonian|||Unit in Glenbog Supersuite.||||
19921|Whitelaw Siltstone|22570|6|Mentioned|p189|Pragian|Lochkovian|||||||
19921|Whitelaw Siltstone|22971|6|Mentioned|p 22|||Jordan River Group.||||||22-DEC-08
19921|Whitelaw Siltstone|23229|4|Described|Table3-3p27, 32|Pragian|Ludlow|||||||
19921|Whitelaw Siltstone|23265|6|Mentioned|p341||Early Devonian|||||||
19921|Whitelaw Siltstone|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Jordan River Group.||||||22-DEC-08
19921|Whitelaw Siltstone|23309|5|Briefly described|p143-145, 148, 155, 173. Table 2.54|||||||||
19921|Whitelaw Siltstone|23522|5|Briefly described|p247 Fig 3|Early Devonian|Silurian|||||||
19921|Whitelaw Siltstone|24177|5|Briefly described|p50 Fig.22|Early Devonian|Late Silurian|Geological Province: Mount Easton Province.||||||
19921|Whitelaw Siltstone|24588|5|Briefly described|p20|Devonian|Silurian|Underlies Eildon Sandstone conformably. See also Whitlaw Siltstone p12 Fig. 3.||||||29-NOV-13
19921|Whitelaw Siltstone|33601|2|Defined|p9|Early Devonian|Late Silurian|Late Silurian - Early Devonian.||||||22-DEC-08
19921|Whitelaw Siltstone|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
19921|Whitelaw Siltstone|35073|5|Briefly described|Table 1.|||||||||
19921|Whitelaw Siltstone|35283|4|Described|p53|||||||||
19921|Whitelaw Siltstone|36389|6|Mentioned|p41|||||||||
19921|Whitelaw Siltstone|38787|6|Mentioned|Fig.2|||||||||
19921|Whitelaw Siltstone|39551|6|Mentioned|Map legend|Lochkovian|Pridolian|Lochkovian to Pridolian.||||||22-DEC-08
19921|Whitelaw Siltstone|39555|6|Mentioned|Map legend|Lochkovian|Pridolian|Lochkovian to Pridolian||||||
19921|Whitelaw Siltstone|41585|4|Described|p112|||||||||
19921|Whitelaw Siltstone|42827|4|Described|p112|||see also Table 4.1||||||
19921|Whitelaw Siltstone|42938|5|Briefly described|p576 Fig.3|||||||||
19921|Whitelaw Siltstone|44187|5|Briefly described|Map Legend||Late Silurian|||||||
19921|Whitelaw Siltstone|60599|5|Briefly described|p47 Fig. 19|Lochkovian|Pridolian|Geological Province: Mount Easton Province, Melbourne Zone, Lachlan Fold Belt.||||||
19921|Whitelaw Siltstone|61185|5|Briefly described|p37, p21 Fig. 6|Lochkovian|Pridolian|Of Jordan River Group (VandenBerg, 1975). Overlies Sinclair Valley Sandstone; underlies Boola Formation, Eildon Sandstone and Wilson Creek Shale. Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
19921|Whitelaw Siltstone|62099|5|Briefly described|p331|Early Devonian|Silurian|In western Melbourne Zone of the Lachlan Orogen. ||||||
19921|Whitelaw Siltstone|64535|5|Briefly described|Map legend|Early Devonian|Late Silurian|Of Jordan River Group. Siltstone, generally finely banded/bioturbated, upper parts often without lamination - rare mass-flow deposits with shelly fossils; pale sandstone thin to v. thinly bedded, quartzitic; deep-marine hemipelagic and turbidite deposits.||||||22-DEC-08
19921|Whitelaw Siltstone|64536|5|Briefly described|Map legend|Early Devonian|Late Silurian|Of Jordan River Group. Siltstone, generally finely banded/bioturbated, upper parts often without lamination - rare mass-flow deposits with shelly fossils; pale sandstone thin to v. thinly bedded, quartzitic; deep-marine hemipelagic and turbidite deposits.||||||07-FEB-11
19921|Whitelaw Siltstone|64537|5|Briefly described|Map legend|Early Devonian|Late Silurian|Of Jordan River Group. Siltstone, generally finely banded/bioturbated, upper parts often without lamination - rare mass-flow deposits with shelly fossils; pale sandstone thin to v. thinly bedded, quartzitic; deep-marine hemipelagic and turbidite deposits.||||||07-FEB-11
19921|Whitelaw Siltstone|64538|5|Briefly described|Map legend|Early Devonian|Late Silurian|Of Jordan River Group. Siltstone, generally finely banded/bioturbated, upper parts often without lamination - rare mass-flow deposits with shelly fossils; pale sandstone thin to v. thinly bedded, quartzitic; deep-marine hemipelagic and turbidite deposits.||||||07-FEB-11
19921|Whitelaw Siltstone|64539|5|Briefly described|Map legend|Early Devonian|Late Silurian|Of Jordan River Group. Siltstone, generally finely banded/bioturbated, upper parts often without lamination - rare mass-flow deposits with shelly fossils; pale sandstone thin to v. thinly bedded, quartzitic; deep-marine hemipelagic and turbidite deposits.||||||22-DEC-08
19921|Whitelaw Siltstone|64540|5|Briefly described|Map legend|Early Devonian|Late Silurian|Of Jordan River Group. Siltstone, generally finely banded/bioturbated, upper parts often without lamination - rare mass-flow deposits with shelly fossils; pale sandstone thin to v. thinly bedded, quartzitic; deep-marine hemipelagic and turbidite deposits.||||||22-DEC-08
19921|Whitelaw Siltstone|64605|5|Briefly described|Map legend|Early Devonian|Silurian|Of the Jordan River Group. Siltstone, minor sandstone, siltstone; deep-marine deposits. Dark to light green and light blue-pink to white in RGB. Nonmagnetic.||||||17-NOV-08
19921|Whitelaw Siltstone|64606|5|Briefly described|Map Legend|Silurian|Silurian|Of Jordan River Group. Siltstone, minor sandstone: deep-marine deposits. Dark to light green and light blue-pink to white in RGB. Nonmagnetic.||||||
19921|Whitelaw Siltstone|64616|3|Fully described|p87, p166 Fig.6.13, p169 Fig.6.16, p173|Early Devonian|Early Devonian|See also p183 Fig.6.29, p197 Fig.6.34, p201 Tb.7.1, p203 Fig.7.3, p285, p287-288, p290, p293, p304. Of Jordan River Group. Gradational contact with underlying Sinclair Valley Sandstone. Overlain by Eildon Sandstone, Wilson Creek Shale (gradationally) and Boola Formation. 250-1200m thick. Age from Monograptus sp. at one location. Massive grey siltstone with fine banding and bioturbation; sporadic thin pale sandstone beds. Geophysical characteristics given.||||||
19921|Whitelaw Siltstone|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Walhalla. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
19921|Whitelaw Siltstone|68116|5|Briefly described|Appendix, Maps 25, 33-34, 42-43, 51-52.|Pragian|Ludlow||||||Siltstone, minor sandstone: siltstone dark grey; generally finely banded and bioturbated; uppermost portion often without lamination; rare mass-flow deposits with shelly fossils; sandstone thin to very thin-bedded; pale; quartzitic.|
37792|Whitimaria Granite|23309|6|Mentioned|p447, Appendix 1|||G623||||||
37792|Whitimaria Granite|60491|4|Described|p53|||Of the Nine Mile Suite. Previously included in the Jeffcott Granite (King, 1976). Intrudes the Jeffcott Granite. I-type.||||||
37792|Whitimaria Granite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Nine Mile Suite. Leucocratic muscovite granite: pale grey, medium grained; very poorly exposed.||||||
37792|Whitimaria Granite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of Nine Mile Suite. Granite; oxidised I-type: generally low radiometric response; G623a: highly magnetic (to 140 nT); G623b: nonmagnetic core.||||||30-SEP-04
37792|Whitimaria Granite|66002|5|Briefly described|p6 Tb.5|||Of Nine Mile Suite. G623. Defined in Bibby and Moore 1998.||||||
37792|Whitimaria Granite|68116|5|Briefly described|Appendix, Map 16.|Early Devonian|Early Devonian||||||Leucocratic muscovite granite: pale grey, medium grained; very poorly exposed.|
75877|Whiting Formation|70028|6|Mentioned|p79|Pleistocene|Miocene|Offshore Gippsland Basin.||||||
75877|Whiting Formation|70076|5|Briefly described|South-Eastern: Fig.2; Regional: Fig.3|Pliocene|Miocene|||Hapuku Subgroup.||Overlies Cod Formation.||
75951|Whitlands Volcanic Group|68115|5|Briefly described|p9.|Cenozoic|Cenozoic|New name. Replaces the former Older Volcanic Group in the Whitlands-Toombullup area. Lies within the Toombullup Subprovince of Price et al. (2003). Several flows on ridge tops cover large areas and may be subdivided into Formations with more detailed mapping.|||||Lava flows of basanite, alkali olivine basalt, hawaiite and olivine tholeiite.|
75951|Whitlands Volcanic Group|68116|5|Briefly described|Appendix, Maps 19, 26.|Priabonian|Lutetian||||||Basalt lava flows: basanite, alkali olivine basalt, hawaiite and olivine tholeiite.|
24102|Wibenduck Limestone|22876|6|Mentioned|p14|||||||||
24102|Wibenduck Limestone|22877|5|Briefly described|map|Silurian|Silurian|||||||
24102|Wibenduck Limestone|23309|5|Briefly described|p92-97. Table 2.34||Silurian|||||||
24102|Wibenduck Limestone|23615|5|Briefly described|p20 Fig.6|Ludlow|Ludlow|Geological Province: Lachlan Fold Belt.||||||
24102|Wibenduck Limestone|24551|5|Briefly described|p120|||||||||
24102|Wibenduck Limestone|41585|4|Described|p131|||||||||
24102|Wibenduck Limestone|42627|5|Briefly described|Map legend|Ludlow||||||||
24102|Wibenduck Limestone|42635|6|Mentioned|p24|||Silurian||||||
24102|Wibenduck Limestone|42647|2|Defined|p28|Ludlow||Supersedes Sardine beds, in part. Age: Late Silurian (late Ludlow)||||||
24102|Wibenduck Limestone|42827|4|Described|p131|||see also Table 4.1||||||
24102|Wibenduck Limestone|43228|5|Briefly described|p9||Late Silurian|||||||
24102|Wibenduck Limestone|50096|6|Mentioned|p78|||Occurrence of Ozarkodina martinssoni auriformis (conodont).||||||
24102|Wibenduck Limestone|61181|5|Briefly described|p124|Silurian|Silurian|Of VandenBerg (1988). Small body of limestone originally included within the Sardine Conglomerate. Sparse fossils suggest a Silurian age.||||||
24102|Wibenduck Limestone|61186|5|Briefly described|p91 Fig. 44|||Limestone, massive, recrystallised, dark-grey to bluish in colour. ||||||
37272|Wickham metamorphics|24002|5|Briefly described|p236|Mesoproterozoic|Mesoproterozoic|Informal name. Underlie the Currie Group on King Island.||||||17-JAN-06
19980|Wickliffe Rhyolite|22768|5|Briefly described|Map15p148,166||Pridoli|Max Age: 410 Ma||||||
19980|Wickliffe Rhyolite|22857|6|Mentioned|p166|Early Devonian|Late Silurian|Felsic volcanics. Age: 410Ma.||||||
19980|Wickliffe Rhyolite|23229|6|Mentioned|p25|||||||||
19980|Wickliffe Rhyolite|23402|3|Fully described|p24, p7 Tb. 1|Silurian|Silurian|Previously correlated with Rocklands Rhyolite (Spencer-Jones, 1988; Simpson & Woodful, 1994).   Intrudes Glenthompson Sandstone as dykes.   Unconformable overlain by Willaura Sandstone.   Geological Province: Adelaide Fold Belt||||||
19980|Wickliffe Rhyolite|33602|6|Mentioned|Table 1|||||||||
19980|Wickliffe Rhyolite|33608|6|Mentioned|p45|||||||||
19980|Wickliffe Rhyolite|35112|6|Mentioned|Table.1|||||||||
19980|Wickliffe Rhyolite|38367|6|Mentioned|Fig.1|||||||||
19980|Wickliffe Rhyolite|39291|4|Described|p214|||||||||
19980|Wickliffe Rhyolite|39331|6|Mentioned|Fig.0-3|||||||||
19980|Wickliffe Rhyolite|39967|5|Briefly described|p33|||||||||
19980|Wickliffe Rhyolite|40172|6|Mentioned|Map legend|Silurian|Silurian|||||||
19980|Wickliffe Rhyolite|40887|3|Fully described|p24|||||||||
19980|Wickliffe Rhyolite|41585|6|Mentioned|p141|||||||||
19980|Wickliffe Rhyolite|42726|5|Briefly described|map legend|||||||||
19980|Wickliffe Rhyolite|42827|5|Briefly described|Fig 4.10|||||||||
19980|Wickliffe Rhyolite|43753|6|Mentioned|p621|||||||||
19980|Wickliffe Rhyolite|61180|5|Briefly described|p5|Early Devonian|Silurian|Overlies Saint Arnaud Beds.||||||
19980|Wickliffe Rhyolite|61187|6|Mentioned|p69, p130.|Silurian|Silurian|Glenelg Zone. Dykes.||||||
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.|
69396|Wild Dog Chert|64536|5|Briefly described|Map legend|Early Devonian|Late Silurian|Dark grey chert, massive to bedded; contains radiolaria. Deep-marine hemipelagic deposits.||||||07-FEB-11
69396|Wild Dog Chert|64537|5|Briefly described|Map legend|Early Devonian|Late Silurian|Dark grey chert, massive to bedded; contains radiolaria. Deep-marine hemipelagic deposits.||||||07-FEB-11
69396|Wild Dog Chert|64538|5|Briefly described|Map legend|Early Devonian|Late Silurian|Dark grey chert, massive to bedded; contains radiolaria. Deep-marine hemipelagic deposits.||||||07-FEB-11
69396|Wild Dog Chert|64606|5|Briefly described|Map Legend|Cambrian|Cambrian|Chert: deep-marine deposits. Blue in RGB. Nonmagnetic.||||||
69396|Wild Dog Chert|64616|3|Fully described|p63, p178-179, p181 Fig.6.28, p182-183|Late Cambrian|Middle Cambrian|See also p197 Fig.6.34, p204, p281-282, p306. New name. Faulted contact with Licola Volcanic Group rocks. Gradationally overlies Wahroonga Breccia. Age inferred. Minimum thickness 200 m at type section. Dark grey, massive to bedded, chert; quartz, graphite and pyrite are practically the only minerals in this rock; contains radiolaria. Bedding extremely rare. Appears as Wild Dog Rocks Chert on p69 and Fig.6.28. Geophysical characteristics given.||||||
69396|Wild Dog Chert|68116|5|Briefly described|Appendix, Map 25.|Early Ordovician|Late Cambrian||||||Chert: dark grey; massive to bedded; contains radiolaria.|
69396|Wild Dog Chert|70601|5|Briefly described|p44|Warendan|Idamean|Licola area.||||Underlies Phosphate Hill Formation. Overlies Wahroonga Breccia.||
20013|Wild Horse Formation|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
20013|Wild Horse Formation|23309|5|Briefly described|p104, 133. Table 2.38|||||||||
20013|Wild Horse Formation|23522|5|Briefly described|p247 Fig 3|Early Devonian|Early Devonian|||||||
20013|Wild Horse Formation|23710|14|Not recorded|p74|||Poorly preserved fauna.||||||
20013|Wild Horse Formation|24551|4|Described|p138|||Of the Wentworth Group.||||||
20013|Wild Horse Formation|31161|5|Briefly described|PA10|||||||||
20013|Wild Horse Formation|32399|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
20013|Wild Horse Formation|33393|6|Mentioned|p163|||||||||
20013|Wild Horse Formation|33602|6|Mentioned|p26|||||||||
20013|Wild Horse Formation|33603|6|Mentioned|Map legend|Devonian|Devonian|||||||
20013|Wild Horse Formation|33606|4|Described|p67|||||||||
20013|Wild Horse Formation|37330|5|Briefly described|p17|||||||||
20013|Wild Horse Formation|41585|4|Described|p132|||Mention Fig.4.9||||||
20013|Wild Horse Formation|42577|5|Briefly described|Fig.3, P28|||||||||
20013|Wild Horse Formation|42827|4|Described|p132|||see also Table 4.1||||||
20013|Wild Horse Formation|43461|14|Not recorded|p628|||||||||
20013|Wild Horse Formation|43547|14|Not recorded|p154||Early Devonian|||||||
20013|Wild Horse Formation|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Unit in Wentworth Group.|||Transgressive: conglomerate, pebbly sandstone, quartzite.|
20013|Wild Horse Formation|61161|5|Briefly described|p114-118, p76-77 Fig 6.1|||Basal formation of Wentworth Group. Underlies Tabberabbera Formation - transitional boundary. Pebbly sandstone and microconglomerate: largely quartz; High-angle unconformity with underlying Pinnak Sandstone. Max thick: 250m. GSV map code: Dww.||||||
20013|Wild Horse Formation|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Wentworth Group. Conglomerate, sandstone, rare mudstone: quartz conglomerate; rare thin interbeds of fine-grained sandstone and mudstone; fluvial deposits. GSV map code: Dww.||||||
20013|Wild Horse Formation|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Wentworth Group. Conglomerate, sandstone, rare mudstone: quartz conglomerate; rare thin interbeds of fine-grained sandstone and mudstone; fluvial deposits. GSV map code: Dww.||||||07-FEB-11
20013|Wild Horse Formation|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Wentworth Group. Conglomerate, sandstone, rare mudstone: quartz conglomerate; rare thin interbeds of fine-grained sandstone and mudstone; fluvial deposits. GSV map code: Dww.||||||
20013|Wild Horse Formation|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Wentworth Group. Conglomerate, sandstone, rare mudstone: quartz conglomerate; rare thin interbeds of fine-grained sandstone and mudstone; fluvial deposits. GSV map code: Dww.||||||
20013|Wild Horse Formation|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Wentworth Group. Conglomerate, sandstone, rare mudstone: moderate gravity response (-330 to -300 ums^-2); nonmagnetic to weakly magnetic (60 nT, k up to 20 x10^-6 cgs); moderate K, low to moderate Th, U and total radioelements. GSV map code: Dww.||||||
20013|Wild Horse Formation|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Tabberabbera. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
20013|Wild Horse Formation|66197|5|Briefly described|p634|Early Devonian|Early Devonian|Of Wentworth Group. Conglomerate, thinning southwards and eastwards, implying a western derivation.||||||14-MAR-12
20013|Wild Horse Formation|68116|5|Briefly described|Appendix, Maps 35, 44.|Early Devonian|Early Devonian|Includes rare thin interbeds of fine-grained sandstone and mudstone.|||||Conglomerate, sandstone, rare mudstone: quartz conglomerate fine-grained with minor lithic pebbles; crudely- to thick-bedded; includes very coarse to coarse sandstone of same composition; tabular(?) cross bedding; channel forms.|
20013|Wild Horse Formation|71040|5|Briefly described|p11|||Thins eastward.|||||Conglomerate.|
20050|Wilkie Sandstone Member|35283|6|Mentioned|p54|||||||||
20050|Wilkie Sandstone Member|41585|5|Briefly described|p111|||||||||
20050|Wilkie Sandstone Member|42827|5|Briefly described|p111|||Of Killingworth Formation.||||||27-OCT-08
20050|Wilkie Sandstone Member|60599|6|Mentioned|p56|||Of Garratt 1986).  See also Wilkie Member. ||||||
20050|Wilkie Sandstone Member|61185|6|Mentioned|p45|||Of Garratt (1986). Probable continuation of Flowerdale Sandstone Member (Garrat 1986). See also Wilkie Member and Wilke Member.||||||07-FEB-11
20055|Wilkinson Creek Conglomerate|23309|4|Described|p112 Table 2.40|||Of the Timbarra Subgroup.  Maximum Thickness:~500m.||||||
20055|Wilkinson Creek Conglomerate|23615|3|Fully described|p87, p22|Early Devonian|Early Devonian|Of Timbarra Subgroup.  Overlain by Windarra Formation. See also p211 App.2.  Type section is in Wilkinson Creek west of Windarra. Age:410-395Ma.||||||
20055|Wilkinson Creek Conglomerate|24551|4|Described|p142|||Of the Timbarra Subgroup.||||||
20055|Wilkinson Creek Conglomerate|41585|6|Mentioned|p135|||||||||
20055|Wilkinson Creek Conglomerate|42827|5|Briefly described|p135|||||||||
20055|Wilkinson Creek Conglomerate|43206|5|Briefly described|map legend||Ludlow|Timbarra Subgroup||||||
20055|Wilkinson Creek Conglomerate|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Sedolithic conglomerate, breccia; pebbles of quartzite, sandstone, minor granite, shale, chert; minor medium to coarse grained sandstone; poorly bedded; pebbly sandstone interbeds.|
24575|Williamsons Road Serpentinite|23229|6|Mentioned|p16|||Intrusion?||||||
24575|Williamsons Road Serpentinite|23309|6|Mentioned|p378|||||||||
24575|Williamsons Road Serpentinite|24551|5|Briefly described|p78|||Of the Mount Stavely Volcanic Complex.||||||
24575|Williamsons Road Serpentinite|38436|4|Described|p425|||See also Fig.2.||||||
24575|Williamsons Road Serpentinite|40172|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
24575|Williamsons Road Serpentinite|40761|5|Briefly described|Table 1|||||||||
24575|Williamsons Road Serpentinite|40887|2|Defined|p20|Cambrian|Cambrian|Prob. Cambrian||||||
24575|Williamsons Road Serpentinite|41571|5|Briefly described|p39|||||||||
24575|Williamsons Road Serpentinite|42827|5|Briefly described|p39|||of Mount Stavely Volcanic Complex||||||
24575|Williamsons Road Serpentinite|50371|5|Briefly described|Map Legend|Cambrian|Cambrian|Of Mount Stavely Volcanic Complex.||||||
24575|Williamsons Road Serpentinite|60454|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt. Of the Dimboola Igneous Complex. Unit does not appear on this map.||||||27-MAY-13
24575|Williamsons Road Serpentinite|60456|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt. Of the Dimboola Igneous Complex. Serpentinite; serpentine-chromite-quartz-magnetite rock.||||||27-MAY-13
24575|Williamsons Road Serpentinite|60457|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Dimboola Igneous Complex. Geological Province: Delamerian Fold Belt. Unit does not appear on this map.||||||27-MAY-13
24575|Williamsons Road Serpentinite|60458|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Dimboola Igneous Complex. Unit does not appear on this map.||||||15-OCT-04
24575|Williamsons Road Serpentinite|60459|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Delamerian Fold Belt. Of the Dimboola Igneous Complex. Serpentinite.||||||27-MAY-13
24575|Williamsons Road Serpentinite|61187|5|Briefly described|p69 Fig.2, p130.|Early Cambrian|Early Cambrian|Produces narrow, linear, NNW-trending high magnetic responses.||Unit in Mount Stavely Volcanic Complex.||||
24575|Williamsons Road Serpentinite|68116|5|Briefly described|Appendix, Map 39.|Cambrian|Cambrian||||||Serpentinite: serpentine-chromite-quartz-magnetite rock; highly magnetic.|
24575|Williamsons Road Serpentinite|70211|6|Mentioned|p1, p21|||A slice is fault-emplaced into the Mount Stavely Volcanic Complex.||||||
24575|Williamsons Road Serpentinite|70877|5|Briefly described|p10-11|||Grampians-Stavely Zone.|||||Ultramafic-tholeiite boninite.|
24575|Williamsons Road Serpentinite|70967|6|Mentioned|p9, 28, 41|||Stavely Arc. Occurs as narrow fault slices.|||||Serpentinised peridotite.|
24575|Williamsons Road Serpentinite|71593|5|Briefly described|p9, p12, p23, p29, p72, p95|||Grampians-Stavely Zone. Appears as Williams Road Serpentinite on p9. Intersected in a number of drillholes in the region. See also  p102, p122, p127, p133, p137, p150, p163, p172, p188, p199.||Mount Stavely Volcanic Complex|||Serpentinised ultramafic rocks.|
24575|Williamsons Road Serpentinite|72445|5|Briefly described|p8; App.1, App 2.|||App.2 is a .csv format file.  Identified in Stavely 10.||Mount Stavely Volcanic Complex||Overlain by Renmark Group with sharp contact.|Includes sheared, foliated serpentinite breccia with clasts of mafic igneous rock, red mudstone, serpentinite and fractured quartz veins. Highly fractured and rubbly. Rare ultramafic rocks consisting of serpentinised peridotite.|
32501|Willimigongong Ignimbrite|22886|5|Briefly described|p15|||||||||
32501|Willimigongong Ignimbrite|23309|5|Briefly described|p170, 347|||||||||
32501|Willimigongong Ignimbrite|24551|5|Briefly described|p160|||Same as Mount Macedon Dacite of Mikucki (1991), both authors referring to the Upper Volcanic series of the Mount Macedon Igneous Complex.||||||08-OCT-10
32501|Willimigongong Ignimbrite|44197|5|Briefly described|Map Legend||Late Devonian|||||||
32501|Willimigongong Ignimbrite|64619|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Macedon Volcanics Group.  Biotite-enstatite rhyodacite ignimbrite; dense blue-black, medium-grained, massive, recrystallised, pyroclastic deposits.||||||
32501|Willimigongong Ignimbrite|65715|3|Fully described|p5-6, p7 Tb.4, p25 Fig.1a|Devonian|Devonian|Of Macedon Igneous Complex. Overlies Hesket Ignimbrite. Name adapted from Willimigongong Dacites (Gregory, 1902) and Willimigongong Creek Dacite (Summers, 1914). Phenocryst-rich, dark grey, medium-grained enstatite-feldspar ignimbrite. Type locality is a large road cutting on Anzac Road, Macedon (MGA ref given), on the E side of Macedon Creek. Outcrops over ~30 sq. km. Contact with Castlemaine Group is inferred to be faulted. Contact with Kerrie Group is possibly unconformable. Thickness at least 400 m but may be much thicker.||||Intruded  and metamorphosed by Barringo Granodiorite.||02-FEB-15
32501|Willimigongong Ignimbrite|68116|5|Briefly described|Appendix, Map 32,|Late Devonian|Late Devonian||||||Enstatite-feldspar rhyodacite with high phenocryst content: dark grey; mostly recrystallised but some layers contain abundant lithic fragments including: basalt, siltstone, and glassy felsic volcanic rock.|
32501|Willimigongong Ignimbrite|68990|6|Mentioned|p455|Devonian|Devonian|Occurs at Mount Macedon.||||||22-APR-14
26219|Wilson Creek Shale|22570|6|Mentioned|p189|Emsian|Pragian|Of the Melbourne Trough.||||||22-DEC-08
26219|Wilson Creek Shale|22628|6|Mentioned|p115|||||||||
26219|Wilson Creek Shale|22885|5|Briefly described|map|Early Devonian|Early Devonian|||||||
26219|Wilson Creek Shale|22886|4|Described|p14|Emsian|Pragian|||||||
26219|Wilson Creek Shale|23229|5|Briefly described|Table3-3p27, 31|Pragian|Pragian|||||||
26219|Wilson Creek Shale|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Jordan River Group.||||||22-DEC-08
26219|Wilson Creek Shale|23309|5|Briefly described|p142-155. Table 2.54|Emsian|Pragian|||||||
26219|Wilson Creek Shale|23522|5|Briefly described|p246|Middle Devonian|Early Devonian|||||||
26219|Wilson Creek Shale|24002|5|Briefly described|p247|Early Devonian|Early Devonian|||||||
26219|Wilson Creek Shale|24098|6|Mentioned|p27 Fig. 2|Emsian|Emsian|Geological Province: Melbourne Zone, Lachlan Fold Belt.||||||
26219|Wilson Creek Shale|24177|3|Fully described|p59, p50 Fig.22, p58 Fig.25|Emsian|Pragian|Of the Jordan River Group. Overlain by the Norton Gully Sandstone. Overlies the Humevale Siltstone. Geological Province: Melbourne Trough. Less than 500m thick.||||||
26219|Wilson Creek Shale|24224|5|Briefly described|p263|Early Devonian|Early Devonian|Geological Province: Turtons Creek Inlier.||||||
26219|Wilson Creek Shale|24328|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent: Jordan River Group.||||||27-OCT-08
26219|Wilson Creek Shale|24329|5|Briefly described|Map legend|Early Devonian|Early Devonian|Parent: Jordan River Group.||||||27-OCT-08
26219|Wilson Creek Shale|24551|6|Mentioned|p606, 123|Devonian|Devonian|||||||
26219|Wilson Creek Shale|24588|5|Briefly described|p22-23, p12 Fig.3, p32|Emsian|Pragian|Geological Province: Mount Easton Province. Of Jordan River Group.  Conformably overlies Eildon Sandstone. Overlain by Walhalla Group. Creek is Ck in text.||||||29-NOV-13
26219|Wilson Creek Shale|31339|6|Mentioned|p426|||||||||
26219|Wilson Creek Shale|32984|6|Mentioned|p343|||Graptolites||||||
26219|Wilson Creek Shale|33238|5|Briefly described|p642|||||||||
26219|Wilson Creek Shale|33601|2|Defined|p17|Early Devonian|Early Devonian|||||||
26219|Wilson Creek Shale|33602|6|Mentioned|Fig.2|||||||||
26219|Wilson Creek Shale|33604|6|Mentioned|p17|||L.Dev. Correlation chart||||||
26219|Wilson Creek Shale|33606|6|Mentioned|p70|||||||||
26219|Wilson Creek Shale|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
26219|Wilson Creek Shale|34815|6|Mentioned|p18|||||||||
26219|Wilson Creek Shale|35073|5|Briefly described|Table 1.|||||||||
26219|Wilson Creek Shale|35112|6|Mentioned|Fig.9|||||||||
26219|Wilson Creek Shale|35283|3|Fully described|p54|||||||||
26219|Wilson Creek Shale|35864|6|Mentioned|p307|||||||||
26219|Wilson Creek Shale|37727|6|Mentioned|p57|||||||||
26219|Wilson Creek Shale|38787|6|Mentioned|p125|||||||||
26219|Wilson Creek Shale|39331|6|Mentioned|Table 2-1|||||||||
26219|Wilson Creek Shale|39551|6|Mentioned|Map legend|Pragian|Pragian|||||||
26219|Wilson Creek Shale|39555|6|Mentioned|Map legend|Pragian|Pragian|||||||
26219|Wilson Creek Shale|41572|6|Mentioned|p13|||||||||
26219|Wilson Creek Shale|41585|4|Described|p114|||||||||
26219|Wilson Creek Shale|41868|6|Mentioned|p580|||||||||
26219|Wilson Creek Shale|41909|6|Mentioned|p111|||||||||
26219|Wilson Creek Shale|42032|6|Mentioned|p498|||||||||
26219|Wilson Creek Shale|42033|6|Mentioned|p654|||||||||
26219|Wilson Creek Shale|42051|5|Briefly described|p140|||||||||
26219|Wilson Creek Shale|42827|4|Described|p114|||see also Table 4.1||||||
26219|Wilson Creek Shale|42938|5|Briefly described|p576 Fig.3|||||||||
26219|Wilson Creek Shale|43461|14|Not recorded|p627|||||||||
26219|Wilson Creek Shale|43871|14|Not recorded|p13-55||Early Devonian|||||||
26219|Wilson Creek Shale|44187|5|Briefly described|Map Legend||Early Devonian|||||||
26219|Wilson Creek Shale|44197|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
26219|Wilson Creek Shale|60529|5|Briefly described|Map Legend|Emsian|Pragian|Of the Jordon River Group. Deep water pelagic (anoxic) sediment: paper laminated shale; dark grey, commonly pyritic, minor burrows, minor siltstone laminations indurated with iron, minor slump deposits.||||||
26219|Wilson Creek Shale|60599|5|Briefly described|p13, p14|Pragian|Silurian|Of Walhalla Group. Pelagic sedimentary sequence deposited in deep anoxic water. Overlies Humevale Siltstone. Geological Province: Melbourne Zone, Lachlan Fold Belt. See also p67.||||||
26219|Wilson Creek Shale|61120|6|Mentioned|p2 Fig.1, p3.  |Late Pragian|Middle Pragian|Correlated (VandenBerg 1988) with a horizon above the base of the Lilydale Limestone.||||Is overlain by Yeringberg Formation.||
26219|Wilson Creek Shale|61185|2|Defined|p37, p39-41, p21 Fig.6, p23-25, p49, p46|Emsian|Lochkovian|Of Thomas (1953). Revised VandenBerg (1975). Conformable over Humevale Siltst; over Eildon Sst, Boola Fm, Whitelaw Siltst; under Norton Valley Sst (fault), White Hills Gravel (ang. unconform.) and Yeringberg Fm; interfingers Coopers Ck Limest.||||||07-FEB-11
26219|Wilson Creek Shale|61187|5|Briefly described|p5 Fig.3.|Early Devonian|Early Devonian|Melbourne Zone, Melbourne Terrane. Correlative of Wentworth Group (Tabberabbera Zone, Benambra Terrane) and Buchan Group (Buchan and Mallacoota Zones, Benambra Terrane).||||||
26219|Wilson Creek Shale|61701|5|Briefly described|Map Legend|Emsian|Pragian|Of the Jordon River Group. Deep water pelagic (anoxic) sediment: paper laminated shale; dark grey, commonly pyritic, minor burrows, minor siltstone laminations indurated with iron, minor slump deposits.||||||25-JUL-06
26219|Wilson Creek Shale|61702|5|Briefly described|Map Legend|Emsian|Pragian|Of the Jordon River Group. Deep water pelagic (anoxic) sediment: paper laminated shale; dark grey, commonly pyritic, minor burrows, minor siltstone laminations indurated with iron, minor slump deposits.||||||25-JUL-06
26219|Wilson Creek Shale|61703|5|Briefly described|Map Legend|Emsian|Pragian|Of the Jordon River Group. Deep water pelagic (anoxic) sediment: paper laminated shale; dark grey, commonly pyritic, minor burrows, minor siltstone laminations indurated with iron, minor slump deposits.||||||25-JUL-06
26219|Wilson Creek Shale|61704|6|Mentioned|Map legend|Devonian|Devonian|Low K, variable Th.||||||
26219|Wilson Creek Shale|62099|5|Briefly described|p331|Early Devonian|Silurian|In the Melbourne Zone of the Lachlan Orogen. ||||||
26219|Wilson Creek Shale|62469|5|Briefly described|p5 Fig. 2|Pragian|Pragian|Geological Province: Darraweit Guim Province.||||||07-FEB-11
26219|Wilson Creek Shale|64535|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Group. Shale, siltstone, minor calcareous clastics: shale and siltstone black, laminated-thick-bedded, sparsely fossiliferous with plant fossils + graptolites; more lithological details included; deep-marine hemipelagic deposits.||||||22-DEC-08
26219|Wilson Creek Shale|64536|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Group. Shale, siltstone: black, laminated-thick-bedded, sparsely fossiliferous with plant fossils + graptolites; more lithological details included; deep-marine hemipelagic deposits.||||||07-FEB-11
26219|Wilson Creek Shale|64537|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Group. Shale, siltstone: black, laminated-thick-bedded, sparsely fossiliferous with plant fossils + graptolites; more lithological details included; deep-marine hemipelagic deposits.||||||07-FEB-11
26219|Wilson Creek Shale|64538|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Group. Shale, siltstone: black, laminated-thick-bedded, sparsely fossiliferous with plant fossils + graptolites; more lithological details included; deep-marine hemipelagic deposits.||||||07-FEB-11
26219|Wilson Creek Shale|64539|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Group. Shale, siltstone, minor calcareous clastics: shale and siltstone black, laminated-thick-bedded, sparsely fossiliferous with plant fossils + graptolites; more lithological details included; deep-marine hemipelagic deposits.||||||22-DEC-08
26219|Wilson Creek Shale|64540|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Group. Shale, siltstone, minor calcareous clastics: shale and siltstone black, laminated-thick-bedded, sparsely fossiliferous with plant fossils + graptolites; more lithological details included; deep-marine hemipelagic deposits.||||||22-DEC-08
26219|Wilson Creek Shale|64605|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Jordan River Group. Shale, siltstone; deep-marine deposits. Speckled blue-pink in RGB, speckled brown on plateau west of St Clair. Low magnetic response.||||||17-NOV-08
26219|Wilson Creek Shale|64606|5|Briefly described|Map Legend|Early Devonian|Silurian|Of Jordan River Group. Shale, siltstone: deep-marine deposits. Speckled blue-pink in RGB, speckled brown on plateau west of Saint Clair. Low magnetic response.||||||
26219|Wilson Creek Shale|64612|6|Mentioned|p27|Early Devonian|Early Devonian|Black shale.||||||07-FEB-11
26219|Wilson Creek Shale|64616|3|Fully described|p97, p160, p161-164, p166, p171|Emsian|Pragian|See also p183 Fig.6.29, p197 Fig.6.34, p201 Tb.7.1, p202-203, p281, p286-288, p290, p293-294, p304, p386, p390. Top of Jordan River Group. Exposures rare. Conformable between various Jordan River Group units and various Walhalla Group units. Thickness: 100-~200m. Black shale, locally phosphatic. Graptolites, conodonts and other marine fossils (including Phacopid trilobite) plus land plants give age. Highly recessive. Geophysical characteristics given.||||||
26219|Wilson Creek Shale|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Walhalla. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
26219|Wilson Creek Shale|65969|6|Mentioned|p15|||A small part of this unit is magnetic.||||||
26219|Wilson Creek Shale|66197|6|Mentioned|p636|Pragian|Pragian|Deposition was preceded by an interbedded sandstone-mudstone succession derived from the west and south.||||||14-MAR-12
26219|Wilson Creek Shale|66244|4|Described|p3.|||||||Is overlain conformably by Woori Yallock Formation.||
26219|Wilson Creek Shale|68116|5|Briefly described|Appendix, Maps 25, 33, 42-43, 52.|Emsian|Pragian|Shown on the maps separately (code Sji) and locally in combination with Easts Lookout Siltstone (Dne-Sji).|||||Pyritic black shale, siltstone: black; laminated to thick-bedded; sparsely fossiliferous with plant fossils and graptolites.|
26219|Wilson Creek Shale|69089|5|Briefly described|Map legend|Early Devonian|Early Devonian||||||Marine: siltstone, minor sandstone.|
26219|Wilson Creek Shale|70487|6|Mentioned|p9, p11 Fig.5|Emsian|Pragian|Agreement in age of Pragian-Emsian by Edwards et al (1997), VandenBerg et al (2000), Sandford (2005), Welch et al (2011) and Earp (2015).||||Overlies Broadford Formation in Yea area. Shown as overlying Wilson Creek Shale (Earp 2015) and underlying Norton Gully Sandstone.|Fossiliferous shale.|
26219|Wilson Creek Shale|70742|6|Mentioned|p162|||||Jordan River Group.||Is overlain by Norton Gully Sandstone.||
26219|Wilson Creek Shale|71040|6|Mentioned|p26|Emsian|Pragian|Widespread unit in the Melbourne Zone.||||||
26219|Wilson Creek Shale|73497|5|Briefly described|Map legend|Devonian|Devonian|Marine.||Jordan River Group|||Black shale, siltstone: weak magnetic responses; low K and variable Th and U.|
20179|Wilsons Promontory Granite|23266|5|Briefly described|p353, 355||Middle Devonian|Intrusion at 384 Ma.||||||
20179|Wilsons Promontory Granite|23309|6|Mentioned|p447 App1|||G623.||||||
20179|Wilsons Promontory Granite|24551|5|Briefly described|p158, 160, 492|||||||||
20179|Wilsons Promontory Granite|37501|6|Mentioned|p405|||||||||
20179|Wilsons Promontory Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
20179|Wilsons Promontory Granite|61723|5|Briefly described|p824|||S-type granite. Age: 395+/-4Ma. In Victoria. ||||||
20179|Wilsons Promontory Granite|67802|6|Mentioned|p29|Devonian|Devonian|SHRIMP zircon age.  This pushes back the date of the Tabberabberan Orogeny in Melbourne Zone from previous estimate of 385 Ma.|395 +/- 4 Ma (Eburg, 1996).|||||
20179|Wilsons Promontory Granite|68116|5|Briefly described|Appendix, Map 57.|Middle Devonian|Middle Devonian||||||Biotite granite: coarse grained, porphyritic; with some garnet; S-type.|
20179|Wilsons Promontory Granite|71040|5|Briefly described|p8 Fig.5, p12|||Melbourne Zone.|395 +/- 4 Ma; U-Pb zircon age (Elburg, 1996).|||||
23217|Windarra Formation|23309|4|Described|p112. Table 2.40|||Of the Timbarra Subgroup.  Maximum Thickness: ~700m.  Underlies: Fluke Knob Ignimbrite.||||||
23217|Windarra Formation|23615|3|Fully described|p88, p23|Early Devonian|Early Devonian|Of Timbarra Subgroup. Overlain by Statham Ignimbrite, overlies Wilkinson Creek Conglomerate. See also p211 App.2.  Type section is on the Timbarra Road southeast of Timbarra.  Age:410-395Ma.||||||10-SEP-18
23217|Windarra Formation|24551|4|Described|p142|||Of the Timbarra Subgroup.||||||
23217|Windarra Formation|43206|5|Briefly described|map legend||Ludlow|Timbarra Subgroup||||||
23217|Windarra Formation|43312|5|Briefly described|Map Legend||Early Devonian|of Timbarra Subgroup||||||
23217|Windarra Formation|43313|5|Briefly described|Map Legend||Early Devonian|of Timbarra Subgroup.||||||
23217|Windarra Formation|60542|4|Described|p50|Early Devonian|Early Devonian|Of Timbarra Subgroup. Formerly of Mount Johnson Member. Rubbly conglomerate in sandy matrix. Unconformable on Pinnak Sandstone. Overlain by Fluke Knob Ignimbrite, Kanni Ignimbrite, Johnson Mudstone. Max. thickness: ~600m. ||||||
23217|Windarra Formation|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Sedolithic and volcanilithic conglomerate, sandstone, mudstone: poorly bedded; alluvial fan deposits; hornblende andesite, rhyolite and quartz latite lava; lava flows.|
20219|Windermere Sandstone Member|12781|6|Mentioned|p386|Early Cretaceous|Early Cretaceous|Otway Basin. Maximum thickness 21m.||Eumeralla Formation.||Unconformably overlies Katnook Sandstone.||
20219|Windermere Sandstone Member|22674|5|Briefly described|Fig.2 p719|Aptian|Aptian|Part of Otway Supergroup.||||||16-OCT-07
20219|Windermere Sandstone Member|22686|5|Briefly described|Fig3p745|||Basal sand unit of Eumeralla Formation. Shown only as Windermere Sandstone in Fig. 3.  Geological Province: Otway Basin.||||||17-JAN-06
20219|Windermere Sandstone Member|24314|5|Briefly described|p61 Fig.2|Aptian||Geological Province: Otway Basin. Max. Thickness 21m. Of the Otway Supergroup.||||||30-NOV-04
20219|Windermere Sandstone Member|24453|5|Briefly described|p809 Fig.2|Aptian|Aptian|Of Otway Group. Overlain by Eumeralla Formation. Geological Province: Otway Basin.||||||07-FEB-11
20219|Windermere Sandstone Member|24551|5|Briefly described|p251|||||||||
20219|Windermere Sandstone Member|42361|3|Fully described|p9|Aptian||||||||
20219|Windermere Sandstone Member|42545|5|Briefly described|Fig.4 P15|||||||||
20219|Windermere Sandstone Member|43171|6|Mentioned|5-8|||Of Eumeralla Formation. Age: 120-125Ma||||||
20219|Windermere Sandstone Member|43195|5|Briefly described|Map Legend||Early Cretaceous|See also commentary on back of map.Of Crayfish Group.||||||
20219|Windermere Sandstone Member|43733|6|Mentioned|Fig.2.11,p65||Early Cretaceous|||||||
20219|Windermere Sandstone Member|43744|6|Mentioned|Fig.3,p3|||||||||
20219|Windermere Sandstone Member|43814|6|Mentioned|Fig.3,p115|||||||||
20219|Windermere Sandstone Member|44133|5|Briefly described|p144|Aptian|Aptian|Geological Province: Otway Basin. Of the Eumeralla Formation. Thickness: 100m.||||||
20219|Windermere Sandstone Member|61017|6|Mentioned|p6|||||||||07-FEB-11
20219|Windermere Sandstone Member|61329|6|Mentioned|p121|||||||||
20219|Windermere Sandstone Member|61547|6|Mentioned|p461 Fig.2. |Barremian|Barremian|||Unit in Eumeralla Formation.||Overlies unconformably the Katnook Sandstone.||
20219|Windermere Sandstone Member|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Otway Supergroup. Geological Province: Otway Basin.||||||07-FEB-11
20219|Windermere Sandstone Member|61627|5|Briefly described|p500 Fig. 2|Early Cretaceous|Early Cretaceous|Of Eumeralla Formation. Geological Province: Otway Basin.||||||07-FEB-11
20219|Windermere Sandstone Member|63122|5|Briefly described|p17 Fig. 4.3|Aptian|Barremian|Of Eumeralla Formation (Otway Supergroup). Geological Province: Otway Basin. ||||||
20219|Windermere Sandstone Member|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p73|Barremian|Barremian|Supersedes Windemere Member. Of Eumeralla Formation. Unconformable over Crayfish Group. Age: 125-119Ma. Max. thickness: 16m; 160m in Victoria. Geological Province: Otway Basin.Crayfish Group.||||||31-JAN-08
20219|Windermere Sandstone Member|63125|6|Mentioned|p116 Tb.7.6, p121 Tb. 7.11|||Geological Province: Otway Basin||||||
20219|Windermere Sandstone Member|63129|5|Briefly described|p127, p132|||Of the Otway Supergroup. Max. thickness: 16m. Geological Province: Otway Basin.||||||30-JAN-08
20219|Windermere Sandstone Member|63267|5|Briefly described|p485 Fig.2, p496|Early Cretaceous|Early Cretaceous|Penola Trough, Otway Basin. Abbreviated to Windermere Sandstone on p496.||Eumeralla Formation.||Unconformably overlies Katnook Sandstone.||
20219|Windermere Sandstone Member|63431|5|Briefly described|p677 Fig. 2|Barremian|Barremian|Of the Eumeralla Formation (Otway Supergroup). Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
20219|Windermere Sandstone Member|69948|6|Mentioned|Fig.4.2|||Otway Basin (a rift basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Eromanga Basin (an intracratonic basin).||Eumeralla Formation.||Overlies Katnook Sandstone.||
20219|Windermere Sandstone Member|70077|5|Briefly described|Regional: Fig.4|Aptian|Aptian|Otway Basin: Robe-Penola Trough.||Eumeralla Formation.||Overlies Katnook Sandstone.||
20219|Windermere Sandstone Member|71342|6|Mentioned|Ch4 p9 Fig 4.2|||Otway Basin.||||||
20219|Windermere Sandstone Member|72050|5|Briefly described|p235-236|Aptian|Aptian|Kopsen and Scholefield (1990).||Basal Eumeralla Formation.||Unconformably overlies Katnook Sandstone.|Quartzose sandstone.|
38052|Windgelli Clay|23402|3|Fully described|p35|Late Pleistocene|Late Pleistocene|Thickness: 2m.   Underlying unit: Newer Volcanics.   Geological Province: Adelaide Fold Belt||||||
38052|Windgelli Clay|66012|4|Described|p4, p9 Tb.1, p19-21, p23, p27, p32|Pleistocene|Pleistocene|Calcareous, aeolian clay. Forms a thin veneer over most Paleozoic rocks and all but the youngest basalt flows of the Newer Volcanic Group. Up to 2m thick. Possible correlative of Woorinen Formation. Late Pleistocene| | | | | |16-FEB-15
20243|Wingan Granite|23309|6|Mentioned|p447 App1|||G9 I-Type.||||||
20243|Wingan Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
20243|Wingan Granite|68115|5|Briefly described|p6.|||On the geophysical interpretation map of Oranskaia (1997a), this non-magnetic unit surrounds the magnetic Skerries Granite pluton. The eponymous Skerries islands are non-magnetic, so the names of the plutons have been swapped.||||||
20243|Wingan Granite|68116|5|Briefly described|Appendix, Map 46.|Early Devonian|Early Devonian||||||Granite: magnetic; I-type.|
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.|
23229|Wiridjil Gravel|12796|5|Briefly described|p460|||Possibly misspelt? See also Wiridjil Gravels. Unconsolidated gravel and coarse sand with minor pebble and cobble layers and white clay clasts. Interpreted as lateral facies equivalent of the youngest part of Timboon Sandstone.||||||
23229|Wiridjil Gravel|22875|5|Briefly described|p14|Middle Eocene|Paleocene|Of the Wangerrip Group.||||||30-JAN-07
23229|Wiridjil Gravel|23322|5|Briefly described|957 Fig.2|Paleocene|Paleocene|Of the Wangerrip Group.  Geological Province: Otway Basin.||||||07-SEP-09
23229|Wiridjil Gravel|24551|6|Mentioned|p292, 467|||Of the Pebble Point Formation.||||||
23229|Wiridjil Gravel|43590|4|Described|p18||Paleocene|||||||
23229|Wiridjil Gravel|43937|5|Briefly described|Map Legend|Paleocene|Santonian|||||||
23229|Wiridjil Gravel|61181|6|Mentioned|p183|||Contains relatively pure sands for various forms of silica. Geological Province: Otway Basin. ||||||
23229|Wiridjil Gravel|61182|3|Fully described|p19, p21, p169|||Of Wangerrip Gp. Non-marine, unconsolidated gravel and coarse sand, minor pebble layers. Grading out of, and locally overlying, Moomowroong Sand - both lateral equivalents of Pebble Point Fm. Also overlies Timboon Sand Member. Geol.Prov: Otway Basin.||||||06-JAN-10
23229|Wiridjil Gravel|65715|5|Briefly described|p11 Tb.7|Paleogene|Paleogene|Of Wangerrip Group. Formation rank.||||||
23229|Wiridjil Gravel|66002|3|Fully described|p10 Tb.7, Tb.8, p11, p12, p16, p35-59|Paleogene|Paleogene|Of Wangerrip Group. Wiridjil Gravel Member of Edwards et al. (1994). Type section is unrepresentative. Diamictite. Generally poorly sorted silt & sand, <10% pebbles. Indistinguishable from Dilwyn Formation; VandenBerg (2009) recommends that inland outcrops of Dilwyn Formation be mostly reassigned to this unit. Interfingers  Moomowroong Sand. Overlies Otway Group rocks. Submarine deltaic deposit. Defined by Tickell et al 1992.||||||28-MAY-13
23229|Wiridjil Gravel|68116|5|Briefly described|Appendix, Maps 49, 54-55.|Paleocene|Late Cretaceous||||||Quartz sand, silt, clay, pebbles, rare clay clasts; pebbles mostly dispersed, less commonly in horizontal layers; cohesive, sorting mostly poor, rare volcanic and metamorphic lithic cobbles and pebbles; occasional large-scale tabular cross-bedding.|
23229|Wiridjil Gravel|69297|5|Briefly described|p79, p98|Maastrichtian|Maastrichtian|Otway Basin. ||Wangerrip Group||Overlies the Timboon Sandstone. Overlain by the Massacre Shale. |Gravel and sandstone. |
23229|Wiridjil Gravel|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Maastrichtian|Maastrichtian|Otway Basin: Port Campbell Embayment.||Wangerrip Group.||Overlies Timboon Sandstone. Is overlain by Massacre Shale.||
23229|Wiridjil Gravel|70193|6|Mentioned|p284 Fig 2|Maastrichtian|Maastrichtian|Geological province: Otway Basin.  Part of the Sherbrook Supersequence.||||||
30480|Wirrah Conglomerate|43145|5|Briefly described|p17|Early Paleocene|Cenomanian|||||||
83432|Woleebee pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G609.||Of Glenloth Suite|||Magnetic response to 30 nT; gravity response difficult to separate from those from adjacent plutons.|
69414|Wollonaby Granite|61160|3|Fully described|p83, p32 Tb. 5.2|Early Devonian|Early Devonian|I-type. Medium-grained, equigranular biotite granite, grey and homogeneous with no enclaves observed. Adjacent to migmatite of the Omeo Metamorphic Complex and the Cobungra Granite. See also p58-59 Fig. 6.8.||||||
69414|Wollonaby Granite|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite granite: grey; medium grained; equigranular; pervasive mylonitic fabric, commonly S-C fabric; non magnetic; I-type intrusion. GSV map code: G166.||||||
69414|Wollonaby Granite|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite granite: grey; medium grained; equigranular; pervasive mylonitic fabric, commonly S-C fabric; non magnetic; I-type intrusion. GSV map code: G166.||||||
69414|Wollonaby Granite|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite granite: grey; medium grained; equigranular; pervasive mylonitic fabric, commonly S-C fabric; non magnetic; I-type intrusion. GSV map code: G166.||||||
69414|Wollonaby Granite|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite granite: grey; medium grained; equigranular; pervasive mylonitic fabric, commonly S-C fabric; non magnetic; I-type intrusion. GSV map code: G166.||||||07-FEB-11
69414|Wollonaby Granite|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite granite: I-type; non magnetic (kv = 0-20 x10^-6 cgs); low gravity; variable radiometric response. GSV map code: G166.||||||
69414|Wollonaby Granite|68116|5|Briefly described|Appendix, Map 27a.|Pridoli|Llandovery||||||Biotite granite: grey; medium grained; equigranular; pervasive mylonitic fabric, commonly S-C fabric; non magnetic; I-type.|
23240|Wombargo Subgroup|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Snowy River Volcanics||||||
23240|Wombargo Subgroup|23309|4|Described|p113. Table 2.40|||Of the Snowy River Volcanics.  Maximum Thickness: ca 3000m.||||||
23240|Wombargo Subgroup|23615|3|Fully described|p94, p22|Early Devonian|Early Devonian|Of the Snowy River Volcanics.  Max. thickness: ~3000m. Probably overlain by the Statham Ignimbrite.||||||
23240|Wombargo Subgroup|24551|4|Described|p142, p141 Fig. 5.32|||Of the Snowy River Volcanics.||||||
23240|Wombargo Subgroup|43206|5|Briefly described|map legend||Ludlow|Of Snowy River Volcanics||||||
23240|Wombargo Subgroup|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Unit in Snowy River Volcanics.|||Extrusive, fluvial: conglomerate, sandstone, felsic ignimbrite.|
23240|Wombargo Subgroup|68116|5|Briefly described|Appendix, Maps 28, 36.|Pragian|Lochkovian||||||Ignimbrite, conglomerate and sandstone: pink crystal-rich quartz ignimbrite with quartzite and rhyolitic lava lithic clasts and small pumice fragments; sedimentary units: clast-supported conglomerate, interbedded pebbly and massive sandstone.|
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).|||||
75870|Wombat Volcanics|70076|5|Briefly described|Regional: Fig.3|Turonian|Turonian|||Emperor Subgroup.||Overlies Wonthaggi Formation. Is overlain by Admiral Formation.||
36817|Wonga Schist|23857|6|Mentioned|p903 Fig 2b|||||||||
36817|Wonga Schist|24087|6|Mentioned|p330 Fig. 4|||Geological Province: Lachlan Fold Belt.||||||
36817|Wonga Schist|24100|6|Mentioned|p95|||Geological Province: Lachlan Fold Belt.||||||
36817|Wonga Schist|50546|5|Briefly described|p1232 Fig.1c|||Geological Province: Lachlan Fold Belt.||||||30-NOV-04
36817|Wonga Schist|60454|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Unit does not appear on this map.||||||
36817|Wonga Schist|60456|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Unit does not appear on this map.||||||
36817|Wonga Schist|60457|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Informal name for contact metamorphosed Warrak Formation, Deenicull Schist and Lexington Schist in Stawell region only.||||||
36817|Wonga Schist|60458|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Informal name for contact metamorphosed  Warrak Formation, Deenicull Schist and Lexington Schist in Stawell region only.||||||
36817|Wonga Schist|61410|5|Briefly described|p11-16, p18-19, p41|||Formerly thought to overlie the Mine Schist. Now thought to be part of the same unit. Also appears as Wonga schist and Wonga schists. Hosts the Wonga (gold) lode in the Stawell Granite aureole. Deformation described.||||Intruded by the Stawell Granite.|Laminated (1-100mm) psammopelitic rock (turbidites) distinguished by the presence of biotite, less chlorite and sparsely interbedded, thicker psammite beds (10-100mm).|
36817|Wonga Schist|62751|6|Mentioned|p760 Fig. 1b|||||||||
36817|Wonga Schist|62752|6|Mentioned|p760 Fig. 1b|||||||||
36817|Wonga Schist|63793|6|Mentioned|p65.|||Informal name for the rock forming the hanging wall in the Magdala gold mine, Victoria.||||||
36817|Wonga Schist|68116|5|Briefly described|Appendix, Map 30.|Cambrian|Cambrian||||||Quartz-biotite (cordierite) schist: numerous thin boudinaged quartz veins; psammite beds (1-50 cm) occasionally preserved; nonmagnetic.|
36817|Wonga Schist|68314|5|Briefly described|p750-751|||Watchorn and Wilson (1989). The authors propose this name be abandoned.||Unit in Saint Arnaud Group.|||Quartz-rich sandstones; muscovite-altered.|
33943|Wonthaggi Formation|22476|6|Mentioned|p953|||Repeat of informal name for upper Strzelecki Group from other literature.||||||22-DEC-08
33943|Wonthaggi Formation|23911|4|Described|p93, p95 Fig. 9B|Albian|Barremian|Geological Province: Gippsland Basin.  Max. Thickness: >2500m.  Of the Strzelecki Group.  Underlying Unit: Tyers Subgroup.||||||
33943|Wonthaggi Formation|24164|5|Briefly described|p9 Fig.4, p19, p23, p25, p41 Tb.2||Late Jurassic|Younger part of the Strzelecki Group includes almost all the onshore outcrops. Basalt flows lie below some of oldest parts of Wonthaggi Formation. Interflow sediments at base of the underyling flows are Late Jurassic, ~150 Ma, spore pollens (R. watherooensis).||Strzelecki Group||Overlies Tyers River Subgroup|Mafic volcaniclastic detritus|
33943|Wonthaggi Formation|24551|6|Mentioned|p566|||||||||
33943|Wonthaggi Formation|24561|6|Mentioned|p41|Cenomanian|Barremian|Upper part of Strzelecki Group. Geological Province: Gippsland Basin.||||||04-FEB-08
33943|Wonthaggi Formation|50043|5|Briefly described|p2, p6, 8, 12|Early Aptian|Early Aptian|Description of Serendipaceratops arthurcclarkei sp.nov. holotype and type location.||Of Strzelecki Group.||||27-MAR-12
33943|Wonthaggi Formation|61302|5|Briefly described|p9, p11 Fig.4|Cretaceous|Cretaceous|Of the Strzelecki Group. Overlies the Tyers Conglomerate. Geological Province: Gippsland Basin.||||||
33943|Wonthaggi Formation|63445|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|||Strzelecki Group.|||Fluvial: lithic sandstone, siltstone, minor conglomerate, coal.|
33943|Wonthaggi Formation|64570|5|Briefly described|p858|||Of Otway Group. Geological Province: Gippsland Basin.||||||22-DEC-08
33943|Wonthaggi Formation|64616|6|Mentioned|p141,142|||Informal. Considered to be a synonym of Eumeralla Formation, which is preferred here.||||||
33943|Wonthaggi Formation|66244|5|Briefly described|p5, p6.|||Re-named the Eumeralla Formation by VandenBerg et al. (2006) and VandenBerg (2008); it has identical mineralogical and radiometric RGB image characteristics across southern Victoria. Because of its entrenched use in the petroleum industry, the Wonthaggi Formation name is retained for Eumeralla Formation-equivalent rocks in the Gippsland Basin.||||Is overlain unconformably by the Thorpdale and Neerim Volcanic Groups.||
33943|Wonthaggi Formation|68116|5|Briefly described|Appendix, Maps 51-52, 56-57.|Early Cretaceous|Early Cretaceous||||||Lithic volcaniclastic sandstone, arkose, siltstone, minor conglomerate and coal; fluvial.|
33943|Wonthaggi Formation|70076|5|Briefly described|South-Eastern: Fig.5|Albian|Barremian|||Korumburra Subgroup.||Is overlain by Kersop Arkose.||
33943|Wonthaggi Formation|70378|5|Briefly described|p700|Early Cretaceous|Early Cretaceous|||Strzelecki Group.||Overlies Exalt Member (Rintoul Creek Formation).||
33943|Wonthaggi Formation|71601|6|Mentioned|p120, p121|Albian|Hauterivian|Historical name no longer used. Rocks now included in Eumeralla Formation. Coastal Victoria. Ankylosaurian remains have been identified.||||||
33943|Wonthaggi Formation|75065|6|Mentioned|p157-159|||Constantine (2001). Gippsland Basin. Appears as Wonthaggi Coal Measures on p159.||||Unconformably overlies Tyers River Subgroup locally. Equivalent to Korumburra Subgroup?||
29167|Woodbine Basalt|24551|6|Mentioned|p343|Pleistocene|Pliocene|Age: 1.8Ma.||||||
29167|Woodbine Basalt|29425|6|Mentioned|p103|||||||||
29167|Woodbine Basalt|30993|6|Mentioned|p144|||Refers Gill (1967)||||||
29167|Woodbine Basalt|31004|6|Mentioned|p394|||||||||
29167|Woodbine Basalt|32102|6|Mentioned|p175|||||||||
29167|Woodbine Basalt|34993|4|Described|p300|||||||||
29167|Woodbine Basalt|35722|6|Mentioned|Table 2|||Quaternary stratigraphic units and nature of components.||||||
29167|Woodbine Basalt|41701|6|Mentioned|Map legend|Pleistocene||||||||
29167|Woodbine Basalt|41769|4|Described|p38|||||||||
29167|Woodbine Basalt|41848|4|Described|p375|||Age 300000 yrs K-Ar||||||
29167|Woodbine Basalt|42827|4|Described|p375|||||||||
20527|Woods Point Dyke Swarm|22628|6|Mentioned|p119||Middle Devonian|||||||
20527|Woods Point Dyke Swarm|24588|6|Mentioned|p32|||387+/-14 Ma (Richards and Singleton, 1981, p403).||||||04-SEP-14
20527|Woods Point Dyke Swarm|42827|4|Described|p150|||||||||
20527|Woods Point Dyke Swarm|60412|5|Briefly described|p229, 233, 236, 242, 246-247|Middle Devonian|Middle Devonian|Melbourne Zone, western subprovince of the Lachlan Fold Belt. Associated with a significant number of gold deposits. Mineralisation post-dates or is synchronous with intrusion. Appears throughout, until the final mention, as Woods Point Dike Swarm.|387 +/- 14 Ma and 372 +/- 2 Ma.||||Mafic to felsic.|
20527|Woods Point Dyke Swarm|61410|6|Mentioned|p20|||Melbourne Zone. Intrusion was synchronous with, or just before, the Walhalla and Great Rand mineralisation event(s).||||||
20527|Woods Point Dyke Swarm|64396|6|Mentioned|p224, p225|||In Victoria. Hosts gold deposits.||||||08-DEC-08
20527|Woods Point Dyke Swarm|64535|5|Briefly described|Map legend|Late Devonian|Late Devonian|Hornblende-biotite quartz diorite and quartz monzonite. Hornblende-biotite gabbro, hornblende-augite-biotite quartz gabbro, kaersutite-phlogopite peridotite; medium-grained, hydrothermal alteration common; commonly weathered to ornage sandy clay; I-type.||||||
20527|Woods Point Dyke Swarm|64536|5|Briefly described|Map legend|Late Devonian|Late Devonian|Hornblende-biotite quartz diorite + quartz monzonite.Hornblende-biotite gabbro, hornblende-augite-biotite quartz gabbro, kaersutite-phlogopite peridotite; medium-grained, hydrothermal alteration common; commonly weathered to ornage sandy clay; intrusive.||||||07-FEB-11
20527|Woods Point Dyke Swarm|64537|5|Briefly described|Map legend|Late Devonian|Late Devonian|Hornblende-biotite quartz diorite + quartz monzonite.Hornblende-biotite gabbro, hornblende-augite-biotite quartz gabbro, kaersutite-phlogopite peridotite; medium-grained, hydrothermal alteration common; commonly weathered to ornage sandy clay; intrusive.||||||07-FEB-11
20527|Woods Point Dyke Swarm|64538|5|Briefly described|Map legend|Late Devonian|Late Devonian|Hornblende-biotite quartz diorite + quartz monzonite.Hornblende-biotite gabbro, hornblende-augite-biotite quartz gabbro, kaersutite-phlogopite peridotite; medium-grained, hydrothermal alteration common; commonly weathered to ornage sandy clay; intrusive.||||||07-FEB-11
20527|Woods Point Dyke Swarm|64539|5|Briefly described|Map legend|Late Devonian|Late Devonian|Hornblende-biotite quartz diorite and quartz monzonite. Hornblende-biotite gabbro, hornblende-augite-biotite quartz gabbro, kaersutite-phlogopite peridotite; medium-grained, hydrothermal alteration common; commonly weathered to ornage sandy clay; I-type.||||||
20527|Woods Point Dyke Swarm|64540|5|Briefly described|Map legend|Late Devonian|Late Devonian|Hornblende-biotite quartz diorite and quartz monzonite. Hornblende-biotite gabbro, hornblende-augite-biotite quartz gabbro, kaersutite-phlogopite peridotite; medium-grained, hydrothermal alteration common; commonly weathered to ornage sandy clay; I-type.||||||
20527|Woods Point Dyke Swarm|64605|5|Briefly described|Map legend|Late Devonian|Late Devonian|Quartz diorite and quartz monzonite, gabbro, peridotite, quartz-feldspar porphyry, granophyre; dykes and sills. Blue-black or dark red in RGB where visible, moderately magnetic.||||||17-NOV-08
20527|Woods Point Dyke Swarm|64606|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Quartz diorite and quartz monzonite, gabbro, peridotite, quartz-feldspar porphyry, granophyre: dykes and sills. Blue-black or dark red in RGB where visible. Nonmagnetic to moderately magnetic.||||||12-NOV-08
20527|Woods Point Dyke Swarm|64616|3|Fully described|p118, p156 Fig.6.5, p157, p167, p177|Late Devonian|Middle Devonian|See also p191, p205-206, p209, p212-214, p241, p250, p252, p255-260, p280, p286-287, p290, p302, p434-435. Of Hills (1952). K-Ar, Ar-Ar dates of Morning Star, Jericho, A1 and Mountain Home dykes ~375-387 Ma. Dating of deformation and gold mineralisation at 374 Ma sets minimum emplacement age. Hornblende Ar-Ar ages from 374 +/- 2 Ma to 387 +/- 14 Ma. Peridotite, pyroxenite, hornblendite, gabbro (common), quartzdiorite and granite dykes. Undergone two stages of hydrothermal fluids alteration. Abbreviated to Woods Point Dykes in Fig.6.5. Also hosts Cu-Ni-PGE mineralisation in mafic and ultramafic dykes. Geophysical characteristics given.||||||
20527|Woods Point Dyke Swarm|66576|5|Briefly described|pp970-972, p990.|||150 km long north-northwest trending belt of ultramafic to intermediate composition, consistent with fractional crystallisation of a single peridotitic parental magma. Underwent three stages of alteration; the last including gold mineralisation.|378-376 Ma  (Bierlein et al. 2001b).|||Intrudes Walhalla Synclinorium.|Highly-differentiated calc-alkaline series: peridotite, basic gabbros, hornblende diorites.|04-SEP-14
20527|Woods Point Dyke Swarm|67847|6|Mentioned|p45|||||||||
20527|Woods Point Dyke Swarm|68116|5|Briefly described|Appendix, Map 43.|Late Devonian|Late Devonian|Commonly weathered to orange sandy clay.|||||Hornblende-biotite quartz diorite and quartz monzonite, hornblende-biotite gabbro, hornblende-augite-biotite quartz gabbro, kaersutite-phlogopite peridotite, quartz and feldspar bearing porphyry; medium grained; common hydrothermal alteration.|
20528|Woodside Basalt|31007|6|Mentioned|p253|||See also Fig.1.  Age: 300,000 years.||||||10-OCT-07
20547|Woolamai Granite|23309|6|Mentioned|p447 App1|||G261 I-Type.||||||
20547|Woolamai Granite|24551|6|Mentioned|p266|||||||||
20547|Woolamai Granite|31510|5|Briefly described|p10|||See also Table 1.||||||
20547|Woolamai Granite|32002|6|Mentioned|p118|||||||||
20547|Woolamai Granite|33358|6|Mentioned|p23|||||||||
20547|Woolamai Granite|35290|5|Briefly described|p22|||||||||
20547|Woolamai Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
20547|Woolamai Granite|63445|5|Briefly described|Map legend.|Late Devonian|Late Devonian||||||I-type granite.|
20547|Woolamai Granite|68116|5|Briefly described|Appendix, Map 56.|Late Devonian|Late Devonian||||||Biotite granite: pink coarse-grained leucocratic; contains quartz, perthite, oligoclase, biotite and accessory apatite and zircon; veins of aplite and pegmatite present locally.|
20558|Woollybutt Quartz Monzodiorite|22876|5|Briefly described|p27|||||||||
20558|Woollybutt Quartz Monzodiorite|22877|5|Briefly described|map|Silurian|Silurian|G53. Hornblende-biotite-quartz. I-Type.||||||26-OCT-04
20558|Woollybutt Quartz Monzodiorite|23309|6|Mentioned|p447 App1|||G53 I-Type. Supersedes Woollybutt Granite.||||||
20558|Woollybutt Quartz Monzodiorite|42627|5|Briefly described|Map legend|Wenlock|Wenlock|||||||
20558|Woollybutt Quartz Monzodiorite|42647|5|Briefly described|p46|||||||||
20558|Woollybutt Quartz Monzodiorite|68116|5|Briefly described|Appendix, Map 36.|Devonian|Silurian||||||Actinolite quartz monzodiorite: porphyritic; medium grained; dark green; pyritic; I-type.|
23255|Woolshed Creek Ignimbrite|23309|4|Described|p110. Table 2.40|||Maximum Thickness: 150m.  Of the Mount Dawson Subgroup.||||||
23255|Woolshed Creek Ignimbrite|23615|3|Fully described|p104|Early Devonian|Early Devonian|Of Mount Dawson Subgroup.  Overlies Timbarra Subgroup.  150m thick at type section.||||||
23255|Woolshed Creek Ignimbrite|24551|5|Briefly described|p144|||Of the Little River Subgroup.||||||
23255|Woolshed Creek Ignimbrite|43206|5|Briefly described|map legend||Ludlow|Of Mount Dawson Subgroup.||||||
23255|Woolshed Creek Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Feldspar ignimbrite: orange with a granular appearance and minor quartz phenocrysts.|
20581|Woolshed Valley Granite|22971|5|Briefly described|p 33|||||||||
20581|Woolshed Valley Granite|23309|5|Briefly described|p349|||G193 I-Type. Supersedes Woolshed Valley Adamellite.||||||
20581|Woolshed Valley Granite|42154|6|Mentioned|Table 1 P334|||||||||
20581|Woolshed Valley Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
20581|Woolshed Valley Granite|68116|5|Briefly described|Appendix, Map 19.|Late Devonian|Late Devonian||||||Biotite-muscovite granite: coarse phenocrysts of K-feldspar, plagioclase and quartz; K-feldspar shows plagioclase overgrowths and granophyric texture with quartz.|
74951|Woori Yallock Formation|66244|3|Fully described|p3.|||New name. Derived from Woori Yallock Creek, in the Coldstream-Seville area. Mapped on the Ringwood 1:63 360 sheet (Geological Survey of Victoria 1981) as an un-named sandstone member of Humevale Siltstone; its position above Wilson Creek Shale shows it belongs instead to the Walhalla Group.||Unit in Walhalla Group.||Overlies conformably the Wilson Creek Shale. Its top is not exposed.|Turbiditic sandstone, siltstone and shale with rare diamictite and conglomerate beds; sandstone varies from quartz-rich to micaceous to lithic; shelly fossil fragments locally present.|11-FEB-15
74951|Woori Yallock Formation|68116|5|Briefly described|Appendix, Map 42.|Early Devonian|Early Devonian||||||Sandstone, siltstone, conglomerate.|
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.|
42135|Wooroonook Granite|60491|6|Mentioned|p54|||||||||
37794|Woosang Granite|23309|6|Mentioned|p447, Appendix 1|||G628, S-Type.||||||
37794|Woosang Granite|60491|4|Described|p52|||Of the Nine Mile Suite. Intrudes the Nardoo Granite and Foleys Hill pluton. S-type.||||||
37794|Woosang Granite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Nine Mile Suite. Muscovite granite: S-type, reduced; medium grained, weakly porphyritic; contains biotite and cordierite.||||||
37794|Woosang Granite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of Nine Mile Suite. Granite; reduced S-type: possible gravity response confused by responses from other intrusions nearby; K, Th and U higher than surrounding alluvium. G628a; weakly magnetic (< 10 nT) rim. G628b: essentially nonmagnetic (< 2 nT)||||||30-SEP-04
37794|Woosang Granite|66002|5|Briefly described|p6 Tb.5|||Of Nine Mile Suite. G628. Defined in Bibby and Moore 1998.||||||
37794|Woosang Granite|68116|5|Briefly described|Appendix, Map 16.|Middle Devonian|Early Devonian||||||Biotite granodiorite: S-type, reduced; medium grained; weakly porphyritic; contains cordierite.|
24123|Woranga Member|38929|6|Mentioned|Fig.6|||||||||
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.||
20629|World Hill Granite|36201|6|Mentioned|Fig.3|||||||||
83440|Wortongie pluton|73496|5|Briefly described|Map legend|Middle Devonian|Early Devonian|G653.|||||Strongly magnetically zoned, with an outer response to 150 nT above the surrounds and a nonmagnetic core; a gravity low 50 micrometres/second/second below surounds.|
83440|Wortongie pluton|73505|5|Briefly described|p19, p21|||Newly named unit in Swan Hill and parts of Balranald and Deniliquin 1:250 000 map areas, (G653). Named after Wortongie Parish. Elliptical 18 by 10 km intrusion about 10 km SE of Sea Lake. On the NW edge of Lalbert Batholith. Strongly magnetically zoned with an outer response to 150 nT above the surrounds and a nonmagnetic core. Gravity low of 50 micrometres/second/second below surrounds.|||||Granite.|
23265|Wrens Flat Andesite|23309|5|Briefly described|p36 Table 2.7|||Of the Jamieson Volcanics.||||||
23265|Wrens Flat Andesite|24551|5|Briefly described|p87|||Of the Jamieson Volcanics (fig 3.15).||||||
23265|Wrens Flat Andesite|24576|6|Mentioned|p731|||Geological Province: Lachlan Fold Belt||||||
23265|Wrens Flat Andesite|61187|5|Briefly described|p50.|Early Cambrian|Early Cambrian|||Unit in Jamieson Volcanics.||Is faulted against Warrambat Andesite Breccia.||
23265|Wrens Flat Andesite|68116|5|Briefly described|Appendix, Map 34.|Cambrian|Cambrian||||||Andesite lava, massive and pillowed.|
30507|Wroxham Granodiorite|22878|4|Described|p85|||||||||
30507|Wroxham Granodiorite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Biotite-hornblende granodiorite: grey, medium to coarse grained with abundant mafic inclusions; massive to moderately foliated; contains thin mylonite zones.||||||01-OCT-04
30507|Wroxham Granodiorite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Biotite-hornblende granodiorite: grey, medium to coarse grained with abundant mafic inclusions; massive to moderately foliated; contains thin mylonite zones.||||||01-OCT-04
30507|Wroxham Granodiorite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Biotite-hornblende granodiorite: Highly magnetic in the east (200-250 nT), non-magnetic along western margin. High K, low Th and U.||||||06-OCT-04
30507|Wroxham Granodiorite|23309|6|Mentioned|p447 App1|||G522 I-Type.||||||
30507|Wroxham Granodiorite|68116|5|Briefly described|Appendix, Map 37.|Early Devonian|Early Devonian||||||Biotite-hornblende granodiorite: grey, medium to coarse grained with abundant mafic inclusions; massive to moderately foliated; contains thin mylonite zones.|
20658|Wuk Wuk Marl|23768|5|Briefly described|p28 Fig.5, p30 Fig. 6|Middle Miocene|Middle Miocene|Geological Province: Gippsland Basin. Presented as Wuk Wuk only in the figures. See also p45, p71.||||||30-MAR-05
20658|Wuk Wuk Marl|23909|5|Briefly described|p290 Fig.3|Miocene|Miocene|Of Seaspray Group.  Geological Province: Gippsland Basin.||||||
20658|Wuk Wuk Marl|24038|5|Briefly described|p439 Fig.2|Miocene|Miocene|Geological Province: Gippsland Basin||||||
20658|Wuk Wuk Marl|24468|5|Briefly described|p405 Fig.2|Miocene|Miocene|Geological Province: Gippsland Basin||||||
20658|Wuk Wuk Marl|24551|5|Briefly described|p327 Fig. 10.33, 608|Miocene|Miocene|Of the Gippsland Limestone.||||||
20658|Wuk Wuk Marl|33459|6|Mentioned|Table 1|||||||||
20658|Wuk Wuk Marl|34954|6|Mentioned|Fig.35|||||||||
20658|Wuk Wuk Marl|37330|5|Briefly described|Table 4|||||||||
20658|Wuk Wuk Marl|41043|6|Mentioned|p105|||||||||
20658|Wuk Wuk Marl|42635|5|Briefly described|p90|||||||||
20658|Wuk Wuk Marl|42827|6|Mentioned|p334|||||||||
20658|Wuk Wuk Marl|43667|6|Mentioned|Fig.3,p12||Miocene|||||||
20658|Wuk Wuk Marl|60538|5|Briefly described|p482 Fig. 21|||Of the Seaspray Group. Geological Province: Gippsland Basin.||||||
20658|Wuk Wuk Marl|61181|5|Briefly described|p134|Middle Miocene|Middle Miocene|Of the Gippsland Limestone. Poorly bedded, brown and grey bryozoal marl. Conformably overlain by Bairnsdale Limestone Member. Max. thickness: >25m.||||||
20658|Wuk Wuk Marl|62899|5|Briefly described|p35, p37 Fig. 2|Middle Miocene|Middle Miocene|Contains ostracode assemblages.  See also p42.||||||12-DEC-06
20658|Wuk Wuk Marl|63217|5|Briefly described|p95, p98, p102.|||Gippsland Basin. Contemporaneous with Yallourn Seam; lateral equivalent to Yallourn Formation.|16.4 - 14.5 Ma.||||Marine limestone, marl and sand.|
20658|Wuk Wuk Marl|63739|5|Briefly described|p35-63|Middle Miocene|Middle Miocene|Overlies Gippsland Limestone; underlies Tambo River Formation. Geological province: Gippsland Basin.||||||01-JUL-08
20658|Wuk Wuk Marl|65717|6|Mentioned|p12|Pliocene|Miocene|Part of unnamed marine sequence.||||Unconformably overlies Gippsland Limestone.||05-SEP-17
20658|Wuk Wuk Marl|65718|6|Mentioned|p16, p10 Fig 3.2|Pliocene|Miocene|Middle Miocene minimum age.||Of the Seaspray Group.||||
20658|Wuk Wuk Marl|66181|6|Mentioned|p311|Miocene||||||||
20658|Wuk Wuk Marl|67061|6|Mentioned|p554 Fig.10.|Miocene|Miocene|Gippsland Basin, onshore.||Unit in Seaspray Group.||Overlies Gippsland Formation. Is overlain by Bairnsdale Limestone.||
20658|Wuk Wuk Marl|70076|5|Briefly described|Regional: Fig.3|Langhian|Langhian|||Seaspray Group.||Overlies Longford Limestone or Glencoe Limestone Member (Gippsland Limestone). Is overlain by Bairnsdale Limestone.||
20658|Wuk Wuk Marl|70862|6|Mentioned|p48 Fig.1|||Latrobe Valley, Gippsland Basin.||Seaspray Group.||Overlies Gippsland Limestone Formation. Is overlain by Bairnsdale Limestone.||
20658|Wuk Wuk Marl|73289|5|Briefly described|p765 Fig.2|Miocene|Miocene|||Seaspray Group.||Overlies Gippsland Limestone Formation. Is overlain by Tambo River, Bairnsdale Limestone Formations. Interfingers with (lateral facies variation of) Balook Formation.||16-MAY-23
20658|Wuk Wuk Marl|73488|5|Briefly described|p634 Fig.4|||||Seaspray Group|||Marine marls.|
75750|Wulgulmerang Volcaniclastics|68115|5|Briefly described|p4.|Devonian|Devonian|Originally Wulgulmerang Tuff (Ringwood 1955a, b); later Wulgulmerang Tuffs (Talent et al. 1975) and Wulgulmerang Ashstone (Orth et al. 1995). This last term is not recommended by the IUGS; and as the unit includes clastic and pyroclastic deposits, the name Wulgulmerang Volcaniclastics is preferred.||Unit in Snowy River Volcanic Group.||||
75750|Wulgulmerang Volcaniclastics|68116|5|Briefly described|Appendix, Map 36.|Pragian|Lochkovian||||||Sandstone, ash, pumice rich ash, mudstone, poorly welded ignimbrite, conglomerate, breccia.|
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|||
20676|Wurruk Sand Member|24468|5|Briefly described|p405 Fig.2|Pliocene|Miocene|Geological Province: Gippsland Basin||||||
20676|Wurruk Sand Member|24551|5|Briefly described|p327 Fig. 10.33|Pliocene|Pliocene|||||||
20676|Wurruk Sand Member|35273|4|Described|p262|||||||||
20676|Wurruk Sand Member|37809|6|Mentioned|p5|||||||||
20676|Wurruk Sand Member|42827|4|Described|p336|||Of the Boisdale Formation.||||||13-DEC-06
20676|Wurruk Sand Member|61207|5|Briefly described|p280 Fig. 2||Late Pliocene|Geological Province: onshore Gippsland Basin.||||||12-JAN-06
20676|Wurruk Sand Member|62899|5|Briefly described|p37 Fig. 2|||Geological province: Lakes Entrance Platform.||||||12-DEC-06
20676|Wurruk Sand Member|63739|5|Briefly described|p37 Fig. 2|||Geological province: Gippsland Basin.||||||01-JUL-08
20676|Wurruk Sand Member|65718|6|Mentioned|p10 Fig 3.2|Pleistocene|Pliocene|||||||
20679|Wurutwun Formation|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Jordan River Group.||||||27-OCT-08
20679|Wurutwun Formation|23309|5|Briefly described|p142, 144-157. Table 2.54.||Lochkovian|||||||
20679|Wurutwun Formation|24177|5|Briefly described|p50 Fig.22|Early Devonian|Early Devonian|Geological Province: Mount Easton Province.||||||
20679|Wurutwun Formation|24551|5|Briefly described|p123|||Of the Jordan River Group?||||||
20679|Wurutwun Formation|41571|6|Mentioned|Fig.2.7|||||||||
20679|Wurutwun Formation|41585|4|Described|p118|||||||||
20679|Wurutwun Formation|41868|5|Briefly described|p574|||||||||
20679|Wurutwun Formation|42418|5|Briefly described|p235|||Supersedes? Coopers Creek Formation?||||||
20679|Wurutwun Formation|42827|4|Described|p118|||see also Table 4.1||||||
20679|Wurutwun Formation|44187|5|Briefly described|Map Legend||Early Devonian|||||||
20679|Wurutwun Formation|60599|5|Briefly described|p47 Fig. 19|Emsian|Lochkovian|Geological Province: Melbourne Zone, Lachlan Fold Belt.||||||
20679|Wurutwun Formation|61185|6|Mentioned|p39|||Part of this unit correlates with Wilson Creek Shale near Walhalla (Carey, 1975).||||||07-FEB-11
20679|Wurutwun Formation|64535|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Gp. Siltstone, lithic sandstone, conglomerate, limestone, chert, rare black shale; siltstone, well bedded/finely banded, coarser components lenticular; chert, black shale bodies+ limestone are olistoliths; deep-marine+ mass-flow deposits.||||||22-DEC-08
20679|Wurutwun Formation|64536|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Gp. Siltstone, lithic sandstone, conglomerate, limestone, chert, rare black shale; siltstone, well bedded/finely banded, coarser components lenticular; chert, black shale bodies+ limestone are olistoliths; deep-marine+ mass-flow deposits.||||||07-FEB-11
20679|Wurutwun Formation|64537|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Gp. Siltstone, lithic sandstone, conglomerate, limestone, chert, rare black shale; siltstone, well bedded/finely banded, coarser components lenticular; chert, black shale bodies+ limestone are olistoliths; deep-marine+ mass-flow deposits.||||||07-FEB-11
20679|Wurutwun Formation|64538|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Gp. Siltstone, lithic sandstone, conglomerate, limestone, chert, rare black shale; siltstone, well bedded/finely banded, coarser components lenticular; chert, black shale bodies+ limestone are olistoliths; deep-marine+ mass-flow deposits.||||||07-FEB-11
20679|Wurutwun Formation|64539|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Gp. Siltstone, lithic sandstone, conglomerate, limestone, chert, rare black shale; siltstone, well bedded/finely banded, coarser components lenticular; chert, black shale bodies+ limestone are olistoliths; deep-marine+ mass-flow deposits.||||||22-DEC-08
20679|Wurutwun Formation|64540|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of Jordan River Gp. Siltstone, lithic sandstone, conglomerate, limestone, chert, rare black shale; siltstone, well bedded/finely banded, coarser components lenticular; chert, black shale bodies+ limestone are olistoliths; deep-marine+ mass-flow deposits.||||||22-DEC-08
20679|Wurutwun Formation|64605|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Jordan River Group. Siltstone, lithic sandstone, conglomerate, limestone lenses; black shale, chert; deep-marine deposits. Speckled blue-green to yellow-pink in RGB. Nonmagnetic.||||||17-NOV-08
20679|Wurutwun Formation|64616|3|Fully described|p97, p155, p173-175, p286, p295, p304|Pragian|Lochkovian|See also p385 Tb.1, p387, p390. Of Jordan River Group. Faulted against Walhalla Group to west and Jordan River Group to east. 100-180m estimated thickness. Age from fossils in limestone olistoliths and correlation with Wilson Creek Shale and Coopers Creek Limestone. Black siltstone interbedded with quartz sandstone; contains megaclasts of chert and limestone. Geophysical characteristics given. Trilobite fossils listed.||||||
20679|Wurutwun Formation|68116|5|Briefly described|Appendix, Maps 43, 52.|Emsian|Lochkovian|Limestone occurs as sharply bounded pods tens of metres across with discordant bedding.|||||Siltstone, with minor lithic sandstone, conglomerate, limestone lenses, black shale, chert; occasional thick conglomerate with mudstone matrix, large clasts of lithic sandstone and granulestone, chert, siltstone, basalt, limestone.|
20684|Wy Yung Gravel Member|35273|5|Briefly described|p261|||||||||
20684|Wy Yung Gravel Member|41075|6|Mentioned|p24|||||||||
20684|Wy Yung Gravel Member|42827|5|Briefly described|p335|||of Tambo River Formation||||||
20707|Wycheproof Granite|23309|5|Briefly described|p339.|Devonian|Silurian|G332 S-Type. Age: 399+/-8Ma, 387+/-6Ma, 405+/-8Ma, 407+/-6Ma.||||||
20707|Wycheproof Granite|24551|6|Mentioned|p665, 717 Table 2.4|Early Devonian|Early Devonian|Age: 399 +/- 8Ma.||||||
20707|Wycheproof Granite|35278|6|Mentioned|p353|||||||||
20707|Wycheproof Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
20707|Wycheproof Granite|60491|4|Described|p31, p38|Devonian|Late Silurian|Of the Glenloth Suite. Age: 407+/-6 Ma to 387+/-6 Ma (K/Ar). Intruded by the Jeffcott Granite and the Narraport pluton.||||||
20707|Wycheproof Granite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Glenloth Suite. Leucocratic granite: white to grey coarse grained; highly fractionated; very rare garnet, biotite and topaz.||||||29-SEP-04
20707|Wycheproof Granite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of the Glenloth Suite. Age: 399+/-8, 400+/-6, 407+/-6 Ma (K/Ar). Granite; reduced S-type; gravity response part of southern edge regional low; rare outcrops show K & U higher, Th lower than surrounding alluvium.||||||
20707|Wycheproof Granite|66002|5|Briefly described|p6 Tb.5|||Of Glenloth Suite. G332. Defined in Bibby and Moore 1998.||||||
20707|Wycheproof Granite|67347|5|Briefly described|p836, p838, p842, p844|Early Devonian|Early Devonian|Intrusion that projects through the Cenozoic sediments of the Murray Basin. Sampled for uranium phosphate weathering minerals.||||||11-MAY-12
20707|Wycheproof Granite|68116|5|Briefly described|Appendix, Map 16.|Middle Devonian|Early Devonian||||||Biotite-muscovite granite: coarse grained, pale grey.|
20707|Wycheproof Granite|68189|6|Mentioned|p42 App.2|Carboniferous|Devonian|A range of ages is provided from several researchers.|407 +/- 6 to 331 +/- 15 Ma.|||||30-JUN-14
20707|Wycheproof Granite|73505|5|Briefly described|p6 Tb.3.1, p34|Middle Devonian|Early Devonian|Of Lalbert Batholith. Ages provided from Richards and Singleton, (1981), Bowen (1975), McKenzie et al., (1984).|399+/-8 Ma, 407+/-6 Ma K/Ar on muscovite|||||
27022|Wychitella Granite|23309|5|Briefly described|App1|||G363 I-Type.||||||
27022|Wychitella Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
27022|Wychitella Granite|60491|4|Described|p50|Devonian|Devonian|Of the Mount Cole Suite. Age: 370+/-1 Ma (Rb/Sr). Intrudes the Yeungroon Granite and the Foleys Hill pluton. I-type.||||||
27022|Wychitella Granite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Mount Cole Suite. Biotite granite: I-type, oxidised; medium grained, pinkish grey, with rare mafic enclaves.||||||
27022|Wychitella Granite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of the Mount Cole Suite. Age: 395 +/- 1 Ma (Rb/Sr). Granite; oxidised I-type: highly magnetic (to 400 nT), showing concentric layering; rare outcrops show high K, moderate Th, U.||||||30-SEP-04
27022|Wychitella Granite|66002|5|Briefly described|p7 Tb.5|||Of Mount Cole Suite. G363. Defined in Bibby and Moore 1998.||||||
27022|Wychitella Granite|68116|5|Briefly described|Appendix, Map 16.|Middle Devonian|Early Devonian||||||Biotite granite: I-type, oxidised; medium grained pinkish grey, with rare mafic enclaves.|
32186|Xmas Quartz Monzonite|22815|4|Described|p85|||||||||
32186|Xmas Quartz Monzonite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Xmas Suite.||||||
31665|Xmas Suite|22815|4|Described|p85|||Consists of two members.||||||
31665|Xmas Suite|22878|6|Mentioned|p83|||||||||
31665|Xmas Suite|24551|6|Mentioned|p236|||||||||
31665|Xmas Suite|42726|5|Briefly described|Map Legend||Early Devonian|||||||
31665|Xmas Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||
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.|
31667|Yabba Suite|42726|5|Briefly described|Map Legend||Silurian|||||||
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.||||||
20753|Yalca Member|35091|6|Mentioned|Table 1|||||||||
20753|Yalca Member|42966|5|Briefly described|p410, p201|||of Shepparton Formation. Variation on Yalca Sand Member.||||||
24593|Yallock Formation|23262|5|Briefly described|Fig13-1.1p290, 292, 302|Pliocene|Oligocene|||||||
24593|Yallock Formation|36197|4|Described|p10|||See also Table 1.||||||
24593|Yallock Formation|37366|5|Briefly described|p4|||||||||
24593|Yallock Formation|40523|6|Mentioned|Table 1|||||||||
24593|Yallock Formation|41868|5|Briefly described|p553|||||||||
24593|Yallock Formation|42827|6|Mentioned|p553|||||||||
24593|Yallock Formation|61181|6|Mentioned|p183|||Useful quartz sand resource in west central Gippsland. ||||||
20769|Yallourn Formation|23230|5|Briefly described|Table4-1p40|Miocene|Miocene|||||||
20769|Yallourn Formation|23264|5|Briefly described|Table13-3.1p325||Miocene|||||||
20769|Yallourn Formation|23909|5|Briefly described|p290 Fig.3|Miocene|Miocene|Geological Province: Gippsland Basin.||||||
20769|Yallourn Formation|24002|5|Briefly described|p241 fig. 10|Miocene|Oligocene|Geological Province: Gippsland Basin.||||||25-SEP-08
20769|Yallourn Formation|24053|5|Briefly described|p37|Miocene|Eocene|Of Latrobe Group. Geological Basin: Gippsland Basin.||||||25-SEP-08
20769|Yallourn Formation|24551|5|Briefly described|p325, 498 Fig. 16.8|Miocene|Miocene|Of the Latrobe Valley Group.||||||
20769|Yallourn Formation|31188|6|Mentioned|p108|||Middle Miocene||||||
20769|Yallourn Formation|31352|6|Mentioned|Fig. 3|||Miocene||||||
20769|Yallourn Formation|32679|6|Mentioned|p94|||Strat. diagram||||||
20769|Yallourn Formation|34815|6|Mentioned|p15|||||||||
20769|Yallourn Formation|34991|6|Mentioned|p382|||||||||
20769|Yallourn Formation|35273|5|Briefly described|p257|||See also P266.||||||
20769|Yallourn Formation|37530|5|Briefly described|p9|||||||||
20769|Yallourn Formation|38417|6|Mentioned|p87|||||||||
20769|Yallourn Formation|38928|6|Mentioned|Fig.14|||||||||
20769|Yallourn Formation|38929|6|Mentioned|p51|||||||||
20769|Yallourn Formation|38973|6|Mentioned|Fig.2|||||||||
20769|Yallourn Formation|40114|6|Mentioned|p1|||||||||
20769|Yallourn Formation|40117|6|Mentioned|p61|||||||||
20769|Yallourn Formation|41868|5|Briefly described|p521|||||||||
20769|Yallourn Formation|42184|6|Mentioned|Fig.2 P348|||||||||
20769|Yallourn Formation|42648|5|Briefly described|p45|||||||||
20769|Yallourn Formation|42649|4|Described|p204|||||||||
20769|Yallourn Formation|42827|5|Briefly described|p341|||||||||
20769|Yallourn Formation|43145|6|Mentioned|p11|Middle Miocene|Early Miocene|Of Latrobe Valley Coal Measures.||||||25-SEP-08
20769|Yallourn Formation|60538|5|Briefly described|p472 Fig. 11, 488 Fig. 27|Middle Miocene|Early Miocene|||||||
20769|Yallourn Formation|61155|5|Briefly described|p4, p18|Late Miocene|Early Miocene|Of the Latrobe Group. Thick sequences of lignite and clastics accumulated in peat swamps. Thickness: 250m. Geological Province: Gippsland Basin (LaTrobe Valley).||||||
20769|Yallourn Formation|61336|4|Described|p(v) Fig. 5|Middle Miocene|Early Miocene|Of Seaspray Gp. Comprises mainly the Yallourn coal seam, but may include up to 200m of clay above the seam in deeper synclines. Conformably overlies Morwell Fm; grades laterally into the Seaspray Gp barrier sands.||||||07-FEB-11
20769|Yallourn Formation|63217|6|Mentioned|p96 Fig.1, p105.  |||Gippsland Basin. Lateral equivalent to Wuk Wuk Marl Formation.||||||
20769|Yallourn Formation|65718|6|Mentioned|p10, p12|Miocene|Miocene|||Of the Latrobe Valley Group.||||
20769|Yallourn Formation|67061|6|Mentioned|p554 Fig.10.|Miocene|Miocene|Latrobe Valley, Gippsland Basin.||Unit in Latrobe Valley Group.||Overlies Morwell Formation.||
20769|Yallourn Formation|67727|5|Briefly described|p55. |Neogene|Neogene|Onshore coal-bearing equivalent of the Seaspray Group.||||Overlies Traralgon Formation.||
20769|Yallourn Formation|69016|5|Briefly described|p88-89|||Of the Gippsland Basin. Sands are major aquifers with hydraulic conductivities of up to 100 m/day.||Unit of Latrobe Valley Group.||Laterally grades into upper unit of Balook Formation.|Predominantly coal seams interbedded with sands and clays.|
20769|Yallourn Formation|69750|6|Mentioned|p68|Miocene|Miocene|On-shore Gippsland Basin.||Latrobe Valley Group.||Overlies Morwell Formation. Is overlain unconformably by Haunted Hills Formation.||
20769|Yallourn Formation|70076|5|Briefly described|Regional: Fig.3|Tortonian|Burdigalian|Also is shown with an uppermost subunit marked Post Yallourn Clay.||Latrobe Valley Subgroup.|Yallourn Seam and Yallourn Clay.|Overlies Morwell Formation. Is overlain by Haunted Hills Formation (Sale Subgroup).||
20769|Yallourn Formation|70862|6|Mentioned|p48 Fig.1, p49-50|||Latrobe Valley, Gippsland Basin. Middle Miocene. The name Yallourn Seam (also presented as Yallourn seam) is apparently used as an equivalent term; see p50-51, 55, 59.|15.9-11.6 Ma (Holdgate et al., 2007).|Latrobe Valley Group.||Overlies Morwell Formation. Is overlain unconformably by the Haunted Hill Formation.||
20769|Yallourn Formation|73289|5|Briefly described|p764, 765 Fig.2|Miocene|Miocene|||||Overlies Morwell Formation. Is overlain unconformably by Haunted Hill Formation.|Coal seams.|
20769|Yallourn Formation|73488|5|Briefly described|p631-632, p634 Fig.4, p636-637, p644|Miocene|Miocene|Gippsland Basin, Latrobe Valley depression. Approximately equates with Triporopollenites bellus (miospore) Zone of Partridge (1971).||||Overlies Morwell Formation, grades laterally into the Balook Formation. Correlated with upper part of Gippsland Limestone.|Non-marine claystones and sandstones, brown coal seams.|
20769|Yallourn Formation|73562|6|Mentioned|p300, 303-304, 306, 310, 313|Miocene|Miocene|Gippsland Basin; onshore.||||||
20769|Yallourn Formation|75065|5|Briefly described|p151|Miocene|Miocene|Gippsland Basin; onshore.||Latrobe Valley Group.||Overlies Morwell Formation. Is overlain unconformably by Sale Group.|Coal.|
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.|
27026|Yaloak Formation|24038|4|Described|p441|Eocene|Eocene|Geological Province: Port Phillip Basin.||||||12-JAN-10
27026|Yaloak Formation|24551|6|Mentioned|p310 Fig. 10.18|||||||||
27026|Yaloak Formation|30929|6|Mentioned|Map legend|Paleocene|Paleocene|||||||
27026|Yaloak Formation|33458|6|Mentioned|Fig.2|||||||||
27026|Yaloak Formation|33464|6|Mentioned|Table 1|||||||||
27026|Yaloak Formation|33604|6|Mentioned|p20|||||||||
27026|Yaloak Formation|34956|6|Mentioned|p84|||||||||
27026|Yaloak Formation|34961|6|Mentioned|p428|||||||||
27026|Yaloak Formation|34992|6|Mentioned|p406|||||||||
27026|Yaloak Formation|39865|5|Briefly described|p28|||||||||
27026|Yaloak Formation|42827|5|Briefly described|p310 Fig. 10.18, p315|||||||||19-JUL-04
27026|Yaloak Formation|60083|5|Briefly described|Map legend|Oligocene|Oligocene|Stated to be synonymous with Werribee Formation.  Sand, sandy and silty clay, with pyritic and lignitic bands.||||||
27026|Yaloak Formation|64314|5|Briefly described|p498 Fig. 3, p502 Fig. 7|||Thickness: ~140m. See also p500 Fig. 5.||||||21-OCT-08
27026|Yaloak Formation|65715|5|Briefly described|p11 Tb.7, p12-13|Paleogene|Maastrichtian|Of Thomas and Baragwanath (1950). Said to underlie 'Lerderderg Formation' [?Lerderderg Gravel Member]. Holdgate et al. (2002) report spores/pollen as old as Maastrichtian. Poor description makes this unit difficult to distinguish lithologically from Werribee Formation. Grey clays with fossiliferous ferruginous bands, gravels and thin coal seams. Potentially laterally continuous with White Hills Gravel. See also Lal Lal Formation.||||||06-FEB-15
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.|
30512|Yambulla Granodiorite|22878|4|Described|p83|||||||||
30512|Yambulla Granodiorite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Of the Kameruka Supersuite. Biotite granodiorite: pale grey, medium grained, massive||||||01-OCT-04
30512|Yambulla Granodiorite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Kameruka Supersuite. Biotite granodiorite: pale grey, medium grained, massive||||||01-OCT-04
30512|Yambulla Granodiorite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Kameruka Supersuite. Biotite granodiorite: highly magnetic (300-320 nT). High K, low Th and U.||||||06-OCT-04
30512|Yambulla Granodiorite|23309|6|Mentioned|p448 App1|||G521 I-Type.||||||
30512|Yambulla Granodiorite|68116|5|Briefly described|Appendix, Map 37.|Early Devonian|Early Devonian||||||Biotite granodiorite: pale grey, medium grained, massive.|
20800|Yan Yean Formation|22542|6|Mentioned|p662|||||||||
20800|Yan Yean Formation|22684|4|Described|p752, Fig.2 p746|Ludlow|Wenlock|See also p745, p755.||||||14-APR-08
20800|Yan Yean Formation|23309|5|Briefly described|p139-141, 150.|||||||||
20800|Yan Yean Formation|31852|6|Mentioned|p720|||Ludlovian. Correlation. See also Fig.5.||||||14-APR-08
20800|Yan Yean Formation|33020|6|Mentioned|p234|||Frequency anal. of sand-silt ratio of couplets.||||||
20800|Yan Yean Formation|33326|6|Mentioned|p431|||Fauna.||||||
20800|Yan Yean Formation|33599|6|Mentioned|p3|||Refers Williams (1964).||||||
20800|Yan Yean Formation|35283|5|Briefly described|p47|||||||||
20800|Yan Yean Formation|37727|5|Briefly described|p53|||See also P35.||||||
20800|Yan Yean Formation|42826|6|Mentioned|p45|||||||||
20800|Yan Yean Formation|61138|5|Briefly described|p218|Early Ludlow|Late Wenlock|Four cephala described as Ananaspis sp. 1 (Sandford 1996) belong to Lochkovella longisculcata.||||||
20800|Yan Yean Formation|61185|6|Mentioned|p22, p24-25 Fig. 7, p45|||Of Williams (1964). Conformable under Humevale Siltstone. A Dargile Formation equivalent.||||||07-FEB-11
20800|Yan Yean Formation|62469|6|Mentioned|p5 Fig. 2, p35, p15|Ludlow|Wenlock|Unit in Victoria. Includes Mullum Mullum Sandstone Member in Melbourne-Lilydale area. Geological Province: Darraweit Guim Province. See also p20 Fig. 11.||||||12-FEB-15
20800|Yan Yean Formation|63083|5|Briefly described|p216 Tb. 1, p217|Ludlow|Wenlock|See also p225.||||||07-FEB-11
20800|Yan Yean Formation|66244|5|Briefly described|p3.|||Shown as Dargile Formation on the Yan Yean 1:63 360 map (Garratt 1972). Now replaced by the Humevale Siltstone in the Merriang-Wandong area, continuing all the way to Kilmore.||||Is overlain by Clonbinane and Mount Phillipa Members.||
25661|Yanakie Granite|23309|6|Mentioned|p448 App1|||G254 S-Type.||||||
25661|Yanakie Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
25661|Yanakie Granite|68116|5|Briefly described|Appendix, Map 57.|Middle Devonian|Middle Devonian||||||Granite, S-type.|
39709|Yando Member|2967|5|Briefly described|p31 Fig.2.15|||Western Loddon Plain, eastern Murray Basin. Is presented also as Yando Clay (p14, 32, 40, 46) and Yando Clay Member (p22, 30).||Shepparton Formation.||Overlies Calivil Formation.|Red and grey clay.|
39709|Yando Member|24439|5|Briefly described|p37|||Basal unit of the Shepparton Formation.||||||
20821|Yangery Basalt|31004|6|Mentioned|p394|||||||||
20821|Yangery Basalt|32102|6|Mentioned|p175|||Late Pliocene age||||||
20821|Yangery Basalt|34993|6|Mentioned|p303|||||||||
20821|Yangery Basalt|35625|6|Mentioned|Fig.1|||||||||
20821|Yangery Basalt|41848|6|Mentioned|p378|||Age 1.95 my K-Ar||||||
29702|Yarak Granite|23309|6|Mentioned|p448 App1|||G501 I-Type.||||||
29702|Yarak Granite|43314|5|Briefly described|Map Legend|Wenlock|Wenlock|I-type. Weakly foliated porphyritic biotite hornblende felsic granite||||||22-OCT-04
29702|Yarak Granite|43315|5|Briefly described|Map Legend|Wenlock|Wenlock|I-type granite. Weakly foliated porphyritic biotite hornblende felsic granite.||||||03-MAY-05
29702|Yarak Granite|60541|5|Briefly described|p68-69|Silurian|Silurian|Newly defined felsic intrusive body overlain by Tertiary gravels- with varied distribution of mafic minerals (biotite and rarely hornblende). Geological Province: Lachlan Fold Belt.  Type locality given. See also p18 Tb. 1.||||||27-JUN-14
29702|Yarak Granite|68116|5|Briefly described|Appendix,|Devonian|Silurian||||||Biotite-hornblende granite: felsic; porphyritic; weakly foliated; I-type.|
29186|Yarra Delta Group|24551|5|Briefly described|p388 Fig. 11.2|Late Pleistocene|Early Pleistocene|||||||
29186|Yarra Delta Group|35011|3|Fully described|p311|||||||||
29186|Yarra Delta Group|35712|6|Mentioned|Table 6|||||||||
29186|Yarra Delta Group|41848|5|Briefly described|p389, Table 9.7|Quaternary|Quaternary|||||||
29186|Yarra Delta Group|42827|5|Briefly described|Table 9.7|||||||||
29186|Yarra Delta Group|71277|5|Briefly described|p302-303, p307|Quaternary|Quaternary|Nielson and Jenkin (1967).|||Port Melbourne Sand, Coode Island Silt, Fishermens Bend Silt, Moray Street Gravels, Jolimont Clay, Burnley Basalt Flow.|||
83446|Yarraberb pluton|73497|5|Briefly described|Map legend|Devonian|Silurian|G344.|||||Granite: highly magnetic (up to 300 nT) with a moderately magnetic part (100 nT) and nonmagnetic core; gravity low of 60 micrometres/second/second.|
24138|Yarragon Formation|24551|6|Mentioned|p504|||See Yallourn Formation.||||||
24138|Yarragon Formation|40114|2|Defined|Appdx II|middle Miocene|middle Miocene|||||||
24138|Yarragon Formation|41868|6|Mentioned|p498|||||||||
24138|Yarragon Formation|42827|5|Briefly described|p341|||||||||
24138|Yarragon Formation|61336|5|Briefly described|p(ix) Fig. 9|Late Miocene|Middle Miocene|Coal-bearing sequence in Moe Swamp Basin of similar age to Yallourn Fm - including upper A seam (15m thick) and lower B seam (36m thick). Max. thick: 200m. Geological Province: Gippsland Basin. See also p(xiii).||||||07-FEB-11
24138|Yarragon Formation|69016|6|Mentioned|p89|||Of the Gippsland Basin.||||||
24138|Yarragon Formation|73289|6|Mentioned|p767|Miocene|Miocene|Thorpdale-Moe area, Gippsland Basin.||||Overlies Thorpdale Volcanics.||
24138|Yarragon Formation|73488|6|Mentioned|p632 Fig.2|Miocene|Miocene|Gippsland Basin. Shown as laterally equivalent to Yallourn Formation plus the upper part of the Morwell Formation.|||Shown as including the Moe A and Moe B Seams.|||
20880|Yarram Formation|24551|5|Briefly described|p327 Fig. 10.33, p498 Fig. 16.8|Eocene|Paleocene|||||||
20880|Yarram Formation|34842|4|Described|p19|||||||||
20880|Yarram Formation|35273|4|Described|p256|||||||||
20880|Yarram Formation|37530|3|Fully described|p5|||||||||
20880|Yarram Formation|38929|6|Mentioned|p45|||||||||
20880|Yarram Formation|38930|5|Briefly described|p58|||||||||
20880|Yarram Formation|38931|6|Mentioned|p80|||||||||
20880|Yarram Formation|42184|6|Mentioned|Fig.2 P348|||||||||
20880|Yarram Formation|42649|5|Briefly described|Fig.3 P197-198|||||||||
20880|Yarram Formation|42827|4|Described|p330|||see also Fig 8.20||||||
20880|Yarram Formation|61336|5|Briefly described|p(v) Fig. 5, p(ix)|Late Paleocene|Middle Paleocene|Of Latrobe Group. Comprised predominantly of pebbly to coarse-grained sands; no known coal seams of any significance. Max. thickness: 47m. Geological Province: Gippsland Basin. See also p(ix) Fig. 9.||||||07-FEB-11
20880|Yarram Formation|65718|5|Briefly described|p10 Fig 3.2, p12, p38|Eocene|Late Cretaceous|Equivalent in age to the Halibut Subgroup.||||Overlain by the Carrajung Volcanics.|Comprises fluvial/alluvial conglomerates, sandstones, thin coals and shales.|
20880|Yarram Formation|75065|5|Briefly described|p151|Paleocene|Paleocene|Gippsland Basin; onshore.||Halibut Subgroup.||Abuts Barracouta Formation. Is overlain by Currajung Volcanics.|Non-marine conglomerate, siltstone.|
40705|Yat Nat Ignimbrite|23309|5|Briefly described|p81|||Of the Rocklands Volcanics.||||||
40705|Yat Nat Ignimbrite|50154|2|Defined|p118, p245 App.5|Devonian|Devonian|Of the Rocklands Volcanic Group. Overlain by the Barangaroo Ignimbrite.||||||15-SEP-04
40705|Yat Nat Ignimbrite|50155|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Quartz-feldspar ignimbrite||||||
40705|Yat Nat Ignimbrite|50156|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pumice-rich, lithic-poor, up to 10% orthoclase phenocrysts up to 3mm in a densely welded matrix||||||
40705|Yat Nat Ignimbrite|50157|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pumice-rich, lithic-poor, up to 10% orthoclase phenocrysts up to 3mm in a densely welded matrix||||||
40705|Yat Nat Ignimbrite|50158|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pumice-rich, lithic-poor, up to 10% orthoclase phenocrysts up to 3mm in a densely welded matrix||||||
40705|Yat Nat Ignimbrite|50159|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pumice-rich, lithic-poor, up to 10% orthoclase phenocrysts up to 3mm in a densely welded matrix||||||24-JUN-04
40705|Yat Nat Ignimbrite|50160|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz-feldspar ignimbrite||||||
40705|Yat Nat Ignimbrite|50161|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pumice-rich, lithic-poor, up to 10% orthoclase phenocrysts up to 3mm in a densely welded matrix||||||24-JUN-04
40705|Yat Nat Ignimbrite|50162|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pumice-rich, lithic-poor, up to 10% orthoclase phenocrysts up to 3mm in a densely welded matrix||||||24-JUN-04
40705|Yat Nat Ignimbrite|50163|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of Rocklands Volcanic Group. Quartz feldspar ignimbrite: pumice-rich, lithic-poor, up to 10% orthoclase phenocrysts up to 3mm in a densely welded matrix||||||21-JUN-04
40705|Yat Nat Ignimbrite|66002|5|Briefly described|p6 Tb.4|Devonian|Devonian|Of Rocklands Volcanic Group. Defined by Simpson in Morand et al. 2003.||||||
77105|Yaugher Volcanic Group|65715|5|Briefly described|p11 Tb.7|Paleogene|Paleogene|Lava and breccia. Subdivided by Tickell et al. (1992 [actually 1991]) into four unnamed units.||||||
77105|Yaugher Volcanic Group|66002|5|Briefly described|p10 Tb.7|Paleogene|Paleogene|Lava and breccia. Four unnamed units recognised by Tickell et al. (1992)[actually 1991].||||||27-MAY-13
77105|Yaugher Volcanic Group|68116|5|Briefly described|Appendix, Maps 49, 55.|Eocene|Eocene||||||Olivine basalt, tuff, microgabbro, minor sedimentary rocks.|
24139|Yea Formation|13996|6|Mentioned|p148-149|Ludlow|Ludlow|Yea area. Hosts a teleostome tail, the only Silurian articulated vertebrate yet found in Australia. Hosts Baragwanatha flora in the lower plant horizon, as well as thallophytes (named).||||||
24139|Yea Formation|23229|6|Mentioned|Plate3-3p35||Late Silurian|||||||
24139|Yea Formation|23309|5|Briefly described|p140|||||||||
24139|Yea Formation|24177|5|Briefly described|p50 Fig.22|Ludlow|Ludlow|Geological Province: Darraweit Guim Province.||||||27-OCT-08
24139|Yea Formation|24249|5|Briefly described|p90 Fig.3, p93|Pridoli|Pridoli|Overlying Unit: Humevale Formation.||||||27-OCT-08
24139|Yea Formation|38787|6|Mentioned|p124|||||||||
24139|Yea Formation|41585|4|Described|p110|||||||||
24139|Yea Formation|41933|6|Mentioned|p649|||||||||
24139|Yea Formation|42033|5|Briefly described|p649|||||||||
24139|Yea Formation|42827|4|Described|p110|||see also Table 4.1||||||
24139|Yea Formation|60599|5|Briefly described|p47 Fig. 19, p56, p67|Ludlow|Ludlow|Geological Province: Darraweit Guim Province, Melbourne Zone, Lachlan Fold Belt. In the Yea area considered as part of the lithologically variable Norton Gully Sandstone.||||||
24139|Yea Formation|61185|5|Briefly described|p45, p21 Fig. 6, p24-25 Fig. 7|Ludlow|Ludlow|Of Garratt (1986). Formerly considered to be overlain by superdseded Humevale Formation (now Siltstone). Now considered to belong to Norton Gully Sandstone. Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
24139|Yea Formation|66498|6|Mentioned|p41|||||||||
24139|Yea Formation|68298|5|Briefly described|p219|Ludlow|Ludlow|An indeterminate acanthodian fish from Yea district of Victoria is associated with the plant Baragwanathia in the uppermost beds of this formation (eg. Garratt and Wright 1988).||||||
24139|Yea Formation|70487|6|Mentioned|p9|Devonian|Devonian|Of Garratt (1977, 1983). Replaced by Broadford Formation in the Yea Anticline.||||||
30049|Yeerung River Volcanics|23309|5|Briefly described|p124. Table 2.48|||not included in the Snowy River Volcanics||||||19-MAY-05
30049|Yeerung River Volcanics|24551|5|Briefly described|p151|||See also Yerrung River volcanics.||||||
30049|Yeerung River Volcanics|43314|5|Briefly described|Map Legend||Emsian|of Snowy River Volcanics.||||||
30049|Yeerung River Volcanics|43315|5|Briefly described|Map Legend|Emsian|Emsian|Of the Snowy River Volcanics. Quartz-feldspar porphyry with large phenocrysts; undifferentiated volcanic pyroclastics and epiclastics.||||||03-MAY-05
30049|Yeerung River Volcanics|60541|4|Described|p13, p57|Early Devonian|Early Devonian|See also Yeerung Volcanics - names used interchangeably. Composed of lithic clasts (plagioclase and anhedral quartz grains in a very fine matrix), predominantly volcanic in composition, with some quartzite and calcite. A Snowy River Volcanics equivalent.||||||12-JAN-06
30049|Yeerung River Volcanics|68116|5|Briefly described|Appendix, Map 45.|Early Devonian|Early Devonian|Informally subdivided into a porphyritic phase.|||||Volcanic breccia: lithic clasts of felsic lava and minor quartzite and limestone; pyroclastic or epiclastic deposit. Porphyry: quartz-feldspar porphyry with large phenocrysts; subvolcanic intrusive.|
76921|Yellingbo Porphyry|66244|5|Briefly described|p4.|||New name. A series of small ring dykes NE of Melbourne, previously shown as un-named felsic porphyry dykes; non-continuous and linked by faults including the Yellingbo Fault running NE from the Dandenong Igneous Complex.|||||Mid-dark grey quartz-feldspar porphyry with large quartz and smaller feldspar phenocrysts, and minor biotite in a fine-grained groundmass.|
76921|Yellingbo Porphyry|68116|5|Briefly described|Appendix, Map 42.|Late Devonian|Late Devonian||||||Quartz-feldspar porphyry: mid- to dark grey; large quartz and smaller feldspar phenocrysts, minor biotite in fine-grained groundmass.|
20932|Yellow Bluff beds|41043|6|Mentioned|p96|||||||||
23302|Yellow Waterholes Ignimbrite|23309|4|Described|p111. Table 2.40|||||||||
23302|Yellow Waterholes Ignimbrite|23615|3|Fully described|p119, p23, p92|Early Devonian|Early Devonian|Of Little River Subgroup.  Overlain by Fairy Sandstone, overlies Timbarra Subgroup.  Maximum thickness: 400m.  Age: Early Devonian ~410-395Ma.||||||16-AUG-18
23302|Yellow Waterholes Ignimbrite|24551|5|Briefly described|p143|||Of the Tara Range Subgroup.||||||
23302|Yellow Waterholes Ignimbrite|43206|5|Briefly described|map legend||Lochkovian|of Little River Subgroup.||||||
23302|Yellow Waterholes Ignimbrite|43312|5|Briefly described|Map Legend||Early Devonian|of Mount Dawson Subgroup||||||
23302|Yellow Waterholes Ignimbrite|43313|5|Briefly described|Map Legend||Early Devonian|of Mount Dawson Subgroup||||||
23302|Yellow Waterholes Ignimbrite|60542|3|Fully described|p53, p14|Early Devonian|Early Devonian|Tentatively placed in Mount Dawson Subgroup (Snowy River Volc's). Previously grouped in Little River Subgroup. Three members: pyroclastics, pyroclastic mass flows, and ignimbrite with interbedded fall deposits and fluvial sed's. ||||||
23302|Yellow Waterholes Ignimbrite|68115|5|Briefly described|p4.|Devonian|Devonian|Previously part of the Little River Subgroup (Orth et al. 1995); included in the Tara Range Subgroup by VandenBerg et al. (2000).||Unit in Tara Range Subgroup.||||
23302|Yellow Waterholes Ignimbrite|68116|5|Briefly described|Appendix, Map 36.|Pragian|Pragian||||||Quartz-feldspar ignimbrite: small phenocrysts, pink to purple vitric matrix.|
20967|Yeringberg Formation|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Walhalla Group.||||||27-OCT-08
20967|Yeringberg Formation|23309|5|Briefly described|p146. Table 2.55|||||||||
20967|Yeringberg Formation|24177|5|Briefly described|p50 Fig.22|Emsian|Emsian|Geological Province: Darraweit Guim Province.||||||27-OCT-08
20967|Yeringberg Formation|41585|4|Described|p111|||see also Table 4.1||||||
20967|Yeringberg Formation|60599|5|Briefly described|p47 Fig. 19|Emsian|Emsian|Geological Province: Darraweit Guim Province, Melbourne Zone, Lachlan Fold Belt.||||||
20967|Yeringberg Formation|61120|5|Briefly described|pp1-4, p7. |Emsian|Late Pragian|Trilobite-bearing. Correlated (VandenBerg 1975) with Norton Gully Formation.|||Includes Seville Limestone.|Overlies Wilson Creek Shale.|Richly fossiliferous mudstone and calcareous siltstone.|
20967|Yeringberg Formation|61185|5|Briefly described|p21 Fig. 6|Emsian|Emsian|Overlies Wilson Creek Shale. Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
20967|Yeringberg Formation|64616|6|Mentioned|p385|Early Devonian|Early Devonian|Siltstones in this unit at Seville contain a diverse and abundant trilobite assemblage, contemporary with and closely comparable to that of mudstones associated with limestones in Norton Gully Sandstone at Loyola.||||||
40915|Yeronga Basalt|24177|5|Briefly described|p73|||Of the Newer Volcanics. Disconformably overlies Wild Duck Formation and unconformably overlies Castlemain Group. Maximum Thickness: 25m.||||||11-MAY-04
40915|Yeronga Basalt|60591|5|Briefly described|Map Legend|Pliocene|Miocene|Of the Newer Volcanics. Lava flow: olivine basalt; olivine, plagioclase and clinopyroxene phenocrysts; moderately vesicular.||||||
40915|Yeronga Basalt|60592|5|Briefly described|Map Legend|Pliocene|Miocene|Of the Newer Volcanics. Lava flow: olivine basalt; olivine, plagioclase and clinopyroxene phenocrysts; moderately vesicular.||||||
40915|Yeronga Basalt|60593|5|Briefly described|Map Legend|Pliocene|Miocene|Of the Newer Volcanics. Lava flow: olivine basalt; olivine, plagioclase and clinopyroxene phenocrysts; moderately vesicular.||||||
40915|Yeronga Basalt|60595|5|Briefly described|Map Legend|Pliocene|Miocene|Of the Newer Volcanics. Lava flow: olivine basalt; olivine, plagioclase and clinopyroxene phenocrysts; moderately vesicular.||||||
40915|Yeronga Basalt|60596|5|Briefly described|Map Legend|Pliocene|Miocene|Of the Newer Volcanics. Lava flow: olivine basalt; olivine, plagioclase and clinopyroxene phenocrysts; moderately vesicular.||||||
40915|Yeronga Basalt|60597|5|Briefly described|Map Legend|Pliocene|Miocene|Of the Newer Volcanics. Basaltic lava flow: high frequency, moderately magnetic response (reversely magnetised, -125 nT); low K, Th, U.||||||
40915|Yeronga Basalt|60599|2|Defined|p91|Early Pliocene|Late Miocene|Moderately weathered, variably vesicular black to grey olivine basalt: with olivine, clinopyroxene and plagioclase phenocrysts. Unconformably overlies Castlemaine Supergroup rocks; disconformable on Wild Duck Formation. Thick: at least 25m in HEATHCOTE.||||||
37795|Yeungroon Granite|23309|6|Mentioned|p448 Appendix 1|||G362, S-Type. Supersedes Yeungroon Granodiorite.||||||
37795|Yeungroon Granite|60491|4|Described|p48|Devonian|Devonian|Of the Coonooer Suite. Age: 370 +/- 1 Ma (Rb/Sr biotite). Intruded the Wescotts Granite. Intruded by the Wychitella Granite. S-type.||||||
37795|Yeungroon Granite|60492|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Coonooer Suite. Leucocratic granite: S-type, reduced; pale cream to grey; coarse grained, porphyritic; plagioclase crystals to 3cm in length; rare muscovite rich enclaves to 5cm diameter.||||||
37795|Yeungroon Granite|60493|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of the Coonooer Suite. Granite; reduced S-type; nonmagnetic; near the centre of a regional gravity low; K high, Th generally moderate, high U.||||||27-JUN-14
37795|Yeungroon Granite|66002|5|Briefly described|p6 Tb.5|||Of Coonooer Suite. G362. Defined in Bibby and Moore 1998.||||||
37795|Yeungroon Granite|68116|5|Briefly described|Appendix, Map 16.|Middle Devonian|Early Devonian||||||Leucocratic granite: S-type, reduced, pale cream to grey; coarse grained, porphyritic; plagioclase crystals to 3 cm in length; rare muscovite-rich enclaves to 5 cm diameter.|
20980|Yielima Member|35091|6|Mentioned|Table 1|||||||||
20980|Yielima Member|42966|5|Briefly described|p201|||Of Shepparton Formation. Variation on Yielima Sand Member?||||||10-NOV-08
30508|Yoke Up Creek Granite|22878|4|Described|p87|||||||||
30508|Yoke Up Creek Granite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Leucocratic granite: largely concealed, pale grey, coarse grained, massive; biotite poor||||||01-OCT-04
30508|Yoke Up Creek Granite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Leucocratic granite: largely concealed, pale grey, coarse grained, massive; biotite poor||||||01-OCT-04
30508|Yoke Up Creek Granite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Leucocratic granite: Highly magnetic (300-320 nT). High K, low Th and U.||||||06-OCT-04
30508|Yoke Up Creek Granite|23309|5|Briefly described|App1|||G18 I-Type. Supersedes Thurra Granite.||||||
30508|Yoke Up Creek Granite|68116|5|Briefly described|Appendix, Maps 37, 46.|Early Devonian|Early Devonian||||||Leucocratic granite; pale grey, coarse grained, massive; biotite-poor.|
21013|You Yangs Granite|22885|5|Briefly described|map|||||||||
21013|You Yangs Granite|23239|5|Briefly described|Table1p109, 118|Late Devonian||||||||
21013|You Yangs Granite|23269|6|Mentioned|Fig14-3.1p403|||||||||
21013|You Yangs Granite|23309|5|Briefly described|p347.|Devonian|Devonian|G277 I-Type. Age: 365+/- 18 Ma.||||||
21013|You Yangs Granite|24551|5|Briefly described|p225, 717 Table 2.4|Late Devonian|Late Devonian|Age: 365 +/- 2Ma.||||||
21013|You Yangs Granite|32001|6|Mentioned|p78|||||||||
21013|You Yangs Granite|34954|6|Mentioned|p199|||||||||
21013|You Yangs Granite|35274|6|Mentioned|p425|||||||||
21013|You Yangs Granite|35277|6|Mentioned|p98|||||||||
21013|You Yangs Granite|35290|6|Mentioned|p21|||||||||
21013|You Yangs Granite|37385|4|Described|p6|||||||||
21013|You Yangs Granite|38144|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
21013|You Yangs Granite|38159|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
21013|You Yangs Granite|41641|6|Mentioned|p168|||||||||
21013|You Yangs Granite|41868|6|Mentioned|p485|||||||||
21013|You Yangs Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
21013|You Yangs Granite|42827|5|Briefly described|p168|||||||||
21013|You Yangs Granite|43282|6|Mentioned|p74|||||||||
21013|You Yangs Granite|44197|5|Briefly described|Map Legend||Late Devonian|G277 I-type.||||||
21013|You Yangs Granite|62897|6|Mentioned|p118|Devonian|Devonian|||||||18-MAR-08
21013|You Yangs Granite|63741|6|Mentioned|p118|Devonian|Devonian|Granite. ||||||
21013|You Yangs Granite|65715|5|Briefly described|p7 Tb.4, p9, p10|||Here regarded as a senior synonym of Dog Rocks Granite. Of Tynong Suite. G277. Outcrop occurs on the edge of a large gravity low, which probably represents a larger zoned pluton.||||||
21013|You Yangs Granite|68116|5|Briefly described|Appendix, Maps 41, 50.|Late Devonian|Late Devonian||||||Hornblende granite: coarse grained, K-feldspar phyric; I-type.|
27633|Youarang Granite|22971|5|Briefly described|p 20|||||||||
27633|Youarang Granite|23309|5|Briefly described|p447 App1|||G208 S-Type.||||||27-AUG-04
27633|Youarang Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
27633|Youarang Granite|68116|5|Briefly described|Appendix, Map 18.|Late Devonian|Late Devonian||||||Biotite-cordierite granite: coarse-grained, porphyritic in both feldspars (K-feldspar to 40 mm, plagioclase to 30 mm), with miarolitic cavities and abundant tourmaline nodules.|
29196|Younger Volcanics|24038|6|Mentioned|p439|||||||||
29196|Younger Volcanics|31424|4|Described|p14|||Described from core. See also P7.||||||
29196|Younger Volcanics|36832|6|Mentioned|p185|||||||||
29196|Younger Volcanics|62370|6|Mentioned|p451, p452 Fig.4|||||||||
29196|Younger Volcanics|71277|6|Mentioned|p309 Fig.8|Quaternary|Quaternary|||||||
21037|Yowang granite|37385|6|Mentioned|p6|||Name refers to an outcrop area only.||||||
35517|Ythan Creek Rhyodacite|23309|4|Described|p165. Table 2.61|||||||||22-FEB-10
35517|Ythan Creek Rhyodacite|68116|5|Briefly described|Appendix, Map 42.|Late Devonian|Late Devonian||||||Rhyolite to rhyodacite: ignimbrite; recrystallized; contains large unbroken phenocrysts of plagioclase, small quartz, aggregates of secondary biotite in a fine devitrified groundmass; flow-banded.|
77292|Yungabulla Formation|65715|2|Defined|p17-18, p18 Tb.9, p103-108|Miocene|Miocene|Newly defined here. Of Smokers Creek Volcanic Subgroup. Overlain by Newham Diatomite. Variable lithofacies, but predominantly pyroclastics. No more than a few tens of m thick. Type section is along unnamed tributary of Deep Creek in Yungabulla property at Newham (MGA reference given).||||||
77292|Yungabulla Formation|68116|5|Briefly described|Appendix, Map 32.|Pliocene|Miocene||||||Diamictic tuff, lapilli deposits: generally dark colours; massive to bedded; lapilli and blocks of trachyte, slate, sandstone vein quartz, occasional pumice in massive ash matrix; poorly consolidated to lithified.|
74847|Yungaburra Formation|64619|5|Briefly described|Map legend|Pliocene|Miocene|Diamictic tuff, lapilli deposits; cream to pink; lapilli and blocks of trachyte, hornfels and occasionally mugearite in massive ash matrix; poorly consolidated to lithified; lapilli deposits stratified and mod'erately sorted; pyroclastic deposits.||||||30-OCT-08
21078|Zeally Limestone Member|23240|5|Briefly described|Fig11-2.1p120, 121-3|||||||||
21078|Zeally Limestone Member|30576|5|Briefly described|Table 2|||||||||
21078|Zeally Limestone Member|35276|4|Described|p235|||||||||
21078|Zeally Limestone Member|35290|6|Mentioned|p33|||||||||
21078|Zeally Limestone Member|36499|5|Briefly described|p47|||||||||
21078|Zeally Limestone Member|42318|6|Mentioned|Fig.2 P10|||||||||
21078|Zeally Limestone Member|42827|5|Briefly described|p309|||of Puebla Formation||||||
21078|Zeally Limestone Member|48911|6|Mentioned|Chart 1|||||||||
21078|Zeally Limestone Member|65687|5|Briefly described|p189, p191|Miocene|Miocene|Of the Puebla Formation (Torquay Group), NW Torquay Basin. Indicated age: late Early Miocene (p191). Restricted to the northwestern margin of the Torquay Basin. It is a 9m thick sequence of bryozoal calcarenite, including planktonic foraminifera.||||||09-MAY-11
